1984
Lipiarski, I.; Ćmiel, S. R.
The geological conditions of the occurrence of Carboniferous coal in the northwestern part of Sorkap Land in West Spitsbergen. Journal Article
In: Polish Polar Research, vol. 5, no. 3-4, pp. 255-266, 1984, ISSN: 01380338, (6).
@article{2-s2.0-0021553783,
title = {The geological conditions of the occurrence of Carboniferous coal in the northwestern part of Sorkap Land in West Spitsbergen.},
author = { I. Lipiarski and S.R. Ćmiel},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021553783&partnerID=40&md5=a3bd53d97e6290f10fdfd1d163651a1b},
issn = {01380338},
year = {1984},
date = {1984-01-01},
journal = {Polish Polar Research},
volume = {5},
number = {3-4},
pages = {255-266},
abstract = {The aim of geological investigations was to identify the presence of Carboniferous coal in the area south of Hornsund. The field investigations were carried out by the scientific expedition organized by the Institute of Geophysics of the Polish Academy of Sciences. The investigations covered the northwestern part of Sorkappland, south of Hornsund and W of the Wurmbrandegga and Wiederfjellet. -from Authors},
note = {6},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The aim of geological investigations was to identify the presence of Carboniferous coal in the area south of Hornsund. The field investigations were carried out by the scientific expedition organized by the Institute of Geophysics of the Polish Academy of Sciences. The investigations covered the northwestern part of Sorkappland, south of Hornsund and W of the Wurmbrandegga and Wiederfjellet. -from Authors
Hess, M. T.; Niedźwiedź, T.; Obrębska-Starkelowa, B.
A method of characterizing the thermal relations in mountainous areas / the lower Beskid range in the Polish Carpathians as example Journal Article
In: GeoJournal, vol. 8, no. 3, pp. 251-257, 1984, ISSN: 03432521, (3).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0021541484,
title = {A method of characterizing the thermal relations in mountainous areas / the lower Beskid range in the Polish Carpathians as example},
author = { M.T. Hess and T. Niedźwiedź and B. Obrębska-Starkelowa},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021541484&doi=10.1007%2fBF00446474&partnerID=40&md5=d34cd333cf3f06003b65b65fbe8ce938},
doi = {10.1007/BF00446474},
issn = {03432521},
year = {1984},
date = {1984-01-01},
journal = {GeoJournal},
volume = {8},
number = {3},
pages = {251-257},
publisher = {Kluwer Academic Publishers},
abstract = {The method discussed in the present paper permits the determination in detail of the mesoclimatic conditions on the basis of standard data provided by a network of a measurement stations. The passage from the data available at certain points and obtained from meteorological stations to spatial conceptions leads along the determination of the relationships between the altitude, various forms of the relief, and the thermal indices of climate. Resulting from these data, the duration of the frostless period is a sensitive index in the scale of mesoclimate, besides all the other indices connected with the minimum air temperatures. The nomographs applied by the authors make it possible to construct detailed climatic maps, which - with the maps of other elements of the geographical environment - form a basis for the elaboration e.g. an agrocological map of habitats. Presented method of the evaluation of climate conditions can be applied to all mountain territories, in which a network of measurement stations enables the determination of the interdependencies between the chosen thermal parameters and the altitude, and the distinction of the impact of the convex and concave forms. © 1984 D. Reidel Publishing Company.},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The method discussed in the present paper permits the determination in detail of the mesoclimatic conditions on the basis of standard data provided by a network of a measurement stations. The passage from the data available at certain points and obtained from meteorological stations to spatial conceptions leads along the determination of the relationships between the altitude, various forms of the relief, and the thermal indices of climate. Resulting from these data, the duration of the frostless period is a sensitive index in the scale of mesoclimate, besides all the other indices connected with the minimum air temperatures. The nomographs applied by the authors make it possible to construct detailed climatic maps, which - with the maps of other elements of the geographical environment - form a basis for the elaboration e.g. an agrocological map of habitats. Presented method of the evaluation of climate conditions can be applied to all mountain territories, in which a network of measurement stations enables the determination of the interdependencies between the chosen thermal parameters and the altitude, and the distinction of the impact of the convex and concave forms. © 1984 D. Reidel Publishing Company.
Żaba, J.
In: Geologia Sudetica, vol. 19, no. 2, pp. 89-192, 1984, ISSN: 0072100X, (11).
@article{2-s2.0-0021534801,
title = {Polish with English summary & abstract [(Genesis and metamorphic evolution of gneisses and granitoids of the Izerski Stog massif (Western Sudetes).)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021534801&partnerID=40&md5=5bab827a1dc3767fa872a45d5fb18072},
issn = {0072100X},
year = {1984},
date = {1984-01-01},
journal = {Geologia Sudetica},
volume = {19},
number = {2},
pages = {89-192},
abstract = {Geological mapping, petrographic and petrochemical studies, mineral investigation and mesostructural analysis of the little-known massif of Izerski Stog have been carried out to explain the genesis and evolution of the rocks, particularly the gneisses and granites. The evolution of these rocks has been divided into nine stages: 1) geosynclinal; 2) Barrow-type regional metamorphism; 3) recrystallization; 4) retrogressive metamorphism; 5) microclinization and pegmatization; 6) regional metasomatism; 7) faint deformation; 8) local metasomatism and 9) contact metamorphism.-R.E.S.},
note = {11},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Geological mapping, petrographic and petrochemical studies, mineral investigation and mesostructural analysis of the little-known massif of Izerski Stog have been carried out to explain the genesis and evolution of the rocks, particularly the gneisses and granites. The evolution of these rocks has been divided into nine stages: 1) geosynclinal; 2) Barrow-type regional metamorphism; 3) recrystallization; 4) retrogressive metamorphism; 5) microclinization and pegmatization; 6) regional metasomatism; 7) faint deformation; 8) local metasomatism and 9) contact metamorphism.-R.E.S.
Pulina, M.; Pereyma, J.; Kida, J.; Krawczyk, W. E.
Characteristics of the polar hydrological year 1979/1980 in the basin of the Werenskiold Glacier, SW Spitzbergen. Journal Article
In: Polish Polar Research, vol. 5, no. 3-4, pp. 165-182, 1984, ISSN: 01380338, (12).
@article{2-s2.0-0021534451,
title = {Characteristics of the polar hydrological year 1979/1980 in the basin of the Werenskiold Glacier, SW Spitzbergen.},
author = { M. Pulina and J. Pereyma and J. Kida and W.E. Krawczyk},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021534451&partnerID=40&md5=672834eb1dacf1d71470a7a147980322},
issn = {01380338},
year = {1984},
date = {1984-01-01},
journal = {Polish Polar Research},
volume = {5},
number = {3-4},
pages = {165-182},
abstract = {Contains the results of hydrological and hydrochemical investigations carried out in the basin of Werenskiold Glacier against the background of determining climate elements. It also gives chosen elements of the water balance and mass balance determined from year-long investigations of the polar hydrological year 1979-1980. -Authors},
note = {12},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Contains the results of hydrological and hydrochemical investigations carried out in the basin of Werenskiold Glacier against the background of determining climate elements. It also gives chosen elements of the water balance and mass balance determined from year-long investigations of the polar hydrological year 1979-1980. -Authors
Pulina, M.; Krawczyk, W. E.; Pereyma, J.
Water balance and chemical denudation in the unglaciated Fugleberget basin (SW Spitsbergen). Journal Article
In: Polish Polar Research, vol. 5, no. 3-4, pp. 183-205, 1984, ISSN: 01380338, (20).
@article{2-s2.0-0021532729,
title = {Water balance and chemical denudation in the unglaciated Fugleberget basin (SW Spitsbergen).},
author = { M. Pulina and W.E. Krawczyk and J. Pereyma},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021532729&partnerID=40&md5=b7475e072d5451a766f540126cc2ad71},
issn = {01380338},
year = {1984},
date = {1984-01-01},
journal = {Polish Polar Research},
volume = {5},
number = {3-4},
pages = {183-205},
abstract = {The aim of investigations was to determine such fluvial processes as the duration of the hydrological period, the manner of water supply to the basin and an attempt to define the elements of the water balance. In addition studies were made on hydrological processes, particularly changes in the chemical composition of water, and the magnitude of denudation determined. -from Authors},
note = {20},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The aim of investigations was to determine such fluvial processes as the duration of the hydrological period, the manner of water supply to the basin and an attempt to define the elements of the water balance. In addition studies were made on hydrological processes, particularly changes in the chemical composition of water, and the magnitude of denudation determined. -from Authors
Żaba, J.
Some remarks on pre-Variscan contact metamorphism of rocks of the Izera block (western Sudetes). Journal Article
In: Bulletin of the Polish Academy of Sciences: Earth Sciences, vol. 32, no. 1-4, pp. 73-80, 1984, (3).
@article{2-s2.0-0021369992,
title = {Some remarks on pre-Variscan contact metamorphism of rocks of the Izera block (western Sudetes).},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021369992&partnerID=40&md5=4098c8edcb02c16f921d5acf1930f905},
year = {1984},
date = {1984-01-01},
journal = {Bulletin of the Polish Academy of Sciences: Earth Sciences},
volume = {32},
number = {1-4},
pages = {73-80},
abstract = {The Polish pre-Variscan contact metamorphism caused by intrusions of palingenetic magma in mantle rocks approx 500-450 m.y. ago probably occurred in the K-feldspar-cordierite hornfels facies at 635o-655oC (locally up to 695oC) with PH2O approx 2.5 kbar at a depth of approx 9-10 km.-R.A.H.},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Polish pre-Variscan contact metamorphism caused by intrusions of palingenetic magma in mantle rocks approx 500-450 m.y. ago probably occurred in the K-feldspar-cordierite hornfels facies at 635o-655oC (locally up to 695oC) with PH2O approx 2.5 kbar at a depth of approx 9-10 km.-R.A.H.
Sawicka, T. J.; Łaszczyca, P.; Smylla, B.; Jethon, Z.
Metabolic adaptation of muscles to exercise, vibration and raised temperature under the influence of cernitins Journal Article
In: Acta Physiologica Polonica, vol. 35, no. 2, pp. 141-150, 1984, ISSN: 00446033.
@article{2-s2.0-0021628753,
title = {Metabolic adaptation of muscles to exercise, vibration and raised temperature under the influence of cernitins},
author = { T.J. Sawicka and P. Łaszczyca and B. Smylla and Z. Jethon},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021628753&partnerID=40&md5=5edd5c3a8cccb091b90f81376149a569},
issn = {00446033},
year = {1984},
date = {1984-01-01},
journal = {Acta Physiologica Polonica},
volume = {35},
number = {2},
pages = {141-150},
abstract = {Wistar rats were used to study the effects of cernitins, i.e. aqueous and oil extracts or pollens, on the metabolic adaptation of the soleus muscle to exercise, vibration and raised ambient temperature. The animals were exposed to selected combinations of these factors for 5 days during 1.5 hour daily. A part of the animals was given orally cernitins in daily doses of 6 mg/kg of body weight for 10 days before the exposure. Among the adaptation changes studied in the soleus muscle, 24 hours after the last exposure, cernitins caused: 1) a reduction of the amount of total protein, 2) an increase in the proportion of soluble proteins in the protein fraction, 3) an increase in the tissue oxygen consumption, 4) an increase of already elevated pyruvate kinase activity, 5) a further rise in ATP level, 6) an increase in lactic dehydrogenase activity, 7) a rise in the activity of cholinesterases. Moreover, it increased significantly the body weight and the weight of the studied soleus muscle. Cernitins, in combination with certain types of exposure used in this experiment, exerted a catabolic action, increased the rate of anaerobic metabolism and enhanced adaptation to exercise, vibration and temperature. The direction of the adaptation changes depended on the type of exposure to environmental factors.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Wistar rats were used to study the effects of cernitins, i.e. aqueous and oil extracts or pollens, on the metabolic adaptation of the soleus muscle to exercise, vibration and raised ambient temperature. The animals were exposed to selected combinations of these factors for 5 days during 1.5 hour daily. A part of the animals was given orally cernitins in daily doses of 6 mg/kg of body weight for 10 days before the exposure. Among the adaptation changes studied in the soleus muscle, 24 hours after the last exposure, cernitins caused: 1) a reduction of the amount of total protein, 2) an increase in the proportion of soluble proteins in the protein fraction, 3) an increase in the tissue oxygen consumption, 4) an increase of already elevated pyruvate kinase activity, 5) a further rise in ATP level, 6) an increase in lactic dehydrogenase activity, 7) a rise in the activity of cholinesterases. Moreover, it increased significantly the body weight and the weight of the studied soleus muscle. Cernitins, in combination with certain types of exposure used in this experiment, exerted a catabolic action, increased the rate of anaerobic metabolism and enhanced adaptation to exercise, vibration and temperature. The direction of the adaptation changes depended on the type of exposure to environmental factors.
Hejnowicz, Z.; Nakielski, J.; Hejnowicz, K.
Modeling of spatial variations of growth within apical domes by means of the growth tensor. II. Growth specified on dome surface Journal Article
In: Acta Societatis Botanicorum Poloniae, vol. 53, no. 3, pp. 301-316, 1984, ISSN: 00016977, (18).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-84989235554,
title = {Modeling of spatial variations of growth within apical domes by means of the growth tensor. II. Growth specified on dome surface},
author = { Z. Hejnowicz and J. Nakielski and K. Hejnowicz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84989235554&doi=10.5586%2fasbp.1984.027&partnerID=40&md5=849b0bb82b866d74b1eaf0c9ff82feff},
doi = {10.5586/asbp.1984.027},
issn = {00016977},
year = {1984},
date = {1984-01-01},
journal = {Acta Societatis Botanicorum Poloniae},
volume = {53},
number = {3},
pages = {301-316},
publisher = {Polskie Towarzystwo Botaniczne},
abstract = {Variations of the elemental relative rate of growth are modeled for parabolic, elliptic and hyperbolic domes of shoot apices by using the growth tensor in a suitable curvilinear coordinate system when the mode of area growth on the dome surface is known. Variations of growth rates within the domes are obtained in forms of computer-made maps for the following variants of growth on the dome surface: (1) constant meridional growth rate, (2) isotropic area growth, (3) anisotropy of area growth which becomes more intensive with increasing distance from the vertex. In variants 1 and 2 a maximum of volumetric growth rate appears in the center of the dome. Such a distribution of growth seems to be unrealistic. However, the corresponding growth tensors are interesting because they can be used in combination with other growth tensors to get the expected minimum volumetric growth rate in the dome center.},
note = {18},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Variations of the elemental relative rate of growth are modeled for parabolic, elliptic and hyperbolic domes of shoot apices by using the growth tensor in a suitable curvilinear coordinate system when the mode of area growth on the dome surface is known. Variations of growth rates within the domes are obtained in forms of computer-made maps for the following variants of growth on the dome surface: (1) constant meridional growth rate, (2) isotropic area growth, (3) anisotropy of area growth which becomes more intensive with increasing distance from the vertex. In variants 1 and 2 a maximum of volumetric growth rate appears in the center of the dome. Such a distribution of growth seems to be unrealistic. However, the corresponding growth tensors are interesting because they can be used in combination with other growth tensors to get the expected minimum volumetric growth rate in the dome center.
Duber, S.; Więckowski, A. B.
Excited triplet states in bituminous coal Journal Article
In: Fuel, vol. 63, no. 10, pp. 1474-1475, 1984, ISSN: 00162361, (14).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0041096263,
title = {Excited triplet states in bituminous coal},
author = { S. Duber and A.B. Więckowski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0041096263&doi=10.1016%2f0016-2361%2884%2990363-6&partnerID=40&md5=a0242257eb6d666297545e1522ed29fd},
doi = {10.1016/0016-2361(84)90363-6},
issn = {00162361},
year = {1984},
date = {1984-01-01},
journal = {Fuel},
volume = {63},
number = {10},
pages = {1474-1475},
abstract = {The intensities of the broad and narrow lines constituting the e.p.r. spectrum of coal depend on the temperature of measurement. The system of paramagnetic centres related to the broad line does not obey the Curie law and consists of free radicals (S = 1 2) and of centres with singlet ground state (S = 0) and lowest-excited triplet state (S = 1). The singlet-triplet excitation energy, J, is comparable with thermal energy, kT, of lattice vibrations. The system of paramagnetic centres related to the narrow line obeys the Curie law (S = 1 2). © 1984.},
note = {14},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The intensities of the broad and narrow lines constituting the e.p.r. spectrum of coal depend on the temperature of measurement. The system of paramagnetic centres related to the broad line does not obey the Curie law and consists of free radicals (S = 1 2) and of centres with singlet ground state (S = 0) and lowest-excited triplet state (S = 1). The singlet-triplet excitation energy, J, is comparable with thermal energy, kT, of lattice vibrations. The system of paramagnetic centres related to the narrow line obeys the Curie law (S = 1 2). © 1984.
Duber, S.; Więckowski, A. B.
Effects of organic solvents on the EPR spectrum of coal Journal Article
In: Fuel, vol. 63, no. 12, pp. 1641-1644, 1984, ISSN: 00162361, (21).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0021616904,
title = {Effects of organic solvents on the EPR spectrum of coal},
author = { S. Duber and A.B. Więckowski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021616904&doi=10.1016%2f0016-2361%2884%2990092-9&partnerID=40&md5=deefbc28793b00395331b144d29f6ad7},
doi = {10.1016/0016-2361(84)90092-9},
issn = {00162361},
year = {1984},
date = {1984-01-01},
journal = {Fuel},
volume = {63},
number = {12},
pages = {1641-1644},
abstract = {EPR studies have been carried out on coal and the products of its extraction with ethylenediamine, pyridine and tetrahydrofuran. The spectrum of the coal and the residue after extraction consisted of two lines. In the case of the extraction residue the width of the narrow line remains practically unchanged compared to the initial coal whereas that of the broad component decreases. The extracts exhibit a single line with a width close to that of the broad component from the extraction residue. The concentration of paramagnetic centres in the residue and extracts is lower than in the coal. The decrease in concentration is higher when the extraction yield obtained with the solvent is higher. Quenching of paramagnetic centres is found to be related to the destruction of intermolecular bonds of the donor-acceptor type in the coal. © 1984.},
note = {21},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
EPR studies have been carried out on coal and the products of its extraction with ethylenediamine, pyridine and tetrahydrofuran. The spectrum of the coal and the residue after extraction consisted of two lines. In the case of the extraction residue the width of the narrow line remains practically unchanged compared to the initial coal whereas that of the broad component decreases. The extracts exhibit a single line with a width close to that of the broad component from the extraction residue. The concentration of paramagnetic centres in the residue and extracts is lower than in the coal. The decrease in concentration is higher when the extraction yield obtained with the solvent is higher. Quenching of paramagnetic centres is found to be related to the destruction of intermolecular bonds of the donor-acceptor type in the coal. © 1984.
Narkiewicz, M.; Racki, G.
(Stratigraphy of the Devonian of the Debnik anticline). [Stratigrafia dewonu antykliny Debnika.] Journal Article
In: Kwartalnik Geologiczny, vol. 28, no. 3-4, pp. 513-546, 1984, ISSN: 00235873, (24).
@article{2-s2.0-0021568410,
title = {(Stratigraphy of the Devonian of the Debnik anticline). [Stratigrafia dewonu antykliny Debnika.]},
author = { M. Narkiewicz and G. Racki},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021568410&partnerID=40&md5=843cf8cf02daa77fea4a8c5ecc925546},
issn = {00235873},
year = {1984},
date = {1984-01-01},
journal = {Kwartalnik Geologiczny},
volume = {28},
number = {3-4},
pages = {513-546},
abstract = {The Devonian and Carboniferous carbonates outcropping near Debnik in southern Poland form a unique reference section which is important for detailed correlations with similar deposits covered by the Carpathian nappes and underlying the Upper Silesian Coal Basin. Basing on the cored borings and on outcrops six informal lithostratigraphic units have been described representing the Devonian sequence of this area (from base to top): 1) Zbrza Dolostone - thickness over 260 m. 2) Debnik Limestone - 35 m. 3) Nodular Limestone - 28 m. 4) Grained Limestone - over 34 m. 5) Platy Limestone - over 70 m. 6) Grained and Micritic Limestone - thickness unknown. The described carbonates rest discordantly on the quartz porphyry intrusion of the post-Devonian age. Their upper boundary is unknown and overlying Lower Carboniferous strata are developed in highly comparable carbonate platform lithofacies. The lack of key fossils precludes dating of the basal part of the profile. The lowermost biostratigraphic data were obtained from near the contact of the Zbrza Dolostones with the Debnik Limestone. They point to the Givetian age, just below the Polygnathus asymmetricus conodont Zone. Basing on the conodonts the Givetian/Frasnian boundary corresponds more or less to a lithologic transition between the Debnik Lst. and the Nodular Lst. The Frasnian/Famennian boundary runs within the Platy Lst. unit. The youngest conodont fauna found within the lower Grained and Micritic Lst. unit corresponds to the crepida- rhomboidea Zones of the standard conodont division. English summary},
note = {24},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Devonian and Carboniferous carbonates outcropping near Debnik in southern Poland form a unique reference section which is important for detailed correlations with similar deposits covered by the Carpathian nappes and underlying the Upper Silesian Coal Basin. Basing on the cored borings and on outcrops six informal lithostratigraphic units have been described representing the Devonian sequence of this area (from base to top): 1) Zbrza Dolostone - thickness over 260 m. 2) Debnik Limestone - 35 m. 3) Nodular Limestone - 28 m. 4) Grained Limestone - over 34 m. 5) Platy Limestone - over 70 m. 6) Grained and Micritic Limestone - thickness unknown. The described carbonates rest discordantly on the quartz porphyry intrusion of the post-Devonian age. Their upper boundary is unknown and overlying Lower Carboniferous strata are developed in highly comparable carbonate platform lithofacies. The lack of key fossils precludes dating of the basal part of the profile. The lowermost biostratigraphic data were obtained from near the contact of the Zbrza Dolostones with the Debnik Limestone. They point to the Givetian age, just below the Polygnathus asymmetricus conodont Zone. Basing on the conodonts the Givetian/Frasnian boundary corresponds more or less to a lithologic transition between the Debnik Lst. and the Nodular Lst. The Frasnian/Famennian boundary runs within the Platy Lst. unit. The youngest conodont fauna found within the lower Grained and Micritic Lst. unit corresponds to the crepida- rhomboidea Zones of the standard conodont division. English summary
1983
Janeczek, J.
Polish with English summary [(Transformations of minerals in pegmatites from Strzegom Lower Silesia.)] Journal Article
In: Archiwum Mineralogiczne, Polska Akademia Nauk, vol. 39, no. 1, pp. 39-51, 1983, (2).
@article{2-s2.0-0021060250,
title = {Polish with English summary [(Transformations of minerals in pegmatites from Strzegom Lower Silesia.)]},
author = { J. Janeczek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021060250&partnerID=40&md5=4fcac0ac782108a68b82d5ad6c060625},
year = {1983},
date = {1983-01-01},
journal = {Archiwum Mineralogiczne, Polska Akademia Nauk},
volume = {39},
number = {1},
pages = {39-51},
abstract = {A transformation sequence of iron-bearing sheet-silicates is reported from miarolitic pegmatites in granitic rocks near Strzegom: lepidomelane rt arrow Fe-chlorite rt arrow stilpnomelane rt arrow Fe-celadonite (but zinnwaldite, ferrostilpnomelane and ferristilpnomelane also develop). Mention is also made of the development of laumontite from K-feldspar and recognition of pseudomorphs of fluorite after apophyllite.-R.A.H.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
A transformation sequence of iron-bearing sheet-silicates is reported from miarolitic pegmatites in granitic rocks near Strzegom: lepidomelane rt arrow Fe-chlorite rt arrow stilpnomelane rt arrow Fe-celadonite (but zinnwaldite, ferrostilpnomelane and ferristilpnomelane also develop). Mention is also made of the development of laumontite from K-feldspar and recognition of pseudomorphs of fluorite after apophyllite.-R.A.H.
Karwowski, Ł.; Włodyka, R.; Kurdziel, M.
Polish with English abstract [(Conditions of formation of druse minerals from Michalowice (Karkonosze Massif-southwestern Poland).)] Journal Article
In: Archiwum Mineralogiczne, vol. 39, no. 1, pp. 29-37, 1983, (4).
@article{2-s2.0-0021056738,
title = {Polish with English abstract [(Conditions of formation of druse minerals from Michalowice (Karkonosze Massif-southwestern Poland).)]},
author = { Ł. Karwowski and R. Włodyka and M. Kurdziel},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021056738&partnerID=40&md5=97cf095a8513dba6ab8cedc888d533ac},
year = {1983},
date = {1983-01-01},
journal = {Archiwum Mineralogiczne},
volume = {39},
number = {1},
pages = {29-37},
abstract = {Crystallization of quartz, albite, cleavelandite, sphene, fluorite, epidote and calcite from pneumatolytic fluid began at >500oC and continued at approx 450oC and 85-80 MPa to 100oC and 50 MPa. -R.A.H.},
note = {4},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Crystallization of quartz, albite, cleavelandite, sphene, fluorite, epidote and calcite from pneumatolytic fluid began at >500oC and continued at approx 450oC and 85-80 MPa to 100oC and 50 MPa. -R.A.H.
Włodyka, R.; Karwowski, Ł.; Bzowski, Z.
Polish with English summary [(Beryl-bearing pegmatite from the environs of Jakuszyce (Karkonosze Mts).)] Journal Article
In: Archiwum Mineralogiczne, vol. 39, no. 1, pp. 17-28, 1983, (2).
@article{2-s2.0-0021052445,
title = {Polish with English summary [(Beryl-bearing pegmatite from the environs of Jakuszyce (Karkonosze Mts).)]},
author = { R. Włodyka and Ł. Karwowski and Z. Bzowski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021052445&partnerID=40&md5=1701556e9a98ea568d46b8d0110a4546},
year = {1983},
date = {1983-01-01},
journal = {Archiwum Mineralogiczne},
volume = {39},
number = {1},
pages = {17-28},
abstract = {A pegmatitic vein concordant with horizontal fractures in the host granite near Jakuszyce contains K-feldspar, plagioclase, quartz, tourmaline, beryl, biotite, muscovite, magnetite and pyrite. A study of fluid inclusions indicates that crystallization started at approx 500oC, P approx 82 MPa. A later albitization stage developed at 400-300oC with P down to 60 MPa, resulting in the albite-muscovite-quartz paragenesis. In the final stage of pegmatite formation, beryl, tourmaline and quartz crystallized down to approx 100oC and 47 MPa. IR absorption spectra are given for beryl, tourmaline, microcline, albite and magnetite.-R.A.H.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
A pegmatitic vein concordant with horizontal fractures in the host granite near Jakuszyce contains K-feldspar, plagioclase, quartz, tourmaline, beryl, biotite, muscovite, magnetite and pyrite. A study of fluid inclusions indicates that crystallization started at approx 500oC, P approx 82 MPa. A later albitization stage developed at 400-300oC with P down to 60 MPa, resulting in the albite-muscovite-quartz paragenesis. In the final stage of pegmatite formation, beryl, tourmaline and quartz crystallized down to approx 100oC and 47 MPa. IR absorption spectra are given for beryl, tourmaline, microcline, albite and magnetite.-R.A.H.
Zuberek, W. M.
In: Acta Geophysica Polonica, vol. 31, no. 4, pp. 343-354, 1983, ISSN: 00015725.
@article{2-s2.0-0020869056,
title = {Probabilistic interpretation of the frequency- energy distribution of seismic activity and of the amplitude distribution of seismoacoustic activity ( Poland).},
author = { W.M. Zuberek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020869056&partnerID=40&md5=1729b98daa5f32ead3f20f8c582cd457},
issn = {00015725},
year = {1983},
date = {1983-01-01},
journal = {Acta Geophysica Polonica},
volume = {31},
number = {4},
pages = {343-354},
abstract = {Tries to explain the frequency-energy distribution of seimsic activity and the amplitude distribution of seismoacoustic activity using the extreme value theory. A good accordance of the energy distribution of mining tremors recorded in the Upper Silesian Coal Basin in the period of 1977-1980 with the second asymptotic distribution of maximum values was found. The estimation of the distribution parameters allows to calculate the probability of tremor occurrence in the range of high seismic energies.-Author},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Tries to explain the frequency-energy distribution of seimsic activity and the amplitude distribution of seismoacoustic activity using the extreme value theory. A good accordance of the energy distribution of mining tremors recorded in the Upper Silesian Coal Basin in the period of 1977-1980 with the second asymptotic distribution of maximum values was found. The estimation of the distribution parameters allows to calculate the probability of tremor occurrence in the range of high seismic energies.-Author
Czaja, M. B.
The occurrence of mixed-layer chlorite/vermiculite at Lubiechowa (the Kaczawskie Mts.). Journal Article
In: Mineralogia Polonica, vol. 14, no. 1-2, pp. 67-74, 1983.
@article{2-s2.0-0020866536,
title = {The occurrence of mixed-layer chlorite/vermiculite at Lubiechowa (the Kaczawskie Mts.).},
author = { M.B. Czaja},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020866536&partnerID=40&md5=994f27fd9f8923e60c87c98be9e7ea96},
year = {1983},
date = {1983-01-01},
journal = {Mineralogia Polonica},
volume = {14},
number = {1-2},
pages = {67-74},
abstract = {One of the clay minerals filling vesicles in melaphyres at Lubiechowa was subjected to various treatments involving saturation with Mg and K ions and treatment with ethylene glycol and glycerol. It was found that the mineral consists of chlorite and mixed-layer chlorite/vermiculite. Using Mering's method it is shown that two types of structure are present: the chlorite content is 80% in one type and approx 30% in the other. The effect of acetic acid treatment on the layers making up the structure of the mineral was also studied.-P.Br.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
One of the clay minerals filling vesicles in melaphyres at Lubiechowa was subjected to various treatments involving saturation with Mg and K ions and treatment with ethylene glycol and glycerol. It was found that the mineral consists of chlorite and mixed-layer chlorite/vermiculite. Using Mering's method it is shown that two types of structure are present: the chlorite content is 80% in one type and approx 30% in the other. The effect of acetic acid treatment on the layers making up the structure of the mineral was also studied.-P.Br.
Kozlowski, K.; Żaba, J.
Clinopyroxenes in skarn from the vicinity of Glucholazy (Eastern Sudetes). Journal Article
In: Bulletin of the Polish Academy of Sciences, Earth Sciences, vol. 31, no. 1-4, pp. 79-87, 1983, ISSN: 02397277.
@article{2-s2.0-0020859951,
title = {Clinopyroxenes in skarn from the vicinity of Glucholazy (Eastern Sudetes).},
author = { K. Kozlowski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020859951&partnerID=40&md5=b1654e5e6ddba0a444b73fd90d5861fa},
issn = {02397277},
year = {1983},
date = {1983-01-01},
journal = {Bulletin of the Polish Academy of Sciences, Earth Sciences},
volume = {31},
number = {1-4},
pages = {79-87},
abstract = {Clinopyroxene crystals from this skarn have been analysed and found to contain diopside 73.70%, hedenbergite 22.33%, tschermakite 2.98% and acmite 0.99%. The optical properties are alpha 1.680, beta 1.685, gamma 1.704, gamma :c 40o. The diffractogram of this mineral indicates a pyroxene close to diopside with reflections shifted towards higher d-values. Fibrous amphiboles in the skarn belong to the tremolite-actinolite series and were formed as a result of secondary alterations of clinopyroxenes.-R.E.S.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Clinopyroxene crystals from this skarn have been analysed and found to contain diopside 73.70%, hedenbergite 22.33%, tschermakite 2.98% and acmite 0.99%. The optical properties are alpha 1.680, beta 1.685, gamma 1.704, gamma :c 40o. The diffractogram of this mineral indicates a pyroxene close to diopside with reflections shifted towards higher d-values. Fibrous amphiboles in the skarn belong to the tremolite-actinolite series and were formed as a result of secondary alterations of clinopyroxenes.-R.E.S.
1982
Żaba, J.
Polish with English summary [(Proposed classification and nomenclature of the gneisses and granites of the Izera block (western Sudetes.)] Journal Article
In: Geologia Sudetica, vol. 17, no. 1-2, pp. 141-154, 1982, ISSN: 0072100X, (6).
@article{2-s2.0-0020387711,
title = {Polish with English summary [(Proposed classification and nomenclature of the gneisses and granites of the Izera block (western Sudetes.)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020387711&partnerID=40&md5=80851e36e622844e6edb89bb1775a405},
issn = {0072100X},
year = {1982},
date = {1982-01-01},
journal = {Geologia Sudetica},
volume = {17},
number = {1-2},
pages = {141-154},
abstract = {This classification of the gneisses and granites of this part of the Czech-Polish Sudetes Mts is based on the rock structures and colour index, but also includes grain size and size ratios between grains of individual rock-forming minerals. Rocks with directional structures are sub-divided into laminated, flaser-type and granite gneisses.-R.A.H.},
note = {6},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This classification of the gneisses and granites of this part of the Czech-Polish Sudetes Mts is based on the rock structures and colour index, but also includes grain size and size ratios between grains of individual rock-forming minerals. Rocks with directional structures are sub-divided into laminated, flaser-type and granite gneisses.-R.A.H.
Teper, L.; Teper, E.
Polish with English abstract [(The origin of tin-bearing garnet schists in the Izere Mts. (West Sudetes, Poland).)] Journal Article
In: Rudy i Metale Niezelazne, vol. 27, no. 9, pp. 420-422, 1982, ISSN: 00359696, (1).
@article{2-s2.0-0019911901,
title = {Polish with English abstract [(The origin of tin-bearing garnet schists in the Izere Mts. (West Sudetes, Poland).)]},
author = { L. Teper and E. Teper},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019911901&partnerID=40&md5=eb5969340a865494abbd708ed12428f2},
issn = {00359696},
year = {1982},
date = {1982-01-01},
journal = {Rudy i Metale Niezelazne},
volume = {27},
number = {9},
pages = {420-422},
abstract = {On the basis of a structural analysis in tin-bearing areas of the West Sudetes, it is reported that the garnetiferous schists occur along axial surfaces in the anticlinal cores of isolated macrofolds and are of tectonic origin. The tin deposit has an epitectonic nature and is genetically related to the Variscan Karkonose granitic rocks. -R.A.H.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
On the basis of a structural analysis in tin-bearing areas of the West Sudetes, it is reported that the garnetiferous schists occur along axial surfaces in the anticlinal cores of isolated macrofolds and are of tectonic origin. The tin deposit has an epitectonic nature and is genetically related to the Variscan Karkonose granitic rocks. -R.A.H.
Duber, S.; Więckowski, A. B.
E.p.r. study of molecular phases in coal Journal Article
In: Fuel, vol. 61, no. 5, pp. 433-436, 1982, ISSN: 00162361, (45).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0000277205,
title = {E.p.r. study of molecular phases in coal},
author = { S. Duber and A.B. Więckowski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0000277205&doi=10.1016%2f0016-2361%2882%2990067-9&partnerID=40&md5=a3e68fffa1f52de3378fc83ca8395261},
doi = {10.1016/0016-2361(82)90067-9},
issn = {00162361},
year = {1982},
date = {1982-01-01},
journal = {Fuel},
volume = {61},
number = {5},
pages = {433-436},
abstract = {E.p.r. spectra from coals of various carbon content are reported. The e.p.r. signal from coals in a vacuum consists of two lines with different widths. The results are interpreted using the Larsen-Kovac structural model (Am. Chem. Soc. Div. Fuel Chem. Preprints 1977, 22, 181). The paramagnetic centres, disposed in the macromolecular phase, give a narrow line whereas the spins of the molecular phase are responsible for the broad line. These results provide a good interpretation of the changes in e.p.r. signal-shape under the influence of various organic solvents observed by Yokokawa (Fuel 1968, 47, 273; Fuel 1969, 48, 29). © 1982.},
note = {45},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
E.p.r. spectra from coals of various carbon content are reported. The e.p.r. signal from coals in a vacuum consists of two lines with different widths. The results are interpreted using the Larsen-Kovac structural model (Am. Chem. Soc. Div. Fuel Chem. Preprints 1977, 22, 181). The paramagnetic centres, disposed in the macromolecular phase, give a narrow line whereas the spins of the molecular phase are responsible for the broad line. These results provide a good interpretation of the changes in e.p.r. signal-shape under the influence of various organic solvents observed by Yokokawa (Fuel 1968, 47, 273; Fuel 1969, 48, 29). © 1982.
1981
Artukh, A. G.; Gridnev, G. F.; Gruszecki, M.; Karcz, W.; Mezentsev, A. N.; Mikheev, V. L.; Pomorski, L.; Popescu, A.; Popescu, D. G.; Volkov, V. V.
Multi-nucleon transfer reactions and the formation of light charged particles in the systemnatAg+40Ar (285 MeV) Journal Article
In: Zeitschrift für Physik A Atoms and Nuclei, vol. 303, no. 1, pp. 41-49, 1981, ISSN: 03402193, (8).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-34147119838,
title = {Multi-nucleon transfer reactions and the formation of light charged particles in the systemnatAg+40Ar (285 MeV)},
author = { A.G. Artukh and G.F. Gridnev and M. Gruszecki and W. Karcz and A.N. Mezentsev and V.L. Mikheev and L. Pomorski and A. Popescu and D.G. Popescu and V.V. Volkov},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-34147119838&doi=10.1007%2fBF01420009&partnerID=40&md5=8d1ccce74d3f156f57644e9d069ab0d0},
doi = {10.1007/BF01420009},
issn = {03402193},
year = {1981},
date = {1981-01-01},
journal = {Zeitschrift für Physik A Atoms and Nuclei},
volume = {303},
number = {1},
pages = {41-49},
publisher = {Springer-Verlag},
abstract = {In the reactionnatAg+40Ar (285 MeV) there have been measured the energy spectra of the isotopes of elements from H to Cl at an emission angle of 40°, the energy spectra and angular distributions of1H,2H,3H, and4He, and the angular distributions of Li, Be, B, and C. The contribution from multinucleon transfer reactions to the formation of light charged particles is discussed. © 1981 Springer-Verlag.},
note = {8},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
In the reactionnatAg+40Ar (285 MeV) there have been measured the energy spectra of the isotopes of elements from H to Cl at an emission angle of 40°, the energy spectra and angular distributions of1H,2H,3H, and4He, and the angular distributions of Li, Be, B, and C. The contribution from multinucleon transfer reactions to the formation of light charged particles is discussed. © 1981 Springer-Verlag.
Jura, D.; Trzepierczyński, J.
( Textural features of Quaternary deposits in the Gozdnica region). [Cechy teksturalne osadow czwatorzedowych rejonu Gozdnicy.] Journal Article
In: Kwartalnik Geologiczny, vol. 25, no. 2, pp. 387-397, 1981, ISSN: 00235873.
@article{2-s2.0-0019869654,
title = {( Textural features of Quaternary deposits in the Gozdnica region). [Cechy teksturalne osadow czwatorzedowych rejonu Gozdnicy.]},
author = { D. Jura and J. Trzepierczyński},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019869654&partnerID=40&md5=0bd08620732759ba63e3cc4ed87d0015},
issn = {00235873},
year = {1981},
date = {1981-01-01},
journal = {Kwartalnik Geologiczny},
volume = {25},
number = {2},
pages = {387-397},
abstract = {Geological units differentiated in the course of geological mapping are characterized on the basis of 150 granulometric analyses. For example, till from southern Gozdnica region is sandy-gravel, with polymodal grain-size distribution and it represents bottom moraine, whereas that from the northern region is sandy, with unimodal, flattened grain-size distribution. Three granulometric types of fluvioglacial sands and gravels are differentiated. Sands and muds of the Kwisa ancient valley are characterized by symmetrically steep distributions with modal class of 2phi. The methods of granulometric analyses appeared insufficiently sensitive to show differences in origin of deposits made similar to one another by repeated reworking under different sedimentary conditions in the Gozdnica area. -from English summary},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Geological units differentiated in the course of geological mapping are characterized on the basis of 150 granulometric analyses. For example, till from southern Gozdnica region is sandy-gravel, with polymodal grain-size distribution and it represents bottom moraine, whereas that from the northern region is sandy, with unimodal, flattened grain-size distribution. Three granulometric types of fluvioglacial sands and gravels are differentiated. Sands and muds of the Kwisa ancient valley are characterized by symmetrically steep distributions with modal class of 2phi. The methods of granulometric analyses appeared insufficiently sensitive to show differences in origin of deposits made similar to one another by repeated reworking under different sedimentary conditions in the Gozdnica area. -from English summary
Niedźwiedź, T.
In: Dokumentacja Geograficzna, vol. 3, pp. 22-42, 1981, ISSN: 00125032.
@article{2-s2.0-0019749508,
title = {(Natural conditions of the Homerka catchment basin and its surroundings: climate, Bedkid Sadecki)). [Warunki naturalne zlewni Homerki i jej otoczenia: klimat.]},
author = { T. Niedźwiedź},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019749508&partnerID=40&md5=19b12972184dedac14b2095bbc386c4d},
issn = {00125032},
year = {1981},
date = {1981-01-01},
journal = {Dokumentacja Geograficzna},
volume = {3},
pages = {22-42},
abstract = {The study presents temporal and areal differentiation of air temperature, precipitation and snow cover in the Kamienica Nawojowska catchment basin in the northeastern part of the Beskid Sadecki. -from English summary},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The study presents temporal and areal differentiation of air temperature, precipitation and snow cover in the Kamienica Nawojowska catchment basin in the northeastern part of the Beskid Sadecki. -from English summary
Furmanczyk, K.; Jania, J. A.
(Remote sensing methods in polar researches). [Metody teledetekcji w badaniach polarnych.] Journal Article
In: Czasopismo Geograficzne, vol. 52, no. 4, pp. 379-396, 1981, ISSN: 00459453.
@article{2-s2.0-0019738027,
title = {(Remote sensing methods in polar researches). [Metody teledetekcji w badaniach polarnych.]},
author = { K. Furmanczyk and J.A. Jania},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019738027&partnerID=40&md5=53513c180c695c6a5bfa56191c67891f},
issn = {00459453},
year = {1981},
date = {1981-01-01},
journal = {Czasopismo Geograficzne},
volume = {52},
number = {4},
pages = {379-396},
abstract = {We distinguish some characteristic stages in the development of remote sensing in polar research.-from English summary},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
We distinguish some characteristic stages in the development of remote sensing in polar research.-from English summary
Niedźwiedź, T.; Obrebska-Starklowa, B.; Suchanek, R.
In: Studia Osrodka Dokumentacji Fizjograficznej, vol. 8, pp. 17-44, 1981, ISSN: 01372939.
@article{2-s2.0-0019734431,
title = {(The climate and microclimate of the ' Gora Chelm' preserve near Zawiercie, Poland). [Klimat i mikroklimat rezerwatu 'Gora Chelm' kolo Zawiercia.]},
author = { T. Niedźwiedź and B. Obrebska-Starklowa and R. Suchanek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019734431&partnerID=40&md5=d19110e9e973e73c999f76f88ae198ec},
issn = {01372939},
year = {1981},
date = {1981-01-01},
journal = {Studia Osrodka Dokumentacji Fizjograficznej},
volume = {8},
pages = {17-44},
abstract = {The environs of the 'Gora Chelm' nature preserve belong to those least investigated with respect to climate, for which the lack of meteorological stations in its environment is responsible. The area is classed as Section D1-Silesia-Cracow, and is characterized by the type of climate of the Polish central uplands. The mean values of the particular elements and indices of climate are given. -from English summary},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The environs of the 'Gora Chelm' nature preserve belong to those least investigated with respect to climate, for which the lack of meteorological stations in its environment is responsible. The area is classed as Section D1-Silesia-Cracow, and is characterized by the type of climate of the Polish central uplands. The mean values of the particular elements and indices of climate are given. -from English summary
Karwowski, Ł.; Włodyka, R.
Stannite in the cassiterite-sulfide deposits of the Izera Mts (Sudetes). Journal Article
In: Acta Geologica Polonica, vol. 31, no. 1-2, pp. 41-47, 1981, ISSN: 00015709, (4).
@article{2-s2.0-0019715654,
title = {Stannite in the cassiterite-sulfide deposits of the Izera Mts (Sudetes).},
author = { Ł. Karwowski and R. Włodyka},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019715654&partnerID=40&md5=a2f85b305fd00d4a0b48d2124c3ed1fd},
issn = {00015709},
year = {1981},
date = {1981-01-01},
journal = {Acta Geologica Polonica},
volume = {31},
number = {1-2},
pages = {41-47},
abstract = {Stannite is reported in association with chalcopyrite, sphalerite, pyrrhotite and other sulphides in the cassiterite-sulphide deposits of the Kamienica range (Izera Mts.). It is grey with an olive-green tint; bireflectivity distinct in oil but rarely visible in air. Electron microprobe analysis for stannite from Gierczyn gave Sn 27.99, Cu 29.61, Fe 12.94, S 28.47, = 99.01, i.e. very close to the ideal composition Cu2FeSnS4. Newly recognized post-sulphide cassiterite was probably formed by stannite decomposition. The occurrence of stannite confirms the hydrothermal origin of the cassiterite-sulphide mineralization of the Izera Mts. -R.A.H.},
note = {4},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Stannite is reported in association with chalcopyrite, sphalerite, pyrrhotite and other sulphides in the cassiterite-sulphide deposits of the Kamienica range (Izera Mts.). It is grey with an olive-green tint; bireflectivity distinct in oil but rarely visible in air. Electron microprobe analysis for stannite from Gierczyn gave Sn 27.99, Cu 29.61, Fe 12.94, S 28.47, = 99.01, i.e. very close to the ideal composition Cu2FeSnS4. Newly recognized post-sulphide cassiterite was probably formed by stannite decomposition. The occurrence of stannite confirms the hydrothermal origin of the cassiterite-sulphide mineralization of the Izera Mts. -R.A.H.
1980
Brzezniak, E.; Niedźwiedź, T.
Vertical variability of climatic conditions in the Khangai Mountains ( Mongolia). Journal Article
In: Prace Geograficzne, Instytut Geografii i Przestrzennego Zagospodarowania PAN, vol. 136, pp. 28-40, 1980, (2).
@article{2-s2.0-0019204281,
title = {Vertical variability of climatic conditions in the Khangai Mountains ( Mongolia).},
author = { E. Brzezniak and T. Niedźwiedź},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019204281&partnerID=40&md5=8b6dcb099833c2d1e0e49bffd7efb3af},
year = {1980},
date = {1980-01-01},
journal = {Prace Geograficzne, Instytut Geografii i Przestrzennego Zagospodarowania PAN},
volume = {136},
pages = {28-40},
abstract = {One of nine papers studying vertical zonality in the area by the Polish-Mongolian, Physico-Geographical Expedition. Examines circulation, winds, radiation, thermal conditions, ground temperatures and precipitation in the mountains to explain the variation of climatic belts with height. -M.Forsey},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
One of nine papers studying vertical zonality in the area by the Polish-Mongolian, Physico-Geographical Expedition. Examines circulation, winds, radiation, thermal conditions, ground temperatures and precipitation in the mountains to explain the variation of climatic belts with height. -M.Forsey
Hess, M. T.; Niedźwiedź, T.; Obrebska-Starklowa, B.
The value of fixed-time interval air temperature data in the evaluation of mesoclimatic conditions. Journal Article
In: Geographia Polonica, vol. 43, pp. 35-48, 1980, ISSN: 00167282.
@article{2-s2.0-0019144914,
title = {The value of fixed-time interval air temperature data in the evaluation of mesoclimatic conditions.},
author = { M.T. Hess and T. Niedźwiedź and B. Obrebska-Starklowa},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0019144914&partnerID=40&md5=a82078c17f2a92ee9f710e97b1b1457b},
issn = {00167282},
year = {1980},
date = {1980-01-01},
journal = {Geographia Polonica},
volume = {43},
pages = {35-48},
abstract = {It is shown that there exist highly significant correlations bewtween the monthly mean maximum temperatures and the monthly mean air temperatures at 1 p.m. On the basis of an arbitrary mean monthly value at 1 p.m. not only can the mean maximum for the same month be determined with the help of regression equations, but also siilar values for other months can be reproduced with high accuracy, and the frequency of days with typical threshold temperatures in the year can be calculated.- from Authors},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
It is shown that there exist highly significant correlations bewtween the monthly mean maximum temperatures and the monthly mean air temperatures at 1 p.m. On the basis of an arbitrary mean monthly value at 1 p.m. not only can the mean maximum for the same month be determined with the help of regression equations, but also siilar values for other months can be reproduced with high accuracy, and the frequency of days with typical threshold temperatures in the year can be calculated.- from Authors
1979
Kornowski, J.; Trombik, M.; Zuberek, W. M.
In: Wybrane zagadnienia geofizycznych badan w kopalniach, Swierklaniec 1976, pp. 181-197, 1979.
@article{2-s2.0-0018666913,
title = {(Results of microseismic source location at the ' Szombierki' coal mine). [Wyniki lokalizacji ognisk impulsow sejsmoakustycznych w kopalni wegla kamiennego 'Szombierki'.]},
author = { J. Kornowski and M. Trombik and W.M. Zuberek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0018666913&partnerID=40&md5=c9f9c45e89aaba60c50acc672c6c75a0},
year = {1979},
date = {1979-01-01},
journal = {Wybrane zagadnienia geofizycznych badan w kopalniach, Swierklaniec 1976},
pages = {181-197},
publisher = {Publications-Institute of Geophysics, P.A.N. , M-2, no 123},
abstract = {Results of research on the possibility of determining fracture zones of the rock mass, particularly in seams liable to rock bursts, with the use microseismic source location technique are presented. A network of geophones was installed ahead of a working face and the microseismic activity initiated by blastings was recorded on a multichannel tape recorder. Reading off the time differences of first arrivals on consecutive channels with an accuracy of 0.2 ms, and determining the P-wave velocity in the area, the source co-ordinates of a number of impulses were calculated. The measuring method and detailed results are described. The location error was verified in practive, and for sharp arrivals it was no greater than 10m. The analysis of results indicates the fracturing of the rock mass ahead of the longwall face, mainly in the coal seam and in the firect roof rocks. Taking into account the possibility of attaining such a location accuracy, we may expect to be able to apply this method to determining the rock mass fracturing zones in coal seams liable to coal bumps; its practical use, however, seems to be conditioned by automation of labour-consuming interpretation of the records.-English summary},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Results of research on the possibility of determining fracture zones of the rock mass, particularly in seams liable to rock bursts, with the use microseismic source location technique are presented. A network of geophones was installed ahead of a working face and the microseismic activity initiated by blastings was recorded on a multichannel tape recorder. Reading off the time differences of first arrivals on consecutive channels with an accuracy of 0.2 ms, and determining the P-wave velocity in the area, the source co-ordinates of a number of impulses were calculated. The measuring method and detailed results are described. The location error was verified in practive, and for sharp arrivals it was no greater than 10m. The analysis of results indicates the fracturing of the rock mass ahead of the longwall face, mainly in the coal seam and in the firect roof rocks. Taking into account the possibility of attaining such a location accuracy, we may expect to be able to apply this method to determining the rock mass fracturing zones in coal seams liable to coal bumps; its practical use, however, seems to be conditioned by automation of labour-consuming interpretation of the records.-English summary
Hejnowicz, Z.; Nakielski, J.
Modeling of growth in shoot apical dome Journal Article
In: Acta Societatis Botanicorum Poloniae, vol. 48, no. 3, pp. 423-441, 1979, ISSN: 00016977, (8).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-84983268842,
title = {Modeling of growth in shoot apical dome},
author = { Z. Hejnowicz and J. Nakielski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84983268842&doi=10.5586%2fasbp.1979.034&partnerID=40&md5=c9382c78615fa2a2b969ec0b17de402a},
doi = {10.5586/asbp.1979.034},
issn = {00016977},
year = {1979},
date = {1979-01-01},
journal = {Acta Societatis Botanicorum Poloniae},
volume = {48},
number = {3},
pages = {423-441},
publisher = {Polskie Towarzystwo Botaniczne},
abstract = {The vectorial field of displacement velocities V in growing apical dome is calculated from the scalar field adjusted to the geometry of the dome and to different variants of the distribution of linear growth rate along axis. The distribution of growth rate in volume and the temporal COnI-Se of cell wall net deformation in the apical dome calculated fiom the V fit within the range of empirical data when the linear growth rate along the axis increases with disstance from the tip. The distribution of volume growth rate attains the minimum inside the distal region of the dome where the zone of central mother cells occurs.},
note = {8},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The vectorial field of displacement velocities V in growing apical dome is calculated from the scalar field adjusted to the geometry of the dome and to different variants of the distribution of linear growth rate along axis. The distribution of growth rate in volume and the temporal COnI-Se of cell wall net deformation in the apical dome calculated fiom the V fit within the range of empirical data when the linear growth rate along the axis increases with disstance from the tip. The distribution of volume growth rate attains the minimum inside the distal region of the dome where the zone of central mother cells occurs.
1978
Niedźwiedź, T.
In: Folia Geographica, Series Geographica-Physica, no. PAN Krakow, 11, pp. 75-84, 1978, (2).
@article{2-s2.0-0018207328,
title = {The impact of synoptic situations on the differentiation of the mean diurnal air temperature in winter and in summer studied in the upper Vistula basin.},
author = { T. Niedźwiedź},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0018207328&partnerID=40&md5=a21273c51237c032ba2bbfa1e0e9d412},
year = {1978},
date = {1978-01-01},
journal = {Folia Geographica, Series Geographica-Physica},
number = {PAN Krakow, 11},
pages = {75-84},
abstract = {Winter and summer temperature contrasts in the upper Vistula Basin are studied with reference to atmospheric circulation. Synoptic maps for 1966 and 1975 are classified according to weather types over south Poland. This classification comprises sixteen directional and four pressure pattern weather types. Regression equations relating temperatures for each weather type with altitude and mean seasonal temperature are discussed. -J. A. Kington},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Winter and summer temperature contrasts in the upper Vistula Basin are studied with reference to atmospheric circulation. Synoptic maps for 1966 and 1975 are classified according to weather types over south Poland. This classification comprises sixteen directional and four pressure pattern weather types. Regression equations relating temperatures for each weather type with altitude and mean seasonal temperature are discussed. -J. A. Kington
Niedźwiedź, T.
The changes of the atmospheric circulation indices over the Polish West Carpathians during the last 27 years ( Nowy Sacz). Journal Article
In: Schweizerische Meteorologische Zentralanstalt, Veroffentlichung, vol. 40, pp. 19-22, 1978, (5).
@article{2-s2.0-0018052674,
title = {The changes of the atmospheric circulation indices over the Polish West Carpathians during the last 27 years ( Nowy Sacz).},
author = { T. Niedźwiedź},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0018052674&partnerID=40&md5=e1c4cc8959753c493e1208ff50459a30},
year = {1978},
date = {1978-01-01},
journal = {Schweizerische Meteorologische Zentralanstalt, Veroffentlichung},
volume = {40},
pages = {19-22},
abstract = {Monthly values are given of circulation indices of: progression - P, meridionality - M, southern circulation - S, and cyclonicity - C over the Polish West Carpathians. Great changeability of those indices is stated over 1951-1977. On the basis of data from the meteorological station of Nowy Sacz, influence of these indices was examined on temperature and precipitation in January and July. - from STAR, 17(17), 1979},
note = {5},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Monthly values are given of circulation indices of: progression - P, meridionality - M, southern circulation - S, and cyclonicity - C over the Polish West Carpathians. Great changeability of those indices is stated over 1951-1977. On the basis of data from the meteorological station of Nowy Sacz, influence of these indices was examined on temperature and precipitation in January and July. - from STAR, 17(17), 1979
Hess, M. T.; Niedźwiedź, T.; Brebska-Starkel, B.
In: Schweizerische Meteorologische Zentralanstalt, Veroffentlichung, vol. 40, pp. 108-112, 1978.
@article{2-s2.0-0018049310,
title = {(Characterizing thermal conditions in mountainous regions from the standpoint of requirments for cultivated plant growth). [Zur Charakteristik der thermischen Verhaltnisse den Berggebieten vom Standpunkt der Vegetationsbedurfnisse der Kulturpflanzen.]},
author = { M.T. Hess and T. Niedźwiedź and B. Brebska-Starkel},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0018049310&partnerID=40&md5=a5c984b50001a9d4739c9c0041e8da48},
year = {1978},
date = {1978-01-01},
journal = {Schweizerische Meteorologische Zentralanstalt, Veroffentlichung},
volume = {40},
pages = {108-112},
abstract = {Use was made of the daily data concerning air tempertures recorded in the period from 1951 to 1970 by 15 stations situated in the Lower Beskid range. The probability of the occurrence of extreme air temperatures are discussed, and those values which set limits to the growing of agricultural plants were considered. - from STAR, 17(17), 1979},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Use was made of the daily data concerning air tempertures recorded in the period from 1951 to 1970 by 15 stations situated in the Lower Beskid range. The probability of the occurrence of extreme air temperatures are discussed, and those values which set limits to the growing of agricultural plants were considered. - from STAR, 17(17), 1979
Kornowski, J.; Trombik, M.; Zuberek, W. M.
Locating Zones of Concentration of Seismoacoustic Pulse Centers. [LOKALIZACJA STREF KONCENTRACJI OGNISK IMPULSOW SEJSMOAKUSTYCZNYCH.] Journal Article
In: Przegl Gorn, vol. 33, no. 2, pp. 72-79, 1978.
@article{2-s2.0-0017936239,
title = {Locating Zones of Concentration of Seismoacoustic Pulse Centers. [LOKALIZACJA STREF KONCENTRACJI OGNISK IMPULSOW SEJSMOAKUSTYCZNYCH.]},
author = { J. Kornowski and M. Trombik and W.M. Zuberek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0017936239&partnerID=40&md5=c4bf732da4d488573820394a7784a373},
year = {1978},
date = {1978-01-01},
journal = {Przegl Gorn},
volume = {33},
number = {2},
pages = {72-79},
abstract = {The results of tests on the locating of seismoacoustic pulse centers in a coal seam being worked are presented. A network of 4 to 6 geophones installed ahead of the working face at distances of 40 to 100 m apart was used. Using controlled blasting the P wave velocity was determined in the observed area. The locating of the pulse centers was carried out on the basis of differences in the pulse arrival times at successive sensors and on the basis of the known wave propagation velocity. In the case of sharp pulse arrivals the location error is less than 10 m. Seismoacoustic pulse center distributions obtained after two concussion blastings are presented.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The results of tests on the locating of seismoacoustic pulse centers in a coal seam being worked are presented. A network of 4 to 6 geophones installed ahead of the working face at distances of 40 to 100 m apart was used. Using controlled blasting the P wave velocity was determined in the observed area. The locating of the pulse centers was carried out on the basis of differences in the pulse arrival times at successive sensors and on the basis of the known wave propagation velocity. In the case of sharp pulse arrivals the location error is less than 10 m. Seismoacoustic pulse center distributions obtained after two concussion blastings are presented.
1976
Hankiewicz, J.; Swierczek, E.
Lysozymes and their role in clinical medicine [Lizozym -- zagadnienia biochemiczne i kliniczne] Journal Article
In: Postepy higieny i medycyny doswiadczalnej, vol. 30, no. 5, pp. 609-623, 1976, ISSN: 00325449, (1).
@article{2-s2.0-0017221053,
title = {Lysozymes and their role in clinical medicine [Lizozym -- zagadnienia biochemiczne i kliniczne]},
author = { J. Hankiewicz and E. Swierczek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0017221053&partnerID=40&md5=3e7bb8a00b740ce8a7fa9d37261b25f1},
issn = {00325449},
year = {1976},
date = {1976-01-01},
journal = {Postepy higieny i medycyny doswiadczalnej},
volume = {30},
number = {5},
pages = {609-623},
abstract = {[No abstract available]},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
Kossobudzka, H.; Otlik, A.; Duber, S.
In: Polimery/Polymers, vol. 21, no. 8, pp. 354-357, 1976, ISSN: 00322725.
@article{2-s2.0-0016991040,
title = {Primary Results of Studies of the Nature of Changes in Polyacrylonitrile (PAN) Fibers During Heat Treatment. [WSTEPNE BADANIA ZMIAN ZACHODZACYCH WE WLOKACH PAN PODCZAS OBROBKI TERMICZNEJ.]},
author = { H. Kossobudzka and A. Otlik and S. Duber},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0016991040&partnerID=40&md5=d5cabb5c68ac00cdafdd6c921b69a6cd},
issn = {00322725},
year = {1976},
date = {1976-01-01},
journal = {Polimery/Polymers},
volume = {21},
number = {8},
pages = {354-357},
abstract = {General characteristics of PAN fibers' properties being important in the process of carbon fibers formation from Anilana fibers was presented. Some studies were made at various temperatures using X-ray and microscopy techniques on the determination of specific temperature values and ranges of transitions occurring during heat treatment of raw, oxidized and carbonized fibers and changes in their structure. The strongest changes of fibers were found at oxidizing treatment temperature; such fibers are characterized by high exothermic effect, change of crystallites symmetry and occurrence of optical anisotropy.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
General characteristics of PAN fibers' properties being important in the process of carbon fibers formation from Anilana fibers was presented. Some studies were made at various temperatures using X-ray and microscopy techniques on the determination of specific temperature values and ranges of transitions occurring during heat treatment of raw, oxidized and carbonized fibers and changes in their structure. The strongest changes of fibers were found at oxidizing treatment temperature; such fibers are characterized by high exothermic effect, change of crystallites symmetry and occurrence of optical anisotropy.
Kossobudzka, H.; Otlik, A.; Duber, S.
Some initial studies of the nature of changes in polyacrylonitrile (PAN) fibres during heat treatment Journal Article
In: 1976.
@article{2-s2.0-0016898740,
title = {Some initial studies of the nature of changes in polyacrylonitrile (PAN) fibres during heat treatment},
author = { H. Kossobudzka and A. Otlik and S. Duber},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0016898740&partnerID=40&md5=3e9291c1d79cbbddff21ff1cb3093c2f},
year = {1976},
date = {1976-01-01},
abstract = {[No abstract available]},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
Kossobudzka, H.; Otlik, A.; Duber, S.
Preliminary studies of the changes occurring in polyacrylonitrile fibres during heat treatment Journal Article
In: 1976.
@article{2-s2.0-0016885316,
title = {Preliminary studies of the changes occurring in polyacrylonitrile fibres during heat treatment},
author = { H. Kossobudzka and A. Otlik and S. Duber},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0016885316&partnerID=40&md5=c24a1e2e588589de8fd9bffe3f9cac0d},
year = {1976},
date = {1976-01-01},
abstract = {[No abstract available]},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
1975
Hankiewicz, J.; Swierczek, E.
In: Przeglad Lekarski, vol. 32, no. 4, pp. 376-378, 1975, ISSN: 00332240, (9).
@article{2-s2.0-17444453798,
title = {A comparative evaluation of lysozyme using diffusion-plate and nephelometric methods (author's transl) [Porównawcze oznaczenia lizozymu metoda dyfuzji płytkowej i metoda nefelometryczna?]},
author = { J. Hankiewicz and E. Swierczek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-17444453798&partnerID=40&md5=358c916607c343b301ab5892c5d35b29},
issn = {00332240},
year = {1975},
date = {1975-01-01},
journal = {Przeglad Lekarski},
volume = {32},
number = {4},
pages = {376-378},
abstract = {[No abstract available]},
note = {9},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
1974
Hankiewicz, J.; Swierczek, E.
Lysozyme in human body fluids Journal Article
In: Clinica Chimica Acta, vol. 57, no. 3, pp. 205-209, 1974, ISSN: 00098981, (137).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0016266396,
title = {Lysozyme in human body fluids},
author = { J. Hankiewicz and E. Swierczek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0016266396&doi=10.1016%2f0009-8981%2874%2990398-2&partnerID=40&md5=ee0968a00dfa51d34e349179fcf569ac},
doi = {10.1016/0009-8981(74)90398-2},
issn = {00098981},
year = {1974},
date = {1974-01-01},
journal = {Clinica Chimica Acta},
volume = {57},
number = {3},
pages = {205-209},
abstract = {The activity of lysozyme was studied in the following body fluids using the diffusion method on agarose gel: blood serum of adults and children, umbilical cord blood serum, cerebrospinal fluid, amniotic fluid, urine, saliva, gastric juice, bile, tears, mothers' milk, sperm of a healthy subject, and exudates. From the results obtained it was found that lysozyme is present in almost all body fluids, though in different amounts. In serum its activity is normally from 7 to 13 mg/l. The highest content was found in tears, about 120 times higher than in serum. A considerable amount of lysozyme was found in gastric juice, about 8 times more than in normal serum. Lysozyme activity is lowest in or absent from urine, bile and cerebrospinal fluid. In other body fluids the activity of lysozyme was found to be the same as in serum. © 1974.},
note = {137},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The activity of lysozyme was studied in the following body fluids using the diffusion method on agarose gel: blood serum of adults and children, umbilical cord blood serum, cerebrospinal fluid, amniotic fluid, urine, saliva, gastric juice, bile, tears, mothers' milk, sperm of a healthy subject, and exudates. From the results obtained it was found that lysozyme is present in almost all body fluids, though in different amounts. In serum its activity is normally from 7 to 13 mg/l. The highest content was found in tears, about 120 times higher than in serum. A considerable amount of lysozyme was found in gastric juice, about 8 times more than in normal serum. Lysozyme activity is lowest in or absent from urine, bile and cerebrospinal fluid. In other body fluids the activity of lysozyme was found to be the same as in serum. © 1974.
Kozłowski, A.; Karwowski, Ł.
Chlorine/bromine ratio in fluid inclusions Journal Article
In: Economic Geology, vol. 69, no. 2, pp. 268-271, 1974, ISSN: 03610128, (7).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0005429647,
title = {Chlorine/bromine ratio in fluid inclusions},
author = { A. Kozłowski and Ł. Karwowski},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0005429647&doi=10.2113%2fgsecongeo.69.2.268&partnerID=40&md5=cef68db53adb79d76602c61558d4d75f},
doi = {10.2113/gsecongeo.69.2.268},
issn = {03610128},
year = {1974},
date = {1974-01-01},
journal = {Economic Geology},
volume = {69},
number = {2},
pages = {268-271},
abstract = {[No abstract available]},
note = {7},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
Hankiewicz, J.; Swierczek, E.
Results of personal investigations on serum and urinary lysozyme (Polish) Journal Article
In: Polskie Archiwum Medycyny Wewnetrznej, vol. 51, no. 6, pp. 591-597, 1974, ISSN: 00323772, (11).
@article{2-s2.0-0016155220,
title = {Results of personal investigations on serum and urinary lysozyme (Polish)},
author = { J. Hankiewicz and E. Swierczek},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0016155220&partnerID=40&md5=0e391814af2245d5f7d145964517b131},
issn = {00323772},
year = {1974},
date = {1974-01-01},
journal = {Polskie Archiwum Medycyny Wewnetrznej},
volume = {51},
number = {6},
pages = {591-597},
abstract = {It was observed that the activity of lysozyme in the serum and urine is significantly raised in cases of myeloid leukemia and in certain renal diseases. A rise in the serum lysozyme level was found also in patients with Hodgkin's disease. In cases of lymphatic leukemia the serum activity of this enzyme was low, lower even than in the healthy subjects. In the light of these results the authors suggest that determinations of lysozyme in serum and urine may be clinically useful and should be included into the complex of routine laboratory investigations.},
note = {11},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
It was observed that the activity of lysozyme in the serum and urine is significantly raised in cases of myeloid leukemia and in certain renal diseases. A rise in the serum lysozyme level was found also in patients with Hodgkin's disease. In cases of lymphatic leukemia the serum activity of this enzyme was low, lower even than in the healthy subjects. In the light of these results the authors suggest that determinations of lysozyme in serum and urine may be clinically useful and should be included into the complex of routine laboratory investigations.
1972
Budzanowski, A.; Freindl, L.; Karcz, W.; Kuźmiński, J.; Łazarska, B.; Zipper, W.
Polarization of protons from the 9Be(d, p)10Be reaction at Ed = 12.0 MeV Journal Article
In: Nuclear Physics, Section A, vol. 195, no. 1, pp. 280-288, 1972, ISSN: 03759474, (3).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-0346631587,
title = {Polarization of protons from the 9Be(d, p)10Be reaction at Ed = 12.0 MeV},
author = { A. Budzanowski and L. Freindl and W. Karcz and J. Kuźmiński and B. Łazarska and W. Zipper},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0346631587&doi=10.1016%2f0375-9474%2872%2990736-1&partnerID=40&md5=bde076716bbd3a017658f442b6d21678},
doi = {10.1016/0375-9474(72)90736-1},
issn = {03759474},
year = {1972},
date = {1972-01-01},
journal = {Nuclear Physics, Section A},
volume = {195},
number = {1},
pages = {280-288},
abstract = {The polarization of protons from the 9Be(d,p)10Be reaction at Ed = 12.0 MeV was measured for the ground state and first excited state transitions. The results obtained are compared with the predictions of DWBA theory. It was found that better fits to the experimental data can be obtained using volume absorption in the distorting potential of the deuteron elastic channel. A comparison of the present polarization data with the vector analysing power for the same reaction and the same incident deuteron energy has also been made. © 1972.},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The polarization of protons from the 9Be(d,p)10Be reaction at Ed = 12.0 MeV was measured for the ground state and first excited state transitions. The results obtained are compared with the predictions of DWBA theory. It was found that better fits to the experimental data can be obtained using volume absorption in the distorting potential of the deuteron elastic channel. A comparison of the present polarization data with the vector analysing power for the same reaction and the same incident deuteron energy has also been made. © 1972.
1971
Budzanowski, A.; Freindl, L.; Karcz, W.; Łazarska, B.; Zipper, W.
Polarization of protons from the 12C(d, p)13C reaction at Ed = 12.4 MeV Journal Article
In: Nuclear Physics, Section A, vol. 161, no. 2, pp. 610-620, 1971, ISSN: 03759474, (5).
Abstract | Links | BibTeX | Altmetric
@article{2-s2.0-49649149716,
title = {Polarization of protons from the 12C(d, p)13C reaction at Ed = 12.4 MeV},
author = { A. Budzanowski and L. Freindl and W. Karcz and B. Łazarska and W. Zipper},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-49649149716&doi=10.1016%2f0375-9474%2871%2990389-7&partnerID=40&md5=26e53fda3bee05d165bfe973a65be248},
doi = {10.1016/0375-9474(71)90389-7},
issn = {03759474},
year = {1971},
date = {1971-01-01},
journal = {Nuclear Physics, Section A},
volume = {161},
number = {2},
pages = {610-620},
abstract = {The polarization of protons from the 12C(d, p)13C reaction at Ed = 12.4 MeV was measured for the ground state and first excited state transitions. The results obtained are compared with the vector analysing power (VAP) data for the same reaction and at the same energy of the incident deuterons. An attempt to fit the polarization data with the DWBA theory is also presented. © 1970.},
note = {5},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The polarization of protons from the 12C(d, p)13C reaction at Ed = 12.4 MeV was measured for the ground state and first excited state transitions. The results obtained are compared with the vector analysing power (VAP) data for the same reaction and at the same energy of the incident deuterons. An attempt to fit the polarization data with the DWBA theory is also presented. © 1970.