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Zarys krajobrazowo-geochemiczny środkowego Mazowsza na zachód od Warszawy

100%

Wicik B.

Prace i Studia Geograficzne

|

1992

|

tom 14

Three physicogeographical mesoregions which are adjecent to Warsaw to its West occupy various hypsometric levels and display the features of the spatial setting of cascade structure. Individual altitudinal degrees (links) of the setting are connected via hydrological migratory flow, directed from the autonomous landscapes of Rawa Upland towards North. On the slopes of the Upland, fulfilling the role of transitory landscape units, the gradient of the flow is at some 5 per mille, and the significant degree of erosion of the glacial forms appearing here results in low contents of calcium (up to 60 miligrams per litre) and magnesium (usually less than 7 mg/l) in water solutions. Błonie Plain, taking the middle link in the setting is formed by the supraqual geocomplexes with weakly alcalic and gley enviromnents of hypergenetic zone. Groundwater in this subordinate landscape unit, richer in calcium (up to 300 mg/l) and magnesium (some 40-70 mg/l), displays a slight inclination (approx. 0,8 per mille) in Western direction. The thus important differences in physical and chemical parameters of the flow (migration medium) result inevitably in a barrier effect, especially strongly marked along the border of Błonie Plain with Rawa Upland. A narrow zone of geocomplexes displaying, for instance, very high ferrous and calcary contents persists there. Warsaw Dale, occupying hypsometrically the lowest degree of the whole setting has only in its Southern fringe part the features of a unit subordinated with regard to Błonie Plain. This third unit is in its greater part covered by the systems of dune and peat-gley geocomplexes displaying, in principle, autonomy of their functioning.

2

Akumulacja zelaza w dolinie Narwi pod Tykocinem

100%

Wicik B.

Roczniki Gleboznawcze. Suplement

|

2001

|

tom 52

65-69

3

Cechy chemiczne wód gruntowych Ponidzia Pińczowskiego

100%

Wicik B.

Prace i Studia Geograficzne

|

2000

|

tom 27

The chemistry of water is determined by regional hydrogeological factors. In the marls and limestones of the Jędrzejów Plateau, Wodzisław Hummock and Pińczów Hummock, bicarbonate lime waters occur, with the main ion content of approximately 0.6 g/dm³. In the Solec Basin, sulphuric lime waters are quite common, which normally contain over 1.0 SO₄/dm³.

4

Przydatność związków tytanu, jako wskaźnika przy wyróżnianiu utworów i poziomów wietrzeniowo-glebowych

100%

Wicik B.

Prace i Studia Instytutu Geograficznego Uniwersytetu Warszawskiego. Geografia Fizyczna

|

1972

|

tom 10

|

nr 4

5

Budowa i funkcjonowanie systemów krajobrazowo-geochemicznych środkowego Mazowsza

100%

Wicik B.

Prace i Studia Geograficzne

|

1992

|

tom 13

The paper presents the scheme of the structure and functioning of the physicogeographic mesoregion of Central Masovian Lowland, the area within the reach of influence of Warsaw urban-industrial agglomeration. Landscape units, distinguished as to their general chemical characteristics, may form the basis for forecasting of mobility of chemical substances brought here with the hydrological and atmospherical flow of migration of matter.

6

Chemizm wod i osadow jezior Na Jazach w Kotlinie Plockiej

100%

Wicik B.

Polish Botanical Studies. Guidebook Series

|

1993

|

tom 08

7

Cechy chemiczne krajobrazów Kampinowskiego Parku Narodowego

100%

Wicik B.

Prace i Studia Geograficzne

|

1997

|

tom 21

The western part of Warsaw basin covered by the Kampinos National Park, exists as a space system mainly consisting of 3 laying evenly with a parallel of latitude links: south, central and northern. As far as chemical and hydrological features are concerned, the south one is quite strongly subordinated to the area of glacial plains. The central link embracing the depression of Łasica river and situated along a belt of dunes, shows a significant function autonomy. Here the substances transported as a colloidal solutions have a essential influence on habitats' trophic levels. Strongly changed, already in historical times, by floods the northern link is quite strongly subordinated to hidrological influence of the Vistula river. On the basis of chemical features the homogeneous units of the soil weathering zone were isolated, which could also be treated as a fundamental geochemical landscapes distinctly reacting to any human influence.

8

Pasowość zjawisk hipergenicznych na obszarze Wysoczyzny Rawskiej i Równiny Błońskiej

100%

Wicik B.

Prace i Studia Instytutu Geograficznego Uniwersytetu Warszawskiego. Geografia Fizyczna

|

1972

|

tom 10

|

nr 4

9

Osady jezior tatrzańskich i etapy ich akumulacji

100%

Wicik B.

Prace i Studia Geograficzne

|

1984

|

tom 05

Partial results of studies of the lake deposits are reported. The lake sediments were sampled by a research team from the Warsaw University and the Polish Academy of Sciences. The lakes examined are found to be of various age. The oldest deposits connected with the oldest Dryas (or earlier) are found in a few lakes of a very cold climatic zone. The lakes of cold and moderately-cold stages of the mountains are younger; the beginnings of their operation fall at the Boreal and the early Atlantic periods. The youngest sediments were found in the lake Zadni Staw situated in the moderately cold climatic stage. The age of the Tatra lakes was conditioned by the hydrogeological characteristics of that area (older lakes) related to the tectonic systems, and the hydrothermal properties of the postglacial geographic environment of that area (younger lakes). However, the time of deglaciation onset in that part of the Carpathians has not been determined.

10

Marek Prószyński

100%

Wicik B.

Prace i Studia Geograficzne

|

2008

|

tom 40

Marek Prószyński was born on 27 April 1906, in Warsaw, a son of the didactic activist, writer, and publisher Konrad Prószyński (alias Kazimierz Promyk). In 1932 he graduated of the University of Warsaw with a degree in geography and in 1934 he was promoted a doctor. In the latter part of his studies and in the following years he participated in the geological research of the Stanisław Lencewicz's group in Polesie and simultaneously served his apprenticeship as a geography teacher at Warsaw schools. In 1938 he took a post at the National Geologie Institute. After the subjugation of the Institute by the Nazis, he mined and delivered chalk in 1940-1941; then in 1942- 1944 he conducted the pedologie research under the guidance of T. Mieczyński . In 1945- 1956 he was employed in the Capital City Reconstruction Bureau as the Director of the Physiographic Laboratory. In 1956 he took a post at the Institute of Geography of the University of Warsaw. He organized the Department of the Soils Geography at the Chair of Physical Geography, he equipped it with the basic appliances and reagents, and with the help o chemists MChem. M. Hoff and MEng I. Dąbrowska he adopted the methodology of the chemical analysis of soils and grounds to the Institute's geography didactics. In 1974-76 he organized the Laboratory of Termoluminescence. He improved and simplified the modernly applied areometric method of assay of the granular composition of soils (so-called Prószyński's modification of the Casagrande's method). He edited the manuscriptal Map of the Surface Formations of the Warsaw Urban Agglomeration; and he participated in the preparation of the Map of the Polish Soils 1 :300 000 (Warsaw). He is the author of Historical study on changes in the Vistula river valley hetween Góra Kalwaria and Warsaw. In 1945- 1960 he taught at the Warsaw University of Life Science and in 1948- 1950 at the Technical University. During his work at the University of Warsaw he held courses on the soils geography and pedology, as well as on soil studies for engineers and physical geographic research methods for geographers and archaeologists (for a few years). He tutored 24 master's thesis and 3 doctor's dissertations. Docent Marek Prószyński died on 24 April 2003, in Warsaw.

11

Krajobrazy gipsowe Ponidzia Pińczowskiego

100%

Wicik B.

Prace i Studia Geograficzne

|

2000

|

tom 27

Particular attention is devoted to the gypsum waste mantle of the Solec and Połaniec Basins. In well dried places, gypsum rock is covered with strontium-abundant (Sr) carbonate waste mantle. In hydrogenic landscapes, where groundwater and frequently bituminous substances are agents in the dissolving of gypsum, black clays with concretions are formed, including such elements as Mn or Fe.

12

Skład chemiczny próchnic nakładowych i opadów atmosferycznych w borach sosnowych Równiny Charzykowskiej, na Pojezierzu Południowopomorskim

100%

Wicik B.

Prace i Studia Geograficzne

|

2005

|

tom 36

Investigation of chemical composition of raw humus were fulfilled in Bory Tucholskie in accordance to a contract with National Park authority. The area of case study is about 50 km² and includes sander plain, covered by pine coniferous forest with moss and lichen Cladonia undergrowth. The dominant parent rock of rusty soils is loose sand. Actual development of flora composition is mainly determined by nutrients from raw humus and atmospheric precipitation. Raw humus type is moder and moder-mor. Sublayer Of containes around 33,4% C and 1,12% N, but Ofh-30,7% C and 1,26% N. The organic whole layer on the area of 1 m² contains around 50g N, 3,7 g K, 2,7 g Fe, 0,1 g Cu. Atmospheric precipitation at the level of 478 mm annually (year 2001) consists another important source of nutrients for the local ecosystems. For example: atmospheric input brings 5% of N and even 85% of Mg in the raw humus. Distribution of these proportions may impact on eutrophisation of protected habitats in the Park.

13

Studium porównawcze gleb okolic Warszawy i Moskwy

100%

Wicik B.

Prace i Studia Instytutu Geograficznego Uniwersytetu Warszawskiego. Geografia Fizyczna

|

1979

|

tom 23

|

nr 8

14

Substancje humusowe gleb w swietle wynikow ekstrakcji goraca woda [gleba plowa, szara gleba lesna, czarnoziem]

63%

Harasimiuk A., Wicik B.

Roczniki Gleboznawcze

|

2010

|

tom 61

|

nr 1

38-44

15

Charakterystyka gleb Parku Narodowego Gor Stolowych

51%

Szerszen L., Kabala C., Wicik B.

Szczeliniec

|

1996

71-77

16

Wpływ zanieczyszczeń metalurgicznych na charakterystyki magnetyczne czarnoziemów

51%

Hasso-Agopsowicz A., Jelenska M., Wicik B.

Przegląd Naukowy. Inżynieria i Kształtowanie Środowiska

|

2006

|

tom 15

|

nr 1[33]

17

Lake Gosciaz - a site of annually laminated sediments covering 12000 years

51%

Ralska-Jasiewiczowa M., Wicik B., Wieckowski K.

Bulletin of the Polish Academy of Sciences. Earth Sciences

|

1987

|

tom 35

|

nr 2

18

Geneza, wlasciwosci i systematyka gleb Parku Narodowego Gor Stolowych

51%

Kabala C., Szerszen L., Wicik B.

Szczeliniec

|

2002

|

tom 06

21-94

19

Radiocarbon chronology of annually laminated sediments from the Gosciaz Lake

51%

Pazdur A., Pazdur M. F., Wicik B., Wieckowski K.

Bulletin of the Polish Academy of Sciences. Earth Sciences

|

1987

|

tom 35

|

nr 2

20

Marek Prószyński (1906-2003) Wspomnienie o nauczycielu i wychowawcy

50%

Wicik B.

Prace i Studia Geograficzne

|

2005

|

tom 36

Ograniczanie wyników

Zarys krajobrazowo-geochemiczny środkowego Mazowsza na zachód od Warszawy

Akumulacja zelaza w dolinie Narwi pod Tykocinem

Cechy chemiczne wód gruntowych Ponidzia Pińczowskiego

Przydatność związków tytanu, jako wskaźnika przy wyróżnianiu utworów i poziomów wietrzeniowo-glebowych

Budowa i funkcjonowanie systemów krajobrazowo-geochemicznych środkowego Mazowsza

Chemizm wod i osadow jezior Na Jazach w Kotlinie Plockiej

Cechy chemiczne krajobrazów Kampinowskiego Parku Narodowego

Pasowość zjawisk hipergenicznych na obszarze Wysoczyzny Rawskiej i Równiny Błońskiej

Osady jezior tatrzańskich i etapy ich akumulacji

Marek Prószyński

Krajobrazy gipsowe Ponidzia Pińczowskiego

Skład chemiczny próchnic nakładowych i opadów atmosferycznych w borach sosnowych Równiny Charzykowskiej, na Pojezierzu Południowopomorskim

Studium porównawcze gleb okolic Warszawy i Moskwy

Substancje humusowe gleb w swietle wynikow ekstrakcji goraca woda [gleba plowa, szara gleba lesna, czarnoziem]

Charakterystyka gleb Parku Narodowego Gor Stolowych

Wpływ zanieczyszczeń metalurgicznych na charakterystyki magnetyczne czarnoziemów

Lake Gosciaz - a site of annually laminated sediments covering 12000 years

Geneza, wlasciwosci i systematyka gleb Parku Narodowego Gor Stolowych

Radiocarbon chronology of annually laminated sediments from the Gosciaz Lake

Marek Prószyński (1906-2003) Wspomnienie o nauczycielu i wychowawcy