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1

Charakterystyka warunkow wystepowania i morfologia gleb z orsztynem na obszarze Parku Krajobrazowego Lasy Janowskie

100%
Chodorowski J.
Roczniki Gleboznawcze
|
2000
|
tom 51
|
nr 1-2
113-124
2

Impact of altitude diversity on the phosphorus content in Chornohora soils [Eastern Carpathians, Ukraine]

63%
Chodorowski J., Melke J.
Polish Journal of Soil Science
|
2009
|
tom 42
|
nr 1
69-76
In this paper the results of studies on three different forms of phosphorus – total, organic and inorganic – in soils of the Chornohora massif (Eastern Carpathians, Ukraine), depending on altitude, have been presented. The studied gleyed acid brown soils are situated in the belt of alpine meadows (1760 and 2057 m a.s.l.) and in the forest layer (1020 and 1120 m a.s.l.).
3

Formation of Arctic soils in Chamberlindalen, Bellsund, Spitsbergen

63%
Melke J., Chodorowski J.
Polish Polar Research
|
2006
|
tom 27
|
nr 2
119-132
Soils in the Chamberlindalen area (Bellsund, Spitsbergen) have been formed under polar climatic conditions, influenced by many years of permafrost, and chemical and physical weathering. The type of bedrock and local water conditions are considered to be significant soil-forming factors. The following soil units were distinguished according to the FAO-UNESCO Revised Legend (1997): Gelic Leptosols, Gelic Regosols, Gelic Gley- sols, and Gelic Cambisols. The basic properties of the soils studied are (i) shallow soil profile with poorly differentiated genetic horizons, (ii) the particle size distribution of sands and loams, (iii) a considerable content of the silt fraction, (iv) different pH, and a considerable organic carbon content.
4

Pollen analysis from fossil podzol soils within a dune at Kaczorki (Middle Roztocze, Poland)

63%
Balaga K., Chodorowski J.
Acta Palaeobotanica
|
2006
|
tom 46
|
nr 2
5

Badanie podatnosci do tlenia wybranych materialow drzewnych

63%
Chodorowski J., Babel K.
Przemysł Drzewny
|
2006
|
tom 57
|
nr 11
34-38
6
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Sulphur in soils within the impact zone of the metallurgy-sulphur railroad in the Roztoczanski National Park

63%
Debicki R., Chodorowski J.
Acta Agrophysica
|
2000
|
tom 35
The aitn of the research was to evaluate the influence of the metallurgy-sulphur railroad (LHS) on some soil properties of the Roztoczański National Park. Special attention was paid to sulphur risks, due to sulphur transport that way, although in smaller quantities as compared to the previous decade. The study Was based on the analysis of basic properties of selected soils and content of total and sulphate sulphur in soif samples taken in 2 cross-section profiles, located 400 and 900 m from the border of the Park and 50, 100, and 150 m from the rails; from 3 levels of forest soils; litter, 0-10 cm, and 30-40 em. Pedological survey indicated that within the study area predominated light soils. They are derived from river sands (mainly gley, gley-podzolic, podzolic soils, and black earth), and contain low amounts of the fine fraction. It was found that the line, which runs across the protected areas of the national park, does not exert nowadays a direct negative influence on the investigated soil properties (C-organic, reaction, mobile aluminium). The amount of total and /sulphate sulphur reniainjjon the level characteristic for such soil types in natural environment. No decrease in the content of both forms of sulphur was found along with the distance of sampling points from the LHS rails.
7

The content of total and DTPA-TEA extracted forms of Zn, Cu, Mn, Pb, Co and Ni in Chornohora [Ukraine] mountain soils

51%
Melke J., Chodorowski J., Debicki R.
Polish Journal of Soil Science
|
2005
|
tom 38
|
nr 1
51-60
The aim of the studies was to determine the various forms of heavy metals (Zn, Cu, Mn, Pb,Co, and Ni) in the soil profiles of Gleyi-Dystric Cambisols in the mountain massive of Chornohora (Ukraine). The soil environment of Chornohora appeared to be not polluted with the heavy metals analyzed. Minor excess can only be observed in the content of the following metals (in mg per kg): total Pb – 142.41, Pb(DTPA) – 106.93 (profile 1, organic horizon O), total Zn – 232.92 (profile 3, organic horizon O). The above alleviated amounts of some metals can be attributed to progressive anthropopressure on Carpathian soils.
8

Influence of land use on the content of select forms of Cd, Cr, Cu, Ni, Pb, and Zn in urban soils

51%
Plak A., Chodorowski J., Melke J., Bis M.
Polish Journal of Environmental Studies
|
2015
|
tom 24
|
nr 6
9

Soil formation and soil properties in the areas of Lyellstranda, Dystrad Logne in the region of Bellsund (West Spitsbergen)

51%
Melke J., Chodorowski J., Uziak S.
Polish Journal of Soil Science
|
1990
|
tom 23
|
nr 2
10

Porównanie wybranych właściwości podtypów rędzin kredowych porośniętych murawą kserotermiczną i próba ich klasyfikacji w różnych systematykach

51%
Kalicka M., Chodorowski J., Debicki R.
Acta Agrophysica. Rozprawy i Monografie
|
2004
|
nr 5[108]
11

The influence of the grain size distribution of dystric Cambisols on the content of various forms of cadmium, lead, and manganese

51%
Melke J., Plak A., Chodorowski J., Uziak S.
Polish Journal of Soil Science
|
2008
|
tom 41
|
nr 1
35-49
The analysis of distribution of various forms of Cd, Pb, and Mn in the profile was carried out in Dystric Cambisols on the example of the Western Bieszczady soils (SE Poland). In the soil material, the grain size distribution was determined and the sequential analysis of cadmium, lead, and manganese was performed resulting in the following forms: F1 – exchangeable form; F2 – form bound with organic matter; F3 – form bound with manganese oxides; F4 – form bound with slightly crystalline iron oxides; F5 – form bound with crystalline iron oxides; F6 – residue. The contents of produced forms (Cd, Pb, Mn) determined in the particular textural groups differ substantially. The residual forms of cadmium, lead, and manganese dominated in almost all the textural groups of the soils examined. Also lead in the form bound with amorphous iron oxides showed an increased concentration in all the textural groups. The smallest content of lead and cadmium was determined in the form bound with manganese oxides, whereas the smallest content of manganese was determined in the form bound with organic matter.
12

Selected geochemical criteria in mire profiles of Poreby Wojslawskie (Sandomierz Basin, Poland SE)

51%
Plak A., Chodorowski J., Pidek I. A., Dobrowolski J.
Polish Journal of Soil Science
|
2015
|
tom 48
|
nr 1
The geochemical analysis of biogenic sediments was used to reconstruct environmental conditions and the impact of human activity from a small mire geo-system in the Sandomierz Basin (Poland SE). Changes in the nature of selected geochemical indicators show a significant impact on the transformation of the mire during the early stages of human activity. It is reflected in the geochemical record by means of a high proportion of heavy metals – cadmium, lead and copper. Evident variability of main geochemical components concentration is also visible in a vertical record of analysed cores. This is a consequence of the sedimentary basin asymmetric configuration and the ensuing variable biogenic sedimentary succession.
13

Specificity of Arctic tundra soils of Spitsbergen

51%
Klimowicz Z., Melke J., Uziak S., Chodorowski J.
Polish Journal of Soil Science
|
2009
|
tom 42
|
nr 1
97-109
The study concludes the results of research conducted for over 20 years in Spitsbergen by the Department of Soil Science of the Maria Curie-Skłodowska University. The results have been presented in nine figures provided with concise commentaries and in the form of seven conclusions.
14

Propozycje nowych jednostek w systematyce gleb polski

51%
Klimowicz Z., Chodorowski J., Debicki R., Uziak S.
Acta Agrophysica. Rozprawy i Monografie
|
2004
|
nr 5[108]
15
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Content available

Acidity and buffering properties of selected soil types of the Lasy Janowskie Landscape Park

51%
Chodorowski J., Debicki R., Smalej M.
Acta Agrophysica
|
2001
|
tom 50
The aim of this study was to analyse the acidity and buffer abilities of selected soils occurring within terrestrial (forest, arable and meadow) ecosystems, under specific form of protection within the Lasy Janowskie Landscape Park. The results of the study indicate that the very acid and acid reaction of the soil environment is the result of natural processes, such as relations between mother rock and plant cover (low pH, high value of hydrolytic and exchangeable acidity, and high content of mobile aluminum), and low degree of saturation of the sorption complex with bases. The greatest buffering abilities showed typic gley soil (Dystric Gleysol), peat soil (Terric Histosol), and accumulation horizons of other soil types.
16

Changes in the properties of the eroded loess soils cultivated since the 18th century

51%
Klimowicz Z., Chodorowski J., Debicki R., Melke J.
Polish Journal of Soil Science
|
2006
|
tom 39
|
nr 1
The studies were carried out within a catena of loess soils of the West Roztocze region. These are typical grey-brown podzolic soils (Haplic Luvisols) in various stages of erosion and deluvial soil (Eutric Fluvisol). Research shows the great variation in the morphology and the physical-chemical properties of the soils. Differences observed included the content of humus, range of soil reaction, depth of decalcification, hydrolytic acidity, and the content of exchangeable cations. The reasons for such a differentiation lie in various forms of economic human influence on the surface formations of the lithosphere, including the soil cover, occurring both now and in the past.
17
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Content available

Anthropogenical transformation of soil within the grave-mound

39%
Klimowicz Z., Chodorowski J., Debicki R., Bis M., Kokowski A., Sadowski S.
International Agrophysics
|
2009
|
tom 23
|
nr 4
333-341
18
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Cutaneous and subcutaneous abdominal necrosis in a morbidly obese patient – a case report

39%
Prystupa A., Lachowska-Kotowska P., Dybala A., Chodorowski J., Krasowska D., Mosiewicz J.
Journal of Pre-Clinical and Clinical Research
|
2009
|
tom 03
|
nr 1
19

Professor Doctor Jerzy Melke (1941-2013)

32%
Chodorowski J., Debicki R., Klimowicz Z.
Polish Journal of Soil Science
|
2013
|
tom 46
|
nr 2
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