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Changes of vegetation efects in soil properties in the post-agriculture landscapes (south-eastern Poland)

100%
Sosnowska A. J.
Miscellanea Geographica. Regional Studies on Development
|
2019
|
vol. 23
|
issue 1
63-70
EN
Plant succession is quite a common phenomenon in Poland, especially in agricultural landscapes. At the turn of the 21st century there was a significant increase in the area of fallow lands. That increased the area occupied by ruderal and segetal vegetation. The development of vegetation on post-agricultural lands transforms soils. The aim of this paper is to determine changes in vegetation and soil properties that occur as a result of secondary succession on post-agricultural lands in loess landscapes
2

Some characteristics of forest-tundra (West Siberia) soil groups distinguished on the basis of thermal properties

86%
Valdayskikh V., Nekrasova O., Nekrasova O., Jouzel J., Uchaev A., Radchenko T.
Prace Geograficzne
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2013
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issue 135
73 – 86
EN
This paper contains the results of the forest-tundra soils studying. The key sites were situated on the permafrost territory, which is under scrutiny in connection with the global climate changes. The soil position in landscape, parent rock texture, vegetation conditions and thickness of organic horizons were taken into account. On the base of seasonal thawing or active layer depth measurements and soil temperature vertical gradients calculating, four main soil groups which are different in their thermal properties were identified. The physical-chemistry properties are rather close in various soil types. Similarities in the profile distribution of humus fractions are also revealed in the soil humus formed under different conditions. Despite of estimated relatively low level of carbon stocks in forest-tundra soils, half of them exist in mobile humus forms, which are less stable. ata on the soil thermal regime types and stocks of different humus forms in soils of various conditions are useful or long-term forecasting of soil status.
3
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Zmiany w środowisku glebowym i ich skutki

58%
Gruszczyński S.
Przyszłość. Świat-Europa-Polska
|
2014
|
issue 2/30/
36-63
PL
Gleby ulegają ciągłym zmianom związanym z przebiegiem procesów glebotwórczych oraz oddziaływaniem przedsięwzięć gospodarczych czło-wieka. Głównym problemem jest przypuszczalnie zabezpieczanie przeciwerozyjne gleb, choć na tle Europy Polska należy do krajów mniej zagrożonych tym zjawiskiem. Stosunkowo duże jest zagrożenie ruchami masowymi. Obserwuje się ubytek węgla organicznego w glebach spowodowany po części wzrostem głębokości uprawy, odwodnieniem, jak też prawdopodobnie podniesieniem się temperatury powietrza. Poza rejonami intensywnego oddziaływania przemysłu gleby można uznać za czyste, choć może budzić niepokój znaczny wzrost zużycia środków ochrony roślin. Obserwuje się silny trend w urbanizacji Polski: w ciągu dziesięciu lat powierzchnia terenów zurbanizowanych wzrosła z poziomu 4,66% do ponad 5,15%, co oznacza ubytek gleb uprawnych kosztem terenów potencjalnie separowanych około 40 ha na dobę. Zagęszczanie jest następstwem unowocześniania i wzrostu masy urządzeń uprawowych; rolnictwo, jako działanie najbardziej dotknięte tym problemem dysponuje środkami technicznymi na przeciwdziałanie jego skutkom. Znaczna część problemów związanych z tymi zagrożeniami może zostać złagodzona dzięki kompetentnie sporządzonym planom zagospodarowania przestrzennego i wdrożeniu metod ochrony przeciwerozyjnej. Pewne możliwości przeciwdziałania ubytkowi glebowego węgla organicznego są dostępne dla gospodarstwa rolnego i leśnego. Doprowadzenie do odpowiedniego stanu obszarów zanieczyszczonych wymaga podjęcia remediacji gleb.
EN
Soils are constantly evolving due to the soil-forming processes and the impact of human economic activities. The main problem is likely to protect soil erosion, but comparing to Europe, Poland is a country less threatened by this phenomenon. Relatively large is the threat of mass movements. The loss of soil organic carbon is due in part to an increase in the depth of planting, dehydration, and also probably because of increase the air temperature. Beyond impact of intensive industry, soil can be considered clean, although a significant increase in the use of plant protection products may be worrying. There is a strong trend in urbanization: in ten years, an urban area in Poland increased from 4.66% to 5.15%, which means the loss of agricultural soils about 40 hectares a day. Densification is a consequence of the modernization and growth of the equipment for cultivation; agriculture, as the activity most affected by this problem has the technical means to counteract its effects. A large part of the problems associated with these risks can be mitigated through competently prepared spatial develop-ment plans and implementation methods for erosion protection. Some ways of preventing the depletion of soil organic carbon are available for agriculture or forestry. Bring contaminated sites to an appropriate state requires a soil remediation.
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