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Global Soil Change and Land Degradation in Conditions of Slovakia

机译:斯洛伐克条件下的全球土壤变革与土地退化

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Slovakia is situated in Central Europe of temperate climatic region. Climatic oscillations (greenhouse effect) as well as human activity in different economical conditions are more or less significant on global soil change and land degradation especially since 1990 year. By the influence of global warming also in temperate climate regions the extension of more or less dry period is often indicated especially during last decade. Further also medium and strong mineralisation of groundwater has been confirmed. It can indicate the next development of alkaline and saline soils in the warmest regions of Slovakia referring to global climate change. Soil acidification has developed particularly in soils developed mostly on acidic parent materials particularly under humid conditions. The decrease of humus content is remarkable in all arable soils. In general, on the basis of obtained results it may be said that soils in Slovakia are not polluted. Not more than 0.4 % of soil cover is strongly polluted. The change of heavy metal content in soils is not significant during last decade. The result of a soil global change depends to a great extent on its degree of reversibility. Finally, irreversible change is related to land degradation.
机译:斯洛伐克位于温带气候区中欧中欧。在不同经济条件下的气候振荡(温室效应)以及人类活动在全球土壤变化和土地退化中,特别是自1990年以来,在全球土壤变化和土地退化中的程度上更为显着。由于全球变暖的影响也在温带气候区域中,通常在去年的延伸或多或少的干燥期间延伸。还证实了地下水的中等和强矿化。它可以指示斯洛伐克最温暖的地区碱性和盐土壤的下一次发展,提及全球气候变化。土壤酸化特别开发,特别是在酸性母材料上产生的土壤中,特别是在潮湿的条件下。所有可耕作的土壤中腐殖质含量的降低都是显着的。一般来说,在获得的结果的基础上,可能会说斯洛伐克的土壤没有污染。不超过0.4%的土壤覆盖受到强烈污染。在过去十年中,土壤中重金属含量的变化并不重要。土壤全球变化的结果在很大程度上取决于其可逆性程度。最后,不可逆转的变化与土地退化有关。

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