生物结皮藻培养对侵蚀和土壤脱水影响下农田土壤退化和土壤结构的比较分析

P. Fűtő, B. Madarász, G. Bernát, Máté Futó, G. Jakab, J. Kutasi
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引用次数: 0

摘要

与气候有关的土地退化和荒漠化威胁着大约一半的欧盟成员国。在匈牙利,风蚀和水蚀影响了230万公顷的土地。土壤退化最重要的指标之一是土壤的保水能力。因此,主要目标是维持或增加它。由于对极端环境条件的适应能力,土壤藻类可以在干旱地区生存。由于它们的贡献,可以在土壤的顶层形成生物土壤结皮。土壤结皮可以稳定土壤表面,增强土壤的保水性,从而间接促进更高层次的沉降
本文章由计算机程序翻译,如有差异,请以英文原文为准。
COMPARATIVE ANALYSIS OF SOIL DEGRADATION AND SOIL STRUCTURE IN CROPLANDS AFFECTED BY EROSION AND SOIL DEHYDRATION TREATED WITH A BIOLOGICAL SOIL CRUST FORMING ALGAL CULTURE
Climate-related land degradation and desertification threaten around half of EU member states. In Hungary, wind and water erosion affects 2.3 million hectares of land. One of the most important indicators of soil degradation is the water retention capacity of the soil. Therefore, the primary objective is to maintain or increase it. Due to their adaptation to extreme enviromental conditions, soil algae can survive in drought-stricken areas. With their contribution, biological soil crusts can be formed on the top layer of the soil. Soil crusts can stabilize the surface of the soils, enhance the water retainment, thus indirectly contributing to the settlement of higher order
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