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The Effect of Land Use Change on Transformation of Relief and Modification of Soils in Undulating Loess Area of East Poland

机译:波兰东部黄土起伏地区土地利用变化对土壤浮雕和土壤改良的影响

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摘要

The change of primary forest areas into arable land involves the transformation of relief and modification of soils. In this study, we hypothesized that relatively flat loess area was largely transformed after the change of land use due to erosion. The modifications in soil pedons and distribution of soil properties were studied after 185 years of arable land use. Structure of pedons and solum depth were measured in 128 and soil texture and soil organic carbon in 39 points. Results showed that soils of noneroded and eroded profiles occupied 14 and 50%, respectively, and depositional soils 36% of the area. As a consequence, the clay, silt, and SOC concentration varied greatly in the plowed layer and subsoil. The reconstructed profiles of eroded soils and depositional soils without the accumulation were used to develop the map of past relief. The average inclination of slopes decreased from 4.3 to 2.2°, and slopes >5° vanished in the present topography. Total erosion was 23.8 Mg ha−1 year−1. From that amount, 88% was deposited within the study area, and 12% was removed outside. The study confirmed the hypothesis of the significant effect of the land use change on relief and soils in loess areas.
机译:将原始森林面积转变为耕地涉及到浮雕的改造和土壤的改良。在这项研究中,我们假设相对较平坦的黄土区域在土地利用因侵蚀而改变后发生了很大的变化。在185年的耕地利用之后,研究了土壤ped的改良和土壤特性的分布。测量了128个脚踏板的结构和深度,并在39个点测量了土壤质地和土壤有机碳。结果表明,未剥蚀和侵蚀的土壤分别占该地区的14%和50%,沉积土壤占该地区的36%。结果,耕层和下层土壤中的粘土,淤泥和SOC浓度变化很大。利用未积累的侵蚀土壤和沉积土壤的重建剖面来绘制过去的地形图。在目前的地形中,坡度的平均倾斜度从4.3度降低到2.2度,大于5度的坡度消失了。总侵蚀量为23.8 Mg ha -1 -1 。从这个数量中,有88%被沉积在研究区域内,而12%被移除到外部。该研究证实了黄土区土地利用变化对救济和土壤产生重大影响的假设。

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