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ECO-ENVIRONMENT CHANGE AND SOIL EROSION PROCESS IN THE RECLAIMED FORESTLAND OF THE LOESS PLATEAU

机译:黄土高原退耕还林生态环境变化与土壤侵蚀过程

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摘要

Serious soil erosion has made the eco-environment fragile in the Loess Plateau. Based on the 10-year data observed from 1989 to 1998 in the Ziwuling Survey Station in loess hilly region, the eco-environment change and soil erosion process in reclaimed forestland were studied in this paper. The results showed that the intensity of man-made soil erosion caused by forestland reclamation was 1000 times more than that of the natural erosion. From the analysis of soil physical and mechanical properties, in the 10th year after forestland was reclaimed, the clay content and physical clay content decreased 2.74 percentage point and 3.01 percentage point respectively, the >0.25mm water-stable aggregate content decreased 31.59 percentage point, the soil bulk density increased and soil shear strength decreased, all of which were easier to cause soil erosion. The correlation analysis showed that >0.25mm waterstable aggregate content was the key factor affecting soil erosion, and the secondary factors were soil coarse grain and soil shear strength. The relation between the >0.25mm waterstable aggregate content, the soil sheer strength and the soil erosion intensity were analyzed, which showed that the first year and the seventh erosion year were the turn years of the soil erosion intensity after the forestland was reclaimed, revealed that the change of eco-environment was the main cause to accelerate soil erosion, and the worse environment caused soil erosion to be serious rapidly.
机译:严重的水土流失使黄土高原的生态环境变得脆弱。本文以黄土丘陵区子午岭站1989年至1998年的10年观测资料为基础,对开垦林地的生态环境变化及水土流失过程进行了研究。结果表明,森林开垦造成的人为土壤侵蚀强度是自然侵蚀强度的1000倍。从土壤物理力学性质分析,开垦后第10年,黏土含量和物理黏土含量分别下降2.74个百分点和3.01个百分点,> 0.25mm水稳性骨料含量下降31.59个百分点,土壤容重增加,土壤抗剪强度下降,均较易引起土壤侵蚀。相关分析表明,> 0.25mm的稳定骨料含量是影响水土流失的关键因素,次要因素是土壤粗粒和抗剪强度。分析了> 0.25mm水稳性骨料含量,土壤剪切强度与水土流失强度之间的关系,揭示了第一年和第七年是林地复垦后水土流失强度的转折年。生态环境的变化是加剧土壤侵蚀的主要原因,而恶劣的环境使土壤侵蚀迅速加剧。

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