首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Study on Response Relation between Eco-Environment Change and Soil Erosion Process in Reclaimed Forestland of Loess Hilly Region in China
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Study on Response Relation between Eco-Environment Change and Soil Erosion Process in Reclaimed Forestland of Loess Hilly Region in China

机译:黄土丘陵区退耕地生态环境变化与土壤侵蚀过程的响应关系研究。

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The soil erosion of Loess Plateau is the main cause of the worse eco-environment, and the control of erosion environment is the key to ensure the eco-environment construction successfully. Based on the 10 year's data observed in the Loess hilly region, the paper studied the response relation between eco-environment change and soil erosion process after forestlands reclaimed. The results showed that when the man-made changed the eco-environment to reclaim forestland, the intensity of man-made soil erosion was more 1,000 times than that of the natural erosion. Taken the soil erosion modulus unit erosivity of rainfall as the index, the soil erosion intensity increased apparently with the erosive time eroded. Then from the analysis of soil physical and forces properties, in 10th year eroded after forestland reclaimed, the clay content and physical clay content decreased 2.74% and 3.01% respectively, which showed the soil particles had the tendency to skeleton soil, and the > 0.25mm water stable aggregate content also decreased 58.7%, the soil unit weight increased and the soil shear strength decreased, all of which were easier to occur soil erosion. The correlation analysis showed that > 0.25mm water stable aggregate content was the maximum effect factor to soil erosion, the partial correlated coefficient was 0.9728, and then were soil coarse grain and soil shear strength, the partial correlated coefficients were 0.8879 and 0.6020 respectively. The relation between the > 0.25mm water stable aggregate content, the soil sheer strength and the soil erosion intensity were analyzed, which showed that the first and seventh year were the turn years of the soil erosion intensity after the forestlands reclaimed, revealed the change of eco-environment was the main cause to accelerate soil erosion. The degenerative soil eroded and eco-environment formed the peculiar erosion environment, which increased the soil erosion rapidly. So to return slope farmland into forest and grassland, to recover and reconstruct vegetation and improve the eco-environment were the key measurement to control soil erosion of Loess Plateau.
机译:黄土高原水土流失是生态环境恶化的主要原因,控制侵蚀环境是确保生态环境建设成功的关键。基于黄土丘陵区10年的观测资料,研究了退耕还林后生态环境变化与土壤侵蚀过程的响应关系。结果表明,人为改变生态环境开垦林地时,人为土壤侵蚀强度是自然侵蚀强度的1000倍以上。以侵蚀的土壤侵蚀模量单位侵蚀力为指标,随着侵蚀时间的延长,土壤侵蚀强度明显增加。然后通过对土壤物理和力学特性的分析,林地开垦后第10年侵蚀,粘土含量和物理粘土含量分别下降了2.74%和3.01%,表明土壤颗粒具有骨架化的趋势,且> 0.25毫米水稳性团聚体含量也降低了58.7%,土壤单位重量增加,土壤抗剪强度降低,所有这些都更容易发生水土流失。相关分析表明,> 0.25mm水稳性骨料含量是影响土壤侵蚀的最大因素,偏相关系数为0.9728,其次为土壤粗粒和抗剪强度,偏相关系数分别为0.8879和0.6020。分析了> 0.25mm水稳性骨料含量,土壤剪切强度和水土流失强度之间的关系,表明第一年和第七年是退耕还林后水土流失强度的转折年。生态环境是加速水土流失的主要原因。退化的土壤侵蚀和生态环境形成了特殊的侵蚀环境,这使土壤侵蚀迅速增加。因此,退耕还林还草,恢复植被重建,改善生态环境是控制黄土高原水土流失的关键措施。

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