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Analysis of Impact of Soil Erosion on the Slope Farmland on the Loess Plateau

机译:黄土高原坡面耕地水土流失影响分析

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摘要

The serious soil erosion brought soil fertility degradation, soil environment quality deterioration, and lead to low yield grain production in loess plateau. Soil nutrient loss, soil physical property degeneration and soil enzyme activity reduction to cause low yield were discussed by combining located observation, typical field investigation and laboratory analysis. When the degree of slope increased from 4o to 16owithout fertilizer application, the loss of organic matter increased from 107.9kg ha-1 to 210.0kg ha-1, total nitrogen from 14.8kg ha-1 to 26.1 kg ha-1 and total phosphorus from 4.41 kg ha-1 to 13.3 kg ha-1. These results lead to "barrenness", "coarseness" and "calcification" of the loess soil. Due to soil erosion, the content of particle size less than O.Olmm in slope farmland accounts for only 21.5%, which is equal to a half of that without erosion. At same time soil fertility and amylase activity in slope land decrease with the slope degree increase, and the relationships between them can be described by the index function. According to the data, a simple assessment of the impact of erosion on soil quality was made and divided the quality levels were divided into five grades, including good, fairly good, poor, extremely poor and deteriorated. This scheme provides a scientific basis for remaking and using soil resource.
机译:严重的水土流失使土壤肥力下降,土壤环境质量恶化,导致黄土高原地区粮食减产。通过现场观察,典型田间调查和实验室分析相结合的方法,探讨了土壤养分流失,土壤物理性质退化和土壤酶活性降低导致低产的问题。在不施肥的情况下,当坡度从4o增加到16o时,有机质的损失从107.9kg ha-1增加到210.0kg ha-1,总氮从14.8kg ha-1增加到26.1 kg ha-1。 4.41千克ha-1至13.3千克ha-1。这些结果导致黄土的“贫瘠”,“粗糙”和“钙化”。由于水土流失,坡耕地中小于0.01mm的颗粒含量仅占21.5%,仅相当于未遭受侵蚀的一半。同时,坡地土壤肥力和淀粉酶活性随坡度的增加而降低,二者之间的关系可用指标函数来描述。根据数据,对侵蚀对土壤质量的影响进行了简单评估,并将质量等级分为五个等级,包括好,相当好,差,极差和恶化。该方案为土壤资源的改造和利用提供了科学依据。

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