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2000 年至 2015 年中国东北黑土区土壤侵蚀的时空变化。

Spatial and temporal variability of soil erosion in the black soil region of Northeast China from 2000 to 2015.

机构信息

Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing, 100101, China.

University of Chinese Academy of Sciences, Beijing, 100049, China.

出版信息

Environ Monit Assess. 2020 May 15;192(6):370. doi: 10.1007/s10661-020-08298-y.

Abstract

The black soil region in Northeast China is an important production base of commodity grain. However, soil erosion is a major threat that has caused a decline in arable land area and productivity and a series of environmental problems in recent years. To understand the current situation of soil erosion and its changes in the whole black soil region, including six treatment regions, we used the spatial-temporal analysis of soil erosion from 2000 to 2015 and the overlay analysis with its drivers; additionally, soil erosion was evaluated qualitatively with the integrated evaluation method, and its change was indicated by the soil erosion change index (SECI). We found that soil erosion that caused soil loss occurred in each treatment region mainly at the light level in 2015. Water erosion, the most widely distributed erosion type, affected the largest area, while most serious erosion at intensive or higher levels stemmed from wind erosion. Although the situation of water erosion was improved in 2015 compared to that in 2000, the overall situation of soil erosion was worse due to the deterioration of wind and freeze-thaw erosion. Grassland, woodland, and cultivated land changes, such as the conversion from grassland to cultivated land, from woodland to sparse woodland and from dry land to paddy land, revealed these changes to a great extent.

摘要

中国东北黑土区是重要的商品粮生产基地。然而,近年来土壤侵蚀是一个主要威胁,导致耕地面积和生产力下降,以及一系列环境问题。为了了解整个黑土区(包括六个治理区)的土壤侵蚀现状及其变化,我们利用 2000 年至 2015 年土壤侵蚀的时空分析以及与驱动力的叠加分析;此外,采用综合评价方法对土壤侵蚀进行定性评价,并通过土壤侵蚀变化指数(SECI)表示其变化。我们发现,2015 年各治理区发生的土壤侵蚀导致土壤流失主要处于轻度水平。水蚀是分布最广的侵蚀类型,影响面积最大,而强度或更高水平的侵蚀主要是风蚀造成的。尽管与 2000 年相比,2015 年水蚀情况有所改善,但由于风蚀和冻融侵蚀的恶化,土壤侵蚀的总体情况更糟。草原、林地和耕地的变化,如草原向耕地的转化、林地向疏林的转化以及旱地向水田的转化,在很大程度上揭示了这些变化。

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