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首页> 外文期刊>Mountain Research & Development >Land cover change and its environmental impact in the Upper reaches of the Yellow River, Northeast Qinghai-Tibetan Plateau
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Land cover change and its environmental impact in the Upper reaches of the Yellow River, Northeast Qinghai-Tibetan Plateau

机译:青藏高原东北部黄河上游土地覆被变化及其环境影响

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摘要

Many studies have focused on desertification processes in northern China in an attempt to understand desertification-related ecological problems. Desertification on the Qinghai-Tibetan Plateau has received little attention, even though desertification resulting from overgrazing is a widespread phenomenon there. This study focuses on the Gonghe Basin in the upper reaches of the Yellow River, located on the northeast Qinghai-Tibetan Plateau, to shed light on desertification processes and associated environmental impacts during a 10-year period from 1987 to 1996. We first used 2 thematic mapper images to classify land cover for 2 summers (1987 and 1996) into 9 land cover types related to desertification. To assess the severity of desertification and to calculate the total soil carbon emission caused by desertification, we first defined severity by comparing land cover differences between 1987 and 1996 and then determined the differences in organic carbon content of the soil in grasslands during different stages of desertification between 1987 and 1996. The results showed that about 240 km(2) of grasslands was lost to agricultural encroachment and about 190 km(2) became sand-covered area between 1987 and 1996. During the same period, desertification affected 569.6 km(2) of grasslands, with desertification assessed as very severe for 41.8%, severe for 15.1%, and Moderate for 43.1% of the area, The results also show that carbon emissions from grassland deterioration caused by desertification amounted to 2.06 x 10(6) tC during the 10-year period, the average annual emission rate being 0.206 x 10(6) tC.
机译:为了了解荒漠化相关的生态问题,许多研究集中在中国北方的荒漠化过程。尽管过度放牧造成的荒漠化是该地区的普遍现象,但青藏高原的荒漠化却鲜有受到关注。这项研究的重点是位于青藏高原东北部的黄河上游的共和盆地,以揭示1987年至1996年的10年期间的荒漠化过程及相关的环境影响。我们首先使用2专题地图图像将2个夏季(1987年和1996年)的土地覆被分类为9种与荒漠化有关的土地覆被类型。为了评估荒漠化的严重程度并计算由荒漠化引起的土壤总碳排放量,我们首先通过比较1987年和1996年之间的土地覆盖差异来定义严重程度,然后确定荒漠化不同阶段草地土壤有机碳含量的差异1987年至1996年之间。结果表明,在1987年至1996年之间,约240 km(2)的草地被农业侵蚀所破坏,约190 km(2)变成了被沙覆盖的区域。在同一时期,荒漠化影响了569.6 km(2)。 )的草地,荒漠化被评估为该地区的严重程度为41.8%,严重为15.1%,中度为43.1%,结果还显示,荒漠化导致的草地退化造成的碳排放量为2.06 x 10(6)tC在10年期间,年平均排放率为0.206 x 10(6)tC。

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