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Wind Erosion during Sandstorm Events in Hetian, China

机译:中国和田沙尘暴事件期间的风蚀

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摘要

Hetian in Xinjiang is a region with extensive wind erosion, severe desertification and various aeolian sand hazards. To assess the variation in wind erosion of surface soil in the region, the quantity of wind-eroded soil and some surface properties (vegetation cover and surface soil moisture) were concurrently measured and analyzed in six land use types during two sandstorm events in 2004. The amount of surface soil transported varied in the following order:abandoned farmland > intermediate zone of desert and rural section > active sand dunes on the edge of the desert > the country roads > film-mulched cotton plot > alfalfa. On 20 May 2004, the quantity of eroded soil in the abandoned farmland was 76.8 g cm- 2, 40 times greater than film-mulched cotton plot and the Alfalfa. When the vegetation cover was about more than 50% or the water content of soil was above 4%, the rate of sand transport was reduced. With an increase in distance, the amounts of sand transported from Taklimakan Desert to other surfaces varied exponentially. At 400 m, the amounts of sand transported declined from 30 gcm-2 to 1 g cm-2, and the difference was not too much among surfaces after that point. Under the vegetation cover, the amounts of sand transported from the film-mulched cotton and alfalfa plots were more than their down tuyering and increased with sampling height, but those in the abandoned farmland, intermediate zone of desert and rural section, country roads and active sand dunes on the edge of the desert were more at 20 cm and decreased with height. The quantity of eroded soil and damage from wind erosion was extremely high in the abandoned farmland, intermediate zone of desert and rural section, country roads and active sand dunes on the edge of the desert. These were the most potent sources of dust in the area of Hetian. Measures are needed to reduce wind erosion and sandstorm in Hetian, such as expanding the area under winter-wheat, planting perennial herbs and green crops, implementing protective cultivation systems, avoiding over-grazing and laying the country roads with Gobi, gravel, and asphalt.
机译:新疆和田地区风蚀严重,沙漠化严重,风沙危害严重。为了评估该地区表层土壤的风蚀变化,在2004年的两次沙尘暴事件中,同时测量和分析了六种土地利用类型的风蚀土壤数量和一些表面特性(植被覆盖度和表层土壤水分)。表层土壤的运输量按以下顺序变化:废弃的农田>沙漠和农村地区的中间地带>沙漠边缘的活跃沙丘>乡间小路>地膜棉田>苜蓿。 2004年5月20日,废弃农田的侵蚀土壤数量为76.8 g·cm-2,是覆膜棉田和苜蓿的40倍。当植被覆盖率超过50%或土壤含水量超过4%时,沙的运移速度就会降低。随着距离的增加,从塔克拉玛干沙漠运送到其他地面的沙量呈指数变化。在400 m处,沙的输送量从30 gcm-2下降到1 g cm-2,此后各表面之间的差异不太大。在植被覆盖下,覆膜棉花和苜蓿地块的沙土输送量大于向下的风口,并随采样高度的增加而增加,但在弃耕地,沙漠和农村地区的中部地区,乡村道路和活跃地区沙漠边缘的沙丘在20厘米处更多,并随高度降低。在荒芜的耕地,沙漠和农村地区的中间地带,乡村道路和沙漠边缘的活跃沙丘上,侵蚀土壤和风蚀破坏的数量非常高。这些是和田地区最有效的粉尘源。需要采取措施减少和田的风蚀和沙尘暴,例如扩大冬小麦种植面积,种植多年生草本植物和绿色作物,实施保护性耕作制度,避免过度放牧并在戈壁,砾石和沥青铺设乡间道路。

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