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Ecological restoration and recovery in the wind-blown sand hazard areas of northern China: relationship between soil water and carrying capacity for vegetation in the Tengger Desert

机译:中国北方风沙灾害区的生态修复与恢复:腾格里沙漠土壤水分与植被承载力的关系

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The main prevention and control area for wind-blown sand hazards in northern China is about 320000 km2 in size and includes sandlands to the east of the Helan Mountain and sandy deserts and desert-steppe transitional regions to the west of the Helan Mountain. Vegetation recovery and restoration is an important and effective approach for constraining wind-blown sand hazards in these areas. After more than 50 years of long-term ecological studies in the Shapotou region of the Tengger Desert, we found that revegetation changed the hydrological processes of the original sand dune system through the utilization and space-time redistribution of soil water. The spatiotemporal dynamics of soil water was significantly related to the dynamics of the replanted vegetation for a given regional precipitation condition. The long-term changes in hydrological processes in desert areas also drive replanted vegetation succession. The soil water carrying capacity of vegetation and the model for sand fixation by revegetation in aeolian desert areas where precipitation levels are less than 200 mm are also discussed.
机译:中国北方风沙危害的主要防治区面积约320000 km 2 ,包括贺兰山以东的沙地和沙质荒漠。贺兰山以西的荒漠草原过渡区。植被恢复和恢复是限制这些地区风沙危害的重要而有效的方法。在腾格里沙漠沙坡头地区进行了50多年的长期生态研究之后,我们发现植被恢复通过土壤水的利用和时空再分配改变了原始沙丘系统的水文过程。在给定的区域降水条件下,土壤水分的时空动态与重新种植的植被的动态显着相关。沙漠地区水文过程的长期变化也驱使重新种植的植被演替。还讨论了降水水平小于200 mm的风沙区植被的土壤水分承载力和通过植被固沙的模型。

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