荒漠化
风积作用
干旱
中国
土地退化
沙丘稳定
腐蚀
自然地理学
地质学
水文学(农业)
环境科学
地理
地球科学
土地利用
地貌学
生态学
岩土工程
古生物学
考古
生物
作者
Tao Wang,Chen Guang-ting,Halin Zhao,Honglang Xiao
出处
期刊:Springer eBooks
[Springer Nature]
日期:2022-01-01
卷期号:: 199-220
被引量:4
标识
DOI:10.1007/978-981-16-7916-2_15
摘要
AbstractDesertification in China mainly includes the following types: soil erosion, aeolian desertification and salinization. Desertification in most parts of northern China is mainly manifested in land aeolian desertification. Aeolian desertification is defined as land degradation in arid, semiarid and parts of semi-humid regions with the occurrence of blown sand activities (deflation, ground surface coarsening, and sand dune formation, etc.) on former non-desert areas as the main mark resulting from various factors including overusing land and upsetting the fragile ecological balance under the conditions of dry and windy climate and loose sand surface (CCICCD 1994).
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