关键词 长江下游 黄土高原 黏土矿物 古气候 [gap=1809]Key words lower reaches of Yangtze River, Chinese Loess Plateau, clay mineral, palaeoclimate
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The Holocene loess-soil sequence on the Chinese Loess Plateau constitutes an excellent record of evolution of soil formation, monsoonal climate, eolian dust accumulation and influence of arable farming of over 10000 years.
黄土高原的全新世黄土-土壤地层系列很好地记录了过去一万多年土壤发育、季风气候、风尘堆积和农业耕作影响的演变。
参考来源 - 临汾盆地全新世成壤环境演变及人类活动影响·2,447,543篇论文数据,部分数据来源于NoteExpress
The Chinese Loess Plateau is an extreme example of human-induced soil erosion and the resulted economic sufferings.
中国的黄土高原是人类活动加剧土壤侵蚀,从而使经济受损的一个极端例子。
This research focuses on the erosion problem of ZuLi River basin in the western part of the Chinese Loess Plateau using GIS-assisted soil erosion model.
本研究重点利用GIS辅助土壤侵蚀模型对黄土高原西部的祖厉河流域的土壤侵蚀问题进行了研究。
As a information carriers of the research of global change, the loess in Chinese loess Plateau is the most consecutive sediment and has the most abundance information since Quaternary.
中国黄土高原的黄土,作为全球变化研究的信息载体,是连续性最好、蕴藏信息最丰富的第四纪陆相沉积物。
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