气候变化领域集成服务门户(CCPortal): 柴达木盆地苏干湖表层沉积与尘暴事件-元素示踪的初步结果

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	柴达木盆地苏干湖表层沉积与尘暴事件-元素示踪的初步结果
其他题名	Surface sediments of Lake Sugan and dust storm in the Northern Qaidam Basin, China: preliminary results of elemental tracers
	强明瑞; 鲁瑞洁; 张家武; 肖舜; 陈发虎
发表日期	2006
ISSN	1003-5427
卷号	18 期号:6 页码:590-596
中文摘要	通过分析苏干湖地区10个地表表层沉积物、9个大气降尘(含2个尘暴降尘)、16个湖泊表层沉积物等样品的8种常量-微量元素和11种稀土元素的含量，以及同类沉积不同元素含量和不同沉积同一元素含量的相关性，结果表明，在湖泊沉积体系中Al、Fe、Sc含量的变化与强风-尘暴过程有关，指示了湖泊沉积碎屑颗粒风成输入的可能性．元素Fe、Sc含量在3种不同的沉积物巾差异不大，与尘暴事件的强度和频次有关．稀土元素结果显示3类沉积具有同源性．苏干湖沉积可以用来重建研究区尘暴演化历史．
英文摘要	To understand the role of atmospheric dust in the global climate system further, it is necessary that a longer sequence of dust storm history should be established using geological archives in dust provenance area. Hydrologically closed lakes in the arid regions of China could be ideal objectives to trace dust storm evolution since the most of Northwest China has been recognized as an important source area for global dust loading. Lake Sugan, a closed lake located at the northern margin of the Qinghai-Tibetan Plateau, would be employed to study on the dust storm history in the Qaidam Basin. Here, 8 elements and 11 rare-earth elements were analyzed for three different sediments/deposits in the Sugan Lake region, namely, the surface sediments of Lake Sugan, the settled sand dust including materials collected during dust storm durations, and the surface deposits of the region. The results show the element of Al has been enriched by 11% relative to the surface ground deposits. The composition of the element in lake sediments is nearly half of the settled dust, which may be diluted by the carbonate accounting for about 50% of the lake sediment. Two of Al, Fe and Sc exhibit apparent positive correlations in the lake sediments. Also, for one of the three elements positive correlation was found between the settled sand dust and the lake sediments. However, there are negative correlations between the catchment deposits and the settled sand dust, and between the catchment deposits and the lake sediment for Al and Sc. Variations in Fe and Se compositions exhibit an apparent positive correlation not only with intensity of dust storm events, but also with frequency of the events. The Fe and Sc compositions seem to be changeless for the three kinds of sediments/ deposits. In addition, the results of rare-earth elements analyses show that the lake sediments, the settled sand dust and the surface ground deposits may derive from a homologous source. The elements of Al, Fe, Sc are most likely to be transported into lake through strong wind and dust storm processes. Therefore, sediments of Lake Sugan could be used to trace dust storm in this region, and the elements of Al, Fe, Se could be applied in reconstruction of dust storm history.
关键词	尘暴事件降尘元素示踪苏干湖
英文关键词	Dust storm;the settled sand dust;elemental tracers;Lake Sugan
语种	中文
WOS研究方向	Geology
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
CSCD记录号	CSCD:2570337
来源期刊	湖泊科学
来源机构	兰州大学 ; 中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/1817
推荐引用方式 GB/T 7714	强明瑞,鲁瑞洁,张家武,等. 柴达木盆地苏干湖表层沉积与尘暴事件-元素示踪的初步结果[J]. 兰州大学, 中国科学院青藏高原研究所,2006,18(6):590-596.
APA	强明瑞,鲁瑞洁,张家武,肖舜,&陈发虎.(2006).柴达木盆地苏干湖表层沉积与尘暴事件-元素示踪的初步结果.湖泊科学,18(6),590-596.
MLA	强明瑞,et al."柴达木盆地苏干湖表层沉积与尘暴事件-元素示踪的初步结果".湖泊科学 18.6(2006):590-596.