收稿日期: 2020-05-13
修回日期: 2020-11-15
网络出版日期: 2021-04-14
基金资助
中国地质科学院水文地质环境地质研究所基本科研业务费项目(SK202012);中央高校基本科研业务费项目(lzujbky-2018-it82);国家自然科学基金资助(41871021)
Analysis of sand source for Badain Jaran Desert based on CMB model
Received date: 2020-05-13
Revised date: 2020-11-15
Online published: 2021-04-14
沙漠因其高反照率、低比热容的下垫面以及粉尘高输出率的特征对全球和区域环境有重要的作用。作为具有高大沙山的第二大流动性沙漠,其物质来源一直是地球科学研究热点。通过对巴丹吉林沙漠及周边地区表层沉积物进行矿物分析,在此基础上对巴丹吉林沙漠的可能物源区进行分析,进一步利用化学质量平衡(CMB)模型探讨了各物源区对巴丹吉林沙漠的贡献率。结果表明:巴丹吉林沙漠的表层沉积物中主要矿物包括相对比较稳定钠长石、钙长石、歪长石、黑云母、斜顽辉石、透辉石、铁辉石、微斜长石、白云母、正长石、石英和榍石以及不具区域代表性的斜绿泥石、石膏、角闪石、方解石、岩盐;主要物源区包括沙漠湖积平原沙、洪积平原沙、现代湖泊沉积物、外源沙和岩石风化壳;其中岩石风化壳和现代湖泊沉积物属于就地起沙,基本只影响其周边区域,来自沙漠北部的冲洪积沙和来自沙漠西北的外源沙是沙漠的主要物源。这与中国东部沙漠以湖泊沉积就地起沙有明显不同,可能和沙漠的发育过程、地质历史时期湖泊退缩规模和气候环境状况有关。
宁凯,王乃昂,李卓仑,杨振京,毕志伟,王奕心,王攀,孙杰 . 基于CMB模型的巴丹吉林沙漠沙源区分析[J]. 干旱区地理, 2021 , 44(2) : 389 -399 . DOI: 10.12118/j.issn.1000–6060.2021.02.10
Desert ecosystems play an important role in global and regional environments due to their high albedo, low specific heat capacity, and high dust output. As the second largest mobile desert in China, the source of sediment in the Badain Jaran Desert has always been a subject of interest in earth science research. In this paper, the composition of surface sediments collected from the Badain Jaran Desert and surrounding areas were analyzed to identify their provenance, and the chemical mass balance model was used to estimate the contribution rates of source or sources. The results show that the main minerals in the surface sediments of the Badain Jaran Desert include relatively stable albite, albite, anorthite, anorthoclase, biotite, clinoenstatite, enstatite, microcline, muscovite, orthoclase, quartz, titanite, and non-regionally representative clinochlore, gypsum, hornblende, calcite, and halite, and the main provenances include desert lacustrine plain sands, alluvial plain sands, modern lake sediments, exogenous sands, and weathered rock crusts. The weathered rock crusts and modern lake sediments belong to in situ sanding and thus only affects the surrounding area. Alluvial sand from north of the desert and exogenous sand from the northwest are the main sources of the Badain Jaran Desert sands. These are very different from the desert sediments in the eastern parts of China which are attributed to lake sedimentation and may be related to the evolution of the desert, the scale of retreat of lakes in the region throughout geological history, and the climate and environmental conditions.
Key words: minerals; aeolian sand; CMB model; provenance analysis; Badain Jaran Desert
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