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中国沙漠 ›› 2014, Vol. 34 ›› Issue (6): 1552-1557.DOI: 10.7522/j.issn.1000-694X.2013.00425

• 生物与土壤 • 上一篇    下一篇

罗布泊盐湖表层土地球化学及沉积特征

徐莉1, 李艳红1, 杨甲全2   

  1. 1. 新疆师范大学 新疆干旱区湖泊环境与资源实验室/地理科学与旅游学院, 新疆 乌鲁木齐 830054;
    2. 新疆地质矿产局 第六地质大队, 新疆 哈密 839000
  • 收稿日期:2013-09-16 修回日期:2013-10-12 出版日期:2014-11-20 发布日期:2014-11-20
  • 作者简介:徐莉(1986- ),女,新疆博乐人,硕士研究生,研究方向为干旱区气候与环境.Email:xuli1986317@126.com
  • 基金资助:
    新疆干旱区湖泊环境与资源实验室基金项目(XJDX0909-2010-05);国家自然科学基金项目(41161010);新疆师范大学研究生创新基金项目(20121203)资助

The Characteristics of Geochemistry and Sedimentary of Surface Soil in the Salt Lakes of Lop Nor

Xu Li1, Li Yanhong1, Yang Jiaquan2   

  1. 1. Xinjiang Laboratory of Lake Environment and Resources in Arid Area/College of Geographic Science and Tourism, Xinjiang Normal University, Urumqi 830054, China;
    2. No.6 Geological Party, BGMRED of Xinjiang, Hami 839000, Xinjiang, China
  • Received:2013-09-16 Revised:2013-10-12 Online:2014-11-20 Published:2014-11-20
  • Contact: 李艳红(Email:lyh0704@126.com)

摘要: 对罗布泊典型地区表层土磁性特征、粒度及地球化学特征的研究表明:(1)总体样品磁性矿物含量均较低;各样地间磁化率差异较为明显,阿奇克谷地西部磁化率值最高(2.1×10-7 m3·kg-1),耳轮区最低(0.47×10-7 m3·kg-1),该区磁化率值总体表现为东部略高于西部.(2)样品粒度组分总体以粉砂(2~63 μm)为主,平均约占74.17%,分选性较差,细颗粒占主导地位,且各粒度组分之间的含量变化幅度较小.(3)易溶性盐主要是由Cl-、SO4-2、Na+和K+构成,Mg2+、Ca2+含量较低,HCO3-、CO32-含量很低,易溶性盐类型主要为Cl--SO4-2-Na+和K+型;样品总有机碳平均含量约为0.66%;pH值变化范围为6.98~8.00,且耳轮区样品值均高于阿奇克谷地西部.综上所述,该区当时气候已转向干旱化趋势发展,而且气候持续干化与补给变化对该区物质形成具有一定影响,是该区物质空间分布的主要成因.

关键词: 罗布泊, 磁化率, 粒度, 地球化学, 沉积特征

Abstract: The characteristics of magnetic and grain-size and geochemistry in surface soil of the Lop Nor area were investigated. The results showed that: (1)All samples of Magnetic mineral content were lower;there are obviously different magnetic susceptibility in different places, the maximum value of magnetic susceptibility was 2.1×10-7 m3·kg-1 in the Aqike Valley West, the minimum value was 0.47×10-7 m3·kg-1 in the helix region, overall, the magnetic susceptibility values of the eastern was slightly higher than the western in the Lop Nor Area. (2)Component of grain size in the sample was mainly silt sand (2-63 μm), the average wass 74.17%, poorly sorted,dominate particles was fine particles,and there were small magnitude changes between each particle size fractions. (3)Soluble salts were mainly composed of Cl-, SO42-, Na+ and K+, Mg2+, Ca2+ were lower content, and the lowest were HCO3- and CO32-, the soluble salt type was mainly Cl--SO42--Na+ and K+; the average content of TOC was about 0.66%, the pH value ranged between 6.98-8.0, there were in alkaline environment, and the values in the helix region were higher than in west of Aqike Valley. To sum up, the area of climate had shifted to the drought trend, and continuous dry climate and supply variation had certain effect on the material form, this would be the main cause of the material distribution in this area.

Key words: Lop Nor, magnetic susceptibility, grain size, geochemistry, sedimentary characteristics

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