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中国沙漠 ›› 2013, Vol. 33 ›› Issue (5): 1426-1432.DOI: 10.7522/j.issn.1000-694X.2013.00208

• 生物与土壤 • 上一篇    下一篇

艾比湖干涸湖底不同景观类型下富盐沉积物盐分积聚特征

吉力力·阿不都外力1, 米热班·阿布里米提1,2, 刘东伟3, 葛拥晓1,4   

  1. 1.中国科学院新疆生态与地理研究所 荒漠与绿洲生态国家重点实验室, 新疆 乌鲁木齐 830011;
    2.新疆大学 资源与环境科学学院, 新疆 乌鲁木齐 830046;
    3.内蒙古大学 环境与资源学院, 内蒙古 呼和浩特 010021;
    4.中国科学院大学, 北京 100049
  • 收稿日期:2012-08-22 修回日期:2012-11-09 出版日期:2013-09-20 发布日期:2012-11-09

Characteristics of Salt Accumulation in Salt-rich Sediments under Different Landscapes in the Ebinur Lake Playa, Xinjiang, China

Abuduwaili Jilili1, Abulimiti Mireban1,2, LIU Dong-wei3, GE Yong-xiao1,4   

  1. 1.State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
    2.College of Resources and Environment Science of Xinjiang University, Urumqi 830046, China;
    3.College of Environment and Resources of Inner Mongolia University, Hohhot 010021, China;
    4.University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2012-08-22 Revised:2012-11-09 Online:2013-09-20 Published:2012-11-09

摘要:

以艾比湖东南部历史时期干涸湖底为研究区,对6种不同景观类型下富盐沉积物进行采样分析。运用经典统计研究了干涸湖底各景观类型下富盐沉积物盐分含量及盐分积聚特征。结果表明:不同景观类型的沉积物可溶性盐分含量差异显著。从平均值角度看,各景观类型表层沉积物中0~30 cm层的盐分含量占0~60 cm层盐分含量的70%,即沉积物盐分垂直分布呈强表聚性。各景观类型的沉积物盐分含量均属于中等变异强度(30%<CV≤90%,中等变异性)。富盐沉积物中阴离子以SO2-4和Cl-为主,CO2-3和HCO-3含量甚微;阳离子以Na+、Ca2+和Mg2+为主。不同景观类型沉积物盐分含量平均值从高到低规律是:梭梭荒漠带>无植被覆盖带>胡杨林带>芦苇荒漠带>草本结合带>乔本草本结合带。

关键词: 艾比湖, 干涸湖底, 景观类型, 富盐沉积物

Abstract:

Due to strong wind erosion, dry lake bed (playa) has become one of the main sources of saline-alkali dust storms in arid areas. In order to identify salt distribution characteristics under different landscapes in the dry lake-bed, salt contents in salt-rich sediments and their accumulation characteristics were studied using the methods of classical statistics under six different landscape types in the playa of Ebinur Lake, Xinjiang.The results showed that the soluble salt content of the sediments under different landscapes had significant differences. The average salt content of soil depth from 0 cm to 30 cm accounted for 70.3% of the entire soil (0-60 cm), that is, salt content showed strong vertical gradient. Salt content of sediments under the different landscapes had a moderate variation in the study area (CV=30%-90%, moderate variability). The average surface salt content in salt-rich sediments under different landscape types followed the order of Haloxylon ammodendron>bare desert>Populus euphratica>Phragmites australis>herbs>other trees. Sulfates and chlorides are the major anions while sodium, magnesium and calcium are the main cat ions. The result will provide basic data and scientific references for wind erosion control of dry lake-bed and prevention of salt dust storms.

Key words: dry lake bed, landscape types, salt-rich sediments, Ebinur Lake

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