干旱区研究

干旱区研究 ›› 2013, Vol. 30 ›› Issue (2): 226-230.

• 水土资源 • 上一篇    下一篇

新疆博斯腾湖湖周水体碳和盐离子的空间分布

房传苓1,2，王秀君1,3 ，王家平1,2   

  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.中国科学院大学，北京 100049； 3.美国马里兰大学地球科学交叉学科研究中心，美国 马里兰州 20740
  • 收稿日期:2012-09-18 修回日期:2012-11-10 出版日期:2013-03-15 发布日期:2013-03-29
  • 通讯作者: 王秀君. E-mail: wwang@essic.umd.edu
  • 作者简介:房传苓（1986-）,女，硕士研究生，主要从事干旱区水体碳循环方面的研究. E-mail: fangchuanling1@163.com
  • 基金资助:

    中国科学院“百人计划”项目（0972021001）

Spatial Distributions of Organic Carbon and Dissolved Ions in the Bosten Lake, Xinjiang

FANG Chuan-ling 1,2 ，WANG Xiu-jun 1,3 ,WANG Jia-ping 1,2   

  1. 1. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang,China;2. University of Chinese Academy of Sciences, Beijing 100049, China; 3. Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740, USA
  • Received:2012-09-18 Revised:2012-11-10 Online:2013-03-15 Published:2013-03-29

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被引次数

14

摘要： 以博斯腾湖为研究对象，在大湖区周边及开都河取水样和表层土样，分析湖周水体中颗粒有机碳（POC）和溶解有机碳（DOC）在秋季的空间分布特征及其与周围土壤碳及水体盐离子的关系。结果表明：湖周水体中POC浓度的空间变化较大（0.1~1.2 mg•L-1），而DOC浓度的变化较小（8.5~12.3 mg•L-1）。两者在出湖口和入湖口处的浓度均较低，与开都河的浓度相近。与早期相比，博斯腾湖水中无机碳存在由CO3 2-向HCO3-转化的现象。回归分析显示，水体中各形态碳与土壤碳之间没有显著的线性关系，表明水体中碳的含量受周围土壤的影响不大。

关键词: 颗粒有机碳, 溶解有机碳, 土壤碳, 盐离子, 空间分布, 博斯腾湖, 新疆

Abstract: In order to study the spatial distribution of organic carbon, some water and topsoil samples were collected in and around the Bosten Lake in Xinjiang, China in November 2011. Particulate organic carbon (POC), dissolved organic carbon (DOC) and dissolved ions in water samples, and organic and inorganic carbon contents in soil samples were measured. The results showed that there was a wide range of POC (0.1-1.2 mg•L-1) but a narrow one of DOC (8.5-12.3 mg•L-1) in the Bosten Lake. Concentrations of POC and DOC near the inlet and outlet of the lake were similar to those in the Kaidu River, but much lower than the average values of the lake. Our analysis suggested that there might be a transformation of CO3 2-to HCO3- in the Bosten Lake in recent 30 years. There was no significant correlation between soil carbon content and POC or DOC, which suggested that the effect of soil on carbon content in Bosten Lake water was not significant.

Key words: particulate organic carbon, dissolved organic carbon, soil carbon, dissolved ions, spatial distribution, Bosten Lake, Xinjiang