地理科学 ›› 2011, Vol. 31 ›› Issue (9): 1131-1137.doi: 10.13249/j.cnki.sgs.2011.09.1131

• 论文 • 上一篇    下一篇

渭干河灌区地下水埋深与矿化度时空分布动态

吐尔逊·艾山1,2, 塔西甫拉提·特依拜1, 买买提·阿扎提3, 买买提依明·买买提1   

  1. 1. 新疆大学资源与环境科学学院新疆绿洲生态教育部重点实验室, 新疆 乌鲁木齐 830046;
    2. 新疆农业 资源区划办公室, 新疆 乌鲁木齐 830002;
    3. 阿克苏地区渭干河流域管理局, 新疆 库车县 842100
  • 收稿日期:2010-09-23 修回日期:2011-01-19 出版日期:1997-09-20 发布日期:1997-09-20
  • 通讯作者: 塔西甫拉提·特依拜。E-mail:tash@xju.edu.cn E-mail:tash@xju.edu.cn
  • 基金资助:
    国家自然科学基金项目(40961025、 40901163)、新疆自然科学基金项目(200821128)资助。

Spatial and Temporal Dynamic Distribution of Groundwater Depth and Mineralization in Weigan River Irrigation District

TURSUN·Hasan1,2, TASHPOLAT·Tiyip1, MAMAT·Gazat3, MAMTIMIN·Mamat1   

  1. 1. Key Laboratory of Oasis Ecology, Ministry of Education, College of Resource and Environment Sciences, Xinjiang University, Urumqi, Xinjiang 830046, China;
    2. Xinjiang Agricultural Resources and Regional Planning Office, Urumqi, Xinjiang 830004, China;
    3. Management Bureau of Ugan River Basin, Aksu Region, Kuqa, Xinjiang 842100, China
  • Received:2010-09-23 Revised:2011-01-19 Online:1997-09-20 Published:1997-09-20

摘要: 以新疆渭干河灌区为例,利用渭干河灌区38眼监测井的1997~2007年期间地下水埋深和地下水矿化度数据,对渭干河灌区地下水位及地下水矿化度的年际变化、季节变化动态及空间分布特征及其变化原因进行初步的分析。结果表明:11 a期间,研究区春季地下水位最高,研究区地下水位从灌区上部往下部或边缘有明显的上升特征。地下水矿化度的整体趋势为灌区上游的矿化度值较低,灌区下游和边缘地区的矿化度较高。灌区年均地下水位和地下水矿化度总体上有下降趋势。

Abstract: Taking Xinjiang Weigan River irrigation district as an example, 38 observation wells’ data from 1997 to 2007 of groundwater depth and groundwater mineralization were used in the paper to analyze annual change of groundwater depth and the groundwater mineralization of Weigan River irrigation district, and their seasonal dynamics and spatial distribution. The results showed that in the 11 years period, the highest groundwater level appeared in spring. The groundwater level rose significantly from the top of irrigation district to the periphery of the oasis. The overall trend of groundwater mineralization is that groundwater mineralization is relatively low in the upper reaches of the irrigation district, and relatively high in the lower edge and downstream of the irrigation district. The annual groundwater depth and groundwater mineralization generally decreased in the irrigation district.

中图分类号: 

  • K928.4