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2000—2014年塔里木河下游地下水补给量及合理需求量
引用本文:王希义,徐海量,潘存德,凌红波,郭宏伟.2000—2014年塔里木河下游地下水补给量及合理需求量[J].水资源保护,2017,33(4):32-39.
作者姓名:王希义  徐海量  潘存德  凌红波  郭宏伟
作者单位:;1.新疆农业大学草业与环境科学学院;2.中国科学院新疆生态与地理研究所
基金项目:国家自然科学基金(31370551,41471099,31400466);中国科学院“西部之光”人才培养计划(XBBS-2014-13)
摘    要:以塔里木河下游为研究区,以区域内9个固定监测断面为基础,依据断面内各个地下水监测井,收集了输水前和第15次输水后的地下水位数据,结合土壤饱和差计算方法,分析了第15次输水后的地下水补给量,并联系植被生长所需的合理水位探讨了地下水到达合理水位所需的水量,以期评价生态输水的阶段性效果,为调整生态输水方案提供理论参考。结果表明:(1)生态输水前地下水埋深在6~13 m之间,第15次生态输水后,地下水最大升高幅度达到8.26 m;(2)第15次生态输水后,塔里木河下游地下水补给量约为20.44亿m3;(3)为使地下水达到植被生长所需适宜水位,塔里木河下游地下水的合理需求量约为24.08亿m3。

关 键 词:生态输水  合理水位  补给量  合理需求量  塔里木河下游
收稿时间:2016/12/9 0:00:00

Study on groundwater recharge amount and suitable demand amount in lower reaches of Tarim River from 2000 to 2014
WANG Xiyi,XU Hailiang,PAN Cunde,LING Hongbo and GUO Hongwei.Study on groundwater recharge amount and suitable demand amount in lower reaches of Tarim River from 2000 to 2014[J].Water Resources Protection,2017,33(4):32-39.
Authors:WANG Xiyi  XU Hailiang  PAN Cunde  LING Hongbo and GUO Hongwei
Affiliation:College of Grassland and Environment Sciences, Xinjiang Agricultural University, Urumqi 830052, China,Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China,College of Grassland and Environment Sciences, Xinjiang Agricultural University, Urumqi 830052, China,Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China and Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
Abstract:The lower reaches of the Tarim River was selected as the study area. First, the data of groundwater level were collected before water transport and after the water transport was carried out 15 times, based on the locations of groundwater monitoring wells at nine sections. Then, the groundwater recharge amount after the 15th time of water transport was analyzed using the calculation method of saturation deficit of soil. Finally, the suitable demand amount of groundwater that enables the groundwater level to reach a water level suitable for plant growth was determined. This study aimed to evaluate the effects of ecological water transport at different stages and provide theoretical references for the adjustment of water transport. The results are as follows: (1)the depth to water table ranged from 6 m to 13 m before ecological water transport, and its maximum increment reached 8. 26 m after the 15th time of water transport; (2)the recharge amount of groundwater was about 20. 44 × 108 m3 in the lower reaches of the Tarim River after the 15th time of water transport; and(3)the suitable amount of groundwater in the lower reaches of the Tarim River should be about 24. 08 × 108 m3, in order to guarantee the suitable water level for plant growth.
Keywords:ecological water transport  suitable water level  recharge amount  suitable demand amount  lower reaches of Tarim River
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