水土资源

塔里木河下游生态输水策略分析

  • 杨鹏年 ,
  • 吴文强 ,
  • 买合木提·巴拉提 ,
  • 魏光辉
展开
  • 1.新疆农业大学水利与土木工程学院,新疆 乌鲁木齐 830052;
    2.中国水利水电科学研究院,北京 100038;
    3.新疆维吾尔自治区塔里木河流域管理局干流管理处,新疆 库尔勒 841000
杨鹏年(1966-),男,副教授,主要从事干旱区水资源利用研究. E-mail:Ypn10@163.com

收稿日期: 2013-12-24

  修回日期: 2014-03-20

  网络出版日期: 2014-09-25

基金资助

国家自然科学基金(51009128);新疆塔里木河流域管理局项目“塔里木河下游生态保护目标及措施研究”与新疆维吾尔自治区水文学及水资源重点学科基金(xjswszyzdxk20101202)联合资助

Strategy of Ecological Water Conveyance to the Lower Reaches of Tarim River, Xinjiang, China

  • YANG Peng-nian ,
  • WU Wen-qiang ,
  • MAIHEMUTI Balati ,
  • WEI Guang-hui
Expand
  • 1. College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China;
    2. China Institute of Water Resources and Hydropower Research, Beijing 100038, China;
    3. Department of Mainstream, Tarim River Basin Authority, Korla 84100, Xinjiang, China

Received date: 2013-12-24

  Revised date: 2014-03-20

  Online published: 2014-09-25

摘要

自2000年5月至2011年间的12次生态输水,对塔里木河下游地下水恢复发挥了重要的作用。截至到2011年10月的实测数据,相较于输水前,英苏、阿拉干、库尔干和老英苏各断面的地下水位均有不同程度的上升,上升幅度与离河距离相关。距河1 km处的上升幅度分别为2.0、3.0、4.0 m和1.0 m左右,地下水位均有较明显的恢复。当地下水埋深达到4.0、3.5 m和3.0 m时,与此相对应的植被生存状态分别称之为维持生存、基本生存与适合生存。由此可以计算出,塔里木河下游距河1.0 km范围内3种植被生存状态对应的耗水量分别为1.6×108、2.2×108 m3和2.7×108 m3。大西海子水库以下的下泄水量可分别在春、秋、冬季3个时段进行。据此,近期的输水策略为:年输水量应维持在2.7×108 m3以上,输水适宜时段为春、夏季,以尽快恢复下游地下水环境并逐步满足河畔植被适合生存的耗水量;远期输水则可视上游来水的情况,采用满足维持生存、基本生存与适合生存3种耗水量的交替输水方式,输水量的下限为1.6×108 m3,以达到有限水资源条件下提高水资源利用率与维持生态系统稳定的目标。

本文引用格式

杨鹏年 , 吴文强 , 买合木提·巴拉提 , 魏光辉 . 塔里木河下游生态输水策略分析[J]. 干旱区研究, 2014 , 31(5) : 785 -791 . DOI: 10.13866/j.azr.2014.05.01

Abstract

Ecological degeneration in the Green Corridor in lower reaches of the Tarim River was mainly caused by the 30-year last stream cutoff downstream from the Daxihaizi Reservoir in lower reaches of the Tarim River from 1972. From May 2000 to 2011, 12 times ecological water conveyance were implemented so as to rise the groundwater level and improve the ecology in the lower reaches. The observed data up to October 2011 showed that the groundwater level along the Yengisu, Aragan, Korgan and old Yengisu sections of was risen up to a certain degree compared with that before implementing the project. Groundwater level near the river was risen by 3.5 m, 6.0 m, 5.0 m and 3.0 m along these sections above respectively, but by 2.0 m, 3.0 m, 4.0 m and 1.0 m at the places 1 km away from the river. Namely, the rising extent of groundwater level was closely related to the distance away from the river. As a result, the groundwater level was obviously risen up. When the groundwater depth was risen to 4.0 m, 3.5 m and 3.0 m respectively, the vegetation survival conditions were accordingly called the “survival maintaining conditions”, “basic survival conditions” and “suitable survival conditions”. On which it was calculated that the water consumptions of vegetation within a wide extent 1 km away from the river were 1.6×108 m3, 2.2×108 m3 and 2.7×108 m3 respectively. Water release from the Daxihaizi Reservoir could be scheduled in spring, summer and winter for germination of plant seeds and regeneration of Populus euphratica. The annual water release of 2.7×108 m3 should be maintained in recent years so as to improve the groundwater environment in the lower reaches and to meet water consumption of vegetation at the suitable survival level.

参考文献

〔1〕 段建军,王彦国,王晓风,等.1957—2006年塔里木河流域气候变化和人类活动对水资源和生态环境的影响〔J〕.冰川冻土,2009,31(5):781-790.〔Duan Jianjun,Wang Yanguo,Wang Xiaofeng,et al.Impact of climate change and human activities on the water resources and ecological environments in the Tarim River Basin in 1957-2006〔J〕.Journal of Glaciology and Geocryology,2009,31(5):781-790.〕
〔2〕 陈忠升,陈亚宁,徐长春.近50 a来塔里木河干流年径流量变化趋势及预测〔J〕.干旱区地理,2011,34(1):43-51.〔Chen Zhongsheng,Chen Yaning,Xu Changchun.Change trend and prediction of annual runoff in mainstream area of the Tarim R iver in recent 50 years〔J〕.Arid Land Geography,2011,34(1):43-51.〕
〔3〕 叶朝霞,陈亚宁,张霞,等.塔里木河断流与未来水文情势分析〔J〕.干旱区地理,2009,32(6):841-849〔Ye Zhaoxia,Chen Yaning,Zhang Xia,et al.Dried-up river way of Tarim River and the future state of hydrology〔J〕.Arid Land Geography,2009,32(6):841-849.〕
〔4〕 叶茂,徐海量,任铭.塔里木河下游生态输水的合理时间初探〔J〕.干旱区研究,2012,29(5):907-912.〔Ye Mao,Xu Hailiang,Ren Ming.Primary study on the rational time of ecological water conveyance to lower reaches of the Tarim River〔J〕.Arid Zone Research,2012,29(5):907-912.〕
〔5〕 刘新华,徐海量,凌红波,等.塔里木河下游生态需水估算〔J〕.中国沙漠,2013,33(4):1 198-1 205.〔Liu Xinhua,Xu Hailiang,Ling Hongbo,et al.Ecological water requirements in the lower reaches of the Tarim River〔J〕.Journal of Desert Research,2013,33(4):1 198-1 205.〕
〔6〕 樊自立,徐海量,傅荩仪,等.塔里木河下游生态保护目标和措施〔J〕.中国沙漠,2013,33(4):1 191-1 197.〔Fan Zili,Xu Hailiang,Fu Jinyi,et al.Ecological protection objects and restoration measures in the Lower Reaches of Tarim River〔J〕.Journal of Desert Research,2013,33(4):1 191-1 197.〕
〔7〕 陈永金,李卫红,陈亚宁,等.塔里木河流域综合治理的生态效应〔J〕.中国环境科学,2007,27(1):24-28.〔Chen Yongjin,Li Weihong,Chen Yaning,et al.Ecological effect of synthesized governing in Tarim River valley〔J〕.China Environmental,2007,27(1):24-28.〕
〔8〕 杨鹏年,张胜江,董新光.塔里木河干流下游生态输水后水量转化特征〔J〕.干旱区研究,2007,24(2):174-178.〔Yang Pengnian,Zhang Shengjiang,Dong Xinguang.Study on the characteristics of water conversion after conveying stream water to the lower reaches of the Tarim River for regenerating the ecology〔J〕.Arid Zone Research,2007,24(2):174-178.〕
〔9〕 陈连勤,刘耻非,于庆和,等.塔里木河干流流域水文地质及地下水开发利用调查〔R〕.乌鲁木齐:新疆维吾尔自治区地质矿产局第一勘察院,1990:83-88.〔Chen Lianqin,Liu Chifei,Yu Qinghe,et al.The Surveys of Hydrogeology and Groundwater Exploitation in the Mainstream of Tarim River Basin〔R〕.Urumqi:The First Survey Institute of Hydrogeology of the Mineral Bureau in Xinjiang Uygur Autonomous Region,1990:83-88.〕
〔10〕 郝兴明,陈亚宁,李卫红.新疆塔里木河下游物种多样性与地下水位的关系〔J〕.生态学报,2007,27(10):4 106-4 112.〔Hao Xingming,Chen Yaning,Li Weihong.The relationship between species diversity and groundwater table in the low reaches of the Tarmi River,Xinjiang,China〔J〕.Acta Ecologica Sinica,2007,27(10):4 106-4 112.〕
〔11〕 蒋良群,陈曦,包安明.塔里木河下游地下水变化动态分析〔J〕.干旱区地理,2005,28(1):33-37.〔Jiang Liangqun,Chen Xi,Bao Anming.Analysis on the changing dynamics of groundwater level in the lower reaches of the Tarim River,Xinjiang〔J〕.Arid Land Geography,2005,28(1):33-37.〕
〔12〕 宋郁东,樊自立,雷志栋,等.中国塔里木河水资源与生态问题研究〔M〕.乌鲁木齐:新疆人民出版社,2000:401-405.〔Song Yudong,Fan Zili,Lei Zhidong,et al.Research on Water Resources and Ecology of Tarim River〔M〕.Urumqi:Xinjiang People's Press,2000:401-405.〕
〔13〕 黄金廷,侯光才,尹立河,等.干旱半干旱区天然植被的地下水水文生态响应研究〔J〕.干旱区地理,2011,34(5):787-793〔Huang Jinting,Hou Guangcai,Yin Lihe,et al.Eco-hydrological response of natural vegetation in arid and semi-arid area:A review〔J〕.Arid Land Geography,2011,34(5):787-793〕.
〔14〕 杨鹏年.塔里木河下游间歇输水条件下地下水恢复与植被响应研究〔D〕.乌鲁木齐:新疆农业大学,2005.〔Yang Pengnian.Study on Restoration of Groundwater and Vegetation in Lower reaches of Tarim River After Intermittent Water Release〔D〕.Urumqi:Xinjiang Agricultural University,2005.〕
〔15〕 何斌,陈亚宁,李卫红,等.塔里木河下游地区胡杨蒸腾耗水规律及其对生态输水的响应〔J〕.资源科学,2009,31(9):1 545-1 552.〔He Bin,Chen Yaning,Li Weihong,et al.Analysis of the variation of transpiration of Popular euphratica and its response to ecological water supply at the Lower Reaches of Tarim River〔J〕.Resources Science,2009,31(9):1 545-1 552.〕
〔16〕 刘加珍,陈亚宁,李卫红,等.塔里木河下游植物群落分布与衰退演替趋势分析〔J〕.生态学报,2004,24(2):379-383.〔Liu Jiazhen,Chen Yaning,Li Weihong,et al.Analysis on the distribution and degraded succession of plant communities at lower reaches of Tarim River〔J〕.Acta Ecologica Sinica,2004,24(2):379-383.〕
〔17〕 李卫红,陈永金,陈亚鹏,等.新疆塔里木河下游生态输水对地下水位和水质的影响〔J〕.资源科学,2006,28(5):157-163.〔Li Weihong,Chen Yongjin,Chen Yapeng,et al.Effects of ecological stream water transfusion on groundwater level and quality in the lower reaches of the Tarim River〔J〕.Resources Science,2006,28(5):157-163.〕
〔18〕 芦艳玲,叶朝霞.塔里木河下游地下水位对生态输水的响应〔J〕.干旱区研究,2012,29(4):574-578.〔Lu Yanling,Ye Zhaoxia.Response of groundwater level to the ecological water conveyance in the Lower Reaches of Tarim River〔J〕.Arid Zone Research,2012,29(4):574-578.〕
〔19〕 唐晓岚,杜瑶.干旱区生态治理及绿色基础设施构建:以新疆塔里木河下游为例〔J〕.干旱区研究,2011,28(3):413-420.〔Tang Xiaolan,Du Yao.Study on ecological management and building of green infrastructure in arid area〔J〕.Arid Zone Research,2011,28(3):413-420.〕
文章导航

/