塔里木河下游生态输水对地下水埋深变化的影响

doi:10.12118/j.issn.1000–6060.2021.03.07

干旱区地理 ›› 2021, Vol. 44 ›› Issue (3): 651-658.doi: 10.12118/j.issn.1000–6060.2021.03.07

• 塔里木河流域生态与环境 • 上一篇下一篇

塔里木河下游生态输水对地下水埋深变化的影响

陈永金¹(),艾克热木·阿布拉²,张天举^3,⁴(),陈亚鹏³,朱成刚³,程勇²,刘璐^3,⁴,李肖杨^3,⁴,张齐飞^3,⁴

1.聊城大学环境与规划学院,山东聊城 252059
2.新疆塔里木河流域管理局,新疆库尔勒 841000
3.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
4.中国科学院大学,北京 100049

收稿日期:2021-02-07 修回日期:2021-04-21 出版日期:2021-05-25 发布日期:2021-06-01
通讯作者: 张天举
作者简介:陈永金（1968-）,男,副教授,主要从事生态系统修复等方面研究. E-mail: chenyongjin@lcu.edu.cn
基金资助:
科技部科技基础资源调查专项(2019FY100203)

Effects of ecological water conveyance on groundwater depth in the lower reaches of Tarim River

CHEN Yongjin¹(),Aikeremu Abula²,ZHANG Tianju^3,⁴(),CHEN Yapeng³,ZHU Chenggang³,CHENG Yong²,LIU Lu^3,⁴,LI Xiaoyang^3,⁴,ZHANG Qifei^3,⁴

1. School of Environment and Planning, Liaocheng University, Liaocheng 252059, Shandong, China
2. Xinjiang Tarim River Basin Authority, Korla 841000, Xinjiang, China
3. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China
4. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2021-02-07 Revised:2021-04-21 Online:2021-05-25 Published:2021-06-01
Contact: Tianju ZHANG

摘要/Abstract

摘要：

地下水是维系荒漠河岸植被生存、生长的关键因子,对于退化植被的恢复具有重要的意义。结合塔里木河下游生态输水过程中地下水埋深的实测数据,详尽分析了2000—2020年地下水埋深的时空变化及对生态输水的响应。监测结果显示：在生态输水条件下,塔里木河下游河道两侧地下水埋深大幅抬升。（1）在纵向上,自上游段的英苏、中游段的喀尔达依,至下游段的依干不及麻,在距河道100 m处,地下水埋深分别由输水前的7.76 m、9.31 m、7.82 m抬升至3.70 m、4.48 m和2.69 m;在距河道300 m处,地下水埋深分别由输水前的8.09 m、9.15 m、8.25 m抬升至4.53 m、5.00 m和3.29 m;在距河道500 m处,地下水埋深分别由输水前的8.21 m、9.45 m、9.08 m抬升至6.61 m、5.46 m和3.82 m。（2）在垂直于河道方向上,根据地下水井监测数据,生态输水对塔里木河下游的上、中、下3个区段地下水位的影响范围均达到了1050 m,分别抬升了2.69 m、1.38 m、1.59 m。（3）生态输水前期（2000—2009年）,上、中段地下水位抬升迅速,2009年以后,下游段依干不及麻地下水位抬升幅度明显高于英苏（0.88~4.65 m）和喀尔达依（0.53~4.07 m）。并且,70.5%监测井地下水位波动趋于稳定,说明间歇性的生态输水有助于抬高地下水埋深,是地下水补给的主要来源,对于维持地下水较高水位的动态平衡具有一定的促进作用。

关键词: 生态输水, 地下水位, 断面, 塔里木河

Abstract:

Groundwater is a key factor for maintaining the survival and growth of desert riparian vegetation, which is essential for the restoration of degraded vegetation. In this study, based on the measured data of groundwater depth in the process of ecological water conveyance in the lower reaches of Tarim River in Xinjiang, China, the temporal and spatial changes of groundwater as well as its response to ecological water conveyance from 2000 to 2020 are analyzed. The monitoring results showed that groundwater depth on both sides of the lower reaches of Tarim River rose significantly under the condition of ecological water conveyance. (1) In the longitudinal direction, from Yingsu in the upstream section and Kaldayi in the middle section to Yiganyuma in the downstream section, at 100 m away from the river, the groundwater depth rises from 7.76 m, 9.31 m, 7.82 m to 3.70 m, 4.48 m and 2.69 m after water conveyance, respectively; at 300 m away from the river, the groundwater depth rises from 8.09 m, 9.15 m, 8.25 m to 4.53 m, 5.00 m and 3.29 m after water conveyance, respectively; at 500 m away from the river, the groundwater depth rises from 8.21 m, 9.45 m, 9.08 m to 6.61 m, 5.46 m and 3.82 m after water conveyance, respectively. (2) In the vertical direction of the river, according to the monitoring data of underground wells, the influence range of ecological water conveyance on the groundwater depth of the upper, middle, and lower reaches of Tarim River reached 1050 m and water level rising of 2.69 m, 1.38 m and 1.59 m, respectively. (3) In the early stage of ecological water conveyance (2000—2009), the groundwater depth in the upper and middle reaches of the river rose rapidly. After 2009, the groundwater depth in the lower reaches of the river was significantly higher than that in Yingsu (0.88-4.65 m) and Kaldayi (0.53-4.07 m). Moreover, the groundwater depth fluctuation of 70.5% monitoring wells tended to be stable. It shows that intermittent ecological water conveyance is helpful in raising the groundwater depth, which is the main source of groundwater recharge and has a certain role in maintaining the dynamic balance of higher groundwater levels.

Key words: ecological water conveyance, groundwater depth, section, Tarim River

陈永金,艾克热木·阿布拉,张天举,陈亚鹏,朱成刚,程勇,刘璐,李肖杨,张齐飞. 塔里木河下游生态输水对地下水埋深变化的影响[J]. 干旱区地理, 2021, 44(3): 651-658.

CHEN Yongjin,Aikeremu Abula,ZHANG Tianju,CHEN Yapeng,ZHU Chenggang,CHENG Yong,LIU Lu,LI Xiaoyang,ZHANG Qifei. Effects of ecological water conveyance on groundwater depth in the lower reaches of Tarim River[J]. Arid Land Geography, 2021, 44(3): 651-658.

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参考文献 31

[1]	陈永金, 刘加珍, 陈亚宁, 等. 输水前后塔里木河下游物种多样性与水因子的关系[J]. 生态学报, 2013,33(7):2212-2224.
	[ Chen Yongjin, Liu Jiazhen, Chen Yaning, et al. Analysis of the relationship between species diversity and hydrologic factors during an interval of intermittent water delivery at the lower reaches of Tarim River, China[J]. Acta Ecologica Sinica, 2013,33(7):2212-2224. ]
[2]	徐海量, 宋郁东, 李卫红, 等. 生态输水后塔里木河下游地下水水盐动态变化[J]. 干旱区资源与环境, 2004,18(3):63-67.
	[ Xu Hailiang, Song Yudong, Li Weihong, et al. The dynamics of water and salt after ecological water transport to the lower reaches of Tarim River[J]. Journal of Arid Land Resources and Environment, 2004,18(3):63-67. ]
[3]	陈亚宁, 李稚, 范煜婷, 等. 西北干旱区气候变化对水文水资源影响研究进展[J]. 地理学报, 2014,69(9):1295-1304. doi: 10.11821/dlxb201409005
	[ Chen Yaning, Li Zhi, Fan Yuting, et al. Research progress on the impact of climate change on water resources in the arid region of northwest China[J]. Acta Geographica Sinica, 2014,69(9):1295-1304. ] doi: 10.11821/dlxb201409005
[4]	陈亚宁, 徐宗学. 全球气候变化对新疆塔里木河流域水资源的可能性影响[J]. 中国科学(地球科学), 2004,34(11):1047-1053.
	[ Chen Yaning, Xu Zongxue. Possible impacts of global climate change on water resources in Tarim River Basin, Xinjiang[J]. Scientia Sinica (Earth Sciences), 2004,34(11):1047-1053. ]
[5]	孙天瑶, 李雪梅, 许民, 等. 2000—2018年塔里木河流域植被覆盖时空格局[J]. 干旱区地理, 2020,43(2):415-1424.
	[ Sun Tianyao, Li Xuemei, Xu Min, et al. Spatial-temporal variations of vegetation coverage in the Tarim River Basin from 2000 to 2018[J]. Arid Land Geography, 2020,43(2):415-1424. ]
[6]	Engels J G, Jensen K. Patterns of wetland plant diversity along estuarine stress gradients of the Elbe (Germany) and Connecticut (USA) Rivers[J]. Plant Ecology & Diversity, 2009,2(3):301-311.
[7]	Wang Y G, Deng C Y, Liu Y, et al. Identifying change in spatial accumulation of soil salinity in an inland river watershed, China[J]. Science of the Total Environment, 2018,621:177-185. doi: 10.1016/j.scitotenv.2017.11.222
[8]	崔旺诚, 李卫红, 徐海量. 塔里木河下游输水与生态保育[J]. 干旱区地理, 2004,27(2):172-178.
	[ Cui Wangcheng, Li Weihong, Xu Hailiang. Research on the response scope of natural vegetation in the lower reaches of Tarim River after water transport[J]. Arid Land Geography, 2004,27(2):172-178. ]
[9]	李丽君, 张小清, 陈长清, 等. 近20 a塔里木河下游输水对生态环境的影响[J]. 干旱区地理, 2018,41(2):238-247.
	[ Li Lijun, Zhang Xiaoqing, Chen Changqing, et al. Ecological effects of water conveyance on the lower reaches of Tarim River in recent twenty years[J]. Arid Land Geography, 2018,41(2):238-247. ]
[10]	蔚亮, 李均力, 包安明, 等. 塔里木河下游湿地面积时序变化及对生态输水的响应[J]. 植物生态学报, 2020,44(6):616-627. doi: 10.17521/cjpe.2019.0267
	[ Yu Liang, Li Junli, Bao Anming, et al. Temporal areal changes of wetlands in the lower reaches of the Tarim River and their responses to ecological water conveyance[J]. Chinese Journal of Plant Ecology, 2020,44(6):616-627. ] doi: 10.17521/cjpe.2019.0267
[11]	李梦怡, 邓铭江, 凌红波, 等. 塔里木河下游水生态安全评价及驱动要素分析[J]. 干旱区研究, 2021,38(1):39-47.
	[ Li Mengyi, Deng Mingjiang, Ling Hongbo, et al. Evaluation of ecological water security and analysis of driving factor in the lower Tarim River[J]. Arid Zone Research, 2021,38(1):39-47. ]
[12]	王珊珊, 王金林, 周可法, 等. 塔里木河下游土地利用/覆被变化对生态输水的响应[J]. 水资源保护, 2021,37(2):69-74, 80.
	[ Wang Shanshan, Wang Jinlin, Zhou Kefa, et al. Response of land use/land cover change to ecological water transmission in the lower reach of Tarim River[J]. Water Resources Protection, 2021,37(2):69-74, 80. ]
[13]	夏力哈尔·俄坦. 塔里木河干流地下水变化动态研究[J]. 水利科技与经济, 2020,26(9):10-15.
	[ Harlechhal Ertan. Study on the dynamic change of groundwater in the main stream of Tarim River[J]. Water Conservancy Science and Technology and Economy, 2020,26(9):10-15. ]
[14]	刘迁迁, 古力米热·哈那提, 王光焰, 等. 间歇性生态输水塔里木河下游断面地下水位变化模拟[J]. 生态学报, 2018,38(15):5519-5528.
	[ Liu Qianqian, Gulimire Hanati, Wang Guangyan, et al. Simulation of sectional groundwater level variation in the lower reaches of Tarim River under intermittent ecological water conveyance[J]. Acta Ecologica Sinica, 2018,38(15):5519-5528. ]
[15]	刘迁迁, 古力米热·哈那提, 苏里坦, 等. 塔里木河下游河岸带地下水埋深对生态输水的响应过程[J]. 干旱区地理, 2017,40(5):979-986.
	[ Liu Qianqian, Gulimire Hanati, Sulitan, et al. Response process of groundwater table to ecological water conveyance in the lower reaches of Tarim River riparian zone[J]. Arid Land Geography, 2017,40(5):979-986. ]
[16]	努热曼古丽·图尔荪, 玉米提·哈力克, 塔吉古丽·艾麦提. 生态输水对塔里木河下游地下水变化的影响分析[J]. 宁夏农林科技, 2014,55(7):58-60.
	[ Nuremanguli Tuersun, Umut Halik, Tajiguli Aimaiti. An analysis on effects of ecological water transportation on groundwater changes of lower reaches of Tarim River[J]. Ningxia Journal of Agriculture and Forestry Science and Technology, 2014,55(7):58-60. ]
[17]	马剑, 刘贤德, 李广, 等. 祁连山北麓中段青海云杉林土壤水热时空变化特征[J]. 干旱区地理, 2020,43(4):1033-1040.
	[ Ma Jian, Liu Xiande, Li Guang, et al. Spatial and temporal variations of soil moisture and temperature of Picea crassifolia forest in north piedmont of central Qilian Mountains[J]. Arid Land Geography, 2020,43(4):1033-1040. ]
[18]	刘睿明, 孔东升, 王立, 等. 黑河湿地自然保护区沼泽湿地地下水埋深和土壤水分时空分布规律[J]. 草业科学, 2019,36(9):2223-2232.
	[ Liu Ruiming, Kong Dongsheng, Wang Li, et al. Spatial and temporal distribution of groundwater depth and soil moisture in marsh wetland across the Heihe Wetland Nature Reserve[J]. Pratacultural Science, 2019,36(9):2223-2232. ]
[19]	张钧泳, 丁建丽, 谭娇. 基于SVM的绿洲荒漠交错带土壤水分与地下水埋深反演[J]. 农业机械学报, 2019,50(3):221-230.
	[ Zhang Junyong, Ding Jianli, Tan Jiao. Inversion of soil moisture and shallow groundwater depth based on SVM in arid oasis-desert ecotone[J]. Transactions of the Chinese Society for Agricultural Machinery, 2019,50(3):221-230. ]
[20]	武敏, 冯绍元. 不同地下水埋深土壤水分入渗规律研究[J]. 灌溉排水学报, 2019,38(增刊):79-81.
	[ Wu Min, Feng Shaoyuan. Study on soil water infiltration law under different water tables[J]. Journal of Irrigation and Drainage, 2019,38(Suppl. 1):79-81. ]
[21]	李小倩, 夏江宝, 赵西梅, 等. 不同潜水埋深下浅层土壤的水盐分布特征[J]. 中国水土保持科学, 2017,15(2):43-50.
	[ Li Xiaoqian, Xiao Jiangbao, Zhao Ximei, et al. Water and salt distribution characteristics of shallow soil at different diving water levels[J]. Science of Soil and Water Conservation, 2017,15(2):43-50. ]
[22]	马晓东, 李卫红, 朱成刚, 等. 塔里木河下游土壤水分与植被时空变化特征[J]. 生态学报, 2010,30(15):4035-4045.
	[ Ma Xiaodong, Li Weihong, Zhu Chenggang, et al. Spatio-temporal variation in soil moisture and vegetation along the lower reaches of Tarim River, China[J]. Acta Ecologica Sinica, 2010,30(15):4035-4045. ]
[23]	杜伟宏, 管文轲, 霍艾迪, 等. 塔里木河干流胡杨林下土壤的水盐特征研究[J]. 西南林业大学学报(自然科学), 2019,39(5):92-99.
	[ Du Weihong, Guan Wenke, Huo Aidi, et al. Water and salt characteristics of soil under Populus euphratica forest in the main stream of Tarim River[J]. Journal of Southwest Forestry University (Natural Sciences), 2019,39(5):92-99. ]
[24]	朱成刚, 李卫红, 马建新, 等. 塔里木河下游地下水位对柽柳叶绿素荧光特性的影响[J]. 应用生态学报, 2010,21(7):1689-1696.
	[ Zhu Chenggang, Li Weihong, Ma Jianxin, et al. Effects of groundwater level on chlorophyll fluorescence characteristics of Tamarix hispida in lower reaches of Tarim River[J]. Chinese Journal of Applied Ecology, 2010,21(7):1689-1696. ]
[25]	王建宏. 塔里木河流域干旱区地下水生态调节与监测预警分析[J]. 河南水利与南水北调, 2020,49(2):13-15, 26.
	[ Wang Jianhong. Analysis on ecological regulation, monitoring and early warning on groundwater in arid area of Tarim River Basin[J]. Henan Water Resources & South-to-North Water Diversion, 2020,49(2):13-15, 26. ]
[26]	唐建, 王光焰, 徐生武. 塔里木河干流生态廊道时空变化及保护对策[J]. 水利规划与设计, 2020(8):49-53.
	[ Tang Jian, Wang Guangyan, Xu Shengwu. Spatio-temporal change and protection plan of ecological corridor along mainstream of Tarim River[J]. Water Resources Planning and Design, 2020(8):49-53. ]
[27]	李均力, 肖昊, 沈占锋, 等. 2013—2018年塔里木河下游植被动态变化及其对生态输水的响应[J]. 干旱区研究, 2020,37(4):985-992.
	[ Li Junli, Xiao Hao, Shen Zhanfeng, et al. Vegetation changes during the 2013—2018 period and its response to ecological water transport in the lower reaches of the Tarim River[J]. Arid Zone Research, 2020,37(4):985-992. ]
[28]	任强, 龙爱华, 杨永民, 等. 近20年塔里木河干流生态环境变化遥感监测分析[J]. 水利水电技术, 2021,52(3):103-111.
	[ Ren Qiang, Long Aihua, Yang Yongmin, et al. Analysis on remote sensing monitoring of eco-environment variation of main stream basin of Tarim River in recent 20 years[J]. Water Resources and Hydropower Engineering, 2021,52(3):103-111. ]
[29]	阿迪力江·买买提. 浅析塔里木河流域综合治理及生态输水成效[J]. 水电与新能源, 2020,34(7):57-59, 63.
	[ Adeline Maimaiti. Comprehensive management and ecological water supply in Tarim River Basin[J]. Hydropower and New Energy, 2020,34(7):57-59, 63. ]
[30]	霍天赐, 颜伟, 马晓飞. 内陆河尾闾湖泊水域面积变化及驱动因素研究——以台特玛湖地区为例[J]. 国土资源遥感, 2020,32(3):149-156.
	[ Huo Tianci, Yan Wei, Ma Xiaofei. A study of the variation and driving factors of the water area of the terminal lake of inland river: A case study of Taitema Lake region[J]. Remote Sensing for Land & Resources, 2020,32(3):149-156. ]
[31]	沈海岑, 薛联青. 基于土地利用变化的塔里木河下游区近20 a景观生态风险研究[J]. 中国农村水利水电, 2020(11):77-82.
	[ Shen Haicen, Xue Lianqing. Landscape ecological risk assessment of the lower reaches of Tarim River based on land use change in recent 20 years[J]. China Rural Water and Hydropower, 2020(11):77-82. ]

塔里木河下游生态输水对地下水埋深变化的影响

Effects of ecological water conveyance on groundwater depth in the lower reaches of Tarim River

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年份	地下水埋深/m
年份	英苏	喀尔达依	依干不及麻
2010	7.88	7.98	7.08
2020	5.19	6.60	5.49
抬升	2.69	1.38	1.59

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