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基于地下水恢复的塔里木河下游生态需水量估算
引用本文:白元,徐海量,张青青,叶茂.基于地下水恢复的塔里木河下游生态需水量估算[J].生态学报,2015,35(3):630-640.
作者姓名:白元  徐海量  张青青  叶茂
作者单位: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;中国科学院大学;新疆师范大学地理科学与旅游学院
基金项目:国家自然科学基金(41171427,31370551,41101534)
摘    要:为探明生态输水后地下水响应带范围及地下水恢复下生态需水量,以塔里木河下游大西海子水库至台特玛湖段为研究区,基于2000—2010年生态输水和地下水埋深分布特征,分析了塔里木河下游生态输水后两岸地下水位恢复状况,并借助遥感和地理信息系统技术对研究区生态需水量进行了研究。结果表明:塔河下游地下水位的抬升幅度与输水量的大小呈一定的正相关关系,并存在一定的时效性。2004—2010年地下水处于长期的负均衡状态,多年下降幅度明显。塔河下游英苏、喀尔达依、阿拉干和依干不及麻断面地下水响应幅度分别为1195、1050、2281 m和1000 m。历经11a输水后,塔里木河下游地下水总恢复需水量为7.06×108m3,其中,齐文阔尔河段为4.98×108m3,老塔里木河段为2.09×108m3,地下水恢复至生态水位4.5m需要5—8a的时间。保护塔里木河下游大西海子以下所有天然植被面积(96114.09 hm2)的生态需水量为0.587×108m3,保护下游地下水响应带天然植被面积(41439.85 hm2)的生态需水量为0.21×108m3。

关 键 词:生态需水量  地下水恢复  植被  塔里木河下游
收稿时间:2013/5/7 0:00:00
修稿时间:2014/11/10 0:00:00

Evaluation on ecological water requirement in the lower reaches of Tarim River based on groundwater restoration
BAI Yuan,XU Hailiang,ZHANG Qingqing and YE Mao.Evaluation on ecological water requirement in the lower reaches of Tarim River based on groundwater restoration[J].Acta Ecologica Sinica,2015,35(3):630-640.
Authors:BAI Yuan  XU Hailiang  ZHANG Qingqing and YE Mao
Institution:BAI Yuan;XU Hailiang;ZHANG Qingqing;YE Mao;Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,State Key Laboratory of Desert and Oasis Ecology;University of Chinese Academy of Sciences;School of Geography Science and Tourism,Xinjiang Normal University;
Abstract:Located in the extremely arid region, Tarim River is the longest continental river in the northwest of China where the environment is vulnerable. Since the construction of Daxihaizi Reservoir in 1970''s, the river channel in the lower reaches of Tarim River with 321km distances from the Daxihaizi Reservoir to Tatema Lake has been dried up for more than thirty years. Cut-off of river water along the lower Tarim River and the excessive and unbridled utilization of water resources resulted in a series of ecological environment problems such as groundwater level decline, natural vegetation deterioration, desertification acceleration and so on, which has been accelerating environmental degradation and strongly influenced local agricultural development. In order to conserve the natural vegetation and further to control the desertification and restore the severely degraded ecosystem, an emergency plan-the ecological water conveyance project (EWCP) for synthetically harnessing deteriorate ecological environment were implemented in the lower Tarim River since 2000. After 12 times of ecological water conveyance (The deadline is January 2011), the groundwater level showed some degree of raising along the main river channel of the lower reaches of Tarim River.Groundwater level has played a key role in the degraded natural vegetation restoration due to the natural vegetation growth mostly depended on groundwater in extremely arid region. Ecological water requirement in the river channel along the lower Tarim river was highly related to elevation of the groundwater level while the elevation of groundwater level is supplemented from the EWCP. To estimate the requirement of the ecological water, firstly two main river along lower Tarim River channels were set up, including the new river channel from Daxihaizi reservoir to Taitema Lake and the old river channel from Daxihaizi reservoir to Alagan, then to analyze the response range of groundwater level to the ecological water conveyance and evaluate the ecological water requirement based on the groundwater restoration by investigating the response width of groundwater restoration after the ecological water conveyance. The phreatic evaporation method was applied to analyze the ecological water requirement in virtue of the Remote Sensing and GIS techniques. The results showed that: (1) The range of groundwater level change was positively related with the amount of water transferring to the channel in the Lower Tarim River. It was charactered by a temporal hysteresis with the response of the groundwater level to the amount of watering to the river channel. The groundwater level decreased obviously from 2004 to 2010, and that was in a negative equilibrium state. The response range of the groundwater to water transfer was 1195 metres, 1050 metres, 2281 metres, and 1000 metres in the transections of Yusu, Kaerdayi, Alagan, and Yiganbujima respectively. (2) After 12 times (for 11 years) of ecological water conveyance in the lower reaches of Tarim River, the total amount of water requirement based on the groundwater restoration was 7.06×108 m3, including 4.98×108 m3 from Daxihaizi reservoir to Taitema Lake and 2.09×108 m3 from Daxihaizi reservoir to Alagan transaction. And it needs about 5 to 8 years that the groundwater depth elevate to 4.5m (equal to ecological groundwater level).(3) The amount of ecological water requirement for the natural vegetation protection is 0.587×108 m3 to meet up with the requirement of the total area of 96114.09 hm2 of natural vegetation strip from Daxihai reservoir to Taitema Lake. Moreover, the amount of ecological water requirement is 0.21×108 m3 for the natural vegetation protection zone of 41439.85 hm2 in the area of the groundwater level responding to the ecological water conveyance.
Keywords:ecological water requirement  undergroundwater restoration  vegetation  the lower reaches of Tarim River
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