干旱区生态环境知识资源中心(Arid): 基于地下水恢复的塔里木河下游生态需水量估算

Arid

	基于地下水恢复的塔里木河下游生态需水量估算
其他题名	Evaluation on ecological water requirement in the lower reaches of Tarim River based on groundwater restoration
	白元 1; 徐海量1 ; 张青青 1; 叶茂 2
来源期刊	生态学报
ISSN	1000-0933
出版年	2015
卷号	35 期号:3 页码:630-640
中文摘要	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20002010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。20042010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7.0610~8 m~3,其中,齐文阔尔河段为4.9810~8 m~3,老塔里木河段为2.0910~8 m~3,地下水恢复至生态水位4.5 m需要58a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 hm~2)的生态需水量为0.58710~8 m~3,保护下游地下水响应带天然植被面积(41439.85 hm~2)的生态需水量为0.21*10~8 m~3。
英文摘要	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 7.0610~8m~3,including 4.9810~8m~3 from Daxihaizi reservoir to Taitema Lake and 2.0910~8 m~3 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 0.58710~8m~3 to meet up with the requirement of the total area of 96114.09 hm~2 of natural vegetation strip from Daxihai reservoir to Taitema Lake. Moreover, the amount of ecological water requirement is 0.21*10~8m~3 for the natural vegetation protection zone of 41439.85 hm~2 in the area of the groundwater level responding to the ecological water conveyance.
中文关键词	生态需水量 ; 地下水恢复 ; 植被 ; 塔里木河下游
英文关键词	ecological water requirement undergroundwater restoration vegetation the lower reaches of Tarim River
语种	中文
国家	中国
收录类别	CSCD
WOS类目	BIOLOGY
WOS研究方向	Life Sciences & Biomedicine - Other Topics
CSCD记录号	CSCD:5346268
来源机构	中国科学院新疆生态与地理研究所 ; 新疆师范大学
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/233142
作者单位	1.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, 乌鲁木齐, 新疆 830011, 中国; 2.新疆师范大学地理科学与旅游学院, 乌鲁木齐, 新疆 830054, 中国
推荐引用方式 GB/T 7714	白元,徐海量,张青青,等. 基于地下水恢复的塔里木河下游生态需水量估算[J]. 中国科学院新疆生态与地理研究所, 新疆师范大学,2015,35(3):630-640.
APA	白元,徐海量,张青青,&叶茂.(2015).基于地下水恢复的塔里木河下游生态需水量估算.生态学报,35(3),630-640.
MLA	白元,et al."基于地下水恢复的塔里木河下游生态需水量估算".生态学报 35.3(2015):630-640.