PDF Download

[1]SHANG Hai-min,WANG Wen-ke,DUAN Lei,et al.Simulation on Groundwater Regulation Based on Ecological Water Table in the Northern Foot of Tianshan Mountain[J].Research of Soil and Water Conservation,2014,21(06):144-147.

Copy

Simulation on Groundwater Regulation Based on Ecological Water Table in the Northern Foot of Tianshan Mountain

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 21 Number of periods: 2014 06 Page number: 144-147 Column: Public date: 2014-12-28

Title:: Simulation on Groundwater Regulation Based on Ecological Water Table in the Northern Foot of Tianshan Mountain

Author(s):: SHANG Hai-min¹, WANG Wen-ke¹, DUAN Lei¹, HUO Chuan-ying²; 1. Key Laboratory of Subsurface Hydrology and Ecology in Arid Areas, Ministry of Education, Chang’an University, Xi’an 710054, China;
2. Institute of Geological Environment Monitoring, Xinjiang Uygur Autonomous Region, Urumqi 830000, China

Keywords:: groundwater; ecological water table; numerical simulation; northern foot of Tianshan Mountain

CLC:: X143

DOI:: -

Abstract:: To coordinate development between sustainable utilization of groundwater resources and supergene ecology, ecological water depth was drawn from 3 m to 6 m based on field survey and previous achievements. In the current and regulated exploitation of groundwater resources, potential ecological effects induced by water-level fluctuations were compared and analyzed by numerical simulation. Results of this study indicated that negative effects of supergene ecology had been not only induced in the current exploitation of groundwater resources, but also lots of water resources had been wasted. Furthermore, the coordinated development could be achieved by regulating groundwater status. The calculated threshold values of groundwater exploitation were 0.73 billion m³/a, 1.64 billion m³/a and 0.24 billion m³/a in the piedmont Gobi, alluvial plain and desert edge, respectively.

References:: [1] Su Y Z, Zhao W Z, Su P X, et al. Ecological effects of desertification control and desertified land reclamation in an oasis-desert ecotone in an arid region:a case study in Hexi Corridor, northwest China[J]. Ecological Engineering,2007,29(2):117-124.
[2] 柴政,玉米提,哈力克,等.新疆柴窝堡水源地地下水超采引发的环境问题[J].水土保持研究,2008,15(5):132-135.
[3] Jeevarathinam C, Rajasekar S, Sanjuan M A F. Vibrational resonance in groundwater-dependent plant ecosystems[J]. Ecological Complexity,2013,15:33-42.
[4] Chui T F M, Low S Y, Liong S Y. An ecohydrological model for studying groundwater-vegetation interactions in wetlands[J]. Journal of Hydrology,2011,409(1):291-304.
[5] Song G, Chen Y, Tian M, et al. The ecological vulnerability evaluation in southwestern mountain region of China based on GIS and AHP method[J]. Procedia Environmental Sciences,2010(2):465-475.
[6] 杨泽元,王文科.干旱半干旱区地下水引起的生态效应的研究现状与发展趋势[J].干旱区地理,2009,32(5):739-745.
[7] Zhao C, Wang Y, Chen X I, et al. Simulation of the effects of groundwater level on vegetation change by combining FEFLOW software[J]. Ecological Modelling,2005,187(2):341-351.
[8] 孙才志,刘玉兰,杨俊.下辽河平原地下水生态水位与可持续开发调控研究[J].吉林大学学报:地球科学版,2007,37(2):249-254.
[9] 张惠昌.干旱区地下水生态平衡埋深[J].勘察科学技术,1992(6):9-13.
[10] 周绪,刘志辉,戴维,等.干旱区地下水位降幅对天然植被衰退过程的影响分析:以新疆鄯善南部绿洲群为例[J].水土保持研究,2006,13(3):143-145.
[11] Wang W, Yang Z, Kong J, et al. Ecological impacts induced by groundwater and their thresholds in the arid areas in Northwest China[J]. Environmental Engineering and Management Journal,2013,12(7):1497-1507.
[12] 程东会,王文科,侯光才,等.毛乌素沙地植被与地下水关系[J].吉林大学学报:地球科学版,2012,42(1):184-189.
[13] 王文科,杨泽元,程东会,等.面向生态的干旱半干旱地区区域地下水资源评价的方法体系[J].吉林大学学报:地球科学版,2011,41(1):159-167.
[14] Bear J. Dynamics of Fluids in Porous Media[M]. New York:Courier Dover Publications, 2013.

Similar References:

Memo

Last Update: 1900-01-01