全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地球学报  2006 

太行山前平原地下调蓄能力研究

DOI: 10.3975/cagsb.2006.02.15

Keywords: 山前平原,地下调蓄能力,多元指标量化,南水北调

Full-Text   Cite this paper   Add to My Lib

Abstract:

本文通过地下调蓄库容、受水能力、给水能力和地表汇水输水条件的指标等级量化,建立的百分制多元指标评价方法比较客观地量化出太行山山前平原5个洪积扇区、8个靶区的地下调蓄能力及其可利用性。综合评价结果,石景山—大兴靶区、石家庄—晋县靶区和邢台靶区可作为南水北调地下调蓄首选目标,房山—容城靶区、望都—定县—新乐靶区和磁县—安阳靶区可作为南水北调地下调蓄的主要备选场所,邯郸靶区和辉县—新乡靶区适宜作为井灌小型地下调蓄场所。

References

[1]  Marios Sophocleous,Interactions between groundwater and surface water: the state of the science,Hydrogeology journal?,2002, 10(1).
[2]  Richard W. Healy ;Peter G. Cook,Using groundwater levels to estimate recharge,Hydrogeology journal?,2002, 10(1).
[3]  Jacobus J. de Vries ;Ian Simmers,Groundwater recharge: an overview of processes and challenges,Hydrogeology journal?,2002, 10(1).
[4]  Ward Sanford,Recharge and groundwater models: an overview,Hydrogeology journal?,2002, 10(1).
[5]  徐曙光;王淑梅,太行山前平原南水北调地下调蓄潜力与效益的科技查新报告(编号2003-002),北京:科学出版社,2003.
[6]  Zhang Zonghu;Zhang Guanghui.The evolution of continental water cyclic system and its environmental significance[J].Acta Geoscientia Sinica,2001(04)
[7]  Zhang Guanghui;Fei Yuhong;Wang Jinzhe.Evolution characteristics and trend of shoallow groundwater recharge in Taihangshan piedmont plain over the last 300 years[J].Acta Geoscientia Sinica,2003(03)
[8]  Herman Bouwer,Artificial recharge of groundwater: hydrogeology and engineering,Hydrogeology journal?,2002, 10(1).
[9]  张宗祜;张光辉.大陆水循环系统演化及其环境意义[J].地球学报,2001(04)
[10]  籍传茂;王兆兴,地下水资源的可持续利用,北京:地质出版社,1999.
[11]  朱尔明,南水北调工程,北京:商务印书馆,2001.
[12]  Zhang Guanghui;Fei Yuhong;Nie Zhenlong.The evolution regularity of groundwater in piedmont clinoplain of Taihang Mountains since Holocene[J].Acta Geoscientia Sinica,2000(02)
[13]  张光辉;费宇红;王金哲.300年以来太行山前平原地下水补给演化特征与趋势[J].地球学报,2003(03)
[14]  张光辉;费宇红;聂振龙.全新世来太行山前平原地下水演化规律[J].地球学报,2000(02)

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133