Karst Hyporheic Zone及其研究进展

蒲俊兵; 袁道先

Karst Hyporheic Zone及其研究进展

中国地质科学院岩溶地质研究所/国土资源部、广西壮族自治区岩溶动力学重点实验室/国土资源部岩溶生态系统与石漠化治理重点实验室

基金项目: 国家自然科学基金(41202185,41072192);国土资源部公益性行业科研专项(201311148);中国地质调查局地质调查项目(12120113006700)和IGCP/SIDA598项目联合资助

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出版历程
- 收稿日期: 2013-02-19
- 刊出日期: 2013-03-25

Karst Hyporheic Zone and the scientific progress

Institute of Karst Geology，CAGS / Key Laboratory of Karst Dynamics, Ministry of Land and Resources＆ Guangxi/Key Laboratory of Karst Ecological System and Treatment of Rocky Desertification, Ministry of Land and Resources＆Guangxi

摘要

摘要: Karst Hyporheic Zone(笔者将之译为“岩溶交互带”)是近三年来新出现的一个岩溶术语,我国尚未开展“岩溶交互带”的研究工作,它主要是指岩溶地下水与周边岩溶基质(含沉积物、基岩)水之间物质能量活跃交替的地带。本文从“岩溶交互带”的概念来源、含义、最新的研究进展和监测技术发展等方面进行了总结,并就现存的问题和未来研究提出了看法。
- “岩溶交互带” /
- 岩溶术语 /
- 科学意义
Abstract: Karst Hyporheic Zone is a new terminology put forward in the recent 3 years. Karst Hyporheic Zone is an active zone of material and energy exchange in karst flow between karst conduit and matrix. It plays an important role in conduit matrix fluid exchange, biogeochemical processing, karst development, micro scale water cycle, microbial processing, contaminant sequestration and transformation. This article reviews the development of Karst Hyporheic Zone, scientific implications and research advancement as well as monitoring technology. Some ideas for further studies on Karst Hyporheic Zone are also proposed.
- Karst Hyporheic Zone /
- karst terminology /
- scientific implications Origin of the tufa at Jiuzhaigou scenic spot in Sichuan

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参考文献(23)

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