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Volume 32 Issue 1
Mar.  2013
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Article Navigation >  CARSOLOGICA SINICA  > 2013  >  32(1): 7-13
PU Jun bing, YUAN Dao xian. Karst Hyporheic Zone and the scientific progress[J]. CARSOLOGICA SINICA, 2013, 32(1): 7-13. doi: 10.3969/j.issn.1001-4810.2013.01.002
Citation: PU Jun bing, YUAN Dao xian. Karst Hyporheic Zone and the scientific progress[J]. CARSOLOGICA SINICA, 2013, 32(1): 7-13. doi: 10.3969/j.issn.1001-4810.2013.01.002
shu

Karst Hyporheic Zone and the scientific progress

doi: 10.3969/j.issn.1001-4810.2013.01.002

  • 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

  • Received Date: 2013-02-19
  • Publish Date: 2013-03-25
    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.

     

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