Characterizing the heterogeneity of karst critical zone and its hydrological function: An integrated approach

Xi Chen*, Zhicai Zhang, Chris Soulsby, Qinbo Cheng, Andrew Binley, Rui Jiang, Min Tao

*Corresponding author for this work

Research output: Contribution to journalArticle

10 Citations (Scopus)

Abstract

Spatial heterogeneity in the subsurface of karst environments is high, as evidenced by the multiphase porosity of carbonate rocks and complex landform features that result in marked variability of hydrological processes in space and time. This includes complex exchange of various flows (e.g., fast conduit flows and slow fracture flows) in different locations. Here, we integrate various “state-of-the-art” methods to understand the structure and function of this poorly constrained critical zone environment. Geophysical, hydrometric, and tracer tools are used to characterize the hydrological functions of the cockpit karst critical zone in the small catchment of Chenqi, Guizhou Province, China. Geophysical surveys, using electrical resistivity tomography (ERT), inferred the spatial heterogeneity of permeability in the epikarst and underlying aquifer. Water tables in depression wells in valley bottom areas, as well as discharge from springs on steeper hillslopes and at the catchment outlet, showed different hydrodynamic responses to storm event rainwater recharge and hillslope flows. Tracer studies using water temperatures and stable water isotopes (δD and δ18O) could be used alongside insights into aquifer permeability from ERT surveys to explain site- and depth-dependent variability in the groundwater response in terms of the degree to which “new” water from storm rainfall recharges and mixes with “old” pre-event water in karst aquifers. This integrated approach reveals spatial structure in the karst critical zone and provides a conceptual framework of hydrological functions across spatial and temporal scales.

Original languageEnglish
Pages (from-to)2932-2946
Number of pages15
JournalHydrological Processes
Volume32
Issue number19
Early online date8 Aug 2018
DOIs
Publication statusPublished - 15 Sep 2018

Fingerprint

integrated approach
karst
aquifer
hillslope
tomography
electrical resistivity
recharge
tracer
catchment
permeability
fracture flow
geophysical survey
conceptual framework
rainwater
carbonate rock
water
landform
water table
water temperature
hydrodynamics

Keywords

  • cockpit karst
  • critical zone
  • geophysical survey
  • hydrological functions
  • stable isotopes
  • tracers

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

Characterizing the heterogeneity of karst critical zone and its hydrological function : An integrated approach. / Chen, Xi; Zhang, Zhicai; Soulsby, Chris; Cheng, Qinbo; Binley, Andrew; Jiang, Rui; Tao, Min.

In: Hydrological Processes, Vol. 32, No. 19, 15.09.2018, p. 2932-2946.

Research output: Contribution to journalArticle

Chen, Xi ; Zhang, Zhicai ; Soulsby, Chris ; Cheng, Qinbo ; Binley, Andrew ; Jiang, Rui ; Tao, Min. / Characterizing the heterogeneity of karst critical zone and its hydrological function : An integrated approach. In: Hydrological Processes. 2018 ; Vol. 32, No. 19. pp. 2932-2946.
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abstract = "Spatial heterogeneity in the subsurface of karst environments is high, as evidenced by the multiphase porosity of carbonate rocks and complex landform features that result in marked variability of hydrological processes in space and time. This includes complex exchange of various flows (e.g., fast conduit flows and slow fracture flows) in different locations. Here, we integrate various “state-of-the-art” methods to understand the structure and function of this poorly constrained critical zone environment. Geophysical, hydrometric, and tracer tools are used to characterize the hydrological functions of the cockpit karst critical zone in the small catchment of Chenqi, Guizhou Province, China. Geophysical surveys, using electrical resistivity tomography (ERT), inferred the spatial heterogeneity of permeability in the epikarst and underlying aquifer. Water tables in depression wells in valley bottom areas, as well as discharge from springs on steeper hillslopes and at the catchment outlet, showed different hydrodynamic responses to storm event rainwater recharge and hillslope flows. Tracer studies using water temperatures and stable water isotopes (δD and δ18O) could be used alongside insights into aquifer permeability from ERT surveys to explain site- and depth-dependent variability in the groundwater response in terms of the degree to which “new” water from storm rainfall recharges and mixes with “old” pre-event water in karst aquifers. This integrated approach reveals spatial structure in the karst critical zone and provides a conceptual framework of hydrological functions across spatial and temporal scales.",
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