Watershed Characterization and Hydrograph Recession Analysis: A Comparative Look at a Karst vs. Non-Karst Watershed and Implications for Groundwater Resources in Gaolan River Basin, Southern China
| Autor: | Zejun Wang, Mukhtar Habib, Hamza Jakada, Hong Zhou, Zhihua Chen, Mingming Luo |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2019 |
| Předmět: |
Watershed
lcsh:Hydraulic engineering 010504 meteorology & atmospheric sciences Groundwater flow genetic structures Geography Planning and Development 0207 environmental engineering Aquifer Hydrograph 02 engineering and technology Aquatic Science 01 natural sciences Biochemistry Interflow lcsh:Water supply for domestic and industrial purposes lcsh:TC1-978 Streamflow groundwater 020701 environmental engineering 0105 earth and related environmental sciences Water Science and Technology watershed Hydrology geography lcsh:TD201-500 geography.geographical_feature_category hydrograph recession analysis karst Karst GIS Environmental science Groundwater |
| Zdroj: | Water, Vol 11, Iss 4, p 743 (2019) Water Volume 11 Issue 4 |
| ISSN: | 2073-4441 |
| Popis: | Karst watersheds are often treated as non-karst watersheds that can lead to several hazards. Hence, how do karst watersheds differ from non-karst watersheds and what are the effects of karstification on groundwater availability and quality? In this study, we contrast between a karst and non-karst watershed by elucidating their geomorphological peculiarities and potential impact on spatio-temporal availability and quality of groundwater. GIS morphometric mapping and hydrograph recession analysis are applied to map the watershed features and estimate hydrograph recession coefficient to define the groundwater drainage characteristics as well as the influence of karst drainage attributes (KDA). Furthermore, we characterize streamflow components based on the hydrograph recession limbs (segments) and infer their contributing geomorphological factors. Results show that the karst watershed has higher recession coefficients for successive recession limbs. Consequently, it drains larger volumes of groundwater primarily due to the KDAs, which transmit interflow and groundwater flow more rapidly through large cavities to springs as well as stream channels. The KDAs generate what we term karst drainage flow (KDF), defined by the second recession limb which has high recession coefficient as the first limb (overland flow) and strongly contrasts with the non-karst watershed from visual and ANOVA analysis. The effect is that karst aquifer yield over time is significantly lower and highly exposed to pollution compared to the non-karst aquifer. Consequently, sustainable water management practices should be adopted to ensure the availability and safety of groundwater reserves. |
| Databáze: | OpenAIRE |
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