Journal
HYDROLOGICAL PROCESSES
Volume 34, Issue 15, Pages 3156-3174Publisher
WILEY
DOI: 10.1002/hyp.13829
Keywords
-
Categories
Funding
- National Key Research and development Program of China [2016YFC0502602]
- National Natural Science Foundation of China [41571130071, 41971028]
- UK Natural Environment Research Council [NE/N007468/1]
- NERC [NE/N007468/1] Funding Source: UKRI
Ask authors/readers for more resources
Hydrological and biogeochemical processes in karst environments are strongly controlled by heterogeneous fracture-conduit networks. Quantifying the spatio-temporal variability of water transit time and young water fractions in such heterogeneous hydrogeological systems is fundamental to linking discharge and water quality dynamics in the karst critical zone. We used a tracer-aided conceptual hydrological model to track the fate of each hour of rain input individually. Using this approach, the variability of transit time distributions and young water fraction were estimated in the main landscape units in a karst catchment of Chenqi in Guizhou Province, Southwest China. The model predicted that the mean young water (i.e.,
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available