The exponential decline in saturated hydraulic conductivity with depth: a novel method for exploring its effect on water flow paths and transit time distribution-Reference-Cited by-同舟云学术

The exponential decline in saturated hydraulic conductivity with depth: a novel method for exploring its effect on water flow paths and transit time distribution

Published:2016-03-20 Issue:14 Volume:30 Page:2438-2450
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Ameli A. A.¹²³,McDonnell J. J.²⁴,Bishop K.³⁵

Affiliation:

1. Department of Biology University of Western Ontario Ontario Canada

2. Global Institute for Water Security University of Saskatchewan Saskatoon Canada

3. Department of Earth Sciences, Air Water and Landscape Sciences Uppsala University Uppsala Sweden

4. School of Geosciences University of Aberdeen Aberdeen UK

5. Department of Aquatic Sciences and Assessment Swedish University of Agricultural Sciences, (SLU) Uppsala Sweden

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10777

Reference65 articles.

1. Performance assessment of low-order versus high-order numerical schemes in the numerical simulation of aquifer flow

2. Semianalytical series solutions for three-dimensional groundwater-surface water interaction

3. Are all runoff processes the same? Numerical experiments comparing a Darcy-Richards solver to an overland flow-based approach for subsurface storm runoff simulation

4. Series solutions for saturated–unsaturated flow in multi-layer unconfined aquifers

5. The role of topography in controlling throughflow generation

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