Spatial Heterogeneity Enables Higher Root Water Uptake in Dry Soil but Protracts Water Stress After Transpiration Decline: A Numerical Study
Author:
Affiliation:
1. Chair of Soil Physics University of Bayreuth Bayreuth Germany
2. Potsdam Institute for Climate Impact Research (PIK) Leibniz Association Potsdam Germany
Publisher
American Geophysical Union (AGU)
Subject
Water Science and Technology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019WR025501
Reference64 articles.
1. Quantifying preferential flow in soils: A review of different techniques
2. Plant roots use a patterning mechanism to position lateral root branches toward available water
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4. A physically based model of heterogeneous hillslopes: 2. Effective hydraulic conductivities
5. Root hairs enable high transpiration rates in drying soils
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