Hydrological functioning of thawing soil water in a permafrost‐influenced alpine meadow hillslope
Abstract The complex variation of the hydrological functioning of soil water has been widely studied using measurements of the stable isotopic composition of either the bulk soil water (BSW) collected by the cryogenic vacuum extraction method or the mobile soil water (MSW) collected by the zero‐tens...
Main Authors: | Xiong Xiao, Fan Zhang, Xiaoyan Li, Guanxing Wang, Chen Zeng, Xiaonan Shi |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2020-01-01
|
Series: | Vadose Zone Journal |
Online Access: | https://doi.org/10.1002/vzj2.20022 |
Similar Items
-
Field experimental study on the effect of thawed depth of frozen alpine meadow soil on rill erosion by snowmelt waterflow
by: Ying Zheng, et al.
Published: (2024-03-01) -
Experimental study on the effects of multiple factors on spring meltwater erosion on an alpine meadow slope
by: Xiaonan Shi, et al.
Published: (2020-06-01) -
Soil respiration of alpine meadow is controlled by freeze–thaw processes of active layer in the permafrost region of the Qinghai–Tibet Plateau
by: J. Wang, et al.
Published: (2020-09-01) -
Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon
by: Michelle A Walvoord, et al.
Published: (2019-01-01) -
Soil Moisture but Not Warming Dominates Nitrous Oxide Emissions During Freeze–Thaw Cycles in a Qinghai–Tibetan Plateau Alpine Meadow With Discontinuous Permafrost
by: Zhe Chen, et al.
Published: (2021-06-01)