Subsurface permeability contrasts control shallow groundwater flow dynamics in the critical zone of a glaciated, headwater catchment-Reference-Cited by-同舟云学术

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Subsurface permeability contrasts control shallow groundwater flow dynamics in the critical zone of a glaciated, headwater catchment

Published:2022-09 Issue:9 Volume:36 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Benton Joshua R.¹²^ORCID,McGuire Kevin J.³^ORCID,Schreiber Madeline E.¹^ORCID

Affiliation:

1. Department of Geosciences Virginia Tech Blacksburg Virginia USA

2. North Carolina Geological Survey Swannanoa North Carolina USA

3. Department of Forest Resources and Environmental Conservation and Virginia Water Resources Research Center Virginia Tech Blacksburg Virginia USA

Funder

Division of Earth Sciences

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14672

Reference63 articles.

1. Variable‘active’ versus‘contributing’ areas or periods: a necessary distinction

2. Hydrometeorological database for Hubbard Brook Experimental Forest: 1955-2000

3. Influence of landscape position and transient water table on soil development and carbon distribution in a steep, headwater catchment

4. Mineral Weathering and Podzolization Control Acid Neutralization and Streamwater Chemistry Gradients in Upland Glaciated Catchments, Northeastern United States

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Interflow, subsurface stormflow and throughflow: A synthesis of field work and modelling;Hydrological Processes;2024-09

2. Temporal and spatial variation in shallow groundwater gradients in a boreal headwater catchment;Journal of Hydrology;2023-11

3. Development of a lateral topographic weathering gradient in temperate forested podzols;Geoderma;2023-11

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