Salt deliquescence along boulder cracks in the Antarctic Dry Valleys: An overlooked source of moisture for rock weathering processes-Reference-Cited by-同舟云学术

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Salt deliquescence along boulder cracks in the Antarctic Dry Valleys: An overlooked source of moisture for rock weathering processes

Published:2023-09 Issue: Volume:437 Page:108800
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Ben-Asher M.,Mushkin A.,Lensky N.G.,Amit R.,Eppes M.C.,Ming D.W.,Shelef E.,Sletten R.S.

Funder

National Science Foundation

National Aeronautics and Space Administration

NSF EAR

United States-Israel Binational Science Foundation

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference80 articles.

1. Stages and rate of the gravel shattering process by salts in desert Reg soils;Amit;Geoderma,1993

2. Fracture Mechanics: Fundamentals and Applications;Anderson,2005

3. Subcritical crack growth in geological materials;Atkinson;J. Geophys. Res.,1984

4. Production rate of cosmogenic 21Ne in quartz estimated from 10Be, 26Al, and 21Ne concentrations in slowly eroding Antarctic bedrock surfaces;Balco;Earth Planet. Sci. Lett.,2009

5. Origins of sulphate in Antarctic dry-valley soils as deduced from anomalous 17O compositions;Bao;Nature,2000

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