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Contour scaling of a sandstone by salt weathering under simulated hot desert conditions
Author(s) -
Smith B. J.,
McGreevy J. P.
Publication year - 1988
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/esp.3290130804
Subject(s) - weathering , geology , cracking , salt (chemistry) , scaling , mineralogy , distilled water , sodium , block (permutation group theory) , materials science , geochemistry , composite material , chemistry , metallurgy , geometry , chromatography , mathematics
A laboratory study has been used to investigate relationships between salts and contour scaling—a weathering feature commonly observed on rock surfaces in salt‐rich environments. Surface disaggregation and essentially surface‐parallel cracks were produced in sandstone blocks using 10 per cent solutions of sodium sulphate and magnesium sulphate applied daily to single exposed surfaces for sixty days. A control block soaked once in saturated magnesium sulphate and subsequently wetted daily with distilled water showed extensive surface disaggregation, but no cracking. Both surface disaggregation and subsurface cracking were associated with relative concentrations of microcrystalline salt. A tentative model of contour scaling is proposed, which involves linking together potential cracks by salt‐induced fracturing of intervening, crack‐stopping grains. Further control blocks treated respectively with 10 per cent and saturated sodium chloride showed no evidence of subsurface cracking and only limited surface disaggregation of the ‘saturated’ block.