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Soil Structure Degradation and Mellowing of Compacted Soils by Saline‐Sodic Solutions
Author(s) -
Barzegar A. Rahman,
Oades J. Malcolm,
Rengasamy Pichu
Publication year - 1996
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1996.03615995006000020035x
Subject(s) - sodium adsorption ratio , wetting , soil water , soil science , chemistry , soil structure , analytical chemistry (journal) , materials science , mineralogy , chromatography , geology , agronomy , composite material , drip irrigation , irrigation , biology
Aggregates are formed by joining of structural units of different sizes in a hierarchical order. During wetting, the aggregates may either disintegrate completely (slaking) or remain intact with only loosening at the points of weakness (mellowing). This study investigated the effect of saline‐sodic solutions with sodium adsorption ratio (SAR) of 5 and 20 and electrical conductivity (EC) of 0.1 to 4 dS m ‐1 after a number of wetting‐drying cycles on soil mellowing. A Vertic Palexeralf with a coefficient of linear extensibility (COLE) value of 0.15 and a Typic Haploxeralf with COLE of 0.05 were studied. Using a Ca solution, the degree of aggregation in both soils was improved about two times in >50 and 20‐ to 50‐µm aggregates compared with the original soils. The values for the Vertic Palexeralf were three times those of the Typic Haploxeralf. In contrast, sodic solutions led to the collapse of aggregates. Mellowing ratios of aggregates changed after 10 wetting‐drying cycles and were ≈0.6 to 0.7 for SAR 5 and 0.8 to 1 for SAR 20 for the Vertic Palexeralf; for the Typic Haploxeralf they were 0.7 to 0.8 and 0.9 to 1.2 for SARs 5 and 20, respectively. Mellowing ratios between 0.9 and 1 were obtained for the Vertic Paleoxeralf minicores using solutions of SAR 20 and EC 0.1 dS m ‐1 . The mellowing ratio was 0.2 when a solution of SAR 5 and EC 4 dS m ‐1 was used. In soils where aggregates collapsed without hierarchical breakdown, mellowing ratios were always higher, indicating structural degradation.