2002
DOI: 10.1081/css-120005763
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Organic matter mobilization as affected by soil-solution composition and prevailing clay minerals

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Cited by 5 publications
(2 citation statements)
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“…Soil salinity causes soil organic matter (OM) flocculation, which leads to OM loss due to wind erosion and leaching (Artiola and Walworth, 2009;Kida et al, 2017;Martinez et al, 2002;Wong et al, 2010). Salinity not only accelerates the decrease of soil OM but also increases the accumulation of harmful trace elements in plants (Ondrasek et al, 2012), inhibits the microbial activity in soils (Setia et al, 2014), and delays the decomposition of soil organic residues (Peinemann et al, 2005).…”
mentioning
confidence: 99%
“…Soil salinity causes soil organic matter (OM) flocculation, which leads to OM loss due to wind erosion and leaching (Artiola and Walworth, 2009;Kida et al, 2017;Martinez et al, 2002;Wong et al, 2010). Salinity not only accelerates the decrease of soil OM but also increases the accumulation of harmful trace elements in plants (Ondrasek et al, 2012), inhibits the microbial activity in soils (Setia et al, 2014), and delays the decomposition of soil organic residues (Peinemann et al, 2005).…”
mentioning
confidence: 99%
“…The first is that these soils and rocks contain large amounts of calcium in primary calcareous minerals. The second is that, among other cations, Ca ++ is easily absorbed by clay minerals, especially humic substances (Martínez et al 2007). The high content of Ca ++ in the lower horizons of both soils was mostly due to the calcareous rock material, while the sharp decrease in Ca ++ in the B1 and lower horizons can be explained by the drop in the humus content.…”
Section: Exchangeable Cations and Salt Regimementioning
confidence: 99%