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- W2133519229 abstract "Abstract In an incubation experiment, a sandy top soil was mixed with kaolinite- or smectite-rich clay soil at 15, 22.5 and 30% clay addition rates. Compared to sandy soil alone, smectite clay soil addition at 22.5 and 30% reduced cumulative respiration per g organic C whereas kaolinite clay soil addition had no effect. This can be explained by the higher surface area and cation exchange capacity of the smectite compared to kaolinite clay soil which protects native organic C from decomposition by binding. Keywords: Kaolinite, organic C sequestration, respiration, smectite. 1. Introduction Sandy soils have low water and nutrient retention capacity compared to finer textured soils. Addition of clay soils to sandy soil has been shown to increase water and nutrient retention and thereby plant growth ( Hall et al ., 2010). It could also increase organic C retention because binding to clay particles and occlusion within aggregates reduces organic C accessibility to decomposers ( 2007). It has been" @default.
- W2133519229 created "2016-06-24" @default.
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- W2133519229 date "2014-01-01" @default.
- W2133519229 modified "2023-09-30" @default.
- W2133519229 title "Respiration in mixes of sandy and clay soils: influence of clay type and addition rate" @default.
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- W2133519229 doi "https://doi.org/10.4067/s0718-95162014005000070" @default.
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