2010
DOI: 10.1016/j.geoderma.2010.07.016
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Soil dry aggregate stability and wind erodible fraction in a semiarid environment of Argentina

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Cited by 134 publications
(60 citation statements)
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“…The SOC can promote macroaggregation and increase the aggregate stability through biological and physicochemical bonding mechanisms (Tisdall and Oades, 1982;Colazo and Buschiazzo, 2010). Our results cannot be directly compared with other studies as there is limited information on CC effects on soil properties in the central Great Plains under no-till conditions.…”
Section: Cover Cropmentioning
confidence: 79%
“…The SOC can promote macroaggregation and increase the aggregate stability through biological and physicochemical bonding mechanisms (Tisdall and Oades, 1982;Colazo and Buschiazzo, 2010). Our results cannot be directly compared with other studies as there is limited information on CC effects on soil properties in the central Great Plains under no-till conditions.…”
Section: Cover Cropmentioning
confidence: 79%
“…As noted earlier, this would suggest that better soils also have higher resistance against land degradation, albeit that other unobserved effects might be at play as well. The reason that productive soils are more resistant against degradation processes like water (Stanchi et al, 2015) and wind erosion (Herrick and Beh, 2015) is closely related to prevailing aggregate stability (Colazo and Buschiazzo, 2010) that determines important soil production properties like infiltration and permeability while protecting soils against dispersive water and wind forces (Jozefaciuk and Czachor, 2014;Geng et al, 2015). Organic matter that acts as a binding agent and nucleus in the formation of aggregates is the most important component of soil aggregate stability.…”
Section: Resultsmentioning
confidence: 99%
“…The soils of central Argentina are semiarid with a variable moisture regime and humidity restricted to part of the year. This region is generally characterized by poorly developed soils, with little horizon differentiation which are highly drained, with low water-holding capacity and organic matter content (Colazo et al 2010). Due to its poor structure, this soil is highly susceptible to wind and water erosion in vast areas of the region (Peña Zubiate and D'hiriart 2005; Colazo et al 2010).…”
Section: Introductionmentioning
confidence: 99%