2012
DOI: 10.1016/j.crte.2011.12.001
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Analysis of an illustrative interaction between structural features and earthworm populations in Brazilian ferralsols

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Cited by 4 publications
(2 citation statements)
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“…The main characteristics of the soil are its advanced degree of weathering and high contents of iron oxides (greater than 180 g kg À1 ), aluminium, 1:1 clay minerals (kaolinite) and quartz (Reatto et al, 2008), which are characterised by low-activity clay, little differentiation among horizons, and a strong and well developed microgranular structure comprising angular and subangular microaggregates (Reatto et al, 2009;Brossard et al, 2012). These microaggregates are organised into micropeds that are smaller than 1 mm, with a porous massive structure according to Volland-Tuduri et al (2005).…”
Section: Experimental Designmentioning
confidence: 99%
“…The main characteristics of the soil are its advanced degree of weathering and high contents of iron oxides (greater than 180 g kg À1 ), aluminium, 1:1 clay minerals (kaolinite) and quartz (Reatto et al, 2008), which are characterised by low-activity clay, little differentiation among horizons, and a strong and well developed microgranular structure comprising angular and subangular microaggregates (Reatto et al, 2009;Brossard et al, 2012). These microaggregates are organised into micropeds that are smaller than 1 mm, with a porous massive structure according to Volland-Tuduri et al (2005).…”
Section: Experimental Designmentioning
confidence: 99%
“…These structures present significant variations in porosity and size (Balbino et al, 2002b). These microorganizations are in part controlled by soil fauna activities that promote fluctuation in soil porosity (Brossard et al, 2012). The incident energy penetrates $2 mm deep into the sample.…”
Section: Discrimination Between the Soilsmentioning
confidence: 99%