1996
DOI: 10.2136/sssaj1996.03615995006000030032x
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Soil Structural Stability during Rapid Wetting: Influence of Land Use on Some Aggregate Properties

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Cited by 71 publications
(34 citation statements)
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“…The soil of the SDle treatment had passed through tillage only a year before the collection and testing of the soil samples, so that the SDle aggregates were the least age-hardened (Utomo and Dexter, 1981). Thus, the rapid entrance of water into the soil pores during the testing of the dry aggregates in the rain simulator may have led to their rupture (Caron et al, 1996), thereby compromising the soil structural stability. Cerrado).…”
Section: Resultsmentioning
confidence: 99%
“…The soil of the SDle treatment had passed through tillage only a year before the collection and testing of the soil samples, so that the SDle aggregates were the least age-hardened (Utomo and Dexter, 1981). Thus, the rapid entrance of water into the soil pores during the testing of the dry aggregates in the rain simulator may have led to their rupture (Caron et al, 1996), thereby compromising the soil structural stability. Cerrado).…”
Section: Resultsmentioning
confidence: 99%
“…Bulk density data showed the expected difference between management regimes, due to the high degree of stability and settlement of the non-tilled soil. In NT soil, colloidal organic particles could support the occlusion of pores (Caron et al, 1996), decreasing the coarse porosity and increasing the very fine porosity (Table 2). Moreover, the CT site on the MPC soil had been recently ploughed, although it was impossible to detect wheel tracks.…”
Section: General Characteristics Of Soilsmentioning
confidence: 99%
“…Pore character of soil aggregates is the main factor influencing wetting speed, such as pore size and camber. Caron reported that pore camber indexes in NT is three times more compared to in CT, water immerse rate decreased by 70% and increased aggregates stability (Mazurak et al, 1950;Caron et al, 1996). It is suitable to form soil structure for soil pore type and quantity and soil density which was lower in NTR-r and NTRw-r compared to PUR-r that was caused by stable heat capability, relative stable electrical field, continuous immersing and strong water retention ability of labile organic matters which were rotted from root straw internal or external soil pore (Xie et al, 2002;Wei et al, 2006).…”
Section: Organic Carbon In Aggregatesmentioning
confidence: 99%