2013
DOI: 10.3103/s1068367413060153
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Interaction of lime and gypsum with sorption complex of acidic soils

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Cited by 3 publications
(2 citation statements)
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“…Traditionally, in the 0-0.2 m soil depth, there was better lime incorporation, but it did not fully reach 0.2-0.4 and 0.4-0.6 m soil layers. Reductions in the potential acidity are usually observed at 0-0.2 and 0.2-0.4 m soil depth and may be directly attributed to the benefits of lime, which reacts soil carbonate anions and HCO 3 -) with soil potential acidity (H + + Al 3+ ) (Okorkov and Okorkova, 2013). At 0.2-0.4 m soil depth the levels of H + + Al 3+ were great for T4 (desiccation-liming-direct planting) in 2010, and for T3 (liming-harrowing-plowing-harrowing) in both years (Table 2).…”
Section: +mentioning
confidence: 99%
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“…Traditionally, in the 0-0.2 m soil depth, there was better lime incorporation, but it did not fully reach 0.2-0.4 and 0.4-0.6 m soil layers. Reductions in the potential acidity are usually observed at 0-0.2 and 0.2-0.4 m soil depth and may be directly attributed to the benefits of lime, which reacts soil carbonate anions and HCO 3 -) with soil potential acidity (H + + Al 3+ ) (Okorkov and Okorkova, 2013). At 0.2-0.4 m soil depth the levels of H + + Al 3+ were great for T4 (desiccation-liming-direct planting) in 2010, and for T3 (liming-harrowing-plowing-harrowing) in both years (Table 2).…”
Section: +mentioning
confidence: 99%
“…In this experiment, the no-till treatment (T4) presented Ca 2+ content equivalent to treatments with soil revolving at the superficial soil layer (0-0.2 m). A great increase of soil acidity (low pH) and Al 3+ levels are regularly observed at soil layers below 0.4 m due to no influence of lime effects at such depths (Okorkov and Okorkova, 2013). Conyers et al (2003) discussed the movement of lime in soil surface and subsurface in no-till systems and concluded that the physical movement of lime in soil is probably through channels formed by dead roots left intact due to the lack of soil revolving, results that were not observed in this study.…”
Section: Soil Exchangeable Cationsmentioning
confidence: 99%