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Distribution of chemical compartments of soil organic matter and c stocks of a cambisol from south Brazil as affected by Pinus afforestation

机译:松树造林对巴西南部土壤有机质和碳二酚的碳储量化学区室的分布

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Distribution and stocks of soil organic matter (SOM) compartments after Pinus monoculture introduction in a native pasture area of a Cambisol, Santa Catarina, Brazil, were investigated. Pinus introduction increased soil acidity, content of exchangeable Al+3 and diminished soil nutrients. Nevertheless, soil C stock increased in all humic fractions of the 0-5 cm layer after Pinus afforestation. In the subsurface, the vegetation change only promoted SOM redistribution from the NaOH-extractable humic substances to a less hydrophobic humin fraction. Under Pinus, soil organo-mineral interactions were relevant up to a 15 cm depth, while in pasture environment, this mechanism occurred mainly in the surface layer.
机译:在巴西圣卡塔琳娜州的坎比索尔的原生牧草区引入松树单种栽培后,调查了土壤有机质(SOM)隔室的分布和储量。引入松树会增加土壤酸度,可交换的Al + 3含量并减少土壤养分。然而,松林造林后0-5 cm层的所有腐殖质部分土壤C储量均增加。在地下,植被变化仅促进SOM从可从NaOH提取的腐殖质重新分配为疏水性较低的腐殖质部分。在松属植物下,土壤有机矿物质的相互作用在15 cm深处是相关的,而在牧场环境中,这种机理主要发生在表层。

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