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Estoques de carbono e nitrogênio no solo na seqüência floresta-pastagem na região oeste da bacia amazônica brasileira

机译:巴西亚马逊河流域西部地区森林-植被序列中的土壤碳和氮储量

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摘要

We examined two chronosequences of forest, 8-and 20-year-old pasture in Rondônia-Brazil, to investigate how land use change affects the soil carbon and nitrogen stocks and organic matter dynamics of surface soil (0 to 30 cm). Soil total carbon and nitrogen stocks increased in 20-year-old pasture compared with the original forest in one chronosequence but no changes were detected in the other chronosequence. Calculations of the contributions of forest - and pasture-derived carbon from soil ð13C values showed a general pattern of pasture carbon augmenting a slowly declining pool of carbon derived from the original forest. Soil ð13C values at 0 to 10 cm increased from -27 to -28 o/oo in the forests to approximately -20 o/oo in the 20-year-old pastures and reflected greater inputs of pasture-derived C4 carbon in older pastures. If typical of larger areas of pasture in the Amazon Basin, these changes in soil carbon and nitrogen stocks following forest conversion to pasture have important implications for understanding the global biogeochemical cycles
机译:我们研究了Rondônia-Brazil的两个森林,8岁和20岁草场的时间序列,以调查土地利用变化如何影响土壤碳和氮储量以及表层土壤(0至30 cm)的有机质动态。与原始森林相比,20年牧场中的土壤总碳和氮储量在一个时序上与原始森林相比有所增加,但在另一个时序上没有发现变化。根据土壤ð13C值对森林和牧草碳的贡献进行的计算表明,牧草碳的一般模式增加了源自原始森林的缓慢下降的碳库。 0至10 cm处的土壤ð13C值从森林中的-27增加到-28 o / oo,在20年之久的牧场中增加到大约-20 o / oo,这反映了较老的牧场中更多的牧场来源的C4碳输入。如果是亚马逊河流域较大牧场的典型特征,那么森林转化为牧场后土壤碳和氮储量的这些变化对于理解全球生物地球化学循环具有重要意义。

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