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首页> 外文期刊>Global Biogeochemical Cycles >Grazing effects on belowground C and N stocks along a network of cattle exclosures in temperate and subtropical grasslands of South America
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Grazing effects on belowground C and N stocks along a network of cattle exclosures in temperate and subtropical grasslands of South America

机译:南美温带和亚热带草原上的牛排泄物网络对地下C和N种群的放牧影响

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摘要

We evaluated the effects of grazing on C and N belowground pools by comparing 15 grazing-exclosure pairs across the Rio de la Plata grasslands of Uruguay and Argentina. We measured C and N pools of belowground biomass, particulate organic matter (POM), and the mineral associated organic matter (MAOM) in the top meter of the soil. Grazing exclusion in the Rio de la Plata grasslands promoted (1) decreased belowground biomass stocks across all sites, (2) increased soil organic carbon (SOC) and soil organic nitrogen (SON) stocks in upland soils, and (3) decreased stocks in shallow and lowland soils. In all cases, SOC and SON variations were largely derived by changes in MAOM stocks that maintained their C:N ratios unchanged. In contrast, stocks of the labile POM fractions changed little, but C:N ratios of these fractions decreased after grazing removal. We hypothesize that changes in soil organic matter (SOM) contents between grazed and ungrazed stands result from the balance between changes in belowground N allocation patterns (root N retention hypothesis) and the ability of the soil to retain the extra N available after the exclusion of herbivores and the cessation of volatilization and leaching from urine and dung patches (N loss hypothesis). On the basis of our results we suggest that the relative importance of these two cooccurring mechanisms will shape grazing effects on SOM stocks, depending on soil properties, including texture, pH and soil depth, and vegetation type, particularly allocation patterns and C:N ratios of different plant species.
机译:通过比较乌拉圭和阿根廷的里约热内卢草原上的15个放牧绝育对,我们评估了放牧对C和N地下水池的影响。我们测量了土壤表层中地下生物量,颗粒有机质(POM)和矿物相关有机质(MAOM)的C和N池。里约热内卢草原的放牧排斥促进了(1)所有地点地下生物量的减少,(2)旱地土壤有机碳(SOC)和土壤有机氮(SON)的增加,以及(3)浅层和低地土壤。在所有情况下,SOC和SON的变化主要是由MAOM存量的变化(保持C:N比不变)引起的。相比之下,不稳定的POM馏分的库存变化不大,但是在清除放牧后,这些馏分的C:N比降低了。我们假设放牧和未湿地林分之间土壤有机质(SOM)含量的变化是由于地下N分配模式的变化(根系N保留假说)与土壤保留多余N的能力之间的平衡所致。食草动物和停止从尿液和粪便中挥发和浸出(氮损失假说)。根据我们的研究结果,我们认为这两种共生机制的相对重要性将影响放牧对SOM种群的影响,具体取决于土壤性质,包括质地,pH和土壤深度以及植被类型,尤其是分配模式和C:N比不同的植物种类。

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