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Increased contribution of root exudates to soil carbon input during grassland degradation

机译:在草地降解期间,根部渗出的根部渗出的贡献增加了

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The contribution of root exudates to soil carbon (C) inputs is poorly quantified, especially for grasslands under the context of degradation that includes simultaneous shifts in species composition due to long-term overgrazing. The objectives of this study were to examine (1) how grassland degradation affects root exudation rate and (2) to what extent root exudates contribute to soil C inputs compared to litter materials and root turnover during degradation. A field experiment was conducted in a temperate grassland, with different levels of degradation (undegraded control, moderately degraded, and severely degraded), dominated by different species in Inner Mongolia. Aboveground biomass, root biomass, and root exudate rate were measured monthly during a growing season. Root exudation rates differed among dominant plant species across the degradation gradients and grassland degradation significantly increased root exudation rates at the plot level. However, the amount of root exudates released to soils in degraded sites was lower than in undegraded site due to reduced living root biomass. Compared to the undegraded control, the relative contribution of root exudates to soil C inputs was enhanced by grassland degradation as a result of decreased contributions from root turnover. These findings prove grassland degradation can alter the relative contribution of root exudates compared to other soil C inputs and highlight the necessity of further studies to examine how this shift may affect soil organic C formation and long-term storage.
机译:根部渗出物到土壤碳(C)投入的贡献量很差,特别是在降解下的草原上,由于长期过度覆盖,包括在物种组成中同时移位。本研究的目标是检查(1)草地降解如何影响根部渗出速率,(2)在垃圾材料和降解期间的根转周转和根转周转方案有多大程度的渗出物。在温带草地上进行了田间实验,具有不同水平的降解(过度的对照,中度降解,严重降解),由内蒙古不同物种主导。在不断增长的季节期间每月测量地上生物质,根生物量和根渗出速率。在降解梯度和草地降解的主要植物种类中,根部渗出率不同,因此在地区的局部渗出率显着增加。然而,由于生物根生物量减少,降解位点的土壤中释放到降解的土壤中的根部渗出物的量低于未解析的位点。与未扩展的控制相比,由于根转况下降,草地降解,草地退化,根部渗出对土壤C输入的相对贡献得到了增强。这些发现证明了草地降解可以改变根部渗出物的相对贡献与其他土壤C的输入相比,并突出进一步研究的必要性来检查如何影响土壤有机C形成和长期储存。

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