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Long-term rice cultivation stabilizes soil organic carbon and promotes soil microbial activity in a salt marsh derived soil chronosequence

机译:水稻长期耕作可稳定土壤有机碳并促进盐沼衍生的土壤时间序列的土壤微生物活性

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摘要

Soil organic carbon (SOC) sequestration with enhanced stable carbon storage has been widely accepted as a very important ecosystem property. Yet, the link between carbon stability and bio-activity for ecosystem functioning with OC accumulation in field soils has not been characterized. We assessed the changes in microbial activity versus carbon stability along a paddy soil chronosequence shifting from salt marsh in East China. We used mean weight diameter, normalized enzyme activity (NEA) and carbon gain from straw amendment for addressing soil aggregation, microbial biochemical activity and potential C sequestration, respectively. In addition, a response ratio was employed to infer the changes in all analyzed parameters with prolonged rice cultivation. While stable carbon pools varied with total SOC accumulation, soil respiration and both bacterial and fungal diversity were relatively constant in the rice soils. Bacterial abundance and NEA were positively but highly correlated to total SOC accumulation, indicating an enhanced bio-activity with carbon stabilization. This could be linked to an enhancement of particulate organic carbon pool due to physical protection with enhanced soil aggregation in the rice soils under long-term rice cultivation. However, the mechanism underpinning these changes should be explored in future studies in rice soils where dynamic redox conditions exist.
机译:具有增强的稳定碳储存能力的土壤有机碳固存已被广泛接受为一种非常重要的生态系统特性。然而,碳的稳定性和生物活性之间的生态系统功能与田间土壤中OC积累之间的联系尚未得到表征。我们评估了从华东盐沼转移到稻田土壤的时间序列上微生物活性相对于碳稳定性的变化。我们分别使用平均重量直径,归一化酶活性(NEA)和秸秆改良剂获得的碳增加分别处理土壤聚集,微生物生化活性和潜在的C隔离。另外,采用响应比来推断水稻长期栽培中所有分析参数的变化。尽管稳定的碳库随总SOC积累而变化,但稻田土壤中的呼吸作用以及细菌和真菌的多样性均相对恒定。细菌丰度和NEA与总SOC积累呈正相关,但与总SOC高度相关,表明生物活性随碳稳定度增加。这可以归因于长期的水稻种植下的物理保护以及水稻土壤中土壤团聚的增强,从而增加了颗粒有机碳库。然而,在存在动态氧化还原条件的水稻土上的未来研究中,应探索支持这些变化的机制。

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