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Distribution of soil organic carbon and total nitrogen of the cultivated layer under different tillage practices

机译:不同耕作方式下耕层土壤有机碳和全氮的分布

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摘要

To evaluate the carbon and nitrogen sequestration capacity of different tillage practices, soil organic carbon and nitrogen concentrations and storages of the cultivated layer under different tillage practices (conventional tillage, no-tillage and fallow) were compared. The results showed that soil organic carbon under different tillage practices were significantly different among different soil depths and 0 – 5 cm > 5 – 15 cm > 15 – 30 cm (except for the conventional tillage in booting stage). The concentration of soil organic carbon in notillage was higher than that in conventional tillage and fallow. The concentrations of soil total nitrogen were significantly different among different treatments in 5 – 15 cm of jointing stage and 0 – 5 cm of booting and ripening stage, and no-tillage > conventional tillage > fallow. Soil organic carbon storage in the cultivated layer (0 – 30 cm) was increased by no-tillage practice, but soil nitrogen storage was not affected significantly by tillage practices. Soil organic carbon and total nitrogen were negatively correlated with pH, exchangeable K+ and Ca2+.
机译:为了评估不同耕作方式的固碳能力,比较了不同耕作方式(常规耕作,免耕和休耕)下土壤有机碳和氮的浓度以及耕层的储量。结果表明,不同耕作方式的土壤有机碳在不同的土壤深度和0 – 5 cm> 5 – 15 cm> 15 – 30 cm之间有显着差异(除常规耕作阶段的耕作阶段外)。耕作中土壤有机碳的浓度高于常规耕作和休耕方式。在拔节期5 – 15 cm和孕穗成熟期0 – 5 cm期间,不同处理方式的土壤总氮含量差异显着,并且免耕>传统耕作>休耕。免耕措施增加了耕层(0 – 30 cm)中土壤有机碳的存储量,但耕作方法对土壤氮的存储没有显着影响。土壤有机碳和总氮与pH,可交换的K + 和Ca 2 + 呈负相关。

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