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Effect of Tillage Systems on Distribution of Aggregates and Organic Carbon in a Long-term No-tillage Paddy Field

机译:耕作系统对长期无耕田稻田聚集体和有机碳分布的影响

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The effect of different tillage systems on the size distribution of aggregates and organic carbon distribution and storage in different size aggregates in a Hydragric Anthrosol were studied in a long-term experiment in Chongqing, China. The experiment included five tillage treatments, which are conventional tillage with rice only system (DP), conventional tillage with rotation of rice and rape system (SH), no-till and ridge culture with rotation of rice and rape system (LM), no-till and plain culture with rotation of rice and rape system (XM) and tillage and ridge culture with rotation of rice and rape system (LF), respectively. The results showed that the aggregates 0.25-0.05 mm in diameter accounted for the largest proportion in each soil layer under all treatments. The organic carbon mainly exist in aggregates in the 0.25-2 mm and 0.05-0.25 mm diameter in the plough layer, which mainly exist in the 0.25-2 mm in diameter in the bottom layer. Distribution of organic carbon in aggregates in the 0.05-0.25 mm diameter class was highest, followed by the aggregates in the 0.25-2mm diameter class. The organic carbon in aggregates under different tillage systems was in a decreasing order of LM (21.05 g·kg~(-1))> DP (14.13 g·kg~(-1))> XM (13.29 g·kg~(-1))> LF (12.54 g·kg~(-1)) > SH (11.41 g·kg~(-1)). The total organic carbon content showed a significant correlation with the amount of aggregates with diameter >0.005 mm. The results showed that the accumulation of soil organic carbon was mainly affected by aggregates in the >0.005mm diameter class.
机译:在中国重庆的长期实验中,研究了不同耕作系统对含氢蒽醇中不同尺寸聚集体的尺寸分布和储存的效果。该实验包括五种耕作治疗,其常规耕作与稻米(DP),常规耕作,带有水稻和油菜系统(SH)的旋转,无碱和脊髓培养物,带有水稻和油菜系统(LM),没有 - 用水稻和强奸系统(XM)和耕作和脊髓培养物的旋转和平纹文化分别具有水稻和强奸系统(LF)的旋转。结果表明,直径为0.25-0.05mm的聚集体占所有治疗下的每种土壤层中的最大比例。有机碳主要存在于0.25-2mm和0.05-0.25mm的犁层中的聚集体,其主要存在于底层的直径0.25-2mm。在0.05-0.25mm直径上的聚集体中的有机碳分布最高,其次是0.25-2mm直径级别的聚集体。在不同耕作系统下聚集体中的有机碳处于LM的下降(21.05g·kg〜(-1))> dp(14.13g·kg〜(-1))> xm(13.29g·kg〜( - 1)) LF(12.54g·kg〜(-1))> SH(11.41g·kg〜(-1))。总有机碳含量与直径> 0.005mm的聚集量显着相关。结果表明,土壤有机碳的积累主要受到> 0.005mm直径级别的聚集体的影响。

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