持续棉秆还田对新疆棉田土壤可矿化碳库的影响
[Abstract]:Based on the microregional localization experiment of cotton continuous cropping in oasis of Xinjiang for a long time, the mineralization characteristics of soil organic carbon in cotton field and the change of soil organic carbon release with the returning years of cotton straw were studied under straw returning and non-returning treatment. The results showed that the content of total organic carbon (TOC),) mineralizable carbon (MC) and the mineralization rate (MR),) of total organic carbon (TOC),) in the soil layer of 0 ~ 60 cm soil layer were increased compared with the non-return treatment. The content of (MC) and the mineralization rate of the total organic carbon mineralizable carbon (MC) in the soil layer increased with the increase of the number of years of straw returning to the field. After continuous straw returning to the field, the soil organic carbon mineralization rate increased, and the cumulative mineralization discharge (CO_2-C emission) increased, but the mineralization intensity decreased with the straw returning time, and the soil organic carbon mineralization rate increased with the straw returning time, but the mineralization intensity decreased with the increase of soil organic carbon mineralization rate. The change trend of cotton field with continuous cropping but no straw returning to the field was opposite to that of cotton field. The results showed that the measures of returning cotton straw to field increased soil organic carbon content in Xinjiang oasis cotton field. Although soil organic carbon was continuously supplemented, it was not yet saturated, and the carbon sequestration capacity of cotton field decreased with the extension of straw returning time.
【作者单位】: 石河子大学新疆兵团绿洲生态农业重点实验室;克拉玛依市克拉玛依区农林水牧局;
【基金】:国家自然科学基金项目(31260307)资助
【分类号】:S153.6
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