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首页> 外文期刊>Journal of Biotechnology >Wetting-drying cycles do not increase organic carbon and nitrogen mineralization in soils with straw amendment
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Wetting-drying cycles do not increase organic carbon and nitrogen mineralization in soils with straw amendment

机译:润湿干燥循环不会增加秸秆修正的土壤中的有机碳和氮矿化

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摘要

Increasing soil organic matter (SOM) is of primary importance for maintaining soil fertility and mitigating climate change. Leaving crop residues on top of soil is not always an efficient means of increasing SOM because (i) of the high mineralization of the crop residues, (ii) crop residues may increase the mineralization of existing SOM (priming effect) and (iii) wetting-drying cycles may increase mineralization of SOM and crop residues. Little research has been carried out into these mechanisms under Sudano-Sahelian conditions where the rainfall is mostly irregular with wetting-drying cycles during the transition between the wet and the dry season. To evaluate the effect of wetting-drying cycles on the mineralization of SOM and crop residues and the priming effect, an agricultural soil from the North Region of Cameroon with or without (controls) C-13-labeled rice straw amendment as crop residues was either subjected to five wetting-drying cycles or maintained at constant water potential after a single rewetting event. Soil samples were incubated for 70 days at 28 degrees C and the CO2 and (CO2)-C-13 emissions and mineral N were monitored.
机译:增加土壤有机物(SOM)对于维持土壤肥力和缓解气候变化的主要重要性。将作物残留物留在土壤上并不总是增加SOM的有效手段,因为(i)作物残留物的高矿化,(ii)作物残留可能会增加现有SOM的矿化(引发效果)和(iii)润湿 - 上循环可能增加SOM和作物残留物的矿化。在苏丹萨赫州的条件下,在苏丹 - 萨赫伦条件下进行了很少的研究,其中降雨在湿季和干燥季节之间的过渡期间具有润湿干燥循环。为了评估湿润干燥循环对SOM和作物残留物的矿化和引发效果的影响,喀麦隆北部地区的农业土壤有或没有(控制)C-13标记的稻草修正为作物残留物在单次重新润湿事件之后经过五个润湿干燥循环或保持在恒定的水势。将土壤样品在28℃下孵育70天,并监测CO 2和(CO 2)-C-13排放和矿物N。

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