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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Status of humus in soil under various long-term tillage systems
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Status of humus in soil under various long-term tillage systems

机译:长期不同耕作制度下土壤腐殖质状况

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The content and fractional composition of humus in soil exposed to conventional, shallow and minimum tillage for 40 years was investigated on Cambisols. Humus status depended on tillage methods and depth. In cultivated soil, conventional annual tillage can be replaced by shallow or minimum tillage, since this significantly increased soil humus content in the 0-10 and 10-20 cm soil layers. In both experiments with lower (Experiment 1) and higher (Experiment 2) application rates of mineral fertilizer,in the whole 0-30 cm layer in the minimum soil tillage systems (MT1 and MT2), the content of humus significantly increased, and in the shallow tillage system (ShT), it did not differ significantly, compared with conventional tillage (CT). In both experiments, the content of humus in the 0-10 and 10-20 cm layers of the shallow tillage treatment was significantly higher than that in the 20-30 cm layer. Having replaced the conventional soil tillage by shallow or both minimum tillage systems, humus quality(characterized by the parameters of humus fractional composition) remained similar. The data of humus fractional composition showed that abandonment of conventional tillage results in a significant increase in stable soil humus forms. Application of shallow and minimum soil tillage systems significantly increased the content of humic acids strongly bound with the soil clay minerals in the 0-30 cm layer in both experiments, except ShT in Experiment 2. In Experiment 1, with lower application rates of mineral fertilizer, minimum soil tillage systems (MT1 and MT2) significantly increased the E4:E6 ratio of humic acids, which indicated suitable conditions for humification and the existence of high molecular humic acids in the soil.
机译:在Cambisols上研究了常规,浅层和最小耕作40年下土壤中腐殖质的含量和组成成分。腐殖质状况取决于耕作方法和深度。在耕作土壤中,常规的年度耕作可以用浅耕或最小耕作代替,因为这会显着增加0-10和10-20 cm土层的土壤腐殖质含量。在较低(实验1)和较高(实验2)施肥量的两个实验中,在最小土壤耕作系统(MT1和MT2)的整个0-30 cm层中,腐殖质含量显着增加,浅耕系统(ShT)与常规耕作(CT)相比无显着差异。在两个实验中,浅耕处理的0-10和10-20 cm层腐殖质含量均明显高于20-30 cm层。腐殖质的质量(以腐殖质组成成分的参数为特征)已被浅层耕作或两种最小耕作制度取代了传统的土壤耕作。腐殖质分数组成的数据表明,放弃传统耕作会导致稳定的土壤腐殖质形式显着增加。在两个实验中,应用浅层和最小土壤耕作系统均显着增加了与0-30 cm层中土壤粘土矿物牢固结合的腐殖酸含量,但实验2中的ShT除外。在实验1中,矿物肥料的施用率较低最小耕作制度(MT1和MT2)显着提高了腐殖酸的E4:E6比率,这表明了进行腐殖化的合适条件以及土壤中存在高分子腐殖酸。

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