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Effect of long-term tillage on soil aggregates and aggregate-associated carbon in black soil of Northeast China

机译:长期耕作对东北黑土土壤团聚体和团聚体相关碳的影响

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摘要

Soil tillage can affect the stability and formation of soil aggregates by disrupting soil structure. Frequent tillage deteriorates soil structure and weakens soil aggregates, causing them to be susceptible to decay. Different types of tillage systems affect soil physical properties and organic matter content, in turn influencing the formation of aggregates. The objective of this study was to evaluate the effect of long-term tillage on soil aggregates and aggregate-associated carbon in a black soil of Northeast China and to identify the optimal conservation tillage in this system. This research was conducted on a long-term tillage experimental field established in 1983 at the Jilin Academy of Agricultural Sciences, Gongzhuling, China. Plots were treated with four tillage systems including no tillage (NT), spacing tillage (ST), moldboard plowing (MP), and conventional tillage (CT). We took samples every 10cm from 0-60cm depth and demonstrated that water-stable soil aggregates >0.25mm in diameter accounted for over 66.0% of total aggregates for all tillage treatments, and the percentage for the ST treatment was 34.5% higher than in the other treatments. The NT treatment had the highest effect at 0–10cm depth, while the effect for the ST treatment was highest at 0–30cm. SOC storage decreased with soil depth, with a significant accumulation at 0-20cm depth. Across treatments, aggregate-associated C at a depth of 0–10cm was higher in the NT and ST treatments than in the MP and CT treatments. The advantage of the NT treatment weakened with soil depth, while the amount of aggregate-associated C remained higher for the ST treatment. There were more macro-aggregates in the ST and NT treatments than in the MP and CT treatments, while the MP and CT treatments had more micro-aggregates. The sum of macro-aggregate contributing rates for soil organic C (SOC) was significantly superior to that of the micro-aggregates. Water-stable aggregates increased by 34.5% in the ST treatment, effectively improving the soil structure. Furthermore, 0.25–1.00 and 1–2mm aggregates had the highest SOC storage and responded rapidly to the various tillage treatments. Hence, they can serve as indicators for the long-term influence of different tillage treatments on the distribution of aggregates and SOC.
机译:土壤耕作会破坏土壤结构,从而影响土壤团聚体的稳定性和形成。频繁耕作会破坏土壤结构并削弱土壤团聚体,使其易于腐烂。不同类型的耕作系统会影响土壤的物理性质和有机质含量,进而影响聚集体的形成。本研究的目的是评估长期耕作对东北黑土土壤团聚体和团聚体相关碳的影响,并确定该系统中的最佳保护性耕作。这项研究是在1983年在中国公主岭的吉林省农业科学院建立的长期耕作试验场上进行的。用四个耕作系统处理地块,包括免耕(NT),定距耕作(ST),刮土犁(MP)和常规耕作(CT)。我们从0-60cm的深度每10cm取样一次,结果表明,直径> 0.25mm的耐水土壤聚集体在所有耕作处理中占总聚集体的66.0%以上,而ST处理的百分比比土壤耕作高34.5%。其他治疗。 NT处理在0-10cm深度处效果最高,而ST处理在0-30cm处效果最高。 SOC的存储量随土壤深度的增加而减少,在0-20cm的深度有明显的积累。在所有处理中,NT和ST处理的0到10cm深度的骨料相关C高于MP和CT处理。 NT处理的优势随土壤深度而减弱,而ST处理的团聚体C含量仍较高。与MP和CT处理相比,ST和NT处理的宏观聚集体更多,而MP和CT处理的宏观聚集体更多。总体上,土壤有机碳(SOC)的总体贡献率总和显着优于微集料。在ST处理中,水稳性团聚体增加了34.5%,有效地改善了土壤结构。此外,0.25–1.00和1–2mm的骨料具有最高的SOC储存量,并且对各种耕作处理都有快速反应。因此,它们可以作为不同耕作处理对骨料和SOC分布的长期影响的指标。

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