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稳定同位素揭示了源自不同棉秆基材料的腐殖质物质的形成多样性。

Stable isotopes reveal the formation diversity of humic substances derived from different cotton straw-based materials.

机构信息

College of Resources and Environment, Qingdao Agricultural University, Qingdao 266109, PR China; Qingdao Engineering Research Center for Rural Environment, College of Resources and Environment, Qingdao Agricultural University, Qingdao 266109, PR China.

College of Resources and Environment, Qingdao Agricultural University, Qingdao 266109, PR China.

出版信息

Sci Total Environ. 2020 Oct 20;740:140202. doi: 10.1016/j.scitotenv.2020.140202. Epub 2020 Jun 15.

Abstract

Humic substances (HS) are essential in environment processes and carbon (C) sequestration in soils. In this study, organic materials such as cotton straw and its derived compost and biochar were added to the soil on a C-equivalent basis and incubated for 30 and 180 days in order to investigate the different forms of plant biomass derived C sequestration in HS. The C distribution in humic acid (HA), fulvic acid (FA), and humin (Hu) derived from organic materials was investigated using the C isotope method, while the catalase, sucrose, and β-glucosidase activities were also determined. The results showed that C3 distribution of Hu derived from straw, compost and biochar increased from 40.94% to 67.12%, 74.47% and 80.75%, respectively. In addition, the increase of C3 distribution of HA or FA derived from straw, compost and biochar were 4.69%, 10.09% and 1.49%, respectively. There were significantly positive correlations between catalase, sucrase and β-glucosidase activities and C3 derived HA and FA. The principal component analysis showed that catalase, sucrase and β-glucosidase were explained mainly by the first principal component indicating a significant correlation. These findings suggest that straw, compost and biochar are mainly sequestrated in Hu. Comparatively, the straw and compost are more likely to contribute to the formation of HA and FA in soil, but biochar favors the Hu, which helps in soil C sequestration. The formation of HA and FA derived from organic materials was supported by catalase, sucrase and β-glucosidase activities.

摘要

腐殖质(HS)是环境过程和土壤碳(C)固存的重要组成部分。在这项研究中,以碳当量的形式向土壤中添加了棉花秸秆及其衍生的堆肥和生物炭等有机物质,并在 30 和 180 天的时间内进行了孵育,以研究不同形式的源自植物生物质的 C 在 HS 中的固存。使用 C 同位素法研究了源自有机物质的腐殖酸(HA)、富里酸(FA)和胡敏素(Hu)中 C 的分布,同时还测定了过氧化氢酶、蔗糖和β-葡萄糖苷酶的活性。结果表明,秸秆、堆肥和生物炭衍生 Hu 中 C3 的分布分别从 40.94%增加到 67.12%、74.47%和 80.75%。此外,秸秆、堆肥和生物炭衍生 HA 或 FA 中 C3 分布的增加量分别为 4.69%、10.09%和 1.49%。HA 和 FA 中源自秸秆、堆肥和生物炭的 C3 分布与过氧化氢酶、蔗糖酶和β-葡萄糖苷酶活性之间呈显著正相关。主成分分析表明,过氧化氢酶、蔗糖酶和β-葡萄糖苷酶主要由第一主成分解释,表明相关性显著。这些发现表明,秸秆、堆肥和生物炭主要被固存于 Hu 中。相比之下,秸秆和堆肥更有可能有助于 HA 和 FA 在土壤中的形成,但生物炭有利于 Hu 的形成,从而有助于土壤 C 的固存。有机物质衍生的 HA 和 FA 的形成得到了过氧化氢酶、蔗糖酶和β-葡萄糖苷酶活性的支持。

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