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土壤有机碳化学结构对玉米秸秆还田方式的响应。

Response of the chemical structure of soil organic carbon to modes of maize straw return.

机构信息

Heihe Branch Academy of Heilongjiang Academy of Agricultural Sciences, Heihe, 164300, China.

Key Laboratory of Soil Environment and Plant Nutrition of Harbin, Institute of Soil and Fertilizer and Environment Resources, Heilongjiang Academy of Agricultural Sciences, Harbin, 150086, China.

出版信息

Sci Rep. 2021 Mar 22;11(1):6574. doi: 10.1038/s41598-021-84697-6.

Abstract

Elucidating the chemical structure of soil organic matter (SOM) is important for accurately evaluating the stability and function of SOM. Aboveground vegetation directly affects the quantity and quality of exogenous organic matter input into the soil through plant residues and root exudates, which in turn affects soil microbial species, community structure, and activity, and ultimately impacts the chemical structure of SOM. In this study, a C nuclear magnetic resonance technique was used to analyze the chemical structure characteristics of soil organic carbon (SOC) under various rates of straw returning combined with rotary tillage and under full straw mulching. The results showed that full straw returning with rotary tillage and full straw mulching more effectively increased the SOC content than reduced rate of straw returning (1/2 and 1/3 of full straw) with rotary tillage. The contents of alkyl C and alkoxy C in the functional groups of SOC under various straw returning treatments were increased compared with those under the treatment of maize stubble remaining in soil (CK). Furthermore, the contents of aromatic C and carboxyl C were decreased, which were consistent with the chemical shift changes of SOC. Compared with CK treatment, straw returning decreased the content of aromatic C in the functional groups of SOC, but increased the content of alkoxy C, which could be associated with the change in integral areas of absorption peaks of alkyl C and alkoxy C moving toward left and right, respectively. The content of total SOC was significantly positively (P < 0.05) correlated with that of alkoxy C and significantly negatively (P < 0.01) correlated with that of aromatic C. The molecular structure of SOC tends to be simplified due to the decreasing in refractory C and the increasing in easily decomposed C after straw returning to the field.

摘要

阐明土壤有机质(SOM)的化学结构对于准确评估 SOM 的稳定性和功能非常重要。地上植被通过植物残体和根分泌物直接影响进入土壤的外源有机物质的数量和质量,进而影响土壤微生物种类、群落结构和活性,最终影响 SOM 的化学结构。本研究采用 C 核磁共振技术分析了不同秸秆还田方式(旋耕和秸秆全覆盖)与旋耕相结合条件下土壤有机碳(SOC)的化学结构特征。结果表明,与旋耕减少秸秆还田量(全量的 1/2 和 1/3)相比,旋耕与秸秆全覆盖更有效地增加了 SOC 含量。与玉米茬留茬(CK)处理相比,各秸秆还田处理下 SOC 功能基团中烷基 C 和烷氧基 C 的含量增加。此外,芳香族 C 和羧基 C 的含量减少,这与 SOC 的化学位移变化一致。与 CK 处理相比,秸秆还田降低了 SOC 功能基团中芳香族 C 的含量,但增加了烷氧基 C 的含量,这可能与烷基 C 和烷氧基 C 吸收峰积分面积分别向左和向右移动的变化有关。总 SOC 含量与烷氧基 C 含量呈显著正相关(P < 0.05),与芳香族 C 含量呈显著负相关(P < 0.01)。秸秆还田后,由于难分解 C 的减少和易分解 C 的增加,SOC 的分子结构趋于简化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4dca/7985507/fbf94dc75d38/41598_2021_84697_Fig1_HTML.jpg

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