Responses of labile organic carbon fractions and mineralized carbon to straw return combined with fertilizer application in the maize–Melilotus officinalis intercropping system

Wei Zhao, Hongrui Zhao, Ruiqi Li, Shuai Hao, Hongyan Wang, Daqing Wang
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Abstract

Mollisol is crucial for solving food security issues, but long-term excessive application of chemical fertilizers has led to severe Mollisol degradation in Northeast China, especially a rapid decline in soil organic carbon (SOC). In context of the use of crop-herbage intercropping and straw return as alternatives for some chemical fertilizers, it is important to understand how crop-herbage intercropping and straw return combined with chemical fertilizers influence labile organic carbon (LOC) fractions that improve SOC. To address this, this study explored how the combined application of maize (Zea mays L.)–Melilotus officinalis intercropping, straw return, and chemical fertilizers affect LOC fractions and mineralized carbon (MC) from the perspective of physical property-mediated pathways. Thus, a field experiment with six treatments was established in the Songnen Plain of Northeast China: (1) maize monoculture without chemical fertilizers and straw return (CK), (2) maize monoculture with chemical fertilizers and no straw return (CF), (3) maize monoculture with chemical fertilizers and straw return (CFS), (4) maize–M. officinalis intercropping and straw return combined with full application of chemical fertilizers (CFSM), (5) maize–M. officinalis intercropping and straw return combined with half application of chemical fertilizers (1/2CFSM), and (6) maize–M. officinalis intercropping and straw return without chemical fertilizers (SM). The CF and CFS groups had no effect on bulk density and porosity but reduced specific gravity. The CFSM group increased water contents, porosity, LOC fractions, SOC, MC, and CO2 release rate and decreased bulk density and specific gravity. Compared with the CF group, the 1/2CFSM group enhanced water contents, microbial biomass carbon, and water-soluble organic carbon (WSOC) to 6.36%, 17.91%, and 11.6%, respectively. We found that maize–M. officinalis intercropping, straw return, and reducing chemical fertilizers application improved LOC fractions to increase SOC by positively affecting bulk density, specific gravity, and water contents. Further analysis indicated that WSOC was a key determinant of SOC and maize yields. These findings provide a strategy to increase SOC and rehabilitate degraded soils through crop-herbage intercropping and straw return combined with reducing chemical fertilizers application, which will contribute to a sustainable and environmentally friendly agriculture.

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玉米-小麦间作系统中可溶性有机碳组分和矿化碳对秸秆还田和施肥的反应
软土地基对解决粮食安全问题至关重要,但长期过量施用化肥已导致中国东北地区软土地基严重退化,尤其是土壤有机碳(SOC)急剧下降。在使用作物间作套种和秸秆还田替代化肥的背景下,了解作物间作套种和秸秆还田与化肥的结合如何影响提高土壤有机碳(SOC)的可变有机碳(LOC)组分具有重要意义。为此,本研究从物理特性介导途径的角度,探讨了玉米(Zea mays L.)-丝瓜间作、秸秆还田和化肥的联合施用如何影响可溶性有机碳(LOC)组分和矿化碳(MC)。因此,在东北松嫩平原建立了六个处理的田间试验:(1)不施化肥和秸秆还田的玉米单作(CK);(2)施化肥和不施秸秆还田的玉米单作(CF);(3)施化肥和秸秆还田的玉米单作(CFS);(4)玉米-M.(5) 玉米-M. officinalis 间作和秸秆还田与施用全量化肥相结合(CFSM),(5) 玉米-M. officinalis 间作和秸秆还田与施用半量化肥相结合(1/2CFSM),(6) 玉米-M. officinalis 间作和秸秆还田不施用化肥(SM)。CF 组和 CFS 组对容重和孔隙率没有影响,但降低了比重。CFSM 组增加了含水量、孔隙度、LOC 分数、SOC、MC 和 CO2 释放率,降低了容重和比重。与 CF 组相比,1/2CFSM 组的含水量、微生物生物量碳和水溶性有机碳(WSOC)分别提高了 6.36%、17.91% 和 11.6%。我们发现,玉米-M. officinalis间作、秸秆还田和减少化肥施用量通过对容重、比重和含水量产生积极影响,提高了LOC分数,从而增加了SOC。进一步分析表明,WSOC 是决定 SOC 和玉米产量的关键因素。这些研究结果提供了一种策略,即通过作物间作、秸秆还田和减少化肥施用量来增加土壤有机质并恢复退化的土壤,这将有助于实现可持续发展的环境友好型农业。
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