{"title":"Interaction between maize residues and initial soil carbon status on soil labile organic carbon pools","authors":"","doi":"10.1016/j.apsoil.2024.105482","DOIUrl":null,"url":null,"abstract":"<div><p>Crop residue serves as a vital source of energy and nutrients for microbial proliferation, ultimately contributing to the formation of soil organic carbon (SOC). Labile organic C pool (i.e., extractable organic C and microbial biomass C) not only represents a small part of SOC, but also is a sensitive indicator of soil biogeochemical process under agricultural management. However, the interaction between maize residue types and initial soil C status on the fate of residue C in labile organic C pools remains not very clear. Here, we added the <sup>13</sup>C-labeled maize root, stem, and leaf residues into soils with low and high initial C status for 360 days of incubation and analyzed the contents of residue derived- salt-extractable organic C (SEOC) and microbial biomass C (MBC). The results showed that average 7.31 % and 6.46 % of SEOC was derived from maize residue C in the low and high C soil during the whole incubation, respectively. The contribution of MBC derived from residue C to total MBC in the high C soil was on average 13.36 % higher than that in the low C soil, which indicated that the high C soil could accelerate the transformation of residue C into microbial biomass by efficient anabolism pathway. The distribution percentage of leaf residue C to MBC was on average 1.73 % higher than those of root residue C and stem residue C to MBC in the low C soil, whereas more root residue C was entered to SEOC and MBC compared with stem residue C and leaf residue C in the high C soil, which demonstrated that the low-quality residue (i.e., maize root) tended to be more susceptible to microbial utilization, but it depended on the initial soil C status. Overall, these findings contribute to understanding the mechanisms of microbial-mediated C transformation processes, and provide insights into the capture and incorporation of plant residue C into labile organic C pools driven by initial soil C status and crop residue returning.</p></div>","PeriodicalId":8099,"journal":{"name":"Applied Soil Ecology","volume":null,"pages":null},"PeriodicalIF":4.8000,"publicationDate":"2024-07-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Soil Ecology","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0929139324002130","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
Abstract
Crop residue serves as a vital source of energy and nutrients for microbial proliferation, ultimately contributing to the formation of soil organic carbon (SOC). Labile organic C pool (i.e., extractable organic C and microbial biomass C) not only represents a small part of SOC, but also is a sensitive indicator of soil biogeochemical process under agricultural management. However, the interaction between maize residue types and initial soil C status on the fate of residue C in labile organic C pools remains not very clear. Here, we added the 13C-labeled maize root, stem, and leaf residues into soils with low and high initial C status for 360 days of incubation and analyzed the contents of residue derived- salt-extractable organic C (SEOC) and microbial biomass C (MBC). The results showed that average 7.31 % and 6.46 % of SEOC was derived from maize residue C in the low and high C soil during the whole incubation, respectively. The contribution of MBC derived from residue C to total MBC in the high C soil was on average 13.36 % higher than that in the low C soil, which indicated that the high C soil could accelerate the transformation of residue C into microbial biomass by efficient anabolism pathway. The distribution percentage of leaf residue C to MBC was on average 1.73 % higher than those of root residue C and stem residue C to MBC in the low C soil, whereas more root residue C was entered to SEOC and MBC compared with stem residue C and leaf residue C in the high C soil, which demonstrated that the low-quality residue (i.e., maize root) tended to be more susceptible to microbial utilization, but it depended on the initial soil C status. Overall, these findings contribute to understanding the mechanisms of microbial-mediated C transformation processes, and provide insights into the capture and incorporation of plant residue C into labile organic C pools driven by initial soil C status and crop residue returning.
作物秸秆是微生物增殖的重要能量和养分来源,最终有助于土壤有机碳(SOC)的形成。可移动有机碳库(即可提取有机碳和微生物生物量碳)不仅是土壤有机碳的一小部分,也是农业管理下土壤生物地球化学过程的一个敏感指标。然而,玉米残留物类型和初始土壤碳状况对可溶性有机碳库中残留物碳归宿的相互作用仍不十分明确。在此,我们将 13C 标记的玉米根、茎和叶残留物添加到初始 C 状态低和初始 C 状态高的土壤中培养 360 天,并分析了残留物衍生的盐提取有机 C(SEOC)和微生物生物量 C(MBC)的含量。结果表明,在整个培养过程中,低碳土壤和高碳土壤中玉米残余物 C 平均分别提取了 7.31% 和 6.46% 的 SEOC。在高 C 值土壤中,残留 C 所产生的 MBC 占总 MBC 的比例平均比低 C 值土壤高 13.36%,这表明高 C 值土壤可以通过高效的合成代谢途径加速残留 C 向微生物生物量的转化。在低C土壤中,叶片残余C转化为MBC的分配比例平均比根残余C和茎残余C转化为MBC的分配比例高1.73%,而在高C土壤中,根残余C转化为SEOC和MBC的比例比茎残余C和叶片残余C的比例高,这表明低质量残余物(即玉米根)往往更容易被微生物利用,但这取决于初始土壤C状况。总之,这些研究结果有助于理解微生物介导的碳转化过程的机制,并为了解植物残留物碳在初始土壤碳状况和作物残留物返回的驱动下被捕获并纳入可变有机碳库提供了见解。
期刊介绍:
Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.