河口土壤微生物坏死体碳和铁结合有机碳随土地利用和盐度的变化

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Chun Liu , Chunhuan He , Liqiong Li , Ping Li , Lisha Zhang , Yuheng Zhang , Chengxi Liu , Chengshuai Liu
{"title":"河口土壤微生物坏死体碳和铁结合有机碳随土地利用和盐度的变化","authors":"Chun Liu ,&nbsp;Chunhuan He ,&nbsp;Liqiong Li ,&nbsp;Ping Li ,&nbsp;Lisha Zhang ,&nbsp;Yuheng Zhang ,&nbsp;Chengxi Liu ,&nbsp;Chengshuai Liu","doi":"10.1016/j.catena.2025.109254","DOIUrl":null,"url":null,"abstract":"<div><div>Natural estuary soils are widely recognized as important carbon sinks for climate change mitigation, however, the soil organic carbon (SOC) accumulation and its underlying mechanism regulated by microbial necromass production and mineral preservation in estuarine soils in relation to land use and salinity still remain unclear. Here, we sampled four representative land uses [e.g., Natural Wetland (NW), Aquaculture Pond (AP), Banana Plantation (BP), and Cultivated Land (CL)] with varying salinities in the Pearl River Estuary, and then the microbial necromass carbon (MNC) and iron-bound organic carbon (Fe-OC) in soils by physical fractionation were analyzed. The results showed that the estuarine soil was dominated by mineral-associated fraction, with increasing proportions as converted by NW and increased by salinity. The MNC content in NW was significantly lower than that in CL, but was higher than those of BP and AP. However, NW had the highest Fe-OC content, followed by CL, BP, and AP. As soil salinity increased, the MNC content decreased, accompanied by an increase in Fe-OC content; however, the particulate Fe-OC exhibited a downward trend, which was opposite to that of bulk and mineral-associated Fe-OC. Increased salinity induced an reduction of MNC contribution and an increase of Fe-OC contribution to SOC pool, respectively; however, the NW conversion increased the contribution of MNC to SOC. The MNC was regulated by iron oxides (Fe<sub>d</sub>) and microbial biomass, while SOC and MNC had significantly positive impacts on Fe-OC. Overall, the MNC contents and its contribution to SOC were generally greater than Fe-OC in soils of the land use. Nevertheless, the importance of Fe-OC became increasingly prominent in SOC accumulation as soil salinity increased. Our findings emphasize the role of microbial necromass production and mineral preservation in SOM sequestration of estuarine soils depending on salinity and land use.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"258 ","pages":"Article 109254"},"PeriodicalIF":5.4000,"publicationDate":"2025-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Changes in the microbial necromass carbon and iron-bound organic carbon following land use and salinity in estuary soils\",\"authors\":\"Chun Liu ,&nbsp;Chunhuan He ,&nbsp;Liqiong Li ,&nbsp;Ping Li ,&nbsp;Lisha Zhang ,&nbsp;Yuheng Zhang ,&nbsp;Chengxi Liu ,&nbsp;Chengshuai Liu\",\"doi\":\"10.1016/j.catena.2025.109254\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Natural estuary soils are widely recognized as important carbon sinks for climate change mitigation, however, the soil organic carbon (SOC) accumulation and its underlying mechanism regulated by microbial necromass production and mineral preservation in estuarine soils in relation to land use and salinity still remain unclear. Here, we sampled four representative land uses [e.g., Natural Wetland (NW), Aquaculture Pond (AP), Banana Plantation (BP), and Cultivated Land (CL)] with varying salinities in the Pearl River Estuary, and then the microbial necromass carbon (MNC) and iron-bound organic carbon (Fe-OC) in soils by physical fractionation were analyzed. The results showed that the estuarine soil was dominated by mineral-associated fraction, with increasing proportions as converted by NW and increased by salinity. The MNC content in NW was significantly lower than that in CL, but was higher than those of BP and AP. However, NW had the highest Fe-OC content, followed by CL, BP, and AP. As soil salinity increased, the MNC content decreased, accompanied by an increase in Fe-OC content; however, the particulate Fe-OC exhibited a downward trend, which was opposite to that of bulk and mineral-associated Fe-OC. Increased salinity induced an reduction of MNC contribution and an increase of Fe-OC contribution to SOC pool, respectively; however, the NW conversion increased the contribution of MNC to SOC. The MNC was regulated by iron oxides (Fe<sub>d</sub>) and microbial biomass, while SOC and MNC had significantly positive impacts on Fe-OC. Overall, the MNC contents and its contribution to SOC were generally greater than Fe-OC in soils of the land use. Nevertheless, the importance of Fe-OC became increasingly prominent in SOC accumulation as soil salinity increased. Our findings emphasize the role of microbial necromass production and mineral preservation in SOM sequestration of estuarine soils depending on salinity and land use.</div></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":\"258 \",\"pages\":\"Article 109254\"},\"PeriodicalIF\":5.4000,\"publicationDate\":\"2025-06-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Catena\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0341816225005569\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225005569","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0

摘要

天然河口土壤是减缓气候变化的重要碳汇,但土壤有机碳(SOC)的积累及其受微生物necromass生产和矿物保存调控的潜在机制与土地利用和盐度的关系尚不清楚。本文以珠江口不同盐度的天然湿地(NW)、水产养殖池(AP)、香蕉种植园(BP)和耕地(CL) 4种典型土地利用为研究对象,采用物理分馏法对土壤微生物坏死体碳(MNC)和铁结合有机碳(Fe-OC)进行了分析。结果表明:河口土壤以矿物伴生组分为主,随着北西向的转化和盐度的增加,矿物伴生组分的比例逐渐增加;NW的MNC含量显著低于CL,但高于BP和AP,而NW的Fe-OC含量最高,其次是CL、BP和AP。随着土壤盐分的增加,MNC含量降低,Fe-OC含量增加;颗粒型Fe-OC呈下降趋势,与块状和矿物伴生Fe-OC相反。盐度升高分别导致MNC和Fe-OC对有机碳库的贡献减少和增加;然而,NW转换增加了MNC对SOC的贡献。MNC受铁氧化物(Fed)和微生物量的调节,SOC和MNC对Fe-OC有显著的正影响。总体而言,不同土地利用方式土壤中MNC含量及其对有机碳的贡献均大于Fe-OC。但随着土壤盐分的增加,Fe-OC在有机碳积累中的重要性日益突出。我们的研究结果强调了微生物坏死体的产生和矿物保存在河口土壤中SOM封存中的作用,这取决于盐度和土地利用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Changes in the microbial necromass carbon and iron-bound organic carbon following land use and salinity in estuary soils

Changes in the microbial necromass carbon and iron-bound organic carbon following land use and salinity in estuary soils
Natural estuary soils are widely recognized as important carbon sinks for climate change mitigation, however, the soil organic carbon (SOC) accumulation and its underlying mechanism regulated by microbial necromass production and mineral preservation in estuarine soils in relation to land use and salinity still remain unclear. Here, we sampled four representative land uses [e.g., Natural Wetland (NW), Aquaculture Pond (AP), Banana Plantation (BP), and Cultivated Land (CL)] with varying salinities in the Pearl River Estuary, and then the microbial necromass carbon (MNC) and iron-bound organic carbon (Fe-OC) in soils by physical fractionation were analyzed. The results showed that the estuarine soil was dominated by mineral-associated fraction, with increasing proportions as converted by NW and increased by salinity. The MNC content in NW was significantly lower than that in CL, but was higher than those of BP and AP. However, NW had the highest Fe-OC content, followed by CL, BP, and AP. As soil salinity increased, the MNC content decreased, accompanied by an increase in Fe-OC content; however, the particulate Fe-OC exhibited a downward trend, which was opposite to that of bulk and mineral-associated Fe-OC. Increased salinity induced an reduction of MNC contribution and an increase of Fe-OC contribution to SOC pool, respectively; however, the NW conversion increased the contribution of MNC to SOC. The MNC was regulated by iron oxides (Fed) and microbial biomass, while SOC and MNC had significantly positive impacts on Fe-OC. Overall, the MNC contents and its contribution to SOC were generally greater than Fe-OC in soils of the land use. Nevertheless, the importance of Fe-OC became increasingly prominent in SOC accumulation as soil salinity increased. Our findings emphasize the role of microbial necromass production and mineral preservation in SOM sequestration of estuarine soils depending on salinity and land use.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信