Enhanced decoupling of multiple elements in coastal reclaimed soils following intensive agricultural use in eastern China

IF 10 1区 环境科学与生态学 Q1 ENGINEERING, ENVIRONMENTAL
Shengzhi Liu, Xiaobo Bian, Yifeng Zhu, Danyang Wang, Aijing Yin, Pengbao Wu, Xiaohui Yang, Zhaofu Li, Qiang Shu, Huan Zhang, Chao Gao
{"title":"Enhanced decoupling of multiple elements in coastal reclaimed soils following intensive agricultural use in eastern China","authors":"Shengzhi Liu, Xiaobo Bian, Yifeng Zhu, Danyang Wang, Aijing Yin, Pengbao Wu, Xiaohui Yang, Zhaofu Li, Qiang Shu, Huan Zhang, Chao Gao","doi":"10.1016/j.jclepro.2026.148093","DOIUrl":null,"url":null,"abstract":"Understanding the biogeochemical coupling of multiple soil elements is essential to evaluating soil health and ecosystem stability. However, the effects of long-term coastal wetland reclamation on soil elemental enrichment and geochemical interactions remain poorly understood. This study aimed to elucidate the evolution of multi-element behavior in soils across a chronosequence (0, 10, 30, 65, and 90 years) of coastal reclamation. We conducted a comprehensive analysis of 31 elements (including As, Al, B, Br, Ca, Cd, Cl, Co, Cr, Cu, F, Fe, Hg, I, K, Mg, Mn, Mo, N, Na, Ni,C, P, Pb, Rb, S, Sb, Si, Sn, Sr, Zn) in the soils, focusing on exploring the evolution of element enrichment, dispersion, correlation, and multi-element coupling (MEC) along the reclamation gradient during an increase in reclamation duration. The results revealed that several elements were significantly enriched after reclamation, whereas others remained below background levels. Fertilization, irrigation, and intensive cultivation significantly alter the soil geochemical processes and elemental interactions. With the extension of the reclamation duration, the concentrations of organic carbon (SOC), N, P, Zn, Cu, Cd, Hg, F, and Cl increased, whereas those of S, Na, Mg, Ca, Cr, Mn, Sr, Br, As, and Mo decreased, highlighting the regulatory role of agricultural activities in shaping elemental distribution. Temporal declines in the number of positive correlations, mean correlation coefficients, and MEC values suggest progressive weakening of element coupling under human influence. Major elements maintained higher correlation strengths and coupling degrees than minor elements, indicating greater resistance to anthropogenic disturbances. Partial least squares path modeling (PLS-PM) revealed that while MEC is primarily regulated by stable natural factors such as soil texture, human activities also serve as key drivers of elemental decoupling because of their continuous and cumulative impacts on soil element interactions. This study provides novel insights into the long-term alteration of geochemical interactions in reclaimed soils and emphasizes the need for sustainable management strategies to preserve soil multifunctionality in coastal reclamation regions.","PeriodicalId":349,"journal":{"name":"Journal of Cleaner Production","volume":"24 1","pages":""},"PeriodicalIF":10.0000,"publicationDate":"2026-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Cleaner Production","FirstCategoryId":"93","ListUrlMain":"https://doi.org/10.1016/j.jclepro.2026.148093","RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
引用次数: 0

Abstract

Understanding the biogeochemical coupling of multiple soil elements is essential to evaluating soil health and ecosystem stability. However, the effects of long-term coastal wetland reclamation on soil elemental enrichment and geochemical interactions remain poorly understood. This study aimed to elucidate the evolution of multi-element behavior in soils across a chronosequence (0, 10, 30, 65, and 90 years) of coastal reclamation. We conducted a comprehensive analysis of 31 elements (including As, Al, B, Br, Ca, Cd, Cl, Co, Cr, Cu, F, Fe, Hg, I, K, Mg, Mn, Mo, N, Na, Ni,C, P, Pb, Rb, S, Sb, Si, Sn, Sr, Zn) in the soils, focusing on exploring the evolution of element enrichment, dispersion, correlation, and multi-element coupling (MEC) along the reclamation gradient during an increase in reclamation duration. The results revealed that several elements were significantly enriched after reclamation, whereas others remained below background levels. Fertilization, irrigation, and intensive cultivation significantly alter the soil geochemical processes and elemental interactions. With the extension of the reclamation duration, the concentrations of organic carbon (SOC), N, P, Zn, Cu, Cd, Hg, F, and Cl increased, whereas those of S, Na, Mg, Ca, Cr, Mn, Sr, Br, As, and Mo decreased, highlighting the regulatory role of agricultural activities in shaping elemental distribution. Temporal declines in the number of positive correlations, mean correlation coefficients, and MEC values suggest progressive weakening of element coupling under human influence. Major elements maintained higher correlation strengths and coupling degrees than minor elements, indicating greater resistance to anthropogenic disturbances. Partial least squares path modeling (PLS-PM) revealed that while MEC is primarily regulated by stable natural factors such as soil texture, human activities also serve as key drivers of elemental decoupling because of their continuous and cumulative impacts on soil element interactions. This study provides novel insights into the long-term alteration of geochemical interactions in reclaimed soils and emphasizes the need for sustainable management strategies to preserve soil multifunctionality in coastal reclamation regions.
中国东部沿海垦殖土壤多元素解耦效应增强
了解多种土壤元素的生物地球化学耦合是评价土壤健康和生态系统稳定性的基础。然而,长期滨海湿地围垦对土壤元素富集和地球化学相互作用的影响尚不清楚。本研究旨在阐明沿海填海的不同时间序列(0、10、30、65和90年)土壤多元素行为的演变。对土壤中As、Al、B、Br、Ca、Cd、Cl、Co、Cr、Cu、F、Fe、Hg、I、K、Mg、Mn、Mo、N、Na、Ni、C、P、Pb、Rb、S、Sb、Si、Sn、Sr、Zn等31种元素进行了综合分析,重点探讨了随着开垦时间的延长,土壤中元素的富集、分散、相关性和多元素耦合(MEC)的演变规律。结果显示,填海后一些元素显著富集,而其他元素则低于背景水平。施肥、灌溉和集约耕作显著改变了土壤地球化学过程和元素相互作用。随着垦殖时间的延长,土壤有机碳(SOC)、N、P、Zn、Cu、Cd、Hg、F和Cl的浓度增加,而S、Na、Mg、Ca、Cr、Mn、Sr、Br、As和Mo的浓度降低,表明农业活动对土壤元素分布的调节作用。正相关数、平均相关系数和MEC值的时间下降表明,在人类影响下,元素耦合逐渐减弱。主元素的相关强度和耦合度高于小元素,对人为干扰的抵抗能力更强。偏最小二乘路径模型(PLS-PM)表明,土壤MEC主要受土壤结构等稳定自然因子的调控,但人类活动对土壤要素相互作用的持续和累积影响也成为要素去耦的关键驱动因素。本研究为复垦土壤中地球化学相互作用的长期变化提供了新的见解,并强调了可持续管理策略的必要性,以保持沿海复垦地区土壤的多功能性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Journal of Cleaner Production
Journal of Cleaner Production 环境科学-工程:环境
CiteScore
20.40
自引率
9.00%
发文量
4720
审稿时长
111 days
期刊介绍: The Journal of Cleaner Production is an international, transdisciplinary journal that addresses and discusses theoretical and practical Cleaner Production, Environmental, and Sustainability issues. It aims to help societies become more sustainable by focusing on the concept of 'Cleaner Production', which aims at preventing waste production and increasing efficiencies in energy, water, resources, and human capital use. The journal serves as a platform for corporations, governments, education institutions, regions, and societies to engage in discussions and research related to Cleaner Production, environmental, and sustainability practices.
×
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
小红书