Wenjing Shi , Xinya Zhao , Yizhe Liu , Haoran Xu , Changwei Lü , Weiping Li
{"title":"寒区湖泊冰期FeP耦合对沉积物中砷的影响","authors":"Wenjing Shi , Xinya Zhao , Yizhe Liu , Haoran Xu , Changwei Lü , Weiping Li","doi":"10.1016/j.gexplo.2025.107903","DOIUrl":null,"url":null,"abstract":"<div><div>The redox behavior of iron (Fe) significantly impacts the biogeochemical cycle of arsenic (As), with iron minerals serving as major reservoirs for phosphate (P). The cycle of As inherently associates with its species. However, the effect of Fe<img>P coupling on As species in lake sediments remain largely unknown, especially during the ice-bound period. The novelty of this study is to explore the effect of Fe<img>P coupling on As speciation during an ice-bound period using PLS-SEM model based on As、Fe and P species as well as environmental factors monitoring in sediments. Our findings revealed that Fe<img>P coupling accounts for 95.7 % of As speciation variability, playing a pivotal role in As transformation and partitioning, particularly in labile As pool that contained adsorbed As, moderately labile As pool that closely related to iron species, and pyrite-coprecipitated As. The significant influence of Fe<img>P coupling on the reductive transformation and re-distribution of amorphous and crystalline iron oxides, which in turn affects As adsorption-desorption processes. This interaction subsequently influences the speciation of Fe and P, as well as the release and ecotoxicity of As. Notably, exchangeable phosphorus, iron-bound P fraction and organic P fraction (OP) were identified as the primary P species mediating the effects of Fe<img>P coupling on As speciation. Interesting, OP also play the major role in the effect of Fe<img>P coupling on As species, potentially releasing As adsorbed on crystalline Fe hydroxides during organic matter mineralization. Results emphasize the importance of Fe(hydro)oxides and P in controlling As partitioning, with iron (hydro)oxides being particularly critical in P behavior and its interaction with As. This work provides insights into the cycling of As and the enrichment of P and As in sediment-water systems, providing a reference for environmental monitoring and remediation in sedimentary environments facing dual risks of As pollution and eutrophication.</div></div>","PeriodicalId":16336,"journal":{"name":"Journal of Geochemical Exploration","volume":"280 ","pages":"Article 107903"},"PeriodicalIF":3.3000,"publicationDate":"2025-09-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The effect of FeP coupling on arsenic species in sediments during the ice-bound period of lakes in cold regions\",\"authors\":\"Wenjing Shi , Xinya Zhao , Yizhe Liu , Haoran Xu , Changwei Lü , Weiping Li\",\"doi\":\"10.1016/j.gexplo.2025.107903\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The redox behavior of iron (Fe) significantly impacts the biogeochemical cycle of arsenic (As), with iron minerals serving as major reservoirs for phosphate (P). The cycle of As inherently associates with its species. However, the effect of Fe<img>P coupling on As species in lake sediments remain largely unknown, especially during the ice-bound period. The novelty of this study is to explore the effect of Fe<img>P coupling on As speciation during an ice-bound period using PLS-SEM model based on As、Fe and P species as well as environmental factors monitoring in sediments. Our findings revealed that Fe<img>P coupling accounts for 95.7 % of As speciation variability, playing a pivotal role in As transformation and partitioning, particularly in labile As pool that contained adsorbed As, moderately labile As pool that closely related to iron species, and pyrite-coprecipitated As. The significant influence of Fe<img>P coupling on the reductive transformation and re-distribution of amorphous and crystalline iron oxides, which in turn affects As adsorption-desorption processes. This interaction subsequently influences the speciation of Fe and P, as well as the release and ecotoxicity of As. Notably, exchangeable phosphorus, iron-bound P fraction and organic P fraction (OP) were identified as the primary P species mediating the effects of Fe<img>P coupling on As speciation. Interesting, OP also play the major role in the effect of Fe<img>P coupling on As species, potentially releasing As adsorbed on crystalline Fe hydroxides during organic matter mineralization. Results emphasize the importance of Fe(hydro)oxides and P in controlling As partitioning, with iron (hydro)oxides being particularly critical in P behavior and its interaction with As. This work provides insights into the cycling of As and the enrichment of P and As in sediment-water systems, providing a reference for environmental monitoring and remediation in sedimentary environments facing dual risks of As pollution and eutrophication.</div></div>\",\"PeriodicalId\":16336,\"journal\":{\"name\":\"Journal of Geochemical Exploration\",\"volume\":\"280 \",\"pages\":\"Article 107903\"},\"PeriodicalIF\":3.3000,\"publicationDate\":\"2025-09-09\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geochemical Exploration\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0375674225002353\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geochemical Exploration","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0375674225002353","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
The effect of FeP coupling on arsenic species in sediments during the ice-bound period of lakes in cold regions
The redox behavior of iron (Fe) significantly impacts the biogeochemical cycle of arsenic (As), with iron minerals serving as major reservoirs for phosphate (P). The cycle of As inherently associates with its species. However, the effect of FeP coupling on As species in lake sediments remain largely unknown, especially during the ice-bound period. The novelty of this study is to explore the effect of FeP coupling on As speciation during an ice-bound period using PLS-SEM model based on As、Fe and P species as well as environmental factors monitoring in sediments. Our findings revealed that FeP coupling accounts for 95.7 % of As speciation variability, playing a pivotal role in As transformation and partitioning, particularly in labile As pool that contained adsorbed As, moderately labile As pool that closely related to iron species, and pyrite-coprecipitated As. The significant influence of FeP coupling on the reductive transformation and re-distribution of amorphous and crystalline iron oxides, which in turn affects As adsorption-desorption processes. This interaction subsequently influences the speciation of Fe and P, as well as the release and ecotoxicity of As. Notably, exchangeable phosphorus, iron-bound P fraction and organic P fraction (OP) were identified as the primary P species mediating the effects of FeP coupling on As speciation. Interesting, OP also play the major role in the effect of FeP coupling on As species, potentially releasing As adsorbed on crystalline Fe hydroxides during organic matter mineralization. Results emphasize the importance of Fe(hydro)oxides and P in controlling As partitioning, with iron (hydro)oxides being particularly critical in P behavior and its interaction with As. This work provides insights into the cycling of As and the enrichment of P and As in sediment-water systems, providing a reference for environmental monitoring and remediation in sedimentary environments facing dual risks of As pollution and eutrophication.
期刊介绍:
Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics.
Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to:
define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas.
analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation.
evaluate effects of historical mining activities on the surface environment.
trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices.
assess and quantify natural and technogenic radioactivity in the environment.
determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis.
assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches.
Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.