Large seasonal fluctuations of groundwater radioiodine speciation and concentrations in a riparian wetland in South Carolina

Recent studies evaluating multiple years of groundwater radioiodine (129I) concentration in a riparian wetland located in South Carolina, USA identified strong seasonal concentration fluctuations, such that summer concentrations were much greater than winter concentrations. These fluctuations were o...

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Veröffentlicht in:The Science of the total environment 2022-04, Vol.816, p.151548-151548, Article 151548
Hauptverfasser: Kaplan, Daniel I., Nichols, Ralph, Xu, Chen, Lin, Peng, Yeager, Chris, Santschi, Peter H.
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Nichols, Ralph
Xu, Chen
Lin, Peng
Yeager, Chris
Santschi, Peter H.
description Recent studies evaluating multiple years of groundwater radioiodine (129I) concentration in a riparian wetland located in South Carolina, USA identified strong seasonal concentration fluctuations, such that summer concentrations were much greater than winter concentrations. These fluctuations were observed only in the wetlands but not in the upland portion of the plume and only with 129I, and not with other contaminants of anthropogenic origin: nitrate/nitrite, strontium-90, technecium-99, tritium, or uranium. This unexplained observation was hypothesized to be the result of strongly coupled processes involving hydrology, water temperature, microbiology, and chemistry. To test this hypothesis, an extensive historical groundwater database was evaluated, and additional measurements of total iodine and iodine speciation were made from recently collected samples. During the summer, the water table decreased by as much as 0.7 m, surface water temperature increased by as much as 15 °C, and total iodine concentrations were consistently greater (up to 680%) than the following winter months. Most of the additional iodine observed in the summer could be attributed to proportional gains in organo-iodine, and not iodide or iodate. Furthermore, 129I concentrations were observed to be two-orders-of-magnitude greater at the bottom of the upland aquifer than at the top. A coupled hydrological and biogeochemical conceptual model is proposed to tie these observations together. First, as the surface water temperature increased during the summer, microbial activity was enhanced, which in turn stimulated the formation of mobile organo-I. Hydrological processes were also likely involved in the observed iodine seasonal changes: (1) as the water table decreased in summer, the remaining upland water entering the wetland was comprised of a greater proportion of water containing elevated iodine concentrations from the low depths, and (2) water flow paths in summer changed such that the wells intercepted more of the contaminant plume and less of the diluting rainwater (due to evapotranspiration) and streamwater (as the lower levels promote a predominantly recharging system). These results underscore the importance of coupled processes influencing contaminant concentrations, and the need to assess seasonal contaminant variations to optimize long-term monitoring programs of wetlands. [Display omitted] •Seasonal radioiodine concentrations repeatedly fluctuate as much as two-order-of-mag
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These fluctuations were observed only in the wetlands but not in the upland portion of the plume and only with 129I, and not with other contaminants of anthropogenic origin: nitrate/nitrite, strontium-90, technecium-99, tritium, or uranium. This unexplained observation was hypothesized to be the result of strongly coupled processes involving hydrology, water temperature, microbiology, and chemistry. To test this hypothesis, an extensive historical groundwater database was evaluated, and additional measurements of total iodine and iodine speciation were made from recently collected samples. During the summer, the water table decreased by as much as 0.7 m, surface water temperature increased by as much as 15 °C, and total iodine concentrations were consistently greater (up to 680%) than the following winter months. Most of the additional iodine observed in the summer could be attributed to proportional gains in organo-iodine, and not iodide or iodate. Furthermore, 129I concentrations were observed to be two-orders-of-magnitude greater at the bottom of the upland aquifer than at the top. A coupled hydrological and biogeochemical conceptual model is proposed to tie these observations together. First, as the surface water temperature increased during the summer, microbial activity was enhanced, which in turn stimulated the formation of mobile organo-I. Hydrological processes were also likely involved in the observed iodine seasonal changes: (1) as the water table decreased in summer, the remaining upland water entering the wetland was comprised of a greater proportion of water containing elevated iodine concentrations from the low depths, and (2) water flow paths in summer changed such that the wells intercepted more of the contaminant plume and less of the diluting rainwater (due to evapotranspiration) and streamwater (as the lower levels promote a predominantly recharging system). These results underscore the importance of coupled processes influencing contaminant concentrations, and the need to assess seasonal contaminant variations to optimize long-term monitoring programs of wetlands. [Display omitted] •Seasonal radioiodine concentrations repeatedly fluctuate as much as two-order-of-magnitude.•During summer months, radioiodine and percent organo-iodine increases.•During summer months, groundwater temperature increases and water height decreases.•Cause for seasonal fluctuations due not only to hydrology, but also biogeochemical processes.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2021.151548</identifier><identifier>PMID: 34780820</identifier><language>eng</language><publisher>Netherlands: Elsevier B.V</publisher><subject>Groundwater ; Iodine Radioisotopes - analysis ; Iodine-129 ; Organo-iodine ; Seasons ; South Carolina ; Speciation ; Temperature ; Wetlands</subject><ispartof>The Science of the total environment, 2022-04, Vol.816, p.151548-151548, Article 151548</ispartof><rights>2021 Elsevier B.V.</rights><rights>Copyright © 2021 Elsevier B.V. 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These fluctuations were observed only in the wetlands but not in the upland portion of the plume and only with 129I, and not with other contaminants of anthropogenic origin: nitrate/nitrite, strontium-90, technecium-99, tritium, or uranium. This unexplained observation was hypothesized to be the result of strongly coupled processes involving hydrology, water temperature, microbiology, and chemistry. To test this hypothesis, an extensive historical groundwater database was evaluated, and additional measurements of total iodine and iodine speciation were made from recently collected samples. During the summer, the water table decreased by as much as 0.7 m, surface water temperature increased by as much as 15 °C, and total iodine concentrations were consistently greater (up to 680%) than the following winter months. Most of the additional iodine observed in the summer could be attributed to proportional gains in organo-iodine, and not iodide or iodate. Furthermore, 129I concentrations were observed to be two-orders-of-magnitude greater at the bottom of the upland aquifer than at the top. A coupled hydrological and biogeochemical conceptual model is proposed to tie these observations together. First, as the surface water temperature increased during the summer, microbial activity was enhanced, which in turn stimulated the formation of mobile organo-I. Hydrological processes were also likely involved in the observed iodine seasonal changes: (1) as the water table decreased in summer, the remaining upland water entering the wetland was comprised of a greater proportion of water containing elevated iodine concentrations from the low depths, and (2) water flow paths in summer changed such that the wells intercepted more of the contaminant plume and less of the diluting rainwater (due to evapotranspiration) and streamwater (as the lower levels promote a predominantly recharging system). These results underscore the importance of coupled processes influencing contaminant concentrations, and the need to assess seasonal contaminant variations to optimize long-term monitoring programs of wetlands. [Display omitted] •Seasonal radioiodine concentrations repeatedly fluctuate as much as two-order-of-magnitude.•During summer months, radioiodine and percent organo-iodine increases.•During summer months, groundwater temperature increases and water height decreases.•Cause for seasonal fluctuations due not only to hydrology, but also biogeochemical processes.</description><subject>Groundwater</subject><subject>Iodine Radioisotopes - analysis</subject><subject>Iodine-129</subject><subject>Organo-iodine</subject><subject>Seasons</subject><subject>South Carolina</subject><subject>Speciation</subject><subject>Temperature</subject><subject>Wetlands</subject><issn>0048-9697</issn><issn>1879-1026</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqFkE1PXCEUhkmjqaP2L7Qsu7lTDvcD7tJMamsySRfVNUE4WCZ3YApcjUl_vExndCsbkpPnPR8PIV-ALYHB8G2zzMaXWDA8LjnjsIQe-k5-IAuQYmyA8eGELBjrZDMOozgj5zlvWH1Cwkdy1nZCMsnZgvxb6_SANKPOMeiJumk2ZdbFx5BpdPQhxTnYJ10w0aStjz5aH2pgh8b_x6gOlpoYDIaSjkFfqzT5nU5eB_qEZdpDtfo7zuUPXekUJx_0JTl1esr46fhfkLvr77ern83614-b1dW6MR1npRl7GK0TvXDWWY1tq6UwgjnbdxxYy8FwI6RDhPt2gM7Wi0cLBiS2bgAn2gvy9dB3l-LfGXNRW58NTnUrjHNWvB8lE51sx4qKA2pSzDmhU7vktzo9K2Bqr15t1Jt6tVevDupr8vNxyHy_RfuWe3VdgasDgPXUR49p3wirN-sTmqJs9O8OeQEEIJye</recordid><startdate>20220410</startdate><enddate>20220410</enddate><creator>Kaplan, Daniel I.</creator><creator>Nichols, Ralph</creator><creator>Xu, Chen</creator><creator>Lin, Peng</creator><creator>Yeager, Chris</creator><creator>Santschi, Peter H.</creator><general>Elsevier B.V</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>20220410</creationdate><title>Large seasonal fluctuations of groundwater radioiodine speciation and concentrations in a riparian wetland in South Carolina</title><author>Kaplan, Daniel I. ; Nichols, Ralph ; Xu, Chen ; Lin, Peng ; Yeager, Chris ; Santschi, Peter H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c420t-9519df757fdfdae33a87c70fd54210321c2c78fee1b3614d9699d1c18e3f61f73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Groundwater</topic><topic>Iodine Radioisotopes - analysis</topic><topic>Iodine-129</topic><topic>Organo-iodine</topic><topic>Seasons</topic><topic>South Carolina</topic><topic>Speciation</topic><topic>Temperature</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kaplan, Daniel I.</creatorcontrib><creatorcontrib>Nichols, Ralph</creatorcontrib><creatorcontrib>Xu, Chen</creatorcontrib><creatorcontrib>Lin, Peng</creatorcontrib><creatorcontrib>Yeager, Chris</creatorcontrib><creatorcontrib>Santschi, Peter H.</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>The Science of the total environment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kaplan, Daniel I.</au><au>Nichols, Ralph</au><au>Xu, Chen</au><au>Lin, Peng</au><au>Yeager, Chris</au><au>Santschi, Peter H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Large seasonal fluctuations of groundwater radioiodine speciation and concentrations in a riparian wetland in South Carolina</atitle><jtitle>The Science of the total environment</jtitle><addtitle>Sci Total Environ</addtitle><date>2022-04-10</date><risdate>2022</risdate><volume>816</volume><spage>151548</spage><epage>151548</epage><pages>151548-151548</pages><artnum>151548</artnum><issn>0048-9697</issn><eissn>1879-1026</eissn><abstract>Recent studies evaluating multiple years of groundwater radioiodine (129I) concentration in a riparian wetland located in South Carolina, USA identified strong seasonal concentration fluctuations, such that summer concentrations were much greater than winter concentrations. These fluctuations were observed only in the wetlands but not in the upland portion of the plume and only with 129I, and not with other contaminants of anthropogenic origin: nitrate/nitrite, strontium-90, technecium-99, tritium, or uranium. This unexplained observation was hypothesized to be the result of strongly coupled processes involving hydrology, water temperature, microbiology, and chemistry. To test this hypothesis, an extensive historical groundwater database was evaluated, and additional measurements of total iodine and iodine speciation were made from recently collected samples. During the summer, the water table decreased by as much as 0.7 m, surface water temperature increased by as much as 15 °C, and total iodine concentrations were consistently greater (up to 680%) than the following winter months. Most of the additional iodine observed in the summer could be attributed to proportional gains in organo-iodine, and not iodide or iodate. Furthermore, 129I concentrations were observed to be two-orders-of-magnitude greater at the bottom of the upland aquifer than at the top. A coupled hydrological and biogeochemical conceptual model is proposed to tie these observations together. First, as the surface water temperature increased during the summer, microbial activity was enhanced, which in turn stimulated the formation of mobile organo-I. Hydrological processes were also likely involved in the observed iodine seasonal changes: (1) as the water table decreased in summer, the remaining upland water entering the wetland was comprised of a greater proportion of water containing elevated iodine concentrations from the low depths, and (2) water flow paths in summer changed such that the wells intercepted more of the contaminant plume and less of the diluting rainwater (due to evapotranspiration) and streamwater (as the lower levels promote a predominantly recharging system). These results underscore the importance of coupled processes influencing contaminant concentrations, and the need to assess seasonal contaminant variations to optimize long-term monitoring programs of wetlands. [Display omitted] •Seasonal radioiodine concentrations repeatedly fluctuate as much as two-order-of-magnitude.•During summer months, radioiodine and percent organo-iodine increases.•During summer months, groundwater temperature increases and water height decreases.•Cause for seasonal fluctuations due not only to hydrology, but also biogeochemical processes.</abstract><cop>Netherlands</cop><pub>Elsevier B.V</pub><pmid>34780820</pmid><doi>10.1016/j.scitotenv.2021.151548</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record>
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subjects Groundwater
Iodine Radioisotopes - analysis
Iodine-129
Organo-iodine
Seasons
South Carolina
Speciation
Temperature
Wetlands
title Large seasonal fluctuations of groundwater radioiodine speciation and concentrations in a riparian wetland in South Carolina
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