Chemical Speciation Analysis and Environmental Behaviour of 127I and 129I

Publication: ResearchPh.D. thesis – Annual report year: 2012

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Chemical Speciation Analysis and Environmental Behaviour of 127I and 129I. / Hansen, Violeta; Roos, Per (Supervisor).

2011. (Risø-PhD; No. 81(EN)).

Publication: ResearchPh.D. thesis – Annual report year: 2012

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Hansen, Violeta; Roos, Per (Supervisor) / Chemical Speciation Analysis and Environmental Behaviour of 127I and 129I.

2011. (Risø-PhD; No. 81(EN)).

Publication: ResearchPh.D. thesis – Annual report year: 2012

Bibtex

@phdthesis{f51c8f4fd3f746d0b8b668c6f1c391ae,
title = "Chemical Speciation Analysis and Environmental Behaviour of 127I and 129I",
keywords = "Risø-phd-81, Risø-PhD-81(EN)",
author = "Violeta Hansen and Per Roos",
year = "2011",
series = "Risø-PhD",

}

RIS

TY - BOOK

T1 - Chemical Speciation Analysis and Environmental Behaviour of <sup>127</sup>I and <sup>129</sup>I

A1 - Hansen,Violeta

AU - Hansen,Violeta

A2 - Roos,Per

ED - Roos,Per

PY - 2011

Y1 - 2011

N2 - This thesis deals with chemical speciation analysis and behaviour of the anthropogenic radioisotope 129I as well as stable iodine 127I in environmental samples such as freshwater, seawater, soils, sediments and seaweed. The behaviour and chemical speciation of iodine (127I and 129I) in environmental samples are very complex and strongly dependent on several factors, such as <br/>water/soil/sediment chemistry, seaweed type, different pH, Eh, quantity and quality of organic matter, microbiological activity as well as differences in contaminant origin. The 129I isotope, where the main inventory has been present in the biosphere for a relatively short time, may not show the same behaviour as the stable 127I isotope. The present study illustrates this. <br/>Chemical speciation analysis of 129I and 127I as iodide, iodate and total inorganic iodine in seawater samples from the Baltic Proper, Skagerrak and Kattegat has been carried out. The general trend in variability of the iodide and iodate speciation of the two iodine isotopes is, to a large extent, linked to environmental conditions. The important findings of this study are that the <br/>reduction of iodate and oxidation of iodide in Skagerrak and Kattegat may be a slow process while along the Baltic Sea surface water reduction of iodate is a relatively fast process. Although suboxic or anoxic condition are encountered in some of the Baltic Sea deep basins, the concentration of 129IO3 - increases with water depth indicating that the reduction of iodate in the oxygen <br/>deficient bottom water of the Baltic Sea is a slow process. <br/>Iodine chemical speciation analysis (as iodide, iodate and total iodine including inorganic and organic iodine species) in lake water samples collected from Denmark and southern Sweden has been carried out. Destruction of organic iodine was performed by alkaline oxidation using NaOH – NaClO at 1000C and anion exchange chromatography was used for separation of iodide and <br/>iodate. Iodine-129 concentrations in the lakes ranged from 1.3 – 12.8 ×109 at/L and show elevated concentrations in lakes located in southwest Jutland (Denmark), near the North Sea. Except the Skærsø Lake, were the organic iodine – 127 accounts for 50% of the total iodine, iodide (both 129I and 127I) is the predominant species form in surface water of the studied lakes. <br/>An investigation was conducted in order to quantify the total aquatic iodine ( <br/>129I and 127I as inorganic and organic iodine) from fresh water and seawater samples by adsorption onto activated charcoal and DEAE 32 cellulose followed by alkaline digestion or combustion. The results show that iodide from freshwater samples can easily be adsorbed onto activated charcoal. The sorption was not affected by the pH. The absorption capacity of iodate is low and reduces quickly when its concentration increases. <br/>Compared with activated charcoal, DEAE 32 cellulose showed a lower adsorption capacity of inorganic and organic iodine species. Adsorption of iodine species onto activated charcoal and DEAE 32 cellulose from seawater samples shows that only about 10% of the total iodine in seawater can be adsorbed onto those materials. Adsorption of iodine species from water samples onto activated charcoal/DEAE is not a suitable method for quantifying the total iodine in freshwater and seawater. <br/>An investigation was conducted in order to decompose organic iodine using K2S2O8 in water samples for developing a method for quantification of aquatic organic iodine (129I and 127I). The results show that iodine was quantitatively removed even when the concentration of organic iodine compounds in the studied sample was very high. Due to this, oxidation of iodine organic matter <br/>by using K2S2O8 followed by reduction of iodine species and precipitation with silver can be a potential method for determination of total iodine in fresh water samples. <br/>An improvement was made of the method for 129I and 127I speciation analysis in soil and sediment samples involving the extraction and fractionation of organic matter. The improved method was further used for the partitioning of 127I and 129I in marine sediments and soils. Sequential extraction results point out that partitioning of 127I and 129I within the organic fraction in soil and marine sediments is controlled by pH conditions where pH values below 5.0-5.5 promote occurrence of 127I and 129I in the humic acid, while at pH &gt; 6 the partitioning was in the fulvic acid fraction. Anoxic conditions seemed to increase the mobility and availability of iodine compared to oxic, while suboxic conditions (soils) reduced the availability of the water soluble fraction compared to the subaqueous (marine) one. The distribution of 129I/127I values differed significantly between phases and samples, indicating that equilibrium with stable iodine have not yet been reached for a large fraction of the released <br/>129I. This means that geochemical models based on stable iodine behavior may not necessarily be able to predict the present behavior of I-129. <br/>Concentrations of 129I and 127I in archived Fucus Vesiculosus samples collected between 2002 – 2010 at Romø (German Bight), Klint (Kattegat) and Bornholm were analysed. Since previous investigations have shown that iodine speciation differ between the sites a comparison between 129I/127I ratios in seaweed relative to water at the three sites were done in order to evaluate if <br/>uptake was independent on speciation. The 129I/127I (seaweed) relative 129I/127I (seawater) were found to be 0.5 for the North Sea (2005), 0.7 (2006) for Southern Kattegat and 0.97 (2007) for Bornholm. In spite of the very different iodine speciation at the three sites the concentration ratio seaweed to water is more or less the same indicating that Fucus Vesiculosus can be used as a bio-indicator for iodine-129 in the marine environment. The results shows however that iodide is somewhat more efficient accumulate than iodate in Fucus. <br/>A rapid on-line HPLC-ICP-MS method for direct speciation analysis of 127I (as iodide and iodate) in water samples was developed. The method was further used for the speciation analysis of 127I in freshwater and seawater (following dilution). The results demonstrate that the on-line HPLC – ICP - MS method developed in this study is reliable and efficient for accurate assay for speciation analysis of stable iodine in water samples. Due to the low concentrations of 129I in the environment the HPLC-ICPMS method cannot be applied for speciation analysis of this isotope in environmental samples but can be applied for water samples highly contaminated with 129I.

AB - This thesis deals with chemical speciation analysis and behaviour of the anthropogenic radioisotope 129I as well as stable iodine 127I in environmental samples such as freshwater, seawater, soils, sediments and seaweed. The behaviour and chemical speciation of iodine (127I and 129I) in environmental samples are very complex and strongly dependent on several factors, such as <br/>water/soil/sediment chemistry, seaweed type, different pH, Eh, quantity and quality of organic matter, microbiological activity as well as differences in contaminant origin. The 129I isotope, where the main inventory has been present in the biosphere for a relatively short time, may not show the same behaviour as the stable 127I isotope. The present study illustrates this. <br/>Chemical speciation analysis of 129I and 127I as iodide, iodate and total inorganic iodine in seawater samples from the Baltic Proper, Skagerrak and Kattegat has been carried out. The general trend in variability of the iodide and iodate speciation of the two iodine isotopes is, to a large extent, linked to environmental conditions. The important findings of this study are that the <br/>reduction of iodate and oxidation of iodide in Skagerrak and Kattegat may be a slow process while along the Baltic Sea surface water reduction of iodate is a relatively fast process. Although suboxic or anoxic condition are encountered in some of the Baltic Sea deep basins, the concentration of 129IO3 - increases with water depth indicating that the reduction of iodate in the oxygen <br/>deficient bottom water of the Baltic Sea is a slow process. <br/>Iodine chemical speciation analysis (as iodide, iodate and total iodine including inorganic and organic iodine species) in lake water samples collected from Denmark and southern Sweden has been carried out. Destruction of organic iodine was performed by alkaline oxidation using NaOH – NaClO at 1000C and anion exchange chromatography was used for separation of iodide and <br/>iodate. Iodine-129 concentrations in the lakes ranged from 1.3 – 12.8 ×109 at/L and show elevated concentrations in lakes located in southwest Jutland (Denmark), near the North Sea. Except the Skærsø Lake, were the organic iodine – 127 accounts for 50% of the total iodine, iodide (both 129I and 127I) is the predominant species form in surface water of the studied lakes. <br/>An investigation was conducted in order to quantify the total aquatic iodine ( <br/>129I and 127I as inorganic and organic iodine) from fresh water and seawater samples by adsorption onto activated charcoal and DEAE 32 cellulose followed by alkaline digestion or combustion. The results show that iodide from freshwater samples can easily be adsorbed onto activated charcoal. The sorption was not affected by the pH. The absorption capacity of iodate is low and reduces quickly when its concentration increases. <br/>Compared with activated charcoal, DEAE 32 cellulose showed a lower adsorption capacity of inorganic and organic iodine species. Adsorption of iodine species onto activated charcoal and DEAE 32 cellulose from seawater samples shows that only about 10% of the total iodine in seawater can be adsorbed onto those materials. Adsorption of iodine species from water samples onto activated charcoal/DEAE is not a suitable method for quantifying the total iodine in freshwater and seawater. <br/>An investigation was conducted in order to decompose organic iodine using K2S2O8 in water samples for developing a method for quantification of aquatic organic iodine (129I and 127I). The results show that iodine was quantitatively removed even when the concentration of organic iodine compounds in the studied sample was very high. Due to this, oxidation of iodine organic matter <br/>by using K2S2O8 followed by reduction of iodine species and precipitation with silver can be a potential method for determination of total iodine in fresh water samples. <br/>An improvement was made of the method for 129I and 127I speciation analysis in soil and sediment samples involving the extraction and fractionation of organic matter. The improved method was further used for the partitioning of 127I and 129I in marine sediments and soils. Sequential extraction results point out that partitioning of 127I and 129I within the organic fraction in soil and marine sediments is controlled by pH conditions where pH values below 5.0-5.5 promote occurrence of 127I and 129I in the humic acid, while at pH &gt; 6 the partitioning was in the fulvic acid fraction. Anoxic conditions seemed to increase the mobility and availability of iodine compared to oxic, while suboxic conditions (soils) reduced the availability of the water soluble fraction compared to the subaqueous (marine) one. The distribution of 129I/127I values differed significantly between phases and samples, indicating that equilibrium with stable iodine have not yet been reached for a large fraction of the released <br/>129I. This means that geochemical models based on stable iodine behavior may not necessarily be able to predict the present behavior of I-129. <br/>Concentrations of 129I and 127I in archived Fucus Vesiculosus samples collected between 2002 – 2010 at Romø (German Bight), Klint (Kattegat) and Bornholm were analysed. Since previous investigations have shown that iodine speciation differ between the sites a comparison between 129I/127I ratios in seaweed relative to water at the three sites were done in order to evaluate if <br/>uptake was independent on speciation. The 129I/127I (seaweed) relative 129I/127I (seawater) were found to be 0.5 for the North Sea (2005), 0.7 (2006) for Southern Kattegat and 0.97 (2007) for Bornholm. In spite of the very different iodine speciation at the three sites the concentration ratio seaweed to water is more or less the same indicating that Fucus Vesiculosus can be used as a bio-indicator for iodine-129 in the marine environment. The results shows however that iodide is somewhat more efficient accumulate than iodate in Fucus. <br/>A rapid on-line HPLC-ICP-MS method for direct speciation analysis of 127I (as iodide and iodate) in water samples was developed. The method was further used for the speciation analysis of 127I in freshwater and seawater (following dilution). The results demonstrate that the on-line HPLC – ICP - MS method developed in this study is reliable and efficient for accurate assay for speciation analysis of stable iodine in water samples. Due to the low concentrations of 129I in the environment the HPLC-ICPMS method cannot be applied for speciation analysis of this isotope in environmental samples but can be applied for water samples highly contaminated with 129I.

KW - Risø-phd-81

KW - Risø-PhD-81(EN)

BT - Chemical Speciation Analysis and Environmental Behaviour of <sup>127</sup>I and <sup>129</sup>I

T3 - Risø-PhD

T3 - en_GB

ER -