Z. F.
Chai
*a,
Z. Y.
Zhang
a,
W. Y.
Feng
a,
C. Y.
Chen
a,
D. D.
Xu
a and
X. L.
Hou
b
aLaboratory of Nuclear Analytical Techniques, Institute of High Energy Physics, Chinese Academy of Sciences, P. O. Box 918, Beijing 100039, China. E-mail: chaizf@ihep.ac.cn
bRisø National Laboratory, NUK-202, DK-4000 Roskilde, Denmark
First published on 16th October 2003
The information on the chemical speciation of trace elements in biological and environmental systems is much needed to evaluate their biological and environmental significance. Albeit a number of atomic behavior-based analytical techniques are available for the analysis of chemical speciation of trace elements, nuclear analytical techniques, especially the molecular activation analysis method, can in many cases play a unique role. This review describes the methodology, merits and limitations of nuclear analytical techniques for chemical speciation study in biological and environmental samples. The emphases are focused on the chemical species and the environmental and biological significance of rare earth elements in natural plants and human liver, selenium in a mammalian organism, mercury in rat brain and liver, chromium in rat organs and Cr-rich yeast, organohalogens in pine needles and marine organisms, and iodine in sea-water, soil, atmosphere, marine plants and the thyroid gland for demonstration of the features of nuclear analytical techniques. The future perspectives of nuclear analytical techniques for the study of chemical species of trace elements will be briefly outlined as well.
Methoda | Accuracy | Sensitivity | Space resolution | In situ analysis | Non-destructive analysis | Matrix effect | Time response |
---|---|---|---|---|---|---|---|
a MAA, molecular activation analysis, which, in fact, is a combination of conventional neutron activation analysis with chemical or biological separation; PIXE, proton induced X-ray emission and its derivative SPM, scanning proton microscopy; SRXRF, synchronous radiation X-ray fluorescence; EXAFS, X-ray absorption fine structure spectrometry; XANES, X-ray absorption near edge spectrometry; Möss.Sp., Mössbauer spectrometry; IT, isotopic tracer. | |||||||
MAA | Excellent | High | Low | No | No | Less | Slow |
PIXE | Middle | Middle | Middle–Good | Possible | No | Yes | Fast |
SRXRF | Middle | Middle | Good | Possible | No | Yes | Fast |
EXAFS | Middle | Poor | Good | Yes | Yes | Yes | Slow |
XANES | Middle | Poor | Good | Yes | Yes | Yes | Slow |
Möss.Sp. | Limited | Poor | Poor | Yes | Yes | Yes | Fast |
IT | Good | High | Possible | Possible | Yes | Less | Fast |
ICP-MS | Good | High | Low | No | No | Severe | Slow |
![]() | ||
Fig. 1 Scheme for chemical speciation study of REEs in plant–soil system by MAA. |
It was found that REEs existing as water-soluble forms in soils were the most assimilable species for plant roots.7 Most of REEs in plant roots were firmly bound with cell wall materials,8 whereas the subcellular distributions of REEs in mesophyll protoplasts of Brassia napus clearly indicated that REEs were accumulated in chloroplasts and that every 2000 chlorophyll molecules contained one REE atom. This is one possible reason to explain why REEs are able to enhance the photosynthetic rates of crops.9–11 Moreover, the presence of two REE-binding proteins, four REE-binding polysaccharides and one REE-binding DNA in the leaves of a highly REE-enriched fern, Dicranopteris dichotoma, was demonstrated by MAA.12,13 The molecular weights (MWs) of the two REE-binding proteins were determined to be 800 kD and less than 12.4 kD, respectively. Their SDS-PAGE graphs showed that both contained two proteins subunits, which were likely glycoproteins with different glyco-units. All the four REE-binding polysaccharides were low MW polysaccharides (10–20 kD). Less than 0.1% of total REE in the plant leaves was combined with DNA. To our knowledge, it was the first time that REE-binding biological macromolecules in plants were reported.
REEs have a preferential uptake in liver after they have been absorbed into the bloodstream of a human or animal body.14 The distributions in subcellular fractions of liver cells of both rats and human beings were similar for all REEs, i.e., the highest concentration was found in the microsomal fraction, while the lowest in the cytosolic fraction.15,16 However, in cultured rat cells that were treated with rare earth ions, it was discovered by PIXE that La, Ce, and Gd existed mostly in the nuclear fraction, and then in the cell membrane.17 By means of size-exclusion chromatography (SEC), two soluble REE-binding proteins with MWs of about 68 and more than 40 kD were found in rat livers after the rats were intravenously injected by enriched stable isotope tracer of 152Sm and 168Yb. The elution profiles of 152Sm and proteins were shown in Fig. 2. With the same MAA method, at least three La-binding proteins (MW 335 ± 50, 94.5 ± 15.4, 13.6 ± 3.8 kD), three Ce-binding proteins (MW 335 ± 50, 85 ± 12, 22.8 ± 6.3 kD) and about four Sm-binding proteins (MW 335 ± 70, 82.1 ± 5.4, 32.3 ± 5.8 and 13.6 ± 4.5 kD) were found in the supernatant fraction of human liver samples, which were obtained from normal subjects who had an accidental death. Most of La, Ce and Sm were found in the high-molecular-weight protein region.16
![]() | ||
Fig. 2 Sephadex G-150 column chromatography of liver cytosol from rats injected by 152SmCl3. |
Various analytical methods have been developed for the determination of total Se content in biological samples, such as AAS, AFS, electrochemical detection, ICP-MS, radiochemical and instrumental NAA, PIXE, etc. NATs and the isotopic tracer technique are often imperative in this aspect because of their advantages of high accuracy and precision and freedom from contamination from acids or reagents used in analysis. The main application examples based on NATs for Se speciation are summarized below.
The bioavailability of anionic, cationic and neutral Se compounds and selenoamino acids such as selenocystine, selenocysteine, selenomethionine and Se-methylselenocysteine is of much clinical interest, but low-level determinations of selenium are very difficult. Blotcky et al. determined the Se metabolites, including total Se, trimethylselenonium (TMSe+) ion, selenite, and selenoamino acids in urine and plasma by using MAA combined with anion exchange chromatography.26–28
The basis of selenium’s nutritional role lies in its active involvement with glutathione peroxidase (GPx), iodothyronine deiodinases, thioredoxin reductase (TR) and other selenoenzymes in the form of selenocysteine, which has been confirmed as the 21st amino acid. Until now, about 16 selenoproteins with specific functions have been recognized,18,29,30 which, however, cannot explain all Se biological functions. Thus, there is an increasing interest in characterizing new selenoproteins in different biological species.
For most biological materials, such as tissues, cells, cell fractions and protein, etc., from rats, cattle and humans, the Se content can be determined by the conventional INAA via the short-lived 77mSe (T1/2 = 17.5 s) and long-lived 75Se (T1/2 = 121 d)31–34 with different irradiation conditions. Generally, the detection limits are 5 ng for 77mSe and 0.1 ng for 75Se. The incorporation of Se into protein as peroxidase isozymes in wheat seedlings was studied by an optimized INAA after electrophoretic separation.35 After sodium dodecyl sulfate–polyacrylamide gel electrophoresis (SDS–PAGE), the gel sections containing corresponding protein bands were cut off and subjected to INAA. The lower detection limit of 0.02 ng was achieved through longer irradiation (8.3 d) with higher neutron flux and longer radioactivity counting time. Direct determination of metals in protein bands on the electrophoretic gels by SRXRF after SDS–PAGE or isoelectric focusing separation was also developed in our laboratory.36–38 Recently, an innovative technique for the detection of Se in selenoprotein bands by using monochromator with SRXRF has been established.
Combined with biochemical separation, INAA was applied to selenium speciation in normal human tissues, human hepatocellular carcinoma and their normal liver-adjacent tissues.39–43 The distribution patterns of selenium species in healthy and patient subjects could help to identify the respective physiological roles of various Se species in human liver, heart, kidney and their compartments.31,39 In general, Se was mainly enriched in mitochondria, nuclei and cytosol. In human liver specimens, 45% of total Se was in nuclei and 25% in mitochondria and cytosol, respectively. In human heart specimens, about 70% of the total Se existed in nuclei and 20% in cytosol, while for kidney specimens about 70% was in nuclei and 14% in cytosol and mitochondria, respectively. These new findings indicate the long-term accumulation of Se in human bodies.39,40 Human hepatocellular carcinoma and their normal liver-adjacent tissues were collected from 7 patients. It is of interest to find that the Se level was higher in carcinoma tissues than in the normal adjacent tissues, while the mitochondrial and cytosolic GPx and TR were also higher.
Speciation and subcellular distribution of the Se-containing proteins in human liver were further separated by SEC and SDS–PAGE followed by INAA and HG-AFS. Eight kinds of Se-containing proteins with MWs of 335 ± 20, 249 ± 15, 106 ± 11, 84.6 ± 5.8, 70.5 ± 5.4, 45.6 ± 1.5, 14.8 ± 2.6 and 8.5 ± 1.2 kD were found in the subcellular fractions of human liver.40 The more accurate molecular weight and better resolution were obtained by SDS–PAGE than SEC. Another important advantage of SDS–PAGE was that Se weak binding or non-specific incorporation to protein would be removed after electrophoresis. It was found that about 24 kinds of Se-containing proteins existed in subcellular fractions of normal human liver.41 The MWs of their subunits were mostly in the range of 20–30 kD and 50–80 kD. The 61, 21 and 54 kD proteins were identified as the known selenoproteins such as selenoprotein P, GPx and TR, respectively. Most of the proteins are yet to be identified. The specific subcellular distributions of different Se-containing proteins suggest that they could play specific and important biological roles in each organelle of human liver.41
For a tracer study, both an enriched stable isotope, e.g., 82Se, and a radioactive isotope, 75Se, were used to study the metabolic pathway and the chemical speciation of Se in the organism. The labeled Se-containing proteins were separated by using electrophoretic or chromatographic methods, subsequently analyzed by autoradiography44–49 and ICP-MS.50,51 Selenoprotein P was found firstly in rat liver and plasma by the use of 75Se tracer.31 More than 20 selenoproteins or subunits in liver organelles and other tissues of Se-deficient rats after replenishment with 75Se-labeled selenite were reported by Behne et al.44,45
The advantage of HPLC-ICP-MS with the use of enriched stable isotopes over the conventional use of radioisotopes is that the simultaneous detection of the speciation of exogenous (labeled with enriched stable isotope) and endogenous Se are possible without a requirement for special and expensive radiotracer facilities.50,51 However, one disadvantage of the above method is that it more or less loses the structural information during the element detection process. An alternative is to use tandem mass spectrometry (MS-MS) as a detector to provide the structural and molecular information, allowing the identification of species.52 The applicability of the optimized HPLC-MS-MS system was demonstrated by the analysis of a mixture containing Se-methyl-selenocysteine, selenomethionine, selenocystine, selenoethionine and selenocystamine. For selenoprotein, the structural analysis of selenopeptide after enzymatic digestion was conducted by MALDI-TOF-MS and electrospray ionization triple quadrupole MS.53,54
The analytical methods for Hg determination are diverse. Nevertheless, NAA is usually regarded as a “reference method”, because of its excellent accuracy and high sensitivity. The detection limit for total Hg is as low as 0.1 ng g−1 by RNAA in any medium.55 Therefore, this method is very useful for small amount and rare sample analysis. In order to study the affinity of Hg to metallothionein (MT) in the brain tissue of rats that were exposed to Hg0, after gel filtration separation, Falnoga et al.56 used RNAA to analyze the concentration of Hg in rat brain supernatant. They found that about 80% of the Hg in it was in the fraction of low-molecular-weight proteins. Furthermore, a MT-like protein Hg–Cu–Zn–thionein was isolated and partially characterized.
Although the toxicities of Hg and MeHg have been extensively studied, their poison mechanisms to humans still remain unclear. For the latter study, the isotopic tracer technique would become a very powerful method. 203Hg has a suitable half life (t1/2 = 46.9 d), therefore, it is often chosen as an isotopic tracer in the study. Bhattacharya et al.57 studied the specific binding of Hg2+ to ouabain-sensitive Na(+)–K(+)–ATPase of rat liver plasma membrane using isotopic tracer 203Hg2+. They found that the binding of Hg to the enzyme caused the significant inhibition of the enzyme and that the capability of Hg2+ binding to reduced glutathione (GSH) was stimulated by GSH-S-transferase (GST). Therefore, they proposed that the transport of Hg2+ inside the cell occurred by increased dissociation of Hg2+ from the membrane due to the greater avidity of Hg2+ towards cytosolar GSH binding. The GSH–Hg complex entered the nucleus to induce MT transcription.
EXAFS is a powerful method for structural analysis, which, in recent years, has been widely used for the analysis of protein structures, especially for metalloproteins. Gailer et al.58 reported a study of the mutual detoxification of Hg–Se–S-containing species in rabbit plasma by EXAFS after chromatographic purification. The EXAFS spectroscopy revealed the presence of 4 coordinated Se and Hg entities separated by 2.61 Å. The Hg and Se near-edge X-ray absorption spectra of erythrocytes, plasma and bile of rabbits injected with sodium selenite and mercuric chloride solutions showed that Hg and Se in plasma existed as a Hg–Se–S-species.
Feng et al.59 used 50Cr3+ tracer combined with differential centrifugation and NAA to study the intracellular distribution of Cr(III) in the liver, pancreas, testes and kidney homogenates of diabetic and normal rats. They found that the nuclear fraction contained the highest Cr concentration in the liver cells of both normal and diabetic rats. The diabetic rats retained more Cr in the mitochondrial and lysosomal fractions of liver homogenate than the normal. The concentrations of Cr in the subcellular fractions of pancreas, testes and kidneys in the normal rats were higher than those in the diabetic rats. Additionally, as an advantage of the multi-element analysis ability for NAA, the significant alterations of the levels of other essential trace elements in subcellular fractions of the observed diabetic organs could be simultaneously observed as well.60 These results suggest that the hormone level change may interfere with some trace elements accumulation both in the organs and the subcellular fractions of rats. Furthermore, after intravenous injection of enriched stable isotope 50Cr tracer solution, Feng et al.61,62 separated Cr-containing proteins in the diabetic and normal rat liver cytosol, serum and urine by Sephadex G-25 gel filtration chromatography. The elution fractions were determined by NAA via50Cr(n, γ)51Cr. It was found that Cr was mainly combined with a high-molecular-weight protein in the liver cytosol and serum. A low-molecular-weight, Cr-containing compound (LMWCr) was found in all the observed liver, serum and urine samples of normal and diabetic rats. They concluded that Cr was excreted chiefly as LMWCr in urine. Recently, the fundamental distribution patterns of the Cr-containing proteins in the nucleic, mitochondrial, lysosomal, microsomal and cytosolic subcellular fractions of the rat liver were investigated by means of stable isotopic tracer technique, Sephadex G-100 gel chromatography and NAA.63 A total of 9 kinds of Cr-containing proteins were found in the five subcellular fractions and the relative MWs were identified as 96.6 ± 6.2, 68.2 ± 1.4, 57.9 ± 4.7, 36.6 ± 1.2, 24.2 ± 1.8, 14.0 ± 1.5, 8.8 ± 0.6, 6.9 ± 0.4 and 4.2 ± 0.4 kD. In this research, about 64.5% of Cr proteins were found in the cytosolic fraction. The LMW Cr proteins (<4.2 kD) were mainly observed in mitochondria, lysosomes and microsomes. More than 69% Cr-containing proteins were present in the liver cytosolic fraction of ≥57.9 kD.
As a useful and convenient chromium supplement, Cr-rich yeast is widely used for diabetics. The study of chromium speciation in the yeast is imperative to understand its biological function. Ding et al.64 assessed the Cr distribution in a Cr-rich yeast cell by NAA and found that 80.9% of Cr was accumulated in the protoplast. Furthermore, Ding et al.65 and Liu66 have studied the Cr species combined with biological macromolecular compounds, i.e., DNA, RNA, and proteins, in Cr-rich yeast by gel chromatography and electrophoretic separation followed by NAA. Liu found that in the Cr-rich yeast, most Cr-containing proteins were present as LMW Cr compounds.66
The Cr species in the Cr-rich yeast was analyzed using EXAFS and the results proved that Cr(III) was the main species in the yeast, which assured the safe intake of the high-Cr yeast.66 A new type detector was adopted to determine the XANES spectra of the yeast samples with different Cr(III)/Cr(VI) ratios, and the results showed that Saccharomyces cerevisiae strain could significantly reduce Cr(VI) to Cr(III).66
NAA is a very convenient method for halogen analysis and is also the only method currently available for simultaneously determining EOCl, EOBr and EOI in an extract.70,75,80–82 Another alternative for the analysis of total organohalogens is microcoulometric or potentiometeric titration,83–85 which, however, needs tedious and time-consuming manipulation steps: enrichment, conversion of organohalogens into halide ions and final determination. Further, it is not able to differentiate halogen elements. Thus, NAA is preferred to determine Cl, Br, I, and EOX in various biological and environmental matrices.75,80,82 The literature survey of this aspect is given in Table 2.
Sample | Analyte | Converted into halide-ion | Method | Detection limit | Ref. |
---|---|---|---|---|---|
Water | TO-Cl, -Br, -I | No | NAA | Cl 5 µg L−1: Br, I 1 µg L−1 | 86 |
TOX | Yes | Microcoulometric titration | 10 µg L−1 | 87 | |
AOX | Yes | Microcoulometric titration | 3–30 µg L−1 | 75 | |
EOCl | No | NAA | 17 µg L−1 | 88 | |
EO-Cl, -Br, -I | No | NAA | Cl 20 µg L−1: Br 5 µg L−1: I 3 µg L−1 | 89 | |
Rain and snow | EOCl | No | NAA | 20–80 µg L−1 | 90 |
AO-Cl, -Br, -I | Yes | Capillary zone electrophoresis-UV | Cl 1–3 ng g−1: Br 2–5 ng g−1: I 4–8 ng g−1 | 91 | |
Sediment | AOX, EOX | Yes | Microcoulometric titration | AOX 0.5 µg g−1: EOX 0.05 µg g−1 | 83 |
EOCl | No | NAA | 5 µg g−1 | 75 | |
EO-Cl, -Br, -I | No | NAA | 0.1 µg g−1 | 92 | |
EO-Cl, -Br, -I | No | NAA | 0.2–0.4 µg g−1 | 70 | |
EOX | Yes | Microcoulometric titration | 0.18 µg g−1 | 84 | |
Soil | EOX | Yes | Microcoulometric/pyrolysis titration | 10 µg g−1 | 93 |
Marine organism | EOX | Yes | Microcoulometric titration | 0.02–0.17 µg g−1 | 85 |
Human tissue | EO-Cl, -Br, -I | No | NAA | 0.1 µg g−1 | 92 |
Marine organism | EO-Cl, -Br, -I | No | NAA | 0.1–5 µg g−1 | 75,92 |
Shrimp | EO-Cl, -Br, -I | No | NAA | Cl 16–85 ng g−1: Br 1.0–35 ng g−1: I 0.35–10 ng g−1 | 94 |
Beluga whale | EO-Cl, -Br, -I | No | NAA | Cl 30 ng; Br 6 ng; I, 3 ng | 76 |
Pine needles | EO-Cl, -Br, -I | No | NAA | Cl 50 ng; Br 8 ng; I 3.5 ng | 81 |
Using MAA based on NAA and organic solvent extraction, Xu et al.81,95 found that the concentrations of halogens were in the order of Cl ≫ Br > I in the pine needle samples from 17 Chinese regions, which was in agreement with their elemental abundances in nature. About 0.1–3.9% of total chlorine was EOCl, whereas 0.2–15% and 2–57% of total bromine and iodine were EOBr and EOI, respectively, which suggested that halogens in pine needles mainly existed as inorganic species and non-extractable organochlorinated compounds.81 Similar results were reported for yogurt and apples.82
Further, the extract was treated by different methods before NAA measurement. The results indicated that 69–93% of total EOCl, 20–58% and 20–90% of total EOBr and EOI were water-soluble polar compounds in pine needle extracts.88 It is known that this persistent EOX (EPOX) seems to be more important for organisms. For the INAA determination of EPOX, the extract was first treated with concentrated sulfuric acid. About 1.6–38% of EOCl survived as the species EPOCl in pine needles,81 in comparison with 11.7% in blue mussel,70 11.3–11.9% in the sediment,70 23–58% in yogurt and 29–35% in apples,82 17% in water75 and 0–39% in aerosol.98 It was also found that the EPOCl concentration increased with increasing age of pine needle.81
The MWs of EOCl have been studied by gel permeation chromatography (GPC) combined with NAA75 and about 90% of EOCl in bleach plant effluent were found to be associated with low MW compounds (MW < 300), whereas 60–70% of EOCl in fish and sediment were associated with MW > 300 compounds.75 Jokela et al.99 and Hemming and Lehtinen100 also reported similar results in bleached kraft mill effluent and in rainbow-trout liver effluent.
Known organochlorine compounds were reported to account for 1.4–30.4% of the EPOCl in pine needles from China,81 1–14% in bird, 48% in sediment from the USA97 and 2–18% in marine organism from the Osaka Bay.92 The identified compounds accounted for 10–15% in fish and 5% in sediment from Bornholm in the Baltic Sea,101 whereas 13–58% of EOCl was found in carp from the Buffalo river96 and 2–25% in fish from the USA.97 About 45% of EOCl reported in blubber lipid of beluga whales is attributed to the known compounds.76 Similarly, 25–50% of EOCl in herring gull eggs from Lake Ontario can be explained by the known compounds.102 In Japanese human adipose tissue, about 59% of EOCl can be accounted for by PCBs, DDTs, PCTs and HCHs.92 The above comparison indicates that the unknown proportion of EOCl was higher in almost all environmental and biological samples.
There is debate about the sources of EOCl and EPOCl in environmental matrices, since most compounds with heteroatoms (oxygen or nitrogen atom) or an unsaturated bond, such as most known naturally occurring OCs, can be protonated or destroyed and removed from the extracts after treatment with concentrated sulfuric acid.80,103 It is known that environmental factors have a heavy impact on EPOCl accumulation in pine needles. Thus, a conclusion can be drawn that EPOCl in pine needles is mainly originated from the ambient atmosphere.81 Kiceniuk et al.76 also found that it was impossible to account for the observed high levels of EOCl in tissues of beluga whales from natural compounds. However, in fish and sediment 60–80% of EOCl can be hydrolyzed by lipase and about 30% of EOCl were acidic material.91 By NATs Lunde and Steinnes104 showed that a certain amount of EOCl in marine organism oil was synthesized by natural processes in the marine environment. Grimvall105 found that the major part of organohalogens in freshwater and the marine environment came from the natural incorporation of halogens into humic substances or other macromolecules. Also, it was found that Cl and Br can be bound to aromatic rings in humic substances,106 a chloroperoxidase-like catalyst in soil.107 Until now, although many studies show that organohalogens have many natural sources, the quantitative contribution of the naturally produced organohalogens has not been estimated. Anthropogenic and atmospheric input have still been considered to be the main sources of organohalogens in the Baltic Sea environment.90 Further studies are needed to estimate the contributions of naturally produced and anthropogenic sources in various environmental samples, to characterize the potential toxicity of organohalogens in aquatic and terrestrial ecosystem, and to better understand the unknown EOCl, for which NATs are imperative.
Iodine in water exists as iodate, iodide and organic iodine.108 The distribution of iodide and iodate in sea-water can give a clue to understanding the marine environment and has been quite well studied. Hou et al. developed a MAA method based on NAA and chemical separation for the determination of iodide, iodate, organic iodine and total iodine in water sample.109 A similar technique was also used for the determination of 129I in iodide and iodate species, which can be used to investigate the geochemical cycle of stable iodine.110 It was found that in the coast water from the North Sea, 50–60% of iodine exists as iodate and 40–50% as iodide, while most of iodine exists as iodide (>80%) in the Baltic Sea water. A low concentration of organic iodine was observed in all sea-water samples measured. A similar result was also reported using iodimetric spectrophotometry for iodate, catalytic spectrophotometry for total inorganic iodine and irradiation with UV-light followed by catalytic spectrophotometry for organic iodine in the Baltic Sea.111 Reifanhauser and Heumann112 developed a method by combining isotope dilution mass spectrometry (IDMS) with anion exchange separation to investigate the chemical species of iodine in fresh water. Besides iodide and iodate, anionic organic iodine and non-elutable organic iodine were determined. They observed that most of iodine existed as organic iodine in lake and river water.
Iodine mainly exists as inorganic iodine in sea-water. In open sea-water most of iodine is iodate, while in coastal or anoxic sea-water (such as the Baltic Sea) the concentration of iodide is high. The concentration of organic iodine in lake and river water is higher than that in sea-water. Although the concentration of organic iodine in sea-water is low, it plays a very important role in the global geochemical cycle of iodine, because the transfer of iodine from the iodine rich ocean to the atmosphere, then to the terrestrial environment, is thought to occur primarily through the volatilization of organic iodine hydrocarbon in the sea-water.113 These volatile organic iodine species were also supposed to relate to ozone depletions in the stratosphere.114 Various volatile organic iodine compounds, and CH3I, CH2ClI, CH2I2 and CH3CH2CH2I have been observed in the sea-water.115
The concentration of iodine in the atmosphere ranges from 0.2 to 10 ng m−3; a high iodine concentration was observed in an urban area due to the combustion of oil and coal. In the atmosphere, iodine exists as particle-bound iodine (particulate iodine), inorganic gas iodine (I2, HI, HOI) and organic gas iodine (CHI3, CH2I2, CH3CH2CH2I), whose concentrations vary with various parameters, such as location, season and climate. The particulate iodine is usually separated and collected using Millipore filter or glass microfibre.116–119 I2 and HI can be separated by adsorption using an LiOH (NaOH) impregnated filter117,118 or silver screens.116 HOI is normally collected by tetrabutylammonium hydroxide (TBAH) impregnated filter117 or charcoal filter116 and organic iodine by charcoal bed116,117 or triethylenediamine (TEDA) impregnated charcoal bed.118 Then, the various iodine species can be determined by NAA or ICP-MS.
Due to high concentration of iodine in marine plants, the chemical species of iodine in a plant is mainly focused on seaweed. Hou et al. developed a MAA method for the determination of various chemical species of iodine in seaweed, such as water soluble iodine, soluble organic iodine, iodide, iodate, and protein-, pigment- polyphenol- or polysaccharide-bound iodine.120,121 The results show that 9–99% of iodine is water-soluble in seaweed. In addition, the percentage of water soluble iodine is the highest in brown algae and lowest in green algae. In the water leachate of seaweed, iodine exists mainly as iodide, the percentage of organic iodine makes up 5–40%, and the iodate is lower than 5% in all 30 species of seaweed investigated. In biological macromolecules, iodine is mainly bound with proteins, polyphenol and pigments, but little iodine is bound with polysaccharide. It is also found that iodine in seaweed also exists as iodinated amino acid and non-polar derivatives of secondary metabolites. In addition, iodinated compounds in seaweed can also exist as part of a complex of polyhalogented compounds with bromo- or chloro-analogues. Using alkaline hydrolysis, organic solvent extraction, GC, HPLC and gel chromatography, many iodine-containing compounds, such as monoiodothyrosine (MIT), diiodothyrosine (DIT), triiodothyroine (T3), thyroxine (T4) and 1-iododibromoheptanone were separated and identified from different seaweeds.122–124
Iodine is a normal component of thyroid gland, and mainly exists as iodo-amino acids such as MIT, DIT, T3, rT3, and T4, which are mainly bound with proteins in thyroid but function as free T3 and T4. Beside thyroid, iodine is also distributed in all tissues.125 The radioimmunoassay method is widely used for the determination of T3, T4 and rT3 in blood for diagnosis of thyroid diseases. Hou et al. investigated the distribution of iodine in various subcellular fractions of human liver using gradient centrifugation coupled with NAA126 and observed that the iodine content is in the order of nuclei > cytosol > mitochondria > lysosome > microsome. Furthermore, gel chromatography was used to investigate the combination of iodine with protein in cytosol of human liver, and observed 3 iodine proteins in which iodine is mainly bound with mid- and high-molecular weight proteins. Because most iodine is bound with macromolecular protein, the sample has to be enzymolysed, then iodine ion and various iodo-amino acids can be separated and measured for determination of the concentrations of iodo-amino acids. HPLC was successfully used to determine various chemical species of iodine, such as I, MIT, DIT, T3, T4, rT3 and iodopolypeptide in hydrolyzed solution of thyroid, serum, urine and milk.127–131
Soil is the main source of iodine for terrestrial plants, so that the chemical species of iodine in soil is directly related to the bioavailability of iodine to plant. From the radiation protection point of view, the chemical species of radioactive 129I is the most important issue to affect the transfer of 129I in the environment. Hou et al. studied the chemical fractionation of 129I in soil and sediment using NATs combined with sequential extraction techniques and observed that iodine was mainly bound with organic matter and oxides. Only 10–20% of iodine was in the readily available phase (water soluble and exchangeable fractions).132 The high level of iodine in the organic fraction is attributed to the ability of the humic substance to fix iodine,133 in which a microorganism was thought to participate.134 Solvent extraction and HPLC were used to study the chemical species of iodine in soil solution.112,134 In a similar way to in water, iodine exists as iodide, iodate and organic iodine, in which the iodine is mainly bound with humic substance.
This journal is © The Royal Society of Chemistry 2004 |