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Abstract

Thallium transfer from naturally (pedogeochemically) contaminated soils into vegetables was studied. Three different types of top-soil (heavy, medium, and light) were used for pot experiments. The soils were collected from areas with low, medium, and high levels of pedogeochemical thallium (0.3, 1.5 and 3.3 mg kg(-1)). The samples of vegetables were collected and analysed. The total content of thallium in soil and the type of soil (heavy, medium and light), plant species and plant variety were found to be the main factors influencing thallium uptake by plants. The uptake of thallium from soils with naturally high pedogeochemical content of this element can be high enough to seriously endanger the food chain. These findings are very important because of the high toxicity of thallium and the absence of threshold limits for thallium in soils, agricultural products, feedstuffs and foodstuffs in most countries, including the Czech Republic.
For Peer Review Only
Tl uptake from contaminated soils into vegetables
Journal:
Food Additives and Contaminants
Manuscript ID:
TFAC-2005-330.R1
Manuscript Type:
Original Research Paper
Date Submitted by the
Author:
06-Dec-2005
Complete List of Authors:
Pavlíčková, Jana; MZLU Brno
Zbíral, Jiří; UKZUZ Brno, Soil Sci.
Smatanová, Michaela; UKZUZ Brno, Soil Sci.
Habarta, Petr; MZLU Brno
Houserová, Pavlína; MZLU Brno
Kuban, Vlastimil; Mendel University, Chemistry and Biochemistry
Methods/Techniques:
Metals analysis - ICP, ICP/MS, Risk assessment
Additives/Contaminants:
Environmental contaminants, Toxic elements
Food Types:
Vegetables
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Food Additives and Contaminants
peer-00577579, version 1 - 17 Mar 2011
Author manuscript, published in "Food Additives and Contaminants 23, 05 (2006) 484-491"
DOI : 10.1080/02652030500512052
For Peer Review Only
1
Uptake of Thallium from Naturally Contaminated Soils into Vegetables 1
2
3
Jana Pavlíčková
1
Jiří Zbíral
2†
Michaela Smatano
2†
Petr Habarta
1†
Pavlína Houserová
1†
4
& Vlastimil Kubáň
13†
* 5
6
1
Department of Chemistry and Biochemistry,
Mendel University of Agriculture and 7
Forestry, Zemědělská 1, CZ-613 00 Brno, Czech Republic,
2
Central Institute for 8
Supervising and Testing in Agriculture, Hroznova 2, CZ-656 06 Brno, Czech Republic
3
9
Corresponding author* 10
11
12
* Phone (+420) 545 133 285, fax (+420) 545 212 044; E-mail address: kuban@mendelu.cz 13
These authors contributed equally to this work 14
15
Received xx. November 2005 Accepted in revised form……. 16
17
Key words: thallium; uptake; contamination; vegetables; kale; rape; kohlrabi; cucumber; 18
onion; parsley; celery; pot tests; pot trials 19
20
21
Abstract 22
Thallium transfer from naturally (pedogeochemically) contaminated soils into vegetables 23
was studied. Three different types of top-soil (heavy medium and light) were used for pot 24
experiments. The soils were collected from areas with low, medium and high levels of 25
pedogeochemical thallium (0.3 1.5 and 3.3 mg kg
-1
). The samples of vegetables were 26
collected and analysed. The total content of thallium in soil and the type of soil (heavy, 27
medium, and light), plant species and plant variety were found to be the main factors 28
influencing thallium uptake by plants. The uptake of thallium from soils with naturally high 29
pedogeochemical content of this element can be high enough to seriously endanger food 30
chain. These findings are very important because of the high toxicity of thallium and the 31
absence of threshold limits for thallium in soils, agricultural products, feedstuffs and 32
foodstuffs in most countries, including the the Czech Republic 33
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Introduction 35
36
Thallium is a rare and dispersed element with a geochemical behaviour very near to K and 37
Rb (Rehkämper and Nielsen 2004). Thallium can mimic potassium in metabolic processes 38
(Tremel et al. 1997a) because of similar ionic radii (Tl 170 pm K 164 pm and Rb 172 pm) 39
and it can be found in micaceous minerals (Shannon 1976). But thallium displays also 40
chalcogenic behaviour and can be found in some sulphide minerals and in sulphur 41
containing ores (Merian 1991; Sager 1998; Jones et al. 1990). 42
43
The acute and chronic toxicity of thallium (Tl) is similar to the toxicity of cadmium, mercury 44
and lead (Sager 1998; Sáňka et al. 2000). Thallium is toxic to all organisms in both, 45
monovalent and trivalent form. Human exposure to this element can result in harmful 46
effects including death. Intoxication is associated with disorders of the nerve and digestion 47
systems and Na/K metabolism. Symptoms include polyneuropathy and loss of hair 48
(Repetto et al. 1998). In adults oral lethal doses of thallium are estimated to range 49
between 6 and 40 mg kg
-1
with an average dose of 10-15 mg kg
-1
(ATSDR 1999; Ewerts 50
1988). In spite of the potential toxicity to animals and humans thallium has received only 51
little attention. 52
53
Common thallium contents in mafic rocks range from 0.05 to 0.4 mg kg
-1
and in acid rocks 54
from 0.5 to 2.3 mg kg
-1
. Calcareous sedimentary rocks contain as little as 0.01 to 0.14 mg 55
kg
-1
Tl (Kabata-Pendias and Pendias 2001). The median content of thallium 0.29 mg kg
-1
56
and the maximum more than 50 mg kg
-1
were found for French soils (Tremel et al. 1997a; 57
Tremel et al. 1997b). Content of thallium in soils in the range from 1.5 to 6.9 mg kg
-1
was 58
reported in China in the area of natural Tl-rich sulphide mineralization (Xiao et al. 2004). It 59
was found that pedogeohemical concentration of thallium in some areas of the Czech 60
Republic is more than ten times higher than the median of the values (maximum 3.7 mg 61
kg
-1
; median 0.25 mg kg
-1
). No anthropogenic contamination was proved and higher 62
thallium contents were only of pedogeochemical origin (Zbíral et al. 2000; Zbíral et al. 63
2002; Pavlíčková et al. 2003; Bunzl 2001; Dmowski and Budarek 2002; Medek et al. 64
2001). The highest contents of this element were found in soils derived from granite (2 - 4 65
mg kg
-1
) or paragneiss (0.5 - 1 mg kg
-1
). 66
67
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Anomalous levels of thallium in soils are derived from soil substrate or from an 68
anthropogenic contamination (LaCoste et al. 1991). Ore smelting (Olkusz and Bokowo, 69
Poland; Lanmuchang Metallogenic Belt, China), cement production (Lengerich, Germany) 70
and combustion of fossil fuels are the main anthropogenic sources of soil contamination 71
(Jones et al. 1990; Kemper et al. 1991; Lustigman et al. 2000; Lin et al. 1999a; Lin et al. 72
1999b; Sager 1986; Wierzbicka et al. 2004). 73
74
Uptake of thallium by different plants was studied mainly on anthropogenically 75
contaminated soils or in the field and pot experiments after addition of thallium. It was 76
found that plants exhibit species dependent preferences (Xiao et al. 2004) and particularly 77
brassicaceous plants can reach very high concentrations of thallium in their tissues without 78
any symptoms of phytotoxicity. Iberis intermedia Guers. and Biscutella laevigata L. can 79
have thallium concentration above 1 % dry matter (DM) and can be used for 80
phytoremediation or phytomining of thallium (Anderson et al. 1999). Kale (Brassica 81
oleracea acephala L. cv. Winterbor) was found to have behaviour of thallium 82
hyperaccumulating plant (Husam et al. 2003). Selection of suitable cultivars with low 83
thallium uptake can contribute to reduce the food chain contamination. There were 84
observed only small differences between the studied varieties for rape but there were 85
differences more than twenty fold for the kale varieties (Kurz et al. 1999). Some authors 86
studied equilibrium establishment between plant available and plant non-available 87
fractions of thallium in soils (Pavlíčková et al. 2005). They proved that the equilibrium is 88
soil dependent and diffusion driven process. Plants (especially brassicaceous) can 89
accumulate much more thallium than determined as a plant available fraction by extraction 90
of soil with some weak extractants. 91
92
LaCoste et al. (LaCoste et al. 1991) tested 11 vegetables in pot trials for two levels of soil 93
Tl. 36 crops including 3 wild plants were planted on soils with the thallium content from 1.5 94
to 6.9 mg kg
-1
(soils were derived from the thallium rich sulphide ores). In both cases 95
authors proved very strong species dependent preferences in thallium uptake. Contents up 96
to 495 mg kg
-1
were found in green cabbage (Xiao et al. 2004). Tremel and Mench (Tremel 97
and Mench 1998) recommended monitoring of rape cattle cakes and brassicacea fodders 98
for thallium content because their study demonstrated strong possibility of plant 99
contamination by thallium of pedogeochemical origin. Rape (Brassica napus L.) was tested 100
on soils with different content of added thallium and also on soils with higher 101
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pedogeochemical content of this element. Higher transfer of thallium was observed in the 102
case of artificially contaminated soils. But the uptake of thallium from soils with naturally 103
high content of thallium was found to be high enough to seriously endanger food chain 104
(Zbíral et al. 2000; Zbíral et al. 2002; Pavlíčková et al. 2003; Medek et al. 2001; Pavlíčková 105
et al. 2005). 106
107
No recommended maximum values are available at the present time in most countries. In 108
Germany 0.46 2.24 mg kg
-1
DM (or 0.4 - 2 mg kg
-1
88% DM) was established for feed 109
(anonymous 1997; ananymous 1998). We can take thallium concentration 0.4 - 2 mg kg
-1
110
DM for fodder crops and 0.25 0.5 kg
-1
DM for food as a provisional working limit. The 111
values 0.25 and 0.4 mg kg
-1
DM were used for the evaluation of our results. Our study was 112
focused on two areas in the Czech Republic with naturally higher contents of thallium 113
found in our preliminary studies (Sáňka et al. 2000; Zbíral et al. 2000; Zbíral et al. 2002; 114
Pavlíčková et al. 2003; Medek et al. 2001; Pavlíčková et al. 2005). The main goal was to 115
find suitable crops that can be planted in these areas without contamination of food chain 116
by thallium and also to find plants that should be avoided in the areas because of their 117
ability to accumulate thallium in their tissues. 118
119
MATERIALS AND METHODS 120
121
Instruments 122
Plant samples (except rape seeds) were finely ground using a high-speed mill Grindomix 123
(Retsch, Germany) and digested by nitric acid in the closed high-pressure microwave 124
system (Ethos SEL, Milestone, Italy). Dry matter (DM) was determined (2 g of a sample 125
105 ºC) using a MA 30 moisture analyser (Sartorius GmbH, Goetingen, Germany). A 126
sixteen-position double heating block with digestion tubes and coolers MB 422 BH (Uni 127
Elektro, Hradec Králové, Czech Republic) was applied for soil digestion. A sub-boiling 128
distillation unit BSB-939-IR (Berghof BSB-939-IR, Germany) was used for purification of 129
nitric acid. ICP-MS ELAN 6000 (Perkin-Elmer SCIEX, Norwalk, USA) with a cross flow 130
nebulizer Scott’s type spray chamber and Gilson 212 peristaltic pump was used for 131
determination of Tl. The MS part was regularly checked by a calibrating solution (Perkin-132
Elmer SCIEX, Norwalk, USA). The operating parameters were identical with those given in 133
the previous papers (Zbíral et al. 2000; Zbíral et al. 2002; Pavlíčková et al. 2003; Medek et 134
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al. 2001; Pavlíčková et al. 2005). Operational parameters of the instruments are given in 135
Table 1. 136
Reagents. 137
All reagents and standard solutions were prepared using Milli Q deionised water (Millipore, 138
Bedford, USA). All chemicals were of reagent grade purity purchased from (Analytika, 139
Prague, Czech Republic) and Merck (Darmstadt, Germany). Stock standard solutions 140
1000 ± 2 mg L
-1
Tl in 2% (v/v) nitric acid and 1000 ± 2 mg L
-1
Lu in 2% (v/v)
nitric acid 141
(Analytika, Prague, Czech Republic) were used for preparing of calibrating standard 142
solutions. 143
Pot experiments 144
Soils with different pedogeochemical contents of Tl. Three different soils were collected - 145
Nivnice (heavy soil - HS 0.3 mg Tl kg
–1
DM), Heřmanice (medium soil - MS 1.5 mg Tl kg
–1
146
DM) and Lužice (light soil - LS 3.3 mg Tl kg
–1
DM). The content of thallium (expressed as 147
mg Tl kg
–1
of dry matter - DM) in all cases was only of pedogeochemical origin. Basic 148
characteristics of the soils are summarised in Table 2. 7.5 kg of air-dried soil (particles less 149
than 2 cm) were used for filling a pot. Six replicates for each soil and each plant (90 pots 150
for the experiment) were used. Five crops - spring rape, winter rape, kale, kohlrabi and 151
maize were tested in the first year and celery, parsley, carrot, and onion were tested in the 152
same pots next year (for the scheme of the experiment see Table 3). Winter rape was 153
sowed in each pot in August. Normally developed plants were singled out in September. 154
Other crops were sowed in April and singled out in May. The fully matured plants were 155
harvested in July. The soils were fertilized with N (NH
4
NO
3
), P (CaHPO
4
.2 H
2
O) and K 156
(KCl) according to the individual demands of each crop to provide a sufficient nutrient 157
supply. The pots were protected against rain during the whole period. Soil moisture was 158
adjusted to 60% of maximum water capacity by daily watering with deionized water. During 159
the harvest the plant parts were collected separately weighed and stored for analysis. 160
Sample preparation and digestion. 161
Plant samples were mechanically cleaned immediately after the harvest and subsequently 162
by a quick washing with deionised water to remove the rest of soil and dust particles. Plant 163
samples were dried and finely ground. The rapeseeds were analysed without grinding. The 164
all samples (1 g) were digested by nitric acid (8 ml HNO
3
and 10 ml H
2
O) in the microwave 165
digestion system at 145 ºC and 700 W for 5 min 180 ºC and 600 W for another 5 min and 166
finally at 180 ºC and 1000 W for the next 5 min. The digests were adjusted to the final 167
volume of 50 ml with deionized water. The digests were further diluted 1-20 times by 168
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deionized water before the ICP/MS measurement. Each series consisted of a suitable 169
amount of samples given by the procedure one internal reference standard and two 170
blanks. 171
Soil samples were air-dried gently crushed and sieved. Fraction < 2 mm according 172
to ISO 11464 was used for the analysis. Soils were digested (Pavlíčková et al. 2003) by 173
HNO
3
-H
2
O
2
(2 g soil sample 10 ml HNO
3
and 20 ml H
2
O
2
were used boiling for four hours 174
under cooler). Soil extracts were diluted 5 - 10 times by deionized water before the 175
ICP/MS determination. Each series consisted of a suitable number of samples given by 176
the procedure two internal reference standards and two blanks. 177
Determination of thallium by ICP/MS. 178
Single element calibrating standard solutions were used for calibration of the ICP/MS 179
instrument at five different concentrations of thallium (0, 1, 5, 10 and 50 µg L
-1
). Lutetium 180
at the concentration 10 µg L
-1
was used as an internal standard (
175
Lu signals). The 181
extraction agents acids and lutetium concentrations in the standard calibrating solutions 182
matched their concentrations in the sample solutions. The calibration curve was linear in 183
the whole calibrating range (r 0.9999). Limit of detection 1.2 µg kg
-1
was achieved for the 184
samples (3 S/N criterion). Thallium content was determined from
205
Tl signal. 185
186
RESULTS AND DISCUSSION 187
188
The results of the pot experiments are given in Tables 4 and 5 for Brassicaceous plants 189
and the other crops respectively. The contents of thallium in different parts of the crops for 190
all three investigated soils are given in Figure 1. Average total uptake of thallium from the 191
experimental pot did not follow exactly the concentration of thallium in soil. Uptake of 192
thallium from the light soil (Lužice) with the highest content of thallium (3.3 mg kg
-1
) was 193
ten times higher than from both other soils. 194
195
The bioaccumulating factor - BAF (concentration of thallium in plant (or its 196
part)/concentration of thallium in soil) reflects thallium availability from the given soil. The 197
highest bioaccumulating factors were found for the light soil (Lužice) and than for the 198
heavy soil (Nivnice). Thallium in medium soil (Heřmanice) in spite of its relatively high level 199
(1.5 mg kg
-1
) was found to be less available. BAFs for non-brassicaceous plants were 200
usually below 0.1 even for the soil from Lužice. Higher BAFs for these plants were 201
observed for green parts of vegetables (onion, carrot, parsley) than for other parts. Celery 202
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was the only exception of this rule. The situation was substantially different for plants of 203
the Brassicaceae family. BAFs for spring and winter rape were near 1 as found also in the 204
previous studies focused on this crop (Zbíral et al. 2000; Zbíral et al. 2002; Pavlíčková et 205
al. 2003; Medek et al. 2001; Pavlíčková et al. 2005). BAFs higher than 0.4 were found for 206
the other tested brassicaceous plants (except for stalk of kale and kohlrabi). BAF 2.6 was 207
observed as high as for the green part of kohlrabi. 208
209
The translocation factor TLF (the ratio of thallium concentration in different parts of the 210
plant) shows that for most crops (brassicaceous and others) higher thallium concentration 211
is located in the green part of the plant. The highest TLF was found for kohlrabi (19), kale 212
(10), but also for onion (10) and carrot (8). Concentration of thallium in celeriac part of 213
celery was found to be higher than in the green part. 214
215
If we take thallium concentration 0.4 - 2 mg kg
-1
DM for fodder crops and 0.25 0.5 kg
-1
216
DM for food as a provisional working limit and adopt 0.25 and 0.4 mg kg
-1
for the 217
evaluation (anonymous 1997; anonymous 1998) it can be concluded that for heavy soils 218
from Nivnice, and (a bit surprisingly) medium soils (Heřmanice) most crops and their parts 219
were below the limit. Straw of spring rape was above the limit and leaves of kale just on 220
the limit for food on medium soil (Heřmanice). The green part of kohlrabi was able to 221
accumulate thallium even from soil with only a background content of thallium and this part 222
of plant proved to be unsuitable for food or feed for all investigated soils. Brassicaceous 223
plants grown on light soil (Lužice) substantially exceeded the limits with only one exception 224
stalk of kale. Non-braccicaceous crops showed also relatively high concentration of 225
thallium on light soil (Lužice). The celeriac part of celery and the green part of parsley 226
exceeded the limit for food and the green parts of carrot and onion exceeded the limit for 227
feed. 228
229
CONCLUSIONS 230
231
The total content of thallium in soil, physico-chemical form and form of binding to soil 232
particles seem to be the main factors influencing the uptake by a plant. From the data 233
presented hereby it can be seen that thallium is an exception since the values obtained for 234
other elements in all vegetables are significant smaller than the corresponding plant-soil 235
concentration ratios for the uncontaminated soil. These results demonstrate quantitatively 236
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that the ability of a plant to accumulate a metal compared to a control soil might not exist 237
for an anthropogenically contaminated soils and vice-versa. In addition thallium can be 238
present as Tl(I) or Tl(III) which makes it necessary to distinguish between these two 239
species (Lin et al. 1999a; Lin et al. 1999b). Without this specification a correct toxicological 240
evaluation is not possible particularly since Tl(I) possibly occurs in soluble whereas T(III) in 241
colloidal form. 242
243
Uptake of thallium by plants is species dependent. Plant varieties and plant parts differ in 244
the degree of uptake and accumulation of Tl. Some brassicaceous plants commonly grown 245
as vegetables behave as hyperaccumulators of Tl. Content of thallium in different aerial 246
parts of tested plants can differ substantially (nearly 20 times in maximum). The highest 247
concentration was observed mainly in the green parts of the particular plants. Green part 248
of kohlrabi can contain thallium in concentration exceeding the provisional limit even if 249
grown on soil with very low natural content of Tl. 250
251
The concentration of thallium in vegetables in many cases can substantially exceed the 252
concentration of thallium in soils. Thus thallium content should be monitored and the plants 253
with high thallium accumulation power should be excluded from growing for human or 254
animal nutrition in contaminated areas. The above mentioned facts are often neglected 255
because legal measures are usually taken only for the areas anthropogenically 256
contaminated as a result of a human activity. Uptake of thallium from soils with naturally 257
high content of thallium can be high enough to seriously endanger food chains (directly by 258
consumption of plants grown on contaminated soils indirectly by consumption of meat from 259
animals feed by rape cattle cakes a by-product of rapeseed oil production). 260
261
Acknowledgments 262
263
Financial support from the Grant Agency of the Czech Republic, grant No. GA ČR 264
525/01/0908, and from the Ministry of Education Youth and Sports of the Czech Republic, 265
grant No. MSM 43210001 is gratefully acknowledged. 266
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REFERENCES 267
268
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R, Stewart RB. 1999. Phytomining for nickel, thallium and gold. J. Geochem. Explor. 270
67:407-415. 271
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Fassung vom 19. November 1997. BGBL I Nr. 77 vom 24. November 1997 2714. 274
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Landwirtschaftlichen Tiere. VDI – Richtlinie 2310 Blatt 29 (E). VDI/DIN – Handbuch 277
Reinhaltung der Luft. Band 1a. 278
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ATSDR Toxicological Profiles for Thallium. 1999. Roper WL. (Ed.). CRC Press, Boca 280
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Bunzl K, Trauttmannsheimer M, Schramel P, Reifenhauser W. 2001. Availability of arsenic 283
copper lead thallium and zinc to various vegetables grown in slag-contaminated soils. 284
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of the Boleslaw zinc smelter in Bukowo (Poland). A preliminary study. Acta Biol. 288
Cracov. Bot. 44:57-61. 289
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Ewers U. 1988. Environmental exposure to thallium. Sci. Total Environ. 71:285-292. 291
Husam Al Najar, Schulz R, Rımheld V. 2003. Plant availability of thallium in the 292
rhizosphere of hyperaccumulator plants: a key factor for assessment of 293
phytoextraction. Plant Soil 249:97-105. 294
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Jones KE, Lepp NW, Obbard JP. 1990. Thallium. In: Alloway JB. (Ed.) Heavy Metals in 296
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Kemper FH, Bertram HP. 1991. Thallium. In Metals and their Compounds in the 302
Environment. Merian E. (Ed.). VCH. Weinhaim (FRG): pp. 1227-1241. 303
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Kurz H, Schulz R, Rımheld V. 1999. Selection of cultivars to reduce the concentration of 305
cadmium and thallium in food and fodder plants. J. Plant Nutr. Soil Sci. 162:323-328. 306
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LaCoste Ch, Robinson B, Brooks R. 2001. Uptake of thallium by Vegetables: Its 308
significance for human health phytoremediation and phytomining. J. Plant Nutr. 309
24:1205-1215. 310
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Lin TS, Nriagu J. 1999a. Thallium speciation in the Great Lakes. Environ. Sci. Technol. 312
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Lin TS, Nriagu J. 1999b. Thallium speciation in river waters with Chelex-100 resin. Anal. 315
Chim. Acta 395:301-307. 316
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Anacystis nidulans and Chlamydomonas reinhardtii. Bull. Environ. Contam. Toxicol. 319
64:565-573. 320
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Medek P, Pavlíčková J, Zbíral J, Čižmárová E, Kubáň V. 2001. Inductively Coupled 322
Plasma Mass Spectrometric Determination of Thallium in Soils and Winter Rapeseeds. 323
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Procedures for Extraction of Twenty One Elements from Soils. Anal. 330
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Pavlíčková J, Zbíral J, Smatanová M, Houserová P, Čižmárová E, Havlíková Š, Kubáň V. 333
2005. Uptake of Thallium from Artificially and Naturally Contaminated Soils into Rape 334
(Brassica napus L.). J. Agric. Food Chem. 53:2867-2871. 335
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Rehkämper M, Nielsen SG. 2004. The mass balance of dissolved thallium in oceans. Mar. 337
Chem. 85:125-139. 338
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Repetto G, del Peso A, Repetto M. 1998. Human thallium toxicity. In: Nriagu JO. (Ed.). 340
Thallium in the Environment. Wiley, New York: pp. 167-199. 341
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Sager M. 1998 Thallium in agricultural practice. In: Nriagu JO. (Ed.). Thallium in the 343
Environment. Wiley, New York: pp. 59-87. 344
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Sager M. 1986. Trace Analysis of Thallium. (In German). Georg Thieme Vrlg: Stuttgart 346
FRG. 347
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ňka M, Němec P, Havlíková Š. 2000. Evaluation of thallium content in arable spoil and 349
its influence on quality of agricultural production. (In Czech). ÚKZÚZ, Brno, Czech 350
Republic. 351
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Shannon RD. 1976. Revised effective ionic radii and systematic studies of interatomic 353
distances in halides and chalcogenides. Acta Crystallogr. A 32:751-767. 354
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Tremel A, Masson P, Sterckeman T, Baize D, Mench M. 1997a. Thallium in French 356
Agrosystems - I. Thallium Contents in Arable Soils. Environ. Pollut. 95:293-302. 357
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Tremel A, Masson P, Garraud H, Donard OXF, Baize D, Mench M. 1997b. Thallium in 359
French agrosystems - II. Concentration of thallium in field-grown rape and some other 360
plant species. Environ. Pollut. 97:161-168. 361
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Tremel A, Mench M. 1998. Study of the mobility bioavailability and phytotoxicity of thallium 363
from non-point sources. INRA, Villenave d'Ornon (France). 364
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Plants from The Vicinity of Olkusz (Poland). Ecotox. Environm. Safety 59:84-88. 367
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Xiao T, Guha J, Boyle D, Liu C-Q, Chen J. 2004. Environmental Concerns related to high 369
Thallium Levels in Soils and Thallium uptake by Plants in Southwest Guizhou China 370
Sci. Tot. Environm. 318:223-244. 371
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Zbíral J, Medek P, Kubáň V, Čižmárová E, Němec P. 2000. Determination of Thallium in 373
Aqua-regia Soil Extracts by ICP-MS. Commun. Soil. Sci. Plant Anal. 31:2045- 2051. 374
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Zbíral J, Pavlíčková J, Havlíková Š, Čižmárová E, Němec P, Sáňka M, Kubáň V, Medek P. 376
2002. Comparison of Several Soil Extractants for Determination of Thallium. Commun. 377
Soil Sci. Plant Anal. 33:3303-3312. 378
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Caption to figure 379
Fig. 1. Relationship between content of thallium [in mg kg
-1
DM] in the soil and its uptake 380
by separate parts of the test plants [in mg kg
-1
DM] for Brassicaceous family (bottom) and 381
the other crops (top) respectively. 382
383
384
385
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Table 1. Operational parameters of Elan 6000 ICP-MS 386
387
Parameter Value Parameter Value
Rf Power 1050 W Readings/Replicate 1
Nebulizer Gas Flow 0.94 L min
-1
Number of Replicates 5
Lens Voltage 7.3 V Measurement Mode Peak hopping
Detector Dual mode Sample Flow Rate 1 mL min
-1
Sweeps/Readings 10
Dwell Time of Isotopes
100 ms
388
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Table 2. Basic Characteristics of Topsoils
a
Used for Pot Experiments (All Data Given for DM) 389
390
Parameter Unit Nivnice Heřmanice Lužice
Tl
b
mg kg
-1
0.3 1.5 3.3
pH/CaCl
2
6.9 6.1 6.4
P
c
mg kg
-1
105 310 62
K
c
mg kg
-1
798 702 174
Mg
c
mg kg
-1
281 152 636
Ca
c
mg kg
-1
4730 2260 2520
Fraction < 10 µm % 54.3 22.1 17
Fraction < 1 µm % 32.5 7.2 5.2
Fraction 1-10 µm % 21.8 14.9 11.8
Fraction 10-50 µm % 20.8 16.9 16.3
Fraction 50-250 µm % 17.7 18.9 27.4
Fraction 0.25-2 mm % 7.2 42.1 39.3
Nitrogen (tot.) % 0.25 0.18 0.17
Cox
d
% 1.79 2.29 1.72
TEC
e
mM.kg
-1
410 405 368
391
a
Nivnice (heavy soil) Heřmanice (medium soil) and Lužice (light soil). 392
b
Content in H
2
O
2
- HNO
3
extract.
c
Content according to Mehlich 3.
d
oxidized forms of carbon.
e
393
total exchange capacity of the soils394
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Table 3. Species and Cultivars Used in Experiments 395
396
Plant
1
Species Cultivar
2
Pot
3
Symbol
4
Maize
5
Zea mays L. Cemilk H285 12/4 A
Celery
6
Apium graveolens var. Rapaceum Maxim -/2 A
Parsley
6
Petroselinum crispum cvar. Erfurtense Dobra 20/8 B
Carrot
6
Daucus carota L. Berjo 20/8 C
Onion
7
Allium cepa L. Všetana -/6 D
Spring rape
8
Brassica napus L. cvar. Napus
9
Golda 20/10 E
Winter rape
8
Brassica napus L. cvar. Napus Zoro 20/10 D
Kale
8
Brassica oleracea L. var. Acephala Winterbor F1 6/2 B
Kohlrabi
8
Brassica oleraceae L. cvar. Gongylodes Olmia 6/2 C
397
1
family
2
cultivar/trade name
3
number of seeds/plants per pot
4
sequence of the tests in 2002/2003 398
years A/A B/B C/C and D/D
5
Maize
6
Apiaceae
7
Liliaceae
8
Brassicaceae
9
form annua 399
400
401
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Table 4. Non-Brassicaceous Plants. Average Yield of Vegetables (Plants) [g DM] Average Total 402
Uptake of thallium [µg] by Vegetables from One Pot The Biological Absorption Coefficients (BAC 403
= plant/soil concentration quotient) The Translocation Factor (TLF = Leaves (Straw)/Root (Stalk 404
Seeds) thallium Concentration). 405
406
Maize Celery Parsley Carrot Onion
Site
b
Leaves Root
(celeriac)
Leaves
(tops)
Root Leaves Root Leaves Onion Tops
Average Yield in One Pot [g DM]
Nivnice 75.6 (3) 34.8 (12) 26.5 (16) 27.5 (16) 21.8 (10) 27.7 (24) 17.0 (19) 12.7 (26) 2.9 (19)
Heřmanice
63.8 (8) 18.2 (27) 13.8 (16) 22.7 (14) 16.3 (6) 15.3 (15) 8.9 (16) 8.0 (14) 2.3 (12)
Lužice 65.6 (9) 3.8 (42) 4.7 (27) 3.4 (33) 3.8 (28) 5.6 (64) 5.4 (35) 7.0 (24) 1.6 (25)
Average Total Uptake of Thallium from One Pot [µg]
Nivnice 0.13 (3) 0.37 (20) 0.19 (18) 0.12 (12) 0.14 (28) 0.09 (15) 0.40 (30) 0.02 (21) 0.05 (19)
Heřmanice
0.20 (22) 0.79 (25) 0.24 (31) 0.40 (19) 0.53 (24) 0.18 (19) 0.86 (32) 0.05 (17) 0.09 (15)
Lužice 1.99 (7) 1.21 (41) 0.78 (20) 0.67 (36) 1.41 (37) 1.02 (38) 2.84 (25) 0.91 (32) 1.33 (33)
Average BAC
Nivnice 0.006 (0.3)
0.036 (22)
0.024 (20)
0.015 (16)
0.021 (20)
0.011 (18)
0.079 (32)
0.006 (22)
0.057 (24)
Heřmanice
0.002 (21) 0.029 (14)
0.011 (22)
0.012 (11)
0.022 (23)
0.008 (16)
0.066 (35)
0.004 (6) 0.027 (11)
Lužice 0.008 (8) 0.098 (17)
0.051 (16)
0.061 (23)
0.111 (22)
0.071 (14)
0.165 (15)
0.040 (16)
0.243 (14)
Average TLF
Nivnice _ 0.7 (34) 1.5 (29) 7.1 (36) 10.1 (15)
Heřmanice
_ 0.8 (34) 1.8 (19) 8.3 (31) 6.5 (16)
Lužice _ 0.4 (31) 1.8 (21) 2.3 (16) 6.2 (11)
407
a
RSD [%] is given in parenthesis (n = 6).
b
Nivnice (heavy soil) Heřmanice (medium soil) and 408
Lužice (light soil). 409
410
411
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Table 5. Brassicaceous Plants. Average Yield of Vegetables (Plants) [g DM], Average Total Uptake 412
of Thallium g] by Vegetables from One Pot, the Biological Absorption Coefficients (BAC = 413
plant/soil concentration quotient), and the Translocation Factor (TLF = Leaves (Straw)/Root (Stalk 414
Seeds) Thallium Concentration). 415
kale spring rape winter rape (17) kohlrabi
site
b
stalk leaves seeds straw seeds straw root leaves
Average Yield in One Pot [g DM]
Nivnice 3.3 (21) 14.7 (28) 10.7 (18) 34.7 (11) 7.4 (26) 15.4 (26) 9.4 (49) 20.1 (15)
Heřmanice 1.9 (9) 8.2 (14) no seed 24.7 (14) 5.7 (23) 13.4 (22) 7.3 (13) 10.9 (16)
Lužice 2.4 (20) 11.7 (7) 2.2 (46) 30.0 (9) 4.2 (16) 14.2 (18) 7.0 (20) 11.8 (6)
Average Total Uptake of Thallium from One Pot [µg]
Nivnice 0.06(32) 2.23 (26) 1.64 (18) 3.13 (9) 1.21 (37) 2.27 (22) 0.32 (36) 12.0 (17)
Heřmanice 0.05 (16) 2.04 (14) no seed 9.58 (22) 1.13 (26) 2.45 (15) 0.45 (23) 12.2 (23)
Lužice 0.36 (23) 18.1 (7) 5.50 (35) 42.6 (16) 14.7 (29) 36.1 (18) 4.46 (38) 96.4 (31)
Average BAC
Nivnice 0.065 (13) 0.515 (13) 0.511 (5) 0.303 (11) 0.539 (23) 0.500 (13) 0.096 (18) 1.94 (8)
Heřmanice 0.017 (18) 0.166 (6) no seed 0.261 (9) 0.132 (19) 0.124 (13) 0.043 (26) 0.70 (14)
Lužice 0.046 (12) 0.470 (2) 0.804 (21) 0.432 (17) 1.07 (24) 0.743 (24) 0.192 (29) 2.60 (20)
Average TLF
Nivnice 8 (14) 0.6 (12) 1 (21) 19 (17)
Heřmanice 10 (17) No seed 1 (20) 17 (16)
Lužice 10 (12) 0.5 (11) 0.7 (12) 14 (14)
a
RSD [%] is given in parenthesis (n = 6).
b
Nivnice (heavy soil) Heřmanice (medium soil) and Lužice (light soil). 416
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0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1.0
0.3 1.5 3.3 0.3 1.5 3.3 0.3 1.5 3.3 0.3 1.5 3.3 0.3 1.5 3.3
Tl in soil mg.kg
-1
Tl in plant
mg.kg
-1
root
leaves, tops
417
418
419
420
421
422
423
0.0
2.0
4.0
6.0
8.0
10.0
0.3 1.5 3.3 0.3 1.5 3.3 0.3 1.5 3.3 0.3 1.5 3.3
Tl in soil mg.kg
-1
Tl in plant
mg.kg
-1
stalk, seeds, root
leaves, straw
424
Fig 1. Relationship between the content of thallium [in mg kg
-1
DM] in the soil and its uptake by separate parts of test 425
plants [in mg kg
-1
DM] for Brassicaceous plants (bottom) and the other crops (top) respectively. 426
427
spring rape
maize
celery
parsley
carrot
onion
kale
winter rape
kohlrabi
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peer-00577579, version 1 - 17 Mar 2011
... In recent years, Tl has become a technology-critical element because of its utilization in semiconductor and electro-optical industries, which may contribute to new sources of Tl released to the environment [5,6]. When released into the soil, Tl can be taken up by plants and then enter the human food chain [7][8][9][10][11]. The background level of Tl in edible plants is generally low, ranging from 0.03 to 0.3 mg kg −1 [12]. ...
... The background level of Tl in edible plants is generally low, ranging from 0.03 to 0.3 mg kg −1 [12]. In areas with high Tl levels, the Tl contents of edible plants could be much higher [9,11,13,14]. For example, as high as 500 mg kg −1 of Tl in green cabbage was detected in a Tl-contaminated area in China [15]. ...
Article
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This study investigated the uptake of thallium (Tl) by rice seedlings grown in different soils with varying physiochemical properties and Tl levels to elucidate the key factors governing soil Tl availability and accumulation in rice plants. The bioconcentration factors of Tl in rice roots (2.5–25.6) and shoots (1.5–14.7) indicated high soil Tl availability and efficient uptake and translocation of Tl in rice plants, with significant variations across soil types. Growth suppression and visual toxic symptoms, such as stem buckling, yellowish leaf tips, and withering leaf edges, occurred at low soil Tl levels due to high Tl toxicity. The accumulation of Tl by rice plants was influenced by both soil and plant-related factors. Cation exchange reactions primarily influenced the concentration of Tl in soil solution, with potassium ions (K+) acting as competitors for cation exchange sites with Tl+ ions and effective inhibitors of Tl uptake by rice plants. Increasing soil K content may mitigate soil Tl availability in contaminated soils by reducing soil Tl(I) adsorption and plant uptake. This study elucidates the key mechanisms governing soil Tl bioavailability and highlights potential management strategies to reduce Tl accumulation in crops.
... High TI concentrations led to a significant decrease in plant growth, photosynthesis, accompanied by widespread pigment oxidation (Mazur et al., 2016). Furthermore, TI (I) may be able to interfere with S-containing compounds by binding to sulfhydryl groups, and thus exerting toxic effects on amino acids metabolism (Pavlíčková et al., 2006;Queirolo et al., 2009). The uptake of TI by plants differs according to concentration of TI in soil, organic matter of soil and other elements (Kwan and Smith, 1991;Markert, 2017;Vaněk et al., 2011). ...
... For instance, TI concentrations can range from 2 to 100 mg kg -1 in pine trees and reaching 5.5 mg kg -1 in mushrooms with a notably high TI content (Shacklette et al., 1978). In the same context, plants belonging to Brassicaceae are known for their ability to accumulate increased levels of TI, so they are called hyperaccumulator plants (Madejón et al., 2007;Pavlíčková et al., 2006;C. Wang et al., 2013). ...
... The vegetable types were selected due to a high consumption worldwide. The aims of this study were to; 1) conduct a controlled growth experiment to determine concentrations of TCEs in paired soil and vegetable samples; and 2) undertake an assessment of (Chung and Lee, 2013), u (Chitambar, 2010), v (Kim et al., 2018), w (Salminen et al., 2005), x (Tanaka, 2004), y (SGU, 2020a), z (Zheng et al., 2020), aa (Stjernman Forsberg and Eriksson, 2002), bb (SGU, 2020b), cc (Chang et al., 2020b), dd (Veal et al., 2010), ee (Moyer et al., 2002), ff (Nikishina et al., 2013), gg , hh (Ray et al., 2020), ii (Schulz et al., 2017), jj (SGU, 2020c), kk (Kominkova et al., 2017), ll (Roy and Hardej, 2011), mm (Kazantzis, 2000), nn (Duri et al., 2020), oo (Karbowska, 2016), pp (Wang et al., 2013), qq (Liu et al., 2017), rr (Pavlíčková et al., 2006), ss , tt (Heim et al., 2002), uu (Xiao et al., 2004) A. Qvarforth et al. Environment International 169 (2022) 107504 TCEs potential risk for entering food chains by determining bioconcentration factors (BCFs) for the TCEs, and comparing these to the BCFs of five traditional metal contaminants (TMCs; As, Cd, Cu, Pb and Zn) and two major soil elements, of which one (K) is also a major plant nutrient; thus, actively and easily taken up by plant roots, and the other one (Al) constituting an element with a near-negligible root uptake (Engström et al., 2008;McBride et al., 2013). ...
... Karbowska (2016), describe a relatively high solubility of Tl, and many are of the opinion that the Tl uptake is facilitated by its resemblance to K (Duri et al.. 2020;Xiao et al., 2004, Yu et al., 2018. Particularly hyper accumulative edible plants for Tl appear to be Brassicaceous plants such as cabbage (Kazantzis, 2000;LaCoste et al., 2001;Ning et al., 2015;Pavlíčková et al., 2006). However, resulting concentrations in vegetables should in most cases still be low relative to the TMCs, as a result of Tl's low concentration in the soils (Table 2). ...
Article
Technology-critical elements (TCEs) include most rare earth elements (REEs), the platinum group elements (PGEs), and Ga, Ge, In, Nb, Ta, Te, and Tl. Despite increasing recognition of their prolific release into the environment, their soil to plant transfer remains largely unknown. This paper provides an approximation of the potential for plant uptake by calculating bioconcentration factors (BCFs), defined as the concentration in edible vegetable tissues relative to that in cultivation soil. Here data were obtained from an indoor cultivation experiment growing lettuce, chard, and carrot on 22 different European urban soils. Values of BCFs were determined from concentrations of TCEs in vegetable samples after digestion with concentrated HNO3, and from concentrations in soil determined after 1) Aqua Regia digestion and, 2) diluted (0.1 M) HNO3 leaching. For comparison, BCFs were also determined for 5 traditional metal contaminants (TMCs; As, Cd, Cu, Pb, and Zn). The main conclusions of the study were that: 1) BCF values for the REEs were consistently low in the studied vegetables; 2) the BCFs for Ga and Nb were low as well; 3) the BCFs for Tl were high relative to the other measured TCEs and the traditional metal contaminants; and 4) mean BCF values for the investigated TCEs were generally highest in chard and lowest in carrot. These findings provide initial evidence that there are likely to be real and present soil-plant transfer of TCEs, especially in the case of Tl. Improvements in analytical methods and detection limits will allow this to be further investigated in a wider variety of edible plants so that a risk profile may be developed.
... Although literature revealed that, in general, the high bioavailable concentration of PTEs in soils found correspondence with an easier accumulation in plants and other organisms (Karbowska, 2016), Tl uptake by plants was found to be species dependent. Several brassicaceous plants have been reported to behave as (hyper)accumulators of Tl (Pavlíčková et al., 2006;Vaněk et al., 2010;Al-Najar et al., 2003) and also some conifers are able to accumulate Tl in needles, leaves, and wood (Vaněk et al., 2011;Wang et al., 2022). Our study showed peculiar uptake capabilities and high values of Tl also in chestnut trees. ...
... After thallium contaminates the soil, it can be absorbed by plants [17]. Previous studies have indicated that thallium is present in vegetables from various regions, with the type of plant being a significant factor influencing absorption. ...
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This review offers a synthesis of the current understanding of the impact of low-dose thallium (Tl) on public health, specifically emphasizing its diverse effects on various populations and organs. The article integrates insights into the cytotoxic effects, genotoxic potential, and molecular mechanisms of thallium in mammalian cells. Thallium, a non-essential heavy metal present in up to 89 different minerals, has garnered attention due to its adverse effects on human health. As technology and metallurgical industries advance, various forms of thallium, including dust, vapor, and wastewater, can contaminate the environment, extending to the surrounding air, water sources, and soil. Moreover, the metal has been identified in beverages, tobacco, and vegetables, highlighting its pervasive presence in a wide array of food sources. Epidemiological findings underscore associations between thallium exposure and critical health aspects such as kidney function, pregnancy outcomes, smoking-related implications, and potential links to autism spectrum disorder. Thallium primarily exerts cellular toxicity on various tissues through mitochondria-mediated oxidative stress and endoplasmic reticulum stress. This synthesis aims to shed light on the intricate web of thallium exposure and its potential implications for public health, emphasizing the need for vigilant consideration of its risks.
... In this study, the uppermost Tl concentration levels in the woods were noticed in species other than S3. Pavlíčková et al. (2006) stated that the intake of Tl by plants varied between the species and plant organs differed in terms of Tl intake and accumulation. Similar outcomes were also narrated in many previous studies carried out on heavy metals and it was emphasized that heavy metal accumulation significantly varied by species (Erdem et al., 2023) and organs in the same species (Karacocuk et al., 2021). ...
Article
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Background Thallium (Tl), which is one of the most toxic and destructive heavy metals for human and environmental health, has a higher level of chronic and acute toxicity in comparison to many harmful elements (such as Pb, Hg, Cd, and As) in comparison to many harmful elements and is classified as one of 13 primary metal contaminants by the US EPA (United States Environmental Protection Agency) and in ATSDR’s primary pollutant list. Thus, monitoring the Tl pollution in the air and reducing the pollution are among the primary research subjects. The existing study aims to determine the species that are suitable for monitoring and reducing the Tl pollution in Düzce province, Türkiye, which is the fifth-most polluted province in Europe in terms of air pollution. This study analyzed the changes in Tl concentration in the samples (wood, outer and inner bark) taken from species grown in Düzce by species, organ, direction, and age groups in the last 40 years. Results As an outcome, the uppermost Tl concentrations were found in the outer barks, and it is thought to be caused by air pollution. The outcomes achieved in the existing study revealed that the suitable species to be used in watching the Tl pollution in the air are Cupressus arizonica and Picea orientalis, whereas those to be used in reducing the Tl pollution are Pinus pinaster, Cedrus atlantica, Cupressus arizonica, and Pseudotsuga menziesii. Conclusions Cupressus arizonica is a species that can be effectively used in both monitoring and decreasing Tl pollution. Keywords: Biomonitor; Cupresus arizonica; Düzce; Heavy metal; Thallium.
... The following toxic effects in humans are reported in the literature: -Cytotoxic and allergenic effects (for Pt in particular) pp,ss,tt -Damages to lung cells pp,uu -Headaches and dizziness uu -Toxicity to skin, blood, eyes, liver, gut and brain pp,uu a (Ali and Katima, 2020b), b (Carpenter et al., 2015), c (Gwenzi et al., 2018), d (Klinger, 2018) (Kominkova et al., 2017), cc (Roy and Hardej, 2011), dd (Kazantzis, 2000), ee (Duri et al., 2020), ff (Karbowska, 2016), gg (Wang et al., 2013), hh , ii (Pavlíčková et al., 2006), jj (Jiang et al., 2020), kk (Heim et al., 2002), ll (Xiao et al., 2004), mm , nn (Rauch, S. and Morrison, G. 2008), oo (Zientek et al., 2017), pp , qq (Lenntech, 2022), rr (Ermakov and Naboichenko, 2012), ss (Lustig et al., 1996), tt , uu (Švorc et al., 2012 ...
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Thallium (Tl) is a highly toxic environmental contaminant. To understand the mechanism controlling the mobility and availability of Tl in soil, the adsorption and desorption of Tl(I) were evaluated for six soils. The maximum Tl adsorption capacities of the soils ranged from 6.9 to 244.5 mmol kg⁻¹. The corresponding Tl LIII-edge X-ray absorption near-edge structure (XANES) data revealed that illite, vermiculite, and smectite are the preferential soil constituents for adsorbing Tl(I). Tl(I) adsorption by the soils was reversible in the low Tl adsorption regime and exhibited various degrees of hysteresis as the amount of absorbed Tl increased. The Tl(I) adsorption and extent of adsorption reversibility were mainly dependent on the type and content of clay minerals and exchangeable cations in different soils. Despite high Tl(I) adsorption by the soils, the reversibility of Tl(I) adsorption may result in relatively high mobility and availability of Tl(I) in soils, leading to high environmental risk. Ignoring the reversibility of Tl adsorption could lead to an erroneous prediction of the mobility and availability of Tl in soils and a significant underestimation of the environmental risk posed by Tl in the environment.
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Eleven common vegetables (green bean, beetroot, green cabbage, lettuce, onion, pea, radish, spinach, tomato, turnip, and watercress) as well as the thallium hyperaccumulator Iberis intermedia, were grown in pot trials containing 0.7 and 3.7 mg/kg thallium added to a silt loam soil. The aims of the experiments were threefold: to estimate risks to human health of vegetables grown in thallium-rich soils, to demonstrate the potential of crops of these plants to remove thallium from polluted soils (phytoremediation), and finally to establish the degree to which part of the costs of remediation could be recouped by selling the extracted thallium (phytomining). Maximum thallium levels ranged from nearly 400 mg/kg (d.m.) in Iberis down to just over 1 mg/kg in green bean. The four vegetables with the highest thallium levels (watercress, radish, turnip and green cabbage) were all Brassicaceous plants, followed by the Chenopods beet and spinach. At a thallium concentration of 0.7 mg/kg in the soil only green bean, tomato, onion, pea and lettuce would be safe for human consumption. At 3.7 mg/kg thallium, only green bean and tomato could be eaten. The Iberis had by far the best potential for phytoremediation of thallium-contaminated land and would need 5 sequential croppings to reduce 1 mg/kg thallium to 0.1 mg/kg in the soil. By contrast rape would take 9 years and green cabbage over 30 years. Some of the costs of phytoremediation might be recouped by selling the thallium which currently has a world price of $US300/kg. It was concluded that phytoremediation of thallium-contaminated soils containing >1 mg/kg thallium will never be feasible by use of common vegetables. For soils containing 1 mg/kg thallium or less, use would have to be made of Iberis intermedia or Brassica napus(rape) rather than common vegetables.
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High thallium concentrations were found in plants and fungi growing 0.5-2 km from the flotation waste reservoir serving the Bolesław Mining and Metallurgical Works in Bukowno. Rinsed pine needles contained 2.20 ± 0. 72 mg/kg d.w. thallium, moss Pleurozium schreberi 4.89 ± 2.00, moss Catharinea sp. 12.65, lichen Cladonia sp. 2.80 ± 1.01 and edible mushrooms 3.48-4.76. Vegetables from a village (Starczynów) closest to the reservoir contained 1.28-3.70 mg/kg d.w. thallium. The inhabitants are threatened by thallium pollution. In natural conditions the element concentrations in biological samples usually do not exceed 0.0X-0.X mg/kg d.w. Only fruit samples from the studied area and all the control samples were devoid of thallium.
Conference Paper
In our study the method for the determination of Tl by ICP-MS was optimized. Both isotopes, Tl-203 and Tl-205, were used for the measurement. Lutetium at a concentration 0.4 mg L-1 was used as an internal standard. Soil extracts were measured after dilution (1+4 with the solution of lutetium 0.5 mg L-1). Several soils from the International Soil Exchange Programme (WEPAL) were analyzed for the comparison of the results. For all tested samples the achieved results were in a good agreement with the results reported by WEPAL. A detection limit 1.2 mu g kg(-1) was achieved for the samples. The method was used for the determination of thallium in soils collected in the national monitoring programme (200 sites) and in the monitoring programme of the contaminated areas (27 sites). Topsoil and subsoil were sampled on each site and analyzed separately (454 samples were analyzed). The median value for the tested soils was 0.25 mg/kg, lower and upper quartiles 0.19 and 0.32 mg kg(-1) respectively, 10(th) and 90(th) percentiles 0.16 and 0.41 mg kg(-1) respectively and the maximum value was 2.83 mg kg(-1).
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In our study the method for the determination of Tl by ICP‐MS was optimized. Both isotopes, 203Tl and 205Tl, were used for the measurement. Lutetium at a concentration 0.4 mg L‐1 was used as an internal standard. Soil extracts were measured after dilution (1+4 with the solution of lutetium 0.5 mg L‐1). Several soils from the International Soil Exchange Programme (WEPAL) were analyzed for the comparison of the results. For all tested samples the achieved results were in a good agreement with the results reported by WEPAL. A detection limit 1.2 μg kg‐1 was achieved for the samples. The method was used for the determination of thallium in soils collected in the national monitoring programme (200 sites) and in the monitoring programme of the contaminated areas (27 sites). Topsoil and subsoil were sampled on each site and analyzed separately (454 samples were analyzed). The median value for the tested soils was 0.25 mg/kg, lower and upper quartiles 0.19 and 0.32 mg kg‐1 respectively, 10th and 90th percentiles 0.16 and 0.41 mg kg‐1 respectively and the maximum value was 2.83 mg kg‐1.
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Thallium (Tl) and its compounds are toxic to all organisms. Relatively high levels of thallium of pedogeochemical origin have been found in some areas of the Czech Republic. The contents of >2 mg kg of Tl have been found in aqua regia soil extracts of soils originated from melanocratic porphyric hornblende-biotite granite or from hornblende-biotite granodiorite. The contents of Tl in the range of 0.45–1 mg kg have occurred mainly in soils originated from paragneiss. A detailed study of some of these sites has been made. Content of thallium in soils was determined after extraction with aqua regia, 2 M HNO3, DTPA-TEA and 1 M NH4NO3. Plant samples (whole rapeseed kernels) were wet ashed and the total content of Tl was determined. The amount of Tl in soils extracted by the different extracting methods in comparison to aqua regia (100%) was approximately 14% for 2 M HNO3, 0.8% for 1 M NH4NO3 and only about 0.03% for DTPA-TEA. The content of Tl in the rapeseeds was approximately 75% of this element determined in soils after extraction by aqua regia. The relationships among the extractants were found to be relatively close except for 1 M NH4NO3. It was found that the transfer of Tl into rapeseeds depends on the status of this element in the particular soil and that the soil substrate is the main factor influencing this status.
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The ICP/MS method with lutetium, bismuth and indium as internal standards was used for the determination of thallium and other elements, i.e. Ti, V, Cr, Ni, Cu, Zn, Rb, Mo, Cd, As and Pb, in soils and rapeseeds. Samples were collected in two thallium highly pedogeochemicaily contaminated areas situated in South Bohemia and in Czech-Moravian Highlands, in two river alluvia, in two control sites with low levels of TI and in one spot with anthropogenic contamination. Levels higher than 2.5 mg kg have been found in rapeseeds in the highly polluted areas (c. 2.8 mg kg in soils). High correlation coefficients, r > 0.81, between content of TI in top- and sub-soils and rapeseeds were obtained. Thallium concentrations exceed twice of Pb content and by one order of magnitude of Cd amounts. This finding are very important because of the high toxicity of TI and the absence of threshold limits for TI in soils, agricultural products and foodstuffs in the Czech Republic.
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An ion-exchange separation technique followed by analysis with atomic absorption spectroscopy was used to study the chemical forms and distribution of thallium in Lakes Michigan, Huron, and Erie. The dominant thallium form found in water samples analyzed was the oxidized Tl(III) which comprised 68 ± 6% of the total dissolved thallium, contrary to thermodynamic prediction that Tl(I) is favored in natural waters. A significant proportion of Tl(III) may be in colloidal form. No definite spatial (horizontal or vertical) pattern was found in the distribution of total dissolved thallium in the water columns of Lakes Michigan, Huron, and Erie. An overall decline of thallium concentration from Lake Michigan to Lake Erie was observed which may be related to rapid scavenging removal from the water column.
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Pot and field experiments were carried out from 1994 to 1997 to investigate Cd and Tl uptake by various genotypes of maize, spring rape and kale on soils contaminated with i) Cd by the addition of river sediments (aqua regia-extractable Cd: 24 mg kg-1 soil) and ii) with Tl by deposits from a cement plant (HNO3-extraetable Tl: 1.4 mg kg-1 soil). In field experiments on the Cd-contaminated soil, Cd concentrations in shoots and kernels of fifty maize inbred lines differed by a factor of about twenty (from < 1 to 15 mg Cd kg-1 DM in shoots and from 0.02 to 0.5 mg Cd kg-1 DM in kernels). After crossing inbred lines having high and low Cd concentration, Cd concentration of the resulting hybrids decreased, mainly as a result of a higher dry matter production (a dilution effect). In pot and field experiments on the Tl-contaminated soil, the selected cultivars of spring rape showed only small differences in Tl uptake, whereas Tl concentration in shoots of the kale cultivars differed more than twenty-fold (in the pot experiment from < 1 to 24 mg Tl kg-1 DM and in the field experiment from 0.5 to 11.7 mg Tl kg-1 shoot DM). Two groups of cultivars with low and high Tl concentrations could be distinguished. A nutrient solution experiment with radioactively labeled Tl showed that higher Tl concentration of kale in comparison to white cabbage can be attributed mainly to a higher uptake rate in kale (about 30-fold) with subsequent root-to-shoot translocation. The results show that, depending on plant species, selection and growing of cultivars with low heavy metal uptake on contaminated soils can substantially contribute to reduce the concentration of Cd and Tl in food and fodder plants.
Article
The dynamics of thallium (Tl) fractions in the rhizosphere of two Tl hyperaccumulator plants, kale (Brassica oleracea acephala L. cv. Winterbor) and candytuft (Iberis intermedia Guers.), were examined to evaluate the efficiency of their possible use in phytoextraction. Plants were grown in a rhizobox system with a soil contaminated by Tl deposits from a cement plant in Leimen, Germany (1300 g Tl kg–1 soil (aqua regia extraction) and 106 g Tl kg–1 soil NH4NO3-extractable Tl). After 6 and 8 weeks growth of kale and candytuft, respectively, Tl fractions were sequentially extracted and compared with Tl uptake by plants. The uptake from `plant-available' Tl (fraction 1 – 4) in the rhizosphere (0–2 mm distance from root compartment) of both hyperaccumulator plants kale and candytuft accounted for 18 and 21% of the Tl accumulated in their shoots, respectively. The uptake from the `non-plant available' Tl (fraction 5 – 7) accounted for 50 and 40% of the mass of Tl accumulated by kale and candytuft, respectively. The high uptake capacity for Tl and the subsequent marked depletion in the rhizosphere soil might have resulted in a rapid shift in the equilibrium between the various Tl fractions. In addition, the high depletion in the rhizosphere indicates that the transport of Tl to roots is mainly diffusion driven. In conclusion, the easy access of the so called `non-plant available' Tl fraction in the rhizosphere soil by both hyperaccumulator plants indicates a high efficacy of possible phytoremediation of Tl contaminated soils such as the soil at the site in Leimen.
Article
A Chelex-100 resin separation technique followed by analysis with atomic absorption spectroscopy was evaluated for the study of thallium speciation in river waters. The detection limit for the method was 1.0 ng/l for both Tl(I) and Tl(III). Analysis of synthetic solutions consistently yielded >90% recovery of these two thallium forms with negligible cross contamination. Water samples from selected stations in polluted Huron River and Raisin River in Michigan were analyzed. Average dissolved thallium concentrations were found to be 21 ng/l for Huron River and 26 ng/l for Raisin River. The dominant thallium form found in these rivers was oxidized Tl(III) and the proportion of Tl(III) to the total dissolved thallium ranged from 43 to 73% and averaged of 66% in water samples analyzed. A significant proportion of Tl(III) may also be in colloidal form.