comparison of the accumulation of 137cs and 90sr by six spring wheat varieties
TRANSCRIPT
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Comparison of the accumulation of 137Cs and 90Sr by Six Spring Wheat varieties
Yuri V. Putyatin1*, Taisa M. Seraya1 , Oksana M. Petrykevich1, Brenda J. Howard2
1Laboratory of Radioecology, Research Institute for Soil Science and Agrochemistry
(BRISSA), Kazintsa str. 62, 220108, Minsk, Belarus.
Email: [email protected]
Tel: 375 172 120920
Fax: 375 172 120920
2Centre for Ecology & Hydrology, Lancaster Environment Centre, Library Avenue,
Bailrigg, Lancaster LAI 4AP, United Kingdom.
Keywords: 137Cs, 90Sr, bioavailability, genotype, Triticum aestivum, productivity,
concentration ratio, countermeasures
* Corresponding author
Classification : Original paper
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Abstract The uptake of 137Cs and 90Sr by six varieties of spring wheat (Triticum
aestivum), were compared in field trials on land contaminated by the Chernobyl
accident. All the experimental varieties are officially adopted for agricultural use in
Belarus and are used in large-scale production. Under identical conditions of nutrition,
the productivity of the varieties varied significantly by 1.3 fold. The extent of 137Cs and
90Sr accumulation by wheat grain, quantified as the concentration ratio differed
significantly between varieties by 1.6 fold for both radionuclides. There was a
significant linear positive correlation between 90Sr activity concentration in grain with
that of Ca concentration. The correlation between 137Cs and potassium was significant
for grain but not for straw.
The results suggest that certain varieties of spring wheat used in normal
agricultural practice accumulate less 137Cs and 90Sr into grain than others. Some spring
wheat varieties which accumulated relatively less 137Cs did not also accumulate the
lowest content of 90Sr. Thus, selection of the most suitable variety for cultivation needs
to take into account not only its accumulation of both 137Cs and 90Sr but also the relative
density of soil contamination by both 137Cs and 90Sr of soil in each area. However, one
variety, Quattro, had the lowest uptake of both 90Cs and 137Cs, with Manu consistently
the second lowest uptake for both radionuclides. The reduction efficiency achieved by
the use of these varieties is not as high as that achieved by soil amelioration techniques
in the past. Nevertheless, since there are no additional costs or production losses
associated with these varieties, their use in the contaminated areas is recommended as a
simple, practical and effective contribution to reducing the uptake of both 90Sr and 137Cs
and allowing farmers to produce food-grade grain.
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Introduction
After the Chernobyl accident, 137Cs and 90Sr have both been of mid-long term
environmental concern due to their long physical half-lives and relatively high
environmental mobility compared to the other long lived radionuclides released.
Agricultural production in Belarus is currently conducted on 1.3 million hectares of land
contaminated by 137Cs at deposition levels varying between 37-1480 kBq m-2. Some of
this land (0.46 million hectares) is also contaminated by 90Sr at deposition levels
varying between 6-111 kBq m-2.
Plant uptake of 137Cs or 90Sr from soil is an important pathway for their entry into
the human food chain and substantially contributes to internal radiation dose following
contamination. Because of the persistent uptake of 137Cs and 90Sr by crops and animals,
there is potential long term exposure to people via the foodchain. For crop plants, the
contamination route may be direct through the ingestion of edible crops, or indirect
through the use of crops as animal feedingstuffs.
In the last nearly two decades there has been a significant amount of effort
devoted to the development of a large range of different countermeasures to reduce the
uptake of radiocaesium into crops, with some effort also devoted to radiostrontium
(Howard and Desmet 1993; Howard et al 2004; Howard et al in press). These
countermeasures largely focus on various treatments of the soil to reduce root uptake.
Because some plant species have a relatively low ability to accumulate radionuclides
one countermeasure approach has been to select crop species with comparatively low
uptake of the contaminant radionuclide (Makarevitch 1973; Korneyeva 1974; Moiseev
et al 1977; Malikov et al 1981; Smolders et al 1993; Krouglov et al 1997; Bogdevitch et
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al 2001a; Bogdevitch et al 2003b; Vasiluk et al 2001; Buysse et al 1996). Differences in
productivity, the extent of the vegetative period and the mineral nutrition characteristics
of species each influence the extent of radionuclide accumulation both between and
within different plant species (Zhu et al 2000; Tsialtas et al 2003; Waegeneers et al 2001;
Twinning et al 2004; Zheleznov et al 2002). Conversely, the ability of certain plant
species to take up a relatively large amount of certain radionuclides has led to the
suggestion that these species could be used for phytoremediation of contaminated land
(Entry and Watrud 1988; Fuhrmann et al 2002). These approaches has been used in
Belarus, where the cultivation of rapeseed (Brassica napus f.) on contaminated lands
produces safe, edible oil whilst simultaneously decontaminating soil (Bogdevitch et al
2001b; Bogdevitch et al 2001c).
There are relatively few data considering intraspecies variation, compared to that
for interspecies differences in uptake. The selection of different crop varieties has
previously been suggested as a countermeasure in international fora (Alexakhin 1993;
Prister 1992; IAEA 1994). Although Green et al (1996) reported 3-4 fold variation in
uptake of a limited range of varieties they also found a similar variation for the same
variety of crop between years and concluded that (i) the implementation of such a
countermeasure should be based on a comprehensive dataset in which the inherent
variability in transfer factors has been assessed and (ii) combining data from separate
experiments could lead to erroneous conclusions. In a recently produced
countermeasure compendium, variety selection as a countermeasure was not included as
it was felt that there was currently inadequate information to proceed to a consideration
of their potential practical implication (STRATEGY 2003, http://www.strategy-
ec.org.uk). However, the evaluation recommended that the inclusion of this
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countermeasure should be reviewed if there is any future development and testing of
these countermeasures.
Widespread agrochemical countermeasures applied after the Chernobyl accident
in Belarus, Russia and Ukraine on contaminated agricultural lands have changed the soil
agrochemical properties and decreased radionuclide transfer coefficients from soil to
plants (eg. Putyatin et al 2001; Vasiluk et al 2001). At the present time, most of the
treated soils have higher pH and mobile potassium values than was previously the case.
Because of this, the potential efficiency of further soil amelioration protective measures
used in plant production such as liming and higher rate of potassium fertilization are
reduced.
The climatic and soil conditions of the most highly contaminated southern areas
of Belarus are most suitable for cultivation of wheat to produce food-grade grain. More
than 50% of the contaminated arable lands in Belarus are cultivated with cereals.
Permitted levels (PL) currently in force in Belarus (Bogdevitch et al 2003b; RDU-99
1999) are low compared with international limits and those in force in the EC for future
accidents (CEC 1989). The permitted levels for 90Sr are especially low, at 11 Bq kg-1
for food-grade grain and 3.7 Bq kg-1 for bread, whilst for 137Cs the respective PL values
are higher at 90 and 40 Bq kg-1. Given these low PL values, without countermeasure
application the current contamination levels in many areas led to wheat containing
radiocaesium and radiostrontium above the PL values. Soil contamination of just 11
kBq m-2 of 90Sr leads to problems in producing wheat below the PL values and about
190 000 hectare of agricultural lands are contaminated by 90Sr higher than 11 kBq m-2
producing 17 000 - 30 000 tonnes per year of grain with 90Sr contents exceeding the PL.
As a consequence, a significant proportion of the crop can only be used as forage or
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processed, but cannot be sold as food-grade grain which has a higher monetary value for
local farmers. Therefore, it is important to identify additional countermeasures
techniques to reduce the levels of contamination of cereals to enable production of food-
grade grain. Alongside the agrochemical countermeasures already used, there is
potential to further reduce 137Cs and 90Sr accumulation in cereals if we can identify crop
rotation varieties with a relatively low uptake of these two radionuclides.
The aim of this study was to compare the uptake of 137Cs and 90Sr by different
officially adopted varieties of spring wheat to try to identify varieties with low uptake
rates. The study was conducted on a Podzoluvisol loamy sand soil which is a
widespread, representative soil in the affected region (46% of arable lands). The
ultimate goal was to provide an effective additional countermeasure to minimize the
flux of 137Cs and 90Sr into the food chain.
Materials and Methods
Field experiment
In a two-year field experiment (2002-2003), six varieties of spring wheat (Triticum
aestivum) from different countries of origin were studied: Rostan (Belarus), Quattro
(Germany), Manu (Finland), Banty (Poland), Daria (Belarus) and Munk (Germany).
The preceding crop in the normal crop rotation scheme is red clover. The standard
spring wheat variety used in Belarus is Rostan, but each of the other varieties are
adopted as suitable for cultivation in Belarus. The concept of a “standard variety” is
used by the State Seed Committee to compare productivity of adopted varieties and
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every potential new variety with respect to crop yield and quality. If the crop yields of a
new variety is lower than the “standard variety” the new variety will not be adopted.
The experiment was conducted in the Gomel region of Belarus. The surface soil
layer (0-25 cm) of the Podzoluvisol loamy sand soil was characterized by a low content
(14%) of fine fraction particles (< 0.01mm). The agrochemical parameters of the soil
�������������� ����KCl ��������������2�5 197 mg kg-1��������������������������2��
288 mg kg-1 dw, exchangeable Ca 820 mg kg-1 dw and exchangeable Mg 122 mg kg-1
dw. Radionuclide deposition (mean±SD) in soil of 137Cs was 320 ± 19.0 kBq m-2 and
90Sr was 30 ± 4.8 kBq m-2.
Seeds of each of the six varieties were sown in experimental plot areas of 4 m2
and 1 m2 in mid April in both 2002 and 2003. Four replicates was used in a randomized
block design. Fertilizers were applied to the soil before sowing at a rate per m2 of : urea
– 7 g, superphosphate – 7 g �2�5 and potassium chloride – 12 g K2�. Plant samples
were harvested at full maturity (grain and straw) 105 days after germination.
Soil and plant analysis
The following physicochemical parameters were measured in the soil samples using
conventional methods (Sokolov 1975) briefly as follows:
• pH: was determined with a glass electrode in an aqueous suspension of 10 g
of dry soil and 25 ml of 1 N KCl, shaken and left for deposition overnight.
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• Organic matter: was measured using 0.1 N iron ammonium sulphate titration
with diphenylamine, after combustion of 1 g soil in 0.4 N chromic acid for 5
minutes.
• Mobile P2O5 and K2O: were determined by extraction in 0.2 N HCl in a
ratio1:5, followed by determination using calorimetric and flame emission
spectrophotometer (FES) methods respectively.
• Exchangeable Ca and Mg: were determined by extraction in 1 N KCl in a
ratio 1:2.5, followed by determination using Atomic Absorption
Spectroscopy (AAS).
For the plant samples, potassium was determined by FES and calcium by AAS
after wet combustion with concentrated sulphuric acid and hydrogen peroxide.
Radioactivity measurements
Cs-137 activity concentration: Plant and soil samples were homogenized, dried at
room temperature and put into Marinelli beakers (1.0 l) and measured using gamma
spectrometry (HP-Ge detector Canberra GC4019 in a low-background environment).
The relative uncertainty of 137Cs activity measurement in all samples was < 10%.
Results were calculated for each soil sample both as Bq kg-1 and as kBq m-2, using the
bulk density of soil of 1.50 g cm-3 and plough layer 25 cm.
Sr-90 activity concentration: Plant and soil samples were ashed at 6000C. The 90Sr
activity concentration was determined using the oxalate method with separation of 90Y
(Cherenkov counting). Beta activity was measured in a low level liquid scintillation
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counter (CANBERRA Tri-Carb 2750LL). Results were calculated for each soil sample
both as Bq kg-1 and as kBq m-2, using the bulk density of soil of 1.50 g cm-3 and a
plough layer of 25 cm.
Data treatment
For radionuclides, it is generally assumed that the activity concentration of a
radionuclide in a plant or plant part, Cp (Bq kg-1, plant dw), is linearly related to its
concentration in the plough-layer of soil, Cs (Bq kg-1dw), i.e.
Cp = CR Cs. (1) The soil-to-plant concentration ratio CR in Eq. (1), (or transfer factor) was determined
as:
CR = soil) ofdw kgper (Bq soil oflayer plough in nuclide of ionconcentratactivity
plant) ofdw kgper (Bqplant in nuclide of ionconcentratactivity (2)
Conventional regression and multivariate statistical analysis for the obtained data
was carried out using the STATISTICA Program, StatSoft Inc. (2001).
Results
Productivity
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The productivity of the different varieties at final harvest is shown in Figure 1. The
highest grain productivity was found for the Banty and Munk varieties for which the
significantly enhanced yield was 22 % and 13 % (p<0.05) above that of the standard
Rostan variety according to the variance LSD test (Duncan test). The yield of the
Quattro and Manu varieties was similar to that of Rostan, whereas the Daria variety had
a significantly (p<0.05) lower yield than Rostan by 9%. The yield of straw varied from
0.48 up to 0.66 kg m-2 and was highest for the Quattro variety. The lowest ratio of straw
dry matter to grain was found for the Munk variety (0.92), and the highest for the Daria
variety (1.48).
Insert Figure 1.
Radionuclide uptake
The uptake by the Spring wheat varieties (Figure 2) of 137Cs into grain declined in the
following order:
Daria > Rostan > Banty > Munk > Manu > Quattro
and for 90Sr as follows:
Munk > Daria > Banty > Rostan > Manu > Quattro.
The varieties which accumulated least 137Cs were not always those which
accumulated the least 90Sr. The Quattro variety (which had the lowest uptake into grain)
accumulated 137Cs in grain significantly 1.6 fold less than that of the variety with the
highest uptake, Daria. There was a similar significant 1.6 fold difference between the
lowest (Quattro) and highest (Munk) accumulator of 90Sr.
Insert Figure 2. Insert Figure 3.
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Changes in radionuclide accumulation by wheat grain in our experiment cannot
be explained by diferences in crop yield (and associated dilution). The Quattro variety
accumulated least 137Cs and 90Sr. However, the Daria variety accumulating 60% more
137Cs (Bq kg-1 dw basis) than Quattro but had a productivity only 12% lower than
Quattro. On a similar comparison basis, the Munk Variety accumulating 57% more 90Sr
than Quattro with only a 24% higher productivity.
Clearly, the above data for plant contamination are not directly comparable due to
the varying extent of soil contamination. This difference is removed when considering
the CR values shown in Table 1. The CR values for 137Cs were similar for the Manu,
Banty and Munk varieties and for 90Sr for the Rostan, Quattro and Manu varieties. CR
values for 137Cs in straw were higher than those of grain by an average of 4.5 fold with
variation between varieties of 0.051-0.066, 90Sr CR values for straw were an average of
10 fold higher than grain with variation between varieties of 3.12-4.12.
Insert Table 1. The chemical analysis data shows that higher 134Cs or 90Sr uptake was found for
varieties that accumulated more of their close respective analogues, K and Ca (Figures 4
and 5). The 90Sr activity concentration in both grain and straw was significantly and
positively linearly correlated with Ca concentration (R2 = 0.67 and 0.61 respectively).
The correlation between 137Cs activity concentration and potassium concentration in
grain was significant but lower (R2 = 0.44) than that for 90Sr and Ca, and there was no
significant relationship between 137Cs and potassium in straw (R2 = 0.17).
Insert Figure 4. Insert Figure 5.
The total flux of radionuclide into the wheat has been quantified as the total Bq in
wheat per unit deposition (ie Bq kg-1 dw x kg m-2). The lowest total 137Cs and 90Sr
accumulation in grain per unit area was achieved by the Quattro variety (Table 2). This
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variety had the lowest proportion of the radionuclides accumulated in the edible part
(grain) compared with the total accumulation by grain and straw. The variety with the
lowest accumulation also had the lowest proportion (%) in the edible part (the grain)
compared to the other varieties and therefore the lowest flux into the foodchain.
Insert Table 2. Calculation of the Tag value (ie Bq kg-1 dw divided by kBq m2) is a commonly
used method to compare Cs uptake based on total deposition rather than a soil
concentration. Values for Tag for the experiment are given in Table 3 to enable later
comparison with literature, especially that from the former Soviet Union where Tag
values are commonly reported.
Insert Table 3.
Discussion
Quantification of transfer to wheat
The CR values measured in our experiment can be compared to other data on 137Cs and
90Sr uptake by cereals from various soil types reviewed by Nisbet and Woodman (2000)
and given in Table 4. The CR values for Cs and grain for our loamy sand soil varied
from 0.01 to 0.016 which were similar to the recommended values for clay and loam of
Nisbet and Woodman (2000). For Sr, the CR range we measured of 0.284 – 0.446 was
slightly higher than the highest recommended values for sand and loam of Nisbet and
Woodman (2000) but well within the 95% confidence intervals. This agreement is
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perhaps a little surprising given that our deposits are nearly 20 years old and we might
have expected values which were lower than those recommended.
Insert Table 4
Bogdevitch et al (2003a) reported significant variability in 137Cs CR data of spring
wheat grown on sod-podzolic loamy sand soil in 1995 depending on the rates of
potassium fertilizers. Without fertilizers application the CR was 0.009, the CR value
decreased with increasing amounts of fertiliser application (N70P60 - 0.008; N70P60K80 -
0.008; N70P60K160 - 0.006 and N70P60K240 - 0.005).
In the long-term study started in 1987 by Krouglov et al (1997), an initially
observed low 90Sr CR value was measured due to its association with fuel particles,
which subsequently increased with time as the particles dissolved. In the later years of
their observations (1993-1994), when fuel particle dissolution was well established,
their CR values for grain of winter wheat grown on sod-podzolic soils were roughly 12-
15 from straw and 2-3 for grain for 90Sr and less than 1 for both sample types for 137Cs
(values taken from a figure). The 90Sr CR values are higher than those reported here for
a similar soil type (and higher than the 95% confidence intervals reported by Nisbet and
Woodman 2000), possibly because of the gradual release of Sr from the fuel particles
and therefore high transient bioavailability and/or the earlier time period of their
sampling (almost a decade before our experiments).
Tag values for 137Cs and 90Sr for spring wheat grain grown on sod-podzolic loamy
sandy soils collected in 1998-2002 (Bogdevitch et al 2003b), and therefore comparable
to our long term data, were similar to the data reported here. The data of Bogdevitch et
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al (2003b) were for a mixture of spring wheat varieties grown on Podzoluvisol loamy
sand soils; the 137Cs Tag values for grain were 0.02-0.04 m2 kg-1 x 10-3 depending on
exchangeable potassium (range 140-300 ppm �2�����������90Sr they were 1.13-1.62 m2
kg-1 x 10-3 depending on soil acidity (range 5.1-7.0 pHKCl). The equivalent Tag values
for 90Sr were 20-50 fold higher than 137Cs (Bogdevitch et al 2003b) whereas for our
grain the difference was 21-34 fold. Our Tag values for straw were 47.3 – 75.3 fold
higher for 90Sr compared with 137Cs.
Drobyshevskaya et al (2001) reported significant variability in 90Sr Tag values of
grain of spring wheat grown on Podzoluvisol loamy sand soils depending on the year of
the study with a mean Tag value (m2 kg-1 x 10-3 ) of 0.39: 1997-0.61; 1998 – 0.26;
1999 – 0.48; 2000 – 0.23. There was a general trend of a decline in transfer but not
consistently each year.
In our study, grain and straw 90Sr activity concentrations were linearly positively
correlated with Ca concentration. There was also a correlation between 137Cs and
potassium in grain although it was less strong than that of 90Sr, which is expected due to
potassium regulation by the plants. The relationship between Ca and Sr and of K and
Cs has been reported in the radioecological literature for many different plant species
Increased potassium or calcium concentrations in soil generally (but not always)
decrease the plant uptake of Cs or Sr respectively, often by competitive inhibition by
these analogous essential elements (Shirshov & Shain 1971; Moiseev et al 1977;
Judintseva et al 1981; Malikov et al 1981; Alexakhin & Krouglov 2001; Ehlken and
Kirchner 2002). Furthermore, our results are consistent with other data for wheat, such
as the observed greater influx of radiocaesium when there was a deficiency in soil
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potassium (Zhu et al 2000) and higher radiocaesium uptake occurred in plant species that
deplete K in the rhizosphere to a larger extent.
Variation in transfer with variety
Alexakhin (1993) and Prister (1992) provided some of the first review comparisons of
the reduction efficiency in radiocaesium uptake by using different varieties of crops.
Alexakhin (1993) reported reduction efficiencies varying from 1.4 to 4.5 for 15 different
varieties of spring wheat thus varying by 3.1 fold (with CR values ranging from 0.015-
0.046 for the period up to 1991). Similarly, Prister (1992) reported a 2.5 fold variation
in transfer for six varieties of spring wheat, with Tag values for grain varying from 0.56
– 1.4 m2 kg-1 x 10-3, and commented that “the selection of specific plant species
matched to specific soil properties and the corresponding levels of contamination, is one
of the most efficient measures for reducing the concentration of radionuclides in
agricultural products”. In the field experiments reported here, under identical conditions
of plant nutrition, the uptake of both 137Cs and 90Sr varied significantly with the
different varieties of spring wheat used.
The maximum difference in concentration ratios for both 137Cs and 90Sr between
varieties was less than that reported by Alexakhin (1993) and Prister (1992) at 1.6 fold.
Some spring wheat varieties which accumulated relatively less 137Cs did not also
accumulate the lowest content of 90Sr. Thus, selection of the most suitable variety for
cultivation needs to take into account not only its ability to uptake both 137Cs and 90Sr
but also the density of soil contamination by both 137Cs and 90Sr of soil in each
cultivated area.
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The most directly comparable data on variation in uptake with variety is the data
on uptake of 137Cs by winter wheat cultivars reported by Schimmack et al (2004). In a
comprehensive study, they compared the field uptake of 137Cs by grain in 28 different
wheat cultivars at three different sites with different soil types (silty and clayey loams)
in Germany in 1999. Certain cultivars, Flair, Kornett and Previa, had lower 137Cs
uptake compared to the mean of all cultivars at each site. On average, the 137Cs activity
in wheat grains of these cultivars at the three sites was reduced by a factor of 1.7
compared to the cultivar with the highest uptake, whereas at one site this factor was as
high as 3.1 (1.5 and 2.2 at the other 2 sites). The mean CR value for grain also varied
by up to a factor of three both between cultivars within sites and between sites for a
single cultivar. The mean CR values at the three sites were 4.2 x 10-4, 4.9 x 10-4 and 7.5
x 10-4 (ranging from 2.6 x 10-4 to 8.8 x 10-4), showing the importance of soil type, with
no single cultivar showing similar values at all sites. The reported CR values were at the
lower end of the range reported in the review of Nisbet et al (2000) for loamy soils for
wheat grain and are generally at least an order of magnitude lower than those measured
in the Podzoluvisol loamy sand soil in the experiment in Belarus.
The lack of replication at sites for cultivars and the low 137Cs activity
concentrations in the German experiment made statistical analysis of the data somewhat
difficult. The authors noted that there was a need to determine whether the differences
noted between cultivars were due to genotype effects or to intracultivar variation in root
uptake due to different soil conditions. Although not definitively proving the former,
our experiment in Belarus lends weight to the possible genetic basis for the observed
differences, but has not addressed the effect of varying soil type.
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There have been other experiments reporting variation in uptake of radionuclides
by different varieties of the same crop, some of which are only published in the Russian
language literature. In investigations on different crops grown on leached chernozem
soil, differences in 90Sr uptake by 10 varieties of winter wheat were recorded of up to 2
fold, by 5 varieties of winter barley up to 1.4 fold and by 13 varieties of corn up to 2.5
fold (Malikov et al 1981). For 137Cs accumulation in winter wheat, winter barley and
corn the differences were up to 1.9, 2.5, 3.2 fold respectively and there was no
systematic variation in the uptake of Cs and Sr.
In a separate study by Bogdevitch et al (2001b; 2001c) 32 varieties of spring
rapeseed were compared for their ability to accumulate 137Cs and 90Sr in field trials.
Under identical conditions of nutrition, the differences in 137Cs and 90Sr accumulation
between varieties was greater than that reported here at 2.7 and 4 fold respectively. In
contrast, the uptake of 137Cs and 90Sr by three varieties of soybean grown under
identical field conditions on sod-podzolic loamy sandy soil during a two-year period
(1996-1997) was not significantly different. The lack of difference may have been due
to the close genotypic link between the soybean varieties used in the experiment which
were also from the same country of origin (Vedeneeva et al 2000).
In pot experiments, Shirshov and Shain (1971) reported a maximal 3.9 fold
difference in 90Sr accumulation by 14 varieties of fodder beans; and a 2.1 fold
difference in 2 varieties of pea. For the pea varieties, there was a 1.8 fold difference in
137Cs uptake. The pea variety which accumulated the lowest amount of 90Sr
accumulated the higher amount of 137Cs and vice versa. In these experiments, the
coefficients of variation in radionuclide accumulation by parental forms of plants were
much lower than those of cross-bred plants (Shirshov and Shain 1971).
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In addition to the above there is other evidence in the literature that both Sr
(Rasmusson et al 1963, 1964, 1967; Smith et al 1963; Pinkas et al 1966; Kleese 1968)
and Cs (Øhlenschlæger et al 1991, 1993) uptake are under genetic control. Current
genetically based investigations on gene control of uptake (eg. Payne et al 2004) and of
molecular mechanisms of Cs uptake by plants (White et al 2003) suggest that it may be
possible in future to select for genotypes with either a low uptake of radionuclides or a
high uptake to facilitate phytoremediation.
Conclusion
The results presented here suggest that selection of certain varieties of spring
wheat accumulate less 137Cs and 90Sr into grain than other officially adopted varieties
used in normal agricultural practice. However, one variety, Quattro, had the lowest
uptake of both 90Cs and 137Cs, with Manu consistently the second lowest uptake for both
radionuclides. The reduction efficiency achieved by the use of these varieties is not as
high as that achieved by soil amelioration techniques in the past. Nevertheless, since
there are no additional costs or production losses associated with these varieties, their
use in the contaminated areas is recommended as a simple and effective additional
contribution to reducing the uptake of both 90Sr and 137Cs. It is particularly important to
introduce varieties with minimal accumulation of 137Cs and 90Sr on farmland as an
additional countermeasure where it is now not possible to achieve further significant
reductions using traditional countermeasures such as liming and potassium fertilizers
alone. For farmers in contaminated areas, it is important to be able to grow food-grade
grain under the relevant PL values to maximize their income.
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Our results, together with other relevant literature suggest that transfer can vary
with different genotypes of the same species to a sufficient extent to make variation in
crop variety a credible countermeasure. In spite of the fact that differences in
radionuclides uptake amongst some varieties are much less than those between species,
there is some benefit to be gained at no additional cost or inconvenience from selecting
varieties with minimum ability of radionuclide accumulation for cultivation on
contaminated soils.
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28
Table 1 Concentration ratio (CR) of 137Cs or 90Sr of spring wheat varieties (mean ±SD)
CR 137Cs 90Sr
Variety
Grain Straw Grain Straw Rostan 0.015 ±0.0013 0.062 ±0.0044 0.324 ±0.0311 3.16 ±0.2652 Quattro 0.010 ±0.0011 0.051 ±0.0055 0.284 ±0.0307 3.62 ±0.2604 Manu 0.012 ±0.0012 0.066 ±0.0040 0.304 ±0.0292 3.12 ±0.2616 Banty 0.013 ±0.0012 0.061 ±0.0044 0.375 ±0.0316 3.58 ±0.2580 Daria 0.016 ±0.0013 0.064 ±0.0046 0.395 ±0.0332 3.74 ±0.2688 Munk 0.013 ±0.0011 0.055 ±0.0053 0.446 ±0.0374 4.12 ±0.2964
29
Table 2 Total 137Cs and 90Sr flux per unit area into grain and straw by different spring
wheat varieties
137Cs accumulation, Bq m-2 90Sr accumulation, Bq m-2 Variety Grain Straw Total Edible part
% Grain Straw Total Edible part
% Rostan 6 28 34 18 12 134 146 8 Quattro 4 29 33 13 11 191 202 5 Manu 5 28 33 15 12 125 137 9 Banty 6 31 37 17 17 169 186 9 Daria 6 34 40 15 13 185 199 7 Munk 6 22 28 21 19 158 177 10
30
Table 3 Tag values (m2 kg-1 x 10-3) for 137Cs and 90Sr flux into grain and straw by
different spring wheat varieties (mean ± SD)
Tag value (m2 kg-1) 137Cs 90Sr
Variety
Grain Straw Grain Straw Rostan 0.041 ±0.0034 0.165 ±0.0119 0.86 ±0.086 8.43 ±0.767 Quattro 0.027 ±0.0029 0.135 ±0.0146 0.76 ±0.085 9.65 ±0.753 Manu 0.032 ±0.0031 0.176 ±0.0105 0.81 ±0.081 8.32 ±0.758 Banty 0.035 ±0.0034 0.162 ±0.0117 1.00 ±0.088 9.54 ±0.744 Daria 0.043 ±0.0036 0.170 ±0.0123 1.05 ±0.092 9.97 ±0.778 Munk 0.035 ±0.0030 0.146 ±0.0140 1.19 ±0.104 11.00 ±0.858
31
Table 4 Recommended CR values for radiocaesium and radiostrontium transfer to
edible crop parts for cereals with 95% confidence intervals (Nisbet and Woodman 2000)
Soil type n CR value (Bq kg-1 dw per Bq kg-1 dw soil)
Recommended value 95% Confidence intervals Radiocaesium Sand 208 0.021 0.0017 0.25 Loam 358 0.014 0.00045 0.42 Clay 49 0.011 0.00057 0.21 Organic 54 0.043 0.0038 0.49 Radiostrontium Sand 112 0.23 0.03 1.7 Loam 88 0.15 0.022 0.94 Clay 21 0.071 0.022 0.23 Organic 7 0.03 0.0074 0.12
32
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
Rostan Quattro Manu Banty Daria Munk
Variety
Yie
ld, d
w (
kg m
-2)
grain straw
Fig. 1 Putyatin
33
0.0
10.0
20.0
30.0
40.0
50.0
60.0
70.0
Rostan Quattro Manu Banty Daria Munk
Variety
137 C
s, B
q kg
-1, d
wGrain Straw
Fig. 2 Putyatin
34
0.0
50.0
100.0
150.0
200.0
250.0
300.0
350.0
400.0
Rostan Quattro Manu Banty Daria Munk
Variety
90Sr
, Bq
kg-1
, dw
Grain Straw
Fig. 3 Putyatin
35
10.0
60.0
110.0
160.0
210.0
260.0
310.0
Rostan Quattro Manu Banty Daria Munk Variety
90S
r, B
q kg
-1, d
w
0
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
Ca,
%,
dw
�������� ��������� 90Sr in grain 90Sr in straw
Fig. 4 Putyatin
36
0.0
10.0
20.0
30.0
40.0
50.0
60.0
Rostan Quattro Manu Banty Daria Munk Variety
0
0.5
1
1.5
2
2.5
3
K2O
, %, d
w
�2������� �2�������� 137Cs in grain 137Cs in straw
137 C
s, B
q kg
-1, d
w
Fig. 5 Putyatin
37
Figure legends: Fig. 1 Variation in the productivity of the six spring wheat varieties (mean ± LSD05) Fig. 2 137Cs activity concentrations of the six spring wheat varieties (mean field soil deposition was 320 kBq m-2 of 137Cs ) (mean ± LSD05) Fig. 3 90Sr activity concentrations of the six spring wheat varieties (mean field soil deposition was 30 kBq m-2 of 90Sr ) (mean ± LSD05) Fig. 4 Comparison between calcium (%, mean ± LSD05) and 90Sr (Bq kg-1) content in grain and straw of spring wheat varieties Fig. 5 Comparison between potassium (%, mean ± LSD05) and 137Cs (Bq kg-1) content in grain and straw of spring wheat varieties