Radionuclides Transfer from Soil to Tea Leaves and Estimation of Committed Effective Dose to the Bangladesh Populace

Considering the probable health risks due to radioactivity input via drinking tea, the concentrations of 226Ra, 232Th,40K and 137Cs radionuclides in the soil and the corresponding tea leaves of a large tea plantation were measured using high purity germanium (HPGe) γ-ray spectrometry. Different layers of soil and fresh tea leaf samples were collected from the Udalia Tea Estate (UTE) in the Fatickchari area of Chittagong, Bangladesh. The mean concentrations (in Bq/kg) of radionuclides in the studied soil samples were found to be 34 ± 9 to 45 ± 3 for 226Ra, 50 ± 13 to 63 ± 5 for 232Th, 245 ± 30 to 635 ± 35 for 40K and 3 ± 1 to 10 ± 1 for 137Cs, while the respective values in the corresponding tea leaf samples were 3.6 ± 0.7 to 5.7 ± 1.0, 2.4 ± 0.5 to 5.8 ± 0.9, 132 ± 25 to 258 ± 29 and <0.4. The mean transfer factors for 226Ra, 232Th and 40K from soil to tea leaves were calculated to be 0.12, 0.08 and 0.46, respectively, the complete range being 1.1 × 10−2 to 1.0, in accordance with IAEA values. Additionally, the most popularly consumed tea brands available in the Bangladeshi market were also analyzed and, with the exception of 40K, were found to have similar concentrations to the fresh tea leaves collected from the UTE. The committed effective dose via the consumption of tea was estimated to be low in comparison with the United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) reference ingestion dose limit of 290 μSv/y. Current indicative tea consumption of 4 g/day/person shows an insignificant radiological risk to public health, while cumulative dietary exposures may not be entirely negligible, because the UNSCEAR reference dose limit is derived from total dietary exposures. This study suggests a periodic monitoring of radiation levels in tea leaves in seeking to ensure the safety of human health.


Introduction
The most common forms of ionizing radiation on earth, resulting from terrestrial, extraterrestrial and anthropogenic sources, are αand β-particles and γ-rays [1,2]. According to the National Council on Radiation Protection and Measurements (NCRP), environmental radiation is the most significant source of radiation exposure to humans [3]. Interestingly, although the International Atomic Energy Agency (IAEA) reported that the public exposure from natural radiation is of little health concern [4], the World Nuclear Association (WNA) states that any dose of radiation involves a possible risk to human health [5]. Since 238 U and 232 Th decay series and singly occurring 40 K are the most abundant radionuclides found naturally in soil, air, water, rocks, plants and foodstuffs [5], to protect the public against unwanted exposures to natural radiation, the radioactivity in environmental samples, including foodstuffs, needs to be monitored periodically [4].
The surface soil, especially the top layer in the earth, is a mixture of various components in the natural environment [6,7]. Although the main source of U, Th and K is the earth crust, their contents appear at varying levels in the soils of different regions in the world following the variation of the local geology [8]. In addition to the prevailing concentration of terrestrial radionuclides in acidic soils, at high altitudes the contribution from extraterrestrial radioactivity may be enhanced, moreover with fallout of artificial radionuclides that may be subject to greater deposition. The latter concerns atmospheric nuclear device has come to be ranked highly among the existing tea estates in Bangladesh. In meeting the growing domestic demand for premium black and green tea as well as that of international markets, UTE has secured a position not only as a tea producer but also as a multi-product estate. In particular, it enjoys abundant rainfall, is in an area of elevated altitude above sea level and has acidic and well-draining soils, all combining to make favorable conditions for tea production.
Since plants produce their necessary energy via the use of leaves together with the photosynthesis process, the leaves may have more activity than the other parts of plants, therefore they may contain relatively more radionuclides which are normally taken up by the root system along with other minerals. Moreover, leaves are more exposed to aerial deposition, e.g., radionuclides in dust or radionuclide particles themselves, if there are any artificial phenomena in the surrounding environment or nearby countries. Therefore, tea plants may be subjected to direct and indirect contamination of various radionuclides, and these radionuclides can be distributed in different parts of the plants according to the chemical characteristics and parameters of the plants and soil [33]. Since tea forms the second most popular drink (after water) in all populations in Bangladesh, the presence of a low level of radioactive material in tea leaves may produce a non-negligible health hazard via cumulative exposures. By acknowledging that ingestion doses above permissible levels are harmful for human beings [34], assessment of radionuclides due to the consumption of foodstuffs is important for public health. Furthermore, assessment of any release of radioactivity to the environment is important for the protection of public health, especially if the released radioactivity can enter into the food chain [35].
While studies of natural radioactivity in various foodstuffs are available in the literature, information on the distribution and enrichment of radionuclides in tea leaves is sparse, especially in tea leaves collected from the major tea gardens including the UTE in Bangladesh. The main objectives of the present study are to determine the transfer of radionuclides from soil to tea leaves harvested from the Udalia Tea Estate, further calculating the associated health hazards following the consumption of tea by the populace in Bangladesh. The activity concentrations of marketed tea leaves were also analyzed to observe the effect of manufacturing processes. This study may also help to enrich the radioactivity database on tea, i.e., the most popular stimulating drink.

Local Geology of the Udalia Tea Estate
The Udalia Tea Estate (UTE) is located in the hilly region of Fatickchari Upazilla in the Chittagong district of Bangladesh (see in Figure 1). The UTE can be addressed as latitude 22 • 36 39 -22 • 39 41 N and longitude 91 • 45 6 -91 • 51 15 E. The estate is covered by low hill ranges and terraces having an altitude of 30-46 m above sea level and contains an area of 3096 acres (3.9 km × 3.2 km = 12.5 square kilometer) [36]. The climate of this area is tropical monsoon. An average annual rainfall of about 2794 mm is recorded in this area, while July is the wettest month. The soils in this area are mainly yellowish to reddish brown, the texture is mostly clay loam on flat land while the hilly soil is mostly sandy loam to coarse sand, which is characterized by broken shale or sandstone and mottled sand at different depths [37]. The soils are strongly acidic and poor in organic matter and nutrients.

Sample Collection and Preparation
The samples (soil and tea leaves) were collected from different places in the Udalia Tea Estate (UTE). The sampling location was chosen on a random basis, but the distance between each sampling location was almost 700-800 m. Since the estate consists of ranges of low lying hills, separate hills were chosen as different sampling locations. A total of 5 locations were chosen for collecting the tea leaves and the surrounding soil samples throughout the garden. While an approximate amount of 2.5 kg of fresh tea leaf samples were collected from each selected location around the UTE, a total of 4 (×3) soil samples were also collected from three different depths, 0 to 5 cm, 6 to 12 cm and 13 to 20 cm, of the corresponding locations to the tea leaves samples. More specifically, the soil samples were collected from four different points within an area of 1 m 2 around the tea tree. The 25-year-old tea trees were selected for collection of the tea leaf samples. Usually, the branches of the tea plant are cut and are fertilized twice per year, and in some cases fertilizers are used more than twice for influencing the growth of the tea plant in the garden. At present, the UTE produces approximately 0.7 million tons of tea per year with six separate grades of tea including the export quality one. In the local market and throughout the country, this estate supplies one of the popular tea brands "Mostafa tea". Five marketed tea leaf samples were also collected from the local market, allowing comparison of the measured radioactivity from these with that from the fresh tea leaves collected from the UTE.

Sample Collection and Preparation
The samples (soil and tea leaves) were collected from different places in the Udalia Tea Estate (UTE). The sampling location was chosen on a random basis, but the distance between each sampling location was almost 700-800 m. Since the estate consists of ranges of low lying hills, separate hills were chosen as different sampling locations. A total of 5 locations were chosen for collecting the tea leaves and the surrounding soil samples throughout the garden. While an approximate amount of 2.5 kg of fresh tea leaf samples were collected from each selected location around the UTE, a total of 4 (×3) soil samples were also collected from three different depths, 0 to 5 cm, 6 to 12 cm and 13 to 20 cm, of the corresponding locations to the tea leaves samples. More specifically, the soil samples were collected from four different points within an area of 1 m 2 around the tea tree. The 25-year-old tea trees were selected for collection of the tea leaf samples. Usually, the branches of the tea plant are cut and are fertilized twice per year, and in some cases fertilizers are used more than twice for influencing the growth of the tea plant in the garden. At present, the UTE produces approximately 0.7 million tons of tea per year with six separate grades of tea including the export quality one. In the local market and throughout The procedure for sample collection followed that recommended by the IAEA [4]. The collected samples were stored separately in sealed plastic bags and tagged with an identification number, and with the date and location of sampling. The samples were dried under direct sunlight for several days to allow evaporation of moisture content, subsequently being further dried for a period of 24 h in an oven maintained at 85 • C to remove any remaining moisture. The dried samples were then mechanically crushed into a fine powder, homogenized with a mortar and pestle and filtered through a sieve of 0.395 mm mesh size to obtain similarly sized particles. A constant dry weight was measured out for each sample evaluation. For the determination of activity concentration, the dried sample was transferred to an individual cylindrical container having dimension of 3.5 cm height and 8.5 cm diameter. To settle and obtain a homogeneous mixture of the samples, the containers were simply shaken by hand. The containers were then sealed tightly by using an insulating tape to reduce the possibility of moisture contamination. The samples were then kept undisturbed for 5-7 weeks at room temperature to attain secular equilibrium between short-lived progeny with the respective long-lived parents, 226 Ra (from 238 U) and 228 Ra (from 232 Th) [38,39]. It was assumed that 222 Rn and 220 Rn could not escape from the sealed containers during the period of storage. The samples were then ready for subsequent measurement and analysis by γ-ray spectrometry.

Measurement of Radionuclides
This study used a co-axial high-purity germanium (HPGe) γ-ray detector (GC2018, CANBERRA, USA), having a relative efficiency of 20%, resolution of 1.8 keV at 1332 keV of peak of 60 Co source, to measure the samples and standards obtained from the IAEA. The detector was coupled with a digital spectrum analyzer and GENIE 2000 to acquire the γ-ray spectra emitted from the samples. To ensure a low background environment, a cylindrical lead shielded arrangement (5.08 cm thick) with fixed bottom and movable cover was installed. The efficiency of the detector was measured using the reference samples RGU-1, RGTh-1 and RGK-1 provided by the IAEA [40], with results as presented in Figure 2. The standard sources containing known concentrations of 226 Ra, 232 Th and 40 K were supplied by the Canada Center for Mineral and Energy Technology (CAMET) under a contract with the IAEA. Considering the leaves' texture and density, a radioactive standard with leafy vegetables was prepared by mixing/spiking 226 Ra standard source of solid matrices in identical containers to the samples, and using them accordingly. Necessary information on the calibration of the efficiency of the detector is available elsewhere [41]. In this study, each sample was measured for 10,000 seconds to achieve reasonable statistics. The net count rate from the primordial radionuclides originating from the samples was obtained by subtracting the background count from the gross count, both acquired for the same counting time. The activity concentrations of 226 Ra and 232 Th radionuclides were assessed using the characteristic gamma lines of their short-lived progeny [42,43]. The concentrations of 40 K and 137 Cs were determined by the gamma ray lines of 1460.77 keV and 661 keV, respectively. For evaluation of 226 Ra and 232 Th, a weighted mean approach was applied following reference [14].

Calculation of Activity Concentration
Activity concentrations of radionuclides (Bq kg −1 ) in surface soil, sub-surface soils and plant samples were calculated using Equation (1)

Calculation of Activity Concentration
Activity concentrations of radionuclides (Bq kg −1 ) in surface soil, sub-surface soils and plant samples were calculated using Equation (1) [41]: where CPS represents the net counts per second, ε f the efficiency of the detector, Iγ the branching ratio and W s the weight of the sample in kg. The statistical uncertainties were expressed in terms of standard deviation (±σ), where σ is expressed in Equation (2) [41]: where N s and N b represent the sample and background counts in time T s and T b , respectively. The total uncertainty for each measured sample was calculated taking into account the statistical and other components of uncertainty. The combined uncertainty of the activity was estimated by using the quadratic sum of relevant quantities, which can be defined by Equation (3) [44]: where ∆A is the combined uncertainty of each measured value. The symbols ∆N, ∆ε γ , ∆ρ γ and ∆m s represent the uncertainties due to the counting statistics, N (<7%), detection efficiency, ε γ (4%), gamma ray emission probability, ρ γ (<1%), and sample weight, M S (<2%), respectively. The determined radioactivity levels, together with the uncertainties, are presented in Table 1. The lower limit of detection or the minimum detectable activity concentration (MDA) of the measurement system was calculated using Equation (4) [45,46]: where K α represents the statistical coverage factor which is equal to 1.64 (at the 95% confidence level), β is the background count in the energy of interest and the other symbols ε γ , ρ γ , T S and M S represent detection efficiency, gamma-ray emission probability, counting time, and sample weight, respectively. The MDAs for the studied radionuclides 226 Ra, 232 Th, 40 K and 137 Cs were calculated to be 0.32 Bq kg −1 , 0.60 Bq kg −1 , 2.5 Bq kg −1 and 0.4 Bq kg −1 , respectively.

Soil to Tea Leaves Transfer Factor (TF)
Within the food we eat, plants are the principal recipients of radioactive contamination, a result of atmospheric or other releases of radionuclides and from naturally occurring radioactivity within the soil [40]. Basically, the transfer factor defines the uptake of radionuclides from soil to plants, which can be calculated by the ratio of the radioactivity per unit dry weight of plant (C P ) to the radioactivity per unit dry weight of soil (C S ) in the rooting zone, using the Equation (5) [47,48]: Dry weight analysis is preferred, the amount of radioactivity per kilogram dry weight being subject to much less variability than the amount per unit fresh weight, thereby reducing uncertainties in the measured TF (transfer factor) [49]. The calculated TFs for the studied tea leaf samples are shown in Table 1.

Annual Committed Effective Dose (ACED)
Following the consumption characteristics of foodstuffs, the committed effective dose due to the ingestion of radionuclides can be calculated using Equation (6), as below [50]: where C r is the intake of radionuclides through use of the tea leaves, D CF,i are the ingestion dose conversion coefficients of 2.8 × 10 −7 Sv Bq −1 , 2.2 × 10 −7 Sv Bq −1 and 6.2 × 10 −9 Sv Bq −1 for 226 Ra, 232 Th and 40 K, respectively, for an adult [51] and A i is the measured activity concentration (Bq.kg −1 ) of each radionuclide. According to the typical statistics, an average of 2 g of tea leaves is needed to prepare a cup of tea and if one person drinks two cups of tea per day, then an amount of some 1.5 kg/year is consumed by an individual. The two cups of tea is a typical tea consumption characteristic for the Bangladeshi population. The C r is also defined as the consumption rate.

Threshold Consumption Rate of Tea (kg/y)
The threshold consumption rate (DI thresh ) represents a reference dietary level to avoid deleterious health hazards due to the intake of radionuclides via foodstuffs [52]. The particular threshold data due to the drinking of tea can be estimated by using the following Equation (7) [53]: were E ave (290 µSv/y) is the threshold committed effective dose due to the ingestion of radionuclides of interest via the consumption of foodstuffs [54,55], A 1 , A 2 and A 3 are the activity concentrations of 226 Ra, 232 Th and 40 K, respectively, in the tea leaf samples and D cfi is the activity to dose conversion coefficient for the radionuclides of interest, as before.

Carcinogenic Risk
The carcinogenic risk for a population is estimated by assuming a linear no threshold, dose-effect relationship as per ICRP practice. For low doses, the ICRP suggest a fatal cancer risk factor of 0.05 Sv −1 [56], which indicates that the probability of a person dying of cancer is increased by 5% for a total dose of 1 Sv received during a lifetime. The estimated average annual committed effective dose for tea leaves is used herein to calculate the carcinogenic risk for an adult, made of the following relationship Equation (8): where R f is the risk factor per sievert of annual effective dose received by the consumption of tea and A ls is the cumulated time of tea consumption by Bangladeshi populace. Considering the local typical tea consumption characteristics, a duration of 50 years was used for both sexes.

Activity Concentration in the Tea Garden Doil Samples
The mean activity concentrations of 226 Ra, 232 Th, 40 K and 137 Cs in the soil samples collected from five locations of UTE are given in Table 1. The measured values in the investigated soil samples are found in the order 40 K > 232 Th > 226 Ra > 137 Cs. 40 K dominates over the other nuclides, which is not unexpected. This is because potassium is the seventh most abundant element in the Earth's crust, making up 2.6% of the weight of the earth's crust [57]. The greater activity concentration of 232 Th over that of 226 Ra may be attributed to the differences in the physical and chemical characteristics in a natural environment. In the earth's crust, both uranium and thorium tend to occur together due to the some inherent characteristics. However, throughout the various superficial processes like weathering and transportation, and the soil characteristics (pH and redox), they become fractionated. In general, thorium possesses low solubility and accumulates on particular phases whereas uranium is chemically more soluble and mobile. Consequently, uranium can easily be redistributed and transported in various environmental matrices compared to thorium [48]. Table 1 shows the mean activity concentrations of 226 Ra in soil samples for all locations other than that at location 2 to be greater than the UNSCEAR reported worldwide mean value of 35 Bq.kg −1 [49]. Among the three studied layers/depths of soil, the greatest concentration of 226 Ra (53 ± 8 Bq.kg −1 ) was at location 5, at a depth of 13-to 20 cm, whereas, the minimum concentration of 226 Ra (27 ± 7 Bq.kg −1 ) was at location 2, at a depth of 6 to 12 cm. This may be correlated to the ambient environment, i.e., the presence of high moisture content in the clay silty sand soil of this location which allows better solubility of 226 Ra [58].
For all locations the mean activity concentrations of 232 Th are greater than the worldwide mean value of 30 Bq.kg −1 [49], while the 40 K data for all locations other than location 2 are less than the UNSCEAR [49] reported mean concentration of 400 Bq.kg −1 . In respect to the vertical distribution, the greatest concentration of 232 Th (82 ± 11 Bq.kg −1 ) was in soil from location 4, at a depth of 6 to 12 cm, whereas the minimum 232 Th concentration (29 ± 7 Bq.kg −1 ) was from soil at location 5, at a depth of 0 to 5 cm. Soil samples from location 5 are clay silty sand and have large carbonate content, a matter correlating with the low 232 Th concentration. The data show the level of natural radioactivity forming a similar distribution in the surface and deep layered soils.
The greatest concentration of 40 K (672 ± 81 Bq.kg −1 ) was shown to be at location 2, at a depth of 6 to 12 cm, whereas the minimum 40 K concentration (201 ± 78 Bq.kg −1 ) was at location 1, at a depth of 6 to 12 cm. The majority of 40 K is a part of a clay mineral component rather than organic matter and its mobility depends on its solubility in the soil [59]. The low concentration of 40 K may be correlated to the soil texture, i.e., the presence of more sandy soil. Moreover, use of NPK fertilizer at least two times per year for better yield of leaves may contribute to the higher values of 40 K activity [60,61]. 137 Cs, an anthropomorphic nuclide, as detected in trace amounts in the UTE soil, predominantly in the topsoil layers and less so or otherwise not detectable in sub-surface layers. The greatest 137 Cs mean activity concentration, at 10 ± 1 Bq.kg −1 , was found in surface soil at location 1, at a depth of 0 to 5 cm, while the lowest concentration of 3 ± 1 Bq.kg −1 was found at location 5, at the same depth. 137 Cs in other locations was not detected, the one exception being at location 1, at a depth of 6 to 12 cm. The mean 137 Cs concentrations at the different locations were found to be less than the world average value 51 Bqkg −1 as reported by UNSCEAR [49]. The 137 Cs is a quasi-permanent source of external gamma ray exposure, the activity slowly decaying in accordance with a half-life of some 30 years. The small likelihood that this nuclide will form a significant soil to plant pathway is generally acknowledged, the contaminant for the most part being linked to widely publicized nuclear establishment accidents. When detected, most typically at very low levels, the variation in the activity concentrations of the radionuclides are due to meteorological factors, the difference in sampling depth, physiochemical soil characteristics and the time of deposition.

Activity Concentration in Tea Leaf Samples
The measured activity concentrations of 226 Ra, 232 Th, 40 K and 137 Cs radionuclides in tea leaf samples collected from the Udalia Tea Estate as well as from the local market are summarized in Table 1. The concentrations of radionuclides in tea leaf samples are reported in Bq.kg −1 dry weight. The activity concentrations of studied radionuclides in the investigated tea leaf samples were in the order 40 K > 226 Ra > 232 Th > 137 Cs. The activity concentrations of 226 Ra were found to be greater than that of 232 Th in most of the tea leaf samples collected from UTE. One probable reason is that the 238 U ( 226 Ra) tends to move towards the outer extremities of the tree and accumulates more greatly in new leaves and sprouts [62].
The greater concentration of 40 K in tea leaf samples can be attributed for the most part to the specific metabolic processes of potassium involved in plant growth. Furthermore, for faster plant growth, the extra use of muriate (potassium chloride) of potassium fertilizer may be another factor causing the increase of 40 K concentration in the tea leaf samples [60]. It has been reported that about 88-96% of K is taken up by the plant from the soil through the root system [61]. Since plants take up a high amount of potassium and natural potassium contains 0.0117% of 40 K, the detection of high level of 40 K in plants is not unexpected.

Transfer Factors (TF) of Radionuclides from Soil-to-Tea Leaf
Soil to tea leaf transfer factor (TF) values from the five different locations are also presented in Table 1, the values depending on soil properties such as nutrient and moisture contents and pH [51]. It can be observed from the results that the TF values for 226 Ra, 232 Th and 40 K lie within the range 1.1 × 10 −2 to 1.0, in accordance with values reported by the IAEA [63]. 137 Cs in all of the tea leaf samples was found to be below the detection limit, therefore the transfer factors could not be calculated. Note that the IAEA report a TF range of 0.02-3.2 for 137 Cs [63]. This indicates that, compared to 226 Ra, 232 Th and 40 K, 137 Cs is less efficiently transported from soil to the tea bush, as well as to the leaves The transfer factors in the studied tea leaves are in the order 40 K > 226 Ra > 232 Th > 137 Cs, that for 40 K being significantly greater than those of other radionuclides in all samples. It is well known that K is a very essential nutrient for plants metabolism and depending upon the particular metabolism a variable amount of K is taken up by plants from soil. Since elemental potassium is homeostatically controlled by the body (intake and excretion maintaining balance), such amounts of 40 K in tea leaves are not to be considered to be of any particular concern as a potential radiation hazard. The actual concentration of radium in plant species clearly depends on the radium content of soil, its uptake by the plants species and also the metabolic characteristics of the plants [14]. Moreover, the chemical factors such as the presence of exchangeable amount of calcium in the soil may influence the absorption rate of radium by the plants [64]. The calculated TF show mean values of less than 1 for all radionuclides. It is worth mentioning that a value of TF >1 is indicative of radiation hazards to human health via the soil-plant-human body pathway.
On the other hand, a TF = 1 would be indicative of a particular species or plant forming a useful natural process for decontamination of soil affected by a nuclear accident or deliberate nuclear device testing. Table 2 shows a comparison of results from the present study with reported data for tea leaves from the Chittagong region of Bangladesh. Considering the similar geographical conditions, humidity and quality of soil, comparability of data might thus be expected. Within the Chittagong region, there are 17 tea growing estates in Fatickchari, 3 in Rangunia and 1 in Banskhali. In this respect, Table 2 shows the measured radioactivity of 226 Ra to be similar to the available literature data, while UTE values for 232 Th and 40 K show much lower values compared to the reported data in the literature. Moreover, radioactivity in the estate tea leaves from Rize in Turkey also show higher values than the present results from UTE. The activity concentration of the artificial 137 Cs radionuclide for the UTE sample is shown to be below the detection limit (<0.4), while a substantial amount of 137 Cs was reported in estate tea leaf samples from Turkey. Such a result indicates the contamination of sampling area via some known/unknown nuclear activities. There are no available studies on the radioactivity of marketed tea samples in Bangladesh, therefore studies on marketed tea leaf samples imported from abroad have been chosen for comparison. The average activity concentration of 226 Ra and 232 Th and 40 K in tea leaf samples collected from the local market show greater values than the reported data from Turkey (except 40 K) and Serbia. The fact that the concentrations of 226 Ra, 232 Th and 40 K vary substantially across the various regions depends mainly on their concentrations in the bedrock from which the soil originates [65].

Committed Effective Dose, Threshold Consumption Rate and Carcinogenic Risk
The calculated values of committed effective dose, threshold consumption rate and carcinogenic risk are shown in Table 3. The committed effective dose due to the intake of the studied radionuclides via tea consumption was found to be in the range of 4.7-5.6 µSv y −1 with a mean of 5.0 µSv y −1 . This compares with an average worldwide ingestion dose of 226 Ra and 232 Th of 120 µSv y −1 and 170 µSv y −1 for 40 K, making a total annual dose estimate of 290 µSv y −1 from the total diet [49]. The annual effective doses from the ingestion of tea leaves were found much lower than the limiting value recommended by UNSCEAR [49]. Note that the estimated 5.0 µSv y −1 is contributed to by only a single dietary element (here tea leaf), thus such a low value is not unexpected. However, the radiation risk via the cumulative consumption of tea leaf may not be totally negligible, because tea forms only a minor part of the total dietary habits [70,71]. Figure 3 shows the dose contribution due to the individual radionuclides. Among the studied radionuclides, 226 Ra incurred the maximum dose (38%) followed by 40 K (33%) and 232 Th (29%). Exposure to radioactive materials, especially radium, over a prolonged time may result in an increased carcinogenic risk. In addition, higher doses of radium are found to have links with anemia, cataracts, reduction of bone growth, etc. [72].   The estimated mean threshold consumption rate for the studied tea leaf samples was found to be 88 kg/y (equivalent to 241g/d), an untenable value. This parameter indicates that the consumption of tea below the estimated value poses only a negligible radiological health hazard, while a greater rate than the calculated ones indicates enhanced radiologi-226Ra 38% 232Th 29% 40K 33% The estimated mean threshold consumption rate for the studied tea leaf samples was found to be 88 kg/y (equivalent to 241g/d), an untenable value. This parameter indicates that the consumption of tea below the estimated value poses only a negligible radiological health hazard, while a greater rate than the calculated ones indicates enhanced radiological health risk.
Accordingly, the mean cumulative carcinogenic risk via tea leaf consumption (for a period of 50 years) was estimated at 1.3 × 10 −5 , significantly lower than the ICRP given cancer risk of 2.5 × 10 −3 , based on an annual effective dose limit of 1 mSv for the general population [52].

Conclusions
Activity concentrations of 226 Ra, 232 Th, 40 K and 137 Cs in soil and tea leaf samples collected from a large tea estate in the Chittagong region of Bangladesh were measured by HPGe γ-ray spectrometry. In addition, the most popular tea brands available in the local market were also measured to observe the effect of production processes. The transfer factor of radionuclides from soil to tea leaves was found to be less than 1, indicating the corresponding uptake by the tea plant to be insignificant. The estimated committed effective dose and the carcinogenic risk all show values far below the limiting ranges as suggested by various international bodies. Thus, the consumption of tea (at 4 g/day/person or two cups/day/person) produced from the Udalia Tea Estate provides an insignificant radiation risk to the health of the local populace. Considering a number of facts such as the non-availability of the literature data on TFs of the UTE tea leaves, the recommended limiting values for total dietary habits and that for the tea arising from this single entity, and that the radiation risk follows the linear no threshold model, the measured data can act as reference values for any future experimental or modelling studies for the protection of human health.