Open Access

226Ra, 232Th and 40K contents in water samples in part of central deserts in Iran and their potential radiological risk to human population

  • Elham Ehsanpour1,
  • Mohammad Reza Abdi1Email author,
  • Mojtaba Mostajaboddavati2 and
  • Hashem Bagheri3
Contributed equally
Journal of Environmental Health Science and Engineering201412:80

DOI: 10.1186/2052-336X-12-80

Received: 15 October 2013

Accepted: 14 April 2014

Published: 1 May 2014

Abstract

Background

The radiological quality of 226Ra, 232Th and 40K in some samples of water resources collected in Anarak-Khour a desertic area, Iran has been measured by direct gamma ray spectroscopy using high purity germanium detector in this paper.

Result

The concentration ranged from ≤0.5 to 9701 mBq/L for 226Ra; ≤0.2 to 28215 mBq/L for 232Th and < MDA to 10332 mBq/L for 40K. The radium equivalent activity was well below the defined limit of 370Bq/L. The calculated external hazard indices were found to be less than 1 which shows a low dose.

Conclusion

These results can be contributed to the database of this area because it may be used as disposal sites of nuclear waste in future.

Keywords

Activity concentration Gamma spectrometry Water Anarak-khour Iran

Background

The presence of naturally occurring radionuclides as well as some elements provides important information about the quality of water resources especially drinking water [1].

Naturally occurring radioactive materials (NORM) consist of uranium, thorium, potassium and any of their decay products such as radium and radon. Concentrations of these natural radioactive elements are very low in the earth’s crust and atmosphere. These elements can be brought to the surface by human activities. Although the radioactive elements in the earth’s crust are the reasons of presence of radioactivity in water resources, high concentration of radioactive materials in water resources might be accidentally or intentionally [2, 3]. The public can be affected by the environment where is adjacent to the released point of the radioactive materials [4]. If radioactive materials are released into the environment, radionuclides may be moved into the body by inhalation and ingestion, which causes internal exposure. Fakeha et al. analyzed samples from well water and bottled drinking water from the Western Province of Arabia for concentrations of natural radioactivity and their contribution to the absorbed dose from water samples using gamma spectroscopy method [1]. Fasunwon et al. studied the activity concentrations of natural radionuclide levels in well waters of Ago Iwoye, Nigeria by HPGe (high purity germanium) spectrometer [5]. They estimated that radiological health burden on the human populace is very minimal and has neither health implications nor affect the background ionization radiation. In a research article studied that natural radioactivity of different brands of commonly sold bottled drinking water in the federal capital Islamabad and Rawalpindi city of Pakistan and found mean concentrations of 226Ra, 232Th and 40K were 11.3 ± 2.3, 5.2 ± 0.4 and 140.9 ± 30.6 mBq/L, respectively using gamma spectroscopy technique [6].

The United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) estimated that exposure to natural radionuclides contributes around 70% of the population radiation dose. The global average human exposure to natural sources is 2.4mSv/y and the weight of water and food is about 0.3mSv/y.

The objective of this study is to obtain a representative estimate of the concentration levels of natural radionuclides in water resources which might be used as drinking water in some our studied sites from the central deserts of Iran, also estimate the corresponding radiation doses for people consuming this water. With water analysis, soil analyses have been performed in this area. The obtained results can be contributed to the baseline data of radionuclide concentrations in this area.

Description of the study area

The intersection of Uroomieh-Dokhtar Magmatic Belt (UDMB) and the major Great Kavir- Doruneh fault (GKDF) are two dominant structural features in the Anarak-Khour area and the change of direction of Great Kavir-Doruneh fault towards the Nain-Baft fault (Figure 1). This region occupies the north-western corner of the Central-Eastern Iranian microplate. This terrane is an approximately 2300km2 region of moderate relief surrounded by folding and thrust belts within the Alpine-Himalayan orogenic system of western Asia. This terrene is an area of continuous continental deformation in response to ongoing convergence between the Arabian (Gondwana) and Turan (Eurasian) plates [7]. Continental volcanism along the UDMB and in Central Iran, which also comprises the volcanic rocks of the Anarak-Khour area, is attributed to that subduction.
Figure 1

Main structural lineaments in Central Iran and location of the study area (modified from[8]).

In the Anarak-Khour area there are a few compositionally complex hydrothermal Cu-Ni-Co deposits which always interested for researchers. Apart from Cu, Ni and Co the ores contain As and U and occasionally Pb, Zn, Au and Ag. All these deposits are localized in the same area under similar geological environment along the north-western and western surroundings of Anarak-Khour massif (Figure 1). These deposits contain a distinctive set of elements and minerals. In the Anarak area, Co, Ni and As are abundant but there is little Ag or Bi [8]. The deposits also show some U. Cu is different because its concentration is high and in particular the abundance of copper arsenides. As with other deposits, Fe is present in only small amounts and S is rare in the arsenide stage of mineralization. Talmessi and Meskani mines are ancient mines for Cu, Ni and Co products that mining activities have ceased since 1960. Recently, exploration activities were conducted by the atomic energy organization of Iran in the course of uranium exploration but there is not any U mine in this area until now. The most important active mine in the area is Nakhlak lead deposit, 40 Km east of Anarak. In geology and geochemistry, the radioactive deposits are associated with high concentrations of heavy metals such as As, Cd, Co, Cr, Cu, Fe, Hg, Ni, Pb, S, Sb and Zn. It seems the presence of deposits and location of this area along the fault is caused these materials coming from the deeper layers to the surface layers and this can be a reason for founding the radionuclides and assessing the radiological risk in this area.

Experimental

Sampling

Anarak-khour is a landscape that is very dry because of low rainfall amounts (precipitation) then finding water in this area is difficult. Water sampling was taken from well water, reservoir and ground water. The sample locations were recorded in terms of degree-minute-second latitudinal and longitudinal position using a hand-held Global Positioning System (GPS) unit in Table 1. Places that would likely have a greater radioactivity concentration were selected as sample sites. Then the water samples of this area are collected from 33°22’46.52” N (with 53°27’47.90” E) to 34°12’25.12” N (with 55°18’55.40” E). The studied area is located within the rectangular area and is divided into six sites as shown in Figure 2. Reference methods for collecting procedure and handling of the water samples were taken from the International Atomic Energy Agency (IAEA, water sampling and laboratory treatment). Some these samples came from wells with submerged pumps. The water samples were gathered in two liter plastic bottles and were acidified with nitric acid to pH < 2. Physicochemical parameters of water such as temperature and pH were also measured in order to find the impact of these parameters on the concentration of the radionuclides in water. For water samples 800 mL of each sample was transferred to a Marinelli beaker. Then, the Marinelli-beaker was sealed and kept for at least 5 weeks. During this time, the daughter of radon achieves to equilibrium with 226Ra. Then the samples were ready to analysis by gamma spectroscopy [9].
Table 1

Sampling spots information

Longitude

Latitude

Altitude

Temperature

pH

Characteristic

Site no.1 (Talmessi mine)

1

33°22’46.52” N

53°27’47.90” E

1465

13

8

Ground water

2

33°23’9.02” N

53°27’47.16” E

1476

13

8.1

Ground water

Site no.2 (Nakhlak mine)

3

33°29’0.12” N

53°48’6.19” E

1134

21

8.39

Well water

4

33°29’5.23” N

53°48’2.69” E

1134

21

10.5

Well water

5

33°33’1.05” N

53°52’23.30” E

955

22

8.7

Ground water

6

33°33’44.01” N

53°50’23.63” E

1021

21

8.5

Ground water

Site no.3 (Calkafi mine)

7

33°23’58.17” N

54°14’18.91” E

1253

24

8.9

Well water

8

33°26’51.76” N

54° 5’34.70” E

923

24

11

Well water

Site no.4 (Mesr village)

9

34° 2’34.59” N

54°47’45.25” E

850

24

7.28

Well water

10

33°56’41.90” N

55° 1’27.22” E

948

15

7.92

Reservoir

Site no.5 (Ordib zone)

11

33°29’33.80” N

54°55’18.45” E

1081

27

8

Ground water

12

33°32’59.04” N

54°55’58.88” E

1061

43

7.4

Ground water

Site no.6 (Irakan zone)

13

33°58’24.08” N

55° 7’15.04” E

851

15

8.13

Reservoir

14

34° 1’44.81” N

55° 6’13.56” E

984

15

8.04

Reservoir

15

34° 7’51.60” N

55° 6’35.85” E

1016

22

7.77

Well water

16

34°12’25.12” N

55°18’55.40” E

721

30

6.54

Well water

17

34°12’18.67” N

55°19’1.61” E

727

33

6.39

Well water

Figure 2

Sampling sites.

Gamma-ray detection system

The activity of 226Ra, 232Th, 40K and 137Cs in the samples were measured using a P-type coaxial HPGe detector. The detector has a resolution of 1.89keV at 1.33MeV of 60Co. The detector was maintained in a vertical position and shielded by 10 cm thick lead wall, 2 mm cadmium and 3 mm copper to reduce background radiation [10]. Spectrum acquisition was done using the computer software MAESTRO with a multi-channel analyzer (4096-channel) and spectrum analysis was done by using the OMNIGAM software. The reference material IAP-mixed gamma water standard sources (Institute of Atomic Energy POLATOM, Radioisotope Center) containing 241Am, 137Cs and 152Eu were used to obtain efficiency curve. The absolute photopeak efficiencies were determined using following polynomial fit:
ϵ = a + blnE + c lnE 2 + d lnE 3 + e lnE 4 + f lnE 5 + g lnE 6
(1)

Where the constant values a, b, c, d, e, f and g are -0.0004 ± 0.0001, -0.02 ± 0.004, -0.01 ± 0.0006, 0.0001 ± 0.00004, 0.0003 ± 0.00005, 0.000000008 ± 0.000000001 and -0.00000006 ± 0.000000001, respectively.

A wide range of different gamma-ray energy transition lines ranging from about 100 keV up to 1765 keV, associated with the decay products of the 226Ra, 232Th and 40K. The known photopeak lines with background subtraction were used to determine 226Ra, 232Th and 40K. The counting time of sample spectra was also 24 hours.

The activities were measured using following relationship.
A = N t × m × p × ϵ E
(2)

where N, t, m, p and ϵ (E) are net area counts, time, intensity, weight of sample and absolute photopeak efficiency at specific energy, respectively [11]. The specific activity of 226Ra was evaluated from gamma-ray lines of 214Bi at 609.3, 1120.3 and 1764.5keV and 214Pb at 295 and 351keV, while the specific activity of 232Th was evaluated from gamma-ray lines of 228Ac at 338.4, 911.1 and 968.9keV. The specific activity of 40K and 137Cs was determined from its 1460.8 and 661.6keV gamma-ray lines [12]. The minimum detectable activity for each radionuclide was 0.54 mBq/L for 226Ra, 0.21 mBq/L for 232Th and 0.01 mBq/L for 40K.

Results and discussion

The concentrations of radionuclides of 241Am, 137Cs and 152Eu measured in standard reference material (POLATOM) and results are presented in Table 2. The measured concentrations of 241Am, 137Cs and 152Eu had high consistent with the certificate ones, the correlation coefficient for the liner regression between the measured and reference concentrations was 1 as shown in Figure 3.
Table 2

Comparison of radionuclide concentrations of 241 Am, 137 Cs and 152 Eu in POLATOM standard reference material

Radionuclide

Reference activity (kBq)

Determined activity (kBq)

Determined activity (Bq/L)

Am-241

18.13 ± 0.004

18.03 ± 0.004

0.49±0.004

Cs-137

7.77 ± 0.002

7.18 ± 0.002

0.21±0.002

Eu-152

4.07 ± 0.001

3.42 ± 0.001

0.11±0.001

Figure 3

Correlation coefficient for the liner regression between the measured and reference concentrations.

Radioactivity characterization of the subground waters

Radioactivity levels of 226Ra, 232Th and 40K in the water samples collected from different parts of the studied area are presented in Table 3. As shown in Table 3, activity concentrations in the water samples are in the range of 120 ± 30 - 2836 ± 274 mBq/L for 226Ra; 257 ± 39 - 7465 ± 607 mBq/L for 232Th and 2930 ± 490 - 7168 ± 1067 mBq/L for 40K. The maximum activity concentration of 226Ra and 232Th is found on site No.6 (Irakan Zone) which may be related to the geological structure of the region. The maximum activity concentration of 40K is found in site No. 1 (Talmessi mine). Potassium activity varied widely with CV (Coefficient Variation) =38% due to heterogeneous soil characteristics of this area [13]. The activity concentrations of 226Ra and 232Th in our samples are compared with the UNSCEAR reference mean values which are 1 mBq/L and 0.05 mBq/L in United States, respectively [14]. The activity concentrations of 226Ra and 232Th in the studied area are much more than the UNSCEAR reference values in the United States. Comparison of radioactivity of waters with other desertic areas has been done. The concentration of radioactivity of 226Ra in Arabia, Nigeria and Pakistan was reported between < MDA – 2500 mBq/L (with an average 1810 mBq/L), <MDA – 5400 mBq/L (with an average 1200 mBq/L) and 11300 mBq/L, respectively [1, 5, 6]. The mean concentration of 226Ra in Anarak-Khour is lower than the average concentration of it in Arabia, Nigeria and Pakistan and also is lower than its minimum concentration in Egypt. The concentration of radioactivity of 232Th was reported between < MDA and 3300 mBq/L (with an average 1470 mBq/L) in Arbia, < MDA and 6200 mBq/L (with an average 1600 mBq/L) in Nigeria and 5200 mBq/L in Pakistan. The mean concentration of radioactivity of 232Th in Arabia, Nigeria and our studied area is almost identical. The range of concentration of radioactivity of 40K was reported between < MDA and 339200 mBq/L (with an average 17596 mBq/L) in Arabia, < MDA and 50900 mBq/L (with an average 25100 mBq/L) in Nigeria. In Pakistan, the mean concentration of 40K about 140900 mBq/L was reported. Moreover, the results are compared to the World Health Organization proposed the following guidance levels for the activity concentration in drinking water (10000 mBq/L for 226Ra and 1000 mBq/L 232Th) [15]. The measured activities of 226Ra in the samples did not exceed the guidance level recommended by WHO (World Health Organization). For 232Th, Site No.6 had higher activity concentrations (7465 mBq/L >1000 mBq/L) compared to guidance levels recommended by WHO for drinking water. Figure 4 shows the distribution of 226Ra, 232Th and 40K activity concentrations of water samples. As shown in Figure 4, activity concentrations of 232Th were higher in water samples than 226Ra. In the waters in general, the concentration of 232Th was found to be higher than that of the 226Ra because 226Ra may be created on the surface of the host rock or ejected into the aqueous phase via alpha recoil. Both processes would affect in a depletion of 226Ra relative to 232Th. Additionally, 226Ra is more soluble and mobile in ground water than 232Th and may leach from the host rock, independent of the place of creation. There is a relationship between the activity concentration of 226Ra and 232Th with R square value 0.99 from our sampling site. This shows in all sampling sites the ratio of 232Th to 226Ra is more than one.
Table 3

Average activity concentration of 226 Ra, 232 Th and 40 K in water sampling sites

 

Concentration (mBq/L)

226Ra

232Th

40K

Site no.1

120 ± 30

257 ± 39

7168 ± 1067

Site no.2

350 ± 54

562 ± 61

3727 ± 577

Site no.3

128 ± 30

287 ± 44

2930 ± 490

Site no.4

270 ± 49

390 ± 80

2951 ± 496

Site no.5

341 ± 63

914 ± 138

5325 ± 837

Site no.6

2836 ± 274

7465 ± 607

6196 ± 670

Average

674

1646

4716

Stdev

1064

2861

1781

CV (%)

158

174

38

Figure 4

Distribution of activity concentrations of 226 Ra, 232 Th and 40 K in water samples.

Radiological risk assessment

The absorbed dose rates (D) due to gamma radiation in air at 1m above the ground level, assuming uniform distribution of the naturally occurring radionuclides (226Ra, 232Th and 40K) was calculated based on guidelines is given by UNSCEAR (2000) and IRSN reports (2011). The contributions from other naturally occurring radionuclides have been assumed insignificant. Therefore, D in units of nGy.h-1 was calculated according to UNSCEAR (2000) as:
D nGy / h = 0.462 A Ra + 0.621 A Th + 0.0417 A K
(3)
The annual effective outdoor dose rate in units of mSv.year-1 was calculated using the following formula [16]:
Effectivedoserate mSv / year = 1.23 × 10 3 × Doserate
(4)
Radium equivalent activity is an index that has been used to represent the specific activities of 226Ra, 232Th and 40K by a one quantity, which takes into account the radiation hazards associated with them. The radium equivalent activity is a weighted sum of activities of the studied natural radionuclides and is based on the assumption that 370Bq/L of 226Ra, 259Bq/L of 232Th, and 4810Bq/L of 40K produce the same gamma radiation dose rate [16]. The maximum value of Raeq must be less than 370Bq/L for safe use [17]. It is defined as follows:
Ra eq = A Ra + 1.43 × A Th + 0.077 A K
(5)

where ARa, ATh and AK are the activity concentrations of 226Ra, 232Th and 40K, respectively.

A widely used hazard index called the external hazard index Hex is defined as follows [13]:
H ex = A Ra / 370 + A Th / 259 + A K / 4810
(6)
In addition to the external hazard index, radon and its short-lived progeny are also hazardous to the respiratory organs. The internal exposure to radon and its daughter progenies is quantified by the internal hazard index Hin, which is given by the equation [13]:
H in = A Ra / 185 + A Th / 259 + A K / 4810
(7)
The calculated total gamma dose rate due to primordial radionuclides varied from 0.29 to 6.102 nGy/h. The average total gamma dose rate was less than the worldwide average of 55 nGy/h [12]. The annual effective dose obtained in the investigated areas ranged from 0.36 to 7.502μSv for the background area. The reported gamma dose rate and annual effective dose in other places, such as Lake Bosumtwi Basin in Ghana [18] is higher than these areas. But, Abo Zaabal in Egypt [19], Niger Delta (Biseni) flood plain lakes [20], Outer Carpathians in Poland [21] is lower or at least equal to the values of this research. If the value of internal or external radiation hazard index is found to be less than unity, then there is no potential internal or external radiation hazard. The external radiation hazard index (Hex) in water varied from 0.002 to 0.0376 whereas the internal radiation hazard index (Hin) in water varied from 0.002 to 0.0448. This indicated that the water of Anarak-khour area were free from the radiation hazards. The absorbed dose rates (D), annual effective outdoor dose rate, radium equivalent activity (Raeq) Hex and Hin of our samples are calculated and their results are shown in the Table 4. As seen in this table, Hex and Hin of our results are less than unity which shows there is no radiation hazard for the body.
Table 4

Calculated average values of absorbed dose rate and annual effective dose, radium equivalent activity, external and internal radiation hazard

 

Absorbed dose rate (nGy/h)

Radium equivalent activity (Bq/L)

External radiation hazard index (Hex)

Internal radiation hazard index (Hin)

Site no.1

0.525

1.015

0.003

0.003

Site no.2

0.665

1.415

0.004

0.004

Site no.3

0.290

0.625

0.002

0.002

Site no.4

0.490

1.035

0.003

0.003

Site no.5

0.895

1.930

0.005

0.006

Site no.6

6.102

13.770

0.038

0.045

Conclusion

Our estimate of water radioactivity concentration on Anarak-khour area in central of Iran is done using gamma-ray spectrometry. The maximum activity concentration of 226Ra and 232Th is found in Irakan Zone. The maximum activity concentration of 40K is found in Talmessi mine. The measured activities of 226Ra in the samples did not exceed the guidance level recommended by WHO but the measured activities of 232Th in Irakan Zone exceeded. The calculated total gamma dose rate varied from 0.29 to 6.102 nGy/h. The annual effective dose obtained from 0.36 to 7.502μSv for the background area. The internal radiation hazard index (Hin) in water varied from 0.002 to 0.0448. The parameters of absorbed dose rate, annual effective dose, radium equivalent activity, external radiation hazard index and internal radiation hazard index is calculated and their results showed there is no potential internal radiation hazard. This study can be followed by analyzing the deep soil and plants of the studied area. Moreover, because there are a lot of people who physically are impaired, the birth rate of children with defects should be compared with the radiounuclide concentrations in soils, waters and plants in every few years. Our results will contribute to the data base of this area in future. Then it is necessary that after operating the disposal site of nuclear waste all environment samples of the studied area should be performed every year and compared with our results.

Notes

Declarations

Acknowledgement

The authors wish to thank the office of graduate studies of the University of Isfahan for its support. They would also like to thank the staff of central laboratory of University of Isfahan for their assistance. Also, the authors wish to thank Dr. Rezaee for her help and her valuable guidance.

Authors’ Affiliations

(1)
Department of Physics, Faculty of Science, University of Isfahan
(2)
Department of Nuclear Engineering, Faculty of Advanced Sciences & Technologies, University of Isfahan
(3)
Department of Geological Science, Faculty of science, University of Isfahan

References

  1. Fakeha A, Hamidalddin S, Alamoudy Z, Al-Amri MA: Concentrations of natural radioactivity and their contribution to the absorbed dose from water samples from the Western Province, Saudi Arabia. JKAU: Sci 2011, 23(2):17–30.Google Scholar
  2. Selçuk Zorer Ö, Ceylan H, Doğru M: Gross alpha and beta radioactivity concentration in water, soil and sediment of the Bendimahi River and Van. Environ Monit Assess 2009, 148: 39–46. 10.1007/s10661-007-0137-xView ArticleGoogle Scholar
  3. Abdi MR, Kamali M, Vaezifar S: Distribution of radioactive pollution of 226 Ra, 232 Th, 40  K and 137 Cs in northwestern coasts of Persian Gulf, Iran. Mar Pollut Bull 2008, 56: 751–757. 10.1016/j.marpolbul.2007.12.010View ArticleGoogle Scholar
  4. Sherwood Lollar B: Environmental Geochemistry, Volume 9: Treatise on Geochemistry. Amsterdam: Elsevier; 2005.Google Scholar
  5. Fasunwon OO, Alausa SK, Odunaike RK, Alausa IM, Sosanya FM, Ajala BA: Activity concentrations of natural radionuclide levels in well waters of Ago Iwoye. Nigeria Iran J Radiat Res 2010, 7(4):207–210.Google Scholar
  6. Fatima I, Zaidi JH, Arif M, Tahir SNA: Measurement of natural radioactivity in bottled drinking water in Pakistan and consequent dose estimates. Radiat Prot Dosim 2007, 123(2):234–240.View ArticleGoogle Scholar
  7. Ramezani J, Tucker R: The Saghand region, Central Iran: U-Pb geochronology, petrogenesis and implications for Gondwana tectonics. Am J Sci 2003, 303: 622–665. 10.2475/ajs.303.7.622View ArticleGoogle Scholar
  8. Bagheri H, Moore F, Alderton DHM: Cu-Ni-Co-As (U) mineralization in the Anarak area of Central Iran. J Southeast Asian Earth Sci 2006, 29: 651–665.View ArticleGoogle Scholar
  9. Abbas MI: HPGe detector photopeak efficiency calculation including self absorption and coincidence corrections for Marinelli beaker sources using compact analytical expressions. Appl Radiat Isot 2001, 54: 761–768. 10.1016/S0969-8043(00)00308-0View ArticleGoogle Scholar
  10. Debertin K, Helmer RG: Gamma and X-ray spectrometry with semiconductor detectors. Amsterdam: Elsevier; 1988.Google Scholar
  11. Faghihian H, Rahi D, Mostajaboddavati M: Study of natural radionuclides in Karun river region. J Radioanal Nucl Chem 2012, 292: 711–717. 10.1007/s10967-011-1496-xView ArticleGoogle Scholar
  12. Abdi MR, Hassanzadeh S, Kamali M, Raji HR: 226 Ra, 232 Th, 40 K and 137 Cs activity concentrations along the southern coast of the Caspian Sea, Iran. Mar Pollut Bull 2009, 58: 658–662. 10.1016/j.marpolbul.2009.01.009View ArticleGoogle Scholar
  13. Kinyua R, Atambo VO, Ongeri RM: Activity concentrations of 40 K, 232 Th, 226 Ra and radiation exposure levels in the Tabaka soapstone quarries of the Kisii Region, Kenya. African J Environ Sci Tech 2011, 5: 682–688.Google Scholar
  14. UNSCEAR: Sources and Effects of Ionizing Radiation (Report to the General Assembly). New York: United Nations Publication; 2000.Google Scholar
  15. WHO: Guidelines for drinking water quality. Geneva: IWA Publishing; 2004.Google Scholar
  16. Farai IP, Ademola JA: Radium equivalent activity concentrations in concrete building blocks in eight cities in Southwestern Nigeria. J Environ Radioact 2005, 79: 119–125. 10.1016/j.jenvrad.2004.05.016View ArticleGoogle Scholar
  17. Abbady AGE: Estimation of radiation hazard indices from sedimentary rocks in Upper Egypt. Appl Radiat Isot 2004, 60: 111–114. 10.1016/j.apradiso.2003.09.012View ArticleGoogle Scholar
  18. Adu S, Darko EO, Awudu AR, Adukpo OK, Emi-Reynolds G, Obeng M, Otoo F, Faanu A, Agyeman LA, Mensah CK, Hasford F, Ali ID, Agyeman BK, Kpordzro R: Preliminary Study of Natural Radioactivity in the Lake Bosumtwi Basin. Res J Environ Earth Sci 2011, 3: 463–468.Google Scholar
  19. Morsy Z, El-Wahab MA, El-Faramawy N: Determination of natural radioactive elements in Abo Zaabal, Egypt by means of gamma spectroscopy. Ann Nucl Energy 2012, 44: 8–11.View ArticleGoogle Scholar
  20. Agbalagba EO, Onoja RA: Evaluation of natural radioactivity in soil, sediment and water samples of Niger Delta (Biseni) flood plain lakes, Nigeria. J Environ Radioact 2011, 102: 667–671. 10.1016/j.jenvrad.2011.03.002View ArticleGoogle Scholar
  21. Kozłowska B, Walencika A, Dordaa J, Przylibskib TA: Uranium, radium and 40Kisotopes in bottled mineral waters from Outer Carpathians, Poland. Radiat Meas 2007, 42: 1380–1386. 10.1016/j.radmeas.2007.03.004View ArticleGoogle Scholar

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This article is published under license to BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.

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