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Journal of Applied Sciences and Environmental Management
World Bank assisted National Agricultural Research Project (NARP) - University of Port Harcourt
ISSN: 1119-8362
Vol. 9, Num. 3, 2005, pp. 27-29

Journal of Applied Sciences & Environmental Management, Vol. 9, No. 3, 2005, pp. 27-29

Determination of Radionuclide Levels in Soil and Water around Cement Companies in Port Harcourt

AVWIRI, G O

Department of Physics, university of Port Harcourt, P. M. B. 5323, Port Harcourt, Nigeria

*Corresponding author: Email: goavwiri@yahoo.com

Code Number: ja05054

ABSTRACT:

The study of the radionuclide concentration levels in soil and water samples in Eagle, Atlas and rock cement companies in Port Harcourt was carried out.   Soil and water samples collected from the respective premises were analyzed using the gamma -ray spectrometry. The average absorbed dose rates of the soil samples were 49.27nGy/h, 45.21nGy/h and 42.33nGy/h for Eagle, Atlas and Rock cements respectively while the water values were 22.16nGy/h,   20.75nGy/h and 19.37nGy/h for the respective companies.  Mean dose rate equivalents of 0.18mSv/y  and  0.39mS/y were obtained for the water and soil samples.  These results are lower than the International Commission on Radiological Protection (ICRP) maximum permitted limit and therefore, have no significance radiological health burden on the environment and the populace. @JASEM

Industrial and domestic activities such as oil exploration and exploitation, manufacturing and process industries may lead to the perturbation of the natural ecosystem and the environment that ultimately occurs as pollution.   Increase in the background ionization radiation from numerous sources has various health side effects on the populace.  Some of the sources of radiations are cosmic rays and natural radionuclide in air, food and drinking water (NCRP, 1976).  Radiation exposure can be external: natural radionuclides and cosmic rays and internal:  food, drinking water and the mineral contents of the body.     The natural radionuclides in the earth or soil and water of an environment are present as daughters of  uranium (238U), thorium (232Th) isotopes distributed by natural geological and geochemical processes in addition to potassium (4%) and small quantities of fission-product residues 137Cs from atmospheric weapon test (Trimble, 1968). Exposure to excess level of background ionization radiation causes somatic and genetic effects that tend to damage critical and/or radiosensitive organs of the body, which ultimately can lead to death (Ajayi, 1999).  The major raw materials for the production of cement are limestone (CaCO3), shale ash and ion oxide.  They also contain some elements like gypsum, which contains silicates and aluminates that have ionization tendency (White, 1981).

The natural radionuclide levels have been studied in surface soils in Ijero-Ekiti (Ajayi, et, al. (1995)), in soil and water around a cement company in Ewekoro by Jubiri et, al. (1999) and in rocks found in Ekiti by Ajayi et, al(1999).   Results from these studies revealed non-significant levels of radionuclides in the environment. Port Harcourt, a major seaport in the Niger-Delta, plays host to a number of companies that are involve in manufacturing, packaging, processing and oil activities. The various rivers criss-crossing the city encourage the sitting of industries in the hinterland. Three cement companies, sited at Onne and Rumuolumeni exist in the city.  They are Eagle,  Rock and Atlas cements.  Their main operations involve the bulk importation of the cement (dust) and then packaging into various sizes for domestic and industrial usages.  Part of the operations take place in the ship berthed in the river such as the NewCalabarRiver for Eagle cement and River Nmu Ngololo for Rock and Atlas cements.  The locations of these companies are shown in Figures 1 and 2. 

The awareness of the potential degradation of the environment by the activities of these companies is on the increase and there have been various claims and counterclaims of degradation of the surface soil and rivers by the host communities. This study, therefore, determine the level of natural radionuclide concentrations in the soil and water in around the plants, estimates the level of degradation of the radioactive equilibrium of the areas and ascertain the radiological health side effects on the populace and the environment.

EXPERIMENTAL METHODS

Sample Collection and Preparation: Nine soil samples of about 500g were collected from the respective cement company’s premises and three samples were collected from the host community as indicated in Table 1to serve for comparative assessment.  The samples were kept in polyethene bags and were properly labeled as shown in Table 1 and taken to the laboratory for gamma (γ) ray analysis. The water samples were collected from the rivers where the ships are berthed.  About 6 litres of water were collected at three points in each river.   They are the berthing position of the ship, 500m upstream and 500m downstream.  The water samples were stored in a refrigerator and kept for 30 days for secular equilibrium to be established before the γ-ray analysis.

Table 1:  Sampling Points of Soil and Water Samples

Location Index

Locations

S11

Entrance Gate of Eagle Cement Co.

S12

Storage/Bagging Area of Eagle Cement Co.

S13

Admin Block Area of Eagle Cement Co.

S21

Entrance gate of Atlas Cement Co.

S22

Bagging Area of Atlas Cement Co.

S23

Onne Community, hosting Atlas Cement Co.

S31

Loading Area of Rock Cement Co.

S32

Bagging Area of Rock Cement Co.

S33

Admin Block of Rock Cement Co.

W11

500m upstream of Eagle Cement Co along NewCalabarRiver

W12

Berthing Station of Ship/vessel

W13

500m downstream of Eagle Cement along NewCalabarRiver

W21

500m upstream of Atlas Cement Co along Nmu Ngololo River (FOT)

W22

Berthing Station of Ship/vessel

W23

500m downstream of Atlas Cement Co. a long Nmu Ngololo Rivers (FOT)

W31

500m upstream of Rock Cement Co. along Nmu Ngololo River (FOT)

W32

Benthing  Station of Ship/vessel

W33

500m downstream of Rock Cement Co. along Nmu Ngololo River (FOT)

Legend: 1st digit indicates sample Number, 2nd digit indicates company i.e Eagle = 1, Atlas = 2, Rock = 3
Letter indicates type of sample – S = Soil, W = Water

Gamma (γ) ray Analysis: The method of γ-ray spectrometry as has been severally reported (Ajayi et, al. (1990)), Jubiri, et, al.  (1999) was adopted in the analysis.    The spectrometer consists of a Canberra 7.6cm by 7.6cm NaI (Tl) (Model No 802 – series) detector coupled to a Canberra series 10 plus Multichannel Analyzer (MCA) through a pre-amplifier base. The transition lines of 1.460 MeV of 40K, 1764.5 KeV of 214Bi and 2614.7Kev of 208Tl were used to determine the concentrations of 40k, 238U and 232Th respectively. The soil samples were sieved through a 2mm mesh screen and then placed in a container for 28 days to enable them reach secular equilibrium before the analysis.   The spectral for the soils were measured by counting for 2 hours and the area under the photo peaks were computed using the algorithm of the MCA. The water samples were transferred to a one-litre Marinelli sample container, which fits into the detector.   Counting was done for 10 hours because of the natural low activities of radionuclides in water.  The areas under the photopeaks were similarly computed as in the soil samples.   Environmental shielding for the water was achieved using a Canberra 10cm thick lead castle and 5cm thick lead castle was used for the soil (Farai and Sanni, 1992).

The specific activity concentrations Ack, Acu and AcTh for 40K,  238U and 232Th respectively were computed using the relation  (Beck, et. al, 1972 ).

                Ac       =              AAscms
                                            Asm.                     (1)

Where       Ac  = activity of sample, A = full peak area of samples,  Asc = activity concentration of standard sample, ms= mass of standard sample,   As  = full peak of the standard  sample and m = mass of sample.

The absorbed dose rates D, at 1.0m above the ground were calculated using the Beck, et al.  (1972) relation.

D = 0.042 AcK  + 0.429AcU  + 0.666AcTh.          (2)

Where 0.042  = Dose constant for 40K, 0.429  = dose constant for 238U and 0.666 dose constant for 232Th. Using the conversion factor of 0.70Sv/Gy (UNSCEAR), 1988), the dose equivalents in mSv/y were computed.

RESULTS AND DISCUSSION

The mean specific activities of the radionuclides concentration levels are presented in Tables 2 and 3 for soil and water samples respectively.   Table 4 shows the calculated absorbed dose rates for all samples.   The average absorbed dose rates of soil samples range from 49.27 nGy/h for Eagle Cement to 42.35nGy/h for the Rock cement and from 22.16 nGy/h to 19.37 nGy/h for the Eagle cement and Rock Cement’s water samples respectively.   The values of the dose equivalents of the soil samples for all the companies are lower than the average world soil average of 0.7mSv/y (ICRP, 1991). The dose equivalents of all samples are comparable with those reported in literature (Myrick, et al (1983) and  Jubiri et, al.  (1999).   The results show that the Eagle cement company, with longer period of operation has higher absorbed dose rates than the newly established Atlas and Rock Cements. The trend of the results in the soil samples shows that the specific activities of the radionuclides are higher in the storage/baggage area for the companies compared to the other areas within the premises. Also, the radionuclides activities are higher than that of the host community. These results suggest that the sitting of the companies may have degraded the immediate environment minimally. The water samples revealed that the dose rates are highest at the berthing/baggaging stations with a gradual decrease downstream. Though the dose equivalents are within the acceptable values for water, the toxicity of cement will naturally perturb the chemical equilibrium of the riverbanks thus making them unsuitable for natural fish breeding.

Table 2:  Mean Specific Activities of the radionuclides in the Soil Samples

SL

Radionuclides concentration  (Bg/kg)

Abs. Dose rate

nGy/h

40K

238U

232 Th.

S11

241.21

82.02

6.41

49.60

S12

654.12

61.41

4.50

56.92

S13

463.23

43.33

4.91

41.31

S21

389.21

51.21

7.53

43.32

S22

542.02

56.55

6.81

51.52

S23

315.64

45.54

3.01

34.79

S31

564.2

25.14

3.32

36.68

S32

772.19

23.31

8.22

47.91

S33

315.24

6061

4.85

42.47

MEAN

473.9S± 165.27

49.90 ± 17.34

5.51 ± 1.72

44.95 ± 6.75

Table 3.  Mean Specific Activities of the Radionuclides In Water Samples

SL

  Radionuclides concentration  (Bg/l)

Abs. Dose rate

nGy/h

40K

238U

232 Th.

W11

0.1210

41.20

0.0342

17.70

W12

0.1614

60.31

0.0480

28.91

W13

0.1412

53.23

0.0582

22.87

W21

0.3143

32.11

0.0312

13.81

W22

0.6631

71.21

0.0901

30.63

W23

0.5214

41.34

0.0622

17.80

W31

0.2978

35.27

0.0021

15.18

W32

0.4321

56.38

0.0070

24.21

W33

0.610

43.56

0.0081

18.72

MEAN

0.3624± 0.19

48.29 ±12.07

0.0379± 0.0296

20.76 ± 5.18

Table 4.  Absorbed Dose Rates in Soil and Water In mSv/y

Sample location

Absorbed dose rate (nGy/h)

mSv/y

S11

49.60

0.42

S12

56.92

0.48

S13

41.31

0.35

S21

43.32

0.39

S22

51.52

0.44

S23

34.79

0.30

S31

36.68

0.31

S32

47.91

0.41

S33

42.47

0.36

W11

17.70

0.15

W12

25.91

0.22

W13

22.87

0.19

W21

13.81

0.12

W22

30.63

0.26

W23

17.80

0.15

W31

15.18

0.13

W32

24.21

0.21

W33

18.72

0.16

Generally, these results show that the radiological health burden due to the operations of these companies on the human populace is very insignificant and has neither health implications nor affect the background ionization radiation and the results obtained could therefore be that due to natural ionization radiation of the environment.

Conclusion:

The study of the radionuclide concentration levels in soil and water in/around Eagle, Rock and Atlas cement companies in Port Harcourt has been carried out.  The average dose rates equivalent of 0.18mSv/y and 0.39 mSv/y were obtained for the water and soil samples respectively.  These values are lower than the MPL and therefore do not pose health problems to the populace of the host communities and do not affect the background ionization radiation of the environment. However, these values may increase with longer period of operation.

Acknowledgement:

The author is grateful to the University of Port Harcourt for funding this project through the NUC Research grant and the Management and Staff of the Centre for Energy Research and Development (CERD), ObafemiAwolowoUniversity and the cement companies are appreciated.

REFERENCES

  • Ajayi, I.R., Ajayi, O.S. and Fusuyi, A.S. (1995). ‘The Natural Radioactivity of Surface Soils in Ijero – Ekiti, Nigeria’.  Nig. Jour. Of  Phy. Vol. 7,  101 – 103.
  • Ajayi O.S. and Ajayi I.R. (1999)- ‘A Survey of Environmental Gamma  Radiation Levels of Some areas of Ekiti and Ondo States, Southwestern Nigeria’.  Nig. Jour. Of Phy. Vol. 11, 17 – 21.
  • Beck, H.L., Decompo, J. and Gologak, J. (1972). ‘ In-situ Ge (ii)  and NaI (Tl) gamma ray spectrometry’.  Health and Safety Laboratory AEC:  Report HASL 258, N.Y.
  • Farai, I.P. and Sanni, A.O. (1992). ‘ Year long Variability of Rn-222 in a ground water system in Nigeria’, Journal.  Afri Earth Sci., 15,  399.
  • ICRP (International Comm. On Radiological Protection) 1992, The 1990-91 Recommendations of the International Comm.  On Radiological Protection, Publication 60, Ann.  ICRP 21 1 – 3
  • Jibiri N.N. Mabawonku, A.O., Oridate A.A. and Ujiagbedion (1999), ‘Natural Radionuclide Conc.  Levels in Soil and Water around a Cement Factory at Ewekoro, Ogun, Nigeria’ Nig. Jour. of Phy.  Vol 11,  12 – 16.
  • Myrick, TE, Berven, B.A. and Haywood, F.F. (1983).’ Determination of CMC of selected radionuclides in Surface Soil in the U.S’. Health Phys. 45,  631.
  • National Council on Radiation Protection and Measurements, 1976, Environmental Radiation Measurements, NCRP Report, 4050.
  • Trimble, C.A. (1968) Absolute Counting of alpha Decay and the Radioactivity in Water from Hot Springs National Park, Master’s Thesis, University of Arkansas, Arkansas.
  • UNSCEAR (United Nations Scientific Comm. On  the Effects of Atomic Radiations).  (1988).  Sources, Effects and Risk of ionizing Radiations (NY).
  • White, G.R. (1981). Concrete Technology, 3rd Ed. John . Delmar Publishers, USA,   18 – 19

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