M. S. Sultana
Department of Natural Science, Varendra University, Rajshahi, Bangladesh
A. Rahim
Faculty of Science and Engineering, North Bengal International University, Rajshahi, Bangladesh
J. Ferdous*
* Health Physics Division, Atomic Energy Centre, Dhaka, Bangladesh
A. Begum
Bangladesh Atomic Energy Commission, Dhaka, Bangladesh
M. A. Islam
Department of Physics, University of Rajshahi, Bangladesh
Soil, Activity Concentration, Radiological Hazard Parameters, Gamma-Ray Spectrometry System, Kurigram District
Kurigram District, Bangladesh
Risk Management in Agriculture
Pollution, Heavy metal in soil
2.1. Area of Study Bangladesh is located at 88001' E-92041'E longitude and latitude 20034’N-26038’N which is geographically downward to India. Bangladesh is surrounding by the rivers and the source of the rivers in India. Some rivers are situated in Nepal, Bhutan and flown through India. Therefore its land might be contaminated by radioactive sources from upstream. In this present study, the soil samples are collected from most significant regions of Kurigram in Bangladesh. The number of Upazilla (sub district) in Kurigram district is 9, named- KurigramSadar, Ulipur, Chilmary, Nageshary, Vurungamari, CharRajibpur, Roumari, Rajarhat and Fulbari.
2.2. Sample Collection and Preparation Fifty one soil samples from seventeen locations of five upazilas of Kurigram, Bangladesh were collected in January 2014. Three soil samples were collected at 0-5cm, 5cm-10cm and 10-15cm depth from one place and each of the soil samples weighed approximately 1kg. The samples were packed in dried bags which were labeled with sample codes and sealed. Then the samples were moved to the radiation detection laboratories of the health physics division (AEC), Bangladesh. The samples were dehydrated at 1050C - 1100C and it was ensured that any significant moisture was removed from the samples. Each of the samples was grinded separately and kept into container.. The mass of the samples varied because of the varying density of the sample material. The containers were then labeled properly and sealed tightly, rapped with thick vinyl tapes around their screw necks. The samples were stored for at least four weeks to get ready for measurements.
2.3. Experimental Procedure Every soil sample was measured with a gamma-ray counting system, a high resolution High Purity Germanium coaxial detector (EG&G ORTEC) coupled with a SilenaEmcaplus Multichannel Analyzer (MCA) and associate microprocessors. The effective volume of the detector was 83.47 cm3 and energy resolution of the detector was 1.69 keV at 1332 keV energy with a relative efficiency of 19.6%. The detector was shielded with copper ring (2 mm) at the side and lead (76.2 mm) at the side and the top for reducing the background radiation level. Then the sample was located on the detector for counting. The efficiency of the detector for different radionuclides were identified by standard source Eu-152 and different energies such as 122, 245, 344, 411, 444, 779, 963, 1086, 1112 and 1408 keV (figure.5&6) supplied by Health Physics Division, Atomic Energy Centre, Dhaka (AECD). The radioactivity of238U and 232Th were determined from the average concentration of nuclides [214Pb (295.2keV), 214Pb (351.9keV), 214Bi (609.3keV) and 214Bi (1120.2keV)] and [212Pb (238.6keV), 208Tl (583.1keV), and 228Ac (911.2keV), 228Ac (968.9keV)] respectively. The radioactivity of 40K was determined directly by the gamma-ray transitions at 1460.8keV.
Noble International Journal of Scientific Research Vol. 1, No. 1, pp: 18-29, 2017
Journal