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Measurements of radon flux and soil-gas radon concentration along the main central thrust, Garhwal Himalaya, using SRM and RAD7 detectors

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Radon in the Earth’s crust or soil matrix is free to move only if its atoms find their way into pores or capillaries of the matrix. 222Rn atoms from solid mineral grains get into air, filling pores through emanation process. Then 222Rn enters into the atmosphere from air-filled pores by exhalation process. The estimation of radon flux from soil surface is an important parameter for determining the source term for radon concentration modeling. In the present investigation, radon fluxes and soil-gas radon concentration have been measured along and around the Main Central Thrust (MCT) in Uttarkashi district of Garhwal Himalaya, India, by using Scintillation Radon Monitor (SRM) and RAD7 devices, respectively. The soil radon gas concentration measured by RAD7 with soil probe at the constant depth was found to vary from 12 ± 3 to 2330 ± 48 Bq m–3 with geometrical mean value of 302 ± 84 Bq m–3. The significance of this work is its usefulness from radiation protection point of view.
Słowa kluczowe
EN
RAD7   SRM   MCT   radon flux  
Czasopismo
Rocznik
Strony
950--957
Opis fizyczny
Bibliogr. 9 poz.
Twórcy
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
autor
  • Department of Physics, H.N.B. Garhwal University, Badshahi Thaul Campus, Tehri Garhwal, India
Bibliografia
  • Burchfiel, B.C., Z. Chen, K.V. Hodges, Y. Liu, L.H. Royden, C. Deng, and J. Xu (1992), The South Tibetan detachment system, Himalayan orogen: Extension contemporaneous with and parallel to shortening in a collisional mountain belt, Geol. Soc. Am. Sp. Papers 269, 1-41, DOI: 10.1130/ SPE269-p1.
  • Ciotoli, G., M. Guerra, S. Lombardi, and E. Vittori (1998), Soil gas survey for tracing seismogenic faults: A case study in the Fucino Basin, central Italy, J. Geophys. Res. 103, B10, 23781-23794, DOI: 10.1029/98JB01553.
  • Ciotoli, G., S. Lombardi, and A. Annunziatellis (2007), Geostatistical analysis of soil gas data in a high seismic intermontane basin: Fucino Plain, central Italy, J. Geophys. Res. 112, B5, 5407, DOI: 10.1029/2005JB004044.
  • Gansser, A. (1964), Geology of the Himalaya, Interscience, New York, 298 pp.
  • Gapais, D., A. Pêcher, E. Gilbert, and M. Ballèvre (1992), Synconvergence spreading of the higher Himalaya crystalline in Ladakh, Tectonics 11, 5, 1045-1056, DOI: 10.1029/92TC00819.
  • Gupta, S.K. (1977), Geology and petrology of part of Upper Bhagirathi Valley Central crystalline, Dist. Uttarkashi, M.Tech. Thesis, University of Roorkee, Roorkee, India (unpublished).
  • Heim, A.A. and A. Gansser (1939), Central Himalaya: Geological Observations of the Swiss Expedition 1936, Vol. 73, Hindustan Publishing Corporation, New Delhi, 245 pp.
  • Ramola, R.C., Y. Prasad, G. Prasad, S. Kumar, and V.M. Choubey (2008), Soil-gas radon as seismotectonic indicator in Garhwal Himalaya, Appl. Radiat. Isotopes 66, 10, 1523-1530, DOI: 10.1016/j.apradiso.2008.04.006.
  • Ramola, R.C. (2010), Relation between spring water radon anomalies and seismic activity in Garhwal Himalaya, Acta Geophys. 58, 5, 814-827, DOI: 10.2478/s11600-009-0047-0.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-cd6dd533-b732-43ab-8040-4f6918b2d6c7
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