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Geological and tectonic influence on water–soil–radon relationship in Mandi–Manali area, Himachal Himalaya

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Environmental Geology

Abstract

Radon measurements in soil and groundwater (springs, thermal springs and handpumps) were made in a variety of lithological units including major thrusts between Mandi and Manali in Himachal Himalaya. Analysis of radon data in light of lithological controls and influence of deep-seated thrusts has been made to elucidate the causative factors for anomalous emanation of radon. The lithological types include banded gneisses, schists, quartzite, granite, phyllites, volcanics and mylonites. The low-grade metasedimentries of Shali and Dharamsala generally show low and narrow range of radon concentration in water (5.6–13.4 Bq/l) as well as in soil (1.8–3.2 kBq/m3) except for the samples related to thrusts. On the other hand, sheared and deformed rocks of Chail and Jutogh show moderate radon content (average 5.03 kBq/m3, range 2.9–11.1 kBq/m3) in soil. However, the groundwater radon concentration shows wide variation in different types of sources (2.1–80.8 Bq/l). The quartzite and volcanic rocks of Rampur formation in this area present as a window separated by Chail thrust. Radon emanations on these rock types are relatively high (6.3–68.1 Bq/l in water and 5.5–15.9 kBq/m3 in soil) and are exceptionally high in samples that are related to uranium mineralization, deep-seated thrusts and hot springs (13.5–653.5 Bq/l). It is generally observed that anomalous high radon content is associated with mineralization, deeper source and tectonic discontinuities. Whereas it is obvious that subsurface radioactive mineralization would facilitate enhanced radon production, however, thrust plains provide easy pathways for escape of gases from the deeper sources. Shallow and deep sources of the groundwater have contrasting radon content particularly in the deformed and metamorphosed rocks of Jutogh and Chail. Shallow groundwater sources, mainly handpumps, have lower radon concentration due to limited superficial water circulation, whereas deeper sources, mainly perennial springs, show higher radon content because of larger opportunity for water–rock interaction.

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Acknowledgment

The authors (VMC & PKM) are thankful to Director of Wadia Institute of Himalayan Geology, Dehradun for providing necessary facilities. The research work was partially funded by DST sponsored project awarded to BSB and VW.

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Authors and Affiliations

  1. Wadia Institute of Himalayan Geology, 33-General Mahadeo Singh Road, Dehradun, 248001, India

    V. M. Choubey & P. K. Mukherjee

  2. National Center for Research on Earthquake Engineering, Taipei, 106, Taiwan

    Vivek Walia

  3. Department of Physics, Guru Nanak Dev University, Amritsar, 143005, India

    B. S. Bajwa

Authors
  1. V. M. Choubey
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  2. P. K. Mukherjee
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  3. B. S. Bajwa
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  4. Vivek Walia
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Correspondence to V. M. Choubey.

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Choubey, V.M., Mukherjee, P.K., Bajwa, B.S. et al. Geological and tectonic influence on water–soil–radon relationship in Mandi–Manali area, Himachal Himalaya. Environ Geol 52, 1163–1171 (2007). https://doi.org/10.1007/s00254-006-0553-1

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