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pro vyhledávání: '"V.M. Choubey"'
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Akademický článek
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Publikováno v:
Acta Geophysica. 61:977-999
The opening of cracks and influx of fluids in the dilatancy zone of impending earthquake is expected to induce short-term changes in physical/chemical/hydrological properties during earthquake build-up cycle, which should be reflected in time-varying
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::727a7185acb1380bd4518fd6514cfdae
https://doi.org/10.2478/s11600-013-0133-1
https://doi.org/10.2478/s11600-013-0133-1
Publikováno v:
Japanese Journal of Health Physics. 45:278-283
Radon measurements were made in the soil-gas and groundwater present in various lithological units and across the major tectonic zone (Munsiari and Bhatwari-Ramgarh Thrust) located between Ghansali and Ghuttu area in Bhilangana valley of the Garhwal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::05bf6a1e1d895cbc149784e4a64ff9be
https://doi.org/10.5453/jhps.45.278
https://doi.org/10.5453/jhps.45.278
Publikováno v:
Science of The Total Environment. 407:5877-5883
Continuous recording of different geophysical parameters incorporated at a single location as a unified effort for earthquake precursory through geodynamical changes initiated for the first time in the Garhwal Himalaya, India. A 68 m deep borehole, p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b06f208a505c8ea159b330ea59c080e
https://doi.org/10.1016/j.scitotenv.2009.08.010
https://doi.org/10.1016/j.scitotenv.2009.08.010
Publikováno v:
Radiation Measurements. 44:122-126
The radon content in groundwater sources depends on the radium concentration in the rock of the aquifer. Radon was measured in water in many parts of the world, mostly for the risk assessment due to consumption of drinking water. The exposure to rado
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e24ed9cfd645e0951d0fde82d9c1508d
https://doi.org/10.1016/j.radmeas.2008.10.006
https://doi.org/10.1016/j.radmeas.2008.10.006
Publikováno v:
Applied Radiation and Isotopes. 66:1523-1530
Research on earthquake-related radon monitoring has received enormous attention recently. Anomalous behaviour of radon in soil and groundwater can be used as a reliable precursor for an impending earthquake. While earthquake prediction may not yet be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a8b09995894b35e266ae9a5953a3baa8
https://doi.org/10.1016/j.apradiso.2008.04.006
https://doi.org/10.1016/j.apradiso.2008.04.006
Publikováno v:
Radiation Measurements. 43:S369-S374
Ionizing radiation exposure experienced by the general population is mainly due to the indoor radon. Major part of radon comes from the top layer of the earth. The radon emanation is associated with radon in soil and sleepy back radium in the soil. B
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c55b8a08c79d9416c8494048e7cda76c
https://doi.org/10.1016/j.radmeas.2008.04.056
https://doi.org/10.1016/j.radmeas.2008.04.056
Publikováno v:
Radiation Measurements. 43:98-101
This paper presents the results of investigation of radon levels in the soil–gas and groundwater of Uttarkashi, India within the distance of 5 km in vertical and horizontal directions from the landslide of Varunawat hill. Radon release from the soi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1fac2554a97ef81f544cf40430b76c69
https://doi.org/10.1016/j.radmeas.2007.05.054
https://doi.org/10.1016/j.radmeas.2007.05.054
Publikováno v:
Environmental Geology. 52:1163-1171
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 co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9498aa450c5c392e7dc1b5b89b2973c1
https://doi.org/10.1007/s00254-006-0553-1
https://doi.org/10.1007/s00254-006-0553-1