A Novel Assessment of the Surface Heat Flux Role in Radon (Rn-222) Gas Flow within Subsurface Geological Porous Media
A Benkovitz, H Zafrir, Y Reuveni - Remote Sensing, 2023 - mdpi.com
At present, Rn subsurface flow can be described only by diffusion and advection
transportation models within porous media that currently exist. Even though the temperature …
transportation models within porous media that currently exist. Even though the temperature …
The dynamics of Rn-222 cyclic flow within the shallow geological subsurface media as a daily temporal variated source for exhalation into the air
A Benkovitz, H Zafrir, Y Reuveni - Science of The Total Environment, 2024 - Elsevier
Extensive research on the dynamics of radon gas (Rn-222) originating from the radioactive
decay of radium (Ra-226) in geological subsurface media, sheds light on its periodic release …
decay of radium (Ra-226) in geological subsurface media, sheds light on its periodic release …
Seasonal variation of night-time accumulated Rn-222 in central Italy
Observations of Radon-222 taken in the central Italy site of L'Aquila since 2004 have been
analysed with simultaneously collected meteorological data and other atmospheric trace …
analysed with simultaneously collected meteorological data and other atmospheric trace …
Soil heat flux and air temperature as factors of radon (Rn-222) concentration in the near-ground air layer
A Podstawczyńska, W Pawlak - Nukleonika, 2016 - sciendo.com
A unique, highly time-resolved, and synchronous three-year dataset of near-surface
atmospheric radon-222 as well as soil heat flux and air temperature measurements at two …
atmospheric radon-222 as well as soil heat flux and air temperature measurements at two …
The impact of atmospheric and tectonic constraints on Radon-222 and carbon dioxide flow in geological porous media-a dozen-year research summary
H Zafrir, S Barbosa, E Levintal, N Weisbrod… - Frontiers in Earth …, 2020 - frontiersin.org
Long-term monitoring of Rn-222 and CO2 at a depth of several dozen meter at the Sde-
Eliezer site, located within one of the Dead Sea Fault Zone segments in northern Israel, has …
Eliezer site, located within one of the Dead Sea Fault Zone segments in northern Israel, has …
Differentiation between the effect of temperature and pressure on radon within the subsurface geological media
H Zafrir, SM Barbosa, U Malik - Radiation measurements, 2013 - Elsevier
Long-term continuous in-situ radon field monitoring was carried out in the southern region of
Israel, at the Amram Mountain research tunnel in Elat and in shallow boreholes in the …
Israel, at the Amram Mountain research tunnel in Elat and in shallow boreholes in the …
A 40-year retrospective European radon flux inventory including climatological variability
I López-Coto, JL Mas, JP Bolivar - Atmospheric Environment, 2013 - Elsevier
In this work, a 40-year retrospective European radon flux inventory has been calculated.
Average values of the radon exhalation rate, probability distributions and seasonal …
Average values of the radon exhalation rate, probability distributions and seasonal …
Study of abnormal seasonal variations in the radon exhalation rate in a fault zone
PS Miklyaev, TB Petrova - Geochemistry International, 2021 - Springer
Strong seasonal variations in the radon exhalation rate from the soil surface were revealed
during a two-year monitoring cycle in a fault zone on a slope of Mount Beshtau in the …
during a two-year monitoring cycle in a fault zone on a slope of Mount Beshtau in the …
Temporal signatures of advective versus diffusive radon transport at a geothermal zone in Central Nepal
Temporal variation of radon-222 concentration was studied at the Syabru-Bensi hot springs,
located on the Main Central Thrust zone in Central Nepal. This site is characterized by …
located on the Main Central Thrust zone in Central Nepal. This site is characterized by …
Radon-222 survey in Larderello geothermal field, Italy (part I)
F D'Amore - Geothermics;(United States), 1975 - osti.gov
Radon-222 survey in Larderello geothermal field, Italy (part I) (Journal Article) | OSTI.GOV skip
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