Influence of rock type and geophysical properties on radon flux density.

The most significant source of human exposure to ionizing radiation is the radioactive gas radon (basically Rn) and its daughter decay products, creating more than half of the effective dose from all natural sources. Radon enters buildings mainly from dense rocks, which are below building foundations at depths of 1 m and more. In this paper long-term measurements of radon flux density are analyzed, with radon exhalation from the surface of the most common rocks-loams, sandy loams, clays, clay shales, several types of sandy-gravel-pebble deposits, clay and rocky limestone.

The plant for obtaining an aqueous radon solution.

Developing indicator methods to determine the main characteristics of cores extracted from oil-bearing strata presupposes simple, radiation-safe installations of an aqueous radon solution. This study describes such an installation, comprising crushed uranium ores weighing ~45 kg. Herein, we investigated the radon concentration (RC) of water as a function of pumping rate and duration to determine the optimal pumping conditions necessary for achieving a maximum RC in water of ~3 kBq/L.