Radon is released from rocks and then absorbed/dissolved in waters.
Radon doesn't react with water but it is soluble in water.
Radon is an important problem for the atmosphere in the buildings not for the water. Radon from the water can be eliminated by boiling the water. Also because the most important isotope pf radon, 222Rn, has a half life of only 3,8235 days radon disappear after a period of time.
Radon is a gas, water is a liquid. Under the same conditions radon should be many hundreds of times less dense than water. Water's density at STP is about 1 000 kg/m3. Radon's density at STP is about 9.73g/m3. Thus, water is about 103 times denser than radon.
Radon is not abundant. Earth crust: 4.10-19 kg radon/kg of rocks Sea water: 4.10-22 kg radon/L of water
Radon gets its name from the Latin word "radon" which means "radiation" or "ray." It was named so because radon is a radioactive gas that emits alpha particles as it decays.
No. Radon is chemically inert.
The groundwater contain more radon.
Mean concentration of radon in air: 150 atoms/cm3 Radon in the earth crust: 4.10-16 mg/kg Radon in the sea water: 6.10-19 mg/L
No, radon is a naturally occurring radioactive gas found in soil and water. It is not typically present in fuel oil. If high levels of radon are detected in the home, it is more likely due to soil and water sources.
Radon exposure occurs when people breathe in radon gas, which is a naturally occurring radioactive element found in soil, rock, and water. Prolonged exposure to high levels of radon can increase the risk of lung cancer. Testing for radon levels in homes and workplaces is important for identifying and mitigating this risk.
Lisa A Senior has written: 'Radon-222 in the ground water of Chester County, Pennsylvania' -- subject(s): Environmental aspects, Environmental aspects of Radon, Groundwater, Health aspects, Health aspects of Radon, Quality, Radon
The common form of radon is a colorless, odorless, and tasteless gas known as radon-222. It is a naturally occurring radioactive gas that is produced from the decay of uranium in soil, rock, and water.