Radon Sunset

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Radon Sunset

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Radon is also fairly soluble in water and organic solvents. Although reaction with other compounds is comparatively rare, it is not completely inert and forms stable molecules with highly electronegative materials.

Radon is considered a noble gas that occurs in several isotopic forms. Only two are found in significant concentrations in the human environment: radon, and radon Radon is a member of the radioactive decay chain of uranium Radon is formed in the decay chain of thorium Radon decays in a sequence of radionuclides called radon decay products, radon daughters, or radon progeny.

It is radon that most readily occurs in the environment. Atmospheric releases of radon results in the formation of decay products that are radioisotopes of heavy metals polonium, lead, bismuth and rapidly attach to other airborne materials such as dust and other materials facilitating inhalation.

In addition, radon is used to initiate and influence chemical reactions and as a surface label in the study of surface reactions.

It has been obtained by pumping the gasses off of a solution of a radium salt, sparking the gas mixture to combine the hydrogen and oxygen, removing the water and carbon dioxide by adsorption, and freezing out the radon.

Radon is a naturally occurring radioactive gas and comes from the natural breakdown radioactive decay of uranium. It is usually found in igneous rock and soil, but in some cases, well water may also be a source of radon.

Radon in the ground, groundwater, or building materials enters working and living spaces and disintegrates into its decay products.

The likeness of the spectra of these three gases with those of argon, krypton, and xenon, and their observed chemical inertia led Sir William Ramsay to suggest in that the "emanations" might contain a new element of the noble-gas family.

In the early 20th century in the US, gold contaminated with the radon daughter Pb entered the jewelry industry.

This was from gold seeds that had held Rn that had been melted down after the radon had decayed. In , Ramsay and Robert Whytlaw-Gray isolated radon and determined its melting temperature and approximate density.

In , they determined that it was the heaviest known gas. Later, when isotopes were numbered instead of named, the element took the name of the most stable isotope, radon , while Tn was renamed Rn and An was renamed Rn, which caused some confusion in the literature regarding the element's discovery as while Dorn had discovered radon the isotope, he had not been the first to discover radon the element.

As late as the s, the element was also referred to simply as emanation. The name actinon for Rn is rarely encountered today, probably due to the short half-life of that isotope.

In , Paracelsus described a wasting disease of miners, the mala metallorum , and Georg Agricola recommended ventilation in mines to avoid this mountain sickness Bergsucht.

The first major studies with radon and health occurred in the context of uranium mining in the Joachimsthal region of Bohemia. The presence of radon in indoor air was documented as early as Beginning in the s, research was initiated to address sources of indoor radon, determinants of concentration, health effects, and mitigation approaches.

In the US, the problem of indoor radon received widespread publicity and intensified investigation after a widely publicized incident in During routine monitoring at a Pennsylvania nuclear power plant, a worker was found to be contaminated with radioactivity.

A high concentration of radon in his home was subsequently identified as responsible. All discussions of radon concentrations in the environment refer to Rn.

While the average rate of production of Rn from the thorium decay series is about the same as that of Rn, the amount of Rn in the environment is much less than that of Rn because of the short half-life of Rn 55 seconds, versus 3.

One WLM is equivalent to 3. The levels of Pb can be measured. The rate of deposition of this radioisotope is weather-dependent.

Radon concentrations found in natural environments are much too low to be detected by chemical means. Radon is produced by the radioactive decay of radium, which is found in uranium ores, phosphate rock, shales, igneous and metamorphic rocks such as granite, gneiss, and schist, and to a lesser degree, in common rocks such as limestone.

Radon concentration can differ widely from place to place. Radon concentration can be much higher in mining contexts.

Radon mostly appears with the decay chain of the radium and uranium series Rn , and marginally with the thorium series Rn.

The element emanates naturally from the ground, and some building materials, all over the world, wherever traces of uranium or thorium are found, and particularly in regions with soils containing granite or shale , which have a higher concentration of uranium.

Not all granitic regions are prone to high emissions of radon. Being a rare gas, it usually migrates freely through faults and fragmented soils, and may accumulate in caves or water.

Owing to its very short half-life four days for Rn , radon concentration decreases very quickly when the distance from the production area increases.

Radon concentration varies greatly with season and atmospheric conditions. For instance, it has been shown to accumulate in the air if there is a meteorological inversion and little wind.

High concentrations of radon can be found in some spring waters and hot springs. Natural radon concentrations in the Earth's atmosphere are so low that radon-rich water in contact with the atmosphere will continually lose radon by volatilization.

Hence, ground water has a higher concentration of Rn than surface water , because radon is continuously produced by radioactive decay of Ra present in rocks.

Likewise, the saturated zone of a soil frequently has a higher radon content than the unsaturated zone because of diffusional losses to the atmosphere.

The presence of Rn has been inferred later from data obtained from the Lunar Prospector alpha particle spectrometer. Radon is found in some petroleum.

Because radon has a similar pressure and temperature curve to propane , and oil refineries separate petrochemicals based on their boiling points, the piping carrying freshly separated propane in oil refineries can become radioactive because of decaying radon and its products.

Residues from the petroleum and natural gas industry often contain radium and its daughters. The sulfate scale from an oil well can be radium rich, while the water, oil, and gas from a well often contains radon.

Radon decays to form solid radioisotopes that form coatings on the inside of pipework. High concentrations of radon in homes were discovered by chance in after the stringent radiation testing conducted at a new nuclear power plant revealed that Stanley Watras , a construction engineer at the plant, was contaminated by radioactive substances even though the reactor had never been fueled.

Some level of radon will be found in all buildings. Radon mostly enters a building directly from the soil through the lowest level in the building that is in contact with the ground.

High levels of radon in the water supply can also increase indoor radon air levels. Typical entry points of radon into buildings are cracks in solid foundations and walls, construction joints, gaps in suspended floors and around service pipes, cavities inside walls, and the water supply.

Also, the concentration in one room of a building may be significantly different from the concentration in an adjoining room.

Most of the high radon concentrations have been reported from places near fault zones ; hence the existence of a relation between the exhalation rate from faults and indoor radon concentrations is obvious.

The distribution of radon concentrations will generally differ from room to room, and the readings are averaged according to regulatory protocols.

Indoor radon concentration is usually assumed to follow a lognormal distribution on a given territory.

Some of the highest radon hazard in the US is found in Iowa and in the Appalachian Mountain areas in southeastern Pennsylvania.

The second highest readings in Ireland were found in office buildings in the Irish town of Mallow, County Cork , prompting local fears regarding lung cancer.

In a few locations, uranium tailings have been used for landfills and were subsequently built upon, resulting in possible increased exposure to radon.

Since radon is a colorless, odorless gas, the only way to know how much is present in the air or water is to perform tests. In the US, radon test kits are available to the public at retail stores, such as hardware stores, for home use, and testing is available through licensed professionals, who are often home inspectors.

Efforts to reduce indoor radon levels are called radon mitigation. Radon is condensed by liquid nitrogen and purified from residue gases by sublimation.

Gaseous Rn half-life of about four days escapes from the capsule through diffusion. Radon trace concentration above oceans or in Antarctica can be lower than 0.

An earlyth-century form of quackery was the treatment of maladies in a radiotorium. The carcinogenic nature of radon due to its ionizing radiation became apparent later.

Radon's molecule-damaging radioactivity has been used to kill cancerous cells, [98] but it does not increase the health of healthy cells. The ionizing radiation causes the formation of free radicals , which results in cell damage , causing increased rates of illness, including cancer.

Exposure to radon has been suggested to mitigate autoimmune diseases such as arthritis in a process known as radiation hormesis.

The practice is discouraged because of the well-documented ill effects of high-doses of radiation on the body. Radium-rich springs are also used in traditional Japanese onsen in Misasa , Tottori Prefecture.

Drinking therapy is applied in Bad Brambach , Germany. In the US and Europe, there are several "radon spas", where people sit for minutes or hours in a high-radon atmosphere in the belief that low doses of radiation will invigorate or energize them.

Radon has been produced commercially for use in radiation therapy, but for the most part has been replaced by radionuclides made in particle accelerators and nuclear reactors.

Radon has been used in implantable seeds, made of gold or glass, primarily used to treat cancers, known as brachytherapy.

The gold seeds were produced by filling a long tube with radon pumped from a radium source, the tube being then divided into short sections by crimping and cutting.

The gold layer keeps the radon within, and filters out the alpha and beta radiations, while allowing the gamma rays to escape which kill the diseased tissue.

The activities might range from 0. Radon and its first decay products being very short-lived, the seed is left in place. At this stage, the predominant residual activity originates from the radon decay product Pb, whose half-life Radon emanation from the soil varies with soil type and with surface uranium content, so outdoor radon concentrations can be used to track air masses to a limited degree.

This fact has been put to use by some atmospheric scientists. Because of radon's rapid loss to air and comparatively rapid decay, radon is used in hydrologic research that studies the interaction between groundwater and streams.

Any significant concentration of radon in a stream is a good indicator that there are local inputs of groundwater. Radon soil-concentration has been used in an experimental way to map buried close-subsurface geological faults because concentrations are generally higher over the faults.

Some researchers have investigated changes in groundwater radon concentrations for earthquake prediction. For this reason, it has been hypothesized that increases in radon concentration is due to the generation of new cracks underground, which would allow increased groundwater circulation, flushing out radon.

The generation of new cracks might not unreasonably be assumed to precede major earthquakes. In the s and s, scientific measurements of radon emissions near faults found that earthquakes often occurred with no radon signal, and radon was often detected with no earthquake to follow.

It was then dismissed by many as an unreliable indicator. Radon is a known pollutant emitted from geothermal power stations because it is present in the material pumped from deep underground.

It disperses rapidly, and no radiological hazard has been demonstrated in various investigations.

In addition, typical systems re-inject the material deep underground rather than releasing it at the surface, so its environmental impact is minimal.

In the s and '50s, radon was used for industrial radiography. Radon decay products have been classified by the International Agency for Research on Cancer as being carcinogenic to humans, [] and as a gas that can be inhaled, lung cancer is a particular concern for people exposed to elevated levels of radon for sustained periods.

During the s and s, when safety standards requiring expensive ventilation in mines were not widely implemented, [] radon exposure was linked to lung cancer among non-smoking miners of uranium and other hard rock materials in what is now the Czech Republic, and later among miners from the Southwestern US [] [] [] and South Australia.

During this period, several entrepreneurs opened former uranium mines in the US to the general public and advertised alleged health benefits from breathing radon gas underground.

Health benefits claimed included pain, sinus, asthma and arthritis relief, [] [] but these were proven to be false and the government banned such advertisements in Since that time, ventilation and other measures have been used to reduce radon levels in most affected mines that continue to operate.

In recent years, the average annual exposure of uranium miners has fallen to levels similar to the concentrations inhaled in some homes.

This has reduced the risk of occupationally-induced cancer from radon, although health issues may persist for those who are currently employed in affected mines and for those who have been employed in them in the past.

Residues from processing of uranium ore can also be a source of radon. Radon resulting from the high radium content in uncovered dumps and tailing ponds can be easily released into the atmosphere and affect people living in the vicinity.

In addition to lung cancer, researchers have theorized a possible increased risk of leukemia due to radon exposure. Empirical support from studies of the general population is inconsistent, and a study of uranium miners found a correlation between radon exposure and chronic lymphocytic leukemia.

Miners as well as milling and ore transportation workers who worked in the uranium industry in the US between the s and may be eligible for compensation under the Radiation Exposure Compensation Act RECA.

Surviving relatives may also apply in cases where the formerly employed person is deceased. It should be highlighted though that not only uranium mines are affected by elevated levels of radon.

Coal mines in particular are affected as well since coal may contain more uranium and thorium than commercially operational uranium mines.

Radon exposure mostly radon daughters has been linked to lung cancer in numerous case-control studies performed in the US, Europe and China.

There are approximately 21, deaths per year in the US due to radon-induced lung cancers. North American and European pooled analyses further support these findings.

Most models of residential radon exposure are based on studies of miners, and direct estimates of the risks posed to homeowners would be more desirable.

Radon has been considered the second leading cause of lung cancer and leading environmental cause of cancer mortality by the EPA.

The greatest risk of radon exposure arises in buildings that are airtight, insufficiently ventilated, and have foundation leaks that allow air from the soil into basements and dwelling rooms.

A national reference level should not be a limit, but should represent the maximum acceptable annual average radon concentration in a dwelling. Results from epidemiological studies indicate that the risk of lung cancer increases with exposure to residential radon.

A well known example of source of error is smoking, the main risk factor for lung cancer. According to the EPA, the risk of lung cancer for smokers is significant due to synergistic effects of radon and smoking.

For this population about 62 people in a total of 1, will die of lung cancer compared to 7 people in a total of 1, for people who have never smoked.

Radon, like other known or suspected external risk factors for lung cancer, is a threat for smokers and former smokers. This was demonstrated by the European pooling study.

The risk is from smoking, compounded by a synergistic effect of radon for smokers. Without smoking, the effect seems to be so small as to be insignificant.

According to the European pooling study, there is a difference in risk for the histological subtypes of lung cancer and radon exposure.

Small-cell lung carcinoma , which has a high correlation with smoking, have a higher risk after radon exposure. For other histological subtypes such as adenocarcinoma , the type that primarily affects non-smokers, the risk from radon appears to be lower.

A study of radiation from post- mastectomy radiotherapy shows that the simple models previously used to assess the combined and separate risks from radiation and smoking need to be developed.

A study from , which included non-smokers and a control group of non-smokers, showed that exposure to radon increased the risk of lung cancer in non-smokers.

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Body Height cm :. Please select Soft Medium Hard. Cancel Delete Save. Description Radon Sunset 9. Highlights of the Sunset 9.

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Radon Sunset Video

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