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Study Guide for Advanced Radon Measurement Service Provider Course This study guide can help you:

• take notes; • read and study offline; • organize information; and • prepare for assignments and assessments.

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Student Verification & Interactivity Student Verification

By enrolling in this course, the student hereby attests that s/he is the person completing all coursework. S/he understands that having another person complete the coursework for him or her is fraudulent and will result in being denied course completion and corresponding credit hours.

The course provider reserves the right to make contact as necessary to verify the integrity of any information submitted or communicated by the student. The student agrees not to duplicate or distribute any part of this copyrighted work or provide other parties with the answers or copies of the assessments that are part of this course. If plagiarism or copyright infringement is proven, the student will be notified of such and barred from the course and/or have his/her credit hours and/or certification revoked.

Communication on the message board or forum shall be of the person completing all coursework.

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Goal and Objectives Goal: The goal of this course is to teach the student how to perform radon measurements.

Objectives: Upon successful completion of this course, the student shall be able to:

• describe the physics of radon; • describe the health effects of breathing radon; • list the ways radon enters a home; • describe the testing procedures for radon; • follow protocols in non-‐real estate transactions; • follow protocols in real estate transactions; • develop and follow a quality assurance plan and implement quality control

procedures; • properly use passive devices; • properly use active devices; • test for radon in water; • learn how to remove radon from water; • list different ways to approach radon mitigation in homes; • install effective mitigation systems in new homes; • install materials and follow procedures to build radon-‐resistant homes; • inspect radon mitigation systems; and • abide by a code of ethics.

Course Summary Radon is a radioactive gas that emanates from rocks and soils and tends to concentrate in enclosed spaces, such as underground mines or houses. Soil gas infiltration is recognized as the most important source of residential radon. Other sources, including building materials and water extracted from wells, are less important in most circumstances. Radon is a major contributor to the ionizing radiation dose received by the general population.

Studies on indoor radon and lung cancer in Europe, North America, and Asia provide strong evidence that radon causes a substantial number of lung cancer cases in the general population. Estimates of the proportion of lung cancers attributable to radon range from 3% to 14%, depending on the average radon concentration in the

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country concerned and the calculation methods. The analyses indicate that the lung cancer risk increases proportionally with increased radon exposure. As many people are exposed to low and moderate radon concentrations, the majority of lung cancers related to radon are caused by these exposure levels rather than by higher concentrations. Radon is the second-‐leading cause of lung cancer after smoking. Most of the radon-‐induced lung cancer cases occur among smokers due to a strong combined effect of smoking and radon.

Radon measurements are relatively simple to perform and essential to assess radon concentration in homes. They need to be based on standardized protocols to ensure accurate and consistent measurements. Indoor radon concentration varies with the construction of buildings and ventilation habits. These concentrations vary substantially not only with the season, but also from day to day and even from hour to hour. Because of these fluctuations, estimating the annual average concentration of radon in indoor air requires reliable measurements of mean radon concentrations for at least three months and preferably longer. Short-‐term measurements provide only a crude indication of the actual radon concentration. Quality assurance for radon measurement devices is highly recommended in order to ensure the quality of measurements.

Addressing radon is important both in the construction of new buildings (prevention) and in existing buildings (mitigation or remediation). The primary radon prevention and mitigation strategies focus on sealing radon entry routes and on reversing the air pressure differences between the indoor occupied space and the outdoor soil through different soil depressurization techniques. In many cases, a combination of strategies provides the highest reduction of radon concentrations. The choice of radon prevention and mitigation interventions can be based on an analysis of cost effectiveness. In this approach, net healthcare costs are set in relation to net health benefits for a variety of actions or policies, providing an index with which these actions can be prioritized.

Selected analyses indicate that preventive measures in all new buildings are cost effective. Prevention in new homes tends to be more cost effective than mitigation of existing homes. In some low-‐risk areas, the measurement costs may be higher than the mitigation costs (for existing dwellings) due to the high number of homes that will have to be tested compared to the proportion of homes mitigated.

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Even if analyses indicate that remediation programs are not cost effective on a nationwide basis, indoor radon at high concentrations poses a considerable risk of lung cancer for individuals and requires mitigation. Since the general public is often unaware of the risks associated with indoor radon, special risk communication is recommended. Radon risk communication needs to be focused on informing different audiences and recommending appropriate action on reducing indoor radon. A cooperative effort is required, involving technical and communication experts, to develop a set of core messages. Radon risk messages should be kept as simple as possible and quantitative risk information must be expressed to the public in clearly understandable terms. It is useful, for example, to place the risk of lung cancer due to radon in comparison with other cancer risks, or with common risks in everyday life. Public health programs to reduce the radon risk should ideally be developed on a national level. Such national radon programs would be designed to reduce the overall population’s risk from the national average radon concentration as well as the individual risk for people living with high radon concentrations. A national radon policy should focus on identifying geographical areas where populations are most at risk from radon exposures and raising public awareness about the associated health risk. Key elements for a successful national program include collaboration with other health promotion programs (e.g., indoor air quality, tobacco control) and training of building professionals and other stakeholders involved in the implementation of radon prevention and mitigation. Appropriate building codes that require the installation of radon prevention measures in homes under construction should be enacted, and the measurement of radon during the purchase and sale of homes is useful to identify those with high radon concentrations.

A national reference level for radon represents the maximum accepted radon concentration in a residential dwelling and is an important component of a national program. For homes with radon concentrations above these levels, remedial actions may be recommended or required. When setting a reference level, various national factors such as the distribution of radon, the number of existing homes with high radon concentrations, the arithmetic mean indoor radon level, and the prevalence of smoking should be taken into consideration.

Introduction The risks to human health posed by ionizing radiation are well known. Radon gas is by far the most important source of ionizing radiation among gases of natural origin. Radon (Rn-‐222) is a noble gas formed from radium (Ra-‐226), which is a decay product of uranium (U-‐238). Uranium and radium occur naturally in soils and rocks. Other decay products of uranium include the isotopes thoron (Rn-‐220) and actinon (Rn-‐219). Radon gas, which has a half-‐life of 3.8 days, emanates from rocks and soils and tends to concentrate in enclosed spaces, such as underground mines or houses. It is a major contributor to the ionizing radiation dose received by the general population.

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When radon gas is inhaled, densely ionizing alpha particles emitted by the deposited short-‐lived decay products of radon (Po-‐218 and Po-‐214) can interact with biological tissue in the lungs, leading to DNA damage. Cancer generally requires the occurrence of at least one mutation, and proliferation of intermediate cells that have sustained some degree of DNA damage can greatly increase the pool of cells available for the development of cancer. Since even a single alpha particle can cause major genetic damage to a cell, it is possible that radon-‐related DNA damage can occur at any level of exposure. Therefore, it is unlikely that there is a threshold concentration below which radon does not have the potential to cause lung cancer.

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The health effects of radon, most notably lung cancer, have been investigated for several decades. Initially, investigations focused on underground miners exposed to high concentrations of radon in their occupational environment. However, in the early 1980s, several surveys of radon concentrations in homes and other buildings were carried out, and the results of these surveys, together with risk estimates based on the studies of mine workers, provided indirect evidence that radon may be an important cause of lung cancer in the general population.

Recently, efforts to directly investigate the association between indoor radon and lung cancer have provided convincing evidence of increased lung cancer risk causally associated with radon, even at levels commonly found in buildings. Risk assessments for radon in both mines and residential settings have provided clear insights into the health risks due to radon. Radon is now recognized as the second-‐leading cause of lung cancer after smoking in the general population.

The understanding of radon sources and radon transport mechanisms has evolved over several decades. In the 1950s, high concentrations of radon were observed in domestic and drinking water from drilled wells. Initially, concern about radon in water focused on health effects from ingesting the water. Later, it was determined that the primary health risk of radon in water was from the inhalation of radon released indoors. By the mid-‐1970s, emanation of radon from building materials was found to be a problem in some areas due to the use of alum shale with enhanced levels of radium.

By 1978, houses were identified in which the indoor radon concentrations were not associated with well-‐water transport or emanation from building materials. Soil gas infiltration became recognized as the most important source of indoor radon. Other sources, including building materials and well water, are less important in most circumstances.

Epidemiological evidence indicates that indoor radon is responsible for a substantial number of lung cancers in the general population. The distribution of indoor radon in most countries is best represented by a log-‐normal distribution, with the majority of radon concentrations occurring in the lower range. As a result, most radon-‐induced lung cancers are thought to occur following exposure to low and moderate radon concentrations. There is now a remarkable coherence between the risk estimates developed from epidemiological studies of miners and residential

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case-‐control radon studies. While the miner studies provide a strong basis for evaluating risks from radon exposure and for investigating the effects of modifiers to the dose-‐response relation, the results of the recent pooled residential studies provide a direct method of estimating risks to people at home without the need for extrapolation from the miner studies.

Radon has little practical use. Some medical treatments have employed radon in small sealed glass tubes, called seeds, that are specially manufactured to contain the exact amount of radioactivity needed for the application. Radon spas are used extensively in Russia and Central Europe to treat a number of conditions.

What Is Radon? Radon is a gas produced by the radioactive decay of the element radium. Radioactive decay is a natural, spontaneous process in which an atom of one element decays or breaks down to form another element by losing atomic particles (protons, neutrons, or electrons). When solid radium decays to form radon gas, it loses two protons and two neutrons. These two protons and two neutrons are called an alpha particle, which is a type of radiation. Elements that produce radiation are referred to as radioactive. Radon itself is radioactive because it also decays, losing an alpha particle and forming the element polonium.

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Elements that are naturally radioactive include uranium, thorium, carbon and potassium, as well as radon and radium. Uranium is the first element in a long chain of decay that produces radium and radon. Uranium is referred to as the "parent" element, and radium and radon are called "daughters" or "progeny." Radium and radon also form daughter elements as they decay. The progeny of radon are called radon decay products, or RDPs. The decay of each radioactive element occurs at a very specific rate. How fast an element decays is measured in terms of the element's "half-‐life," or the amount of time for one-‐half of a given amount of the element to decay. Uranium has a half-‐life of 4.4 billion years, so a 4.4-‐billion-‐year-‐old rock has only half of the uranium with which it started. The half-‐life of radon is only 3.8 days. If a jar were filled with radon, only half of the radon would be left after 3.8 days. But the newly made daughter products of radon (or RDPs) would also be in the jar, including polonium, bismuth, and lead. Polonium is also radioactive. It is this element which is produced by radon in the air and in people's lungs that can hurt lung tissue and cause lung cancer.

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Radioactivity is commonly measured in picocuries (pCi). Because the level of radioactivity is directly related to the number and type of radioactive atoms present, radon and all other radioactive atoms are measured in picocuries. For instance, a house having 4 picocuries of radon per liter of air (4 pCi/L) has about eight or nine atoms of radon decaying every minute in every liter of air inside the house. A 1,000-‐square-‐foot house with 4 pCi/L of radon has nearly 2 million radon atoms decaying inside it every minute. Radon levels in outdoor air, indoor air, soil air and groundwater can be very different. Outdoor air ranges from less than 0.1 pCi/L to about 30 pCi/L, but it probably averages about 0.2 pCi/L. Radon in indoor air ranges from less than 1 pCi/L to about 3,000 pCi/L, but it probably averages between 1 and 2 pCi/L. Radon in soil air (the air that occupies the pores in soil) ranges from 20 or 30 pCi/L to more than 100,000 pCi/L; most soils in the United States contain between 200 and 2,000 pCi of radon per liter of soil air. The amount of radon dissolved in groundwater ranges from about 100 to nearly 3 million pCi/L.

Natural Radiation Exposure Since the beginning of time, all living creatures have been exposed to radiation. We

live in a radioactive world. There are many natural sources of radiation that have been present since the Earth was formed. In the last century, we have added somewhat to this natural background radiation with artificial sources. However, the naturally occurring sources contribute about four to five times more radiation than human-‐made sources.

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The three major sources of naturally occurring radiation are: • cosmic radiation; • sources in the Earth's crust, also referred to as terrestrial radiation; and • sources in the human body, also referred to as internal sources.

Cosmic The Earth and all living things on it are constantly bombarded by radiation from space, similar to a steady drizzle of rain. Charged particles from the sun and stars interact with Earth’s atmosphere and magnetic field to produce a shower of radiation, typically beta and gamma radiation. The dose from cosmic radiation varies in different parts of the world due to differences in elevation and to the effects of the Earth’s magnetic field. Cosmic radiation comes from the sun and outer space, consisting of positively charged particles as well as gamma radiation. At sea level, the average cosmic radiation dose is about 26 millirems (mrem) per year. At higher elevations, the amount of atmosphere shielding cosmic rays decreases and, thus, the dose increases. The average dose in the United States is approximately 28 mrem per year.

Terrestrial Radioactive material is also found throughout nature. It is in the soil, water, and vegetation. Low levels of uranium, thorium and their decay products are found everywhere. This is called terrestrial radiation. Some of these materials are ingested with food and water, while others, such as radon, are inhaled. The dose from terrestrial sources also varies in different parts of the world. Locations with higher concentrations of uranium and thorium in their soil have higher dose levels. The major isotopes of concern for terrestrial radiation are uranium and its decay products, such as thorium, radium, and radon. There are natural sources of radiation in the ground, rocks, building materials, and potable water supplies. Radon gas is a current health concern. This gas results from the decay of natural uranium in soil. Radon, which emits alpha radiation, rises from the soil under houses and can build up in homes, particularly well-‐insulated homes. In the United States, the average effective whole-‐body dose of radon is about 200 mrem per year, while the lungs receive approximately 2,000 mrem per year.

Internal In addition to cosmic and terrestrial sources, all humans are born with naturally occurring radionuclides, such as potassium-‐40, carbon-‐14, lead-‐210, and other isotopes. The variation in dose from one person to another is not as great as the

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variation in dose from cosmic and terrestrial sources. The average annual "dose" from internal radioactive material is about 40 mrem.

Ionizing Radiation Exposure to the Public This chart shows that of the total annual dose of about 360 millirems, natural sources of radiation account for about 82% of all public exposure, while man-‐made sources account for the remaining 18%.

Definitions • Accuracy: the degree of agreement of a measurement (X) with an accepted

reference or true value (T); usually expressed as the difference between the two values (X – T), or the difference as a percentage of the reference or true value (100[X – T]/T), and sometimes expressed as a ratio (X/T).

• Active radon / radon decay product (RDP) measurement device: a radon or radon decay product measurement system that uses a sampling device, detector, and measurement system integrated as a complete unit or as separate but portable components. Active devices include continuous radon monitors, continuous working-‐level monitors, and grab-‐radon gas and grab working-‐level measurement systems, but do not include devices such as electret ion chamber devices, activated-‐carbon or other adsorbent systems, or alpha-‐track devices.

• Alpha particle: two neutrons and two protons bound as a single particle emitted from the nucleus of certain radioactive isotopes in the process of decay.

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• Background instrument (analysis system or laboratory) count rate: the nuclear counting rate obtained on a given instrument with a background counting sample. Typical instrument background measurements are: • unexposed carbon, for activated-‐carbon measurement systems • a scintillation vial containing scintillant and a sample known to contain no radioactivity, for scintillation counters • background measurements made with continuous radon monitors exposed only to radon-‐free air (aged air or nitrogen).

• Background field measurements (blanks): measurements made by analyzing unexposed (closed) detectors that accompanied exposed detectors to the field. The purpose of field background measurements is to assess any exposure to the detector caused by radon exposure other than from the concentration in the environment to be measured. Results of background field measurements are subtracted from the actual field measurements before calculating the reported concentration. Background levels may be due to electronic noise of the analysis system, leakage of radon into the detector, detector response to gamma radiation, or other causes.

• Background radiation: radiation arising from radioactive material other than that under testing. Background radiation due to cosmic rays and natural radioactivity are always present; background radiation may also be due to the presence of radioactive substances in building materials.

• Becquerel, becquerel (Bq): the International System of Units (SI) definition of activity. 1 Bq = 1 nuclear disintegration per second.

• Calibrate: to determine the response or reading of an instrument relative to a series of known values over the range of the instrument; results are used to develop correction or calibration factors.

• Check source: a radioactive source, not necessarily calibrated, which is used to confirm the continuing satisfactory operation of an instrument.

• Client: the individual or parties who hire(s) the radon tester.

• Closed-‐house/building conditions: During any short-‐term test, closed-‐house conditions should be maintained as much as possible while the test is in progress. In tests lasting fewer than four days, closed-‐house conditions should be maintained for at least twelve hours before starting the test, as well as for the duration of the test. While closed-‐house conditions are not required before starting tests lasting between four and ninety days, they should be maintained as much as possible.

• Coefficient of variation (CV or COV), relative standard deviation (RSD): a measure of precision calculated as the standard deviation of a set of

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values divided by the average, and usually multiplied by 100 to be expressed as a percentage: CV = RSD = / x 100 for a sample CV' = RSD' = / x 100 for a population Also see relative percent difference.

• Curie, curie (Ci): a standard measurement for radioactivity, specifically, the rate of decay for a gram of radium at 37 billion decays per second; a unit of radioactivity equal to 3.7 x 1010 disintegrations per second.

• Duplicate measurements: two measurements made concurrently and in the same location, or side-‐by-‐side; used to evaluate the precision of the measurement method.

• Efficiency or intrinsic detector: the relationship between the number of events recorded (counts, voltage lost, tracks) and the number of radioactive particles incident on the sensitive element of the detector per unit time. Efficiencies for radon detectors are commonly expressed in terms of the calibration factor, which is the number of events (counts) per time (hour or minute) per radon concentration (pCi/L). Methods with high efficiencies will exhibit more counts (signal) per unit time in response to a given radon level than will a method with a low efficiency.

• Equilibrium ratio (for radon): equilibrium ratio = WL(100)/(pCi/L). At complete equilibrium (i.e., at an equilibrium ratio of 1), 1 WL of RDPs would be present at the radon concentration of 100 pCi/L. The ratio is never 1 in a house; due to ventilation and plate-‐out, the RDPs never reach equilibrium in a residential environment. A commonly assumed equilibrium ratio is 0.5 (i.e., the decay products are halfway toward equilibrium), in which case 1 WL would correspond to 200 pCi/L. However, equilibrium ratios vary with time and location, and ratios of 0.3 to 0.7 are commonly observed.

• Equilibrium equivalent concentration (EEC): the radon concentration in equilibrium with its short-‐lived progeny that has the same potential alpha

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energy per unit volume as the environment being measured (also see working level).

• Exposure time: the length of time a specific mail-‐in device must be in contact with radon or radon decay products to get an accurate radon measurement; also called exposure period, exposure parameters, and duration of exposure.

• Gamma radiation: short-‐wavelength electromagnetic radiation of nuclear origin with an energy between 10 keV and 9 MeV.

• Integrating device: a device that measures a single average concentration value over a period of time; also called a time-‐integrating device.

• Lower limit of detection (LLD): the smallest amount of sample activity that will yield a net count for which there is confidence at a predetermined level that activity is present. For example, for a 5% probability of concluding falsely that activity is present, the LLD is approximately equal to 4.65 times the standard deviation of the background counts (assuming large numbers of counts for which Gaussian statistics can be used).

• Lowest level suitable for occupancy: the lowest level currently lived in, or a lower level not currently used (such as a basement), that a prospective buyer could use for living space without renovations. This includes a basement that could be used regularly (for example, a recreation room, bedroom, den or playroom).

• Lowest lived-‐in level: the lowest level or floor of a home that is used regularly (for example, a recreation room, bedroom, den or playroom).

• Passive radon / radon decay product (RDP) measurement device: a radon or radon decay product measurement system in which the sampling device, detector, and measurement system do not function as a complete, integrated unit. Passive devices include electret ion chamber devices, activated-‐carbon or other adsorbent systems, or alpha-‐track devices, but do not include continuous radon/RDP monitors, or grab-‐radon/RDP measurement systems.

• Picocurie (pCi): one pCi is one-‐trillionth of a curie, 0.037 disintegrations per second, or 2.22 disintegrations per minute.

• Picocurie per liter (pCi/L): a unit of radioactivity corresponding to an average of one decay every 27 seconds in a volume of 1 liter, or 0.037 decays per second per liter of air or water. 1 pCi/L = 37 becquerels per cubic meter (Bq/m3).

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• Precision (or precision error): a measure of mutual agreement among individual measurements of the same property, usually under prescribed and similar conditions, most desirably expressed in terms of the standard deviation, but can be expressed in terms of the variance, pooled estimate of variance, range, relative percent difference, or other statistics.

• Quality assurance: a complete program designed to produce results that are valid, scientifically defensible, and of known precision, bias, and accuracy; includes planning, documentation, and quality-‐control activities.

• Quality control: the system of activities to ensure a quality product, including measurements made to ensure and monitor data quality; includes: calibrations; duplicate, blank and spiked measurements; inter-‐laboratory comparisons; and audits.

• Radon (Rn): a colorless, odorless, naturally occurring, radioactive, inert, gaseous element formed by radioactive decay of radium (Ra) atoms. The atomic number is 86. Although other isotopes of radon occur in nature, radon occurring in indoor air is primarily Rn-‐222.

• Radon chamber: an airtight enclosure in which operators can induce and control different levels of radon gas and radon decay products. Volume is such that samples can be taken without affecting the levels of either radon or its decay products within the chamber.

• Relative percent difference (RPD): a measure of precision, calculated by: RPD = (|X1 -‐ X2 |)/Xavg x 100 where: X1 = concentration observed with the first detector or equipment; X2 = concentration observed with the second detector, equipment or absolute value;

studyguide advanced radon - nachipage 7 of 488! ! whenradongasisinhaled,denselyionizingalpha...

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