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Rad (radiation unit)

physical science Maturity 11-13 Next article →

The rad is a specific unit used to measure an absorbed radiation dose. An absorbed dose describes the amount of energy that a substance takes in from radiation. This substance can be anything, including air, water, or human tissue. In modern science, the rad has been largely replaced by the gray (Gy), which is the official SI derived unit. However, the rad remains a common industry standard in the United States. One rad is mathematically equivalent to 0.01 Gy or 0.01 J/kg. Understanding these measurements is vital for safety in medicine and industry.

To understand how the rad works, we must look at the energy transfer process. When radiation passes through matter, it deposits energy into that matter. The rad quantifies this energy deposition. Originally, in 1953, the unit was defined using CGS units. It represented the amount of energy that caused 100 ergs to be absorbed by exactly one gram of matter. This measurement focuses on the energy absorbed rather than the charge of the radiation. Because different materials absorb energy differently, the dose depends on what is being hit.

Radiation doses affect living things in various stages and ways. Small doses can cause subtle changes. For instance, a dose of 25 rad is the lowest level known to cause clinically observable changes in blood. A higher local dose of 200 rad can cause erythema, which is redness of the skin in humans. If a person receives 100 to 200 rad to their entire body in less than a day, they may develop acute radiation syndrome (ARS). This is a serious condition, though it is usually not fatal at those levels. Higher doses are much more dangerous.

As the dose increases, the medical prognosis becomes much worse. Doses between 200 and 1,000 rad delivered within a few hours can cause serious illness. At the higher end of that range, the prognosis is poor. If a person receives a whole-body dose of more than 1,000 rad, it is almost invariably fatal. Scientists use the term LD50 to describe a dose that is fatal to 50% of a population, which is 400 rad for whole-body acute radiation syndrome in humans. The LD100, or the dose that is fatal to 100% of the population, is 1 krad.

History shows how our measurement of radiation has evolved. In the 1930s, the roentgen was the primary unit for radiation exposure. However, the roentgen is now obsolete and lacks a clear definition. In 1940, British physicist Louis Harold Gray, along with William Valentine Mayneord and John Read, proposed a new direction. They suggested the "gram roentgen" (gr) to measure energy increments in tissue. This marked a major shift from measuring charge to measuring energy. Later, in 1945, Herbert Parker introduced the Röntgen equivalent physical (rep) to measure absorbed energy in tissue before biological factors were considered.

The transition to modern units was a long process. The International Commission on Radiological Protection (ICRP) recommended the rad in 1953. By the 1970s, they promoted switching to the gray. While the International Committee for Weights and Measures (CIPM) does not accept the rad, the United States NIST provides its own interpretations. NIST allows the rad for use in the U.S. alongside the SI system. In medical settings like radiotherapy, professionals often use the centigray (cGy), which is a submultiple of the gray, to report absorbed doses.

Different technologies also have different radiation tolerances. While humans are very sensitive to radiation, machines can be much tougher. For example, ordinary microchips have a specific tolerance level. However, "radiation-hardened" microchips are designed to withstand much higher levels, such as 1 Mrad. This comparison shows the massive difference between biological limits and engineered limits. In 1964, a criticality accident at Wood River Junction resulted in a fatal whole-body dose of 10 krad. This event highlights the extreme scales involved in radiation science.

Finally, it is important to distinguish between absorbed dose and effective dose. The absorbed dose, measured in rads, tells us the energy in the tissue. However, the International Commission on Radiological Protection uses a model to calculate effective dose, measured in rem. The rem is better for calculating stochastic risk, which refers to long-term health risks. In power plant scenarios involving X-rays or gamma rays, 1 rad of absorbed dose usually equals 1 rem of effective dose. In other complex situations, the effective dose in rem might be thirty times higher or thousands of times lower than the absorbed dose in rad.

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