The original unit for measuring the amount of radioactivity was the curie (Ci)-first defined to correspond to one gram of radium-226 and more recently defined as:
1 curie = 3.7x1010 radioactive decays per second[exactly].
In the International System of Units (SI) the curie has been replaced by the becquerel (Bq), where
1 becquerel = 1 radioactive decay per second = 2.703x10-11 Ci.
The magnitude of radiation exposures is specified in terms of the radiation dose. There are two important categories of dose:
The biological impact is specified by the dose equivalentH, which is the product of the absorbed dose D and the quality factor Q: H = Q D.
The unit for the dose equivalent is the rem if the absorbed dose is in rads and the sievert (Sv) if the absorbed dose is in grays. Thus, 1 Sv = 100 rem. As discussed below, 1 rem is roughly the average dose received in 3 years of exposure to natural radiation. 1 Sv is at the bottom of the range of doses that, if received over a short period of time, are likely to cause noticeable symptoms of radiation sickness.
The dose equivalent is still not the whole story. If only part of the body is irradiated, the dose must be discounted with an appropriate weighting factor if it is to reflect overall risk. The discounted dose is termed the effective dose equivalent or just the effective dose, expressed in rems or sieverts.
Instruments called Radiacs. There are many kinds of Radiacs, depending on the purpose they are used for. Everything from Geiger counters for instant readings of dose rate to Ionization Chambers to Dosimeters like pen and film-badge dosimeters which are to be read later for keeping individual exposure records.
to measure radioactivity and to make maps
Yes, satellites equipped with sensors can measure radioactivity levels from a remote distance. These sensors can detect gamma rays emitted by radioactive materials on Earth's surface and provide valuable data for monitoring environmental radioactivity levels.
Geiger-Muller counter, scintillation detector, ionization chamber, and Cherenkov detector are common instruments used to detect and measure radioactivity. Each has its own mechanism for detecting the presence of ionizing radiation and measuring its intensity.
The derived SI unit of radioactivity named after a French physicist is the becquerel, symbolized as Bq. It is used to measure the rate of radioactive decay in a substance, with 1 becquerel equaling 1 decay per second. The unit honors Henri Becquerel, who discovered radioactivity in 1896.
no but she built the knowleage of radioactivity.
You cannot measure radioactivity in litres
radioactivity
With a Geiger counter.
A geiger counter measures radioactivity.
to measure radioactivity and to make maps
The isotope 22Na is radioactive but the concentration is extremely low. A measure of the radioactivity is not necessary.
The mass is measured with a balance.The radioactivity is measured with a gamma-radiometer.
Yes, satellites equipped with sensors can measure radioactivity levels from a remote distance. These sensors can detect gamma rays emitted by radioactive materials on Earth's surface and provide valuable data for monitoring environmental radioactivity levels.
Geiger-Muller counter, scintillation detector, ionization chamber, and Cherenkov detector are common instruments used to detect and measure radioactivity. Each has its own mechanism for detecting the presence of ionizing radiation and measuring its intensity.
Devices such as Geiger counters, scintillation detectors, and ionization chambers are commonly used to detect radioactivity. These devices can detect the presence and measure the strength of radiation from radioactive materials.
pH meter to measure the acidityruler or caliper for linear dimensionstape measure for the circumferencescale for the masscolorimeter for the hue or colorthermometer for the temperatureGeiger meter for the radioactivity...
Short answer: Yes, through observation you can tell what happens in a given interval of time.Long answer: It is not possible to measure everythingthat happens in a given interval of time, but only atomic (individual) changes. For instance, if you wanted to measure radioactive decay over a period of time, you would measure the amount of radioactivity at a starting point, measure a set amount of time passing then measure the level of radioactivity at the end. Subtracting the last measured radioactivity from the initial measurement will give you the amount of radioactive decay. In a simpler example, you could measure your height on January 1st of 2012, then again on January 1st of 2013 to see how your height has changed over the course of one year.