radiogenic isotope sentence in Hindi
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- Radiogenic isotopes provide powerful tracers for studying the ages and origins of Earth systems.
- Stable isotope tracers involve only non-radiogenic isotopes and usually are mass-dependent.
- Isotopic tracers are usually subdivided into two categories : stable isotope tracers and radiogenic isotope tracers.
- It also suggests that this temperature means that the concentration of radiogenic isotopes is greater than within the earth.
- Radiogenic isotope tracers are most powerful when used together with other tracers : The more tracers used, the more control on mixing processes.
- Many radiogenic isotope measurements are made by ionization of a solid source, whereas stable isotope measurements of light elements ( e . g.
- Because their abundances are normally quoted as activity ratios rather than atomic ratios, they are best considered separately from the other radiogenic isotope systems.
- These decay-products are termed radiogenic isotopes, in order to distinguish them from the much larger group of'non-radiogenic'isotopes.
- They are particularly useful to understand mixing processes between different components, because ( heavy ) radiogenic isotope ratios are not usually fractionated by chemical processes.
- U-series isotopes are unique amongst radiogenic isotopes because, being in the U-series decay chains, they are both radiogenic and radioactive.
- An alternative approach used to measure the relative abundance of radiogenic isotopes when working with a solid surface is secondary-ion mass spectrometry ( SIMS ).
- Thus, the ratio of the daughter to non-radiogenic isotope will become larger with time, while the ratio of parent to daughter will become smaller.
- Stable isotope geochemistry is largely concerned with isotopic variations arising from mass-dependent isotope fractionation, whereas radiogenic isotope geochemistry is concerned with the products of natural radioactivity.
- On the other hand, radiogenic isotope analysis involves measuring the abundances of decay-products of natural radioactivity, and is used in most long-lived radiometric dating methods.
- As time goes on, some amount of the parent decays into the radiogenic isotope of the daughter, increasing the ratio of the concentration of the radiogenic isotope to that of the daughter.
- As time goes on, some amount of the parent decays into the radiogenic isotope of the daughter, increasing the ratio of the concentration of the radiogenic isotope to that of the daughter.
- Since the ratio of the daughter and non-radiogenic isotopes is proportional to the ratio of the parent and non-radiogenic isotopes, the slope of the isochron gets steeper with time.
- Since the ratio of the daughter and non-radiogenic isotopes is proportional to the ratio of the parent and non-radiogenic isotopes, the slope of the isochron gets steeper with time.
- Clayton's first papers using that idea in 1975 pictured an interstellar medium populated with supernova grains that are rich in the radiogenic isotopes of Ne and Xe that had defined the extinct radioactivities.
- *Refers to radiogenic isotopes, Where t is the required age, ? 238 = 1.55125 x 10 " 10 and ? 235 = 9.8485 x 10 " 10
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