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In geology, where long time scales often are considered, rocks are dated by using decay series like A (parent isotope) → B (daughter isotope), where element A has a very long half-life.
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This may be improved further by using a decaying substrate feeding strategy (Maclean et al. 2008).
By using LAPM, a power series solution is essentially a truncated series solution.
So eventually we decided that it was necessary to do a full analysis of how the Λb decayed by using a quantum mechanical description of the decay that used all the information in the decay besides the J/ψ p mass.
Also, we have obtained photoluminescence (PL) decay curves by using time-resolved spectroscopy and extracted PL decay time constants by fitting the decay curves with multi-exponential decay functions.
The carrier lifetime was measured by using open circuit voltage decay technique.
Furthermore, we show that the solution is exponentially decay by using the Liapunov function method.
In Section 5, we investigate the decay property of Young measure solutions and get a decay rate estimate by using Nakao's lemma.
The measured counts were normalized to an activity of 1 MBq by using the dose calibrator activity measurement for each series, decay-corrected to the time of the scans.
These devices work by using the heat energy released by decaying plutonium atoms to generate precise amounts of electricity.
Decay rates were estimated by using the litterbag method.
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CEO of Professional Science Editing for Scientists @ prosciediting.com