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Comparison of the estimated and measured decay rates showed reasonable agreement.
A mono-exponential function was fitted to the measured, decay corrected time-activity data for each kidney, with a mean fit of R2 of 0.94 ± 0.13 (SD).
So far, the measured decay rates generally match expectations, but the statistical uncertainties are too large to say anything conclusive, physicists working with the gargantuan particle detectors known as ATLAS and CMS reported today at a conference in Tokyo.
For the 2011 Tohoku tsunami, the measured decay rates (Rabinovich et al. 2013) are 17.0 to 19.0 h and 21.3 to 25.0 h at wave periods 6 to 20 min and 20 to 60 min, respectively.
This essentially involves performing a numerical inverse Laplace transform of the measured decay I t) which can be written as g k = 1 2 πi ∫ Br exp - kt I t dt (4).
As discussed in the section 'IGW attenuation' below, comparison with observed tsunami decay rates (Rabinovich et al. 2013) shows that the decay rate predicted by Equation (7) is smaller than measured decay rates.
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The monoexponential fits gave satisfactory results for all measured decays.
The FWHM of the IRF is approximately 40 ps and was de-convoluted from the measured decays with commercial decay analysis software (PicoQuant Fluofit, PicoQuant GmbH, Berlin Germany).
Successive scrolling through 2 dimensional slices (each 1.2 mm thick in the axial images) permitted identification of a pixel of maximum measured decay-corrected uptake, termed the standardized uptake value, or SUV max.
It is a general purpose detector optimized to measure decay products of BB̄ pairs created at the Y(4S) resonance.
In order to investigate the wavelength dependence of the decay rates, we measured PL decay curves in a whole emission wavelength range.
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