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As a result, the net mass change is much smaller in TEABF4 electrolyte.
And the change of the sloshing modeling design variables according to the fluid mass change is also analyzed.
Note that this mass change is much smaller than the 1200 MT value quoted in Allis et al. (2001) for the Geysers geothermal reservoir in several years leading to several hundreds of μGal gravity changes.
While the measured mass change is consistent with the expected value, each Tl ion seems to contribute approximately two charges upon adsorption before the completion of the first UPD layer instead of one.
REF (g) Aged (g) Mass depletion V depletiona Porosity changeb Leached portlandite (g c Porosity changed W/C = 0.48 927 881 46.00 20.81 5.3 44.4 5.12 W/C = 0.62 907 878 29.00 31.12 3.3 29.6 3.41 aCalculated assuming that total mass change is attributed to Portlandite depletion (V depletion = mass change/Portlandite density).
It has been demonstrated that the shift in the amplitude ratio of the coupled-resonators at the in-phase mode-frequency, in response to a mass change, is five orders of magnitude greater than the equivalent resonant frequency shift of a single resonator device.
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Spatial variations in volume and mass change are observed.
Mass change was used to establish the kinetics of corrosion.
To support conclusions from FTIR spectra, mass change was investigated with temperature by TGA (Figure 3b).
Models of volume and mass change are constructed for three time periods of catchment evolution.
The factors affecting the material mass change were identified using an experimental design analysis.
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