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If the basalt activity spans ~6 Myr, the instantaneous volcanic flux would be on the order of 0.1 km3/year or less, being too small to have a significant environmental impact.
Figure 12 shows block scheme of calculation for State I. Using Eq. 14 it is found that the maximum permeate flux would be obtained at the flow rate of 6.75 L min−1.
It was found that the surface temperature along the pipe surface for the same heat flux would be higher for a circular restriction with length of 120 cm and would be smaller for a bell mouth restriction.
In this picture, the key role of arsenic flux would be the reactivation of dissolution of the GaAs substrate by the metallic Ga droplets and further GaAs growth, processes that are also in the origin of the well-known flat depressions beneath the Ga droplets in the absence of an arsenic flux.
Because it seems natural that radionuclide emission flux would be proportional to surface pollution density, there could be radioCs fluxes several orders of magnitude higher than those measured in Tsukuba in areas nearer the FDNPP site whose Cs surface pollution is several orders of magnitude higher than in Tsukuba.
A drastic reduction of the daily fluctuation of the quasi-steady-state heat flux would be possible by using a broad range of heavier walls, something which can be quantified by the introduction of a dimensionless quantity defined as wall damping-out efficiency.
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Moreover, Shiau et al. (2012) proposed that the detritus fluxes would be influenced by regional precipitation in addition to sea level or ice volume change in the area, and also, they suggested that the terrestrial detritus coming from the Papuan Peninsula would contribute a lot to the core site in colder periods based on the 230Th-nomalized analysis.
Estimates of day and night-time degradation rates combined with assessment of the daily in-stream residence time suggest that derived fluxes would be overestimated by up to 19% when diurnal variation was considered due to the highest concentrations of DOC and highest flows being in winter when day lengths are shortest.
We observed that a unique estimation of all four fluxes would be possible only if the mass isotopomers of sedoheptulose 7-phosphate were additionally measured.
The overall small dry season fluxes would be more prone to measurement errors compared to the stronger signal during the wet season.
One recent study has proposed that natural (i.e., pre-HF) upward brine fluxes in the Appalachian Basin are 0.0031 to 6.7 m year−1 and that upward HF fluid fluxes would be even higher (Myers 2012).
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