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"Fluid is distributed across the forehead," Mr. Geller explains in his patent.
The Hashin-Shtrikman upper bound (HS+) and cube models are applicable to cases in which fluid is distributed along the grain boundaries and triple junctions.
A common configuration of a catalytic packed-bed reactor is that of vertical down-flow in which the fluid is distributed uniformly at the top of the reactor and reacts on the catalyst particles as it moves down.
In particular, in the region of Chubu and west Hokkaido, the value is up to ∼ 0.1, which indicates that the pore geometry is near equidimensional, and the fluid is distributed in the spaces between the grains (Waff and Bulau 1979; Takei 2002).
The chemical properties of the vapor and brine phases are quite different from each other and from their parent fluid, because each of the chemical species in the parent fluid is distributed preferentially into the vapor and liquid phases according to their physical and chemical properties during phase separation (Butterfield et al. 2003; Foustoukos and Seyfried 2007).
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Fluid was distributed more slowly to vt in the two treatment groups.
Yet, it remains difficult to determine how subsurface fluids are distributed in heterogeneous rock and soil formations, how fast they flow, how effectively they transport dissolved and suspended materials, and how they are affected by chemical and thermal exchange with the host formations.
In our study, we were able to show that the CO2 fluids are distributed in the region up to 10 to 15 km from the Shinya-Narashi fault (W3, W4, W5, and E3; Figure 3).
Although this scenario cannot be ruled out, it is difficult to explain by decarbonation reactions why CO2-bearing fluids are distributed only in the south of the Murotohanto subbelt.
In the Tokai area, high-pressure fluids are distributed along the subducting plate boundary and are centered around the depth of the Moho (~30 km) (Kodaira et al., 2004; Kato et al., 2010).
The CO2 fluids are distributed preferentially near an out-of-sequence thrust that brings the Murotohanto subbelt into contact with the late Oligocene-early Miocene Nabae subbelt and its many volcanic and intrusive rocks.
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