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For example, the tonnage of copper in El Teniente porphyry Cu Mo mine is at least 31.5 million tonnes.[24] Therefore, a total mass of fluids of ~1017 grams may be reasonable.
It was found that the mean drop size is better correlated to the maximum turbulence energy dissipation rate than to either the average power input per unit mass of fluids, or the tip speed of the impeller.
Consequently, based on the estimated total mass of fluids involved in these two deposits, we assume that the total mass of fluid involved in the formation of a typical W Mo skarn system should be in the neighborhood of ~2 × 1014 grams.
In order to estimate the total mass of fluids involved in the formation of a typical skarn tungsten molybdenum system, the calculated scheelite solubility (39 ppm) in 1.0 mol NaCl solution at 600°C and 2000 bar of Wood and Samson[31] is used.
Previous correlations have focused on the relationship between the mean drop size and the physical properties of the fluids (interfacial tension, density and viscosity), the volume fraction of the dispersed phase and the average power input per unit mass of fluids.
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Therefore, the estimated total mass of fluid involved should be ~1.3 × 1014 grams.
Possible reasons of the oscillations are closed-loop system of the scanner and high mass of fluid cell loaded on the scanner.
The total mass of fluid involved should be ~3.0 × 1014 grams according to the solubility of scheelite cited above, assuming that all the tungsten in the fluid is deposited.
The physical mechanism for the above phenomena is that a large K indicates a thinner EDL, then the region of bulk flow (mass flow) becomes wider, which results in more mass of fluid through the pipe during the same period.
A fluid-loading parameter ε, defined as the ratio of mass of fluid to mass of the structure per unit area, is introduced which when set to zero yields the uncoupled dispersion equation.
When the rotation is a fixed axis with constant angular velocity, Chanillo and Li [3] obtained a priori bound for the support of the relative equilibrium form of a homogeneous, gravitating, and compressible mass of fluid.
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