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The complex lithology neutron-density model for mineral analysis, porosity estimation and saturation calculation is shown in Fig. 13.
Kong (2005) has proposed a decision-making model for mineral resources by a fuzzy method using MADM theory.
This paper developed a new model for mineral fillers wicking a probe liquid; this model established a relationship among the mass of the wicked liquid, the wicking time and the spreading pressure of the probe liquid on the mineral fillers.
This paper presents a study of the development of a fiction force model for mineral oil basestock containing palm olein, and antiwear amine phosphate as additive, tested on a four-ball tribotester.
In this paper, the design of the experimental cells along with observations on gas composition, gas pressure, soil temperature, volumetric water content and mineral composition are presented with the objective to better understand the mineral carbonation processes under natural conditions and to propose a conceptual model for mineral carbonation at the field cell scale.
Our aims were to identify genes coding for ion transporters that are upregulated in the uterine portion of the oviduct during eggshell calcification, compared to other tissues and other physiological states, and incorporate these proteins into a general model for mineral transfer across the tubular gland cells during eggshell formation.
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Solid liquid phase kinetic reaction models for mineral dissolution in acidic solutions mainly include first-order reaction models, interfacial reaction models, and capacity models (Zhong 2006).
Second, thermodynamic models for mineral stability and solubility can only be accurately constructed from experimental data if correct speciations are known.
As peat differs in several aspects from mineral soils, the applicability of standard hydraulic functions (e.g. van Genuchten Mualem model) developed for mineral soils to peat soil moisture dynamics might be questionable.
For the underlying model description, we resort to a non-linear Neo Hookean model for the mineral and to the Arruda Boyce model for the protein, in combination with a cohesive zone approach.
Here empirical models for calculating self-diffusion coefficients and diffusion matrices are combined with MELTS, a thermodynamic model for silicate minerals and melts, to estimate diffusive dissolution rates, interface melt compositions and melt diffusivities.
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