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This study shows that the multiple end-members mixing model is useful to more successfully assess complex hydrogeochemical processes occurring in a salinized aquifer under freshening, as compared to the conventional interpretation using the theoretical mixing line based on only two end-members (i.e., seawater and rainwater).
The mixing model is easy to perform.
On the basis of the experimental results, a phenomenological mixing model is derived.
In this work, a novel variation of the multiple mapping conditioning (MMC) mixing model is proposed.
Here, the parameterized scalar profile (PSP) mixing model is extended to provide the required joint statistics.
In PDF methods, however, a mixing model is required to account for molecular diffusion.
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The end-member mixing model was employed for hydrograph separation.
An isotopic mixing model was employed to estimate the contributions of particulate sources.
A constant-pressure mixing model was adopted to simulate the ejector.
To study polymerization, the mixing model was combined with a kinetic model of the polymerization reaction.
The ternary mixing model was then used to describe arsenic concentrations from the PSW, which varied according to the time of year the well is sampled.
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