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We also propose a particles-interaction mixing model using a mixing volume concept, in which the mixing timescale is determined by relating the decay of scalar variance in the mixing volume to the scalar dissipation rate.
We were not able to use a three source mixing model using wrack detritus or POM because their isotopic signatures overlapped with either supralittoral vegetation or marine macroalgae (T. Romanuk, unpublished data; for a discussion of carbon sources in Howe Sound see [12]).
A two-member mixing model using nitrate, chloride and specific conductance was used to distinguish rainwater versus groundwater inputs.
A two-component mixing model using chloride as a conservative tracer indicated that shallow groundwater in seep areas was primarily (53 75%) comprised of water from a shallow fractured aquifer, which had elevated NO3-N concentrations (5.7 mg L−1).
A mixing model, using δ(202 Hg values and Hg concentrations, yielded estimates of the relative contributions of coal ash, Clinch River, and Emory River sediments for a suite of 71 sediment samples taken over a 30 month time period from 13 locations.
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These results deviated from the predictions of theoretical simple mixing model used.
The mixing model uses the same set of terrestrial and marine basal sources to calculate the relative proportions of terrestrial and marine carbon in the muscle tissue of chum salmon fry, thus the proportions of TC are qualitatively the same as those reported for δ13C.
To quantitatively assess the hydrogeochemical processes, the end-member mixing analysis (EMMA) and the forward mixing modeling using PHREEQC code were conducted.
We used these intersection points in simple mixing models using H isotopes.
A specific objective is to assess the vessel mixing models used in system codes.
Most mixing models used in probability density and filtered density methods, however, are based on non-reactive scalars.
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