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A recently developed chemical osmosis flow continuum model has been used to design the osmosis experiment, and to interpret the water pressure measurements.
Fractional differential equations have been found to be appropriate models for certain phenomena in astro-physics, fractal networks, signal processing, chaotic dynamics, turbulent flow, continuum mechanics, and wave propagation [1 7].
Samples taken in the Burdekin River did not cover all flow conditions, but large flows out of the Burdekin tend to flow above median conditions (> 75%) for several days during wet season sampling, making it difficult to sample along a flow continuum.
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At his prompting, the set list, which hardly changed from night to night, becomes a flowing continuum, one song morphing into the next.
To assess the applicability of the dual flowing continuum, we investigate how the model behaves with respect to its parameters.
A previous work inverting without any prior geostatistical assumption the same set of data based on a single flowing continuum produced nicely structured (spatially correlated) parameter fields.
The concept of dual flowing continuum is a promising approach for modeling solute transport in porous media that includes biofilm phases.
Tracer tests in large laboratory columns using both conservative (fluorescein) and biodegradable (nitrate) solutes are simulated by means of a dual flowing continuum approach.
However, the dual flowing continuum suffers from intrinsic equifinality in the sense that the outlet solute concentration can be the result of several parameter sets of the two flowing phases.
We also show that the behavior of the dual flowing continuum is mainly controlled by the relative fractions of flow passing in each phase and the rate of mass transfer between phases.
Even though the concept of dual flowing continuum appears promising for simulating transport in complex porous media, its inversion onto experimental data really benefits from attempts with simpler models providing a rough pre-evaluation of parameters such as porosity and mean fluid velocity in the system.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com