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The celestite precipitate was primarily localized in a ~0.35 mm wide disk-shaped precipitation front surrounded by small areas of disperse precipitation in approximately the middle of the diffusion cell.
The porosity and petro-physical properties of the compacted sand were determined with mercury intrusion porosimetry (MIP, before the formation of a precipitation front) and µ-CT (before and after the formation of a precipitation front).
Under both resolutions, the precipitation front could be clearly distinguished from the sand grains and water-filled pore space.
A separate imaging procedure was applied to one of the data sets (Prec1) obtained with µ-CT on the celestite precipitation front.
The heterogeneity created by the precipitation front has a very strong influence on the transport parameters, despite the fact that the remaining porosity is fully connected.
This observation is in good agreement with the steady-state through-diffusion HTO data observed after the formation of the precipitation front.
Similar(40)
Sharp fronts are usual in the ground and typical examples are redox fronts and dissolution and precipitation fronts.
However, slight differences can be observed between the two codes, especially when concentration discontinuities are involved, such as precipitation fronts or changes in boundary conditions.
Simulations reveal that the structure and steady-state growth velocity of spatially periodic precipitation fronts depend strongly on the relative magnitudes of the diffusion coefficients.
4. Create a journalist's weather dictionary that defines various types of storms and other weather related terms, and provides general information about weather conditions that reporters might need to know. 5. Map and graph weather patterns (temperature, precipitation, storm fronts, wind data, etc).
Warm-front precipitation is generally much more uniform and widespread than that associated with cold fronts.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com