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Both simulations well support experimental observation.
The simulations well reproduce the slow segregation of the phases and the deformation of the droplet.
Results show that the reactive solute dispersion developed by the Lagrangian model matches the ensemble average of numerical simulations well.
The tsunami simulations well explain the observed tsunami arrival times, polarities of initial wave, and maximum amplitudes obtained by deep-ocean pressure measurements.
If a viscoelastic crustal model is sufficiently realistic and the simulations well compare with the observed data, the crustal model can be refined.
The tsunami simulations well explain the observed tsunami arrival times, maximum amplitudes, and polarities of initial wave observed at the deep ocean-bottom stations.
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Intersection of the reservoir wells with the model and output simulation well data.
Intersection of the reservoir wells with the model and output simulation well data Output the production data in the form of simulations and link to wells.
In all the cases of IBO examined, it is observed that the exact one and simulation well agree.
In addition, numerical simulations were conducted to reveal the feature of temperature fields during cementing through a simulation well.
The WRF simulation well reproduced a vertical structure of a radiosonde observation at the Kushiro station (dashed lines in Fig. 3a).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com