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(iii) Overall, the Slab model simulated a relatively cooler surface and a shallower boundary layer.
Each laboratory model simulated a granular shoulder supported on soft subgrade with geogrid reinforcement at the interface between both layers.
The old model simulated a shallower oil water contact (OWC) and a small oil pool as seen in the comparison between old and new model in Fig. 18.
The model simulated a decrease in global tropospheric O3 mass by ~5%% due to heterogeneous reactions, and implied that the most important heterogeneous reaction was the uptake of HNO3 on the dust surface.
The previous in silico model simulated a similar pattern of plasticity changes during learning, but did not matched up with the gene increment values measured in the mPFC.
Each run of the model simulated a cohort of 10,000 patients.
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At these light-limited sites, the model simulated an unexpectedly (and unrealistic) low perennial fractional cover (MA,p) of 0.28 0.29 for TUM and 0.24 0.25 for CT.
The model simulates a flow of lava from this new vent location onto the surrounding topography.
The model simulates a peak discharge and a runoff volume reduction of more than 40%.
The model simulates a virtual diverse agro-ecosystem with four ecological agents.
First, a mathematical model simulating a time-dependent electrochemical process is developed.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com