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A Strang-type operator splitting is employed for the integration of the conservation laws.
The numerical integration of the conservation equations gives the flame propagation velocity for a given set of parameters.
In the present study, time integration of the conservation equations enabled the capture of the self-excited three-quarter mode of the combustor.
The time consuming numerical integration of the conservation equations is restricted to compute the transfer function (TF) for a broad range of frequencies and spherical harmonics.
Therefore, the integration of the conservation implications of intense, hot-fire suppression (i.e. removal of a potential contributing factor to natural population regulation), the welfare concerns of arson fires and burning during "hot-fire" conditions into fire management strategies for conservation areas is important.
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Flame structures, including formation of species containing two carbon atoms, are measured by gas chromatography of samples withdrawn by fine quartz probes and are calculated by numerical integrations of the conservation equations employing an updated elementary chemical-kinetic data base.
The integration of the mass conservation equation with a nonlinear equilibrium condition at the fiber wall agrees satisfactorily with the results of experiments performed at different initial concentrations of Cr VI) and different values of the linear velocity of the aqueous phase in the range C0 ⩾ 50 g/m3 and 2.95 × 10−3 m/s ⩽ v ⩽ 1.18 × 10−2 m/s.
Results of bifurcation analysis with this flow-field model and a three-step reduced chemical-kinetic scheme show excellent agreement with results of numerical integration of the full conservation equations with detailed chemistry for all degrees of dilution of the fuel feed.
On this basis, we propose a standardised panel of organisms for conservation assessment and describe integration of this conservation panel into a pathogenicity scoring system designed to assess mt-tRNA variation associated with mitochondrial disease.
The adaptation inhibits the integration of the equations of conservation of phytoplankton population and nutrient concentration.
The adaptation of the growth rate to the chemostat environment inhibits integration of the equation of conservation of phytoplankton populations, though eventually when a steady state is reached the growth rate becomes equal to the rate of flow through the chemostat.
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