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Exact(19)
This approximation is valid for.
The last approximation is valid for small.
This approximation is valid for values of situated in the neighborhood of.
This approximation is valid for geological formations whose lateral dimensions are large compared to their thickness.
The extended LDF approximation is valid for both long and short times upon step changes.
This approximation is valid for moderate to high dimensionless fracture conductivity.
Similar(41)
We focus on the evolution of plasma bulk flows, and the MHD approximations are valid for these macroscopic phenomena.
Approximations are valid for both predetermined total flux, when explicit method results, and equivalently when total fluxes must be iterated.
More quantitatively both approximations are valid for the parameter u = RgQ smaller or larger than 1, u representing the product of radius of gyration Rg and scattering vector Q (defined below).
Such approximation is valid only for relatively small values of the argument (pressure P in this case), If for experimental data notable distortion from such simple relation appears one should use the functional, experimental form (preferably).
For example, the simple model of eq 10.4 indicates that this approximation is valid when V ≫ Eμ for all relevant proton levels.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com