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After fibers can no longer be placed on a given plane, we proceed to the next plane, and this procedure is continued until the desired grammage is attained.
Rock failure occurs when the shear stress on a given plane within the rock reaches a critical value; tau_{hbox{max} } = S_{o} + sigma^{prime}tan phi (40).
The addition of radiation scattered from clouds requires knowledge of the distribution and type of clouds, and the accuracy with which a calculation of the scattered flux on a given plane can be made is rather limited.
In fact, when the Internet service on a given plane is not up to the task- we tend to find it annoying.
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These stats are not all drawn from the same sources, but assuming they're all roughly commensurate, you'd be about 1.5 times more likely to be killed by a terrorist attack on any given plane flight than to be killed in a car crash any given time you step into an car.Needless to say, on any given trip, either event is extremely unlikely.
Such oscillations result in varying fractions of slip on a given {1 1 1} plane, resulting in varying degrees of interaction between the two sets of non-coplanar microbands.
The ΔCFF is defined as (1 where Δτ is the shear stress change resolved on a given failure plane (assumed to have a positive value in the fault slip direction); Δσ is the normal stress change (assumed to have a positive value in the compressive direction); μ′ is the effective coefficient of friction, defined by μ′ = μ(1 − B).
The ΔCFF is defined as ΔCFF = Δτ − μ′Δσ, where Δτ is the shear stress changes resolved on a given failure plane (defined as positive in the fault slip direction), Δσ is the normal stress changes (defined as positive in the compressive direction), and μ′ the effective coefficient of friction.
The ΔCFF is defined as ΔCFF = Δτ − μ′Δσ, where Δτ is the shear stress change on a given failure plane (assumed to be positive in the fault-slip direction), Δσ is the normal stress change (assumed to be positive in the compressive direction), and μ′ is the apparent coefficient of friction.
ΔCFF is computed using the following equation, with simplifying assumptions to account for pore pressure effects (King et al., 1994) (1 where Δτ is the shear stress change on a given fault plane (positive in the direction of fault slip), Δσ is the fault-normal stress change (positive when unclamped), and μ′ is the effective coefficient of friction.
Directional anisotropy refers to a difference in diffusion mechanism or rate in a particular direction on a given crystallographic plane.
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CEO of Professional Science Editing for Scientists @ prosciediting.com