Sentence examples for depth of depletion from inspiring English sources

The analytical functions deduced for Δp(D,ε) and W(D,ε) predict a reduction of the range and depth of depletion interaction by an increase in the attraction strength |ε|.

The magnitude of band bending is given by the electrostatic potential φ z) = −ne z − d 2/2ε, where the depth of depletion layer d = (2εφ0/ne)1/2, the z-axis is perpendicular to the surface, ε is the dielectric constant, and φ0 is the magnitude of the electrostatic potential at the surface (z = 0).

The depth dependence of resolution is found to be consistent with the depth dependence of depletion efficiency, suggesting resolution is limited by STED laser propagation through turbid tissue.

The simulations indicated that soil water decreased within 1.0 4.0 m profiles and that the depth of water depletion deepened with plant growth after vegetative restoration.

The width and depth of the depletion layer depends strongly on the molecular weight of the matrix polymer and cannot be simply explained in terms of simple diffusion of the functionalized chains.

The depth of cartilage depletion was determined by measuring to the "tideline" created by the absence of Safranin O fast green or toluidine blue staining, and a percentage relative to the total cartilage depth was generated.

In this case eq 4 can be written as 5 Since the diffusive flux of monomers onto the crystal edge is driven by the concentration gradient, we set F = Dc/ d, where D is the diffusion coefficient, c is the protein concentration, and d is the depth of the depletion layer characterizing the concentration gradient.

Haga et al. (2005) have shown that a depletion depth of a maximum of 1.25 mm can be expected after 100 days of a natural immersion test.

Polybaric melting, due to adiabatic decompression of upwelling mantle, would leave a residual mantle in which the degree of depletion decreases with depth.

Consequently, we propose that the chemical difference between the abyssal and the SiO2-rich cratonic peridotites are due to different water contents and the depth of melting during their melt depletion histories.

In wetland sediments, there is a zone of depletion in the top10 cm and a zone of accumulation at depths from 10to2525 cm.