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The subtrough depth (depletion value) as function of local time (evening night hours) was compared with the vertical plasma drift velocity variations, obtained for the same periods from the AE-E satellite and IS radar (Jicamarca) data.
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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).
Balancing the number of monomers on the perimeter with the number removed from within the depletion depth layer yields an estimate of d = (8/(π ac))1/2 for the depletion depth.
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.
Their dependence on UV intensity in air is explained by means of photoinduced surface depletion depth decrease caused by oxygen desorption induced by photogenerated holes.
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.
Depth to iron depletion (p = 0.0055) was significantly greater and soil carbon (p < 0.0001) was significantly lower in Bed and D/B treatments due to bed elevation above the water table and improved drainage.
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.
Accordingly, the volume density N BT of the buffer trap can be obtained by dividing the sheet density by Debye length ( {L}_D=sqrt{kT{varepsilon}_S{varepsilon}_0/left({q}^2{N}_Dright)} ) as the depletion depth being in the same order of magnitude or smaller than the Debye length [28].
The measured sulfate reduction rates cannot account for the shallow sulfate depletion depth: a 1-D, steady-state, reaction-transport model for sulfate using measured rates predicts that sulfate penetrates to >15 cm (Figure S1).
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