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These steps can be resumed in vanishing line extraction, gradient planes generation, and depth gradient assignment.
Fig. 6 Flowchart of depth values assignment Fig. 7 Six kinds of initial depth gradient hypothesis.
Along the depth gradient, strong significant correlations (P < 0.05) were found between soil As level and %OOC (R2 = 0.9785).
The structure and dynamics of four Mediterranean communities along a depth gradient (5 to 20 m depth) were investigated.
Distribution maps of Ks produced by kriging indicated a pronounced spatial pattern and demonstrated an obvious spatial depth gradient.
For the fourth sector, Karpathos-Rhodes, two distinct subsectors were defined along a depth gradient (50 90 km and 90 180 km, respectively).
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The velocity-depth gradient, which is controlled by the nonlinear exponential term in this equation, gradually decreases with increasing depth.
Our analysis indicates that the S wave velocity-depth gradient is well represented by an exponential asymptotically bounded velocity function (Ravve and Koren 2006).
where V0 is the S wave velocity at z = 0, ΔV is the increment of the S wave velocity at infinite depth, and α is the positive constant for adjusting the velocity-depth gradient.
Soil development on quite homogeneous bedrock appears essentially controlled by relief and climate, underlining the suitability of the region as a model area for in-depth gradient studies on ecosystem processes and land use.
The depth-dependent S-wave velocity function is represented by the following equation: {V}_{mathrm{S}} z)={V}_0+Delta Vleft[1- exp left -frac{alpha z}{Deleft -frac{alphat] (1)where V 0 is the S-wave velocity at the surface (z = 0), ΔV is the increment of the S-wave velocity at infinite depth, and α is the positive constant that determines the velocity-depth gradient.
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