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The main factors that significantly increased soil hydrophobicity were depth and parent material.
These layers were depth of groundwater level, hydraulic conductivity, slope percentage, soil, and land use land cover (LULC).
These were DEPTH, GISA, DataFurnace (NDF), RBX, RUMP, SIMNRA (all analytical codes) and MCERD (a Monte Carlo code).
We found that the important environmental variables were depth and Ub, while no effect of slope was found.
The cone specimen parameters examined by the pathologists were depth and width of invasion, lymph-vascular space invasion (LVSI) and surgical margins status.
After nitrogen implantation, samples were depth profiled by AES (Auger Electron Spectrometry) to confirm the depth distribution of the implanted nitrogen ions.
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The machining parameters under investigation were depth-of-cut, feed rate, surface cutting speed, tool radius, tool rake angle and side rake angle, and cutting fluid.
As with AvTD, latitudinal trends in VarTD were depth-specific.
Latitudinal trends in AvTD were somewhat weaker and were depth-specific.
The receiver functions were depth-converted using the 1D velocity model IASP91 (Kennett and Engdahl, 1991), to be consistent with the PRFs, but also because it effectively represents the continental lithosphere.
Both Si/TiD y /Pd samples, taken prior to and after annealing were depth-profiled using XPS analysis to reveal the Pd, Ti, and Si bulk distribution within both films.
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