The purpose of this paper is to validate the model for the selection of the optimal power cable conductor cross section presented in the IEC Standard 60287-3-2.
The geological layers considered in this work are slightly adapted from the idealized cross section presented in the paper of [Guillou-Frottier (2011]) and inspired by the contribution of [Genter et al. (1997]) and [Genter and Traineau (1992]).
In the representative MT cross sections presented in this paper, low-resistivity geophysical anomalies exist between high-resistivity basaltic zones.
Figure 9 shows a schematic map of the top and base of the Lochkovian succession based on the conceptual geological cross sections presented by Schintgen et al. (2015).
The method of measuring neutron induced charged particle emission cross sections presented here can be expanded to more isotopes of interest to reactor engineers or astrophysicists, as well as to (n,p) reactions.
The direct deposition of coatings with a variable cross-section presents a challenge for the use of physical vapor deposition technology.
The painting on copper is somewhat deviant as the cross-section presents a single preparation layer with mainly lead white, charcoal black and earth pigments.
The vertical cross-section presents histology-like images for diagnosis and quantitative studies of early cancer development.
Black solid lines show the cross-sections presented in Fig. 3, and dashed blue curve shows the current plate boundary (e.g., DeMets et al. 1990).
The thin dashed line represents the position of a cross-section presented by Hirose et al. (2008), which is shown in Fig. 5(b).
