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The design of ground source heat pump systems requires values for the ground thermal conductivity and the borehole thermal resistance.
A number of properties have been considered including the dissociation energy Do, well depth De, equilibrium bond length re, vibrational constants (ωe, ωexe) and rotational constants (Be, αe) and these properties have been compared with the experimental values for the ground state diatomics.
From the cross-validation within each of the five groups of scenes, the optimal values for the ground thresholds were proved to correspond to the distance between the floor and the first step of the stairs for the lower sub-image classifier.
Single point values for the ground temperature are calculated, between the trenches on the axis of symmetry at the average depth of the system (0.0; −1.5 m) and on an undisturbed point, 10 m far from the exchanger (14.0; −1.5 m).
A structural analysis of modeled short-range ordered crystals as well as the values for the ground state energy of various L12-based superstructures suggest that at low temperatures the D023 structure is more stable for stoichiometric Cu3Al than any of the long-period L12-based superstructures observed at higher temperatures.
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A new charging function according to the extended GTCS model is calculated, as well as the value of the ground reflection coefficient for both analyzed strokes.
Finally, the extreme values of a DM are plotted against the corresponding value of the ground motion IM for each intensity level to produce a single-CI-IDA curve for the platform and the chosen earthquake record.
From these findings, it has been observed that the measured ground resistances match closely to the simulated grounding resistance values especially for the grounding grid with rods at the site of the wet soil.
It is also shown that constant values of ground conductivity and permittivity are able to lead to results comparable to those obtained with a dispersive ground model provided a suitable value is selected for the ground relative permittivity.
The significance of the changes in CEC values for ground samples compared to ground and wet sieved with 106 µm cutoff was also evaluated by calculation of P values using Student's t Test (Additional file 1: Table S5).
In addition we add the values we obtain analytically for the ground state (grey dot) and the branch of single doublon-holon pair excitations (grey lines).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com