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We will show that it is possible to prolong the upper state lifetime by more than an order of magnitude in a diagonal transition active region design, that uses transitions between heavy hole ground states of spatially separated quantum wells.
Based on the coupled FE-SPH model, which is validated by experimental results, the swelling movement affected by preformed hole, ground base, thickness of concrete plate, different type of explosive and burial depth of explosive in compact material is investigated by simulations.
Performing numerical experiments with a variation in QD size, we not only show that the strength of ground state inter-band light transitions can be optimized via QD size-engineering, but also find that the hole ground state wavefunction serves as a control factor of transition strengths.
Thus, the AMONIL presence in the hole ground needs a specific RIE process.
However, the hole ground state is also pushed down by the band bending, which leads to a blueshift.
Graphics in row (e) correspond to the variation of the energies of the first two electron states (left panel) and the heavy hole ground state (right panel) as functions of the intense laser field parameter.
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These effects would lead to a hole ground-state character exchange from predominant-hh to -lh, and to the intensity difference between these cross-polarized emissions, experimentally confirmed by Figure 10a.
We will be showing below that mass anisotropy of hole ground-state might be hold responsible for these anisotropic optical emission intensities once the dot confinement strength becomes relaxed in certain directions, whether by dot size anisotropy and/or by inter-dot coupling tuned by the strain fields.
For a better comprehension, we present in Figure 2 the self-consistent heavy-hole (ground state) potential profiles inside the well for the same systems described above.
Three mutually exclusive variables were used to describe nest position (elevated > 1 m in a tree or bush; tree-hole; ground or other substrate or surface).
The tomogram in this study is obtained by inversion of cross-hole ground-penetrating radar (GPR) first-arrival travel time data acquired at the MAcro-Dispersion Experiment (MADE) site in Mississippi (USA).
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