torque and swirl are obtainable with a big bowl segment, although it was observed that a shallow combustion chamber is expected to induce higher torque.
It is observed that at shallow depth, i.e., low resistivity zone (>10 Ω m), redox reactions support the release of As from arseniferous iron oxyhydroxides in the groundwater and the given facts were also validated through geochemical characterization of water samples (Kumar et al. 2010) and the borehole lithology (silty clay).
The migration of radioactive species that has been observed at shallow burial sites for low-level radioactive waste is not an indication that similar migration can be expected for high-level waste located in a repository deep underground.
In this study, it is observed that overpressure starts at shallow depths (1,482 2,145 m) in synclinal section while in flank section it starts deeper (2,653 5,919 m) in Atharamura anticline.
For shallow shells it is observed that the vertical components of the earthquake vibrations, can induce larger stresses in the shell than the horizontal components.
It can be observed that the average depth of the rupture surface was shallow, about 6.5 m, with a depth-to-length ratio of 0.06.
It is observed that the amplification of the ground surface underlain by a shallow cavity is increased in long periods.
For the fourth column, it can be observed that the localization errors of deep sources are higher than those of shallow sources.
Furthermore, it was observed that areas with thin/shallow overburden coincided mostly with areas underlain by variably migmatized gneiss complex, while area with thicker overburden unit coincided with area mainly underlain by schist.
Adult males have been observed gathering in shallow water, which may relate to reproduction.
