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Because of the low sensitivity of this analysis to the event depth, the depth of the induced event is fixed at 8 km, which is a typical depth of earthquakes in Oita region after M7.3 event.
[It is interesting to note that the difference in maximum h'F(2.5) values of 50 km, shown in Fig. 5, is a typical depth of an upwelling (Tsunoda, 2015).] This conclusion is consistent with the 'PSSR' concept, which allows additive growth by the PSSR and upwelling growth.
Based on the data presented in [44, 45] for soil bacterium Bacillus subtilis, the following parameter values for these microorganisms are used: Dm = 1.3 × 10-10 m2/s, Ds = 2.12 × 10-9 m2/s, Δρ = 100 kg/m3, n 0 * = 10 15 cells/m 3, θ = 10-18 m3, and H = 2.5 × 10-3 m (or 2.5 mm, this is a typical depth of a shallow layer; this size is also typical for a microdevice).
Open raceway ponds are ring-channel systems, with a typical depth of 0.2 m.
Where we model cell depth, we assume that each cell type has a typical depth, and thus a Gaussian distribution of s i.
Normal tissue exhibits wrinkles, which have a typical depth of 100 µm and a width between 20 and 50 µm, and regular epithelial cells with a typical diameter of 30 µm.
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Results concerning the transmission loss outside and inside obstacles consisting of three cylindrical rings are given for a typical depth-dependent ocean sound-speed profile.
If the seismic reflections we observed were derived from one of these volcanoes, the reflector is likely to be located at a more typical depth for a magma chamber.
James Wilson of Pennsylvania made the argument for a single officeholder with typical depth and precision: "To control the executive, you must unite it.
In contrast to SEM/EDS which has a typical analysis depth of 1 3 µm, XPS is a surface analysis technique with a typical analysis depth of less than 5 nm.
If one simplistically assumes a level of no motion at certain depth exceeding the typical depth of the ACC, then an effective depth can be defined for the flow field, and Δu and Δv reflect the depth-averaged variation of the geostrophic flow over the water column above the effective depth.
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