Sentence examples for typical depth of from inspiring English sources

Effect of the gate bias on energy band delineates the modulation of 2DEG carriers in the shallow energy quantum well from 1.6×10−3 cm−3 to 9.47×1017 cm−3 with gate bias from 0.5 V to 1.0 V to confirm the drain current conduction with Vth>+0.5 V at typical depth of source and drain Ohmic contacts.

Because of the typical depth of oil reservoirs, the most common types of failure are of breakout and vertical tensile failure.

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.

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.

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).

Typical depths of penetration are on the order of several thousand angstroms, depending on energy, ion type, and target material.

Typical depths of the Texas lagoons vary between 1.25 and 3.5 metres (4 and 11 feet), and their floors are flat.

In Section 2, we evaluated the waveform misfits δFD (Eq. (3)) between the FDM and DWM for water-layer thicknesses of 40 and 160 m (Fig. 2), which correspond to typical depths of MCL and TL, respectively.

Most of the bedrock water wells are unsealed open-hole completions, with casing terminating in the shallow bedrock in order to draw water from multiple horizons at typical depths of 100 to 500 feet beneath ground surface (Lohman 1937, 1939; Taylor 1984; PaGWIS 2011).

The potency release per strike length is F HU/X, where F is the typical depth to the base of each of the numerous faults that cut the outer rise.