Sentence examples for transport depth from inspiring English sources

ENM transport was found to be highly limited in natural soils collected from farmland and grasslands, with the majority of particles being retained in the upper 0 3 cm of the soil profile, while greater transport depth was seen in a commercial potting soil.

The adaptation time T s (unit: s) is determined by the local water depth h, sediment fall velocity w s, and a sediment transport depth factor : (A.1)The formula for sediment fall velocity in XBeach is proposed by Ahrens's (2000) (A.2) (A.3) (A.4)where, A is Archimedes buoyancy index, s = ρs/ρ is specific gravity.

While the available geostatistical characterization of heterogeneity can explain most of the integrated behavior of transport (depth-averaged breakthrough curve), not all multilevel BTCs are described with equal success.

This technology may someday become possible through advanced QSIP architectures having photons of different wavelength continuously absorbed at different depths, and their resulting photocurrents isolated with a vertical grid of contacts or an equivalent mechanism for transporting depth-dependent signal photocurrent to a read-out circuit unit cell.

Large P concentrations (0.23 1.02 mg P L−1) occurred in one plot that occasionally ponded, indicating P transport to depth by preferential flow is a risk in some soils on this landscape.

Instead, our data suggest that faults in Paleozoic rocks play a fundamental role in gas and brine transport from depth, regulate the distribution of their occurrence in shallow aquifers, and influence the geochemistry of shallow groundwater in this petroliferous basin.

Furthermore, because cichlids have physoclistous gas bladders, adult fish have limited tolerance for rapid change in water pressure [ 21], suggesting that few individuals would survive a rapid upward transport from depth through entrainment in dynamic vertically upwelling waters.

We envisage that substantial volume of fluids were transferred from mantle into the lower crust through the younger plume-related Deccan volcanism, as well as the reactivation, fracturing and expulsion of fluids transported to depth during the Mesoproterozoic subduction tectonics.

(3) The fluids seeping on the Oomine Ridge are transported from depth via faults and are mixed with SPF of the accretionary prism sediments and freshwater derived from MH dissociation prior to reaching the seafloor.

The fluids seeping on the Oomine Ridge are transported from depth via faults and are mixed with SPF of the accretionary prism sediments and freshwater derived from MH dissociation prior to reaching the seafloor.

On the other hand, the dilution index indicates a slight tendency towards stochastic convective transport at this depth.