Sentence examples for depth of the uppermost from inspiring English sources

First, plants would promote the weathering of rocks to fine clay minerals, and as rooting systems evolved, and symbiotic relationships with microbes increased, the depth of the uppermost layer of rocky soil in which chemical weathering took place would increase.

We therefore also estimated the number of neurons per neuron type (at the example of the D2 column) using layer borders derived from the recording depths of identified neurons (inset in Fig. 4 A ; layer borders were estimated as the average depth of the uppermost and deepest neuron of 2 neighboring layers, respectively).

Fig. 3. Depth of four uppermost interfaces of the 3-D velocity model: (a) oceanic water layer (sea bottom), (b) oceanic sediments layer, (c) surface low-velocity layer, and (d) upper interface of the subducted oceanic layer 2. Numbers on contours indicate depth in kilometers.

The elastic wave speed of the surrounding bedrock also varies, basically increasing with the depth in the uppermost crust.

Depending on the depth of the peel, peels remove the uppermost layers of the skin.

The degree of metal saturation of soil organic matter (estimated by the (Alp  Fep /Cp molar ratios) increases with depth, especially in the uppermost samples of spodic horizons (Bhs1) where it increases up to 0.1.

SIMS is a high-sensitivity surface analysis technique for the determination of surface composition and contaminant analysis and for depth profile in the uppermost surface layers of a sample, and it can detect very low concentrations of dopants and impurities.

The depth and P-wave velocity of the uppermost mantle (P n velocity) of the PAC correspond with a previous study located at the landward slope along the JT (Miura et al., 2003).

The depth of well in uppermost aquifer varies from 6 to 13 m bgl (below ground level).

Prior studies, that looked at reaches or six to seven rangelines or cross sections on hydrographic surveys document areal, width, and depth increases in the uppermost 80 km (50 mi) of the Atchafalaya River from 1880 to 1974.

The hypocenters relocated by NLLoc show that the absolute location errors of two earthquakes at depths of 50 55 km are < 5 km (Fig. 3b), suggesting that they occurred in the uppermost mantle; the depth of the continental Moho in the region is estimated to be ~ 40 km (Katsumata 2010).