Sentence examples for observations soil from inspiring English sources

Field observations, soil hydraulic properties and dye tracer studies describe different hydrological aspects of the studied sites and complement the information provided by the morphological image indices.

The Vertical Equilibrium Model (VEM) is a simple approach to estimate the catchment-wide soil water storage at a daily time-scale on the basis of water table level observations, soil properties and an assumption of hydrological equilibrium without vertical fluxes above the water table.

The temporal vertical observations of soil moisture and soil water acquisition rates demonstrated the existence of an impermeable soil layer at 30 cm, which had lower soil organic carbon content.

We use a combination of LiDAR analyses, field observations, and soil characterization to examine soil and vegetation at these two sites, and find that the presence of an external sediment or soil source, particularly flood-borne deposits or syn- or post-eruptive tephra, greatly facilitates plant establishment, growth, and survival.

The resulting ET values were compared with independent observations of soil water depletion, obtained from soil neutron probe profiles.

In this paper, an effective stochastic geological modeling framework is proposed based on Markov random field theory, which is conditional on site investigation data, such as observations of soil types from ground surface, borehole logs, and strata orientation from geophysical tests.

In this study, simulation data from climate models and the land surface model, reanalysis data, the Tibetan Plateau permafrost map, the Circum-Arctic map of permafrost and ground ice conditions, and in situ observations of soil temperature were employed to analyze and validate the results.

The model simulated well the general trend of field observations for soil water content and potential (ψs), and the values matched better for the soils with less heterogeneity.

The data inputs used were exposed bedrock (EB) points identified from orthophotos, well record (WR) data, and in-situ observations of soil thickness, for which conditioned Latin hypercube sampling (cLHS) was used to define a set of locations where soil thickness was determined.

A database, consisting of post-earthquake field observations of soil performance, in conjunction with in situ "index" test results is used for the development of probabilistically-based seismic soil liquefaction initiation correlations.

Methods included outcrop observations and soil sampling, and subsurface examination using boreholes and the Standard Penetration Test (SPT).