Sentence examples for infiltration water from inspiring English sources

Infiltration water temperature variations equally influence residence times of the infiltrated water.

In this paper, we look at the influence of temperature variations of the infiltration water in the recharged aquifer.

Seasonally varying temperature in the infiltration water results in a zonation of subsequent lower and higher temperatures in the aquifer.

We test for air infiltration, water penetration, wind loads, heat loss, and in California there's a lot of structural testing for earthquakes.

Infiltration and extraction rate, their ratios and seasonal variability, and location of extraction wells are all contributing factors to the impact of varying temperature of the infiltration water.

However, little evidence has been gained from direct measurements of overland and infiltration water fluxes between bare soil inter-patches and shrub mounds at a scale compatible with available high resolution imagery and hydrological modeling techniques.

It has been confirmed that the application of organic matter to soils affected by salinity can increase sodium chloride (NaCl) leaching, reduce the exchangeable sodium rate and electrical conductivity, and increase water infiltration, water-holding capacity, and aggregate stability (El-Shakweer et al. 1998).

Fluctuations in uranium concentrations in surface-infiltration water can be attributed to releases of uranium from specific sources – migration from phosphate fertilizers and leaching from mineral deposits.

The relationship was used to explain why the finger did not widen behind the tip, and why, upon re-infiltration, water followed the previously established path.

As the removal efficiency of uranium during applied treatment process is negligible, the effect of increase in uranium concentration can be explained by higher U concentration in the surface-infiltration water used for the production of drinking water.

Infiltration of water and ions into the coating can also be measured by EIS to deduce approximate water uptake.