Sentence examples for groundwater flow through from inspiring English sources

The fundamental physical principles of groundwater flow through porous media are discussed.

Groundwater flow through the tailings is mainly horizontal with velocities of 4 8 m/yr.

The Boussinesq equation (BEQ) can be used to describe groundwater flow through an unconfined aquifer.

Accordingly, higher recolonization rates were observed in a peatland located in a groundwater flow through system that had a shallow post-fire WT.

Previous research has demonstrated that this stratigraphy can facilitate preferential groundwater flow through focused linear features, such as paleochannels, or gravelly regions within the vadose zone.

In this study, a new approach is developed to simulate groundwater flow through both an overlying unconfined aquifer and an underlying discrete fracture network.

Mean inter-annual specific conductance (a proxy for salinity) increased along this continuum from wetlands that recharge groundwater being fresh to wetlands that receive groundwater discharge being the most saline, and wetlands that both recharge and discharge to groundwater (i.e., groundwater flow-through wetlands) being of intermediate salinity.

The anthropogenic colloids formed in the borehole were flushed out during groundwater flow-through (Figure 6).

Ultrafiltration was conducted using a 0.2 μm membrane during groundwater flow-through in the sampling intervals in the boreholes.

In contrast to the size-fractionated groundwater and colloid sampling, the groundwater was passed through a 0.2 μm membrane during groundwater flow-through in the sampling interval space in the boreholes.

The concentrations of REEs were approximately constant and within analytical error (±10%) during groundwater flow-through in the sampling intervals in the 09MI20 and 10MI26 boreholes (Figure 9). Figure 8 Size-fractionated concentrations of REEs from boreholes.