A further 64 permits have been issued for groundwater discharge.

However, there is no information available on the interaction between ecosystems and groundwater discharge.

Is there an advantage of this method over traditional groundwater discharge measurements?

It has been described as a groundwater discharge zone.

Most of the groundwater discharge in the South East occurs to the sea.

The lake serves as a groundwater discharge region for higher elevations to the east and west.

Snow is typically dumped near coastal areas and at groundwater discharge sites.

Others, especially those in low-lying areas, may be the receptors for significant amounts of groundwater discharge.

Groundwater discharge contributes 60-70% of stream flow on an annual basis; during the growing season this approaches 100%.

Groundwater discharge Groundwater that comes up to the surface.

Could it affect groundwater discharge or recharge areas?

Consequently, the precise locations of groundwater discharge from deep fractures into local surface water remain uncertain.

Local groundwater discharge occurs on the valley floor where it has been ponded by dykes.

Groundwater constitutes about 40% of this, not including the springs, which are actually groundwater discharges.

• Grab samples of groundwater discharge points (springs, surface water)

They are frequently in areas of groundwater discharge, thus protecting headwaters of streams.

Many streams of the South East are fed by groundwater discharge, which provides baseflow.

To the question of groundwater discharge into the Black Sea in the Gagra area.

Estimation of transpiration by halophytic vegetation: implications for groundwater discharge.

Associated with the groundwater discharge is extensive gas venting, typically nitrogen and carbon dioxide.

Total groundwater discharge, as reported through a specified area, is similarly expressed as:

For applications for water discharge and point source groundwater discharge activities you need to fill in part F2 instead.

Soils are one of the major determinants of runoff potential, infiltration and groundwater discharge.

Groundwater discharge to these rivers support baseflow.

My current research focuses on submarine groundwater discharge from a coastal aquifer into the near-shore environment.

You'd never get this kind of discharge just from groundwater flow.

Inevitably, not all groundwater flow systems will be covered by the current project.

The groundwater flow direction at the site has consistently been toward due south.

No significant residual effects on groundwater flow patterns are expected.

The important effect of groundwater flow in the slope has also been enhanced.

Landslides and changes in the groundwater flow were also reported.

Ideally, groundwater flow should be away from the community or nearby water sources.

To begin each experiment a steady state groundwater flow field was established across the model.

Back at the office, you might put all your data into a computer program and produce models of groundwater flow or water chemistry.

This may have been due to a combination of gravity and groundwater flow.

The groundwater flow rate within a cenote may be very slow.

The direction of groundwater flow should also be considered when selecting a landfill site.

Horizontal components of groundwater flow are directed to the south and east.

Fractures provide the primary pathways for groundwater flow in rock.

Over time, the characteristics of each groundwater flow system becomes better understood and so do the implications for management.

Groundwater flow directions are depicted on Figure 12 by arrows.

Developing a better understanding of the regional aquifers and groundwater flow systems.

The paleocollapse process may continue at some future date, due to deep groundwater flow changes.

The groundwater flow in Clovis is generally to the southwest.

This will be particularly evident in groundwater flow systems of different catchments.

Choosing the most appropriate category depends on the type of groundwater flow system.

Assume that groundwater flow in the aquifer is at steady state.

As a result the groundwater flow is diverted around the tailings.

Other potential future influences on the direction of groundwater flow could be from:

Scientists have now mapped the speed and direction of the area's limited groundwater flow.