Examples of Groundwater recharge areas in a sentence
Groundwater recharge areas may occupy a range of hillslope gradients, shapes, and soil and rock types.
Groundwater recharge areas are those portions of the earth's surface where water infiltrates into the ground to replenish an aquifer.
Groundwater recharge areas provide all of the County’s water supply.
Water resource areas that will be included within this map (and their data sources) are as follows: Lakes, ponds, and rivers – found on DataMIL Wetlands – found within the land use/land cover dataset also on the DataMIL Groundwater recharge areas – environmental features map in your comprehensive plan Watershed boundaries – found on DataMIL FEMA Q3 flood plains – environmental features map in your comprehensive plan, your county’s web site, or FEMA’s web site, www.fema.gov/.
Groundwater recharge areas occur where the saturated net flow is traveling away from the water table, while the discharge areas occur where the saturated net flow is travelling towards the water table (Freeze & Cherry 1979).
Groundwater recharge areas, headwaters and aquifers are key components in the functioning of the hydrologic cycle.
Groundwater recharge areas in the county are located in low pollution susceptibility areas, based on the Georgia Pollution Susceptibility Map prepared by the state department of natural resources in Hydrologic Atlas 20, 1992 Edition.
Groundwater recharge areas relate to local topographic and geologic conditions, with recharge areas located throughout the study area away from watercourses, which are generally associated with areas of discharge.
Determining the practicable level of protection necessary for individual groundwater resources will take account of:• The social, economic and ecological importance of the resource, regionally and/or locally.• The vulnerability of the resource to pollution and other impacts.• Groundwater recharge areas, particularly where these are separate from abstraction areas (e.g. in mountainous areas).
Groundwater recharge areas of deep-seated slides are located in the lands up-slope that can contribute subsurface water to the landslide.