Assertion: aquifer's water | /r/CapableOf | enter the aquifer
Facets:
value: at recharge areas
type: LOCATION
value: locally
type: MANNER
value: by seeping into the land surface
type: MANNER
value: during pleistocene glaciation
type: TEMPORAL
value: in the recharge zone
type: LOCATION
value: easily
type: MANNER
Source sentences:
text: Dye tests in the Edwards usually reveal high hydraulic conductivities and velocities, so while the average residence time is high, there are places and flowpaths where water enters and then leaves the Aquifer very quickly.
text: Soil and rock layers in groundwater recharge zones (a entry point where water enters an aquifer) reduce flooding by absorbing excess runoff after heavy rains and spring snowmelts.
text: Water enters the Aquifer easily in the recharge zone, but the subsurface drainage is generally inadequate to hold all the water that falls in large rain events.
text: When recharge water enters the Aquifer it slows down and the sand and dirt and organic materials it carries begin to settle out (as in the jar above).
text: Water can re-enter the aquifer in these recharge areas.
text: This water enters the aquifer by percolating down from the soil surface or through the permeable soil in the stream or river bed.
text: Water enters the aquifer at recharge areas at or near the outcrop of the aquifer and moves toward the Mississippi River and its tributaries, the Minnesota, St. Croix, Wisconsin, and Rock Rivers, where it is discharged.
text: Potentiometric data for the Ozark aquifer suggest that ground-water movement is controlled by topographic relief; much of the water that enters the aquifer is quickly discharged to local streams as indicated by the irregular shape of the aquifers potentiometric surface (fig.
text: Most of the meteoric water entering the aquifer from the recharge zone moves through the freshwater zone before being discharged.
text: Water enters aquifers by seeping into the land surface at entry points called recharge zones and leaves at exit points called discharge zones.
text: Much of the water that enters the aquifers where they crop out moves along short flow paths and discharges to small streams or springs.
text: Isotopic dating of water in these aquifers near their easternmost extent in South Dakota indicates that water locally entered the aquifers during Pleistocene glaciation.