Groundwater

Groundwater Flow is the another part of the water cycle.



The introduction to runoff page gave a description of the water cycle and various processes in the cycle. After a precipitation event, water can either runoff,infiltrate into the soil, or evaporate. The infiltrated water either is taken up by plants and transpirated or evaporated or becomes part of the groundwater. The term groundwater describes water that is stored underground in the rocks or geologic formations. Over time, the water stored in the groundwater flows (like a very, very slow river) back to the land surface further downhill. Most of the water stored in the groundwater eventually comes back to the land surface as springs or into streams, lakes, and oceans. Some groundwater may go into deep storage and not make it back to the surface.

 



InterWET shows what different factors affect groundwater. The researcher perspective uses a special calculator to show how the seasonal weather, time of the year, land cover, soil properties, and geologic properties affect how much precipitation becomes runoff, groundwater flow, and evapotranspiration, or is stored in the groundwater or as a snow pack. The conservationist perspective gives an interactive map of springs and tables and maps describing the complex groundwater flow systems in the Spring Creek Watershed. The local official perspective uses the results from a hydrologic model to predict how certain local policies may change groundwater flow in the Spring Creek Watershed over the next 20 years.

 

 
 
 

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Questions or Problems? Let me know at parson@andassoc.com.
Last revision 9/9/01.
Created by Shane Parson, Copyright 1999.