Springs are locations where upwelling groundwater discharges to the earth’s surface, the “Big Spring” (pictured above) on the shore of Lake Wingra in the University of Wisconsin-Madison Arboretum, is an example. The flow of fresh water from springs helps supply wetlands, streams, rivers, and lakes. Spring flow supplements rainfall and snowmelt that flows overland or that falls directly on the water body.
Technically, a hydrologist will define a spring as having a volume of 0.25 cubic feet per second (cfs) or about 110 gallons per minute. But, in everyday language people refer to any groundwater discharge as a “spring” if it has a defined stream channel; “seeps” have a more diffuse groundwater discharge that only make a puddle. In Wisconsin, there are 10,000 inventoried springs. But not all have legal protection; only those springs (about 300) that have a flow rate of 1 cfs have protection from destruction by Wisconsin law. See: Modify definition of springs law. The Arboretum “Big Spring” with an average flow of over 1cfs falls in the protected ranks.
Estimates are that there were once several dozen springs around Lake Wingra–today there are only about two dozen that flow regularly. Many were lost to building of roads and houses and others have dried up or flow only intermittently. The drying up of some springs is perhaps because today there is a smaller amount of precipitation–than historically–that actually infiltrates into the groundwater. This lost precipitation instead runs down driveways and streets into storm sewers. The graphic linked to below shows the relative locations or known springs around Lake Wingra in 2005, credit to Friends of Lake Wingra (FLOW)
Locations of Lake Wingra Springs 2005
Despite the importance of groundwater flow to the Lake Wingra water budget, little is known about the number of springs still flowing, their individual flow rates nor the number that have been lost over the years. Research to measure the amount of water flowing from some springs was conducted by Bemis, et.al 2005 and Ballering and Bahr, 2004.
The blogger measures spring flow rates of 6 springs. Springs monitored are: Council Spring and Dancing Sands on Monroe St at Arbor Drive; a spring on the Nakoma Golf Club; and West Spring, Big Spring, and White Clay springs, all in Wingra Woods in the Arboretum. In the future I will post spring flow rates and other information about springs on this blog.
For more information about the springs, listen to springs podcasts featuring local naturalists at Unseen Madison, or read more about the ecological, social, and cultural history of Lake Wingra in “Ten Views of Lake Wingra” in the June, 2012 issue of Madison Magazine.
Ballering, N. and J. Bahr. 2004. Spring flow and water quality in the Lake Wingra Watershed. Undergraduate Research Scholars Program, Department of Geology and Geophysics, University of Wisconsin-Madison.
Bemis, B., D. Gildner, E. Murdock, L. Severson and C. Storrar. 2005. Springflow Gauging for Long-term Monitoring of Groundwater Flow Into Lake Wingra. Hydrolic Measurements (CEE 619) May 12, 2005.