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ARS Home » Midwest Area » Columbia, Missouri » Cropping Systems and Water Quality Research » Research » Publications at this Location » Publication #210434


item Lerch, Robert
item WICKS, C
item MOSS, P

Submitted to: National Cave and Karst Management Symposium
Publication Type: Abstract Only
Publication Acceptance Date: 4/26/2007
Publication Date: 10/8/2007
Citation: Lerch, R.N., Wicks, C.M., Moss, P.L. 2007. Hydrologic characterization of two karst recharge areas in boone county, missouri. Available: National Cave and Karst Management Symposium, October 8-12, 2007, St. Louis, MO.

Interpretive Summary:

Technical Abstract: The Bonne Femme watershed, located in central Missouri, is a karst watershed in a rapidly urbanizing area. This study was undertaken to characterize the hydrology of two karst aquifers within this watershed before significant increases in impervious surface have occurred. The specific objectives of this study were to: 1) use dye tracing to delineate the recharge area for Hunters Cave (HC); 2) quantify and summarize annual and monthly stream discharge at the resurgence of HC and Devils Icebox (DI) caves; and 3) characterize the chemical and physical status of the cave streams relative to temperature, pH, specific conductance, dissolved oxygen, and turbidity. The quantity and quality of the water at the resurgence of both cave streams was monitored from April 1999 to March 2002. Both recharge areas were determined to be of similar size (33.3 km2 for HC and 34.0 km2 for DI) and were formed in the same geologic strata. Average annual discharge was 55,900 m3/km2 at DI and 35,200 m3/km2 at HC. Relative discharge, as a percent of annual precipitation, averaged 6.1% at DI and 3.8% at HC. Average monthly discharge was 2,930 m3/km2 at HC and 4,650 m3/km2 at DI; however, median instantaneous discharge over the three years was about 18% higher at HC (74 m3/h) compared to DI (63 m3/h). Turbidity and pH showed the largest differences between sites over the three years. The higher turbidity and lower pH at DI reflected the greater magnitude and duration of runoff events for this system. The physical characteristics of the two recharge areas explained the observed differences in discharge. The HC recharge area is characterized by limited sub-surface conduit development, small conduits, short flow paths from surface to resurgence, and predominantly allogenic recharge. The DI recharge area is characterized by extensive sub-surface conduit development, large conduits, long flow paths to the resurgence, and autogenic and allogenic recharge.