How Can We Sustain Groundwater Quality in Karst and Fracturedcarbonate. Maureen A. Muldoon Geology Department Univ. Of Wisconsin-Oshkosh

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Transcription:

How Can We Sustain Groundwater Quality in Karst and Fracturedcarbonate Aquifers? Maureen A. Muldoon Geology Department Univ. Of Wisconsin-Oshkosh

The Question Karst and fracturedcarbonates form productive, but quite vulnerable, aquifers. We live, farm, and dispose of waste on top of these fragile systems. Can we sustain the water quality in these aquifers for current & future users?

Bedrock Geology

Silurian Dolomite Aquifer

Silurian Dolomite Aquifer

Silurian Dolomite Aquifer Rapid downward flow in vertical fracture network Rapid lateral flow along bedding-plane parallel fractures Some of these flow zones are laterally continuous at the scale of kilometers

0 1 2 3 4 miles 0 1 2 3 4 kilometers locations of wells and rain gauge used in this study other municipal wells

8/20/99 9/19/99 10/19/99 11/18/99 12/18/99 1/17/00 2/16/00 3/17/00 4/16/00 5/16/00 6/15/00 7/15/00 8/14/00 20.0 15.0 10.0 5.0 0.0 date 9.4 9.2 9.0 8.8 electrical conductivity, ms/cm precip, in fluid temp, o C Well DR-265 Door Co Hwy Garage Precipitation electrical conductivity Downgradient temperature 250 ft below surface; cased to 170 ft 1 0.5

Water Quality Variation NO 3 -N values from three domestic wells completed in the Silurian dolomite Similarity of response in wells located miles apart suggests a diffuse rather than point source of contamination 30 20 10 0 10 0 20 10 7500 700 650 600 2 1 0 Well 20 Well 56 Well 61 MW-1 Head Precipitation JFMAMJJASONDJFMAMJJASONDJFMAMJJASONDJFMAMJJASONDJFMAMJJA 1986 1987 1988 1989 1990

Carbonate is uppermost bedrock Surficial materials < 50 ft thick

Case Study 1: Calumet County Sinnipee Dolomite Maquoketa Shale 1000 Lake Winnebago Silurian Dolomite 800 600 400 200 0 Q Quaternary Glacial Deposits Sil Grp Silurian Dolomite M Fm Maquoketa Formation Sinn Grp Sinnipee Dolomite Ancell, Prairie du Chein, Undifferentiated Cambrian Formations (Sandstone & Dolomite) pє PreCambrian Bedrock Gotkowitz & Gaffield, 2004 Draft pє M Fm Sinn Grp Ancell, PdC, Є Sil Grp Q

2002-2004 Test results 45% < 2 ppm 29% 2 10 ppm 26% > 10 ppm Nitrate Sampling Data and maps provided by Katie Hemauer Calumet County Land & Water Conservation Dept

Coliform Bacteria 2002-2004 Test results 35% of wells tested positive for coliform bacteria Data and maps provided by Katie Hemauer Calumet County Land & Water Conservation Dept

Calumet Co GW Summit County personnel invited approximately 25 folks with expertise in nutrient management, soils, geology & hydrogeology to attend a summit in early April Wanted an answer to the question How do we farm these areas and not degrade groundwater quality?

NRCS Nutrient Management Standards Addresses the application and budgeting of nutrients for plant production All nutrient sources shall be properly credited & utilized Goal is to not apply in excess of crop needs http://www.datcp.state.wi.us/arm/agriculture/land-water/conservation/ nutrient-mngmt/pdf/590_proposed_final_draft.pdf

NRCS Nutrient Management Standards Specific prohibitions for karst and fractured rock areas Recommendations for karst and fractured rock areas Have 6-month storage capacity for manure Apply manure and incorporate into soil twice yearly Credit manure application in nutrient management plan Will it help?

Barnyard Monitoring Project was designed to monitor groundwater quality at two barnyards before and after the introduction of Best Management Practices

Barnyard Monitoring Installed 2 to 3 piezometers/hole Monitored 1-yr prior to initiation of BMPs and 2 yr after Measured nitrate-n at >300 mg/l in water flowing into bedding plane cave Never detected nitrate-n (or other forms of N) > 4 mg/l in wells

Case Study 2: Landfill Expansion An existing landfill in Manitowoc County is reaching capacity and is looking to expand. Site geology consists of approximately 50-90 ft of glacial sediment (tills & outwash) over Silurian dolomite. In portions of the proposed expansion the watertable lies within the dolomite. DNR is concerned about the ability to effectively monitor and remediate the site. The landfill owner and their consultants feel that the site characterization was conducted according to code and should be adequate.

Case Study 2 The landfill siting process is WI is very proscribed. The current code specifies the data that should be included in the various required reports. There are no specifications or guidelines that require fractured rock sites to be characterized any differently than porous medium sites. http://www.dnr.state.wi.us/org/aw/ wm/solid/landfill/siting.htm

Site Characterization The site conceptual model guides characterization Continuum Discrete fracture These data illustrate the effect of test scale on measured hydraulic conductivity values Data were collected from the same corehole

Case Study 2: Landfill Expansion

Summary Existing water quality data indicate that the Silurian dolomite aquifer is quite vulnerable to contamination (evens in areas with 10 s of ft of surficial sediment). We are just beginning to develop agricultural BMPs for these settings and we have few to no data on their effectiveness. Obtaining such data would be costly. While there are some guidelines for the characterization of fractured rock sites, the state of the practice for many (not all) sites is to treat them as porous media sites.