DYE TRACING IN THE JORDAN SANDSTONE NEAR THE CRYSTAL SPRINGS STATE FISH HATCHERY, WINONA COUNTY, MINNESOTA
Two dye traces were attempted in or through the Jordan Sandstone. One dye was injected in a sinking stream in the Kieffer Valley about 600 m northwest, upstream of the 1980/2008 sink point. This sinkpoint was at or just above the Jordan/St. Lawrence contact. A second dye was injected about 2 km southwest of CSSFH near the Oneota Formation/Jordan Sandstone contact in the terminal sink of a sinking stream. Charcoal detectors were installed in 2 springs at CSSFH, 4 other springs, 6 surface stream locations and one private well. The detectors were initially changed on weekly to biweekly intervals and then at monthly intervals for five months. The dye packets were eluted with basic isopropanol and analyzed on a scanning spectrophotometer. No dye was detected from either injection.
Negative dye traces are ambiguous. Four classes of explanations exist: 1) The dye has not yet reached the detection points. The flow is slower than hypothesized and we have not waited long enough. 2) The dye was diluted below the detection limit. We did not use enough dye. 3) The dye flowed to unmonitored locations. We did not look in the right places. 4) The dye may have been adsorbed or chemically changed. The third explanation seems to be the most reasonable in this case, suggesting the groundwater flow systems in this area are more complex than initially assumed.