The application of quantitative fluorescent dye tracing to evaluate karst hydrogeologic response to varying recharge conditions in an urban area

Author:

Gouzie Douglas,Berglund James,Mickus Kevin L.

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Reference16 articles.

1. Berglund J, Mickus K, Gouzie D (2014) Determining a relationship between a newly forming sinkhole and a former dry stream using electrical resistivity tomography and VLF-EM—the root of the problem. Interpretation 2:SF17–SF27

2. Brahana JV (1997) Rationale and methodology for approximating spring-basin boundaries in the mantled karst terrane of the Springfield Plateau, Northwestern Arkansas. In: Beck BF, Stephenson JB (eds) The engineering geology and hydrogeology of karst terranes. Balkema, Rotterdam, pp 77–82

3. Bullard L, Vandike Thomson KC, Vandike JE (2001) The springs of Greene County Missouri. Missouri Department of Natural Resources, Water Resources Report no. 68, Missouri 68

4. Cox R (2009) Ouachita and Ancestral Rockies formations recorded in mesoscale structures on the foreland Springfield Plateau. Tectonophysics 474:675–683

5. Emmett LF, Skelton J, Luckey RR, Miller DE, Thompson TL, Whitfield JW (1978) Water resources and geology of the Springfield Area, Mo. Missouri Department of Natural Resources, Water Resources Report no. 34, Missouri

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