Karst

Karst areas present unique hydrologic and hydrogeological characteristics that
are often challenging to investigate. These characteristics are largely dependent
on the extent of development of solution conduits within the underlying bedrock,
and the resulting integration of surface and subsurface drainage components
into a karst aquifer system. The investigation and characterization of
karst aquifers typically require a multidisciplinary approach and the use of
relatively specialized methods such as tracer testing, spring discharge monitoring,
and various hydrograph separation or modeling techniques. Conventional
methods of hydrologic or hydrogeologic investigation may be applied successfully
for specific purposes; however, proper conceptualization of a given karst
aquifer system is a requirement for effective analysis, modeling, and interpretation
of karst hydrologic and hydrogeologic data.