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While both springs can be traced to sinks, their isotopic signatures reflect how storm water infiltrates and travels within each spring’s recharge area. Tippery is fed by a perennial sinking stream and more developed conduit network, while Near Tippery has a more diffuse recharge area with mixing of different surface inputs. As stable isotopes are unaffected by redox or dissolution processes, they can provide a conservative tracer with which to characterize how other parameters, such as temperature, alkalinity, and turbidity, are reflected in different spring recharge behaviors.

Using Stable Isotopes to Distinguish Sinkhole and Diffuse Storm Infiltration in Two Adjacent Springs