264 Understanding Karst Hydrology and Karst Aquifers Using Innovative Tracers and Other Technologies (Posters)

We welcome submissions applying innovative tracers and other technologies to investigate karst hydrology and karst aquifers, including but not limited to complex interactions between surface water and groundwater, recharge processes, flow pathways, sediment transport, sustainability, and susceptibility to contaminants.

Wednesday, 22 October 2025
8:00 AM - 5:30 PM
HBGCC, Hall 1

Evaluation of Practical Methods to Determine if a Karst Creek is Gaining or Losing: Case Study of Leith Creek

Paper number: 264-4
Program: Technical Sessions
Time: 8:00 AM – 8:00 AM

Authors

Abstract

     Leith Creek is a small stream in Polk County, Missouri fed by two springs and the shallow unconfined Springfield Plateau aquifer, a highly karstified aquifer which is made up of limestone and minor interbedded shale-mudstone units. To determine if Leith Creek is gaining or losing, stream flow, water chemistry and temperature sensors were monitored. A losing stream would have decreasing discharges further downstream, while a gaining stream would have increase discharges further downstream. Another objective of the study was to determine if Leith Creek is being contaminated by sewage, fertilizers, and manure since this county has the 2nd largest number of cattle in Missouri.

     Stream discharge was measured bimonthly at four sites within a 0.4 km creek segment. Water samples were also tested bimonthly for sulfates and nitrate-nitrogen. Results of this study show that Leith Creek is both a losing and gaining stream with a low degree of contamination by animal waste, and that precipitation influences water quality. The water quality reflects dissolution of limestone and contains little sulfur. The nitrate nitrogen amount ranges from 0.09 mg/L to 3.00 mg/L, with an average nitrate nitrogen level of 0.92 mg/L.

 

Geological Society of America Abstracts with Programs. Vol. 57, No. 6

doi: 10.1130/abs/2025AM-412350

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