Characterization of surface and ground water δ18O seasonal variation and its use for estimating groundwater residence times
Version of Record online: 23 DEC 2005
Copyright © 2005 John Wiley & Sons, Ltd.
Volume 20, Issue 8, pages 1753–1772, May 2006
How to Cite
Reddy, M. M., Schuster, P., Kendall, C. and Reddy, M. B. (2006), Characterization of surface and ground water δ18O seasonal variation and its use for estimating groundwater residence times. Hydrol. Process., 20: 1753–1772. doi: 10.1002/hyp.5953
- Issue online: 13 APR 2006
- Version of Record online: 23 DEC 2005
- Manuscript Accepted: 28 MAR 2005
- Manuscript Received: 19 AUG 2003
- surface water;
- seasonal variations;
- groundwater residence time
18O is an ideal tracer for characterizing hydrological processes because it can be reliably measured in several watershed hydrological compartments. Here, we present multiyear isotopic data, i.e. 18O variations (δ18O), for precipitation inputs, surface water and groundwater in the Shingobee River Headwaters Area (SRHA), a well-instrumented research catchment in north-central Minnesota. SRHA surface waters exhibit δ18O seasonal variations similar to those of groundwaters, and seasonal δ18O variations plotted versus time fit seasonal sine functions. These seasonal δ18O variations were interpreted to estimate surface water and groundwater mean residence times (MRTs) at sampling locations near topographically closed-basin lakes. MRT variations of about 1 to 16 years have been estimated over an area covering about 9 km2 from the basin boundary to the most downgradient well. Estimated MRT error (±0·3 to ±0·7 years) is small for short MRTs and is much larger (±10 years) for a well with an MRT (16 years) near the limit of the method. Groundwater transit time estimates based on Darcy's law, tritium content, and the seasonal δ18O amplitude approach appear to be consistent within the limits of each method. The results from this study suggest that use of the δ18O seasonal variation method to determine MRTs can help assess groundwater recharge areas in small headwaters catchments. Copyright © 2005 John Wiley & Sons, Ltd.