Precipitation patterns in semi-arid river systems of the southwestern U.S. make stream-aquifer exchanges an important source of water in perennial rivers. Nonetheless, the spatial and temporal evolution of surface and ground water interaction are not fully understood. This research utilizes diurnal temperature oscillations as a tracer of vertical water fluxes by applying Stallman's analytical solution to a series of temperature time series recorded in the stream and in the streambed of the San Pedro River. Temperature measurements were recorded at four spatial extents using a nested hierarchy during four different periods since last flood. Time since last flood did not affect vertical fluxes significantly, but fluxes exhibited spatial dependence at lengths of 6-24 m. Stream geomorphic features influenced the magnitude of vertical fluxes; runs were more downwelling than riffles. The data suggests that the spatial distribution of vertical fluxes becomes more homogeneous as time since last flood increases.
| Identifer | oai:union.ndltd.org:arizona.edu/oai:arizona.openrepository.com:10150/193384 |
| Date | January 2008 |
| Creators | Soto-Lopez, Carlos Daniel |
| Contributors | Meixner, Thomas, Meixner, Thomas |
| Publisher | The University of Arizona. |
| Source Sets | University of Arizona |
| Language | English |
| Detected Language | English |
| Type | text, Electronic Thesis |
| Rights | Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. |
Page generated in 0.0027 seconds