Authors: Feyan Hoffman, Roshan Abraham, Christine Fowles, Abi Conger, Scott Jenson
Mentors: Daren Nelson
Insitution: Utah Valley University
One of the least understood part of our local water budget is the interaction of groundwater into our lakes and streams. Groundwater models completed by the United States Geological Survey in 2005 for the Utah Lake Watershed suggest zones where groundwater interactions should be either discharging or recharging into our local streams, wetlands, and other water bodies. However, more recent data has suggested that many of these water interaction maps created by the model are inaccurate, and we need a better understanding of how groundwater interacts with these water bodies. Using a water budget analysis, groundwater and surface water interactions are measured by collecting discharge measurements using flow meters at different cross sections along the Provo River and its tributaries. A gaining or losing stream may swap depending on seasonal changes, such as a particular water year being dry or wet–a stream that is typically gaining may be recharging the aquifer during a dry year. The USGS model is a good basic representation of interactions between groundwater and surface water. Our data suggests that due to highly variable water levels of Utah Lake and local groundwater levels, some discharge and recharge zones in the Provo River subbasin are likely to change over time. In addition, some sections of the river may be perched and not interact with the groundwater system at all. In order for us to better manage these important resources, further analysis of flow behaviors in the Provo River and its tributaries need to be completed. This study is part of a larger study that includes adding two new permanent flow gauging stations to provide a long term record that will enable water managers to better decipher why the groundwater and surface interactions are not fitting the USGS model.