NS43A-1952
Basin-fill Aquifer Modeling with Terrestrial Gravity: Assessing Static Offsets in Bulk Datasets using MATLAB; Case Study of Bridgeport, CA
Thursday, 17 December 2015
Poster Hall (Moscone South)
Elijah Thomas Mlawsky1,2, John N Louie3, Greg Pohll1, Chad W Carlson4 and Richard J Blakely5, (1)Desert Research Institute Reno, Reno, NV, United States, (2)University of Nevada, Reno, Reno, NV, United States, (3)University of Nevada Las Vegas, Las Vegas, NV, United States, (4)University of Nevada Reno, Reno, NV, United States, (5)USGS Western Regional Offices Menlo Park, Menlo Park, CA, United States
Abstract:
Understanding the potential availability of water resources in Eastern California aquifers is of critical importance to making water management policy decisions and determining best-use practices for California, as well as for downstream use in Nevada. Hydrologic well log data can provide valuable information on aquifer capacity, but is often proprietarily inaccessible or economically unfeasible to obtain in sufficient quantity. In the case of basin-fill aquifers, it is possible to make estimates of aquifer geometry and volume using geophysical surveys of gravity, constrained by additional geophysical and geological observations. We use terrestrial gravity data to model depth-to-basement about the Bridgeport, CA basin for application in preserving the Walker Lake biome. In constructing the model, we assess several hundred gravity observations, existing and newly collected. We regard these datasets as “bulk,” as the data are compiled from multiple sources. Inconsistencies among datasets can result in “static offsets,” or artificial bull’s-eye contours, within the gradient. Amending suspect offsets requires the attention of the modeler; picking these offsets by hand can be a time-consuming process when modeling large-scale basin features. We develop a MATLAB script for interpolating the residual Bouguer anomaly about the basin using sparse observation points, and leveling offset points with a user-defined sensitivity. The script is also capable of plotting gravity profiles between any two endpoints within the map extent. The resulting anomaly map provides an efficient means of locating and removing static offsets in the data, while also providing a fast visual representation of a bulk dataset. Additionally, we obtain gridded basin gravity models with an open-source alternative to proprietary modeling tools.