T203 Applications of Geophysics to Solve Near-Surface Geological Problems (Posters)

Tuesday, 11 October 2022
2:00 PM - 6:00 PM
Exhibit Hall F


SALINITY MAPPING OF GROUNDWATER IN AND AROUND OIL FIELDS WITH HETEROGENEOUS TEMPERATURE FIELDS

Paper number: T203-6
Program: Technical Sessions
Time: 2:00 PM – 6:00 PM


Authors


Abstract

Using borehole geophysics to map groundwater total dissolved solids (TDS) has become an important method for monitoring groundwater TDS in and around oil fields. This method typically uses a series of empirical relationships, including Archie's equation, to estimate TDS from deep-reading formation resistivity. The method also involves an equation that relates water resistivity to TDS and the temperature of the water; therefore, the method requires an understanding of the temperature field. In some oil fields, temperature follows the local geothermal gradient, which can be estimated using bottom-hole temperature measurements. However, in thermal oil fields, temperature perturbations arising from steam injection prevent accurate TDS calculations unless temperature is observed and modeled.

Here, we present a new method of modeling the temporal and spatial structure of TDS that uses available borehole resistivity and porosity data along with temperature logs from nearby observation wells. This method uses a Gaussian process to jointly model non-collocated resistivity, porosity, temperature, and TDS observations. The model yields volume maps of all four quantities.

We apply this method to the San Ardo Oil Field in Monterey County, California, a field that has undergone extensive thermal-enhanced oil recovery. This oil field has an unusual number of publicly available temperature logs spanning 2006 to 2019, allowing understanding of the temporal and spatial temperature structure during this time. We expect techniques developed here will apply to other thermal oil fields in the future.


Geological Society of America Abstracts with Programs. Vol. 54, No. 6

doi: 10.1130/abs/2022AM-381529

© Copyright 2022 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.