12 Recent Advances in Hydrogeology

Thursday, 4 May 2023
1:30 PM - 5:30 PM
EC 512


ANALYZING POTENTIAL CHEMICAL VARIABILITY AND ITS RELATIONSHIP TO ENGINEERING PROPERTIES IN THE BURLINGTON-KEOKUK FORMATION, SPRINGFIELD, MISSOURI

Paper number: 12-10
Program: Theme Sessions
Time: 4:10 PM – 4:30 PM


Authors


Abstract

The Burlington-Keokuk formation is regionally extensive through Iowa and Missouri and can be roughly-correlated into Arkansas and Oklahoma. This formation is a surficial rock unit in most of the Springfield plateau. It has been studied extensively in Northeast Missouri, Iowa, and Illinois (Banner et al., 1988; Choquette et al., 1991; Hoenig, 2019). Most of these studies looked at the lateral variability of depositional facies with only a few geochemical studies. In southwest Missouri there are a limited amount of geochemical studies. In the Springfield Plateau, many caves, sinkholes, and other karst features exist which appear to relate to the hydrology within the Burlington-Keokuk and adjacent units (Dodd, 2007). This relation may be caused by the amount of chert variability or lithological changes both vertically and horizontally, going from a purely crystalline limestone with an occasional bivalve fossil to a crinoidal packstone. Another change is seen in surface streams, where beds of Burlington-Keokuk appear to serve as aquicludes at certain points in the stream, suggesting vertical variability alongside horizontal change. This project will use geochemical methods to investigate chemical variability in the Burlington-Keokuk. The project will also include LA Abrasion tests to compare chemical differences to the formation’s abrasiveness. Based on literature, it might be possible to observe differences in B/Ga ratios. Anecdotally from local quarry operators suggest that LA Abrasion tests indicate vertical variations, offering a possible chemical reason for the differences. Analytical methods will include Inductive Coupled Plasma Mass Spectrometry and LA Abrasion (ASTM Method C131), expanding as necessary. Areas of interest or question will be studied further as appropriate.

Geological Society of America Abstracts with Programs. Vol. 55, No. 3

doi: 10.1130/abs/2023NC-386683

© Copyright 2023 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.