|2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM|
|Paper No. 287-4|
|Presentation Time: 8:45 AM-9:00 AM|
Field and Laboratory Studies on the Effects of Bioturbation on Porosity and Permeability In the Vadose Zone In Continental Settings: How Ichnopedologic Fabric Shapes and Modifies Aquitards, Aquicludes, Aquifers, and Tomorrow's Reservoirs and Seals
HASIOTIS, Stephen T.1, FAIRCHILD, Justin2, WALLACE, Travis2, COUNTS, John W.3, DEVLIN, J.F.3, HEMBREE, Daniel I.4, and SMITH, Jon J.5, (1) Department of Geology and Natural History Museum and Biodiversity Research Center, University of Kansas, 1475 Jayhawk Blvd, Lawrence, KS 66045, firstname.lastname@example.org, (2) Department of Geology, University of Kansas, 1475 Jayhawk Blvd, 120 Lindley Hall, Lawrence, KS 66045-7613, (3) Department of Geology, University of Kansas, 120 Lindley Hall, 1475 Jayhawk Blvd, Lawrence, KS 66045-7613, (4) Geological Sciences, Ohio University, 316 Clippinger Laboratories, Athens, OH 45701, (5) Kansas Geological Survey, 114 Parker Hall, 1930 Constant Ave, Lawrence, KS 66045-7613|
At any one time the majority of continental settings are subaerially exposed and modified by pedogenic processes that include bioturbation, produced by soil biota as one of the five soil-forming factors. Resulting fabrics are ichnopedologic in nature and have unique biophysicochemical properties compared to sediments in subaqueous settings. Three major differences exist between subaerially and subaqueous settings: 1) bioturbation in subaerial settings is produced mostly in the vadose zone; 2) bioturbation is much more penetrative in subaerial than in subaqueous settings; and 3) fabrics in subaerial settings result from abiotic and biotic pedogenic processes, whereas fabrics in subaqueous settings result mostly from biotic processes. Similar differences exist between continental and marine ichnofabrics, with the major caveat that marine bioturbation was much more prolific in the early Paleozoic. Field studies in fluvial and periaquatic palustrine settings suggest that deep penetrative traces in otherwise tight media can produce leaky aquitards and aquicludes. Bioturbation of subaerially exposed overbank and crevasse-splay deposits result in homogenized ichnopedologic fabrics with a variety of macropores and macrochannels. Laboratory experiments using earthworms, masked chafer beetle larvae, and cicada nymphs reveal a variety of ichnopedologic properties produced by organism activity in the vadose zone. Air trapped in burrows during flooding of experimental setups suggests that diagenetic alteration of bioturbated media will be heterogeneous, likely producing better-cemented media and less permeable areas compared to areas with burrows. Differential compaction of backfilled sediment within burrows and heavily bioturbated areas strongly alters the porosity and permeability of the original deposits. Observed microbial growth along burrow walls may also enhance pathways of greater permeability by binding the burrow walls that maintain these pathways after burial.
2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
General Information for this Meeting
|Session No. 287|
Exploring the Role of Endobenthic Organisms in Enhancing Porosity and Permeability of Sedimentary Aquifers and Reservoirs
George R. Brown Convention Center: 320F
8:00 AM-12:00 PM, Wednesday, 8 October 2008
Geological Society of America Abstracts with Programs, Vol. 40, No. 6, p. 440
© Copyright 2008 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.