Skip to main content
Log in

Detailed hydraulic head profiles as essential data for defining hydrogeologic units in layered fractured sedimentary rock

  • Original Article
  • Published:
Environmental Geology

Abstract

This paper describes a study in southern Wisconsin where vertical hydraulic head profiles measured in exceptional detail provided the key data for defining hydrogeologic units (HGUs) in a layered sequence of sandstone, siltstone, shale, and dolostone. The most important data were obtained from corehole MP-6 which was cored 131 m into bedrock and instrumented using a Westbay® multilevel system with 36 depth discrete monitoring intervals. The resulting head profile is consistant over time and shows eight distinct inflections in hydraulic head. Several of the inflections occur between adjacent permeable units and are likely due to poor vertical connectivity of fracture sets rather than distinct lower permeability layers or aquitards in the conventional sense. No other type of data was capable of identifying the position of such distinct hydrogeologic features. These zones of abrupt head loss provide the primary dataset for delineation of eleven HGUs at MP-6 and are supported by less detailed head profiles at other locations. Although the detailed head profiles are essential, core logs and geophysical logs from other boreholes are nessessary to fully establish the lateral continuity of the HGUs.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Anderson MP (1989) Hydrogeologic facies models to delineate large-scale spatial trends in glacial and glaciofluvial sediments. Geol Soc Am Bull 101(4):501–511

    Article  Google Scholar 

  • ASTM (2004) Standard test for permeability of rocks by flowing air, D 425–04, ASTM International, West Conshohocken

  • Aswasereelert W (2005) Facies distribution and stacking of the Eau Claire Formation, Wisconsin: implications of thin shale-rich strata in fluid flow. Master’s thesis, Department of Geology and Geophysics, University of Wisconsin, Madison

  • Austin DC (2005) Hydrogeologic controls on contaminant distribution within a multi-component DNAPL zone in a sedimentary rock aquifer in south central Wisconsin. Master’s thesis, Earth Sciences Department, University of Waterloo

  • Black WH, Smith HR, Patton FD (1986) Multiple-level ground water monitoring with the MP system. Paper presented at proceedings of the surface and borehole geophysical methods and ground water instrumentation conference and exposition, Denver, Colorado, 15–17 October 1986, NWWA, Dublin, Ohio

  • Bradbury KR, Swanson SK, Krohelski JT, Fritz AK (1999) Hydrogeology of Dane County, Wisconsin, WGNHS open-file report 1999–04. Madison, Wisconsin

    Google Scholar 

  • Bradbury KR, Gotkowitz MB, Hart DJ, Eaton TT, Cherry JA, Parker BL, Borchardt MA (2006) Contaminant transport through aquitards: technical guidance for aquitard assessment. Denver, Colorado, Awwa Research Foundation

  • Cherry JA, Johnson PE (1982) A multilevel device for monitoring in fractured rock. Ground Water Monit Rev 2(3):41–44

    Article  Google Scholar 

  • Cherry JA, Parker BL, Bradbury KR, Eaton TT, Gotkowitz MB, Hart DJ, Borchardt MA (2006) Contaminant transport through aquitards: a state-of-the-science review. Denver, Colorado, Awwa Research Foundation

  • Cherry JA, Parker BL, Keller C (2007) A new depth-discrete multilevel monitoring approach for fractured rock. Ground Water Monit Remed 27(2):57–70

    Article  Google Scholar 

  • Clayton L, Attig JW (1997) Pleistocene geology of Dane County, Wisconsin, WGNHS Bulletin 95. Madison, Wisconsin

    Google Scholar 

  • Cline DR (1965) Geology and ground-water resources of Dane County, Wisconsin, USGS water-supply paper 1779-U. United States Government Printing Office, Washington DC

    Google Scholar 

  • Collins RE (1961) Flow of fluids through porous materials. Reinhold Publishing, New York

    Google Scholar 

  • Cooke ML, Underwood CA (2001) Fracture termination and step-over at bedding interfaces due to frictional slip and interface opening. J Struc Geol 23(2–3):223–238

    Article  Google Scholar 

  • Cooke ML, Simo JA, Underwood CA, Rijken P (2006) Mechanical stratigraphic controls on fracture patterns within carbonates and implications for groundwater flow. Sediment Geol 184(3–4):225–239

    Article  Google Scholar 

  • Davis SN, DeWiest RJM (1966) Hydrogeology. Wiley, New York

    Google Scholar 

  • Einarson MD (2006) Multilevel ground-water monitoring. In: Nielsen DM (ed) Practical handbook of environmental site characterization and ground-water monitoring, vol 11. CRC Press, Boca Raton, pp 808–845

  • Einarson MD, Cherry JA (2002) A new multilevel ground water monitoring system using multichannel tubing. Ground Water Monit Remediat 22(4):52–65

    Article  Google Scholar 

  • Emrich GH (1966) Ironton and Galesville (Cambrian) sandstone in Illinois and adjacent areas, Illinois State Geological Survey Circular 403. Urbana, Illinois

  • Freeze RA, Witherspoon PA (1966) Theoretical analysis of regional groundwater flow: 1. Analytical and numerical solutions to the mathematical model. Water Resour Res 2(4):641–656

    Article  Google Scholar 

  • Freeze RA, Witherspoon PA (1967) Theoretical analysis of regional groundwater flow. 2. Effect of water-table configuration and subsurface permeability variation. Water Resour Res 3(2):623–634

    Article  Google Scholar 

  • Friedman M, Kwon O, French VL (1994) Containment of natural fractures in brittle beds of the Austin Chalk. In: Balkema A.A Paper presented at proceedings of the 1st North American rock mechanics symposium, rock mechanics, models and measurements, challenges from industry, Austin, TX, 1–3 June 1994, Rotterdam, Netherlands

  • Gross MR (1993) The origin and spacing of cross joints: examples from the Monterey Formation, Santa Barbara coastline, California. J Struc Geol 15(6):737–751

    Article  Google Scholar 

  • HSI GeoTrans (1999) DNAPL removal report, Hydrite Chemical Co., Cottage Grove, Wisconsin, project no. 301583125/N152. Brookfield, Wisconsin

    Google Scholar 

  • Hydro-Search Inc. (1989) RCRA facility investigation, task 1 current conditions report, Avganic Industries, Inc. solvent reclamation facility, Cottage Grove, Wisconsin, project no. 158E09293. Brookfield, Wisconsin

  • Krohelski JT, Bradbury KR, Hunt RJ, Swanson SK (2000) Numerical simulation of groundwater flow in Dane county, Wisconsin, WGNHS Bulletin 98. Madison, Wisconsin

    Google Scholar 

  • Macfarlane PA, Doveton JH, Feldman HR, Butler JJ Jr, Combes JM, Collins DR (1994) Aquifer/aquitard units of the Dakota aquifer system in Kansas: methods of delineation and sedimentary architecture effects on ground-water flow and flow properties. J Sediment Res B64(4):464–480

    Google Scholar 

  • Mai H, Dott RH Jr (1985) A subsurface study of the St Peter sandstone in southern and eastern Wisconsin, WGNHS Information Circular Number 47. Madison, Wisconsin

    Google Scholar 

  • Maxey GB (1964) Hydrostratigraphic units. J Hydrol 2(2):124–129

    Article  Google Scholar 

  • McLeod RS (1975) A digital-computer model for estimating drawdowns in the sandstone aquifer in Dane County, Wisconsin, WGNHS Information Circular 28. Madison, Wisconsin

    Google Scholar 

  • Meinzer OE (1923) Outline of ground-water hydrology, with definitions, US Geological Survey Water-Supply Paper 494. United States Government Printing Office, Washington, DC

    Google Scholar 

  • Meyer JR (2005) Migration of a mixed organic contaminant plume in a multilayer sedimentary rock aquifer system. Master’s thesis, Earth Sciences Department, University of Waterloo

  • Muldoon MA (1999) Data from slug tests in the Silurian dolomite using a short-interval straddle-packer assemblage, WGNHS Open-File Report 1999–01. Madison, Wisconsin

    Google Scholar 

  • Muldoon MA, Simo JA, Bradbury KR (2001) Correlation of hydraulic conductivity with stratigraphy in a fractured-dolomite aquifer, northeastern Wisconsin, USA. Hydrogeol J 9(6):570–583

    Article  Google Scholar 

  • Odom EI (1975) Feldspar—grain size relations in Cambrian arenites, upper Mississippi Valley. J Sediment Petrol 45(3):636–650

    Google Scholar 

  • Odom EI (1978) Lithostratigraphy and sedimentology of the Lone Rock and Mazomanie Formations, upper Mississippi valley. In: Lithostratigraphy, petrology, and sedimentology of Late Cambrian–Early Ordovican Rocks Near Madison, Wisconsin. WGNHS Field Trip Guide Book Number 3. Madison, Wisconsin

  • Odom EI, Ostrom ME (1978) Lithostratigraphy, petrology, sedimentology, and depositional environments of the Jordan Formation near Madison, Wisconsin. In: Lithostratigraphy, petrology, and sedimentology of Late Cambrian–Early Ordovican Rocks Near Madison, Wisconsin. WGNHS field trip guide book number 3. Madison, Wisconsin

  • Ostrom ME (1978) Stratigraphic relationships of Lower Paleozoic Rocks of Wisconsin. In: Lithostratigraphy, petrology, and sedimentology of Late Cambrian–Early Ordovican Rocks Near Madison, Wisconsin. WGNHS field trip guide book number 3. Madison, Wisconsin

  • Palmquist RC (1969) The configuration of the Prairie du Chien-St Peter contact in southwestern Wisconsin: an example of an integrated geological–geophysical study. J Geol 77:694–702

    Article  Google Scholar 

  • Parker BL, Cherry JA, Swanson BJ (2006) A multilevel system for high-resolution monitoring in rotasonic boreholes. Ground Water Monit Remed 26(4):57–73

    Article  Google Scholar 

  • Poeter E, Gaylord DR (1990) Influence of aquifer heterogeneity on contaminant transport at the Hanford Site. Ground Water 28(6):900–909

    Article  Google Scholar 

  • Renshaw CE, Pollock DW (1995) An experimentally verified criterion for propagation across unbounded frictional interfaces in brittle, linear elastic materials. Int J Rock Mech Min Sci Geomechan Abstr 32(3):237–249

    Article  Google Scholar 

  • Rijken P, Cooke ML (2001) Role of shale thickness on vertical connectivity of fractures: application of crack-bridging theory to the Austin Chalk, Texas. Tectonophysics 337(1–2):117–133

    Article  Google Scholar 

  • Runkel AC, Tipping RG, Green JA, Mossler JH, Alexander SC, Alexander EC Jr (2003) Hydrogeology of the Paleozoic bedrock in southeastern Minnesota, Minnesota geological survey report of investigations 61. St Paul, Minnesota, University of Minnesota

  • Runkel AC, Tipping RG, Alexander EC Jr, Alexander SC (2006) Hydrostratigraphic characterization of intergranular and secondary porosity in part of the Cambrian sandstone aquifer system of the cratonic interior of North America: improving predictability of hydrogeologic properties. Sediment Geol 184(3–4):281–304

    Article  Google Scholar 

  • Seaber PR (1988) Hydrostratigraphic units. In: Back W, Rosenshein JS, Seaber PR (eds) The geology of North America volume O-2. Boulder, Colorado, The Geological Society of America, vol 2, pp 9–14

  • Smith GL, Simo JA (1997) Carbonate diagenesis and dolomitization of the lower Ordovician Prairie du Chien Group. Geosci Wisconsin 16:1–16

    Google Scholar 

  • Sudicky EA, McLaren RG (1992) The Laplace transform Galerkin technique for large-scale simulation of mass transport in discretely fractured porous formations. Water Resour Res 28(2):499–514

    Article  Google Scholar 

  • Sutherland JL (1986) Stratigraphy and sedimentology of the upper Cambrian Lone Rock Formation, western Wisconsin-focus on the Reno Member. Master’s thesis, Department of Geology and Geophysics, University of Wisconsin, Madison

  • Swanson SK (2007) Lithostratigraphic controls on bedding-plane fractures and the potential for discrete groundwater flow through a siliciclastic sandstone aquifer, southern Wisconsin. Sediment Geol 197(1–2):65–78

    Article  Google Scholar 

  • Swanson SK, Bahr JM (2004) Analytical and numerical models to explain steady rates of spring flow. Ground Water 42(5):747–759

    Article  Google Scholar 

  • Swanson SK, Bahr JM, Bradbury KR, Anderson KM (2006) Evidence for preferential flow through sandstone aquifers in southern Wisconsin. Sediment Geol 184(3–4):331–342

    Article  Google Scholar 

  • Teufel LW, Clark JA (1984) Hydraulic fracture propagation in layered rock: experimental studies of fracture containment. Soc Petrol Eng J 24(1):19–32

    Article  Google Scholar 

  • Toth JA (1962) A theory of ground-water motion in small drainage basins in central Alberta, Canada. J Geophys Res 67(11):4375–4387

    Article  Google Scholar 

  • Toth JA (1963) A theoretical analysis of ground-water flow in small drainage basins. J Geophys Res 68(16):4795–4811

    Article  Google Scholar 

  • Underwood CA, Cooke ML, Simo JA, Muldoon MA (2003) Stratigraphic controls on vertical fracture patterns in Silurian dolomite, northeastern Wisconsin. AAPG Bull 87(1):121–142

    Google Scholar 

Download references

Acknowledgments

This research was funded by Hydrite Chemical Company through the University Consortium for Field-Focused Groundwater Contamination Research and by a grant from NSERC Canada. Financial and technical support was also provided by Westbay® Instruments Inc. (a division of Schlumberger Water Services), FLUTe™, and Solinst® Canada Ltd. In addition, expertise and time were provided by Carl Keller of FLUTe™, Andrew Bessant, Dave Larssen and Frank Magdich of Westbay® Instruments Inc., and Diane Austin formerly of the University of Waterloo (UW). This paper also relied on geophysical logs collected by Peeter Pehme and Daren Mortimer (Dillon Consulting, ON) and Ken Bradbury and others at the WGNHS. In addition, the numerical modeling was performed by Steve Chapman (UW). The authors also benefited from various discussions with all of the above people as well as Sue Swanson (Beloit College), Mike Noel (GeoTrans), and Tom Miazga (Hydrite Chemical Company).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Jessica R. Meyer.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Meyer, J.R., Parker, B.L. & Cherry, J.A. Detailed hydraulic head profiles as essential data for defining hydrogeologic units in layered fractured sedimentary rock. Environ Geol 56, 27–44 (2008). https://doi.org/10.1007/s00254-007-1137-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00254-007-1137-4

Keywords

Navigation