Groundwater Sequence Stratigraphy:

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Groundwater Sequence Stratigraphy: A Geology-based Approach for Developing Accurate and Representative Hydrogeologic Conceptual Models for Successful Groundwater Sustainability Plans Rick Cramer, Burns & McDonnell Chris Bonds, CA-DWR; Mike Shultz, Burns & McDonnell; Colin Plank, Burns & McDonnell; Galen Kenoyer, Burns & McDonnell May 4, 2017 1

Each Plan shall include a descriptive hydrogeologic conceptual model of the basin based on technical studies and qualified maps that characterizes the physical components and interaction of the surface water and groundwater systems in the basin 2

From BMP Document Geologic cross-sections should be constructed by a professional geologist A full understanding of, and appreciation for, the variety of depositional environments, like sequence stratigraphy, is needed to construct accurate geological cross sections. 3

Focus on Geology in the Oil Industry 1960s In the early days of exploration and production production was limited by facilities capacity (engineering focus). However, as production declined the geology became increasingly critical for economical operations. Billions of dollars have been invested in research and development of stratigraphic controls on fluid flow. 4

Focus on Geology in Environmental Industry 2013 At least 126,000 sites across the U.S. have contaminated groundwater that requires remediation Over 12,000 of these sites are considered "complex" due to inherent geologic complexities, restoration within the next 50-100 years is likely not achievable. Alternatives for Managing the Nation's Complex Contaminated Groundwater Sites National Academy of Sciences Committee on Future Options for Management in the Nation's Subsurface Remediation Effort, 2013 5

Environmental Sequence Stratigraphy Technology Considered Best Practice by US EPA US EPA Technical Issue Paper presents Environmental Sequence Stratigraphy (ESS) as an emerging best practice for Conceptual Site Models (Burns & McDonnell) 6

Water supply studies based on assumptions of homogeneous and isotropic conditions, steady-state observations Groundwater Production Industry Traditional Approach to the Subsurface Groundwater gradient = groundwater flow 7

Geology-Based HCM: Groundwater Sequence Stratigraphy (GSS) Process Borehole Log to Graphic Grainsize Log Grain-size increasing Map Cross Section 0 Clay Gravel 100 Uncon Depth (Ft - MSL) 200 300 400 Uncon 1 Determine depositional environment which is the foundation to the GSS evaluation 2 Leverage existing lithology data: format to emphasize vertical grainsize distribution 3 Predict and Map in 3D the subsurface conditions away from the data points 8

GSS is Pattern Recognition Depositional environments have distinctive vertical grain size distributions 9

GSS is Pattern Recognition Depositional environments have distinctive vertical grain size distributions 1

GSS is Pattern Recognition Depositional environments have distinctive vertical grain size distributions 1

GSS is Pattern Recognition Depositional environments have distinctive vertical grain size distributions 1

GSS is Pattern Recognition Depositional environments have distinctive vertical grain size distributions 1

GSS is Pattern Recognition and the associated sand bodies have characteristic/predictable dimensions and continuity. Stratigrapher using GSS methodology can predict subsurface conditions away from the data points. 1

Unleashing the Power of Existing Site Data USCS is not a geologic description of the subsurface Different geologists Different drilling methods Different sampling intervals Etc 1

How to tease out detailed stratigraphy with existing data Existing data is formatted for stratigraphic interpretation Reveals the hidden stratigraphic information that is available with existing lithology data 1

How to tease out detailed stratigraphy with existing data This SM interval is a fine to medium grained Silty Sand 1

How to tease out detailed stratigraphy with existing data This SM interval is a fine to coarse grained Silty Sand with gravel, representative of a channel deposit. 1

How to tease out detailed stratigraphy with existing data 1. Reformatting existing data to identify sequences, and 2. Applying facies models, stratigraphic rules of thumb to correlate and map the subsurface, predict character of heterogeneity present Permeable streaks commonly at bases of channel complex Fining-upward cycles indicative of channel-fills 500 feet Example from GW site in S. CA, USA 1

Mapped Buried Sand Channels 2

USCS-Based Cross Section Mapped Sand Channels ESS-Based Cross Section vs 2

Groundwater Production Projects Groundwater Contamination Projects 2

Dominguez Gap Seawater Intrusion Barrier, West Coast Basin WRD 2

Dominguez Gap Barrier Project 2

Dominguez Gap Barrier Project 2

Dominguez Gap Seawater Intrusion Barrier, West Coast Basin South North 1000 m Layer Cake aquifer stratigraphy: continuous layers From Ehman and Edwards (2014) Aquifer architecture is much more complicated than previously understood. Implications for Seawater intrusion pathways Contaminant migration pathways 2

2

Livermore Groundwater Basin - Zone 7 Water Agency 2

2

3

3

Focus on Geology in Groundwater Production Industry?? 3