Comprehensive Hydraulic Fracturing Study Los Angeles, California Dan Tormey, Ph.D., P.G. Cardno ENTRIX Los Angeles, California

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Comprehensive Hydraulic Fracturing Study Los Angeles, California Dan Tormey, Ph.D., P.G. Cardno ENTRIX Los Angeles, California 2013 JETC hosted by the Society of American Military Engineers HQ and the San Diego Post

Monterey Formation projected to be the richest shale oil in North America, but how to tap it? Monterey Formation projected to be the richest shale oil in North America, but how to tap it?

Environmental Baseline: Los Angeles Oil Basin is the richest in the world by size Urban growth overlain on the many producing fields

Hydraulic Fracturing Study Settlement agreement condition Independent Consultant to prepare study of feasibility and potential impacts of hydraulic fracturing and gravel packing Peer-reviewed factual information on the effects of hydraulic fracturing First Comprehensive Study to Measure All Effects of Specific Hydraulic Fracturing Events

How does hydraulic fracturing work? 500 ft 5,000 ft 10,000 ft Investigate: http://www.api.org/policy-and-issues/hf.aspx

Fluids Used in Inglewood Hydraulic Fracturing Water and Sand 99.51% Full Report: http://www.hydraulicfracturingdisclosure.org/fracfocusfind/

Ground Surface & Aerial Photo on Top Oil Field consists of shales and sandstones, folded and faulted Looking North

Frac Study Wells Sentous Surface Looking North

Nodular Surface on Top Frac Study Wells Looking North

Bradna Surface on Top Frac Study Wells Looking North

Bradna Surface with Faults Frac Study Wells Newport- Inglewood Fault Sentous Thrusts Looking North

Moynier Surface with Faults Frac Study Wells Newport-Inglewood Fault Sentous Thrusts Looking North

Rubel Surface with Faults Frac Study Wells Newport-Inglewood Fault Sentous Thrusts Looking North

Rindge Surface with Faults Frac Study Wells Newport-Inglewood Fault Sentous Thrusts Looking North

H-Sand Surface with Faults Frac Study Wells Newport-Inglewood Fault Sentous Thrusts Looking North

Frac Study Wells Vickers Surface with Faults Newport-Inglewood Fault Sentous Thrusts Looking North

UIHZ Surface with Faults Newport-Inglewood Fault Sentous Thrusts Looking North

PICO Surface with Faults Newport-Inglewood Fault Sentous Thrusts Looking North

PICO Surface w/ Discontinuous Water Bodies & Faults Discontinuous Water Bodies Newport-Inglewood Fault Sentous Thrusts Looking North

Discontinuous Water Bodies Vickers Reservoir Hydrocarbon Seal with Faults Newport-Inglewood Fault Hydrocarbon Seal Sentous Thrusts Looking North

Discontinuous Water Bodies A Newport Inglewood Fault Pico Surface (Freshwater Base) Hydraulic Fracturing ~7,700 ft below Base of Fresh Water Impermeable Hydrocarbon Seal Well 1 Microseismic Well 2 Microseismic The zone affected by hydraulic fracturing is approximately 7,700 feet beneath fresh water (1 ½ miles)

Discontinuous Water Bodies A Newport Inglewood Fault Pico Surface (Freshwater Base) Sentous II Thrust Fault Sentous IIIB Thrust Fault Well 1 Microseismic Events & Frac Model Impermeable Hydrocarbon Seal ~ 7,700 ft. Vickers H Sand Sentous Surface Rindge Surface Well 1 Microseismic Well 2 Microseismic Well 2 Microseismic Events & Frac Model Sentous Surface Rubel Surface

Hydrogeology

Discontinuous Water Bodies Pico Surface (Freshwater Base) Hydraulic Fracturing ~7,700 ft below Base of Fresh Water Impermeable Hydrocarbon Seal Well 1 Microseismic Well 2 Microseismic

Water Quality 2/3 of water for the vicinity of Oil Field comes from the Colorado River or Northern California Not affected by hydraulic fracturing Remainder is from surface water or groundwater sources greater than 1.5 miles away All public water is: Tested quarterly and reported Must meet drinking standards Further Information: http://www.westbasin.org/waterreliability2020/groundwater/overview

Groundwater quality consistently meets drinking water standards, before and after hydraulic fracturing

Ground Movement and Induced Seismicity Surface II. Vibration Monitoring III. CalTech Accelerometer Hydraulic fracturing produces microseismic effects: Richter magnitude of -2 to -3 Tectonic quakes are larger and deeper ~8,500 ft below ground surface Induced seismicity in Ohio and elsewhere is linked to wastewater injection Field has operated a water flood since 1971 without seismicity Hydraulic fracturing is insufficient to induce tectonic earthquakes I. Microseismic Monitoring Looking North Ongoing monitoring

Methane Migration Oil Field is adjacent to City of LA Methane Zone May be included in a County-wide program Methane in shallow soil gas from Inglewood, if detected, has been biogenic Methane detected in groundwater has been thermogenic

Study Findings: monitoring before, during, and after hydraulic fracturing did not detect effects to: Hydrogeology Ground Movement Water Use Induced Seismicity Water Quality Methane (soil gas and Containment of groundwater*) Fractures Air Emissions Well Integrity Noise Slope Stability Vibration Subsidence Community Health* Oil Field has ongoing monitoring for most of these resource categories

Questions and Discussion Dan Tormey, Ph.D., P.G. daniel.tormey@cardno.com (424) 832-1303 Cardno ENTRIX Los Angeles, California