OFR 2019–1114: Multiple-Well Monitoring Site Adjacent to the Lost
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Prepared in cooperation with California State Water Resources Control Board Multiple-Well Monitoring Site Adjacent to the Lost Hills Oil Field, Kern County, California The U.S. Geological Survey (USGS), in cooperation with the California State Study Area Water Resources Control Board, is evaluating several questions about oil and gas The LHSP is in the Kern development and groundwater resources in California, including (1) the location of County subbasin of the San Joaquin groundwater resources; (2) the proximity of oil and gas operations and groundwater and Valley groundwater basin situated the geologic materials between them; (3) evidence for or against fluids from oil and gas on the southern end of the Tulare sources in groundwater; and (4) the pathways or processes responsible when fluids from Lake Hydrologic Region (California oil and gas sources are present in groundwater (U.S. Geological Survey, 2019). As part Department of Water Resources, 2016; of this evaluation, the USGS installed a multiple-well monitoring site in the southern fig. 1). The LHSP is approximately San Joaquin Valley near Lost Hills, California, adjacent to the Lost Hills oil field 1,400 feet (ft) east and downgradient (fig. 1). Data collected at the Lost Hills multiple-well monitoring site (LHSP) provide from the Lost Hills oil and gas field information about the geology, hydrology, geophysics, and geochemistry of the aquifer administrative boundary. system, thus enhancing understanding of relations between adjacent groundwater and Primary water-bearing units that the Lost Hills oil field in an area where there is little groundwater data.This report comprise the major aquifers on the presents construction information for the LHSP and initial geohydrologic data collected west side of the Tulare Lake region from the site. include alluvial and river sediments of Holocene age, older alluvium and Figure 1. Location of Lost Hills multiple-well monitoring well site (LHSP) and selected other terrace deposits of Pleistocene age, wells in relation to the Lost Hills oil field, Kern County, California. and Pliocene-Pleistocene-age Tulare Formation (Woodring, 1940; California Department of Water Resources, 2015). 120° 45' 30' AR C R C EXPLANATION Area of historical produced water storage Oil and gas field administrative boundary 45' County boundary s! Lost Hills multiple-well monitoring site (LHSP) Disposal well 5 33 Injection well s! LHSP Oil and gas production well Plugged or buried well CALIFORNIA 35°37'30" Sacramento Tulare Lake Lost Hills Hydrologic 46 Region Modesto San Joaquin Valley groundwater basin Corcoran Bakersfield Kern County subbasin San Diego Base modified from U.S. Geological Survey and other Federal and State digital data, Oil and gas well data from the California Department of Conservation, 2018. various scales; Albers Equal-Area Conic projection, standard parallels are 29°30’ N. and 45°30’ N.; North American Datum of 1983 0 1 2 3 4 5 MILES 0 1 2 3 4 5 KILOMETERS U.S. Department of the Interior ISSN 2331-1258 (online) Open-File Report 2019–1114 U.S. Geological Survey https://doi.org/10.3133/ofr20191114 February 2020 Most groundwater studies of the Central from a range of historical and current oil natural gamma, resistivity (16- and Valley define hydrogeologic units— and gas development activities. These 64-inch), spontaneous potential (SP), aquifers and confining layers, rather than activities include surface spills, leakage electromagnetic induction (conductivity), stratigraphic units (Faunt, 2009). At the of produced water from disposal ponds, full wave sonic (delta-T), and Nuclear LHSP, the stratigraphic units are defined; injection of fluids into the subsurface for Magnetic Resonance (NMR) porosity therefore, the aquifer system is discussed enhanced recovery and produced-water (fig. 2). Logging in the small-diameter as the alluvial and Tulare aquifer systems disposal, and potential introduction of pilot hole was advantageous because even though they function regionally as preferential pathways through leaky or it allowed for higher-quality logs to be a single water-yielding unit. Numerous improperly abandoned oil and gas wells collected than in the larger diameter lenses of fine-grained sediments are or test holes (Davis and others, 2018a; holes. Well-screen and filter-pack distributed throughout the San Joaquin Gillespie and others, 2019b). intervals were selected based on the Valley; these generally constitute more The land surface and confining clay geophysical and lithologic data. The than 50 percent of the total thickness layers slope downward gradually from pilot hole was then reamed to increase of the valley fill (Faunt, 2009). Faunt the Lost Hills oil field toward the LHSP the borehole diameter to allow for the (2009) also noted that sediments in the borehole (Gillespie and others, 2019b). construction of the five-well monitoring western part of the San Joaquin Valley The LHSP is approximately 4,500 ft site. The deepest well (LHSP #1) was are generally finer-grained than sediments from the nearest active oil well, 4,500 ft constructed with 2.5-inch-diameter located to the east. from the nearest active steam flood well polyvinyl chloride (PVC) casing to allow The primary confining unit in (injection of steam for enhanced recovery for future geophysical logging, and the the aquifer system of the Tulare Lake of oil), 6,000 ft from the nearest produced shallower four wells were constructed Hydrologic Region is the Corcoran water disposal well, and 7,000 ft from with 2-inch-diameter PVC casing. The Clay (Frink and Kues, 1954) and its the nearest water flood well (injection of wells were installed with screened equivalent, the E-clay of Croft (1972). produced water for enhanced recovery intervals from 1,780 to 1,800 (LHSP For the purposes of this brief discussion, of oil). There is a high concentration of #1); 1,110 to 1,130 (LHSP #2); 700 to the Corcoran Clay and the Corcoran oil-production activities near the LHSP. 720 (LHSP #3); 490 to 510 (LHSP #4); Clay equivalent are simply referred to as Activities within 2 mi to the south and and 210 to 230 (LHSP #5) ft bls (fig. 2; the Corcoran Clay. The Corcoran Clay west of the LHSP include 22 water- table 1). A filter pack of #3 sand was underlies approximately the western disposal wells, 1,020 steam-flood wells, installed around each screen, and a low- two thirds of the San Joaquin Valley and 22 water-flood wells that are active, permeability bentonite grout was placed extending from the southern edge of the inactive, or new; 1,480 oil- or gas- in the depth intervals between the filter valley, near Kern Lake (not shown), to production wells that are active, inactive, packs to isolate each of the wells. north of Modesto (Faunt, 2009). The or new; 832 wells that are plugged or After construction was completed, Corcoran Clay is thicker in an area buried; and 3 areas where produced the wells were developed by using between Lost Hills and Corcoran, located water-storage ponds have been or are airlifting and a surging technique with about 35 miles (mi) to the north, and currently located (California Department compressed air to remove drilling fluid may be as thick as 200 ft approximately of Conservation, 2018). and develop the filter pack surrounding 14 mi north of Lost Hills (Faunt, 2009). each monitoring well. The field The Corcoran Clay is between 272 and Drilling and Well Installation parameters that were recorded during the 338 feet below land surface (ft bls) at process include specific conductance, pH, the LHSP. Locally, Faunt (2009) and The LHSP pilot borehole, with a water temperature, apparent color, and diameter ranging from 8 1/ to 7 5/ inches, Gillespie and others (2019b) show the 2 8 turbidity. Well development continued western edge of the clay is generally was drilled to a depth of 1,880 ft until no discernible drilling mud was coincident with the eastern edge of the bls during March 2018 using direct present and field parameters were Lost Hills oil and gas field. mud-rotary drilling techniques. Drill stabilized. The average flow rate and The LHSP location was selected cuttings were collected throughout the development time was used to estimate to provide better information regarding drilling process and analyzed (along the total discharge and total purge vertical and lateral changes in with notes from the on-site geologist) volumes of the casing and sand pack groundwater gradients and water quality to summarize the lithology (fig. 2) (table 2). After well development, the of the alluvial and Tulare aquifer system. following the procedures described by turbidity of all wells, except LHSP #1, The site is located east of the Lost Everett and others (2013). To assist was below 10 nephelometric turbidity Hills field and downgradient from the in the identification of lithologic and units (NTU; table 2). The higher turbidity intensively developed oil field where stratigraphic units, geophysical logging in LHSP #1, 105 NTU, is assumed to the potential presence of oil-field fluids of the borehole was done before well be a result of the formation because in overlying and adjacent groundwater construction using techniques described the appearance of the water resembled zones exist either from naturally by Keys and MacCary, 1971; Shuter the color of the clays and silts of the existing oil and gas shows in aquifers and Teasdale, 1989; Keys, 1990; and formation/cuttings samples collected in proximity to oil fields or resulting Kenyon and others, 1995. Geophysical during drilling. logs