Ross Dress For Less Explosion Investigation Los Angeles California 1985 Meehan Hamilton

Oil field methane leak explodes injuring store employees and customers burn on the street for days
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    December 1969
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CAUSE OF THE 1985 ROSS STORE EXPLOSION AND OTHER GAS VENTINGS, FAIRFAX DISTRICT, LOS ANGELES Douglas H. Hamilton Principal Geologist Earth Sciences Associates. Inc. 701 Welch Road Palo Alto. California 94304 Richard L. Meehan Consulting Civil Engineer 70 I Welch Road Palo Alto. California 94304 INTRODUCTION Late in the afternoon of March 24, 1985, methane gas that had been accumulating ignited in an auxiliary room of the Ross Dress-For-Less Department Store located on Third Street. in the Wilshire-Failiax District of Los Angeles. The resulting explosion blew out the windows and pa;tially col- lapsed the roof of the structure, reduced the store interior to a heap of twisted metal and resulted in injuries requiring hospi- tal treatment of twenty-three people. Police closed off four blocks around an eerie scene of spouting gas flames that con- tinued through the night. In the following days, a drill rig brought to the site was used to test for possible gas accumulations in the alluvial soil beneath the store. A "pocket" of pressurized gas was en- countered at a depth of 42 feet beneath the parking lot be- tween the store building and Third Street. Gas was also en- countered in several other borings at the site in smaller quan- tities and at lower pressures. Pressure gauges, control valves, and. on the hole where the high pressure pocket was en- countered. a valved flare pipe, were installed. Following a brief period during which gas was flared and bled off into the air, the anomalous gas condition at the Ross Store site gradually declined to the norma! gas concentrations charac- teristic of the local area. In 1989 another venting incident occurred. this time at several sites on the north side of Third Street. This second venting fortunately was detected in time, and did not ignite. In this case, water and silt were ejected from outdoor vents along with the gas, in addition to accu- mulation of dangerous levels of gas in several buildings. A blow-out crater several feet deep, from which din and small stones were ejected several feet into the air was formed during this episode which lasted about 24 hours. The setting of the accident- an old-world Levantine market place a few miles from Hollywood; the famed tarry grave- yard of the sabre-toothed tigers; pillars of frre dancing in the darkened streets - these biblical images attracted attention of the press, the bar, and local politicians. And yet, three months later when a hastily convened panel of experts an- nounced that the event was caused by digestive rumblings of an ancient and invisible swamp the whole thing had been mostly forgotten, the explanation accepted as yet another pro- duction of Los Angeles' quirky environment. Outside of a lawsuit that was settled quietly in 1990, the possibility that the accident was caused by the knowing agency of Los An- geles' lesser known industry or that the official report of the experts, rather than being a serious statement of the scientific community, was a heavily edited script with a happily blame- less ending, was not made to the public, as we shall proceed to do here. THE SETTING - TAR PITS AND OIL FIELDS IN THE URBAN ENVIRONMENT The vicinity of the gas ventings lies within a sloping plain between the easternmost Santa Monica Mountains and the isolated topographic high of the Baldwin Hills (Fig. I). The area drains via Ballona Creek. which cuts through Ballona Gap to the coastal plain fringing Santa Monica Bay. The Ross Store is in a neighborhood that has been attracting at- tention since the mid-Pleistocene on account of its hydrocar- Figure 1. Location and Regional Setting bon wealth; the La Brea tar pits are about two blocks to the south. The old Salt Lake oil field, once the biggest producing field in California, directly underlies and extends west and east of the i..--nmediate neighborhood (Fig. 2). Methane gas has been a ubiquitous feature of this area so that urban engineering for both public and private facilities has required consideration of the hazards of flammable gas present in the soil. Ex- amples include the excavation for the L.A. County Flood Control Pan Pacific storm runoff basin and park, the storm drain along Third Street, and the (formerly planned but since relocated) L.A. Metro subway along Fairfax Avenue. Before the Ross Store explosion in 1985, there was general acceptance of the view that the hydrocarbon presence in the surface and shallow subsurface environment had its source iii. the underlying reservoir of the Salt Lake oil field. Upward migration of oil from parts of this reser"'oii was thought to be the source of the "breas" or tar accumulations that had happed many of the Pleistocene residents of the area (Shaw and Quinn, 1986). Gas known to be present at shallow depth within the alluvial soil was likewise considered to have escaped from the reservoir and migrated toward the surface (Converse et al., 1981). The surface accumulation of the re- sidual bitumin "breas" (Spanish for pitch) led to the dis- covery of the once-prolific Salt Lake oil field in 1902. As the field developed, mairJy before 1917, furt .... "ter conl .. Taunica- tion between the confmed oil, gas, and water in the reservoir Source: C.D.O.G. Map 118 , .... ., . r ) Approl!>ro>rimate Alea nf Poa·1 9$1 Oil Fleld e Site of Gas Venting E .. nl Figure 2. Wilshire-Fairfax area and the Salt Lake Oil Field ... ... "'" " -eo... "'• ... ... ..,5 ... .. .. .. .. . ... .. . . Figure 3 Abandoned and Active Oil Welts in the Salt Lake Oil Field 146 C.AUSE OF THE !985 ROSS STORE EXPLOSION AND OTHER GAS VEl\TTJJ--JGS. DISTRICT. LOS and the surface was established by drilling more than 450 wells (Fig. 3). Nearly 50 million barrels of oil were brought to the surface through these wells. Most was conveyed off- site to markets, initially in tanks and thereafter mostly by pipeline, but some was ·spilled and left in sump basins that were then a standa...rd feature of the production system. By the 1930s, the urban development value of the land overlying the Salt Lake oil field exceeded its value as a production site for a declining oil field, and the field was largely abandoned. The legacies of a thirty-year oil boom included several large family and corporate fortunes, a few square miles of land where the natural upward hydrocarbon migration was compli- cated by the presence of hundreds of abandoned wells plus numerous filled sumps and covered-over spills, all underlain by a partially depleied hydrocarbon reservoir. Following the abandonment of most oil production, the area was rapidly covered by the homes, apartments, businesses and industrial facilities that exist today (Fig. 2). The remaining and most notable hydrocarbon presence is manifest in that popular and scientifically important exhibit of the "La Brea Fossil Pits" and Page Museum in Hancock Park on Wilshire Boulevard near Fairfax Avenue. Meanwhile, beneath this urban environment, t . ~ e underlying Salt Lake oil field was again tapped, in 1961, through skillful application of modem oil drilling techniques and production technology. This time, however, the entire surface installa- tion was contained in an unobtrusive, screened complex covering only one acre. This compact facility included the - ~ I .. , I I I I I heads of 43 wells which were slant-drilled to exploit several lease biock hoidings over an an:a of about a square mile (Figs. J, 4), together with necessary equipment for separation of the well-head crude oil into oil, gas, and water com- ponents. The gas was disposed of by injection back into the Gilmore block of the field between 1961 and 1971. Salt water was initially disposed of by discharge into a local storm drain, but for environmental reasons was required to be injected back into the field, also in the Gilmore block, since 1964 (Crowder and Johnson, 1963; California State Division of Oil and Gas [C.D.O.G.], 1974). AFTERMATH OF THE 1985 ROSS STORE EXPLOSION After the flames subsided and the post-explosion exploration and gas-control drilling was completed, a special Task Force was convened at the direction of the Los Angeles City Coun- cil. The Council wanted to know what had happened and how future accidents could be prevented. The Task Force was made up of representatives from both City and State agencies and from industry, and it had available a Geologic Technical Committee which included experts in engineering geology and other relevant disciplines. Concurrent with the deliberations of the Task Force, the Senate of the California State Legislature enacted SB1458, the Roberti Bill, which re- quired a study of the location of all abandoned oil and gas wells within the State of California. IIOUUYAAD EXPLANATION • . • • • • Concllled fiUII ---- Surt.c.Dtceof .... u L Jc... ....... , .. ecJUI..EVAIIIp Figure 4. Surface plan of wells, faults and gas ventings, vicinity of Ross Store S1te CAUSE OF THE 1985 ROSS STORE EXPLOSION AND OTHER GAS VENTINGS. FAIRFAX DISTRICT. LOS ANGELES 147 < own initial interest in abandoned as: a pocten· tial source of the gas and the mandated purpose of the Roberti Bill to study such wells, the Task Force's surprising conclusion was that neither the existence of dozens of such abandoned wells, nor even the presence of the underlying oil and gas field which had been venting to the surface for a hundred millennia, had anything to do with the gas venting accidents. In fact, the oil field operation was not even men- tioned as a possible agent in the Task Force report. Instead, a chemical analysis of a sample of the venting gas led the Task Force to conclude that the gas was of "biogenic" origin, presumably derived from near surface decaying of organic matter in the alluvial soil, rather than being of petrogenic or thermogenic origin, i.e., derived from rock-source hydrocar- bon (oil fieid type) accumulations. The Task Force then went on to present a scenario of shallow "biogenic" methane being displaced and pressurized by a rising water table in the perched fresh-water aquifer beneath the Ross Store. It was an imaginative explanation: what school child is not aware of that primordial scene of mastodons thrashing about in a gassy swamp (as is artfully represented at full scale in the Hancock Park exhibit, only two blocks from the Ross Store). Troublesome legal issues were eliminated by this conclusion, the impiication being that the methane hazard could exist vir- tually anywhere, so no human agency was at fault for its workings. The presence of the abandoned wells, the filled sumps, or anything else having to do with the past and cur- rent exploitation of the Salt Lake oil field evidently was con- sidered no more than coincidence. About a year after the issuance of the Task Force report, the results of two separate studies of the composition and indi- cated origin of near smface gas samples both at the Ross Store and elsewhere in the Los Angeles Basin, became avail- able. One report was prepared under contract to the C.D.O.G., in response to the Roberti Bill (Geoscience Ana- lytical, Inc., 1986). It presented the results of a study of eight selected urban areas sited over oil and gas fieids where there were wells abandoned prior to 1930, and where there was a history of oil and/or gas seepage. This report con- cluded that with few exceptions. the methane present in these areas was, as at the site of the Ross Store building, of bio- genic origin and thus unrelated to the underlying oil and gas accumulations. In their opinion it was essentially swamp gas. This remarkable conclusion was all the more interesting since it turned out that most of the areas sampled are local topographic highs. In any case, the resujts of this massive study assured the public the hazardous conditions identified by the Task Force as existing at the Ross Store, as well as "the vast majority of the high concentration gas samples" taken from the surface areas overlying oil and gas deposits throughout the Los Angeles basin, were also of purely natural swamp gas origin unrelated to human activities or oil field presence. The other study, based on isotopic analysis of samples of gas at the Ross Store building escaping on the day following the l!:u