HomeMy WebLinkAboutSoil Report-Mod-2016March25, 2016
Mr. Rami Batikh
Ramco Gas & Mart, Inc.
2222 F Street
Bakersfield, California 93301
PIPING AND DISPENSER PAN REPLACEMENTSOIL SAMPLINGREPORT FOR THE
RAMCO EXPRESS,2222 F STREETBAKERSFIELD, CALIFORNIA
(BFDPSD PERMIT TO OPERATE 015021000993)
Dear Mr. Batikh:
Complete Fueling Solutions (CFS)wascontracted by Ramco Gas & Mart, Inc.to perform replacement of
theplastic product pipingand dispenser pansat the Ramco Express (site)with fiberglass product piping
and dispenser pans.VVEIR Corp was subcontracted by CFSto conduct soil sampling, laboratory
analysis, and preparation of this Piping and Dispenser Pan ReplacementSoil SamplingReport. Thesoil
samplingactivities were performed onMarch 8, 2016,under permit with the Bakersfield Fire Department
Prevention Services Division (BFDPSD).
SITE DESCRIPTION
The site is located at 2222 F Street, Bakersfield, Kern County, California (seeFigure1-Site Location
Map). The site is located at the southeastcorner of the intersection of F Streetand23rd Street.The site
is located in a commercial area flanking 23rd Streetwith the nearest residential properties500feettothe
west of the site(see Figure 2 -Site Vicinity Aerial. The site is identified as Assessor’s Parcel Number
(APN) 003-131-11(see Figure 3 -Assessor’s Parcel Map). Thesite is at an elevation of405feet above
mean sea level, and the topography is relatively flat with a slight slope to the southwest. The site is
located within the southeast quarter of the northeast quarterof Section 25, Township29 South, Range 27
East, Mount DiabloBaseline and Meridian.
Has beendevelopedas a service stationfor several decades.InMarch1987 the previous fueling facilities
wereremoved andreplaced with three 10,000-gallon,double-walled, fiberglass-cladUSTs with overfill and
overspill protection; single-walled plastic product pipelineswithin a fiber trench liner, and two multiple
product dispensers (MPDs)with single-walled plastic dispenser panson a single island
(seeFigure4-Plot Plan).
Mr. Rami Batikh
Ramco Gas & Mart, Inc.
March 25, 2016 -Page 2
The property owner contact is Mr.Rami Batikh, Ramco Gas & Mart, Inc. 2222 F Street,Bakersfield,
California, 93301, (661) 324-1758. The general contractor contact is Mr.Aaron Koop, CompleteFueling
Solutions,12601Jasmine Avenue, Bakersfield, California, 93312, (661) 706-8688.The environmental
consultant is Mr.Mark R. Magargee, PG, CHg,VVEIR Corp,3410 Fruitvale Avenue, Suite A, Bakersfield,
California, 93308, (661) 631-8347. Theregulatory agency contact is Mr. Shane Gardner, Bakersfield Fire
Department Office of Environmental Services, 1600 Truxtun Avenue, Suite 401, Bakersfield, California
93301, (661) 326-3979.
BACKGROUND
GEOLOGY
The site is located at an elevation of 405feet above MSL, and the topography slopes slightly to the
southwest, toward the center of the San Joaquin Valley. The project areais located inthe southern
portion of the Great Valleygeomorphic province. The Great Valley geomorphic province is a northwest-
southeast trending valley that is also approximately 400 miles long by 50 miles wide, the southern portion
of which is referred to as the San Joaquin Valley. The site is located in the south central area of the San
Joaquin Valley where the Sierra Nevada, Great Valley, and Coastal Range physiographic provinces meet
The southern end of the Sierra Nevada Province is composed of a massive block of igneous and
metamorphic rock of Mesozoic age and older. This Sierran block, 40 to 100 miles wide and 400 miles
long, slopes five to seven degrees beneath the San Joaquin Valley. The Coastal Range province on
the west consists of tectonically deformed and fractured marine and non-marine sedimentary rocks of
Jurassic, Cretaceous, and Tertiary age, which dip eastward beneath the Sand Joaquin Valley. The Great
Valley province is a broad asymmetrical synclinal trough, which is known as the Sacramento Valley in the
north and the San Joaquin Valley in the south.
Beneath the southern San Joaquin Valley floor, the Sierran plutonic and metamorphic rockblock is
overlain by consolidated marine rocks of Jurassic and Cretaceous age. These rocks are overlain by
continental marine and non-marine sedimentary rocks of Tertiary age, which are comprised of continental
deposits of consolidated to semi-consolidated, fossiliferous sandstone, siltstone, and shale which thicken
toward the south and west. Unconsolidated continental deposits consisting of Pliocene to Holocene
river and lake gravel, sand, silt, and clay sediments, in turn, overlie the Tertiary rocks.
Surface features of the floor of the San Joaquin Valley consist of dissected uplands, alluvial fans, overflow
areas, and lake bottoms. Dissected uplands lie between the mountains and the nearly flat Valley floor and
are manifest in low-lying hills through which perennial and intermittent streams flow. These features
consist of reworked older alluvium. The alluvial fans are the sites of active stream deposition of sands
and silts derived from the Sierra Nevada and the dissected uplands. The overflow lands and lake bottoms
Mr. Rami Batikh
Ramco Gas & Mart, Inc.
March 25, 2016 -Page 3
lie in the central part of the Valley where silt and clay accumulate in quiet lake and marsh environments.
Surface soils are classified by the Soils Conservation Services as Kimberlina -Urban Land -Cajon
Complex and are characterized as 35 percent Kimberlina fine, sandy loam; 30 percent Urban land with
impervious surfaces and altered fills; and 20 percent Cajon loamy sand.
HYDROGEOLOGY
The site lies within the Kern County Basin of the San Joaquin Basin Hydrologic Study Areawithin the
Tulare Lake Hydrologic Region (Basin), which is not an adjudicated basin but is managed under a Basin
Plan. Bounding the subbasin are the Kern County line and the Tule Groundwater subbasin to the north,
Sierra Nevada foothills and Tehachapi Mountains to the east, San Emigdio Mountains to the south, and
Coast ranges to the west. The groundwater basin is comprised of deposits of clay, silt, sand, and gravel
and consists of four water bearing formations: Olcese and Santa Margarita Formations, Tulare and Kern
River Formations, Older Alluvium/Stream and terrace Deposits, and Younger Alluvium/Flood Basin
Deposits. The subbasin has a surface area of 3,040 square miles, and receives average precipitation of
5to 13 inches annually.
The site lies within the Kern County Basin of the San Joaquin Basin Hydrologic Study Area (Basin).
Thesite is located within Kern County Improvement District No. 4. Surface water and groundwater in the
San Joaquin Valley are derived predominantly from the Sierra Nevada to the east, and are transported by
five major rivers, the southernmost being the Kern River. The subject site is located approximatelythree
miles south of the Kern River. The site is not located within a Federal Emergency Management Agency
(FEMA) 100 or500 year flood zone.
The Kern County Water Agency (KCWA)publishes annual maps showing the depth to water, and
groundwater qualityfor groundwater basins within Kern County. The depth to the regional unconfined
aquifer is estimated to be in excess of 100 fbg at the site, and the groundwater gradient is to the
southwesttoward the center of the San Joaquin Valley. Perched groundwater at depths as shallow as
20feet is known to be present flanking the current course of the Kern River, but is not known to extend to
the site. There are several municipal water supply wells located within a mile of the site. The groundwater
is considered to be potable and suitable for beneficial use.
The Central Valley of California is underlain by a broad, thick hydrogeologic unit, which consists of soil and
rock with varying porosity and permeability. Physical dimensions are approximately 50 miles wide at the
widest point in the Valley, 400 miles long, and as much as 2,000 feet deep. Recharge to regional aquifers
consists of infiltration of seasonal precipitation and percolation of surface waters. The Valley aquifer of
greatest storage, highest quality, and greatest accessibility for domestic and agricultural use consists of
the alluvial and lacustrine continental deposits extending to the depths of 1,500 to 2,000 feet beneath the
San Joaquin Valley floor. Lithologic and hydraulic properties of these sediments are largely the product of
Mr. Rami Batikh
Ramco Gas & Mart, Inc.
March 25, 2016 -Page 4
the sediment source and the depositional environment. These sediments range in size from clays to
boulders and include all mixtures between the extremes. Those of the west side of the Valley are derived
largely from the Coastal Ranges, which tend to consist of shales and fine sandstones with limited
permeability. The east sediments are derived mainly from granitic materials of the Sierra Nevada which
are generally coarser and much more permeable. Sediments encountered during the previous
investigations at the site consisted of alluvial deposits comprised of fine-to-coarse grained sands
containing quartzite and micas. Permeability in these sediments is high.
PIPINGUPGRADESOIL SAMPLING
CFS was contracted to upgrade the single-walled plastic product piping within a fiber trench liner and
single-walled plastic dispenser pans at the site. On March 8, 2016, the MPDsand dispenser panson the
westernandeasternislandsandthe plastic product piping fromthese MPDsto the USTswereremoved
(seeAttachment 1of a Photographic Log).Subsequently double-walled fiberglass product piping and
dispenser pans have been installed at the site. VVEIR Corp was contracted to provide aCalifornia
Professional Geologist to collect soil samples at the direction of Mr.Shane Gardnerwith the BFDPSD
from beneath the western and easternMPDs, and the western 45 and eastern elbowof the piping run
fromthe MPDsto the USTs.Soil samples WD-2andWD-6were collected from 2and 6 feet beneath the
westernMPD;soil samples ED-2andED-6were collected from 2 and 6 feet beneath the eastern MPD;
soil samples WP45-2 and WP45-6were collected from 2 and 6feet beneath the western 45of the piping
run from the MPDs to the USTs; and soil samples EPE-2and EPE-6were collected from 2 and 6 feet
beneath the eastern elbowof the piping run fromthe MPDsto the USTs(seeFigure 4for the sample
locations).
All sampling equipment was washed with a non-phosphate cleanser, pre-rinsed with tap water, and finally
rinsed with deionized water prior to sampling. The soil samples were collected using a backhoe. The soil
sampleswere stored in 2-inch-diameter stainless steeltubes, sealed with Teflon™ liners and end caps,
labeled, placed in an ice chest at a temperature of less than 4°C, and transported to a California
State-certified laboratory for analysis. Sample identification and chain-of-custody procedures were
followed for the samples to ensure sample integrity and to document sample possession from the time of
collection to the ultimate destination. Thesample labels identified the job number, sampler, date and time
of collection, and a sample number unique to each sample.
Thesoil samples were analyzed at Moore Twining Associates, Inc.(MTA)for total petroleum
hydrocarbons (TPH)as gasolineusing Environmental Protection Agency (EPA) Method 8015M; and
benzene, toluene, ethylbenzene, and total xylenes (BTEX),methyl tertiary butyl ether (MTBE),tertiary
butyl alcohol (TBA),diisopropyl ether(DIPE),ethyl tertiary butyl ether (ETBE),tertiary amyl methyl ether
(TAME),ethylene dibromide (EDB),1,2-dichloroethane (1,2-DCA), and naphthaleneusing EPA Method
8260C.TPH as gasoline,BTEX,MTBE, TBA, DIPE, ETBE, TAME, EDB,1,2-DCA,and naphthalenewere
FIGURE 1 - SITE LOCATION MAP
SITE
LEGEND
REVISED: MARCH 10, 2016: mrm
VEIR Corp
RAMCO GAS & MART, INC.
RAMCO EXPRESS2222 F STREETBAKERSFIELD, CALIFORNIA
FIGURE 2 - SITE VICINITY AERIAL
SITE
LOCATION
LEGEND
VEIR Corp
RAMCO GAS & MART, INC.
RAMCO EXPRESS2222 F STREETBAKERSFIELD, CALIFORNIA
FIGURE 3 - ASSESSOR'S PARCEL MAP
SITE
LOCATION
LEGEND
VEIR Corp
RAMCO GAS & MART, INC.
RAMCO EXPRESS2222 F STREETBAKERSFIELD, CALIFORNIA
SOIL SAMPLE LOCATION
FIGURE 4 - PLOT PLAN
23RD STREET
F
S
T
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E
E
T
RAMCO EXPRESS
USTSDISPENSERS
LEGEND
VEIR Corp
RAMCO GAS & MART, INC.
RAMCO EXPRESS2222 F STREETBAKERSFIELD, CALIFORNIA01020
1 inch = 20 ft.
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ATTACHMENT 1.
PHOTOGRAPHIC LOG
VVEIR Corp
PHOTOGRAPHS OF SITE WORK
PROJECT:
Ramco Express
2222 F Street
Bakersfield, California
Oblique photograph
showing the Ramco
Expressat lower
center withinthe
surrounding
commercial district
which flanks F Street
and23rd Street,and
the residential area of
centralBakersfield in
the upperleft(view
looking north).
Oblique photograph
showing the Ramco
Expressat lower
center within the
surrounding
commercial district
which flanks F Street
and23rd Street,and
the residential area of
central Bakersfield at
right(view looking
south).
Page 1 of 4
VVEIR Corp
PHOTOGRAPHS OF SITE WORK
PROJECT:
Ramco Express
2222 F Street
Bakersfield, California
Photograph showing
the Ramco Express,
with the three 10,000-
gallon gasoline USTs
at left, two multiple
product dispensers at
right, and the
mini-mart building in
thebackground (view
looking south).
Photograph showing
the two multiple
productdispensersat
left, mini mart building
at right, and thethree
10,000-gallon
gasolineUSTs in the
background(view
looking east).
Page 2 of 4
VVEIR Corp
PHOTOGRAPHS OF SITE WORK
PROJECT:
Ramco Express
2222 F Street
Bakersfield, California
Photograph showing
the location of the two
multiple product
dispensers and
product piping(view
looking south).
Photograph showing
the turbine sumps
above the three
10,000-gallon
double-walled
gasoline USTs(view
looking south).
Page 3 of 4
VVEIR Corp
PHOTOGRAPHS OF SITE WORK
PROJECT:
Ramco Express
2222 F Street
Bakersfield, California
Photograph showing
thelocation ofthe two
multiple product
dispensers and
product piping(view
looking east).
Photograph showing
the locationof the
piping run between
the USTs and the
dispensers(view
looking west).
Page 4 of 4
ATTACHMENT 2.
LABORATORYREPORT
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