HomeMy WebLinkAboutCT 76-17; La Costa Vale Unit 2; Soils Report; 1973-01-01.‘~ ‘I ~“,C -.
T. FUNNEKOTTER ENGINEERING GEOLOGY - tmSTERED GEOLOtlST CER,xlFlEC ENGINpNG GEOLOGIST P. o.J,ox 575 ESCONDIDO. CALIF. 92025 746.2793 -
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Benton Engineering Inc. 6741 El Cajon Blvd. San Diego,Calif. 92115 Attn: P. Benton
GEOPHYSlCN IN”ESTlGATIONS
For
S”bdi”iSi0” Design
Pipelinel Roadr
Seismic Rippability Studier
January 1,1973
Dear Sir, Enclosed is the Subsurface
Investigation Report of LaCosta Vale - Unit 2 -
lines Al6 thru E16. Original velocity profile of
these lines is also included.
Very truly yours,
T. Funnekotter
ENGINEERING DEFT. LfBRARY
City of Ca!fspad
2075 Las PalmasWve
Carl&ad, CA 92009-48~59
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T., FUNNEKOTTER ENGINEERING GEOLOGY REGlSTERED GEOLOtlST
CERTlFlED ENGINEERING GEOLOGIST
P. 0.90x 575 ESCONDIDO, CALIF. 92025
746.2793
SUBSURFACE INVESTIGATIOM
LA CCSTk VALE - UNIT 2
ShIkXE.IC LINES Al6 THRU El 6
January 1,1973
GEOPHYSICAL IN”ESTICAflONS
For
S”bdi”i,iO” D&g”
Pipelines Roods
Seismic llippability Studier
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T., FUNNEKOTTER ENGINEERING GEOLOGY GEOPHYSICAL IN”ESTIGATIONS REGISTERED GEOLOGIST For CERTlFlED ENGlNEERlNG GEOLOGlST Subdivision Design P. 0. 80X 575 ESCONDIDO. CALIF. 92025 Pipeliner bx!r 740.2793 Seirmic Rippobility 3udier
Purpose:
Method:
Discussion:
To evaluate subsurface conditions in three select
areas in order to determine what excavation problems
may be encountered.
Refraction Seismography. Geologic reconnaissance.
The Seismic traverses are in the Black Mountain
Vo1cani.c unit - the material ranges from andesite
to rhyolite. This report includes lines A16,B16,C16,
D16,and El6 - located approximately as shown on the
enclosed plat.
In general, three velocity zones were mapped as
follows:
Velocity Range (ft/sec) Material
1300 to 2000 Soil & fill
2800 to 4200 Decomposed & fractured volcanic
7500 to 10,000 Hard, rigid volcanic
Lines A
each other
from 12 fe
16,Bl6, and Cl6 are in one area and cross
. High velocity volcanics were located here
et to 26 feet deep. The intermediate layer
of decomposed and fractured volcanics has a velocity
range of 2800 to 4100 ft/sec. The upper soil layer
has a velocity range of 1300 to 2000 ft/sec and is up
to 12 feet deep. Kost of the high velocity material in
this area appears to fall between a depth of 12 feet
and 20 feet. The area immediately west of line Cl6 has
T; FUNNEKOTTER ENGINEERING GEOLOGY REGISTERED GEOLOGIST
CERTlFlED ENGINEERING GEOLOGIST
P. 0,.80X 575 ESCONDIDO. CALIF. 92025
746.2793
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GEOPHYSICAL IN”ESTIGATIONS
For
sutdvirion Design
Pipeline* Rood,
Seismic Rippobility Studier
Discussion: (can't)
a considerable amount of rubble and boulders on the
surface.
Line D16 is in the second area. high velocity
volcanics were located here at 28 to 32 feet. The
intermediate zone velocity here measured 3500 ft/sec.
Line Elf: is in the third area investigated and
indicates high velocity material at 17 feet. The
overburden velocity here is 42OC ft/sec.
All runs indicate the presence of boulders and
blocks in various degrees of profusion. Some of these
are q,uite large, especially so where indicated on the
profile. These blocks appear to be most concentrated
in the area of line Cl6 and the northwest end of line
1;16.
Conclusion: Hard, rigid volcanic material was located on all
Seismic runs. The depth of this material is from 12
feet to 32 feet - mostly falling between 12 and 20
feet. The overburden velocity falls within a range of
2800 to 4200 ft/sec.
In terms of rippability, based on a D-o Cat, the
following schedule should apply:
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T., FUNNEKOTTER REGISTERED CEOLOGlST
CERTIFIED ENGINEERING GEOtOtlST
P. 0. 80X 575 ESCONDIDO. CALIF. 92025
746.2793
ENGINEERING GEOLOGY
Conclusion: (can't)
Velocity (ft/sec)
0 to 2000
2000 to 5000
5000 to 5500
Over 5500
GEOPHYSICAL lN”ESTlGATlONS
For
S”bdi”iaion Design
Pipelines Roadr
Seismic Rippobility Studier
Excavation Nethod
Scraper
Ripper
Marginal
Drill & Shoot
For trenching, based on a Kohring 505, the following
should apply:
Velocity (ft/sec) Excavation Method
0 to 3GOO Ripper
3800 to 4300 Marginal
Over 4300 Drill & Shoot
Submitted by .- &+V- 7$& i;_cL,>J~:& < ,c 1-i -I-.-
'I'. Funnekotter
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SLISi%IC - RIPPABILITY Ii9FORMATION
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The following points should be considered when evaluating Seismic information:
1. All velocities, depths, and thicknesses are averages and qualified according to the following schedule:
G - good F- fair P - poor VP - very poor ? - questionable
Grades of G, F, and P can be considered reliable; VP and ? should be considered as indi.cations only.
2. Each profile provides information in the immediate area of that profile - extrapolation outward from this area must be considered speculative unless additional information is available.
3. As the velocity of the material increases, ripping becomes progre- ssively more difficult until at some point it is more economical to drill and shoot the material prior to excavation. This point occurs within the marginal zone. Rippability figures vary with the type of material, however, in general, B-9 ripper performance is as follows:
Velocity Range (ft/sec) Excavation Method
0 to 2000 Scraper 2000 to 5000 Ripper 5000 to 5500 Marginal Over 5500 Blasting
These figures are based on several hundred job studies.
4. For trencher and backhoe operations the rippability figures must be adjusted downward, i.e., velocities as low as 3500 ft/sec may indicate material that is not rippable, depending on the homogeneity of that material, whereas material measuring over 4300 ft/sec almost certainly would require explosive work. As an average, materials measuring over 3800 ft/sec would mean difficult trenching and the economics of the situation would probably dictate explosive work first, The above figures are based on a machine similar to the Kohring 505.