HomeMy WebLinkAboutStockdale Ranch Sump #5 Slope Stability Analyses 08-02-214400 YEAGER WAY Phone: 661 831 5100 info@soilsengineering.com
BAKERSFIELD, CA 93313-2019 Fax: 661 831 2111 www.soilsengineering.com
August 2, 2021 SEI File No. 21-17961
Bolthouse Properties, LLC
11601 Bolthouse Drive, Suite 200
Bakersfield, CA 93311
Attention: Mr. Jeff Eittreim
Subject: Addendum 1 - Sump Slope Stability Reference:
GEOTECHNICAL INVESTIGATION REPORT
Stockdale Ranch Sumps and Street Improvements
Corner of Stockdale Hwy & S. Heath Rd, Bakersfield, CA.
In accordance with your request and authorization, we have performed slope-stability analyses for
proposed sumps on the above referenced project.
Our analyses shows that the minimum factor-of-safety for a sump with 13 feet high slopes ranges from
2.87 to 2.89 for the case of saturated slopes and a phreatic surface that parallels the ground surface
at a depth of one foot below between the sump toe and at least 50 feet beyond the top of the slope.
Figures 1 through 3 show the ten failure-surfaces, each yielding the lowest safety factors. Three
methods: Bishops Modified; Spencer; and Janbu; were used to determine three independent safety-
factors.
We hope this provides the information you require. Please contact us if you have any questions or if
you need any further geotechnical services.
Respectfully submitted,
Soils Engineering, Inc.
L Thomas Bayne CE
26106 GE 125
SOILS ENGINEERING, INC.
Geotechnical Engineering Services SEI File No. 21-17961
Project: Stockdale Ranch Sumps and Street Improvements August 2, 2021
Location: Southwest Corner of Stockdale Hwy & S. Heath Rd, Bakersfield, CA Page 2
4400 YEAGER WAY Phone: 661 831 5100 info@soilsengineering.com
BAKERSFIELD, CA 93313-2019 Fax: 661 831 2111 www.soilsengineering.com
Slope Stability
The proposed sump-embankment cross-section was analyzed using the computer program, WinStable
stability for the subject site was assessed using the Spencer, Janbu, and Bishops method.
Strength values were obtained from the results of Direct Shear tests on saturated samples of earth
materials obtained from the upper twelve feet below the existing ground surface.
Slip-surfaces for the Spencer, Janbu, and Bishops methods are shown on Figures 1 through 3.
These methods yielded safety-factors that were comfortably-above the minimum allowed, ranging from
2.87 to 2.89.
Slopes analyzed were selected as representing the most-critical slope locations and configurations
based on our engineering judgment tempered by our experience performing slope-stability-analyses in
the Southwest area of the city of Bakersfield, in Kern County, California.
Since soils were relatively uniform and generally increased in density and strength with depth, critical
circles passing through of the toe of the slope were selected as most representative of the critical
failure mode.
The Entry and Exit method was used to analyze failure surfaces assumed to pass through the toe of
the slope while entering at the top of the slope usually within one slope- height from the top-edge of the
embankment.
Soil shear strengths were assumed to be anisotropic although direct shear tests on existing,
undisturbed native soils promote failure to occur along an essentially horizontal failure plane owing to
the design of the test equipment and the orientation of the test sample.
Slope Stability in Stratified Soils
Natural soils on the site are stratified with stratum thicknesses and sequencing varying extensively
between test boring locations. Little or no lateral continuity exists between test boring locations owing
to the mode of alluvial deposition.
Slope stability analyses were performed using layer sequencing that would produce the lowest safety
factor, i.e. by placing the soils layer with the lowest friction and cohesion at the lowest elevations on the
slope profiles analyzed.
Slope Stability Safety Factors
Computed Safety factors obtained using the Entry and Exit method, the Grid-Radius method, and the
Block method are given in table below.
SLOPE STABILITY FACTORS OF
SAFETY
Janbu’s Method 2.86
Spencer’s Method 2.86
Bishop’s Method 2.87
SOILS ENGINEERING, INC.
Geotechnical Engineering Services SEI File No. 21-17961
Project: Stockdale Ranch Sumps and Street Improvements August 2, 2021
Location: Southwest Corner of Stockdale Hwy & S. Heath Rd, Bakersfield, CA Page 3
4400 YEAGER WAY Phone: 661 831 5100 info@soilsengineering.com
BAKERSFIELD, CA 93313-2019 Fax: 661 831 2111 www.soilsengineering.com
Figures 1 through 3 show the shape and location of the most critical failure surfaces for each of
the cases described above.
Existing and proposed slope configurations were analyzed for static stability. Pseudo-seismic
(pseudo-static) was not assessed. Chart solutions were used to estimate approximate locations for
circle-centers for failure modes simulating two-dimensional circular failure surfaces.
Slopes were analyzed in accordance with the following criteria:
A.Circular failure surfaces were used in our analyses. Because existing stratigraphy is
random and no predominant orientation for bedding exists, circular failure surfaces having
the lowest safety factors were those that were both the thinnest and mostly oriented
parallel to the slope surface.
B.Using Slope/W possible centers for circular failure surfaces were positioned in a
random pattern. The approximate centers for circular failure surfaces most likely to yield
the lowest Factors-of-Safety were usually found at a locations in which failure surfaces
enter near the toe of the slope and exist near the top of the slope and in the height
range of two to two and one-half times (2 x - 2 ½ x ) the height of the slope as measured
from the toe elevation.
C.Plots showing the shape of the failure surface, centers for moment equilibrium, centers
of rotation for failure surfaces, and ranges for entry and exit of slip-circles are shown on
Figures 1, 2, and 3, below.
D.Mohr-Coulomb equation was used to define soil strength for use in stability analyses.
Because most of the materials located within the existing embankments and specified in
recommendations for embankment construction are free-draining, effective-strength
parameters as determined from direct-shear strength tests were used in the analyses.
E.Soil strength values were obtained from our laboratory test data consisting of grain- size
analyses, drained-direct-shear tests. Angles of effective internal friction (∅’) and effective
cohesion (strength-intercept) (c’) were obtained by plotting effective shear stress (τ) in
kips per square foot (ksf) on the ordinate and effective normal stress (s’) in kips per square
foot (ksf) on the abscissa. The lower-bound value line was used to obtain ∅’ and c’. The
plot of shear stress (τ) in kips per square foot (ksf) vs. effective normal stress (s’) in
kips per square foot (ksf).
F.Slopes analyzed were selected to be representative of the most-critical slope locations
and configurations based on the slope height. Slopes are assumed to be saturated with
phreatic surfaces paralleling the ground surfaces near the top, from the top to the
bottom of the slope, and at the toe of the slope and beyond.
H.Analyses that were performed using ranges of entry and exit points for slip-circles were
set-up whereby circles were assumed to pass within a few feet up-slope and down-
slope from the toe of the slope; while exiting near at the top of the slope within the range
SOILS ENGINEERING, INC.
Geotechnical Engineering Services SEI File No. 21-17961
Project: Stockdale Ranch Sumps and Street Improvements August 2, 2021
Location: Southwest Corner of Stockdale Hwy & S. Heath Rd, Bakersfield, CA Page 4
4400 YEAGER WAY Phone: 661 831 5100 info@soilsengineering.com
BAKERSFIELD, CA 93313-2019 Fax: 661 831 2111 www.soilsengineering.com
bounded by points within one slope-height offset away from the edge of the
embankment and a few feet down-slope on the embankment face. Limits for entry and
exit of failure circles are shown on stability analyses plots.
I.Soil shear strengths were assumed to be isotropic although direct shear tests on
existing, undisturbed native soils promote failure to occur along an essentially horizontal
failure plane. This is due to the design of the test equipment and the orientation of the
test sample as taken in the field. Orientation of samples as taken and tested in the
laboratory result in the shear-strength analyses skewed slightly toward the conservative
side. This conservatism occurs because soil bedding of alluvium tends to be horizontal
and parallel to the direction that samples are sheared in the laboratory. Were samples to
be sheared in a direction transverse to the natural soil bedding, shear strength results
would be slightly higher than their horizontally sheared counterparts.
J.Slope Stability in Stratified Soils
Natural soils on the site are layered. Layer thicknesses and sequencing vary randomly
between test boring locations. Little or no lateral continuity exists between test boring
locations owing to the mode of alluvial deposition.
Figure 1 Minimum Safety Factor – Spencer’s Method
Phreatic
Surface
SOILS ENGINEERING, INC.
Figure 2 - Minimum Safety Factor Janbu's Method
Phreatic
Surface
SOILS ENGINEERING, INC.
Figure 3 - Minimum Safety Factor Bishop’s Method
Phreatic
Surface
SOILS ENGINEERING, INC.