Upload
others
View
2
Download
0
Embed Size (px)
Citation preview
MEMORANDUM October 26, 2011 Project No.: 060036-003-05
Page 2
field by measuring from existing Site features. Both borings were located on the east side of the roadway within the gravel shoulder.
Borings EB-12 and EB-13 were advanced to a maximum depth of 51.5 feet and 45.83 feet below the ground surface, respectively. The borings were drilled using a modified B-53 track-mounted hollow-stem auger drill rig equipped with an 8-inch-diameter auger. The drill was operated by Davies Drilling under the direction of Aspect. Split spoon (1 3/8-inch inner diameter) samples were obtained from the borings in general accordance with Standard Penetration Test Procedures (American Society for Testing and Materials [ASTM D-1586]), at 2.5- and 5-foot intervals. The split spoon sampler is driven 18 inches into the soil by a 140-pound hammer falling 30-inches. The number of blows required to drive the sampler are counted for each 6 inches of penetration. The blow count for the first 6 inches of penetration is discarded, and the remaining blow counts are summed to produce the Standard Penetration Resistance (N).
Logs of the borings indicating the type of soils encountered are attached as Appendix A. The depths indicated on the logs where conditions changed may represent gradational variations between soil types. Changes logged between sample intervals in our borings were interpreted. Soils were classified in general accordance with the ASTM D-2488, “Standard Practice for Description and Identification of Soils” (Visual and Manual Procedure).
Stratigraphy As shown on the attached exploration logs, our explorations encountered active landslide debris overlying relatively undisturbed glaciolacustrine. More detailed descriptions of the soils encountered at the Site are provided below:
Fill Road embankment fill was encountered in both borings at the ground surface to a depth of 5 feet below the existing ground surface. The presence of fill was inferred to be the remnants of past grading operations in the area. Typically the roadway fill consisted of loose to medium dense, moist, dark brown, silty, sandy GRAVEL (GM) with scattered asphalt debris.
Landslide Debris The loose to medium dense sand was encountered in both borings underlying the roadway fill and extended to depths of 45.5 and 30.5 feet below the existing ground surface in EB-12 and EB-13, respectively. This unit was interpreted as active landslide debris derived from previously intact, Vashon advance outwash sediments, located upslope of the Site. The landslide debris encountered in the borings is the result of ongoing vertical and horizontal displacement of the soil. The landslide debris typically consisted of loose to medium dense, moist to wet, brown to gray, poorly graded SAND (SP) with varying amounts of silt and gravel and scattered organics debris. Groundwater levels at the time of drilling were encountered in the landslide debris unit at depths of 34.0 feet and 22.5 feet below the existing ground surface in EB-12 and EB-13, respectively.
Vashon Glaciolacustrine Underlying the landslide debris were glaciolacustrine soils. Both borings were terminated in relatively undisturbed and intact glaciolacustrine clay. A disturbed zone of the lacustrine unit ranging from 4.5 to 14.5 feet in thickness was present immediately underlying the landslide debris in both
MEMORANDUM October 26, 2011 Project No.: 060036-003-05
Page 3
borings. This disturbed zone was interpreted as prehistoric landslide debris consisting of highly fractured silty CLAY (CL) with interbedded zones of fine sand. Underlying the disturbed zone, were relatively intact glaciolacustrine soils consisting of hard, moist, blue-gray, silty CLAY (CL) with thin laminae visible and an undisturbed texture.
Based on the presence of groundwater in the overlying landslide debris, the undisturbed glaciolacustrine soils encountered at depth in the borings are interpreted as the base of the active landslide area.
Hydrology Groundwater was encountered in EB-12 at a depth of 34.0 feet and in EB-13 at a depth of 22.5 feet below the existing ground surface at the time of drilling. These depths correspond to elevations of approximately 57 feet and 63.5 feet, respectively. We observed groundwater seepage exposed on the slope, upslope from the right-of-way. The seepage was located above a prominent clay outcrop that represents the contact between the in-place advance outwash sand (above) and the in-place glaciolacustrine (below). The contact represents the undisturbed stratigraphic column outside the active landslide area. The seepage flow rate observed was estimated between 1 and 5 gallons per minute.
Monitoring Station Installations and Details Following completion of the borings, slope inclinometer casings were installed to approximately the bottom of each borehole. The inclinometer casing consisted of a 2.75-inch-outside diameter ABS pipe with a pair of orthogonal slots, or grooves, that permit a calibrated instrument probe to be lowered to the bottom of the pipe. When the ground surrounding the inclinometer casing moves, the casing will distort within the zone of movement allowing the instrument probe to record the deflections and distortion.
A vibrating-wire piezometer (VWP) was also secured to each inclinometer casing to measure groundwater levels. The piezometer (including the porous stone) was saturated and checked for proper function prior to being installed. During installation of the inclinometer casing, the piezometer was attached in an inverted position to the casing at a pre-determined location to be installed below the observed and historic groundwater level. The piezometer and cable were secured to the inclinometer casing using fiberglass tape.
Following installation of the inclinometer casing and the piezometer, the casing was tightly capped, and the annular space between the casing and borehole wall was filled by pumping a cement-bentonite grout into the borehole. Following the grouting process, a single-channel datalogger was connected to the piezometer to record water levels every 12 hours. A metal monument with a flush-mount lid was installed to protect the top of the inclinometer and datalogger.
Monitoring Plan Aspect proposes monitoring these new installations monthly until January 2012. At that time, a summary of data will be prepared and submitted to the County. Changes in the monitoring schedule will be discussed relative to the current weather issues and any changes in the reporting systems for water elevation readings will be discussed.
MEMORANDUM October 26, 2011 Project No.: 060036-003-05
Page 4
References Aspect Consulting, LLC (Aspect), 2006, Subsurface Exploration, Geologic Hazard, And
Geotechnical Engineering Report, Washington Boulevard Landslide Kingston, Washington, prepared for Kitsap County Department of Public Works. March 30, 2006.
Limitations Work for this project was performed and this memorandum prepared in accordance with generally accepted professional practices for the nature and conditions of work completed in the same or similar localities, at the time the work was performed. It is intended for the exclusive use of Kitsap County Department of Public Works for specific application to the referenced Site. This memorandum does not represent a legal opinion. No other warranty, expressed or implied, is made.
Attachments Figure 1 – Site and Exploration Plan – New Explorations and Monitoring Stations Appendix A – Exploration Logs
W:\_GEOTECH\060036 Washington Boulevard Landslide\Deliverables\New Monitoring Stations Memo\Installation Memo.docx
Classifications of soils in this report are based on visual field and/or laboratory observations, which include density/consistency, moisture condition, grain size, and plasticity estimates and should not be construed to imply field or laboratory testing unless presented herein. Visual-manual and/or laboratory classification methods of ASTM D-2487 and D-2488 were used as an identification guide for the Unified Soil Classification System.
Terms Describing Relative Density and Consistency
Estimated Percentage
Symbols
Moisture ContentPercentageby Weight
SamplerType
Sampler TypeDescription
Blows/6" orportion of 6"
Component DefinitionsSize Range and Sieve Number
Larger than 12"Descriptive Term
Smaller than No. 200 (0.075 mm)
3" to 12"
Coarse-Grained Soils
Fine-Grained Soils
DensityVery LooseLooseMedium DenseDenseVery Dense
SPT blows/foot0 to 44 to 1010 to 3030 to 50>50
(2)
0 to 22 to 44 to 88 to 1515 to 30>30
ConsistencyVery SoftSoftMedium StiffStiffVery StiffHard
SPT blows/foot(2)
2.0" OD Split-Spoon Sampler(SPT) Continuous Push
Non-Standard SamplerBulk sample
3.0" OD Thin-Wall Tube Sampler (including Shelby tube)
Grab Sample
Portion not recovered
(1)
ATD = At time of drillingStatic water level (date)
Percentage by dry weight(SPT) Standard Penetration Test (ASTM D-1586)In General Accordance withStandard Practice for Description and Identification of Soils (ASTM D-2488)
Test Symbols
Depth of groundwater(4)
(1)
(2)
(3)
Cement grout surface seal
Groutseal
End cap
Filter pack with blank casing section
Boulders
Silt and Clay
Gravel Coarse Gravel Fine Gravel
Cobbles
Sand Coarse Sand Medium Sand Fine Sand
Dry - Absence of moisture, dusty, dry to the touch
Slightly Moist - Perceptible moisture
Moist - Damp but no visible water
Very Moist - Water visible but not free draining
Wet - Visible free water, usually from below water table
Hig
hly
Org
anic
S
oils
Fin
e-G
rain
ed S
oils
- 5
0%
or
Mor
e P
asse
s N
o. 2
00 S
ieve
(1)
Coa
rse-
Gra
ined
Soi
ls -
Mor
e th
an 5
0%
Ret
aine
d on
No.
200
Sie
ve
Gra
vels
- M
ore
than
50%
o
f Coa
rse
Fra
ctio
n R
etai
ned
on N
o. 4
Sie
ve15
% F
ines
5% F
ines
San
ds -
50%
o
r M
ore
of C
oars
e Fr
actio
n P
asse
s N
o. 4
Sie
veS
ilts
and
Cla
ysLi
quid
Lim
it Le
ss th
an 5
0S
ilts
and
Cla
ysLi
quid
Lim
it 50
or
Mor
e
(5) Combined USCS symbols used for fines between 5% and 15% as estimated in General Accordance with Standard Practice for Description and Identification of Soils (ASTM D-2488)
(1)
(1)
15%
Fin
es5%
Fin
es(5
)(5
)(5
)(5
)
FC = Fines ContentG = Grain SizeM = Moisture Content A = Atterberg Limits C = ConsolidationDD = Dry DensityK = PermeabilityStr = Shear StrengthEnv = EnvironmentalPiD = Photoionization
No. 4 (4.75 mm) to No. 10 (2.00 mm)No. 10 (2.00 mm) to No. 40 (0.425 mm)No. 40 (0.425 mm) to No. 200 (0.075 mm)
3" to No. 4 (4.75 mm)3" to 3/4"3/4" to No. 4 (4.75 mm)
No. 4 (4.75 mm) to No. 200 (0.075 mm)
Well-graded gravel and gravel with sand, little to no fines
Poorly-graded gravel and gravel with sand, little to no fines
Silty gravel and silty gravel with sand
Clayey gravel and clayey gravel with sand
Well-graded sand and sand with gravel, little to no fines
Poorly-graded sand and sand with gravel, little to no fines
Silty sand and silty sand with gravel
Clayey sand and clayey sand with gravel
Silt, sandy silt, gravelly silt, silt with sand or gravel
Clay of low to medium plasticity; silty, sandy, or gravelly clay, lean clay
Organic clay or silt of low plasticity
Elastic silt, clayey silt, silt with micaceous or diato-maceous fine sand or silt
Clay of high plasticity, sandy or gravelly clay, fat clay with sand or gravel
Organic clay or silt of medium to high plasticity
Peat, muck and other highly organic soils
GW
GP
GM
GC
SW
SP
SM
SC
ML
CL
OL
MH
CH
OH
PT
Trace
Slightly (sandy, silty,clayey, gravelly)Sandy, silty, clayey,gravelly)Very (sandy, silty,clayey, gravelly)
Modifier<5
5 to 15
15 to 30
30 to 49
Screened casing or Hydrotip with filter pack
Bentonitechips
FIGURE NO.
PROJECT NO.DATE:
REVISED BY:
DRAWN BY:
DESIGNED BY:
www.aspectconsulting.com
earth + water Exploration Log Key
A-1
Q:\_
AC
AD
Sta
ndar
ds\S
tand
ard
Det
ails
\Exp
lora
tion
Log
Key
A1.
dwg
Detector
Grouted Transducer
BGS = below ground surface
ROAD FILL
Medium dense, slightly moist, brown to black,sandy GRAVEL (GM); poorly graded fine sand,slightly silty.
ACTIVE SLIDE DEBRIS
Loose, slightly moist, brown SAND (SP); poorlygraded fine to medium sand, slightly gravelly, fineto coarse, subrounded gravel, trace silt.
Becomes moist, oxidation and rust staining,scattered organic debris at 10 feet.
Loose, moist, light brown, SAND (SP); poorlygraded fine to medium sand, scattered finegravel.
5710
3510
322
222
S-1
S-2
S-3
S-4
Data logger (S/N
37414) and steel flush
monument at ground
surface
Installed 2-3/4" dia.
slope indicator casing
to 48.33' bgs.
Casing grouted in
place with mix
containing 94 lb
Portland cement, 25 lb
bentonite gel, 30
gallons water.
Grout take estimated at
150% of the theoretical
volume.
Ground Surface Elev
30 40
EB-12Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
5
10
15
0
9/27/2011-9/28/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 2
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
1 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
5
10
15
91
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
90
85
80
75
N-valueWater Content %
34.0
6"
Loose, moist, light brown, SAND (SP); poorlygraded fine to medium sand, scattered finegravel.
Prominent zone of gravel at 22.5 feet based ondrill action.
Loose to medium dense, moist, brown, SAND(SP-SM); poorly graded fine sand, slightly silty,trace fine gravel.
VASHON GLACIOLACUSTRINE
Stiff, slightly moist, gray, CLAY (CL); highlyfractured, intermixed laminae of loose, lightbrown SAND (SP).Medium dense, wet, gray, SAND (SP); poorlygraded fine to medium sand, trace gravel and silt.
Interbedded with stiff, very moist, blue-gray, siltyCLAY (CL); low plasticity, highly fractured,disturbed texture.
424
346
8109
61219
S-5
S-6
S-7
S-8
S-9
Ground Surface Elev
30 40
EB-12Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
25
30
35
0
9/27/2011-9/28/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 2
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
2 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
25
30
35
91
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
70
65
60
55
N-valueWater Content %
34.0
6"
Medium dense, wet, gray, SAND (SP); poorlygraded fine to medium sand, trace gravel and silt.
Interbedded with stiff, very moist, blue-gray, siltyCLAY (CL); low plasticity, highly fractured,disturbed texture.
Hard, moist, gray, CLAY (CL); low to mediumplasticity, slightly silty, frequent lighter coloredlaminae, scattered fine sand laminae, relativelyundisturbed.
Bottom of boring at 51.5 feet.
71110
71716
111018
S-10
S-11
S-12
Vibrating wire piezo
(S/N 11-5477) installed
at 45.5' bgs.
Ground Surface Elev
30 40
EB-12Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
45
50
55
0
9/27/2011-9/28/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 2
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
3 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
45
50
55
91
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
50
45
40
35
N-valueWater Content %
34.0
6"
ROAD FILL
Loose, moist, dark brown, silty, sandy GRAVEL(GM); poorly graded fine to coarse, subroundedto subangular gravel, poorly graded fine tomedium sand, scattered asphalt debris.
ACTIVE SLIDE DEBRIS
Loose, moist, brown SAND (SP); poorly gradedfine to medium sand, trace gravel and silt.
Becomes medium dense, brown to light gray withslight rust staining/oxidation at 10 feet.
Becomes loose at 15 feet.
641
644
487
322
S-1
S-2
S-3
S-4
Data logger (S/N
37415) and steel flush
monument at ground
surface
Installed 2-3/4" dia.
slope indicator casing
to 43.04' bgs.
Casing grouted in
place with mix
containing 94 lb
Portland cement, 25 lb
bentonite gel, 30
gallons water.
Grout take estimated at
110% of the theoretical
volume.
Ground Surface Elev
30 40
EB-13Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
5
10
15
0
9/28/2011-9/30/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 3
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
1 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
5
10
15
86
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
85
80
75
70
N-valueWater Content %
22.5
6"
ACTIVE SLIDE DEBRIS
Loose, moist, brown SAND (SP); poorly gradedfine to medium sand, trace gravel and silt.Becomes very moist to wet at 20 feet.
Becomes very loose at 25 feet.
VASHON GLACIOLACUSTRINE
Stiff, very moist, blue-gray, silty CLAY (CL); lowplasticity, high angle fractures, disturbed texture.
Intermixed zones of medium dense, wet, graySAND (SP); poorly graded fine to medium sandwith scattered gravel.
Hard, moist, blue-gray, silty CLAY (CL); lowplasticity, thin laminae, relatively undisturbed.
123
102
3410
142142
S-5
S-6
S-7
S-8
Vibrating wire piezo
(S/N 11-5478) installed
at 38.04' bgs.
Ground Surface Elev
30 40
EB-13Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
25
30
35
0
9/28/2011-9/30/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 3
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
2 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
25
30
35
86
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
65
60
55
50
N-valueWater Content %
22.5
6"
50+
Hard, moist, blue-gray, silty CLAY (CL); lowplasticity, thin laminae, relatively undisturbed.
Bottom of boring at 45.83 feet.
2650/3.5"
4450/4"
S-9
S-10
Ground Surface Elev
30 40
EB-13Washington Boulevard Landslide
Project Number Sheet
Figure No.
Depth to Water (ft BGS)
45
50
55
0
9/28/2011-9/30/2011
_GE
OT
EC
H B
OR
ING
LO
G W
AS
HIN
GT
ON
BO
ULE
VA
RD
LA
ND
SLI
DE
.GP
J O
ctob
er 2
6, 2
011
Logged by:
Start/Finish Date
A- 3
Davies Drilling / Modified B-53 Track Rig
MR: Mud Rotary
Driller/Equipment:
10 20
Blows/
Approved by:
HSA / Cathead / 140# / 30" Drop
Project Name:
Location:
3 of 3
Boring Log
Borehole Completion MaterialType
SampleType/ID
JLP
Drilling Method:
HSA: Hollow Stem Auger
Washington Boulevard NE, Kingston, WA
45
50
55
86
Depth /Elevation
(feet)
Tests
No Recovery
50
Sampler Type:
Depth(ft)
Drilling Method/Hammer:
Description
AJH
Standard Penetration Test(ASTM D1586)
Boring Number
060036
45
40
35
30
N-valueWater Content %
22.5
6"
50+
50+