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SOILS AND FOUNDATION
REPORT NO. 01-08
PROJECT PRA- DEWA 14(13)
RECONSTRUCTION OF RAYMONDSKILL CREEK BRIDGE
US ROUTE 209
DELAWARE WATER GAP NATIONAL RECREATION AREA
PIKE COUNTY, PENNSYLVANIA
U.S. Department of Transportation Federal Highway Administration
Eastern Federal Lands Highway Division 21400 Ridgetop Circle
Sterling, VA 20147
March 2010
TABLE OF CONTENTS
REPORT PAGE
INTRODUCTION
General Project Description Regional Geology Soil Survey
PROCEDURES AND RESULTS
General Sampling Field Tests and Measurements Data Summary Laboratory Testing Findings
CONCLUSION AND RECOMMENDATIONS
DISCLAIMER/LIMITATIONS CLAUSE
APPENDICES
APPENDIX A – Figures APPENDIX B – Boring Location Plan APPENDIX C – Boring Logs APPENDIX D – Laboratory Data APPENDIX E – Substructure Typicals
APPENDIX F – Concrete Core Petrographic Analysis APPENDIX G – Representative Photographs
Note: Design changes subsequent to publication of this report and prior to the project’s advertisement will be documented by a memo inserted after the title page.
Project: PRA-DEWA 14(13) Reconstruction of Raymondskill Creek Bridge Delaware Water Gap Soils and Foundation Report Pike County, Pennsylvania No. 01-08
U.S. DEPARTMENT OF TRANSPORTATION
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
SOILS AND FOUNDATION
REPORT NO. 01-08
PROJECT PRA-DEWA 14(13)
RECONSTRUCTION OF RAYMONDSKILL CREEK BRIDGE
US ROUTE 209
DELAWARE WATER GAP NATIONAL RECREATIONAL AREA
PIKE COUNTY, PENNSYLVANIA
INTRODUCTION
General
This report presents the results of our geotechnical subsurface investigation and laboratory testing for Project PRA-DEWA 14(13). No design analysis or recommendations were performed for this project since it was planned as a design/build (D/B) contract. The project is located along U.S Route 209 in the Delaware Water Gap National Recreation Area (DEWA NRA), in Pike County, Pennsylvania. The general site location is shown on Figure 1, “Site Location and Vicinity Map,” in Appendix A.
Project Description
U.S. Route 209 is the main north to south highway through DEWA NRA and connects Interstate 84 North with Interstate 80 South. It is located in the northeast corner of PA, between Milford (north) and Stroudsburg (south). The Raymondskill Creek Bridge is located on U.S. Route 209 at MP 18.3 and 2.7 miles south of Route 206. The bridge was constructed in 1955 and consists of concrete abutments and wingwalls supporting fourteen (14) 36” x 27” pre-stressed concrete box beams overlaid with 8 inches of bituminous paving. The exiting bridge total length is 52.0 ft with a clear deck width of 40.5 ft. Both of the roadway approaches are on a horizontally curved alignment with a skew angle of 30º. The bridge superstructure is elevated to accommodate the curvature. No as-built are available.
The proposed project limits are within existing National Park Service (NPS) right-of-way.
The project consist of replacing the existing bridge superstructure with fourteen (14) AASHTO BI-36 adjacent box girders and a 4-inch latex modified concrete (LMC) overlay, constructing new approach slabs and reconstructing the abutment seats, as well as performing suitable wingwall and abutment repairs and other miscellaneous work. Wingwalls, abutments and foundations would require stabilization and strengthening through the use of tiebacks and/or underpinning. This report summarizes Eastern Federal Lands’ subsurface investigations findings. It will be the contractor’s decision to perform additional investigation to help with the substructure strengthening.
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Regional Geology
Accordingly to Department of Conservation and Natural Resources (DCNR) “Geologic Map of Pennsylvania” the bridge is underlain by Devonian Formation. The Devonian Formation is composed of red sandstone, gray and black shale, limestone and chert. In some locations also flagstone, silica, sand clay and lime can be found. Refer to Figure 2 in Appendix A for a “Geologic Map” of the project area.
Soil Survey
Accordingly to United State Department of Agriculture “1969 Soil Survey of Pike County, Pennsylvania” the surficial soil at the site consists of Chenanga - Tunkhannock-Tiaga, Dekalb - Manlius-Oquaga and Stony Land – Rushtown associations.
The Chenanga - Tunkhannock-Tiaga Deep association is a well-drained, nearly level to gently sloping, dominantly gravelly soils on low terrace in major stream valleys. The Dekalb
- Manlius-Oquaga association is moderately deep, well-drained, gently sloping to steep, very stony to shaly, soils on uplands. The Stony Land - Rushtown association is a chiefly steep, stony and shaly areas along the river bluffs. Refer to Figure 3 in Appendix A for a “Soil Survey Map” of the project area.
PROCEDURES AND RESULTS
General
The Eastern Federal Lands Highway Division’s (EFLHD) Subsurface Exploration Team conducted two subsurface investigation programs at the project site. The first subsurface investigation was conducted from November 2 through 4, 2007. Additional subsurface information was required to complete our geotechnical recommendations; therefore a second investigation was conducted from June 24 through 26, 2009. The subsurface investigation program consisted of drilling a total of nine (9) borings, two (2) auger probe, two (2) concrete cores for petrographic analyses and one (1) test pit (TP). Dynamic Cone Penetration (DCP) tests were performed in the TP located near the south abutment.
Borings B-1, B-2, P-1, P-2, auger probe OB-1 and the two (2) concrete core petrographic analyses were performed during November 2007. Auger probe BB-1, borings BB-2, BB-3, BB-4 including DCP and test pit (TP-1) were performed during June 2009.
A summary of the boring locations is provided in Table 1:
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Table 1. Borehole Locations
Borehole Location
B-2 and BB-1 Southbound, North Abutment
OB-1 and BB-2 Southbound, South Abutment
BB-4 Northbound, North Abutment
BB-3 Northbound, South Abutment
P-1 Southbound
P-2 Northbound
Borings were advanced to depth using hollow stem augers and a CME 850 rotary, track-mounted drill rig. The location of each boring may be referenced on Boring Location Plan drawing in Appendix B.
Sampling
The boreholes were drilled to depths ranging from 5.0 to 47.0 ft below the existing ground surface. Borings were advanced using 3¾-in. (inside diameter) hollow stem augers. Standard Penetration Testing (SPT) was performed using a 2¼-in. (outside diameter) split-spoon sampler in accordance with AASHTO 7200-87 and AASHTO T206-87. Samples were obtained by driving the split-spoon sampler a distance of 24-in., or until auger refusal, into the undisturbed soil under the impact of a 140-lb. automatic hammer free-falling 30 inches.
The number of hammer blows required to advance the split-spoon sampler the middle foot of the 24-in. sample interval is designated as the “Standard Penetration Resistance” or N-value.
Auger refusal is defined by 50 blows per 1-inch of penetration of the split-spoon sampler.
The number of blows required to advance the sampler through each 6-in. interval was recorded on field boring logs. Representative portions of split-spoon samples were preserved in glass jars for laboratory testing. The sampling sequence and associated jar samples for each boring are presented on its appropriate Boring Log in Appendix C.
Water levels, if present, were measured in the boring logs at the time and under the conditions stated on boring logs.
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Field Tests and Measurements
The EFLHD geotechnical crew performed the following field tests and took measurements during the course of the subsurface exploration. A field description by color and texture was made for each recovered sample. The boring locations were determined by measuring from features present on-site and by GPS. Boring elevations were determined from plan topography. The approximate location of borings is as shown on the Boring Location Plan sheet in Appendix B.
Data Summary
The results of field tests and measurements were recorded on the driller’s logs and appropriate data sheet in the field. These data sheets and logs contain information concerning the boring methods; samples attempted and recovered; indications of the presence of various material such as gravel, pebbles, organic matter, etc.; and observations of groundwater. They also contain interpretations by the exploration foreman of the subsurface conditions based on the performance of the equipment and cuttings brought to the surface by the drilling tools.
Therefore, the field data represents both factual and interpretative information.
The boring logs in Appendix C of this report represent a compilation of field laboratory data and description of the soil samples by a geotechnical engineer. These records occasionally do not include all data recorded on driller’s logs and field data sheets, but do include all information considered relevant to the design and preparation of this report.
Groundwater level readings were made in the boreholes at the times and under the conditions stated on the boring logs. Fluctuations in groundwater level due to seasonal variations, rainfall, temperature, and other factors not evident at the time measurements were made should be expected.
Laboratory Testing
A laboratory testing program was conducted on representative soil samples recovered during the subsurface explorations conducted on 2009. The primary purpose of the testing program was to aid in classification and evaluation of the engineering properties of soil and rock present at the site. Laboratory tests included are grain size distributions (AASHTO T-88), Atterberg limits (AASHTO T-89, T - 90) and natural water contents (AASHTO T-265). The results of the laboratory testing program are presented in Appendix D and summarized below in Table 1.
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Table 2. Summary of Laboratory Test Results
Moisture Content
Liquid Limit(1)
Plastic Limit(2) Fines Boring
No.
Sample
No.
Sample Depth
(ft) (%) (%) (%) (%)
Classification
BB-3 J-2 20.0-22.0 19.2 --- --- --- ---
BB-3 J-3 23.0-25.0 19.9 ND NP 10.0 A-1-b
BB-3 J-6 30.0-32.0 9.9 ND NP 8.6 A-1-b
BB-3 J-8 40.0-41.4 17.3 ND NP 7.1 A-1-b
BB-4 J-1 18.0-20.0 --- --- --- 13.3 ---
BB-4 J-2 20.0-22.0 13.7 ND NP 14.8 A-1-b
BB-4 J-5 28.0-30.0 12.2 ND NP 8.3 A-1-b
BB-4 J-7 35.0-37.0 10.5 ND NP 8.3 A-1-b
BB-4 J-9 45.0-47.0 20.5 ND NP 20.5 A-1-b
(1) ND = No determine (2) NP = Non-plastic
Findings
Descriptions of the subsurface soil conditions encountered during the subsurface explorations conducted at the site are provided below in order of increasing depth below the ground surface. The stratification lines designating the interfaces between soil types on the boring logs in Appendix C represent approximate boundaries. The transition between materials may be gradual. It should be noted that one or more of the units may be absent at specific locations. As indicated in Table 1, all samples tested were determined to be non-plastic.
ASPHALT – Asphalt pavement sections were encountered from ground surface to a depth of 0.6 to 1.0 ft in all borings.
FILL – Fill consisting of gray to light brown, fine to medium silty sand with some gravel were encountered in dry to moist conditions below the asphalt pavement sections to depths between 15.0 and 20.0 ft in all the borings. SPT resistance values recorded within this material were between 25 and 63 blows per foot (bpf), indicating medium dense to very dense conditions.
GRAVEL – Brown, well-graded gravel with some sand and little silt were encountered in wet conditions below the fill to depths between 25 and 27.5 ft in borings BB-3 and BB-4. SPT resistance values recorded within this material were between 3 and 42 bpf, indicating very loose to dense condition. AASHTO soil classification for this layer was A-1-b.
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
GRAVEL and SAND – Brown and gray, well-graded gravel and sand with trace of silt were encountered in wet conditions below the gravel layer to depths between 37.0 and 42.8 ft in borings BB-3 and BB-4. SPT resistance values recorded within this material were between 25 and auger refusal indicating medium dense to very dense conditions. AASHTO soil classification for this layer is A-1-b.
SILTY SAND – Brown to dark gray, fine to course silty sand with some gravel was encountered in wet conditions below the gravel and sand layer to a depth of 47.3 ft in Boring BB-4. SPT resistance values recorded within this material were 47 bpf to auger refusal indicating very dense conditions. AASHTO soil classification for this layer is A-1-b.
Groundwater was encountered at depths ranging between 16.5 and 23.0 ft in Borings B-1, B- 2, BB-3 and BB-4. Fluctuations in ground water level due to seasonal variations, rainfall, temperature, and other factors not evident at the time measurements were made should be expected.
Two (2) concrete cores of approximately 8 in. long and 4 in. diameter retrieved from the north abutment were tested for compressive strength and subjected to petrographic examination on December 13, 2007 by Dipayan Jana of Construction Materials Consultants, Inc. of Greensburg, PA. The consultant’s report indicated that obtained compressive strengths were 4020 and 3860 psi indicating marginal or less than common industry requirements of at least 4000 to 4500 psi. However, the study concludes that based on the detailed petrographic examination and compressive strength results, the overall condition of the concrete cores are judged to be reasonably sound with no evidence of any distress or deterioration. These samples were retrieved from locations approximately 1 to 2 feet offset from a major vertical crack. The details of the petrographic analysis can be found in the Consultant’s provided report at Appendix F.
TP-1 was performed adjacent to the footings of the south abutment between weepholes 1 and 2 using shovels and small excavator. The test pit was performed with the purpose of identifying the bridge foundation type and soil conditions immediately below the footing.
The test pit was excavated to a maximum depth of 25 in. It was terminated at this depth because the excavated material continued to cave into the hole and water was quickly filling up excavated space. DCP tests measurements were recorded in the gravelly sand and range from 3 to 24 blows/1.75 in. increment. The bottom of the footing was not found within the excavated depth but was estimated to be within 2 to 3 inches of TP termination. The possible footing depth is approximately 28 in. DCP data are presented in Table 3.
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Table 3. DCP Data
Depth
(from top of the footing)
(in.)
Increments
Number of Blows / 1.75
in. increments
Description
8.25
1.75 7 Loose silty sand
10.0
3.5 11 Medium dense silty sand
11.75
5.25 15 Medium dense silty sand
13.5
7.0 20 Medium dense silty sand
15.25
8.75 14 Medium dense silty sand
17.0
10.5 20 Medium dense silty sand
18.75
12.25 24 Medium dense silty sand
20.50
12.5 9 Loose silty sand
20.75
14.25 8 Loose silty sand
22.5
16.0 9 Loose silty sand
24.25
17.75 10 Loose silty sand
26.0
19.5 9 Loose silty sand
27.75
21.25 8 Loose silty sand
29.5
23.0 7 Loose silty sand
31.25
24.75 8 Loose silty sand
33.0
26.5 7 Loose gravel, some sand, little silt
34.75
28.25 5 Loose gravel, some sand, little silt
36.5
30.0 3 Very loose gravel, some sand, little silt
38.25
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VA
Table 3. DCP Test Data (Continue)
(from top of the footing)
Increments
Number of
Blows
Description
31.75 3 Very loose gravel, some sand, little silt 40.0
33.5 5 Loose gravel, some sand, little silt 41.75
35.25 5 Loose gravel, some sand, little silt 43.5
37.0 3 Very loose gravel, some sand, little silt 45.25
38.75 12 Medium dense gravel, some sand, little silt
40.5 20 Medium dense gravel, some sand, little silt 48.75
CONCLUSION AND RECOMMENDATIONS
The data in this report is being provided for the Contractor’s information. A sufficient number of borings, test pit, laboratory testing and measurements were performed at the north and south bridge abutments. However, since this project is proposed as design/build type of contract, it is the contractor’s responsibility to evaluate available data and determine the need for additional testing.
APPENDIX A
Figures
FIGURE 1
SITE LOCATION & VICINITY MAP
U.S. DEPARTMENT OF TRANSPORTATION
FEDERAL LANDS HIGHWAY DIVISION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VIRGINIA
STATEREG
DEWA14(13)NE
SHEET
NO.
PROJECT
TOTAL
SHEETS
3PA
Project: PRA-DEWA 14(13)
TOTAL
SHEETS
3PANE
SHEET
NO.
PROJECT
FIGURE 2
GEOLOGIC MAP
U.S. DEPARTMENT OF TRANSPORTATION
FEDERAL LANDS HIGHWAY DIVISION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VIRGINIA
STATEREG
DEWA14(13)
Project: PRA-DEWA14(13)
Devonian (354-417 million years)
Sandstone, gray and black shale, limestone and chert, flagstone, silica, sand, clay, and lime
Chenanga-Tunkhannock-Tiaga association: Deep, well-drained, nearly level to gently sloping, dominantly gravelly soils on low terrace in major stream valleys.
Dekalb-Manlius-Oquaga association: Moderately deep and deep, well-drained, gently sloping to steep, very stony to shaly, soils on uplands.
Stony land-Rushtown association: Chiefly steep, stony and shaly areas along the river bluffs.
TOTAL
SHEETS
3PANE
SHEET
NO.
PROJECT
FIGURE 2
SOIL SURVEY MAP
U.S. DEPARTMENT OF TRANSPORTATION
FEDERAL LANDS HIGHWAY DIVISION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
STERLING, VIRGINIA
STATEREG
DEWA 14(13)
Project: PRA-DEWA 14(13)
APPENDIX B
Boring Location Plan
APPENDIX C
Boring Logs
Weather:
BB-1
Standard Penetration Test Data Liquid Limit
Operator:
Inspector:
G ra p h ic L o g
MATERIAL DESCRIPTION
B O
R
IN
G L
O G
D
E W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
T
/9
/1
B lo w s p e r in
Pike County, PA
PRA-DEWA14(13)- Raymondskill Bridge
SAMPLE
R ec hrs
(Blows / ft)D ep th S ca le ft)
La ye r D ep th ft)
At Completion:
Completed:
Hole Diameter:
At a depth of 11.4ft auger reached abutment.
-FILL-
11.4
Groundwater Depth:
Boring No.:
Boring Location:
T yp e
Vane Shear
Remarks:
Rock Core Diam:
Boring Method:
Density, Color, Plasticity, Size, Proportions, Moisture
SPT
After
Encountered at:
Sample Types:
N o.
Rock Core Penetrometer
1. Boring backfilled with auger cuttings upon completion.
2. No water was encountered during or after completion of drilling.
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 1
2.3 ft N. from N. Abt. Wall on S. Bound laneProject Location:
Plastic Limit
8.0 in.
Water Content %
806020
396.5 ft
UDAuger Cuttings
30 in.
K.Thornton
E le va tio n (f ee t)
Project Name:
Warm 140 lbs/Automatic R.Kingsley/ D. Hutchins
BORING LOG
6/24/09
HSA
6/24/09Boring Began:Surface Elevation:
Hammer Wt. & Type:
Hammer Drop:
Caved at:
385.1
Liquid Limit Standard Penetration Test Data
Boring No.:
Boring Location:
R ec hrs
B O
R
IN
G L
W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
/1
PRA-DEWA14(13)- Raymondskill Bridge
MATERIAL DESCRIPTION SAMPLE
Vane Shear
Inspector:
Operator:
Weather:
BB-2
2-50/6
Borehole stopped at 20 ft
At a depth of 19.0 ft auger reached abutment.
-FILL-
T yp e
Groundwater Depth:
0.2
20.0
18.5 J-1
Hole Diameter:
(Blows / ft)
Boring Method:
Completed:
D ep th S ca le ft)
La ye r D ep th ft)
At Completion:
Density, Color, Plasticity, Size, Proportions, Moisture
Rock Core Diam:
Project Name:
Encountered at:
Sample Types:
N o.
Penetrometer Rock Core
After
Project Location:
Water Content %
Pike County, PA
B lo w s p e r in
E le va tio n (f ee t)
SPT
1. Boring backfilled with auger cuttings upon completion.
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 1
5.3 ft S. from S. Abt. Wall on S. Bound lane
Plastic Limit
Auger Cuttings
30 in.
UD
G ra p h ic L o g
Remarks:
Hammer Wt. & Type: R.Kingsley/ D. Hutchins K.Thornton
6/24/09
HSA
6/24/09
140 lbs/Automatic Warm
Surface Elevation: Boring Began:
Hammer Drop:
Caved at:
BORING LOG
395.3 ft
8.0 in.
376.8
375.3
62"
Rock Core Diam:
Boring Method:
Density, Color, Plasticity, Size, Proportions, Moisture
Completed:
T yp eD ep th S ca le ft)
La ye r D ep th ft)
At Completion:
Groundwater Depth:
16.5 ft
Weather:
Hole Diameter:
BB-3
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
Vane Shear
B O
R
IN
G L
W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
/1
Boring No.:
Boring Location:
J-5
(Blows / ft)
1.5
0.8
0.9
1.4
27.5
18.0
J-4
J-3
J-2
J-1
20.0
Very dense, brown and gray, well graded GRAVEL and SAND, trace silt [A-1-b] (Wet)
Very loose to dense, brown, well graded GRAVEL, some sand, little silt [A-1-b] (Wet)
Medium dense, brown, SILTY SAND, trace concrete (Wet)
-FILL-
-FILL-
0.5 2-25-50/4
13-14-28-28
5-12-27-5
4-1-2-3
4-7-15-18
6/24/09
Penetrometer Rock CoreSPT
Water Content %
N o.
Sample Types:
E le va tio n (f ee t)
Project Name:
Warm R.Kingsley/ D. Hutchins
K.Thornton 6/24/09
HSA
1. Boring backfilled with auger cuttings upon completion.
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 2
7.5 ft S. from S. Abt. Wall on N. Bound lane
Plastic Limit
Project Location:
After
Encountered at:
Auger Cuttings
G ra p h ic L o g
Remarks:
Boring Began:
UD
hrs
B lo w s p e r in
Pike County, PA
PRA-DEWA14(13)- Raymondskill Bridge
SAMPLE
R ec
Inspector:
Operator:
BORING LOG
395.3 ft
Hammer Wt. & Type:
Caved at:
140 lbs/Automatic
Surface Elevation:
8.0 in.
30 in.Hammer Drop:
377.3
375.3
367.8
4258"
Boring No.:
Boring Location:
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
Operator:
Pike County, PA
PRA-DEWA14(13)- Raymondskill Bridge
B O
R
IN
G L
W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
/1
R ec
Inspector:
Weather:
BB-3
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
1.2
27-49-50/4
19-35-28-31
26-30-33-36
Auger refusal at 42.8ft
1.1
1.5
42.8
J-8
J-7
J-6
D ep th S ca le ft)
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
Very dense, brown and gray, well graded GRAVEL and SAND, trace silt [A-1-b] (Wet) (Continued)
La ye r D ep th ft)
At Completion:
Groundwater Depth:
16.5 ft
(Blows / ft)
Encountered at:
Sample Types:
N o.
Penetrometer Rock CoreSPT
Project Location:
SAMPLE
hrs
E le va tio n (f ee t)
Project Name:
1. Boring backfilled with auger cuttings upon completion.
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 2 of 2
7.5 ft S. from S. Abt. Wall on N. Bound lane
Plastic Limit
After 30 in. Warm
Water Content %
UD
G ra p h ic L o g
Remarks:
B lo w s p e r in
Auger Cuttings
Surface Elevation:
R.Kingsley/ D. Hutchins K.Thornton
6/24/09
HSA
6/24/09Boring Began:
Hammer Wt. & Type:
Hammer Drop:
Caved at:
BORING LOG
395.3 ft
8.0 in.
140 lbs/Automatic
352.5
44933"
Boring Method:
Density, Color, Plasticity, Size, Proportions, Moisture
Completed:
T yp eD ep th S ca le ft)
La ye r D ep th ft)
At Completion:
Groundwater Depth:
18.0 ft
Weather:
Hole Diameter:
BB-4
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
Vane Shear
Boring No.:
Boring Location:
B O
R
IN
G L
W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
/1
J-5
(Blows / ft)
0.8
1.0
0.8
1.0
25.0
0.8
J-4
J-3
J-2
J-1
18.0
Medium dense to very dense, brown, GRAVEL and SAND, trace silt [A-1-b] (Wet)
Loose to medium dense, brown, well graded GRAVEL, some sand, little silt [A-1-b] (Wet)
-FILL-
Pavement
0.9 8-39-19-31
7-11-20-31
7-10-15-17
5-4-6-3
6-6-5-4
Boring Began:
Penetrometer Rock CoreSPT
Water Content %
N o.
Sample Types:
E le va tio n (f ee t)
Project Name:
R.Kingsley/ D. Hutchins
6/25/09
HSA
6/25/09
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 2
6.5 ft. N. from N. Abut. Wall on N. Bound
Plastic Limit
K.Thornton
Project Location:
After
Encountered at:
1. Boring backfilled with auger cuttings upon completion.Auger Cuttings
Surface Elevation:
Warm
G ra p h ic L o g
Remarks:
B lo w s p e r in
UD
hrs
Pike County, PA
PRA-DEWA14(13)- Raymondskill Bridge
SAMPLE
R ec
Inspector:
Operator:140 lbs/Automatic
Caved at:
BORING LOG
396.5 ft
18.7 ft
8.0 in.
Hammer Drop:
30 in.
Hammer Wt. & Type:
395.7
378.5
371.5
Boring Location:
T yp e
Vane Shear
Rock Core Diam:
Boring Method:
Hole Diameter:
Density, Color, Plasticity, Size, Proportions, Moisture
Liquid Limit
SAMPLE
R ec
Inspector:
Operator:
B O
R
IN
G L
W
A
(1
B O
R
IN
G S
.G P
J F
H W
A
V A
.G
/1
Standard Penetration Test Data
MATERIAL DESCRIPTION
47.3
0.9
0.9
1.1
1.0
Completed:
34-50/6
37.0
J-9
J-8
J-7
J-6
Weather:
D ep th S ca le ft)
La ye r D ep th ft)
At Completion:
Groundwater Depth:
18.0 ft
2-11-14-16
17-44-34-50
Auger refusal at a depth of 47.3ft
Very dense, brown to dark gray, fine to course SILTY SAND, some gravel [A-1-b] (Wet)
Medium dense to very dense, brown, GRAVEL and SAND, trace silt [A-1-b] (Wet) (Continued)
11-21-26-36
(Blows / ft)
BB-4
K.Thornton
N o.
Penetrometer Rock CoreSPT
Encountered at:
Water Content %
E le va tio n (f ee t)
Project Name:
Warm R.Kingsley/ D. Hutchins
1. Boring backfilled with auger cuttings upon completion.
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 2 of 2
6.5 ft. N. from N. Abut. Wall on N. Bound
Plastic Limit
Sample Types:
Project Location:
After
6/25/09
Auger Cuttings Remarks:
UD
B lo w s p e r in hrs
Pike County, PA
PRA-DEWA14(13)- Raymondskill Bridge G ra p h ic
L o g
HSA
6/25/09Boring Began:Surface Elevation:
Hammer Drop: 30 in.
Caved at:
BORING LOG
Hammer Wt. & Type:
396.5 ft
20 60
140 lbs/Automatic
18.7 ft
8.0 in.
634"
359.5
349.2
Groundwater Depth:
Inspector:
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
D ep th S ca le ft)
La ye r D ep th ft)
At Completion:
18.0 ft
(Blows / ft)
Loose to very loose, gray-brown to dark brown, fine to medium SILTY SAND and GRAVEL, strong organic odor (Wet)
-ALLUVIUM-
Operator:
Weather:
B-1
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
Boring No.:
B O
R
IN
G L
B
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
/1 7/
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
J-3
1.3
23.0
17.0
0.6
J-7
J-6
Medium dense to very dense, gray to light brown, fine to medium SILTY SAND, some gravel (Dry to Moist)
-FILL-
J-4 1.1
J-2
J-1
J-5
Boring Location:
6-20-20-23
1-1-3-2
3-4-4-5
12-14-20-16
5-13-12-10
0.6
25-22-15-14
1.0
1.4
1.1
1.4
Asphalt Pavement Section
4-25-38-17
Project Name:
1. Groundwater was ecnountered at 18 ft
BORING LOG FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 2
US Rte 209, Northbound; behind south abutment
SPT
Water Content %
E le va tio n (f ee t)
Project Location:
After
Encountered at:
Sample Types:
N o.
Penetrometer Rock Core
B lo w s p e r in
UDAuger Cuttings
G ra p h ic L o g Plastic Limit
Remarks:
hrs
Delaware Water Gap National Recreation Area - Pike County, PA
PRA-DEWA 14(13)
SAMPLE
R ec
Boring Began:
A. Anderson
11/2/07
R. Kingsley/D. Hutchins N/A Sunny 36-41 ºF
11/2/07Surface Elevation:
Hammer Wt. & Type:
Hammer Drop:
8.0 in.
HSA
30 in.
140 lbs/Automatic
395.5 ft Caved at:
372.5
378.5
394.9
B-1
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
Operator:
Boring No.:
Boring Location:
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
G ra p h ic L o g
Remarks:
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
B lo w s p e r in
Weather:
Delaware Water Gap National Recreation Area - Pike County, PA
PRA-DEWA 14(13)
SAMPLE
R ec
Inspector:
hrs
0.9
10-30-30-23
9-20-28-30
12-26-23-21
Borehole Terminated @ 37.0 ft
1.0
1.4
37.0
J-10
J-9
J-8
D ep th S ca le ft)
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
Dense to very dense, gray to dark brown, fine to medium SILTY SAND and GRAVEL (Wet)
-ALLUVIUM- (Continued)
La ye r D ep th ft)
At Completion:
Groundwater Depth:
18.0 ft
(Blows / ft)
U. S. DEPARTMENT OF TRANSPORTATION
Penetrometer Rock CoreSPT
1. Groundwater was ecnountered at 18 ft
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
Sample Types:
Sheet: 2 of 2
Plastic Limit
BORING LOG
N o.
Project Location:
After
Encountered at:
30 in.
395.5 ft
US Rte 209, Northbound; behind south abutment
140 lbs/Automatic
Hammer Drop:
Caved at:
UDAuger Cuttings
Water Content %
8.0 in.Hammer Wt. & Type:
E le va tio n (f ee t)
Project Name:
R. Kingsley/D. Hutchins A. Anderson
11/2/07
N/A
HSA
11/2/07
Sunny 36-41 ºF
Surface Elevation: Boring Began:
358.5 yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
Groundwater Depth:
Boring No.:
Boring Method:
Hole Diameter:
Completed:
D ep th S ca le ft)
La ye r D ep th ft)
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
Delaware Water Gap National Recreation Area - Pike County, PA
PRA-DEWA 14(13)
SAMPLE
R ec
Inspector:
Operator:
Weather:
Boring Location:
B-2
Liquid Limit
MATERIAL DESCRIPTION
J-4
1.2
0.3
1.1
1.3
1.2
19.0
At Completion:
J-5
J-3
J-2
J-1
1.0
23.0 ft
(Blows / ft)
Dense to very dense, gray to yellow-brown, fine to medium SILTY SAND and GRAVEL (Wet)
-ALLUVIUM-
Medium dense to dense, gray to light brown, fine to medium SILTY SAND, some gravel (Dry to Moist)
-FILL-
Asphalt Pavement Section
41-48-50/3"
6-50/1.2"
8-7-21-18
12-16-15-13
20-17-12-8
Plastic Limit
1. Groundwater was ecnountered at 23 ft
BORING LOG FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Standard Penetration Test Data
Penetrometer
Water Content %
Sheet: 1 of 2
SPT Rock Core
Project Location:
After
Encountered at:
Sample Types:
N o.
US Rte 209 Southbound; behind north abutment
140 lbs/Automatic
806020
30 in.
8.0 in.
UD
G ra p h ic L o g
Remarks:
B lo w s p e r in hrs
Boring Began:
E le va tio n (f ee t)
A. Anderson 11/2/07
N/A Sunny 40-45 ºF R. Kingsley/D. Hutchins
Auger Cuttings
11/2/07
HSA
Surface Elevation:
Hammer Wt. & Type:
Hammer Drop:
Caved at:
397.2 ft
Project Name:
9"
378.2
396.2
1.2"
MATERIAL DESCRIPTION
Boring No.:
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
Boring Location:
B lo w s p e r in
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
Delaware Water Gap National Recreation Area - Pike County, PA
Standard Penetration Test Data
B-2
SAMPLE
R ec
Inspector:
Operator:
Weather:Rock Core Diam:
PRA-DEWA 14(13)
8-28-23-18
1.0
0.6
1.4
6-28-26-41
37.0
J-9
J-8
J-7
J-6
0.8
Boring Method:
Hole Diameter:
Completed:
D ep th S ca le ft)
La ye r D ep th ft)
5-14-18-31
Groundwater Depth:
6-23-38-40
23.0 ft
(Blows / ft)
Borehole Terminated @ 37.0 ft
Dense to very dense, gray to yellow-brown, fine to medium SILTY SAND and GRAVEL (Wet)
-ALLUVIUM- (Continued) hrs At Completion:
Sheet: 2 of 2
Rock CoreSPT
1. Groundwater was ecnountered at 23 ft
BORING LOG
U. S. DEPARTMENT OF TRANSPORTATION
N o.
Plastic Limit
Remarks:
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
Penetrometer
Project Location:
After
Encountered at:
Sample Types:
Caved at:
397.2 ft
8.0 in.140 lbs/Automatic
Water Content %
US Rte 209 Southbound; behind north abutment
30 in.
UDAuger Cuttings
G ra p h ic L o g
Project Name:
E le va tio n (f ee t)
Sunny 40-45 ºF R. Kingsley/D. Hutchins
A. Anderson Hammer Wt. & Type:
N/A
HSA
11/2/07Boring Began:Surface Elevation:
Hammer Drop:
11/2/07
360.2
R ec
Inspector:
Operator:
Weather:
UD
OB-1
Liquid Limit
MATERIAL DESCRIPTION
Boring No.:
Auger Cuttings
G ra p h ic L o g
Remarks:
SAMPLE
B lo w s p e r in hrs
Delaware Water Gap National Recreation Area - Pike County, PA
PRA-DEWA 14(13)
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
Boring Location:
Groundwater Depth:
(Blows / ft)
Dark brown, fine to medium SILTY SAND and GRAVEL, organic odor (Moist to Wet)
-ALLUVIUM-
La ye r D ep th ft)
15.0
Gray to brown, fine to medium SILTY SAND, some gravel (Dry to Moist)
-FILL-
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
At Completion:
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
D ep th S ca le ft)
Penetrometer Rock CoreSPT
Encountered at:
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
Sheet: 1 of 2
US Rte 209 Southbound; right shoulder
Plastic Limit
N o.
Sample Types:
Project Location:
After
BORING LOG
1. Probehole to determine if subsurface conditions are consistent with bridge borings.
2. Borehole terminated upon reaching auger refusal on a boulder
Surface Elevation:
Hammer Wt. & Type:
Hammer Drop:
Caved at:
397.0 ft Boring Began:
140 lbs/Automatic 8.0 in.
806020
30 in.
Water Content %
11/4/07
E le va tio n (f ee t)
R. Kingsley/D. Hutchins
HSA
N/A
11/4/07 A. Anderson
Project Name:
Sunny 38-43 ºF
382.0
Operator:
PRA-DEWA 14(13)
SAMPLE
R ec
Inspector:
Weather:
OB-1
Standard Penetration Test Data Liquid Limit
G ra p h ic L o g
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
UDAuger Cuttings
Delaware Water Gap National Recreation Area - Pike County, PA
Remarks:
B lo w s p e r in hrs
MATERIAL DESCRIPTION
D ep th S ca le ft)
La ye r D ep th ft)
Hole Diameter:
Groundwater Depth:
Boring Method:
(Blows / ft)
Borehole Terminated @ 26.0 ft 26.0
At Completion:
Vane Shear
Boring No.:
Boring Location:
Completed:
Density, Color, Plasticity, Size, Proportions, Moisture
Rock Core Diam:
T yp e
N o.
Penetrometer Rock CoreSPT
1. Probehole to determine if subsurface conditions are consistent with bridge borings.
2. Borehole terminated upon reaching auger refusal on a boulder
BORING LOG FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
U. S. DEPARTMENT OF TRANSPORTATION
US Rte 209 Southbound; right shoulder
Sample Types:
Encountered at:
Project Location:
After
Plastic Limit
Caved at:
11/4/07
Sheet: 2 of 2
Surface Elevation:
Hammer Wt. & Type:
Hammer Drop: N/A
HSA
397.0 ft
8.0 in.140 lbs/Automatic
806020
30 in.
Boring Began:
Water Content %
11/4/07
E le va tio n (f ee t)
Project Name:
Sunny 38-43 ºF R. Kingsley/D. Hutchins
A. Anderson
371.0
Remarks:
P-1
Standard Penetration Test Data Liquid Limit
MATERIAL DESCRIPTION
Weather:
Boring Location:
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
PRA-DEWA 14(13)
B lo w s p e r in
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/
Delaware Water Gap National Recreation Area - Pike County, PA
SAMPLE
R ec
Inspector:
Operator:
2.0
Borehole Terminated @ 4.6 ft
Dense to very dense, gray to light brown, fine to medium SILTY SAND, some gravel (Dry to Moist)
-FILL-
Asphalt Pavement Section
35-24-16-18
22-36-28-25
1.6
4.6
0.6
D ep th S ca le ft)
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
La ye r D ep th ft)
At Completion:
Groundwater Depth:
(Blows / ft)
Sheet: 1 of 1
Rock CoreSPT
BORING LOG
U. S. DEPARTMENT OF TRANSPORTATION
N o.
US Rte 209 Southbound hrs
G ra p h ic L o g
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
Penetrometer
Project Location:
After
Encountered at:
Sample Types:
Caved at:
4.5 in.
Water Content %
Plastic Limit
140 lbs/Automatic
UDAuger Cuttings
30 in.
Project Name:
Overcast 40-45 ºF R. Kingsley/D. Hutchins
A. Anderson
N/A
HSA
11/3/07Boring Began:Surface Elevation: 11/3/07
Hammer Drop:
E le va tio n (f ee t)
Hammer Wt. & Type:
MATERIAL DESCRIPTION
Boring Location:
Weather:
T yp eDensity, Color, Plasticity, Size, Proportions, Moisture
Vane Shear
Boring No.:
B lo w s p e r in
B O
R
IN
G L
R
IN
G
L O
G
(A O
A
G P
J F
H W
A _V
A .G
7/ hrs
P-2PRA-DEWA 14(13)
SAMPLE
R ec
Inspector:
Operator:
Delaware Water Gap National Recreation Area - Pike County, PA
Asphalt Pavement Section
21-18-14-10
23-40-501.2
5.0
1.0
J-2
J-1
1.5
Rock Core Diam:
Boring Method:
Hole Diameter:
Completed:
Dense to very dense, gray to light brown, fine to medium SILTY SAND, some gravel (Moist)
-FILL-
La ye r D ep th ft)
Borehole Terminated @ 5.0 ft
At Completion:
Groundwater Depth:
(Blows / ft)D ep th S ca le ft)
US Rte 209 Northbound
Rock CoreSPT
BORING LOG FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
Water Content %
Sheet: 1 of 1
N o.
Remarks:
U. S. DEPARTMENT OF TRANSPORTATION
Penetrometer
Project Location:
After
Encountered at:
Sample Types:
4.5 in.
Plastic Limit
30 in.
Caved at:
140 lbs/Automatic
UDAuger Cuttings
G ra p h ic L o g
Overcast 40-45 ºF
E le va tio n (f ee t)
R. Kingsley/D. Hutchins A. Anderson
11/3/07
HSA
11/3/07Boring Began:Surface Elevation:
Hammer Wt. & Type:
N/A
Project Name:
Hammer Drop:
APPENDIX D
Laboratory Data
SOIL DATA
NO.
AASHTODESCRIPTION
DEPTHSAMPLE
SOURCESYMBOL
Project No.:
Project:
Client:
Particle Size Distribution Report
P E
R C
E N
T F
IN
E
R
100 10 1 0.1 0.01 0.001200 GRAIN SIZE - mm
% + 3" % GRAVEL % SAND % SILT % CLAY
in in in
1- 1/ in in
3/ in
1/ in
3/ in
#4 #1
#2
#3
#4
#6
#1
#1
#2
0.0 51.5 38.5 10.0
(ft.)
DEWA 14(13)
Raymondskill Creek Bridge
GEOTECH
BB-3/J-3 23-25 Poorly graded gravel with silt and sand A-1-a
Particle Size Distribution Report
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
0.0 47.4 44.0 8.6
BB-3/J-6 30-32 Poorly graded gravel with silt and sand A-1-a
0.0 54.2 38.7 7.1
BB-3/J-9 40-41.4 Poorly graded gravel with silt and sand A-1-a
0.0 51.0 34.2 14.8
BB-4/J-2 20-22 Silty gravel with sand A-1-a
0.0 50.0 41.7 8.3
BB-4/J-5 28-30 Poorly graded gravel with silt and sand A-1-a
AASHTODESCRIPTION
DEPTHSAMPLE
SOURCESYMBOL
Project No.:
Project:
Client:
Particle Size Distribution Report
P E
R C
E N
T F
IN
E
R
100 10 1 0.1 0.01 0.001200 GRAIN SIZE - mm
% + 3" % GRAVEL % SAND % SILT % CLAY
in in in
1- 1/ in in
3/ in
1/ in
3/ in
#4 #1
#2
#3
#4
#6
#1
#1
#2
0.0 46.7 43.3 10.0
(ft.)
DEWA 14(13)
Raymondskill Creek Bridge
GEOTECH
BB-4/J-7 35-37 Well-graded gravel with silt and sand A-1-a
Particle Size Distribution Report
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
0.0 38.9 40.6 20.5
BB-4/J-9 45-47 Silty sand with gravel A-1-b
AASHTODESCRIPTION
DEPTHSAMPLE
SOURCESYMBOL
Project No.:
Project:
Client:
Particle Size Distribution Report
P E
R C
E N
T F
IN
E
R
100 10 1 0.1 0.01 0.001200 GRAIN SIZE - mm
% + 3" % GRAVEL % SAND % SILT % CLAY
in in in
1- 1/ in in
3/ in
1/ in
3/ in
#4 #1
#2
#3
#4
#6
#1
#1
#2
0.0 26.6 54.2 19.2
(ft.)
DEWA 14(13)
Raymondskill Creek Bridge
FHWA/EFLHD
Raymondskill BB-3/J-2 20-22
Cr.
Particle Size Distribution Report
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
0.0 43.9 42.8 13.3
Raymondskill BB-4/J-1 18-20
Cr.
INDEXLIMITLIMITCONTENTNO.
PLASTICITYLIQUIDPLASTICWATERDEPTHSAMPLE
NATURAL
SOURCESYMBOL
Project No.:
Project:
Client:
LIQUID AND PLASTIC LIMITS TEST REPORT
(ft.)
AASHTO
DEWA 14(13)
Raymondskill Creek Bridge
GEOTECH
A-1-aNPNVNP19.923-25BB-3/J-3
LIQUID AND PLASTIC LIMITS TEST REPORT
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
A-1-aNPNVNP9.930-32BB-3/J-6
A-1-aNPNVNP17.340-41.4BB-3/J-9
A-1-aNPNVNP13.720-22BB-4/J-2
A-1-aNPNVNP12.228-30BB-4/J-5
10 30 50 70 90 110
LIQUID LIMIT
P
LA
S T
IC
IT
Y
IN
D E
X
PI
=L
L-
A-4 or A-2-4 A-5 or A-2-5
A-7-6
A-6 or A-2-6
A-7-5 or A-2-7
INDEXLIMITLIMITCONTENTNO.
PLASTICITYLIQUIDPLASTICWATERDEPTHSAMPLE
NATURAL
SOURCESYMBOL
Project No.:
Project:
Client:
LIQUID AND PLASTIC LIMITS TEST REPORT
(ft.)
AASHTO
DEWA 14(13)
Raymondskill Creek Bridge
GEOTECH
A-1-aNPNVNP10.535-37BB-4/J-7
LIQUID AND PLASTIC LIMITS TEST REPORT
FEDERAL HIGHWAY ADMINISTRATION
EASTERN FEDERAL LANDS HIGHWAY DIVISION
A-1-bNPNVNP7.845-47BB-4/J-9
10 30 50 70 90 110
LIQUID LIMIT
P
LA
S T
IC
IT
Y
IN
D E
X
PI
=L
L-
A-4 or A-2-4 A-5 or A-2-5
A-7-6
A-6 or A-2-6
A-7-5 or A-2-7
APPENDIX E
Substructure Typicals
APPENDIX F
Concrete Core Petrographic Analysis
DDeecceemmbbeerr 1133,, 22000077
CCMMCC 11110077228888
LLaabboorraattoorryy SSttuuddiieess ooff
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Construction Materials Consultants, Inc.
Berkshire Center, Suite 104
4727 Route 30 Greensburg, PA 15601 USA
Phone: 724-834-3551 Fax: 724-834-3556 www.cmc-concrete.com
Serving the Industry through Testing, Investigation, Evaluation, & Research
LABORATORY STUDIES OF
TWO CONCRETE CORES
FOR
(Raymondskill Creek Bridge)
CMC 1107288
12/13/2007
Construction Materials Consultants, Inc.
Berkshire Center, Suite 104
4727 Route 30 Greensburg, PA 15601 USA
Phone: 724-834-3551 Fax: 724-834-3556 www.cmc-concrete.com
Serving the Industry through Testing, Investigation, Evaluation, & Research
SUMMARY & DISCUSSION
Purpose & Background – Reported herein are the results of detailed laboratory studies of two concrete cores from André Anderson of the Federal Highway Administration. The cores reportedly came from the Raymondskill Creek Bridge, for the Project: DEWA 13(13), in order to assist with determining the need for replacement or repair of the abutment walls for the bridge.
The purposes of the investigation are to determine: (a) the composition, quality, and condition of concrete in the cores; (b) compressive strengths of concrete in both cores; and (c) evidence of any distress or deterioration in the concrete.
Determined Concrete Composition – Based on detailed petrographic examinations, the concrete is determined to be marginally air-entrained, and made using the following ingredients in the following estimated proportions:
(a) Siliceous crushed stone (sandstone-schist) coarse aggregate having a nominal maximum size of 3/4 in.;
(b) Natural siliceous (quartz-quartzite-sandstone-schist) sand fine aggregates having a nominal maximum size of 3/8 in.;
(c) A portland cement content estimated to be 5 to 51/2 bags per cubic yard;
(d) A water-cement ratio estimated to be 0.50 to 0.55; and
(e) An air content estimated to be 31/2 to 4 percent.
There is a deficiency of finer and intermediate sizes of coarse aggregate. Thus, the total aggregate grading is poor. Both coarse and fine aggregate particles are well distributed, and have been sound during their service in the concrete. The concrete is dense and well consolidated.
Surface Condition of Concrete – The exposed surface of the concrete, present at one end of the core, is smooth, gray, and sound, with no evidence of any distress or imperfection. Immediately beneath the exposed surface, however, are a few microcracks developed along the interface between the near-surface aggregate particles and surface mortar, which are judged to have formed by cyclic freezing and thawing of a marginally air-entrained concrete. The microcracks, however, CMC CONSTRUCTION MATERIALS CONSULTANTS, INC. CMC 1107288
Client: Federal Highway Administration; Project: Raymondskill Creek Bridge 12/13/2007 are present in small, localized scale and did not cause any macroscopical distress, such as macrocraking in the concrete. The overall condition of the concrete, even at the surface region, is still sound and serviceable.
Air Content, Air-Void System of Concrete, and Freeze-Thaw Durability – As mentioned, the concrete has a marginal air void system, consisting of a modest amount of entrained air voids, mostly less than 500 microns in size, and a few coarse and near-spherical entrapped air voids. The overall air void distribution is non-uniform; the total air content is estimated to be 31/2 to 4 percent.
The estimated air content is less than the common industry (e.g., ACI)-recommended minimum air content of 41/2 percent for a concrete containing similar aggregates, and exposed to cyclic freezing and thawing at critically saturated conditions. The overall air-void system (i.e., air void size distribution and relative spacing) is judged not consistent with the common industry
(ACI)recommendation for an air-entrained concrete to be durable in a cyclic freezing environment.
Despite having a lower-than-common recommended minimum air and a marginal air void system, the concrete, however, is still sound with no evidence of any major freezing-related distress, such as visible cracking or spalling. The apparent sound condition of concrete may indicate its exposure to freezing at conditions when the concrete was not “critically saturated” (which is not uncommon for vertical concrete structures where moisture does not remain on the concrete surface to increase its degree of saturation).
Compressive Strength – The determined compressive strengths of two cores, Nos. 1 and 2 are
4020 and 3860 psi, respectively. The strength results are consistent with the observed aggregate size, distribution, grading, cement content, and estimated water-cement ratio. The strength values obtained are marginal to, or slightly less than the common industry requirements of at least 4000 to
4500 psi strength for a concrete exposed to cyclic freezing and deicing chemicals (good strength of concrete is necessary to resist freezing-related stresses). The lower-than-industry recommended strength is in line with the estimated water-cement ratio of 0.50 to 0.55, which is higher than the common industry (ACI)-recommended maximum ratio of 0.45, for assuring durability of concrete in an environment of salts and snow.
Depth of Carbonation – The concrete shows approximately 1 in. deep carbonation of portland cement paste, which is higher than that usually observed in a well-consolidated, and well-cured concrete of reasonably good strength and durability. The high depth of carbonation is a consequence of long service life of concrete (prolonged interaction with atmospheric carbon dioxide), and relatively porous and permeable nature of concrete to atmospheric carbon dioxide
(due to its high water-cement ratio). Despite having a deep carbonation, however, the overall condition of concrete at the surface region is still reasonably good, with no evidence of any carbonation-induced significant softening of paste, or strength loss of concrete.
Overall Condition – Based on detailed petrographic examinations and compressive strength testing, the overall condition of concrete is judged to be reasonably sound with no evidence of any distress or deterioration (except a few near-surface microcracking). The concrete has a marginal air void system and low air content, which may not seriously affect the durability as long as the concrete remain under-saturated during freezing.
Based on the present observation, the overall condition and durability of concrete is judged to be reasonable, i.e., the concrete may remain serviceable as long as it is protected from moisture ingress and other deleterious environmental influences.
1. INTRODUCTION
Received for detailed laboratory studies were two concrete cores from André Anderson of the
Federal Highway Administration. The cores reportedly came from the Raymondskill Creek
Bridge for the Project: DEWA 13(13), in order to assist with determining the need for replacement or repair of the abutment walls for the bridge.
The purposes of the investigation are to determine: (a) the composition, quality, and condition of concrete in the cores; (b) compressive strengths of concrete in both cores; and (c) evidence of any distress or deterioration in the concrete.
2. METHODOLOGY
One core was requested for examination using the methods and procedures of ASTM C 856
"Practice for Petrographic Examination of Hardened Concrete." Petrographic examinations include:
(1) Detailed visual examinations of the core, as received;
(2) Low-power, stereomicroscopical examinations of freshly fractured and lapped cross sections of core at magnifications of up to 100X; and
(3) Examinations of oil immersion mounts and blue dye-mixed epoxy-impregnated thin section of concrete in a petrographic microscope at magnifications of up to 1000X.
Additionally, compressive strengths of two cores were tested by using the methods of ASTM C
42 "Standard Test Method for Obtaining and Testing Drilled Cores and Sawed Beams of
Concrete.
3. LABORATORY STUDIES
3.1 SAMPLES
Dimensions – Figures 1 and 2 show the cores, as received. The cores are identified as Nos. 1 and 2, having diameters of 43/4 in. and respective nominal lengths of 63/4 and 91/4 in. Figure 3 shows the lapped cross section of one core.
Surfaces – In both cores, one end is a flat, smooth, sound finished surface, representing the exposed surface of concrete, and the opposite end is a fresh fractured surface.
Cracks, Joints, and Large Voids – There are no large cracks, joints, or voids present. Both cores were received in sound and intact condition.
Embedded Items – The cores do not contain any reinforcing steel or fibers.
Resonance – The cores have a ringing resonance, when hammered.
3.2 PETROGRAPHIC EXAMINATIONS
3.2.1 Coarse Aggregate
Type and Nominal Maximum Size – Coarse aggregate is siliceous crushed stone having a nominal maximum size of 3/4 in.
Properties (Color, Angularity, Density, Hardness, Shape, Alteration, Coating, Cracking) –
Particles contain sandstone, quartzite, schist, and other siliceous rocks (Figures 4 and 5).
Particles are angular, light to dark gray, white, light to dark brown, beige, black, variably dense, hard, massive-textured, equidimensional, unaltered, and uncracked.
Gradation and Distribution – There is a deficiency of finer and intermediate sizes of coarse aggregate (Figure 3). Thus, the coarse aggregate particles are poorly graded (Figure 3), but well distributed, and have been sound during their service in the concrete.
Potential Alkali-Aggregate Reactivity – There is no evidence of alkali-aggregate reaction in the coarse aggregate.
3.2.2 Fine Aggregate
Type and Nominal Maximum Size – Fine aggregate is natural siliceous sand having a nominal maximum size of 3/8 in.
Rock Types – Particles contain major amounts of strained and unstrained quartz and minor amounts of quartzite, sandstone, feldspar, ferruginous rocks, and mafic minerals (Figures 4 and
5).
Properties (Color, Angularity, Density, Hardness, Shape, Alteration, Coating, Cracking) –
Particles are colorless, light gray to brown, subangular to subrounded, dense, hard, equidimensional to elongated, and unaltered.
Gradation and Distribution – Fine aggregate particles are well graded (Figure 3), well distributed, and have been sound during their service in the concrete.
Potential Alkali-Aggregate Reactivity – There is no evidence of alkali-silica reaction in the fine aggregate.
3.2.3 Paste
Properties (Color, Hardness, Porosity, Luster) – Paste is light brown at the top 1 in. and light gray in the interior, moderately hard to moderately soft, and moderately dense. Freshly fractured surfaces have subvitreous lusters and subconchoidal textures.
Residual and Relict Portland Cement Particles – Residual and relict portland cement particles are present and estimated to constitute 6 to 8 percent of the paste volume (Figure 5).
Calcium Hydroxide – The calcium hydroxide component of cement hydration occurs as small, platy, patchy units, and is estimated to constitute 8 to 10 percent of the paste volume.
Degree of Cement Hydration – Hydration of portland cement is normal.
Pozzolanic and Cementitious Materials – Besides portland cement, there is no other pozzolanic or cementitious materials present.
Estimated w/c and Portland Cement Content – The textural and compositional features of the paste are indicative of a portland cement content estimated to be 5 to 51/2 bags per cubic yard, and a water-cement ratio estimated to be 0.50 to 0.55.
Secondary Deposits – Besides carbonation at the surface region, there is no evidence of any secondary deposits in the concrete due to any deleterious reactions.
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