MDMB0010 Supplimental Geotechnical Reports Appendix.pdf
PDF 3 MB Posted
- Solicitation number
- RFQ 171 190000000344 3
- Issued by
- Allegan County, Michigan
About this file
Supplemental Geotechnical Reports Summary
This is a supplemental geotechnical investigation report and laboratory testing documentation prepared by The Mannik & Smith Group, Inc. for the Michigan Department of Technology, Management & Budget regarding dike repair work in Fennville Farms Zone 7, Allegan County, Michigan. The project involves evaluating a State-owned borrow site to determine soil suitability for proposed dike repairs. The investigation included seven test borings (SB-23 through SB-29) advanced to 10 feet below ground surface using Macro-Core sampling methods, with offset borings drilled via hollow stem auger to collect additional samples for laboratory analysis. Laboratory testing encompassed moisture content determinations, sieve analysis and hydrometer testing, Atterberg limits testing, organic content analysis, soil density determinations, modified Proctor compaction testing, and permeability testing in accordance with ASTM standards. The report was completed March 28, 2017, with a permeability testing addendum dated March 31, 2017.
The geotechnical investigation findings indicate two primary soil units within the upper 10 feet of the borrow site: Soil Unit 1 consisting of brown and gray silty clay, and Soil Unit 2 consisting of brown silty and clayey sand. MSG estimates the borrow source contains approximately 30 percent silty clay and 70 percent silty clayey sand by volume, with an estimated 44,000 cubic yards of clay available in bank condition. The report recommends utilizing approximately 3,800 cubic yards of clay (compacted) to construct the dike to full service water level (623 and 622 feet for top/middle and bottom sections, respectively) and an additional 3,925 cubic yards for finished elevations. Key recommendations include geotextile-reinforced aggregate subgrade preparation, compaction to 95 percent of modified Proctor maximum dry density, and implementation of a proof rolling procedure to detect unstable zones. The document emphasizes that without stabilizing the existing subgrade, primary consolidation settlement of 2.5 to 4 feet is anticipated over 3 to 15 years, but proper subgrade preparation can reduce post-construction settlement to 3 to 5 inches.
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March 31, 2017
Michael Richardson, Wildlife Technician Allegan State Game Area 4590 118th Avenue Allegan, Michigan 49010
Re: Addendum to Supplemental Geotechnical Report Permeability Test Results and Discussion
Fennville Farms Zone 7 Dike Repairs Allegan County, Michigan MSG Project No. MDMB0010
Dear Mr. Richardson:
The Mannik & Smith Group, Inc. (MSG) has issued a Supplemental Geotechnical Report for the subject project dated March 28, 2017. The purpose of this addendum is to present the permeability testing results on soil samples collected from a State-owned borrow site. The permeability tests were not completed at the time the Supplemental Geotechnical Report was issued. This addendum also includes a discussion of the test results.
LABORATORY SOIL PERMEABILITY TESTING
The soil samples used in the permeability testing were collected from a State-owned borrow site that may be potentially utilized for the proposed dike repairs. The approximate location of the subject borrow source is depicted in Figure 1 Site Location Map. A total of five permeability tests were performed in accordance with ASTM D5084. The soil samples utilized were collected from four of the seven boring locations. The boring locations are shown on the attached Figure 2 Boring Location Plan. Offset borings were augered next to borings advanced using the Macro Core® to collect additional sample volume for permeability tests. These offset boring locations were termed SB-XX GRAB on the attached testing results. The offset locations were generally within a 3 feet radius of the original borings.
Samples collected from SB-23 GRAB and SB-24 GRAB primarily consisted of clay and samples collected from SB- 25 GRAB and SB-27 GRAB primarily consisted of sand. Based on the investigation findings presented in the Supplemental Geotechnical Report, MSG estimates that the subject borrow source has about 30 percent silty clay (Soil Unit 1 as described in Supplemental Geotechnical Report dated March 28, 2017) and 70 percent silty clayey sand (Soil Unit 2) by volume in the upper 10 feet below existing ground surface. In order to evaluate different material types that could be collected from the borrow source, a mixed sample with about 30 percent Soil Unit 1 and 70 percent Soil Unit 2 was also tested. All samples were tested at their 95 percent of Modified Proctor maximum dry density and optimum moisture content. A brief summary of the testing results are shown in the table below. The complete results are attached to this addendum.
MDMB0010_Add_XZ_GEO_20170331.Docx
2193 Association Drive, Suite 200, Okemos, Michigan 48864 Tel: 517.316.9232 Fax: 517.316.9233 www.MannikSmithGroup.com
2193 Association Dr, Suite 200 Okemos, Michigan 48864 Tel: (517) 316-9232 Fax: (517) 316-9233 www.MannikSmithGroup.com
Figure 1: Site Location Map Fennville Farms Zone 7 Dike Repairs
Allegan County, Michigan
Notes:
The base map was adopted from Google Earth Image.
Tel: (517) 316-9232 Fax: (517) 316-9233 www.MannikSmithGroup.com
Figure 2: Boring Location Plan Fennville Farms Zone 7 Dike Repairs
Allegan County, Michigan
Notes:
RP.Mix-Bulk.xls
Project Name: Project No:
Client's Sample No. Date:
Visual Description: Depth:
Permeant: De-aired tap water 0.01 N CaSO4
Sample Preparation:
Sample was removed from a 3" Shelby tube and trimmed to length in a trimming jig. Any pebbles found on outer surface were removed and resulting voids were filled with material trimmed from the sample.
Material was adjusted to required moisture content and remolded at the required density.
Other: 95% of DD=127.9 pcf @ OMC=9.9%
Soil Properties:
Initial Moisture Content (%)
Initial Wet Density (pcf)
Initial Dry Density
(pcf)
Final Moisture Content
Final Wet Density
(pcf)
Final Dry Density
(pcf)
9.95 131.48 119.58 19.63 144.76 121.00
Formula:
K= h(t1)= a= h(t2)= L= Length of sample (cm) = 7.62 A= Cross-sectional area of RT= sample (cm2) = 41.624846 t= Elapsed time (sec) PB= 140.74
Degree of Saturation:
3/27/2017 7:05am 25.0 22.0 20.0 5.0 5.0 1.0
Permeability Measurement:
23.90 3.60 22.41 18 1.051
14.20 13.70 0.55 18 1.051
14.20 13.70 0.55 18 1.051
4.70 23.40 -20.64 18 1.051
23.60 1.70 24.17 18 1.051
15.10 10.40 5.19 18 1.051
15.10 10.40 5.19 18 1.051
3.30 22.60 -21.30 18 1.051
7.37E-06 cm/sec
Tested By: FRK Date: 3/29/2017
*The certificate shall not be reproduced except in full, without the written approval of MSG.
3/27/2017
6.81E-06
7.04E-06
7.10E-06
7.15E-06
7.40E-06
7.46E-06
RT
(from table) K (cm/sec)
Kcorrected
(cm/sec)
1,980
1,440
2,340
3/27/2017
Silty Sand with Clay
MDMB0010
3/28/2017
0-8'
1 3/27/2017 1,680 7.10E-06
Bias Pressure (cm) = psi x 70.37 cm/psi
7.46E-06
Correction factor for viscosity of water at various temperatures
TimeDate
Civil Engineering, Surveying and Environmental Consulting
TOLEDO CANTON LANSING DETROIT MONROE CLEVELAND COLUMBUS
Permeability Test Remolded
ASTM D5084
Before Saturation After Saturation
Fennville Farms Zone 7 Dike Repairs MIX GRAB (30% Clay + 70% Sand)
AVERAGE CORRECTED COEFFICIENT OF PERMEABILITY (K):
Pore Pressure Increase (psi)
= b
Head Pressure
(psi)
Skempton's Parameter
(B) = (b/a)
Lower Volume Reading
(VL)
h(t1) h(t2)
Confining Pressure Increase (psi) = a
Back Pressure
(psi)
Water Temp.
T (oC)
Reviewed By:MG/KL
Cross-sectional area of burette (cm2) = 0.906 Corrected Coefficient of Permeability (cm/sec)
Cell Pressure
(psi)
Test No. Date t (sec)
Upper Volume Reading
(VU)
3/27/2017 aL PB+h(t1) K= (ln )*RT 2At PB+h(t2)
X
X
VU(t1) - VL(t1) a
VU(t2) - VL(t2) a
RP.SB-23-Bulk.xls
Client's Sample No. Date:
Visual Description: Depth:
Permeant: De-aired tap water 0.01 N CaSO4
Sample Preparation:
Sample was removed from a 3" Shelby tube and trimmed to length in a trimming jig. Any pebbles found on outer surface were removed and resulting voids were filled with material trimmed from the sample.
Material was adjusted to required moisture content and remolded at the required density.
Other: 95% of DD=123.2 pcf @ OMC=12.4%
Soil Properties:
Initial Moisture Content (%)
Initial Wet Density (pcf)
Initial Dry Density
(pcf)
Final Moisture Content
Final Wet Density
(pcf)
Final Dry Density
(pcf)
12.37 132.05 117.51 17.19 138.05 117.79
Formula:
K= h(t1)= a= h(t2)= L= Length of sample (cm) = 7.73 A= Cross-sectional area of RT= sample (cm2) = 41.624846 t= Elapsed time (sec) PB= 140.74
Degree of Saturation:
3/27/2017 7:20 AM 25.0 22.0 20.0 5.0 5.0 1.0
Permeability Measurement:
23.90 2.60 23.51 18 1.051
20.60 5.90 16.23 18 1.051
20.60 5.90 16.23 18 1.051
17.60 9.20 9.27 18 1.051
17.60 9.20 9.27 18 1.051
8.90 18.10 -10.15 18 1.051
24.00 1.10 25.28 18 1.051
13.20 12.00 1.32 18 1.051
7.37E-07 cm/sec
Tested By: FRK Date: 3/29/2017
*The certificate shall not be reproduced except in full, without the written approval of MSG.
3/28/2017
6.29E-07
6.64E-07
6.98E-07
6.61E-07
6.97E-07
7.34E-07
RT
(from table) K (cm/sec)
Kcorrected
(cm/sec)
6,060
17,580
18,780
3/27/2017
Lean Clay with Sand
MDMB0010
3/28/2017
0-8'
1 3/27/2017 4,680 8.15E-07
Bias Pressure (cm) = psi x 70.37 cm/psi
8.57E-07
Correction factor for viscosity of water at various temperatures
TimeDate
Civil Engineering, Surveying and Environmental Consulting
TOLEDO CANTON LANSING DETROIT MONROE CLEVELAND COLUMBUS
Permeability Test Remolded
ASTM D5084
Before Saturation After Saturation
Fennville Farms Zone 7 Dike Repairs
SB-23 GRAB
AVERAGE CORRECTED COEFFICIENT OF PERMEABILITY (K):
Pore Pressure Increase (psi)
= b
Head Pressure
(psi)
Skempton's Parameter
(B) = (b/a)
Lower Volume Reading
(VL)
h(t1) h(t2)
Confining Pressure Increase (psi) = a
Back Pressure
(psi)
Water Temp.
T (oC)
Reviewed By:MG/KL
Cross-sectional area of burette (cm2) = 0.906 Corrected Coefficient of Permeability (cm/sec)
Cell Pressure
(psi)
Test No. Date t (sec)
Upper Volume Reading
(VU)
3/27/2017 aL PB+h(t1) K= (ln )*RT 2At PB+h(t2)
X
X
VU(t1) - VL(t1) a
RP.SB-24-Bulk.xls
Client's Sample No. Date:
Visual Description: Depth:
Permeant: De-aired tap water 0.01 N CaSO4
Sample Preparation:
Sample was removed from a 3" Shelby tube and trimmed to length in a trimming jig. Any pebbles found on outer surface were removed and resulting voids were filled with material trimmed from the sample.
Material was adjusted to required moisture content and remolded at the required density.
Other: 95% of DD=118.3pcf @ OMC=12.2%
Soil Properties:
Initial Moisture Content (%)
Initial Wet Density (pcf)
Initial Dry Density
(pcf)
Final Moisture Content
Final Wet Density
(pcf)
Final Dry Density
(pcf)
12.25 126.20 112.43 23.86 139.43 112.57
Formula:
K= h(t1)= a= h(t2)= L= Length of sample (cm) = 7.61 A= Cross-sectional area of RT= sample (cm2) = 41.624846 t= Elapsed time (sec) PB= 140.74
Degree of Saturation:
3/27/2017 7.25 am 25.0 22.0 20.0 5.0 5.0 1.0
Permeability Measurement:
24.50 2.40 24.39 18 1.051
20.60 6.50 15.56 18 1.051
20.60 6.50 15.56 18 1.051
16.10 11.10 5.52 18 1.051
16.10 11.10 5.52 18 1.051
5.00 22.80 -19.65 18 1.051
24.50 0.40 26.60 18 1.051
11.10 13.90 -3.09 18 1.051
9.60E-07 cm/sec
Tested By: FRK Date: 3/29/2017
*The certificate shall not be reproduced except in full, without the written approval of MSG.
Reviewed By:MG/KL
Cross-sectional area of burette (cm2) = 0.906 Corrected Coefficient of Permeability (cm/sec)
Cell Pressure
(psi)
Test No. Date t (sec)
Upper Volume Reading
(VU)
3/27/2017
AVERAGE CORRECTED COEFFICIENT OF PERMEABILITY (K):
Pore Pressure Increase (psi)
= b
Head Pressure
(psi)
Skempton's Parameter
(B) = (b/a)
Lower Volume Reading
(VL)
h(t1) h(t2)
Confining Pressure Increase (psi) = a
Back Pressure
(psi)
Water Temp.
T (oC)
Correction factor for viscosity of water at various temperatures
TimeDate
Civil Engineering, Surveying and Environmental Consulting
TOLEDO CANTON LANSING DETROIT MONROE CLEVELAND COLUMBUS
Permeability Test Remolded
ASTM D5084
Before Saturation After Saturation
Fennville Farms Zone 7 Dike Repairs
SB-24 GRAB
Lean Clay
MDMB0010
3/28/2017
0-8'
1 3/27/2017 4,620 9.85E-07
Bias Pressure (cm) = psi x 70.37 cm/psi
1.04E-06
RT
(from table) K (cm/sec)
Kcorrected
(cm/sec)
6,060
17,400
18,780
3/27/2017
3/28/2017
9.08E-07
8.99E-07
8.61E-07
9.54E-07
9.45E-07
9.05E-07 aL PB+h(t1) K= (ln )*RT 2At PB+h(t2)
X
X
VU(t1) - VL(t1) a
RP.SB-25-Bulk.xls
Client's Sample No. Date:
Visual Description: Depth:
Permeant: De-aired tap water 0.01 N CaSO4
Sample Preparation:
Sample was removed from a 3" Shelby tube and trimmed to length in a trimming jig. Any pebbles found on outer surface were removed and resulting voids were filled with material trimmed from the sample.
Material was adjusted to required moisture content and remolded at the required density.
Other: 95% of DD=126.3 @ OMC=9.7%
Soil Properties:
Initial Moisture Content (%)
Initial Wet Density (pcf)
Initial Dry Density
(pcf)
Final Moisture Content
Final Wet Density
(pcf)
Final Dry Density
(pcf)
9.84 131.48 119.71 17.28 140.37 119.69
Formula:
K= h(t1)= a= h(t2)= L= Length of sample (cm) = 7.62 A= Cross-sectional area of RT= sample (cm2) = 41.624846 t= Elapsed time (sec) PB= 140.74
Degree of Saturation:
3/27/2017 7:05am 25.0 22.0 20.0 5.0 5.0 1.0
Permeability Measurement:
23.40 2.30 23.29 18 1.051
10.10 15.60 -6.07 18 1.051
22.10 1.50 22.74 18 1.051
9.50 14.10 -5.08 18 1.051
9.50 14.10 -5.08 18 1.051
1.10 22.60 -23.73 18 1.051
24.70 1.20 25.94 18 1.051
2.90 23.20 -22.41 18 1.051
5.59E-06 cm/sec
Tested By: FRK Date: 3/28/2017
*The certificate shall not be reproduced except in full, without the written approval of MSG.
3/28/2017
5.99E-06
5.24E-06
4.60E-06
6.30E-06
5.51E-06
4.83E-06
RT
(from table) K (cm/sec)
Kcorrected
(cm/sec)
2,580
2,340
6,180
3/27/2017
Silty ,Clayey Sand
MDMB0010
3/28/2017
0-8'
1 3/27/2017 3,000 5.45E-06
Bias Pressure (cm) = psi x 70.37 cm/psi
5.73E-06
Correction factor for viscosity of water at various temperatures
TimeDate
Civil Engineering, Surveying and Environmental Consulting
TOLEDO CANTON LANSING DETROIT MONROE CLEVELAND COLUMBUS
Permeability Test Remolded
ASTM D5084
Before Saturation After Saturation
Fennville Farms Zone 7 Dike Repairs
SB-25 GRAB
AVERAGE CORRECTED COEFFICIENT OF PERMEABILITY (K):
Pore Pressure Increase (psi)
= b
Head Pressure
(psi)
Skempton's Parameter
(B) = (b/a)
Lower Volume Reading
(VL)
h(t1) h(t2)
Confining Pressure Increase (psi) = a
Back Pressure
(psi)
Water Temp.
T (oC)
Reviewed By:MG/KL
Cross-sectional area of burette (cm2) = 0.906 Corrected Coefficient of Permeability (cm/sec)
Cell Pressure
(psi)
Test No. Date t (sec)
Upper Volume Reading
(VU)
3/27/2017 aL PB+h(t1) K= (ln )*RT 2At PB+h(t2)
X
X
VU(t1) - VL(t1) a
RP.SB-27-Bulk.xls
Client's Sample No. Date:
Visual Description: Depth:
Permeant: De-aired tap water 0.01 N CaSO4
Sample Preparation:
Sample was removed from a 3" Shelby tube and trimmed to length in a trimming jig. Any pebbles found on outer surface were removed and resulting voids were filled with material trimmed from the sample.
Material was adjusted to required moisture content and remolded at the required density.
Other: 95% of DD=126.7pcf @ OMC=11.5%
Soil Properties:
Initial Moisture Content (%)
Initial Wet Density (pcf)
Initial Dry Density
(pcf)
Final Moisture Content
Final Wet Density
(pcf)
Final Dry Density
(pcf)
11.35 133.96 120.30 12.90 135.80 120.29
Formula:
K= h(t1)= a= h(t2)= L= Length of sample (cm) = 7.62 A= Cross-sectional area of RT= sample (cm2) = 41.624846 t= Elapsed time (sec) PB= 140.74
Degree of Saturation:
3/27/2017 7:05am 25.0 22.0 20.0 5.0 5.0 1.0
Permeability Measurement:
24.20 0.60 26.05 18 1.051
17.30 7.70 10.60 18 1.051
17.30 7.70 10.60 18 1.051
7.30 17.80 -11.59 18 1.051
7.30 17.80 -11.59 18 1.051
1.30 23.70 -24.72 18 1.051
24.00 0.80 25.61 18 1.051
1.30 23.70 -24.72 18 1.051
8.93E-06 cm/sec
Tested By: FRK Date: 3/29/2017
*The certificate shall not be reproduced except in full, without the written approval of MSG.
Reviewed By:MG/KL
Cross-sectional area of burette (cm2) = 0.906 Corrected Coefficient of Permeability (cm/sec)
Cell Pressure
(psi)
Test No. Date t (sec)
Upper Volume Reading
(VU)
3/28/2017
AVERAGE CORRECTED COEFFICIENT OF PERMEABILITY (K):
Pore Pressure Increase (psi)
= b
Head Pressure
(psi)
Skempton's Parameter
(B) = (b/a)
Lower Volume Reading
(VL)
h(t1) h(t2)
Confining Pressure Increase (psi) = a
Back Pressure
(psi)
Water Temp.
T (oC)
Correction factor for viscosity of water at various temperatures
TimeDate
Civil Engineering, Surveying and Environmental Consulting
TOLEDO CANTON LANSING DETROIT MONROE CLEVELAND COLUMBUS
Permeability Test Remolded
ASTM D5084
Before Saturation After Saturation
Fennville Farms Zone 7 Dike Repairs
SB-27 GRAB
Silty Sand
MDMB0010
3/28/2017
0-8'
1 3/28/2017 960 8.40E-06
Bias Pressure (cm) = psi x 70.37 cm/psi
8.83E-06
RT
(from table) K (cm/sec)
Kcorrected
(cm/sec)
1,560
1,020
3,540
3/28/2017
3/28/2017
8.43E-06
8.72E-06
8.44E-06
8.86E-06
9.16E-06
8.87E-06 aL PB+h(t1) K= (ln )*RT 2At PB+h(t2)
X
X
VU(t1) - VL(t1) a
SUPPLEMENTAL GEOTECHNICAL REPORT
FENNVILLE FARMS ZONE 7 DIKE REPAIRS
ALLEGAN COUNTY, MICHIGAN
MARCH 28, 2017
PREPARED FOR:
MICHIGAN DEPARTMENT OF TECHNOLOGY, MANAGEMENT &
BUDGET – DESIGN & CONSTRUCTION DIVISION
P.O. BOX 30026
LANSING, MICHIGAN 48821
THE MANNIK & SMITH GROUP, INC. ES-1
MDMB0010_Rpt_XZ_GEO dc edits xz edits.docx
EXECUTIVE SUMMARY
The Mannik & Smith Group, Inc. (MSG) was retained by Michigan Department of Technology, Management & Budget to conduct a supplemental geotechnical investigation for a State-owned borrow site that may be potentially utilized for the proposed dike repairs in Fennville Farms Zone 7. Previously, MSG prepared a geotechnical investigation report dated June 1, 2015 that presented soil data collected at the subject dike area and at other potential State-owned borrow sources, and provided some recommendations for the proposed dike repairs. Based on our understanding of the desired restoration results of the subject dike and our most recent and previous field and laboratory testing findings, this report presents revised recommendations for the proposed dike repairs. The following is a brief summary of our investigation findings and recommendations. Please refer to subsequent sections within the report for a detailed discussion of these topics.
• For the results of soil data previously collected at the subject dike and other potential borrow sources, please refer to our Geotechnical Investigation Report dated June 1, 2015.
• Our most recent field investigation included seven test borings, identified as SB-23 through SB-29. All borings were advanced to 10 feet below ground surface (bgs) using the Macro-Core® sampling method.
Some borings were offset and drilled again with hollow stem augering to collect additional samples for laboratory testing.
• At the most recently investigated borrow site, beneath the surficial materials (4 to 11 inches of topsoil), the subsurface soils generally consisted of two soil units. Soil Unit 1 consisted of brown and gray silty clay and was typically encountered directly beneath the surficial materials and extended to a depth ranging from 3 to 9 feet bgs. Soil Unit 1 was not encountered in borings SB-27 and SB-28. An approximate 6 inch sand seam was encountered in borings SB-23 and SB-26 between the topsoil and Soil Unit 1. Soil Unit 2 consisted of brown silty and clayey sand and was typically encountered beneath Soil Unit 1 and extended beyond the investigation depth. Silt seams were observed within Soil Unit 2 in borings SB-24 and SB-27.
• Special precautions should be taken due to the extensive very loose and/or very soft organic soils encountered throughout the subject dike area. Construction equipment may have significant difficulties traversing the site. In order to create a working platform for the proposed construction as well as to help reduce the excessive settlement due to the presence of very loose and/or very soft organics soils, MSG recommends the utilization of a geotextile reinforced aggregate subgrade. A conceptual sketch of the reinforced subgrade is shown in Figure 3 Recommended Typical Dike Cross Section.
• We understand that a mobile pump will be used to control the water levels around the dike. When it is in use, the mobile pump will be towed to the site by a pickup truck and set up at the intersection of the three dike sections (i.e., top, middle and bottom). We recommend the areas where the pump will be parked and used, and the truck turnabout be covered by 8 inches of aggregate base.
• As stated in our previous geotechnical report, without stabilizing the existing subgrade, the immediate settlement under the load of the proposed dike is anticipated to be 1 to 3 inches and a primary consolidation settlement of 2.5 to 4 feet. Depending on the thickness of the organic soils at the location, the primary consolidation is expected to occur over a period of 3 to 15 years. If our recommendations stated in Section
5.1 regarding subgrade preparation are properly implemented, we anticipate the post construction primary consolidation settlement can be reduced to 3 to 5 inches, which will significantly prolong the service life of the dike. However the organic soils (i.e., peat) are susceptible to secondary creep settlement, which is anticipated to settle at a rate of 0.2 to 0.6 inches per year after the end of the primary consolidation. Due to the variation in the thickness of the peat layer, differential settlement is expected to be significant.
This Executive Summary articulates selective findings and recommendations and is provided solely for the purposes of overview and should not be counted upon to provide details in its entirety for the design and construction.
THE MANNIK & SMITH GROUP, INC. i
TABLE OF CONTENTS
SECTION: PAGE NO.:
EXECUTIVE SUMMARY ......................................................................................................................................... ES-1
1.0 INTRODUCTION
2.0 PROJECT & SITE DESCRIPTION
3.0 INVESTIGATION METHODS
3.1 Field Investigation
3.2 Laboratory Testing Methods
4.0 INVESTIGATION FINDINGS
4.1 Subsurface Conditions
4.2 Groundwater
5.0 ANALYSES AND RECOMMENDATIONS
5.1 Site Preparation
5.2 Engineered Fill
5.3 Excavation and Slope
5.4 Groundwater
5.5 Dike Restoration Recommendations
6.0 CLOSURE
FIGURES
FIGURE 1 SITE LOCATION MAP
FIGURE 2 BORING LOCATION PLAN
FIGURE 3 RECOMMENDED TYPICAL DIKE CROSS SECTION
APPENDICES
APPENDIX A BORING LOGS
APPENDIX B LABORATORY TEST DATA
THE MANNIK & SMITH GROUP, INC. 1
1.0 INTRODUCTION
The Mannik & Smith Group, Inc., (MSG) was retained by Michigan Department of Technology, Management & Budget to conduct a supplemental geotechnical investigation for a borrow site that may be potentially utilized for the proposed dike repairs in Fennville Farms Zone 7. The approximate location of the subject borrow source is depicted in Figure 1 Site Location Map. Previously, MSG prepared a Geotechnical Investigation Report dated June 1, 2015 that presented soil data collected at the subject dike and other potential borrow sources, and provided some recommendations for the proposed dike repairs. Based on our understanding of the desired restoration results of the subject dike and our most recent and previous field and laboratory testing findings, this report presents revised recommendations for the proposed dike repairs. The recommendations presented in this report supersede the recommendations in our previous Geotechnical Investigation Report dated June 1, 2015 for the subject site. Our work was performed in general accordance with our ISID Discretionary Proposal dated January 27, 2017.
2.0 PROJECT & SITE DESCRIPTION
Based on the drawings prepared by Ducks Unlimited last revised on January 6, 2014, the subject dike is about 4,280 feet long and consists of a top section, a middle section and a bottom section. The current elevations along the center line of the subject dike are approximately 622 feet for the top and middle sections and 621 feet for the bottom section. The proposed repairs will bring the top of dike elevations to 624.5 feet for the top and middle sections and
623.5 feet for the bottom section, which will fulfill the full service water levels of 623 and 622 feet for top/middle and bottom sections, respectively.
As stated in our previous geotechnical report, the subsurface conditions at the subject dike is characterized by very loose and/or very soft organic soils extending to as deep as 25 feet below ground surface (bgs). Special ground improvements will be required to prepare a suitable subgrade to restore the dike and prolong its service life. In addition, it is our opinion that clayey materials with lower permeability will provide a better long term performance to the subject dike. The purpose of our most recent field and laboratory testing was to evaluate a nearby State-owned borrow source to determine if the soils are suitable clayey fills for the proposed repairs.
3.0 INVESTIGATION METHODS
MSG’s investigation consisted of field investigation and laboratory testing methods with are presented below. This section presents the investigation methods used at the potential borrow source for clayey materials. Please refer to our Geotechnical Investigation Report dated June 1, 2015 for the investigation methods used at the subject dike and other potential borrow sources.
3.1 Field Investigation
Our most recent field investigation for this project consisted of the installation of seven (7) soil borings performed on February 28, 2017. The borings were identified as SB-23 through SB-29. All borings were advanced using the Macro-Core® sampling method and extended to a depth of 10 feet bgs. The boring locations and elevations were determined in the field by a MSG project engineer using a hand-held GPS device. Therefore, the boring locations and elevations mentioned in this report should be considered approximate. The boring locations are shown on the attached Figure 2 Boring Location Plan.
The site was drilled using a Geoprobe 7822DT drill rig. The test borings were continuously profiled from ground surface to the terminus of the borehole using a 5-foot long, closed-piston Macro-Core® sampling device. A dedicated clear polyvinyl chloride (PVC) liner was placed within the sampler between each sample interval. In order to collect additional samples for laboratory testing, some borings were offset and drilled again by hollow stem augering.
The borings were backfilled with soil cuttings upon the completion of drilling. Soil samples were sealed in glass jars and buckets and delivered to MSG’s geotechnical laboratory for further examination and the
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assignment of laboratory testing on selected samples. The results of the field investigation have been summarized on the boring logs in Appendix A.
3.2 Laboratory Testing Methods
Each of the soil samples recovered from the borings was examined and visually classified by a geotechnical professional in the laboratory. This examination was performed to verify conditions identified within the field boring logs, perform visual-manual classification of samples not subjected to further laboratory testing and select samples for laboratory testing. Based on the review of the field boring logs and visual examination of the collected samples, MSG completed laboratory testing on selected samples. The laboratory analysis consisted of:
• Six (6) moisture content tests performed in accordance with ASTM D2216;
• Four (3) sieve analysis and hydrometer tests performed in accordance with ASTM D422;
• Four (4) Atterberg limits tests performed in accordance with ASTM D4318;
• Ten (10) organic content tests performed in accordance with ASTM D2974;
• Six (6) soil density determinations performed in accordance with ASTM D7263; and
• Five (5) modified proctor compaction tests performed in accordance with ASTM D1557.
The laboratory test results are presented in Appendix B Laboratory Test Data. The offset borings augered to collected additional samples were termed SB-XX GRAB. In order to evaluate different material types that could be collected from the borrow source, a mixed sample with about 30 percent clay (Soil Unit 1) and 70 percent sand (Soil Unit 2) was tested for compaction and permeability parameters.
For additional laboratory test data on soil samples collected at the subject dike and other potential borrow sources, please refer to our Geotechnical Investigation Report dated June 1, 2015. Laboratory permeability testing was not completed at the time this report was prepared. The permeability results will be issued as an addendum to this report when the tests are completed.
4.0 INVESTIGATION FINDINGS
The following paragraphs describe the subsurface conditions in terms of major soil strata for the purposes of geotechnical investigation. The soil boundaries indicated are inferred from non-continuous sampling and observations of the drilling operations and/or sampling resistance. The subsurface conditions discussed in the following paragraphs and those shown on the boring logs represent an evaluation of the subsurface conditions based on interpretation of the field and laboratory data using normally accepted geotechnical engineering judgement and common engineering practice standards. The subsurface conditions described herein may vary beyond the boring locations and at different times of the year.
Please note that this section presents the investigation findings at the potential borrow source for clayey materials.
Please refer to our Geotechnical Investigation Report dated June 1, 2015 for the investigation findings at the subject dike and other potential borrow sources.
4.1 Subsurface Conditions
Approximately 4 to 11 inches of topsoil was encountered in all borings across the subject borrow field. A generalized profile of the subsurface conditions encountered beginning below the surficial materials and extending downward is as follows:
Soil Unit 1: Brown and Gray Silty Clay Soil Unit 1 consisted of brown and gray silty clay (USCS Classification: CL) and was encountered beneath topsoil and/or a thin sand seam in all borings except SB-27 and SB-28, extending to a depth ranging from 3
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to 9 feet bgs. It appears that the layer of Soil Unit 1 was thicker at the northern portion of the subject borrow site and became thinner toward the southern portion.
Sol Unit 2: Brown Silty and Clayey Sand Soil Unit 2 consisted of silty and clayey sand (SC-SM) and was encountered beneath Soil Unit 1 or topsoil in all borings, extending below the investigation depth. Silt seams were observed within Soil Unit 2 in borings SB-24 and SB-27.
4.2 Groundwater
As the borings were advanced, the drill crew checked the drilling rods and sampling equipment for indications of groundwater or seepage. The boreholes were checked again for groundwater immediately after completion of drilling. Groundwater was encountered in all borings at a depth ranging from 5 to 8 feet bgs. Water levels reported are accurate only for the time and date that the borings were drilled. Long term monitoring of the boreholes was not included as part of our subsurface investigation. The borings were backfilled and sealed the same day that they were completed.
5.0 ANALYSES AND RECOMMENDATIONS
The following evaluations and conclusions are based on interpretations of field and laboratory data obtained during the supplemental geotechnical investigation and MSG’s experience with similar subsurface conditions. Where comments are made with regard to construction or the proposed development, they are provided in order to highlight aspects of construction that could potentially affect the design of the project. Contractors bidding on or undertaking the work should make their own interpretations of the factual results of the investigation as it affects their construction methods, equipment capabilities, costs, schedule, sequencing and the like. This report reflects only the geotechnical aspects of the subsurface conditions at the site. Review and evaluation of environmental aspects of subsurface conditions is beyond the scope of this report.
Based on our understanding of the desired restoration results of the subject dike and our most recent and previous field and laboratory testing findings, this report presents revised recommendations for the proposed dike repairs. The recommendations presented in this report supersede the recommendations in our previous Geotechnical Investigation Report dated June 1, 2015 for the subject site.
During construction, a qualified geotechnical consultant should be retained to monitor subsurface conditions, subgrade preparation and dike restoration to verify that suitable materials are in place.
5.1 Site Preparation
Before proceeding with construction, topsoil, vegetation and other deleterious materials should be stripped from the proposed construction areas. Generally, areas exposed by stripping operations on which subgrade preparations are to be performed should be compacted in place as outlined in Section 5.2.
Special precautions should be taken due to the extensive very loose and/or very soft organic soils encountered throughout the dike area. Construction equipment may have significant difficulties traversing the site. In order to create a working platform for the proposed construction as well as to help reduce the excessive settlement due to the presence of very loose and/or very soft organics soils, MSG recommends the utilization of a geotextile reinforced aggregate subgrade. A conceptual sketch of the reinforced subgrade is shown in Figure 3 Recommended Typical Dike Cross Section. The following procedures should be followed to prepare a suitable subgrade to support the subject dike and prolong its service life:
• Undercut the entire dike, where repairs are required, to an approximate elevation of 620 feet for the top and middle sections and 619 feet for the bottom section. The undercutting should extend a minimum of 4 feet outside the base of the proposed dike in both directions.
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• Place a layer of geotextile (Mirafi RS580i or engineer approved equivalent) on the exposed surface.
• The undercutting should then be backfilled using coarse crushed granular material in accordance with Section 5.2 of this report. The top of the prepared subgrade should have an approximate elevation of 622 feet for the top and middle sections and 621 feet for the bottom section.
• Consideration must be provided to place a layer of clay or other impervious material over the granular backfill to prevent loss of impounded water due to flow through the backfill material.
The reinforced subgrade has been designed using the method proposed by Giround and Han (2004), with the following input parameters and assumptions:
Table 5.1.1
DESIGN INPUT FOR REINFORCED SUBGRADE
Wheel Load (lb) 9,000
Tire Contact Pressure (psi) 80
Number of Passes of Axle 50,000
Allowable Rut Depth (in) 3
California Bearing Ratio for Subgrade Soil - Peat 0.5
California Bearing Ratio for Aggregate Backfill 20
It is also recommended that the prepared subgrade be proof rolled to detect any unstable zones. Proof rolling should be accomplished by making a minimum of two complete passes in each of two perpendicular directions, with a fully-loaded tandem-axle dump truck, or other approved pneumatic-tired vehicle with a minimum weight of 20 tons. If proof rolling reveals the presence of unstable material within the subgrade, additional remedial measures may be required to stabilize the subgrade. The actual undercut depths and additional subgrade remediation methods (if required) should be determined by a geotechnical engineer or his/her designated representative.
5.2 Engineered Fill
All soils to be used as engineered fill should be free of organics, debris, frozen soils or any other deleterious materials. All fine-grained soils should be checked for plasticity index and liquid limit before placement. Fine-grained fill materials should have a liquid limit less than 40 percent and plasticity index less than 20 percent (i.e., non-expansive). In general, the on-site soils are highly organic and should not be used as engineered fill. Based on soil conditions encountered in the borings performed along the subject dike, some of the undercut materials that have an organic content less than 3 percent may be suitable for reuse as engineered fill. Additional field observation and laboratory testing by a qualified geotechnical consultant may be required during construction to verify the suitability.
All engineered fill should be compacted to 95 percent of modified Proctor maximum dry density and at ±2 percent of optimum moisture content. Fill materials should be placed in horizontal lifts and adequately keyed into stripped and scarified subgrade soils and/or adjacent fill. Proper drainage should be maintained during and after fill placement to prevent water from impacting compaction efforts or long-term fill integrity. A qualified geotechnical consultant should be retained to monitor fill placement in order to assure compaction requirements are achieved. Soil density testing should be performed during fill placement activities to assure proper fill compaction. A commonly used testing criterion is one test at least every lift and at least every 200
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feet along the dike. Areas that do not achieve compaction requirements after initial placement should be re-compacted to meet project requirements.
The actual thickness suitable for placement is dependent upon the soil type, compaction equipment, and the compaction specification. In general, fill should be placed in 9-inch loose thickness lifts, assuming appropriately weighted and ballasted compaction equipment is utilized. Sand fills should be compacted using smooth vibratory rollers. Clay fills should be compacted using sheep foot compactor. The geotechnical engineer should be allowed to review the equipment utilized for compaction to confirm suitability relative to the specified loose lift thickness. If necessary, the geotechnical engineer will recommend a revised lift thickness suitable to the equipment performing compaction.
Coarse crushed granular material is recommended as fill for replacement of undercut areas. The coarse crushed granular material may consist of natural or recycled aggregate materials meeting the gradation specification of MDOT Item 21AA, or engineer approved equivalent. Typical lift thickness utilized for this material is 8 inches.
5.3 Excavation and Slope
Familiarity with applicable local state and federal safety regulations, including current Occupational Safety and Hazards Administration (OSHA) excavation and trench safety is vital. Therefore it should be a requisite for both the owner and contractor, with the contractor by and large being responsible for the safety of the site. Slope height, slope inclination, and excavation depth (including utility trench excavations) should in no case exceed those specified in local, state, or federal safety (OSHA Health and Safety Standards for Excavations, 29 CFR Part 1926 Subpart P) regulations. Such regulations are strictly enforced and, if not followed, the Owner, contractor, or earthwork or utility subcontractors could be liable for substantial penalties. Maximum allowable slopes for excavations less than 20 feet based on soil type and angle to horizontal are reflected in Table 5.3.1.
Table 5.3.1
OSHA ALLOWABLE SLOPES
Soil Type H:V Slope Angle Stable Rock Vertical 90°
Type A ¾:1 53° Type B 1:1 45° Type C 1½:1 34°
Type A (Short-term)* ½:1 63° *: For a maximum excavation depth of 12 feet.
The overburden soils encountered at the subject dike primarily consisted of very loose and/or very soft organic soils. Based upon the data obtained, it is anticipated that OSHA will classify the on-site soils as Type C. Flatter slopes will be required if seepage conditions occur during construction.
Considering the maximum height of the proposed dike of about 4.5 feet, it is not anticipated that the design of the dike will be controlled by the global stability. Based on our review of the drawings prepared by Ducks Unlimited, it is our opinion that the side slopes of the dike can be graded no steeper than 3(H):1(V).
5.4 Groundwater
Groundwater was encountered in all borings advanced at the potential clay borrow site, where the groundwater had a depth ranging from 5 to 8 feet bgs. As stated in our previous geotechnical report, shallow
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groundwater was also observed at most of the boring locations in the dike area. Groundwater is likely to be encountered during construction. However, fluctuations in the water level could occur due to seasonal variations in rainfall. The amount and type of dewatering required during construction will depend on the weather, groundwater levels at the time of construction, and the effectiveness of the contractor’s techniques in preventing surface water runoff from entering open excavations and lowering the groundwater table.
5.5 Dike Restoration Recommendations
We understand that a mobile pump will be used to assist in controlling the water levels around the dike.
When it is in use, the mobile pump will be towed to the site by a pickup truck and set up at the intersection of the three dike sections (i.e., top, middle and bottom). We recommend the areas where the pump will be parked and used, and the truck turnabout be covered by 8 inches of aggregate base. The placement and compaction of the aggregate base should be in accordance with Section 5.2 of this report. We also recommend the aggregate base be evaluated by proof rolling in accordance with Section 5.1 of this report.
This pump working area has been designed as an unpaved road using the method proposed by Giround and Han (2004), with the following input parameters and assumptions:
Table 5.5.1
DESIGN INPUT FOR PUMP WORKING AREA
Wheel Load (lb) 3,500
Tire Contact Pressure (psi) 80
Number of Passes of Axle 10,000
Allowable Rut Depth (in) 3
California Bearing Ratio for Subgrade Soil – Stiff Clay 3
California Bearing Ratio for Aggregate Base 20
In order to improve the long term performance of the dike, we recommend using fine grained materials to construct the entire dike. However, considering both the desired performance and the cost, the dike can be built using fine grained materials at least to the elevation of the full service water level, which is 623 and 622 feet for top/middle and bottom sections, respectively. On-site suitable materials or sand fill can then be used to build the dike to its planned elevations. A recommended typical dike cross section is shown in Figure 3. A detailed discussion about the differences between using clay and sand fills will be provided in an addendum to this report when the laboratory permeability testing is completed.
It will require approximately 3,800 cubic yards of clay (in compacted condition) to construct the dike to the full service water level and additional 3,925 cubic yards of sand and/or clay (in compacted condition) to achieve the finished elevation of the dike. Based on the most recent investigation findings in the upper 10 feet of the clay borrow source and an approximate borrow site area of 400,000 square feet, it is anticipated that there is about 44,000 cubic yards of clay (in bank condition). Therefore, we anticipate there is enough clay material that can be borrowed for the proposed construction.
It is MSG’s opinion that reducing long term settlement is the key to prolong the service life of the subject dike. Based on available previous restoration drawings (prepared by Merritt Engineer last revised on November 4, 1998) for the subject dike, the last restoration of the dike was conducted in 1998 and the restored dike should have a top elevation of about 625 feet. The top elevations of the dike at the time of our investigation were about 621 to 622 feet. Assuming the dike was restored in accordance with the drawings, the dike has been settling on an average rate of 2 to 3 inches per year.
THE MANNIK & SMITH GROUP, INC. 7
As stated in our previous geotechnical report, without stabilizing the existing subgrade, the immediate settlement under the load of the proposed dike is anticipated to be 1 to 3 inches and a primary consolidation settlement of 2.5 to 4 feet. Depending on the thickness of the organic soils at the location, the primary consolidation is expected to occur over a period of 3 to 15 years. If our recommendations stated in Section
5.1 regarding subgrade preparation are properly implemented, we anticipate the post construction primary consolidation settlement can be reduced to 3 to 5 inches, which will significantly prolong the service life of the dike. However the organic soils (i.e., peat) are susceptible to secondary creep settlement, which is anticipated to settle at a rate of 0.2 to 0.6 inches per year after the end of the primary consolidation. Due to the variation in the thickness of the peat layer; differential settlement is expected to be significant.
Considering that continuous settlement is anticipated to occur, MSG recommends long term monitoring of the elevation of the top of the dike to decide the time of required maintenance. Additional fill may be needed at various locations along the dike to maintain the required top of dike elevation which will be a significant maintenance cost throughout the service life of the system.
6.0 CLOSURE
The analyses and recommendations in this report are based on our interpretation of the field and laboratory data obtained during the geotechnical investigation, our understanding of the project and our experience with similar sites and subsurface conditions. Data used during this investigation included:
• Seven (7) exploratory borings performed during this study;
• Twenty (20) exploratory borings performed during our previous study;
• Observations of the project site by MSG staff;
• Results of laboratory testing completed to date; and,
• Published and historic soil and geologic data for the project area.
The subsurface conditions discussed in this report and those shown on the boring logs represent an estimate of the subsurface conditions based on interpretation of the boring data using normally accepted geotechnical engineering judgments. Although individual test borings are representative of the subsurface conditions at the boring locations on the dates shown, they are not necessarily indicative of subsurface conditions at other locations or at other times.
MSG is not responsible for independent conclusions, opinions, or recommendations made by others based upon information presented in this report.
The project plans and specifications should be reviewed by the geotechnical engineer to confirm that the geotechnical aspects are generally consistent with the recommendations of this report. In addition, site subgrade preparation and engineered fill compaction activities should be monitored by the geotechnical engineer.
FIGURE 1 – SITE LOCATION MAP
FIGURE 2 – BORING LOCATION PLAN
FIGURE 3 – RECOMMENDED TYPICAL DIKE CROSS SECTION
Tel: (517) 316-9232 Fax: (517) 316-9233 www.MannikSmithGroup.com
Figure 1: Site Location Map Fennville Farms Zone 7 Dike Repairs
Allegan County, Michigan
Notes:
Tel: (517) 316-9232 Fax: (517) 316-9233 www.MannikSmithGroup.com
Figure 2: Boring Location Plan Fennville Farms Zone 7 Dike Repairs
Allegan County, Michigan
Notes:
APPENDIX A
BORING LOGS
2193 Association Drive, Suite 200, Okemos, MI 48864 Tel: 517.316.9232 Fax: 517.316.9233 www.MannikSmithGroup.com
EXHIBIT A
GENERAL SOIL SAMPLE NOTES
Unless noted, all terms utilized herein refer to the Standard Definitions presented in ASTM D653.
Standard Penetration Test (ASTM D1586): A 2.0-inch outside-diameter (O.D.), 1-3/8-inch inside-diameter (I.D.) split barrel sampler is driven into undisturbed soil by means of a 140-pound weight falling freely through a vertical distance of 30 inches. The sampler is normally driven three successive 6-inch increments. The total number of blows required for the final 12 inches of penetration is the Standard Penetration Resistance (N).
COHESIVE SOILS COHESIONLESS SOILS
Consistency Approximate Range of N
Unconfined Compressive Strength (psf)
Density Classification
Approximate Range of N
Very Soft 0 – 1 Below 500 Very Loose 0 – 4 Soft 2 – 4 500 – 1,000 Loose 5 – 10 Medium Stiff 5 – 8 1,000 – 2,000 Medium Dense 11 – 30 Stiff 9 – 15 2,000 – 4,000 Dense 31 – 50 Very Stiff 16 – 30 4,000 – 8,000 Very Dense Over 50 Hard 31 – 50 8,000 – 16,000 Very Hard Over 50 Over 16,000
CLASSIFICATION PARTICLE SIZES
The major soil constituent is the principal noun, i.e.
sand, silt, gravel. The second major soil constituent and other minor constituents are reported as follows:
Boulders - Greater than 12 inches (305 mm) Cobbles - 3 inches (76.2 mm) to 12 inches (305 mm)
Second Major Constituent Minor Constituents Gravel: Coarse - ¾ inches (19.05 mm) to 3 inches (76.2 mm) (percent by weight) (percent by weight) Fine - No.4 (4.75 mm) to ¾ inches (19.05 mm)
Sand: Coarse - No. 10 (2.00 mm) to No. 4 (4.75 mm) Trace – 1% to 11% Trace – 1% to 11% Medium - No. 40 (0.425 mm) to No. 10 (2.00 mm) Fine - No. 200 (0.074 mm) to No. 40 (0.425 mm) Adjective – 12% to 35% Little – 12% to 22% Silt - 0.005 mm to 0.074 mm (clayey, silty, etc.) Clay - Less than 0.005 mm Some – 23% to 33% And – Over 35%
If clay content is sufficient so that clay dominates soil properties, clay becomes the principal noun with the other major soil constituent as modifier: i.e., silty clay. Other minor soil constituents may be included in accordance with the classification breakdown for cohesionless soils: i.e., silty clay, trace sand, little gravel.
If sand particle size is greater than 11% by weight of the total sample weight, the adjective (i.e., fine, medium or coarse) is added to the soil description for the sand portion of the sample, provided sand is the major or second major constituent.
SAMPLE DESIGNATIONS
AS Auger Sample - directly from auger flight ST Shelby Tube Sample - 3-inch diameter unless otherwise noted
BS Miscellaneous Samples - Bottle or Bag PS Piston Sample - 3-inch diameter unless otherwise noted
MC Macro-Core Sample - 2.25-inch O.D., 1.75-inch I.D., 5 feet long polyethylene liner RC Rock Core - NX core unless otherwise noted
LB Large-Bore (Micro-Core) Sample - 1-inch diameter, 2 feet long polyethylene liner CS CME Continuous Sample - 5 feet long, 3-inch diameter unless otherwise noted SS Split Spoon Sample - 1-inch or 2-inch O.D. HA Hand Auger
LS Split Spoon (SS) Sampler with 3 feet long liner insert DP Drive Point
NR No Recovery CM Coring Machine
The Mannik & Smith Group, Inc.
2193 Association Drive, Suite 200, Okemos, MI 48864 ph: (517) 316-9232 fax: (517) 316-9233 www.manniksmithgroup.com
POORLY-GRADED SANDS WITH OR WITHOUT
GRAVEL
TYPICAL NAMES
INORGANIC CLAYS OF HIGH PLASTICITY WITH
OR WITHOUT SAND OR GRAVEL
ORGANIC SILTS OR CLAYS OF HIGH
PLASTICITY WITH OR WITHOUT SAND OR
GRAVEL
PEAT AND OTHER HIGHLY ORGANIC SOILS
GRAVELS
MORE THAN HALF
COARSE FRACTION
IS LARGER THAN
NO. 4 SIEVE
GW
GP
GM
GC
SW
SP
SM
SC
ML
CL
OL
MH
CH
OH
PT
SYMBOLS KEY
SAMPLE TYPES
Shaly Dolomite
Poorly Graded Gravelly Sand
Sandy Silt
Clayey Sand
Poorly Graded Sand with Clay
Topsoil
Shale
MAJOR DIVISIONS
SANDS
MORE THAN HALF
COARSE FRACTION
IS FINER THAN NO.
4 SIEVE SIZE
CLEAN GRAVELS
WITH LESS THAN
15% FINES
GRAVELS WITH
15% OR MORE
FINES
CLEAN SANDS
WITH LESS THAN
15% FINES
WELL-GRADED SANDS WITH OR WITHOUT
GRAVEL
INORGANIC SILTS OF HIGH PLASTICITY WITH
OR WITHOUT SAND OR GRAVEL
WELL-GRADED GRAVELS WITH OR WITHOUT
SAND
Bentonite Pellets
First Encountered Groundwater
Screened Casing
Static Groundwater
BORING / WELL LOG KEY
Blank Casing
Filter Pack
Portland Cement
Well Graded Gravel with Clay
HIGHLY ORGANIC SOILS
SILTY SANDS WITH OR WITHOUT GRAVEL
WELL SYMBOLS
CLAYEY SANDS WITH OR WITHOUT GRAVEL
INORGANIC SILTS OF LOW TO MEDIUM
PLASTICITY WITH OR WITHOUT SAND OR
GRAVEL
INORGANIC CLAYS OF LOW TO MEDIUM
PLASTICITY WITH OR WITHOUT SAND OR
GRAVEL
ORGANIC SILTS OR CLAYS OF LOW TO
MEDIUM PLASTICITY WITH OR WITHOUT SAND
OR GRAVEL
CLAYEY GRAVELS WITH OR WITHOUT SAND
SILTS AND CLAYS
LIQUID LIMIT 50% OR LESS
SILTS AND CLAYS
LIQUID LIMIT GREATER THAN 50%
POORLY-GRADED GRAVELS WITH OR
WITHOUT SAND
SILTY GRAVELS WITH OR WITHOUT SAND
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Grab Sample
Macro-core Sample
Gravelly Silt
Well Graded Gravel with Silt
Well Graded Gravelly Sand
Limestone
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TOPSOIL: 11 inches
Brown clayey and silty SAND, moist
(SC-SM)
Brown and gray silty CLAY, some…
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