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2018-10-12_REVISION - C1982056 (2)
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2018-10-12_REVISION - C1982056 (2)
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Last modified
11/7/2018 7:11:26 AM
Creation date
11/7/2018 7:03:09 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Revision
Doc Date
10/12/2018
Doc Name
Correspondence
From
Twentymile Coal, LLC
To
DRMS
Type & Sequence
TR84
Email Name
TNL
Media Type
D
Archive
No
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Observations from the test pit excavations included the following: <br />• A thin layer of organic rich topsoil was noted at each test pit location, typically to depths of 6 inches <br />to one foot. <br />• Subsurface materials graded from residual clay soils through an intermediate material to a <br />weathered shale over several vertical feet in each excavation, with the bottom of the excavation <br />typically in the weathered shale unit. Material descriptions were made using the Unified Soil <br />Classification System (USCS) and International Society of Rock Mechanics (ISRM) accepted <br />descriptors for soil and rock materials, respectively. <br />• Residual medium (lean) to high (fat) plasticity clay was observed to depths of 4 to 8 feet in all <br />test pits except TP16-3. <br />• Lean clay was observed to a depth of 3 feet in TP16-3, which was excavated on the South <br />slope of the valley. <br />• The intermediate material, between clay and shale was observed in each excavation and ranged <br />from less than 1 to 4 feet thick. <br />• The material was a highly to completely weathered rock, with the geological fabric of the <br />underlying shale that could be broken apart to a mixed medium of clay and gravel sized <br />shale fragments. <br />• A layer with a notably lighter color (likely alkali precipitate) was observed in TP16-3 from a <br />depth of 3 to 4 feet. This layer had the texture of the intermediate material, but was <br />underlain by a stiff lean clay. <br />• The shale that was excavated was moderately to highly weathered and extremely to very weak <br />rock, which could be easily crumbled to gravel sized shale fragments without additional tools. <br />• Bulk samples were collected from the residual soil layer of each excavation. Grab samples were <br />collected of the three material types observed in each excavation and where any notably different <br />soil conditions were observed (e.g. the alkali layer in TP16-3). Note, no testing was performed on <br />grab samples. <br />• Water seepage was observed in 4 of the 6 excavations. The water table typically occurred at the top <br />of or up to a foot above the top of the shale layer. <br />Table 3-1: Geotechnical Laboratory Soil Testing Results <br />Atterberg <br />Test Sample Date Moisture LimitsPercent AASHTO Soil Type <br />LL PI <br />Pit Ip Type Retrieved % pH Passing #200 Class. (USCS) <br />TP16-1 Bulk 04/14/16 21.4 48 26 <br />TP16-2 <br />Bulk <br />04/14/16 <br />24.0 <br />53 <br />TP16-3 <br />Bulk <br />04/14/16 <br />25.9 <br />49 <br />84.9 A-7-6 (23) Lean Clay <br />(CL) <br />32 8.06 94.1 A-7-6(33) F (CHI) y <br />30 97.3 A-76(32) Lean Clay <br />(CL) <br />TP16-5 Bulk 04/14/16 24.2 45 27 7.87 95.8 A.7-6 (27) Lean Clay <br />(CL) <br />TP16-6 Bulk 04/14/16 22-1 46 28 97.8 A-7-6 (291 Lean Clay <br />(CL) <br />TP16-7 Bulk 04/14/16 26-1 53 33 99.5 A-7-6 (37) Fat Clay <br />(CH) <br />PEABODY FINAL OESIGN TM 20181010 3-2 <br />COPYRIGHT 2012 BY CH2M HILL INC • COMPANY CONFIDENTIAL <br />
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