My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2006-03-17_REVISION - M1982015
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1982015
>
2006-03-17_REVISION - M1982015
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/15/2021 2:56:06 PM
Creation date
11/21/2007 9:41:26 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1982015
IBM Index Class Name
Revision
Doc Date
3/17/2006
Doc Name
112 Permit Application
From
Siegrist Construction Co.
To
DMG
Type & Sequence
AM1
Media Type
D
Archive
No
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
273
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Supplemental Geotechnical Engineering Report <br />Proposed Slurry Cut-off Walls @ St. Vrain Development <br />Weld County, Colorado <br />Terracon Project No. 25045300 <br />Terracon <br />were also encountered, predominantly on the eastern portion of the site. Claystone and/or <br />sandstone bedrock were encountered beneath the native soils in the majority of the borings <br />at depths ranging from about 7 to 30 feet below existing site grade and extended to the full <br />depth of exploration. Bedrock was not encountered to the full depth of exploration in Boring <br />Nos.1 and 8. Auger refusal was encountered in these borings at depths ranging from about <br />5 to 18 feet below existing site grade and appears to be in gravel and/or cobble sized <br />materials. in addition, auger refusal was encountered in very hard and strongly cemented <br />sandstone bedrock materials at depths ranging from about 13 to 20 feet below existing site <br />grade in Boring Nos. 45, 47 and 48. <br />Field and Laboratory Test Results: The predominant sand materials overlying the bedrock <br />generally classify as silty sand (SM) per the Unified Soil Classification System (USCS) and <br />have varying amounts of clay, silt, and gravel. The amount of fines (predominantly silt) <br />within the overburden materials encountered in the packer testing locations varied from <br />about 24 to 28 percent. Laboratory test results are included in Appendix B. Field test results <br />from the current and previous studies indicate that the claystone bedrock materials vary <br />from medium hard to very hard in hardness. The claystone bedrock materials appear to be <br />generally intact to moderately fractured in terms structure. The sandstone bedrock materials <br />within the western portion of the site are very hard in hardness and strongly cemented but <br />have a higher degree of fractures within the upper approximate 5 to 10 feet. Auger refusal <br />on the sandstone bedrock was generally encountered ih these areas. Results of the packer <br />permeability testing are as follows: <br />Table No. 1 <br /> Depth of Test Bedrock Total Head RQD Average (%) Permeability <br />Location <br /> Interval(ft) Description (ft) (in/sec) <br />Packer 1 7' 2" to 12' 2" a w/ <br />San 38.75 82 7.24 x 10'5 <br /> Clay <br />Packer 1 12' 5" to 17' 3" San C <br />ay e.wl 43.6 55 8.5 x 10~ <br /> l <br />Packer 2 27' %" to 32' Sandy 69.3 86 'Less than 10"' <br /> Claystone <br />Packer 3 11' 10" to 16' 7" l 33.7 80 9.8 x 10"~ <br /> dstone <br />San <br />Packer 4 27' to 32' Claystone 92.4 86 'Less than 10- <br />'accepteq no water under the specitieq neap pressure <br />Groundwater Conditions: Groundwater was encountered in the majority of the borings at <br />depths ranging from about 3 to 19 feet below existing site grade at the time of field <br />exploration from the previous study. When checked a minimum of one day after drilling, <br />groundwater was measured at depths of about Z fo 25 feet below existing site grade in <br />some of the borings. However, some of the borings caved-in under wet conditions at depths <br />5 <br />
The URL can be used to link to this page
Your browser does not support the video tag.