My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2009-11-30_REVISION - M2000156 (7)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M2000156
>
2009-11-30_REVISION - M2000156 (7)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/15/2021 2:20:38 PM
Creation date
12/2/2009 11:57:09 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2000156
IBM Index Class Name
REVISION
Doc Date
11/30/2009
Doc Name
Submittal
From
Coulson Excavating Co., Inc.
To
DRMS
Type & Sequence
AM1
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
51
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
6.4.5 Exhibit E — Reclamation Plan <br />6) Following backfilling Phase 2 Cell 3, begin constructing the clay liner for <br />the main lake by ripping weathered shale from pit floor and placing on the <br />slopes and compacting. <br />7) Replace topsoil as shown in Exhibit F — Reclamation Plan (40,333 cy). <br />8) Disk, seed and fertilize areas as shown in Exhibit F — Reclamation Plan. <br />Pond Liner Design and Specification <br />The purpose of this section is to provide design specifications for the pond liner. <br />The objective is to design a post- mining, compacted clay liner that will prevent <br />groundwater leakage into the pond, at a rate greater than or equal to 0.03 feet / <br />day / feee. <br />The borrow source for the compacted clay liner will be the weathered zone of <br />Pierre shale occurring an average of 17 feet below ground surface. Texturally <br />and mineralogically continuous in a lateral direction, the Pierre shale is flat lying <br />in this area (Porter, 1976). The weathered zone is a friable silty clay consisting of <br />illites and small amounts of smectites (Gill et al, 1996). <br />Approximately 69,000 cy of weathered Pierre shale will be required to construct <br />the clay liner for the 55 acre lake and 11,500 cy with be required for the 2 acre <br />lake. <br />Source Material Sampling /Laboratory Analysis <br />A 5- gallon sample of weathered Pierre shale was collected from a gravel <br />operation to the west. <br />Collected from the upper 3 to 4 feet of the weathered horizon, the shale <br />appeared very consistent with respect to color and texture with that of the <br />weathered shale within the proposed excavation area. Moreover, personal <br />communication with local excavators and drillers confirm the consistency of the <br />Pierre shale throughout eastern Loveland. This consistency is most likely due to <br />the flat lying nature of the shale in this region. <br />If the source material shows any variability with respect to color, texture, or <br />content from the sampled material, a full suite of geotechnical tests will be <br />performed. <br />Field data recorded during sample collection included: <br />Color— dark gray <br />Texture — Very fine- grained clay and silt with larger clumps that are friable with <br />moderate pressure between fingertips <br />Plasticity — Low <br />Moisture — Moist <br />The field sample was delivered to Aguirre Geotechnical Engineers of Englewood, <br />Colorado, and the following tests were performed: <br />
The URL can be used to link to this page
Your browser does not support the video tag.