My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2013-10-30_REVISION - M1977310 (3)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1977310
>
2013-10-30_REVISION - M1977310 (3)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/15/2021 2:28:45 PM
Creation date
11/5/2013 5:47:39 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977310
IBM Index Class Name
REVISION
Doc Date
10/30/2013
Doc Name
DRAINAGE DESIGN PLAN FOR THE JD6 MINE
From
COTTER
To
DRMS
Type & Sequence
AM1
Email Name
TC1
SJM
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.
/
101
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
JD -6 Mine — Drainage Design Plan 10 <br />3. HYDROLOGIC CHARACTERISTICS OF SITE SOILS <br />The dominant soil types in the JD -6 Mine facilities area are Bodot and Ustic Torriorthents, which are <br />shown as soil type 23 on Figure 4 of the EPP. Additionally, a thin exposure of rock outcrop — Orthents <br />complex has been mapped along the ridgeline (MRCS, 2012b) in the headwaters of Sub -basin 132. The thin <br />soils that occur on steeper areas of pinyon - juniper woodlands in the vicinity of the JD -6 Mine (Unit 23) are <br />classified as fine, montmorillonitic, calcareous, mesic Ustic Torriorthents and are mapped as Hydrologic <br />Soil Group C (Table 4). Rocky outcrop areas are mapped as Group D. These soil groups are defined by <br />the NRCS (2012a) as: <br />Group C. Soils having a slow infiltration rate when thoroughly wet. These consist chiefly <br />of soils having a layer that impedes the downward movement of water or soils of <br />moderately fine texture or fine texture. These soils have a slow rate of water transmission. <br />Group D. Soils having a very slow infiltration rate (high runoffpotential) when thoroughly <br />wet. These consist chiefly of clays that have a high shrink -swell potential, soils that have a <br />high water table, soils that have a claypan or clay layer at or near the surface, and soils <br />that are shallow over nearly impervious material. These soils have a very slow rate of <br />water transmission. <br />Table 4. Soils Types in Vicinity of the JD -6 Mine Facilities (Sub -Basin B2) <br />Map <br />14.11 -42.23 <br />Hydro Depth <br />K Sat (micro <br />Soil Name <br />Unit <br />Taxonomic Classification <br />Group (in) <br />m /sec) <br />Fine, montmorillonitic <br />0 -3 <br />1.41 -4.23 <br />Bodot, dry <br />(calcareous), mesic Ustic <br />3 -30 <br />0.42 -1.41 <br />Torriorthents <br />C 30 -34 <br />0.00 -14.11 <br />23 <br />0 -4 <br />1.41 -4.23 <br />Ustic <br />Ustic Torriorthents <br />4 -31 <br />1.41 -4.23 <br />Torriorthents <br />31 -35 <br />0.42 -1.41 <br />Rock outcrop --- <br />88 <br />Orthents Orthents <br />D 0 -60 0.00 -0.03 <br />0 -1 <br />14.11 -42.23 <br />1 -14 <br />14.11 -42.23 <br />B <br />14 -24 <br />1.40 -14.00 <br />24 -60 <br />1.40 -14.00 <br />The runoff curve numbers for the site were selected based on soil type, land use, and vegetative cover. A <br />curve number of 73 was applied for pinyon juniper with grass understory, in fair condition (30 -70% <br />vegetative cover) and group C soils (Table 5). A curve number of 89 was applied to areas occupied by the <br />gravel access road (County Road EE19). A curve number of 85 was applied to the disturbed ground and <br />waste rock piles in the mine facilities area. For sub -basins containing more than one soil or cover type, a <br />weighted average curve number was calculated based on the relative areas of each CN. Site curve numbers <br />are listed in Table 6 and area - weighted average curve numbers are provided in Attachment 4. <br />4148A.131028 Whetstone Associates <br />
The URL can be used to link to this page
Your browser does not support the video tag.