My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2014-04-09_REVISION - M1977493 (2)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1977493
>
2014-04-09_REVISION - M1977493 (2)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 5:43:06 PM
Creation date
4/10/2014 3:48:07 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977493
IBM Index Class Name
REVISION
Doc Date
4/9/2014
Doc Name
Evaluation of clean water interceptor system TR18
From
Climax Molybdenum
To
DRMS
Type & Sequence
TR18
Email Name
ECS
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.
/
27
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
Ray Lazuk <br />March 19, 2014 <br />Page 12 <br />The overflow structure at Kokomo Creek consists of a 48 -inch CMP crossing under the service <br />road. The overflow structure at Searle Gulch consists of a 10- foot -wide weir that discharges <br />into a box culvert crossing under the service road. The two 24 -inch slide gates that can be used <br />to divert water into the Climax industrial area at the Searle Gulch diversion structure were <br />assumed to be closed for this analysis. <br />Table 3 provides a summary of the flow rate and percentage of the peak flow rate that would <br />overflow at these structures for the storm events considered, assuming that the gates into the <br />interceptor were fully open. <br />Table 3. West Interceptor Overflow Structure Flow Rates. <br />The West Interceptor after Searle Gulch consists of 46 -inch to 50- inch - diameter CMP until the <br />end of the West Interceptor at Tucker Creek. The runoff entering this piped section during the <br />10 -year rainfall and rain -on -snow events exceeds the gravity -flow capacity of the pipe, causing <br />the inlet at the Searle Gulch diversion structure to be submerged. The capacity of this piped <br />section apparently has been exceeded before, as indicated by several overflow culverts that <br />have been installed near existing interceptor inlets to route runoff over and across the <br />interceptor pipe and into the industrial area. The locations of the interceptor inlets — two of <br />which have been capped — and the overflow culverts are shown on Figure 7b. Any water that <br />crosses the West Interceptor through these overflow culverts would discharge into and be fully <br />contained in Mayflower TSF. <br />10 -Year Rain - <br />Overflow <br />10 -Year Rainfall <br />On -Snow <br />Structure <br />Event <br />Event <br />Kokomo Creek <br />21 cfs (21 %) <br />28 cfs (25 %) <br />Searle Gulch <br />140 cfs (54 %) <br />154 cfs (56 %) <br />The West Interceptor after Searle Gulch consists of 46 -inch to 50- inch - diameter CMP until the <br />end of the West Interceptor at Tucker Creek. The runoff entering this piped section during the <br />10 -year rainfall and rain -on -snow events exceeds the gravity -flow capacity of the pipe, causing <br />the inlet at the Searle Gulch diversion structure to be submerged. The capacity of this piped <br />section apparently has been exceeded before, as indicated by several overflow culverts that <br />have been installed near existing interceptor inlets to route runoff over and across the <br />interceptor pipe and into the industrial area. The locations of the interceptor inlets — two of <br />which have been capped — and the overflow culverts are shown on Figure 7b. Any water that <br />crosses the West Interceptor through these overflow culverts would discharge into and be fully <br />contained in Mayflower TSF. <br />
The URL can be used to link to this page
Your browser does not support the video tag.