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ARCHIVED REPORTS_2013_4
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ARCHIVED REPORTS_2013_4
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Last modified
7/17/2020 3:53:43 PM
Creation date
7/3/2020 10:57:16 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2013_4
RECORD_ID
PR0440005
PE
4433
FACILITY_ID
FA0004516
FACILITY_NAME
FORWARD DISPOSAL SITE
STREET_NUMBER
9999
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106001-3, 5
CURRENT_STATUS
01
SITE_LOCATION
9999 AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2013_4.tif
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EHD - Public
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® 2.2 Flood Control <br /> The realigned channel needs to carry the 100-year flood flows within its banks. Erosion protection <br /> should be provided in areas with high velocities or sharp bends. A U.S. Army Corps of Engineers <br /> HEC-RAS hydraulic model was used to determine design water surface elevations and estimate <br /> channel velocities and other pertinent flow parameters for stable channel design. <br /> 2.3 Stable Chatinel Design <br /> The new channel realignment needs to be stable and function as a natural system. Excessive bank <br /> erosion and meandering has to be minimized. The design needs to anticipate the vegetative <br /> succession and perform without flooding or sustaining excessive bank erosion under those <br /> conditions. <br /> 3.0 DESIGN CONSIDERATIONS AND METHODOLOGIES <br /> The following discussion outlines the primary design parameters that were considered and <br /> incorporated into the project design. <br /> 3.1 Hydrologic Considerations <br /> One of the basic design parameters of a channel is the amount of flow the channel must carry. <br /> Typically only the maximum flow is considered.However,in order to design a natural stable channel <br /> a full spectrum of flows must be taken into account. Though large magnitude flows are important <br /> from a flood control standpoint they typically do not occur at frequent intervals and thus do not <br /> contribute to the year in and year out forces acting on the channel, which really shape the channel. <br /> This typically is referred to as the channel forming discharge.Large magnitude discharges typically <br /> cause catastrophic bank failures and play a role in the molding the general channel configuration,at <br /> least locally. However,it is the typical winter flows that occur on the order of every one to two years <br /> that drive general channel shape and morphology through erosion and sediment transport <br /> The hydrologic regime of the North Branch of the South Fork of Littlejohn's Creek is somewhat <br /> unusual. Farmington Reservoir is a flood control reservoir operated by the U.S. Army of Corps of <br /> Engineers located upstream,that controls stormwater flows in the North Branch of the South Fork of <br /> Littlejohn's Creek. A review of average daily releases from Farmington Reservoir for 21 water years <br /> (1979 to 1999)shows the maximum release was 2,420 cubic feet per second(cfs).This stormwater is <br /> divided several tributaries. Often, and especially during drought years, there was no release from <br /> Farmington Reservoir. <br /> FEMA Flood Flows <br /> The Federal Emergency Management Agency (FEMA) routinely publishes stream flows <br /> associated with return interval(years)for flood insurance purposes.Table 1 below indicates the <br /> magnitude and recurrence interval for peak events at the Austin Road Landfill. <br /> Questa Engineering Corporation 2 99279CMApril b, 2000 <br />
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