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SU0004916
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SU0004916
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Last modified
12/13/2019 9:43:57 AM
Creation date
9/5/2019 10:44:07 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004916
PE
2638
FACILITY_NAME
PA-0500142
STREET_NUMBER
18353
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
MOUNTAIN HOUSE
ENTERED_DATE
3/17/2005 12:00:00 AM
SITE_LOCATION
18353 W GRANT LINE RD
RECEIVED_DATE
3/15/2005 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\sballwahn
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\MIGRATIONS\G\GRANT LINE\18353\PA-0500142\SU0004916\COLLEGE PRK SP III.PDF
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EHD - Public
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4 <br /> ► Any new or expanded storm-drain facilities required to safely collect,convey,and in some cases treat,the <br /> .. runoff to be generated by new development under the College Park project must be in place before <br /> construction.It has not been determined how extensive of water treatment would be required,if any. The San <br /> Joaquin General Plan requires treatment of stormwater runoff from industrial uses prior to release into the <br /> stormwater conveyance system,in this case,stormwater from the residential and commercial uses. The type <br /> of treatment facility needed to serve the industrial uses associated with the proposed project shall be <br /> determined by the College Park developers' engineer and provided in construction documents to the County <br /> and MHCSD for approval. <br /> Under the proposed College Park project,impervious surfaces at the project site would increase from <br /> approximately 15%of the total land area to approximately 47%(MacKay& Somps 2004).The increase in <br /> .. impervious surfaces would increase the quantity of runoff generated on the project site.Table 4.7-2 below <br /> identifies the modeled stormwater runoff quantities for the three on-site watersheds under the following scenarios: <br /> existing conditions,development of the College Park site under the existing MHMP, and development of the <br /> College Park site as currently proposed. <br /> Watershed A would result in a net decrease in peak flow as shown when analyzed for existing and proposed <br /> ` conditions. This is because of the timing effect of the subareas in the watershed. A large portion of Watershed A <br /> is undeveloped, located in the upstream portion of the watershed,and the runoff would increase in peak flow and <br /> volume of runoff; however,flow would peak sooner than when the watershed is undeveloped. The juxtaposition <br /> of the flows from the undeveloped area and the developed area would have a wider gap in times of peak. The <br /> resultant peak flow decreases; however,volume of runoff would increase. <br /> Table 4.7-2 <br /> College Park Existing/Future Stormwater Runoff Quantities ' <br /> On-site Watersheds Existing 100-Year Developed Under MHMP 100- Proposed Project 100- <br /> Runoff(cfs)b Year Runoff(cfs) Year Runoff(cfs) <br /> Watershed A 610` 602` 607` <br /> (Central Parkway System) <br /> Watershed B 282' 5004 472° <br /> (DeAnza Boulevard System) <br /> Watershed D 38e 147` 1270 <br /> (Mountain House Parkway System) <br /> Total 930' 1,249' 1,206' <br /> Note:Above values include stormwater drainage originating from off-site watersheds(i.e.,Watersheds D,E,B,and SB9A). <br /> ' The runoff quantities in this table are in cis and represent the runoff entering or eating the project site. <br /> b These values were calculated by PACE in the Mountain House Drainage Master Drainage Plan Update,May 27,2003. <br /> } ` Approximately 491 cfs of this is runoff from off-site(pass-through flows). <br /> e <br /> Approximately 158 cfs of this is runoff from off-site(pass-through flows). <br /> ' All of these flows originate on-site. <br /> ' Approximately 649 cis of this is runoff from off-site(pass-through flows). <br /> Source:MacKay&Somps 2004. <br /> As shown in Table 4.7-2,the proposed project would increase the total stormwater runoff from the project site <br /> during a 100-year storm event from 930 to 1,206 cfs,a 29.7%increase in runoff.A slight decrease in existing <br /> runoff would occur in the on-site portion of Watershed A,while relatively large increases in runoff would occur <br /> .� in on-site Watersheds B and D.However,whether the increase in runoff under the proposed project would exceed <br /> the capacity of the existing downstream infrastructure is determined by comparing the runoff quantities of the <br /> College Park project to runoff from development of the site under the existing MHMP. <br /> As indicated in Table 4.7-2,the proposed project would result in a smaller increase in total stormwater runoff <br /> from the project site during a 100-year storm event than would buildout of the project site under the existing <br /> 4 College Park at Mountain House Specific Plan III Draft EIR EDAW <br /> San Joaquin County 4.7-15 Drainage <br />
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