HomeMy WebLinkAboutB940152 LEVEL I DRAINAGE ANALYSIS
FOR ..
ST. !ANTHONY PARISH
LOCATED AT 406 SOUTH 4TH STREET'
_ _ _ __ __
RENTON, WASHINGTON
OUR JOB NO. 5091
PREPARED BY:
BARGHAUSEN CONSULTING ENGINEERS, INC.
18215 72nd Avenue South
Kent, Washington 98032
T. Co
(206) 251-6222 f W �-
O P �
2PS02 lv�
MAY 3, 1994 ASS/aVAL d
5/5199
EXPIRES 4/10/ q5
SCI &OWL
LEVEL I DRAINAGE ANALYSIS
FOR ST. ANTHONY'S PARISH, RENTON, WASHINGTON
OUR JOB NO. 5091
1. INTRODUCTION/GENERAL INFORMATION
The project lies within a portion of the Southeast quarter of Section 18, Township 23 North,
Range 5 East, Willamette Meridian, King County, Washington. The project lies within the
corporate limits of the City of Renton. The existing site consists of an asphalt-paved parking area,
sidewalks, and some landscaped areas. The site is bounded by Whitworth Avenue on the east,
South 4th Avenue on the south, and an existing alley on the west. The project is bounded by
additional property owned by St. Anthony's Parish on the north. The site is 0.33 acres in size.
The overall topography of the site generally slopes from the building at 1 to 2 percent toward the
street and/or alley. The on-site soils as mapped in the United States Department of Agriculture
Soils Survey for King County is mapped as urban land soil. The soil is characteristic of disturbed
natural soil layers with additional fill of varied thickness. The proposed project is for the
remodeling of the existing parish ministry center and addition of an elevator.
II. UPSTREAM DRAINAGE CONSIDERATIONS
From the site inspection of the project, it is apparent that the site does not receive any storm
drainage runoff from upstream properties. Surrounding properties from the site are located at
approximately equal elevation. The drainage from adjacent properties slopes away from the lots
toward the existing roadway. All drainage from adjacent properties drains into an existing public
right-of-way and stormwater collection systems within the streets.
III. ON-SITE DRAINAGE CONSIDERATIONS
As mentioned in the introduction section of this report, the site drains from the existing building
to the south and east across existing landscape. This runoff then enters the public right-of-way
where it drains across the existing sidewalks into the stormwater collection system in the street.
Surface runoff from the northerly parking lot drains westerly to the existing alley. Once the
drainage enters this alley, a catch basin, located at the south end of the alley, collects the drainage.
From this point, the storm drainage is tightlined into the public stormline located within
South 4th Street. Please refer to the enclosed map which defines the drainage conditions on the
site.
IV. DOWNSTREAM DRAINAGE CONSIDERATIONS
Storm drainage runoff from the existing site sheet flows over the existing sidewalks into the
stormwater collection system in South 4th Street. Portions of the drainage from the site sheet flows
easterly also across the sidewalk and into the right-of-way drainage system in
Whitworth Avenue South. The stormwater drainage, once entering the previously-referenced
public streets, enters a stormwater collection system located at the intersection of South 4th Street
and Whitworth Avenue South. The stormwater is collected through an underground conveyance
system and tightlined through a 12-inch storm main running east and west on South 4th Street.
Stormwater in this main line flows westerly to Shattuck Avenue South. Once entering the storm
-1- M.364 [DTC/sdc]
drain manholes at the intersection of Shattuck Avenue South and South 4th Street, the stormwater
flows southerly through a 12-inch diameter pipe along Shattuck Avenue South to the intersection
of South 4th Place. At this intersection, the stormwater enters a storm drainage manhole which
also operates as an overflow structure. The southerly outlet is designed to act as an overflow storm
pipe only. The primary stormwater flow proceeds along the 18-inch diameter storm main located
in South 4th Place to the intersection with Rainier Avenue South. The stormwater then flows to
the westerly side of Rainier Avenue South and turns to head southerly to an 18-inch diameter storm
main. From here, the stormwater continues to run south of the storm drainage tightline.collection
system in Rainier Avenue South where it increases to a 24-inch diameter before entering the
stormwater lift station located at the Burlington Northern Railroad track crossing. Once stormwater
enters the existing stormwater lift station, it is pumped up and through a 48-inch diameter
corrugated metal pipe westerly, paralleling the south edge of the Burlington Northern Railroad
right-of-way. This 48-inch CMP stormwater pipe is routed westerly where two additional storm
drain lines connect at the crossing of Hardie Avenue S.W. From the connection point in
Hardie Avenue S.W., the 48-inch CMP stormwater pipeline proceeds westerly where it will
eventually connect to a stormline in South 7th Street. From this point, the stormwater runs
westerly where it eventually outfalls into the Black River system. This description of the
downstream analysis is in excess of the quarter-mile minimum required.
V. EXISTING DOWNSTREAM CAPACITY PROBLEMS
After research with the City of Renton Stormwater Section, there appear to be no existing capacity
problems with the. downstream conveyance system from the previously-mentioned site.
VI. DOWNSTREAM FLOODING COMPLAINTS
After research with the City of Renton Storm Drainage Section, it appears that no complaints have
been filed on the downstream drainage system from the proposed site.
VII. The following information has been obtained from the available resources through King County:
1. Sensitive area of folio, page no. 6.
a. The project is located in the Green River Drainage Basin.
b. No wetlands or open water exist on site. The closest wetland shown on the
sensitive area of folio is approximately 1.5 miles to the east.
C. No stream or 100-year flood plain is shown on the site.
d. No erosion is mapped on site.
e. No landslide area is mapped within the site.
f. No seismic hazard area has been mapped on site.
g. No coal mine hazard area is mapped for the project.
-2- M.364 [DTC/sdcl
2. Adopted basin plan and finalized drainage study.
This site is located in the Green River Drainage Basin.
3. Flood plain/FEMA map.
No flood plain has been show on site on the FEMA map.
4. Critical drainage maps.
The project site does not lie within a critical drainage basin.
5. Request for complaints have been filed with the City of Renton. No complaint information
was on record for this area.
6. Basin reconnaissance summary report.
See enclosed information.
7. Soil Survey for King County area, Washington.
See enclosed.
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FIRM
FLOOD INSURANCE RATE MAP
KING COUNTY,
WASHINGTON AND
INCORPORATED AREAS
PANEL 327 OF 650
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PANEL LOCATION
CONTAINS:
COMMUNITY NUMBER PANEL SUFFIX
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RENTON,CITY OF 530088 0327 0
'II UNINCORPORATED AREAS 530071 0327 0
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F MAN EFFECTIVE DATE:
SEPTEMBER 29, 1989
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UNITED STATES DEPARTMENT OF AGRICI -TURE
Soil Conservation Service
in cooperation with
WASHINGTON AGRICULTURAL EXPERIMB T STATION
Issued November 1973
If drained, this soil is used for row crops. It Ap2--3 to 8 inches, gray (SY 5/1) silty clay loam,
is also used for pasture. Capability unit IIw-3; light brownish gray (2.5Y 6/2) dry; many,
no woodland classification. fine, prominent, dark reddish-brown (5YR 3/3
and 3/4) mottles and common, fine, prominent
mottles of strong brown (7.5YR S/6) and red-
Urban Land dish yellow (7.5YR 6/6) dry; moderate, fine
and very fine, angular blocky structure; hard,
Urban land (Ur) is soil that has been modified by friable, sticky, plastic; common fine roots;
disturbance of the natural layers with additions of medium acid; abrupt, wavy boundary. 4 to 6
fill material several feet thick to accommodate large inches thick.
industrial and housing installations. In the Green B21g--8 to. 38 inches, gray (SY 5/1) silty-clay loam,
River Valley the fill ranges from about 3 to more gray (5Y 6/1) dry; common, fine, prominent,
than 12 feet in thickness, and from gravelly sandy brown (7.5YR 4/4) mottles and medium, promi-
loam to gravelly loam in texture. nent mottles of brownish yellow (10YR 6/6) dry;
The erosion hazard is slight to moderate. No 25 percent of matrix is lenses of very dark
capability or woodland classification. brown (10YR-2/2) and dark yellowish-brown
(10YR 3/4) peaty muck, brown (7.SYR 4/2) dry;
massive; hard, firm, sticky, plastic; few fine
Woodinville Series roots; medium acid; clear, smooth boundary.
30 to 40 inches thick.
The Woodinville series is made up of nearly level B22g--38 to 60 inches, greenish-gray (SBG 5/1) silt
and gently undulating, poorly drained soils that loam, gray (SY 6/1) dry; few, fine, prominent
formed under grass and sedges, in alluvium, on. stream mottles of brownish yellow (10YR 6/6) dry;
bottoms. Slopes are 0 to 2 percent. The annual massive; hard, very friable, slightly sticky,
precipitation ranges from 35 to 55 inches, and the slightly plastic; strongly acid.
mean annual air temperature is about 50' F. The
frost-free season is about 190 days. Elevation The A horizon ranges from dark grayish brown to
ranges from about sea level to about 85 feet. gray and from silt loam to silty clay loam. The B
In a representative profile, gray silt loam, horizon ranges from gray and grayish brown to olive
silty clay loam, and layers of peaty muck extend to gray and greenish gray and from silty clay loam to
a depth of about 38 inches. This is underlain by silt loam. In places there are thin lenses of very
greenish-gray silt loam that extends to a depth of fine sandy loam and loamy fine sand. Peaty lenses
60 inches and more. are common in the B horizon. These lenses are thin,
Woodinville soils are used for row crops, pasture, and their combined thickness, between depths of 10
and urban development. and 40 inches, does not exceed 10 inches.
Soils included with this soil in mapping make up
Woodinville silt loam (Wo) .--This soil is in elon- no more than 25 percent of the total acreage. Some
gated and blocky shaped areas that range from 5 to areas are up to 15 percent Puget soils; some are up
nearly 300 acres in size. It is nearly level and to 10 percent Snohomish soils; and some areas are up
gently undulating. Slopes are less than 2 percent. to 10 percent Oridia, Briscot, Puyallup, Newberg,
Representative profile of Woodinville silt loam, and Nooksack soils.
in pasture, 1,700 feet south and 400 feet west of Permeability is moderately slow. There is a sea-
the north quarter corner of sec. 6, T. 25 N., R. 7 sonal high water table at or near the surface. In
E : drained areas, the effective rooting depth is 60
inches or more. In undrained areas, rooting depth
Apl--O to 3 inches, gray (5Y 5/1) silt. loam, grayish is restricted. The available water capacity is
brown (IOYR 5/2) dry; common, fine, prominent, high. Runoff is slow, and the hazard of erosion is
dark reddish-brown (5YR 3/4) and reddish-brown slight. Stream overflow is a severe hazard unless
(5YR 5/4) mottles; moderate, medium, crumb flood protection is provided (pl. III, top) .
structure; hard, friable, sticky, plastic; This soil is used for row crops, pasture, and
many fine roots; medium acid; clear, smooth urban development. Capability unit IIw-2; woodland
boundary. 2 to 4 inches thick. group 3w2.
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