Laserfiche WebLink
SOUNDVIEW TECHNOLOGY CENTER EVERETT, WA <br /> Basin B <br /> This drainage Basin B is conveyed to a steep ravine that intersects the property along the northern <br /> property line. The ravine has signs of surface flow at the low point.The stormwater is then conveyed along <br /> the forested swale, where it intersects a home-built wall and asphalt pavement over the flow path. The <br /> pavement is associated with an adjacent residence. The wall and asphalt pavement are shown in the <br /> photo 4.1 and 4.2 below. <br /> Just below this wall, a homemade 2-foot wide swale was constructed in the natural low point of the Swale <br /> to convey stormwater.This swale was rimmed on both sides with concrete test cylinders (see photo 5) <br /> with minor tree debris was observed in the swale. The stormwater is conveyed within this swale for <br /> approximately 60', and then discharges back to a more natural forest swale. The approximate slope of <br /> this swale is 20%. The stormwater then continues down in the natural swale until entering a 15" diameter <br /> culvert on the south side of Debrelon Lane. The culvert opening was clear at the time of the downstream <br /> analysis. <br /> The storm water is conveyed through catch basins for approximately 300 feet, and connects to a plastic <br /> storm pipe outlet. This pipe outlets to a catch basin with grate. See Picture 6.1 below. This catch basin <br /> connects to the existing 18-inch culvert under Lamar Drive where it discharges into an "Unnamed Stream," <br /> as documented by the Snohomish County GIS, located in the ravine above Edgewater Creek to the <br /> northeast.The unnamed stream discharges to Edgewater Creek. <br /> Navix attempted to locate the outfall from the pipe that heads northwest from the CB in Lamar Drive <br /> through private property, but was unable to obtain permission from the property owner to follow the <br /> pipe's path and locate the outfall. However, the angle of the pipe leaving the CB appears to head directly <br /> towards the unnamed stream and the contours of the land match what would be expected of a stream <br /> channel. See pictures 6.2, 6.3, and 6.4 below. <br /> Refer to Figures 1, 2, and 3 on pages 30-31 for the maps and photos of the drainage path. <br /> One potential issue of this basin outfall is the private wall and asphalt pavement constructed across the <br /> forest swale. Per an older downstream analysis prepared by Datum Pacific, there is a 12" CSP culvert <br /> underneath this wall connecting the forest swale with the 2' wide created swale.This could not be verified <br /> in the field. There are two 4" concrete pipes that outfall at the base of the wall, but since no inlet for these <br /> pipes could be found it can be assumed that they are there for sub-drainage behind the wall. There was <br /> evidence of water traveling around the eastern side of the wall to get to the ditch. There is also evidence <br /> of surface flow across the pavement, which will continue in the future. <br /> Since this project will detain the release rates to the predeveloped release rates in excess of the release <br /> rates required for the project (0.5 CFS max. discharge to this basin), no additional measures are proposed <br /> and the release flows will be dispersed on-site at the low point of the Swale. <br /> SEPTEMBER 23, 2022 STORMWATER DRAINAGE REPORT PAGE 11 <br />