Laserfiche WebLink
I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br />I <br />I <br />I <br />I <br />I <br />! <br />I <br /> <br />DEPARTMENT: <br /> <br />i Natural Resources <br />!Division of Waters <br /> <br /> STATE OF MINNESOTA <br />Office Memorandum <br /> <br />DATE: iNovember 21, 1995 <br /> <br /> TO: [Tom Hovey, Area Hydrologist <br /> '-Region 6 <br /> <br />FROM: Jim Solstad <br /> iSenior Hydrologist <br /> <br /> PHONE: <br />SUBJECT: <br /> <br />297-3851 <br /> <br />~UNWOOD DRIVE MITIGATION (2-114P) <br /> <br />As requested, I ex',tmined possible mitigation options for protected basin 2-114. This mitigation <br />is in regard to a p~,,rmit application (94-6209) for a bridge and fill wetland crossing. I didn't do <br />everything you ask,ed, but hopefully the following data and recommendations meet your needs. <br /> <br />I quickly eliminate,It consideration of any type of ditch block at the surveyed Section No. 1. The <br />houses along KryOton Street are extremely low. Any action at Section 1 could subject these <br />structures to additional flood risk. I therefore concentrated my review and analysis at sections 2 <br />and 3. <br /> <br />The contributing w~atershed area to Section 2 is 325 acres and the area of the wetland above this <br />point is approxima!ely 75 acres. The approximate watershed to wetland area ratio is 4.3:1. This <br />watershed is locatq~d in the Anoka sandplain. The Anoka County soil survey indicates that the <br />soils in the CD 43 ~vatershed are highly permeable generally having a hydrologic classification of <br />"A". The low watershed to wetland area ratio coupled with the highly permeable soils suggests <br />that there should ~not be a significant bounce following a heavy rainfall/runoff event. This <br />conclusion is supported by the fact that the OHW for the southern portion of the basin is only <br />0.8 feet above its rUnout. <br /> <br />I developed a ver~ simple watershed model using the Corps of Engineers' HEC-1 computer <br />program for the CD 43 watershed above Section 2. I assumed the worst-case scenario was the <br />10-day runoff' eveflt (curve number = 100) and ran the model for the 10- and 100-year storms <br />(4.8 and 7.3 inchei, respectively). Rounding the numbers off, I found that the bounce for the <br />10- and 100~year ,events was 1.0 and 1.5 feet, respectively. These results seem reasonable <br />irrespective of whit options we take for the ditch blocks. Again, these numbers are pretty <br />rough, but hopefully they give a ball park estimate of the high levels which may occur. <br /> <br />I've reconsidered m~y recommendations since our telephone conversation. Let me know if the <br />following seems re~tsonable. <br /> <br /> <br />