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<br />Prepared by: Bolton & Menk, Inc. PROPOSED IMPROVEMENTS <br />2026 PMP Street & Utility Improvements ǀ 25X.137753 Page 8 <br />normal water level. Submerged pipes that outlet stormwater into static, or <br />landlocked, water bodies typically build up sediment due to standing water. The <br />outlets into Karth Lake were unobstructed likely due to the following: <br />• Sufficient Flow Rate and Velocity - MnDOT recommends RCP stormwater <br />pipes are designed to have a full flow velocity of at least 3 feet per second. <br />This velocity is typically found to ‘self-clean’ stormwater pipes. Sand and small <br />suspended solids are unable to drop out of the stormwater flow. <br />• Depth of Receiving Water - Karth Lake has sufficient depth and volume for <br />water to freely exit each outfall. No underwater deltas have formed creating a <br />hydraulic jump for water and sediment to backflow into the storm outfalls. <br />Additional risks associated with submerged pipes include: <br />• Freeze/Thaw Cycles – Submerged pipes are subject to increased risk of pitting <br />and cracking due to expanding ice in winter months. Throughout the lifespan <br />of the pipe the structural integrity is much lower than a non-submerged pipe. <br />Many factors can contribute to how fast a submerged pipe cracks including <br />water depth, bedding material, pipe diameter, and weather. <br />Ice build-up is another risk that could lead to upstream flooding particularly in <br />snow melt events. If an outlet is completely blocked with ice, snow melt will <br />be unable to discharge from the drainage system and present surface flooding <br />issues. The amount of freezing weather in any winter season will drive the <br />depth of ice in Karth Lake. The deepest outlets are approximately five feet <br />under the ordinary high water level in Karth Lake and are unlikely to fully <br />freeze. The shallower outlets are more susceptible to being encapsulated by <br />fully freezing conditions but the weather will play a factor in the effect <br />freeze/thaw cycles have on backups to the system and long-term effects. <br />• Sediment Build-Up – No sediment build-up is occurring at these submerged <br />outlets, but the risk is higher than non-submerged outlets. It is possible that in <br />a future snowmelt event or large rain event that transports an unusually high <br />amount of suspended solids and organic matter will clog and fill the pipe. This <br />may create flooding upstream of the clogged outlet and present surface <br />flooding issues. That being said, these observations may be due to the fact <br />that the majority of the existing outlets into the lake have existing grit <br />chambers that are properly performing in general to minimize sediment <br />transport. The fact that there are additional proposed improvements to add <br />or improve sediment capture devices prior to outletting stormwater at <br />remaining locations should help alleviate this concern further. <br />No improvements to the storm outlets are proposed and it is recommended to <br />complete regular condition inspections on each apron to address <br />repairs/replacements on an as-needed basis. Additional evaluation can be completed <br />if proactive improvements are desired which would likely include adding an inline <br />storm structure and flattening the outlet apron to be above the ordinary high water <br />level. <br /> Stormwater Management <br />1. Accumulated Sediment Removal <br />A bathymetric survey was performed in April 2025 to assess the sediment load near <br />the five outlets into Karth Lake. The survey found some organic sediment was <br />DRAFT