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Low Impact Development Manual for Michigan - OSEH - University ...

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Research in the Saginaw River valley has shown (<strong>for</strong><br />

the winter of 1996-1997) that soils in cultivated areas<br />

with little to no snow cover froze to depths of up to<br />

eight inches, while in areas with <strong>for</strong>est cover, leaf litter,<br />

and thin but persistent snow cover, frost depths only<br />

reached about an inch (Schaetzl and Tomczak, 2002).<br />

One conclusion that can be drawn from this is that plant<br />

material should be left in applicable stormwater BMPs<br />

to provide insulation through the winter. The ability of<br />

persistent snow cover to act as insulation also suggests<br />

that some BMPs such as bioretention areas, infiltration<br />

basins, and vegetated swales can be used <strong>for</strong> snow storage<br />

(as long as it does not cause physical damage to the<br />

vegetation or other BMP components). However, large<br />

amounts of sand or salt should be kept out of vegetated<br />

and infiltration BMPs. Sand and salt can smother and/<br />

or kill plants and reduce infiltration/storage capacity.<br />

Sand should also never be used on or adjacent to porous<br />

pavement systems (see detailed BMP section).<br />

In addition, some BMPs, such as bioretention areas<br />

should be installed with a mulch layer that is two to<br />

three inches thick. For maximum insulation effectiveness,<br />

the mulch should be spread evenly and consistently<br />

throughout the BMP (<strong>for</strong> details on mulch see the individual<br />

BMP sections).<br />

All biological activity is mediated by temperature.<br />

Cold winter temperatures significantly decrease nutrient<br />

uptake and pollutant conversion processes by plants<br />

and microbes; however, soil microbes still live and<br />

consume nutrients even in the dead of winter. Accumulation<br />

of chloride is generally not a problem in shallow<br />

biological systems, as long as very highly concentrated<br />

levels are not directly routed to them.<br />

Infiltration considerations<br />

As water cools its viscosity increases, reducing particlesettling<br />

velocities and infiltration rates into the soil. The<br />

problem with infiltration in cold weather is the ice that<br />

<strong>for</strong>ms both over the tops of infiltration practices and in<br />

the soil pore spaces. To avoid these problems to the extent<br />

possible, the BMP must be actively managed to keep it<br />

dry be<strong>for</strong>e it freezes in the fall. This can be done by various<br />

methods including limiting inflow, under-drainage,<br />

and surface disking. Routing the first highly soluble<br />

portions of snowmelt to an infiltration BMP provides the<br />

opportunity <strong>for</strong> soil infiltration and treatment.<br />

Winter Pollution Prevention Tips<br />

• Choose proper de-icing materials<br />

• Consider pre-wetting brine treatments to salt <strong>for</strong><br />

better application<br />

• Load salt trucks on covered, impervious pads<br />

• Calibrate salting vehicles often<br />

• Properly manage salt storage piles<br />

• Identify and avoid salt-sensitive areas prior to<br />

plowing or salting<br />

Snow Storage Tip<br />

Commercial and industrial areas that plow their parking<br />

and paved areas into big piles on top of pavement<br />

could greatly improve runoff management if instead<br />

they dedicated a pervious area within their property <strong>for</strong><br />

the snow. Even pushing the plowed snow up and over<br />

a curb onto a pervious grassed area will provide more<br />

treatment than allowing it to melt on a paved surface<br />

and run into a storm sewer.<br />

Vegetation in winter at George George Park,<br />

Clinton Township, MI<br />

LID <strong>Manual</strong> <strong>for</strong> <strong>Michigan</strong> – Chapter 7 Page 127

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