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Detailed Stormwater Management Practice Design - Tauranga City ...

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As = WQV/((fd)(i)(t)-p)<br />

Where:<br />

As = surface area of the trench (m 2 )<br />

WQV = water quality volume (m 3 )<br />

fd = infiltration rate (m/hr) - rate reduced by ½ from measured<br />

i = hydraulic gradient (m/m) - assumed to be 1<br />

t = time to drain from full condition (hours) - maximum time 48 hours<br />

p = rainfall depth for water quality storm (m)<br />

There is a simple test to see how deep an infiltration practice can be to achieve<br />

the discharge of the water quality storm. Any deeper than the amount calculated<br />

will not achieve the two-day draw down period. The equation is the following:<br />

dmax = fd(t/Vr)<br />

Where:<br />

dmax = maximum depth of trench<br />

fd = infiltration rate (m/hr)<br />

t = time to drain from full condition (hours)<br />

Vr = void ratio of reservoir stone (normally 0.35 or 0.5 if scoria is used), 1 for<br />

infiltration basins<br />

Once dmax has been defined, the actual needed depth can be calculated. If the<br />

actual depth exceeds the maximum depth the surface area must be increased to<br />

account<br />

d) Find the practice volume to provide storage for 37% of the volume required to<br />

infiltrate. This allows for storage of excess runoff during those periods when the<br />

runoff exceeds the infiltration rate.<br />

V = 0.37(WQV + pAs/Vr)<br />

Where:<br />

V = practice volume with any aggregate added<br />

NOTE: Permeable paving does not usually have a contributing drainage area<br />

draining to it. As such the volume of storage equals the following:<br />

V = pAs/vr where p is the design rainfall event (at least the water quality storm<br />

but generally will be up to the 10-year rainfall event)<br />

Page 45 Updated 01/11/2012

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