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City of Prince George - Snow Disposal at the Lansdowne Road ...

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espectively. Under future conditions, assuming th<strong>at</strong> <strong>the</strong> snow collection area were not<br />

expanded, <strong>the</strong> disposal times would be similar, due to a combin<strong>at</strong>ion <strong>of</strong> increased dilution<br />

capacity caused by increased flow r<strong>at</strong>es <strong>at</strong> <strong>the</strong> plant, and lower permitted effluent TSS<br />

concentr<strong>at</strong>ions.<br />

The second factor limiting snow disposal <strong>at</strong> <strong>the</strong> WWTC is <strong>the</strong> melting capacity <strong>of</strong> <strong>the</strong> chlorine<br />

contact tank. Based on <strong>the</strong> test d<strong>at</strong>a, <strong>the</strong> times required to dispose <strong>of</strong> <strong>the</strong> collected snow from<br />

<strong>the</strong> annual minimum, annual mean, and annual maximum snow falls under present conditions<br />

(assuming 24 hour per day oper<strong>at</strong>ion) are 38 days, 53 days, and 76 days, respectively. Under<br />

future conditions, <strong>the</strong> disposal times would be similar, due to a combin<strong>at</strong>ion <strong>of</strong> increased flow<br />

<strong>at</strong> <strong>the</strong> plant and lower permitted effluent TSS concentr<strong>at</strong>ions. Note th<strong>at</strong> <strong>the</strong> d<strong>at</strong>a in Table 4 are<br />

based on rel<strong>at</strong>ively cold temper<strong>at</strong>ures (<strong>the</strong> air temper<strong>at</strong>ure was in <strong>the</strong> range 25-30 degrees C<br />

below zero). At warmer temper<strong>at</strong>ures, <strong>the</strong> available energy (i.e., <strong>the</strong> temper<strong>at</strong>ure <strong>of</strong> <strong>the</strong> tank<br />

influent) might be higher, and <strong>the</strong> energy required to raise <strong>the</strong> temper<strong>at</strong>ure <strong>of</strong> <strong>the</strong> snow to <strong>the</strong><br />

melting point would be lower. However, note th<strong>at</strong> in <strong>the</strong> <strong>the</strong>oretical calcul<strong>at</strong>ion carried out in<br />

Section 4.1, <strong>of</strong> <strong>the</strong> total energy required (375.5 MJ/tonne), nearly 90% (333.5 MJ/tonne) was<br />

required to melt <strong>the</strong> ice, and only 10% was required to bring <strong>the</strong> ice to <strong>the</strong> melting point.<br />

5.4 <strong>Snow</strong> Storage Requirements<br />

The d<strong>at</strong>a summarized in Table 5 take no account <strong>of</strong> <strong>the</strong> depth and frequencies <strong>of</strong> individual<br />

snowfalls.<br />

The limited snow disposal capacity <strong>of</strong> <strong>the</strong> WWTC means th<strong>at</strong> a storage area for collected snow<br />

may be required for extreme snowfall events. Th<strong>at</strong> is, during periods <strong>of</strong> high snowfall, <strong>the</strong><br />

snow collection r<strong>at</strong>e may exceed <strong>the</strong> maximum snow disposal r<strong>at</strong>e. The storage area required<br />

will depend on we<strong>at</strong>her p<strong>at</strong>terns, which are impossible to predict accur<strong>at</strong>ely. However, an<br />

estim<strong>at</strong>e <strong>of</strong> <strong>the</strong> maximum snow storage volume was made, based on <strong>the</strong> historical snowfall<br />

d<strong>at</strong>a included in <strong>the</strong> report by Stanley & Associ<strong>at</strong>es (1993).<br />

Dayton & Knight Ltd. Page 5-7

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