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The impact of urban groundwater upon surface water - eTheses ...

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MONITORING NETWORKS AND METHODS<br />

grain size that is 10% finer by weight is between 0.1 and 3.0 mm. <strong>The</strong> Hazen approximation<br />

is:<br />

K=C(d10) 2<br />

K = hydraulic conductivity (cms -1 )<br />

d10 = the effective grain size, (10% finer by weight) (cm).<br />

C = coefficient based on sorting see Table 4.2, (cm -1 s -1 )<br />

Table 4.2 Representative values <strong>of</strong> the Hazen coefficient for different grain sizes and degrees<br />

<strong>of</strong> sorting (Fetter, 1994).<br />

Sediment character<br />

Range <strong>of</strong> ‘C’ coefficient<br />

(cm -1 s -1 )<br />

Very fine sand, poorly sorted 40 – 80<br />

Fine sand with appreciable fines 40 – 80<br />

Medium sand, well sorted 80 – 120<br />

Coarse sand, poorly sorted 80 – 120<br />

Coarse sand, well sorted, clean 120 – 150<br />

Additional work has been carried out by Shepherd (1989) in which he developed a<br />

relationship between grain size and conductivity based on field and laboratory data from 18<br />

published studies. <strong>The</strong> general formula for the relationship is<br />

K = Cd50 j<br />

86

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