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Ground-water development in East St. Louis area, Illinois. Urbana, IL ...

Ground-water development in East St. Louis area, Illinois. Urbana, IL ...

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wells conta<strong>in</strong> slotted pipe screens. Irrigation wells range<br />

<strong>in</strong> diameter from 8 to 16 <strong>in</strong>ches and usually have pack<br />

thicknesses of 6 to 8 <strong>in</strong>ches. Lengths of slotted pipe<br />

screens range from 10 to 40 feet.<br />

Service Life of Wells and Collector Wells<br />

One of the problems <strong>in</strong> the <strong>East</strong> <strong>St</strong>. <strong>Louis</strong> <strong>area</strong> associated<br />

with the <strong>development</strong> of ground-<strong>water</strong> resources<br />

is the short life expectancy of wells. Accord<strong>in</strong>g to a<br />

study by Bru<strong>in</strong> and Smith (1953), the median service<br />

life of municipal wells term<strong>in</strong>at<strong>in</strong>g <strong>in</strong> sand and gravel<br />

formations <strong>in</strong> the <strong>East</strong> <strong>St</strong>. <strong>Louis</strong> <strong>area</strong> is about half that<br />

for similar municipal wells <strong>in</strong> other parts of the state.<br />

Nearly all of the wells retired <strong>in</strong> the <strong>area</strong> were taken<br />

out of service either because the screens had become partially<br />

clogged or the wells had filled with sand.<br />

The results of mechanical analyses presented by<br />

Bergstrom and Walker (1956) are shown <strong>in</strong> figures 26<br />

through 28. Accord<strong>in</strong>g to Bergstrom and Walker the<br />

analyses must be accepted with caution because the conditions<br />

of collect<strong>in</strong>g most of the samples are not known,<br />

and because of the highly variable nature of the valleyfill<br />

deposits <strong>in</strong> the <strong>area</strong>. A careful exam<strong>in</strong>ation of the<br />

mechanical analysis curves suggests that the valley-fill<br />

deposits conta<strong>in</strong> a rather high percentage of f<strong>in</strong>e materials<br />

which could, under heavy pump<strong>in</strong>g conditions,<br />

migrate toward a screen and partially clog the well wall<br />

and screen open<strong>in</strong>gs. As <strong>in</strong>dicated by data <strong>in</strong> the files of<br />

<strong>in</strong>dustries and municipalities, specific capacities of exist<strong>in</strong>g<br />

production wells decrease markedly after a few years<br />

and <strong>in</strong> some cases after a few months of operation.<br />

Specific capacities are generally determ<strong>in</strong>ed by the driller<br />

after completion of the well by pump<strong>in</strong>g the well at<br />

different rates for short periods of time, generally less<br />

than 24 hours, and by frequently measur<strong>in</strong>g drawdowns<br />

<strong>in</strong> the pumped well. This method of measur<strong>in</strong>g specific<br />

capacity is cont<strong>in</strong>ued by <strong>in</strong>dustrial and municipal personnel<br />

periodically.<br />

It is a general practice of <strong>in</strong>dustries and municipalities<br />

to place a well <strong>in</strong> operation and pump it at high rates,<br />

often about 1000 gpm. As the result of heavy pump<strong>in</strong>g,<br />

f<strong>in</strong>e materials migrate towards the well and partially<br />

clog screen open<strong>in</strong>gs and the voids of the formation surround<strong>in</strong>g<br />

the well. The well-loss constant <strong>in</strong>creases rapidly<br />

and, because well loss varies as the square of the discharge<br />

rate, drawdown <strong>in</strong>creases rapidly. The relation<br />

between well-loss constant and drawdown due to well<br />

loss is shown <strong>in</strong> figure 29. As drawdown <strong>in</strong>creases the specific<br />

capacity and, therefore, the yield of the well decreases.<br />

Typical decreases <strong>in</strong> specific capacity due to<br />

<strong>in</strong>creases <strong>in</strong> the well-loss constant are given <strong>in</strong> table 19.<br />

Theoretical specific capacities of wells with a nom<strong>in</strong>al<br />

radius of 15 <strong>in</strong>ches and with 40 feet of screen given <strong>in</strong><br />

table 19 were determ<strong>in</strong>ed for values of the coefficient of<br />

transmissibility rang<strong>in</strong>g from 100,000 to 300,000 gpd/ft,<br />

Figure 26.<br />

Mechanical analyses of samples from wells<br />

27

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