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

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city of Wood River is given <strong>in</strong> figure 30. The specific capacity<br />

of the collector well decl<strong>in</strong>ed from a peak of 270<br />

gpm/ft <strong>in</strong> August 1954 to about 50 gpm/ft <strong>in</strong> March 1963.<br />

A part of the decl<strong>in</strong>e <strong>in</strong> specific capacity can be attributed<br />

to the partial clogg<strong>in</strong>g of the laterals by <strong>in</strong>crustation<br />

and with sand and silt. Mechanical clean<strong>in</strong>g of one<br />

lateral <strong>in</strong> June 1962 <strong>in</strong>creased the specific capacity from<br />

about 50 gpm/ft to 55 gpm/ft.<br />

Figure 29.<br />

Relation between well-loss constant and<br />

drawdown due to well loss<br />

and sometimes impossible to restore the orig<strong>in</strong>al capacity<br />

if the well-loss constant is greater than 40 sec 2 /<br />

ft 5 .<br />

Periodic well treatment by acidiz<strong>in</strong>g or other methods<br />

has been used successfully to rehabilitate old wells.<br />

However, <strong>in</strong> many cases wells are abandoned as their<br />

yields decrease and new wells are drilled nearby.<br />

Based on data for production wells which have been<br />

<strong>in</strong> service a number of years, the average specific capacity<br />

of wells <strong>in</strong> the <strong>East</strong> <strong>St</strong>. <strong>Louis</strong> <strong>area</strong> is about 30 gpm/ft.<br />

An average well yield of 450 gpm can be obta<strong>in</strong>ed with<br />

a long service life if sufficient screen is provided.<br />

A graph show<strong>in</strong>g the decrease of specific capacity of<br />

a collector well owned by the Shell Oil Ref<strong>in</strong>ery near the<br />

Table 19. Theoretical Decreases <strong>in</strong> Specific Capacity<br />

Due to Increases <strong>in</strong> Well-Loss Constant<br />

Coefficient<br />

of<br />

transmissibility<br />

(gpd/it)<br />

Pump<strong>in</strong>g<br />

rate<br />

(gpm)<br />

Well-loss<br />

coefficient<br />

of 1 sec 2 /ft 5<br />

Speci-<br />

Draw- fic capadown*<br />

city*<br />

(ft) (gpm/ft)<br />

Well-loss<br />

coefficient<br />

of 5 sec 2 /ft 5<br />

Well-loss<br />

coefficient<br />

of 10 sec 2 /ft 5<br />

Specific<br />

capa-<br />

city*<br />

(gpm/ft)<br />

Drawdown*<br />

(ft)<br />

Specific<br />

Draw- capadown*<br />

city*<br />

(ft) (gpm/ft)<br />

300,000 900 9.3 96.9 25.3 35.6 45.3 19.9<br />

250,000 900 10.3 87.4 26.3 34.2 46.3 19.4<br />

200,000 900 11.9 75.6 27.9 32.2 47.9 18.8<br />

150,000 900 14.4 62.5 30.4 28.6 50.4 17.9<br />

100,000 900 19.7 45.7 35.7 25.2 55.7 16.1<br />

300,000 450 3.7 122.2 7.7 58.4 12.7 35.4<br />

250,000 450 4.2 110.7 8.2 54.9 13.2 34.1<br />

200,000 450 4.9 91.9 8.9 50.6 13.9 32.4<br />

150,000 450 6.1 73.8 10.1 44.5 15.1 29.8<br />

100,000 450 8.4 53.6 12.4 36.3 17.4 25.9<br />

*Theoretical<br />

Figure 30.<br />

Well Design Criteria<br />

Specific-capacity data for collector well,<br />

1954 to March 1963<br />

Walton (1962) gave criteria for well design <strong>in</strong> unconsolidated<br />

formations <strong>in</strong> Ill<strong>in</strong>ois. Screen design criteria<br />

are applicable to <strong>in</strong>dustrial, municipal, and irrigation<br />

wells. The objective is to design an efficient and economical<br />

well with a service life of at least 10 years.<br />

Accord<strong>in</strong>g to Ahrens (1957) artificial pack wells are<br />

usually justified when the aquifer is homogeneous, has a<br />

uniformity coefficient less than 3.0, and/or has an effective<br />

gra<strong>in</strong> size less than 0.01 <strong>in</strong>ch. The uniformity coefficient,<br />

C u , is the ratio of the sieve size that will reta<strong>in</strong><br />

40 percent of the aquifer materials to the effective size.<br />

The sieve size that reta<strong>in</strong>s 90 percent of the aquifer materials<br />

is the effective size. In addition, an artificial pack<br />

is sometimes needed to stabilize well-graded aquifers<br />

hav<strong>in</strong>g a large percentage of f<strong>in</strong>es <strong>in</strong> order to avoid excessive<br />

settlement of materials above the screen or to<br />

permit the use of larger screen slots. The uniformity coefficients<br />

based on mechanical analyses of samples <strong>in</strong><br />

figures 26 through 28 are less than 3 and/or the effective<br />

gra<strong>in</strong> size is less than 0.01 <strong>in</strong>ch, <strong>in</strong>dicat<strong>in</strong>g that an<br />

artificial pack well should be constructed at each site.<br />

Selection of the artificial pack is based on the mechanical<br />

analysis of the aquifer. A criterion that has been<br />

successfully used <strong>in</strong> Ill<strong>in</strong>ois is that the ratio of the 50<br />

percent sizes of the pack and the aquifer (the P-A ratio)<br />

be 5 (Smith, 1954). Artificial packs should range<br />

<strong>in</strong> thickness from 6 to 9 <strong>in</strong>ches (Walton, 1962).<br />

29

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