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PART 12 Aquifer pumping tests - Dr. M. Zreda - University of Arizona

PART 12 Aquifer pumping tests - Dr. M. Zreda - University of Arizona

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<strong>Aquifer</strong> <strong>pumping</strong> <strong>tests</strong> 103<br />

Partial penetration<br />

We have 3-D flow due to partial<br />

penetration.<br />

If s = const, partially penetrating<br />

wells give less Q than fully penetrating<br />

wells because more energy<br />

is required to get water up (less<br />

area?).<br />

If Q = const, partially penetrating<br />

well causes more drawdown than<br />

does fully penetrating one.<br />

<strong>Dr</strong>awdown curve far away from s<br />

the <strong>pumping</strong> well looks like fully<br />

penetrating and the slope <strong>of</strong> drawdown curve approaches slope <strong>of</strong> fully penetrating well drawdown.<br />

Penetration is important in calculating S. Do not use the late curve (straight line); use the early<br />

one.<br />

Large diameter well<br />

Has storage, usually built in low-K<br />

aquifers. Specific yield <strong>of</strong> the<br />

well: S y = 1. S is overestimated<br />

(t 1 ). Use t 0 to get S.<br />

s<br />

t 0<br />

wrong<br />

estimation<br />

<strong>of</strong> S<br />

actual<br />

drawdown<br />

fully<br />

penetrating<br />

Hydrogeology, 431/531 - <strong>University</strong> <strong>of</strong> <strong>Arizona</strong> - Fall 2007 <strong>Dr</strong>. Marek <strong>Zreda</strong><br />

t 1<br />

small<br />

diameter<br />

well<br />

t 0<br />

use this to get S<br />

large<br />

diameter<br />

well<br />

log t<br />

log t

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