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<br /> <br />A <br /> <br />. <br /> <br />-' <br /> <br />- ' <br /> <br />/,1 I" --> I ,....- <br />-.... "// <br /> <br />Water table <br />------------ ------ ----- <br /> <br />\ <br /> <br />'" <br /> <br />----- <br /> <br />Unconfined aquifer <br /> <br />--- <br /> <br />B <br /> <br />--' <br /> <br />Recharge area <br />---land surface --::: <br />-- - ..... <br /> <br />===---- <br /> <br />E <br />. <br />~ <br />'" <br /> <br />\ <br /> <br />" <br /> <br />-~ <br />- " <br />2' ........... <br />----- <br />,-------- "- <br />........ --- <br />----- - - <br /> <br />-- <br /> <br />--- <br /> <br />-- <br /> <br />-- <br /> <br />\ <br /> <br />-------- <br /> <br />_-.- - Q, -8 <br />- land surface -..::::- :~ <br />- - ..... .... c <br />--\---- Y'C~t!!!~~~.___\----------- -----\----------=-~-----~-- ~ 1?-:' <br /> <br />\ ----- ,,----:::. <br />" "-...... '-.... " '\ / I\...-=.:: <br />..... _______ '---. '-..-1 /" <br />---- -- - ------- <br />--- <br /> <br />-' <br /> <br />/11 \ /,1 I ,....- <br />-....' //,/ <br /> <br />----- <br /> <br />Unconfined aquifer <br /> <br />--- <br /> <br />c <br /> <br />-' <br /> <br />//1' /,1 I ,........ <br />_" 1..--..... <br /> <br />Water table <br />---------------------------------- <br />\ \ <br />'" <br /> <br />----- <br /> <br />Unconfined aquifer <br /> <br />--- <br /> <br />~ <br /> <br />"-... <br /> <br />- <br /> <br />----- <br /> <br />-- <br /> <br />Confining bed <br /> <br />Confining bed <br /> <br />-- <br /> <br />--land surface -::::- <br />-- - .... <br /> <br />"-...... <br /> <br />\------- <br />'-.... -----------------", <br /> <br />------- '---. -- ' <br />- <br /> <br />------- <br /> <br />--- <br /> <br />-- <br /> <br />Confining bed <br /> <br /> <br />Q2 <br /> <br />E <br />. <br />~ <br />'" <br /> <br />.:: <br /> <br />" <br />2' <br /> <br /> <br />15 <br /> <br />Figure C-1. In a schematic hydrologic <br />setting where ground water discharges <br />to a stream under natural conditions (A), <br />placement of a well pumping at a rate <br />(0,) near the stream will intercept part <br />of the ground water that would have <br />discharged to the stream (B), If the well <br />is pumped at an even greater rate (021, <br />it can intercept additional water that <br />would have discharged to the stream <br />in the vicinity of the well and can draw <br />water from the stream to the well (e), <br />