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tv <br />I-+ <br />Figure 5 <br />Schematic Illustration of "Wild Brining" <br />to <br />, abandoned wcllbores <br />- - "'t~;. <br />-- _ with open annuli <br />__ -.~ - - --- -t- <br />_ ~ - ~ _T_i_ -- // 1-r~T- <br />.. ti. I I ~~tt_ <br />--~;=7St <br />,~ <br /> 1 r. <br />~ <br />1 .: <br />l'~~. <br />r% <br />C. ..I--T •f <br />_ <br />. <br />.. t 1 <br />- <br />7 <br />-I-r•~ .1 <br />_ <br />. <br />... <br />=~L~- t '-- <br /> <br />~. ~`- <br />brlnc cavity `•. <br />brine withdrawal well <br />' --_ <br />71 _' =S 1 <br />1 <br />`~- l.. • <br />it-T-~ t J_'T._~... <br />~~ F <br />~ I•• .. <br />drinc cavity l _ • <br />• _ r <br />• ~_~'~R `y l"' _c.~~~, 'rye--~~~__ I ~ _~ •r-- •. <br />~~ \ <br />4 `~ i <br />Modified from Tully (1985). Brine cavity is recharged by water entry through open wellbores and annuli <br />as well as fractures associated with subsidegce features. <br />R~1~1 /~Ifl ~1 llllfl ~~ ~!n 111 An ~n wlsnl resRr i+.+~ tit .~...,. ..._. _- -- _ <br />• <br />• <br />