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<br />Figure 2-lA (Chapter 2) shows a schematic flow diagram of the water <br />budget as averaged for the l8-year evaluation period. <br /> <br />~ <br />.~ <br /> <br />Water not used by crops is percolating into the ground and <br />dissolving large quantities of salt from the aquifer bedrock, which <br />is made up of the Bridger and Green River Rock Formations. The <br />major salts contributing to the total dissolved solids in the Big <br />Sandy River are sulfates, sodium, and magnesium. <br /> <br />f"-f:~ <br />f'<.'i <br />*, <br /> <br />.. <br />~ <br /> <br />~~~ <br />\,},,~ <br />t'.71 <br />;u:.;I <br /> <br />Annual salt contributions to the Big Sandy River are shown in <br />Table 2-5 in Chapter 2. The average annual salt loading for the <br />18-year period (1960-1977) is estimated at 149,180 tons (at Gasson <br />Bridge) . <br /> <br />f" <br />~,'1 <br />,~ <br />;;:j <br /> <br />,~(~ <br />~~ <br /> <br />1'>..0; <br />~ <br /> <br />,.;~: <br />.;.'1 <br />...L; <br /> <br />.~ <br />,~ <br /> <br />~ <br /> <br />'e.i:...t <br /> <br />~:.t. <br /> <br />!:;t <br />~~{ <br />"" <br /> <br />, , 1" . 0. <br />,\., ! --- V <br />,,-I,w .L ~ <br /> <br />,r~ <br />,~-'" <br />.,~ <br /> <br />1-4 <br /> <br />~ <br />G; <br />