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<br /> <br />12 <br /> <br />beginning in 1941, as was done previously. <br /> <br />o <br />w <br />(;0 <br />~ <br /> <br />2. The model be modified to include the salt pick-up and <br /> <br />bank storage relationships discussed above. <br /> <br />J. Tributary inflow of water and salt to the river reach <br /> <br />between Lees ~erry and Grand Canyon be based on the period <br /> <br />beginning in 1954 rather than 1941, as was done previously. <br /> <br />The studies discussed in this report should be re-evaluated <br /> <br />as more data becomes available. In addition, consideration <br /> <br />should be given to initiating a study; similar to that now being <br /> <br />conducted by the U. S. Geological Survey at Flaming Gorge <br /> <br />to evaluate gains and losses of salt in Lake Powell more <br /> <br />than is now possible. <br /> <br />. '-~' ..'~".."'... .... ---. <br /> <br /> <br />:~ <br /> <br />i1~h.j <br />