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17 <br /> 0 <br /> 0 <br /> 0 <br /> m <br /> 0 <br /> a <br /> matters that we deemed should be wade to adjust them before =: <br /> we submitted full details to th- Con 4Sasion. <br /> -I <br /> First of all, in the study itself we have made an Z <br /> assumption of siltation that we found is not entirely Jueti.. <br /> fled. In other words, we found that the reservoir vie empty. < <br /> and that we were operating on natural stream flow conditions Nj <br /> for approximately 40 per Cent of the summer months of this <br /> whole period. ?ho initial assumption that we made was that <br /> the quantities of water carried in the river as silt would be <br /> derposited in this reservoir. Now, we realize, having made <br /> the study, that the silt in that water when the gates are open <br /> and the reservoir is eapty will be carried through and down. <br /> stream, and will not be deposited in the reservoir, and there- <br /> tore in a subsequent study we propose to adjust that siltation <br /> esthtaate accordingly. It won' t sake any large differenos, but <br /> it will ,sake some. <br /> Now, there were two points as to release that we at;., <br /> tempted to adjust. First, It didn't seem logical to assense <br /> a plan that would permit of an increase upstream in 0a44o4 <br /> and permit an increase downstream in Kansas aeeoapanied by a <br /> total, increase in diversions in District 6?, and our effort <br /> is directed now toward a plea of operation which will remedy <br /> that minus value that showed up in that one area along the <br /> river. <br /> The other point was that tnpre was a alight mat_., <br />