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<br />18 <br /> <br />450 <br /> <br /> <br /> 400 <br /> Note.--No allowance modo for <br /> evaporation and seepagl <br /> k>SS8S. <br />Vl 350 <br />>- <br />.. <br />a <br />Vl <br />LL <br />U <br />LL <br />a <br />Vl <br />a <br />z <br />.. <br />Vl <br />::> <br />a 250 <br />:I: <br />I- <br />~ <br />LL <br />LL <br />0 200 <br />z <br />::> <br />'" <br />LL <br />a <br />w <br />::E 150 <br />::> <br />...J <br />0 <br />> <br />~ <br />W <br />I- <br />.. 100 <br />...J <br />::> <br />::E natural <br />::> <br />u <br />u <br />.. <br /> 50 <br /> ~ys a outflow rates <br /> <br />o <br /> <br /> <br />1951 <br /> <br /> <br />Figure 3,--Mass <br />station <br /> <br />1952 1953 1954 1955 1956 <br />YEARS <br />curve and outflow-storage lines for 1952 -57 drought <br />66. Delaware River at Valley Falls. Kans. <br />(Talal drainage areo, 922 sq mil <br /> <br />1957 <br /> <br />flow at <br />