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<br />w <br />w <br />w <br />(J1 <br /> <br /> 17,5 <br />~ <br />E <br />~ <br />Ul <br />0 15.0 <br />.s:::. <br />E <br />E <br />~ <br /> <br />U <br />I.LI <br />~12,5 <br />I- <br />> <br />I- <br />u <br />:::> 10,0 <br />o <br />Z <br />o <br />U <br />..J <br /><l: 7,5 <br />u <br />ii:: <br />I- <br />U <br />I.LI <br />..J <br />I.LI 5.0 <br /> <br /> LEGEND EC <br />1. FEATHER RIVER WATER 0.10 <br />2, GRAND RIVER WATER 0.94 <br />3, MISSOURI RIVER WATER 0.91 <br />4, SALT RIVER WATER 1.56 <br />5. COLORADO RIVER WATER 1. 27 <br />6, SEVIER RIVER WATER 2.03 <br />7, GILA RIVER WATER 3.14 <br />8. PECOS RIVER WATER 3.26 <br /> <br /> <br />2,5 <br /> <br />o <br />0.10 <br /> <br />0.15 0.20 0,25 0,30 <br />LEACHING FRACTION. LF <br /> <br />(f) <br />@ <br /> <br /> <br />@ <br /> <br />@ <br /> <br />~ <br /> <br />CD <br /> <br />Figure 2.2. <br /> <br />Average composition of drainage waters from noncalcarious lysimeters, spring of <br />year, (After Rhoades et al. 1973.) <br /> <br />7 <br />