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44 <br />40 <br />36 <br />32 <br />W 28 <br />t= <br />_J <br />e: <br />w <br />a 24 <br />F- <br />Z <br />w <br />20 <br />d <br />w <br />J <br />J 16 <br />1 <br /> <br />EXPLANATION °D <br />00 <br />Carbonate plus bicarbonate a^, <br />Sulfate <br />¦ Chloride <br />Calcium <br />® Magnesium <br />Sodium plus potassium <br />(1948 - 50) Period of record <br />used for analysis 8 <br />OD <br />v <br />rn <br />io <br />n <br />o> <br />m <br />M <br />00 <br />r` <br />r` <br />? O <br />M <br />2 0? obi <br />a <br />m ?- <br />0? 0? I W La r? <br />rn rn <br />rn <br />i ,. <br />C <br />58 61 62 63 64 67 68 69 70 <br />Figure 21. Mean chemical composition of dissolved solids at selected sites in San Juan region. Cations on left, anions <br />on right. <br />per year (table 10). This trend represents a 12-percent change <br />in the median annual concentration during the 20-year period. <br />Animas River at Farmington, N. Mex. (site 62) <br />The Animas River is the largest tributary of the San <br />Juan River. At site 62 (table 3, pl. 1), near the mouth of <br />the river, mean annual runoff averages about 8.1 in. (table <br />9). Streamflow is somewhat regulated by Lemon Reservoir <br />and Electra Lake, and about 30,000 acres is irrigated up- <br />stream from the site. The streamflow hydrograph shows a <br />typical snowmelt-runoff peak in June and steady base flow <br />during the winter months (fig. 22C). Mean annual flow- <br />weighted dissolved-solids concentration is greater than at site <br />61, averaging about 263 mg/L. Calcium and bicarbonate are <br />the predominant ions during the high-flow season. Calcium <br />and sulfate predominate during the low-flow season. <br />No statistically significant annual monotonic trends in <br />streamflow or dissolved solids were detected during 1955-83. <br />However, monthly concentrations of dissolved sodium and <br />chloride decreased significantly, mainly during the low-flow <br />season. <br />San Juan River at Farmington, N. Mex. (site 63) <br />Site 63 (table 3, pl. 1) is just downstream from the <br />mouth of the Animas River. Irrigated area upstream from <br />the site totals about 86,000 acres. Streamflow is controlled <br />partly by Navajo Reservoir, and the period of record <br />(1962-82) is essentially the same as the postintervention <br />period for site 61. Streamflow is a combination of the <br />regulated streamflow of the San Juan River and the seasonal <br />streamflow of the Animas River. Streamflow peaks during <br />June, and it is maintained at about 1,200 ft3/s during the <br />San Juan Subregion 51