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<br />, <br /> <br />Water is also diverted into the non-project Percha and Bonita Laterals. The Percha <br />Lateral comes off the east side of the river at the Percha Diversion Dam and the Bonita Lateral <br />comes off the west side at Caballo Dam. <br /> <br />The Garfield, Hatch, Angostura, and Rincon Drains are the main drainage facilities in the <br />Rincon Valley. These facilities were constructed for the most part during the late 19108 and <br />early 1920s. All discharge to the river in the Rincon Valley. The historical discharges to the <br />river from these drains are discussed in Section 4 of this report. <br /> <br />The major aquifer in the Rincon Valley is the flood-plain alluvium. It typically is 60 to 80 <br />feet thick, consisting of a basal layer of gravel overlain by sand, silt, and clay. It extends over <br />the entire length of the valley, but is not more than 2 miles wide. Although basin fill deposits of <br />the Santa Fe Group underlies and borders the flood-plain alluvium in the Rincon Valley, they <br />consist primarily of a thick sequence of clay. The development of irrigation wells in the flood- <br />plain alluvium has been significant, but we have not been able to obtain specific data for the <br />number of wells constructed or the amount of pumpage.3J Additional wells have been <br />developed in narrow strips of alluvial fill in the tributary arroyos. Such wells provide not only <br />supplemental water for project and non-project lands, but also sole sources of irrigation <br />supplies. Yields for irrigation wells in the valley are reported to range from 320 to 2,360 gpm <br />with an average of 1,050 gpm. Recharge to these aquifers is from irrigation, precipitation, and <br />seepage from canals and the Rio Grande and its tributaries. Overall, the aquifer is reported to <br />be in balance; however, the water table declines as much as 10-feet in dry years when the <br />pumping tends to be high and the recharge tends to be low (Wilson and others, 1981, pp. 28- <br />32). Much of the ground water in the flood-plain alluvium has concentrations of total dissolved <br />solids of more than 1,000 milligrams per liter (White and others, 1981, p.83), <br /> <br />3J Much of the limited data and information that are presently available relate either to the Mesilla Valley or <br />to both the Rincon and Mesilla Valleys. This limited data and information are discussed later in this report <br />section. <br /> <br />r - <br /> <br />(' ... ,""\ <br />'" ..' v <br /> <br />2-9 <br /> <br />~--_. <br />