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<br />0')''''' <br />UVLJU <br /> <br />7 <br /> <br />ENVJRONJVfENlj\t DEFENSE FUND <br /> <br />Figure 4. Water Flows at the Southern International Boundary, 1997 <br />(Valdes-Casillas et at., 7998a) <br /> <br />J J <br /> <br /> <br />'e 160 <br />= <br />=> <br />~ 120 <br />Q,l <br />'" <br />s... <br />Q,l <br />Q. 80 <br />,;; <br />~ <br />e <br />~ 40 <br />:c <br />= <br />u <br /> 0 <br /> <br /> <br />J <br /> <br />F <br /> <br />M <br /> <br />A M <br /> <br />A <br /> <br />s <br /> <br />o <br /> <br />N <br /> <br />D <br /> <br />Date (1997) <br /> <br />AGRICULTURAL WASTEWATER <br /> <br />Delta wetlands with significant conservation interest <br />also survive on agricultural wastewater. Seventeen <br />agricultural drains from the Mexicali Valley flow into <br />the Rio Hardy/Colorado River system, carrying an av- <br />erage annual volume of 51,000 acre-feet (6.33 x 107 m3) <br />(Valdes-Casillas et aI., 1998a). Another 125,000 acre-feet <br />(1.5 x 108 m3) of mildly saline (3000 parts per million) <br />agricultural wastewater pumped from Arizona's <br />Wellton-Mohawk Irrigation District is delivered to <br />Mexico at the Southern International Boundary. This <br />water is disposed in the eastern delta after travelling 48 <br />miles (77 km) in a concrete canal called the Main Outlet <br />Drain Extension (MODE). MODE water joins about <br />25,000 acre-feet (3.1 x 107 m3) of agricultural wastewater <br />(from the Riito drain) to support la Cienega de Santa <br />Clara. <br /> <br />La Cienega de Santa Clara was once part of a Colorado <br />River channel that ran along the edge of the Sonoran <br />Mesa. As the channel shifted westward, this shallow <br />depression (formed by a branch of the San Andreas fault) <br />nearly dried up. In 1973, before MODE water arrived, <br /> <br />the wetland covered only 490 acres (200 ha), fed by <br />artesian springs and the Riito drain (Glenn et al., 1996). <br />After 1977, when the MODE water started emptying into <br />the Santa Clara pepression, flows supported wetlands <br />of up to 50,000 acres (20,000 ha). In 1993, floods on the <br />Gila River required the MODE to be closed for repairs <br />for about eight months. As a result, wetlands in la <br />Cienega de Santa Clara decreased in size to 2700 acres <br />(1100 ha). With the restoration of flows, the marsh <br />returned to its former dimensions within five months <br />(Glenn et aI., 1996; ZengeI et aI., 1995). [See Box 2.] <br /> <br />Agricultural wastewater can change ecosystem health <br />since it tends to affect the concentration of pollutants, <br />salts, and minerals. High levels of selenium, for example, <br />are found in many delta areas that receive wastewater, <br />and selenium is known to affect birds and other wild- <br />life. Although agricultural wastewater has been a fairly <br />constant source for la Cienega de Santa Clara, over the <br />years the MODE canal has carried less water and its <br />salinity has declined. This is due to lower pumping rates <br />and lower groundwater salinity. Wastewater flows from <br /> <br />15 <br />