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<br />1,..'" <br />..... <br />~ <br />N <br />o <br />o <br /> <br />downstream from Santa Rosa, near Roswell, snd south of Car1sbadin- <br />~reaaes the salinity of surface flows. During periods of low stream- <br />flow the saline content of surface water exceeds the tolerance of <br />many irrigated crops. <br /> <br />Large sediment loads have silted stream channels and greatly <br />reduced the' capacity of reeervoirs.ThJ.e problem will be partly <br />alleviated by sediment storage in authorized reservoirs, however, <br />land treatment and other conservation measures are. required to <br />reduce sediment loads. <br /> <br />Phreatophyte growth invades stream channels and reservoir <br />areas. <br /> <br />Problem Area 5, ASA's 1302 and 1301.:... In areas where groundwater <br />is being mined, pumping. from wells exceeds recharge and groundwater <br />levels are being lowered. <br /> <br />Throughout the Rio Grande Region i~ New Mexico, most of the <br />groundwater supplies are within boundaries of underground water <br />I;>asins as declared by the State Engineer., In these areas, new <br />appropriations cannot be made if such appropriations will impair <br />an existing right. ' <br /> <br />Groundwater supplies used for irrigation'and other purposes <br />in the Rio Grande 'Region in New Mexico are furnished from multiple- <br />aquifer sources. Sources, static water levels,' and yields vary <br />throughout tl)e region. Details can be found in reports l'isted <br />in the reference list, . Chapter VI.' <br /> <br />The f.:>llowing tabulation shows acreage irrigated from ground7 <br />water supplies in 1975 and the withdrawals and depletions from <br />this source. Part of. the acreage ree..i..ed. ~pp1.ies from both <br />surfac!' and groundwater, however, withdrawals and depletions <br />furnished from surface-water sources are not included as part of <br />this tabulation. <br /> <br />17 <br /> <br />.', ,.-",: <br /> <br />.. <br />. ' <br /> <br /> <br />:.?{: <br /> <br />I <br />