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<br />16 . <br /> <br />COLORADO WATER <br /> <br />, <br /> <br />~~;Jt 1997 <br /> <br />0273 <br /> <br />. <br /> <br />u.s. GEOLOGICAL SURVEY DATA COLLECTION <br />AND STUDIES IN THE ARKANSAS RIVER BASIN <br /> <br />by Doug Cain, Subdistril:t Chief <br /> <br />Editor's nole: Doug Cain. Subdistricl Chief. U.S. Geological Survey, presenJed the following <br />paper aI lhe Arkansas River Basin Waler Forum, "A River of Dreams and Realilies," <br />January 22.23. 1997. The forum was held in Pueblo. Colorado. Cain describes the USGS <br />data colleClion efforts and lhe slatus of water quality in the valley. <br /> <br />The U.S. Geological Survey has taleen on additional responsibilities within the last year. In the past, we were the nation's <br />mapmalcers, geologists and hydrologists. We have recently incorporated the National Biological Survey as one or our divisions. <br />so now we have the capability to do biological studies also. Another thing I should mention about the USGS is that we are nOl a <br />regulatory agency; we are a scientific agency. We are proud of our unbiased approach to science. <br /> <br />Our office in Pueblo is responsible for water resources data collection and studies, both in the Arleansas Valley and the San Luis <br />Valley of Colorado. I will focus on the Arleansas Valley today. Within the basin. we worle with about 20 local agencies to do data <br />collection and studies and with about five other federal agencies that provide us funding for various activities related to water. <br />The office in Pueblo includes aboUI 35 people. mostly hydrologists and hydrologic technicians, who collect data and do studies on <br />waler. <br /> <br />I would Iilee to give you an overview of our activities before I go into detail about some of the results of our worle. We are <br />responsible for data collection and studies in the basin, and that includes the operation of a large number of stream gages and <br />continuously recording water qualily monilors. We collect data on surface and groundwater quality. suspended sediment in <br />streams. and precipitation primarily related to studies that we have in process. Another site that we operate in this basin, near the <br />Las Animas fish hatchery, is a part of the National Trends Networle, which looles at the acidity of precipitation. We have a <br />number of groundwater level networles in the Arleansas River Basin. For many of the stream gage and water quality monitoring <br />siles, the data (both real.time and historic) have been available on the Internet now for about twO years. The same address (web <br />server.cr.usgs.gov/home.htmlf) can provide you links to get real-time stream /low information for virtually the entire United <br />States. You might want to talee a loole althat website. <br /> <br />I will talle today about the results of either recent or <br />ongoing studies that we have done in the basin. I will <br />stan by loolcing at groundwater levels in the basin. <br />We have a number of water level networles in the <br />basin, the largest of which is in the alluvial aquifer <br />along the Arleansas River between Pueblo and the <br />Kansas state line. There, we have measured water <br />levels in a number of wells for more than 25 years. In <br />the last year, we have gone bacle and looked at data <br />from a number of those wells that had been measured <br />for that entire period to see if we can identify trends. <br /> <br />Many of you know that there is concern about high <br />water-table conditions in the basin, and I think Figure <br />1 will give you an idea of what we have seen. It <br />shows the average change in water level (in feet). <br /> <br />0-" <br />W <br />W <br />U. <br />Z <br />-. <br />..; <br />w <br />> <br />w <br />-', <br />a: <br />w <br />0- <br />< <br /><:, <br />i!!: <br />w <br />Cl <br />z, <br />< <br />:l: <br />o <br />w <br />Cll <br />< <br />a: <br />w <br />> <br /><0 <br /> <br />n=53 <br /> <br />n=34 <br /> <br />n=56 <br /> <br /> <br />PUEBLO TO FT. <br />LYON CANAL <br />HEADGATE <br /> <br />FT. LYON CANAL <br />HEADGATE TO <br />JII. <br /> <br />JMA TO STATE <br />UNE <br /> <br />RIVER REACH <br /> <br />These are all increases in water level. and this is the <br />level where groundwater will stand in a well below the Fig. 1. Aperage 25-Year (1969.94) Change in Groundwater upels. <br /> <br />