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(:ANSE'14 LUJAN & ASSO CIA'i ES <br />Hydrogeologiral and Environmental Consultants <br />Evaluation of U.S.G. S. and CDWR Stream Gauge Records on the South Platte River <br />in the Vicinity of the Bachofer Property and Fort Lupton Area <br />Discharge data from the Fort Lupton Gauging Station on the South Platter River were <br />obtained online from the USGS National Water Information System. The station is located <br />on the South Platte River on CR 18 '/Z mile north of the Bachofer property. Data have been <br />collected intermittently since 1930 to the present. Early data from 1930 to 1957 were <br />collected from the original station that was located approximately 3 miles upstream from the <br />present location on CR 18. No data were collected from 1958 to 2002 and the station was <br />moved to its present location in 2002 (oral comm. Rick Crowfood, USGS), where stream <br />data have been collected since 2003. Annual peak flows at Fort Lupton Station are shown <br />below on Figure 2. <br />Figure 2 <br />Peak Flows at Fort Lupton <br />South Platte River <br />Flow data from the missing years, 1958 to 2002 were calculated by using a linear regression <br />analysis of flow data (2002 to 2012) from the Henderson station located approximately 14 <br />miles upstream from the Fort Lupton station. Peak flows from this station are presented on <br />Figure 3 below. Data from this station are collected by the Colorado Division of Water <br />Resources (CDRW) State Engineer's Office and was obtained online. <br />The results of the regression analysis with the regression equation are shown on Figure 4 <br />and were used to estimate discharge at the Fort Lupton station. Figure 2 shows these <br />estimated predicted data with a dashed line and hollow symbol marker. In the years <br />preceding the existence of the present Fort Lupton gauge from 1987 to 1995, Mr. Bachofer <br />reported that peak flows at the Henderson station exceeding 11,000 cfs on Figure 3, did not <br />4 <br />35,000 <br />30,000 <br />, <br />Slurry wall constructed <br />25,000 <br />; i <br />around 01ts <br />Prior to slurry wall <br />20,000 <br />�+ no flooding occurs <br />" i <br />' <br />_,---+. _- Fort <br />tt ; flows over <br />i <br />P Hoods <br />with flows over <br />Lupton <br />4 <br />15,000 <br />t_,_a <br />6'4ro q cfs post <br />�. Predicted <br />10,000 <br />5,000 <br />, t , -; <br />�1 <br />v <br />3 <br />Ale, <br />t; <br />I <br />Q <br />0' <br />O <br />eMQ� n 00 <br />Ln 0) <br />T O Q1 0 <br />N <br />C14 <br />Date <br />N <br />a <br />`- <br />T to t0 <br />N <br />O i <br />Flow data from the missing years, 1958 to 2002 were calculated by using a linear regression <br />analysis of flow data (2002 to 2012) from the Henderson station located approximately 14 <br />miles upstream from the Fort Lupton station. Peak flows from this station are presented on <br />Figure 3 below. Data from this station are collected by the Colorado Division of Water <br />Resources (CDRW) State Engineer's Office and was obtained online. <br />The results of the regression analysis with the regression equation are shown on Figure 4 <br />and were used to estimate discharge at the Fort Lupton station. Figure 2 shows these <br />estimated predicted data with a dashed line and hollow symbol marker. In the years <br />preceding the existence of the present Fort Lupton gauge from 1987 to 1995, Mr. Bachofer <br />reported that peak flows at the Henderson station exceeding 11,000 cfs on Figure 3, did not <br />4 <br />