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Comparison of Two Approaces for Determining Ground-Water Discharge and Pumpage in the Lower Arkansas River Basin Colorado 1997-98
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Comparison of Two Approaces for Determining Ground-Water Discharge and Pumpage in the Lower Arkansas River Basin Colorado 1997-98
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Water Supply Protection
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Comparison of Two Approaces for Determining Ground-Water Discharge and Pumpage in the Lower Arkansas River Basin Colorado 1997-98
State
CO
Basin
Arkansas
Author
Dash, Russell; Troutman, Brent; Edelmann, Patrick
Title
Comparison of Two Approaces for Determining Ground-Water Discharge and Pumpage in the Lower Arkansas River Basin Colorado 1997-98
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Report/Study
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and end of a monitoring period. The same TFM moni- <br />toring period was used with each PCC in 1998 for <br />determining the TFM pumpage at each site. <br />Quality Control of Data <br />Data for this study were collected by CDWR <br />personnel and transmitted to the USGS in electronic <br />and paper files for data analysis. Several procedures <br />were used to check the quality of the data. Quality - <br />control checks consisted of developing a form <br />(referred to as a field form) to be completed onsite <br />during each site visit, making periodic site visits <br />with CDWR personnel to observe onsite data collec- <br />tion, reviewing field forms for completeness, and <br />comparing electronic data to written data recorded <br />on the field forms. <br />Personnel from the USGS visited the sites to <br />ensure that TFM's were installed according to the <br />manufacturer's specifications. In addition, USGS <br />personnel periodically visited selected sites with <br />CDWR personnel to ensure that field techniques were <br />being used correctly. During these visits, USGS <br />personnel checked that (1) site information and essen- <br />tial test information were documented on field forms, <br />(2) multiple water -level measurements were made to <br />confirm that the pumping water level had not changed <br />more than 10 percent in the hour prior to making a <br />well discharge measurement and collecting the PCC <br />data, (3) portable flowmeter discharge measurements <br />were done properly, (4) consistent methods were used <br />in measuring TFM discharge, and (5) electrical power <br />meter measurements were consistently determined. <br />Field forms were used to document various <br />characteristics of network wells. Site identifier, test <br />date, and test methods used at each well during a PCC <br />measurement also were recorded on field forms. Other <br />data recorded on the field forms included a description <br />of the discharge test procedures used and any type of <br />problem during the measurement, instantaneous <br />discharge (pumping rate), static and pumping water - <br />level measurements, and PCC's determined for each <br />portable flowmeter method used during a site visit. <br />Personnel from the USGS reviewed the field forms for <br />completeness, tabulations, and consistency with estab- <br />lished collection procedures. About 10 percent of the <br />electronic data were verified against copies of the orig- <br />inal field forms, and all electronic data were scruti- <br />nized for anomalous data. <br />In addition to these quality - control measures, <br />the three types of portable flowmeters used in the <br />study were tested at the Great Plains Meter, Inc., <br />facility in Aurora, Nebraska, before the start of the <br />1998 irrigation season. The accuracy of the method P <br />portable flowmeter was checked by releasing a known <br />volume of water three times through the test apparatus <br />at the facility, while total elapsed time was measured <br />to calculate an average rate of discharge. The <br />discharge measured by the method P portable flow- <br />meter for each timed release ranged from 99 to <br />101 percent of the known discharge. The accuracy of <br />the method C portable flowmeter was checked by <br />maintaining a constant flow of water through the test <br />section at the facility. The method C portable flow- <br />meter was installed in a straight length of pipe, and <br />manometer readings were taken at two points in the <br />cross section of the pipe. The instantaneous discharge <br />measured by the method C portable flowmeter ranged <br />from 103 to 104 percent of the discharge measured by <br />a flowmeter installed in the test section at the facility. <br />The test facility did not make any calibration adjust- <br />ments to either the method P or the method C portable <br />flowmeters. Because the measurements using <br />method P and method C portable flowmeters were <br />within 5 percent of known values, no adjustments <br />were made to the well discharge data collected with <br />these portable flowmeters. <br />The accuracy of each method M portable <br />flowmeter was checked using a one -point flow test <br />and then calibrated using a three -point flow test. <br />The rate of flow used during these tests ranged from <br />about 100 gal/min for the 4 -in. flowmeter, to about <br />3,000 gal/min for the 10 -in. flowmeter. After calibra- <br />tion adjustments, the flows measured by the method M <br />portable flowmeters ranged from 98 to 102 percent of <br />the known flows. <br />Overview of the Statistics Used for <br />Comparing Discharge and Pumpage <br />A statistical procedure known as analysis of <br />variance was used to make comparisons of well <br />discharge and pumpage made using the TFM's and the <br />PCC approaches. These comparisons were made by <br />computing the differences in well discharge and <br />pumpage between the two different approaches. The <br />analysis of variance evaluates whether the average or <br />mean difference in values is statistically different and <br />10 Comparison of Two Approaches for Determining Ground -Water Discharge and Pumpage in the <br />Lower Arkansas River Basin, Colorado, 1997 -98 <br />
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