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A system for detecting fluorescent tracers in streamflow

dc.contributor.authorSteppuhn, Harold Wolfgang, author
dc.contributor.authorMeiman, James R. (James Richard), advisor
dc.contributor.authorDils, Robert E., committee member
dc.contributor.authorHarris, David V., committee member
dc.contributor.authorJohnson, Gestur, 1910, committee member
dc.contributor.authorDuke, Harold R. (Harold Ray), 1940-, committee member
dc.date.accessioned2021-12-07T02:44:02Z
dc.date.available2021-12-07T02:44:02Z
dc.date.issued1970
dc.descriptionCovers not scanned.
dc.descriptionPrint version deaccessioned 2021.
dc.description.abstractA system is developed capable of continuously monitoring the relative concentration of a fluorescent tracer in streamflow. Streamside instrumentation automatically registers stream-borne tracer concentrations as a function of time on a gelatin-coated film. The film is routed through a device which passes a continuous sample-aliquot diverted from the tracer-dosed stream over a small segment of the film. The "exposed" film is periodically gathered from stream sites and analyzed in a laboratory-based fluorometer. Utility of the system is studied for the gaging of streamflow to produce a hydrograph, to measure stream discharge instantaneously, and to determine time-of-stream-travel. Hydrographs resulting from 640 hours of gaging two Colorado mountain streams with the system are compared to those obtained from closely located sharp-crested weirs. The maximum instantaneous deviation between hydrographs reaches 10% and average absolute departure equals 1.8%, while algebraic departure averages +0.3%. The practicality of using this system to obtain time-of-stream travels is demonstrated for five Colorado mountain streams. A total of 62 traveling tracer-clouds are registered on gelatin-coated film, from which time-of-stream-travels are determined. Processes involved in the system and factors affecting its precision are investigated. Theoretical and experimental evidence strongly indicates that the bulk of tracer uptake by gelatin follows processes that are physical rather than chemical in nature. Stream temperature changes and duration of film-tracer contact are the two most important factors affecting precision of the system. Neither major factor caused any unsolvable problem when field operations were standardized. The system will have utility in operations where an expensive, temperature-sensitive fluorometer can not be stationed stream-side, and where the particular objectives of stream measurements do not justify the cost of conventional techniques, but where fair accuracy and continuous records of short to moderate duration are desired.
dc.format.mediumdoctoral dissertations
dc.identifier.urihttps://hdl.handle.net/10217/234093
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationMMS ID: 991004407599703361
dc.relationGB1225.C6 S7
dc.relation.ispartof1950-1979
dc.relation.isreferencedbyMeiman, James R. Little South Poudre Watershed and Pingree Park Campus. Colorado State University, College of Forestry and Natural Resources (1971). http://hdl.handle.net/10217/70382
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectStream measurements -- Colorado
dc.subjectFluorimetry
dc.titleA system for detecting fluorescent tracers in streamflow
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineWatershed Sciences
thesis.degree.grantorColorado State University
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy (Ph.D.)

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