2005
DOI: 10.3133/sir20045164
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Using the tracer-dilution discharge method to develop streamflow records for ice-affected streams in Colorado

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Cited by 4 publications
(6 citation statements)
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“…For chronic exposure over the course of 7 days, a worst-case scenario of an upper bound of 1 ppm is envisioned. This estimation is based on actual tracing scenarios, , where tracer dilution varied from ×10 2 to ×10 4 from start to endpoint.…”
Section: Resultsmentioning
confidence: 99%
“…For chronic exposure over the course of 7 days, a worst-case scenario of an upper bound of 1 ppm is envisioned. This estimation is based on actual tracing scenarios, , where tracer dilution varied from ×10 2 to ×10 4 from start to endpoint.…”
Section: Resultsmentioning
confidence: 99%
“…During winter in cold regions of the world, ice and snow can partially fill stream channels, altering channel morphology, and create varying backwater conditions (Figure 1) [ Capesius et al , 2005]. These conditions change the stage‐discharge relation, leading to inaccuracies in discharge values calculated using continuous stage records and rating equations.…”
Section: Introductionmentioning
confidence: 99%
“…Although suitable during springtime when air temperatures are not far below 0°C, salt solutions do not provide adequate freezing protection in the central Rocky Mountains during midwinter, when temperatures sometimes drop below −25°C. In a test of a tracer dilution system in Colorado during winter 2002, an approximately 100,000 mg L −1 sodium chloride solution was injected into a stream using a metering pump [ Capesius et al , 2005]. Despite the strength of the salt solution, partial freezing caused substantial problems in system operation.…”
Section: Introductionmentioning
confidence: 99%
“…Organisms require these elements for optimal health, however, excessive amounts can disrupt normal metabolic processes (Evans and Frick, 2001; Environment Canada and Health Canada, 2001; Fischel, 2001; Lewis, 2001). Previous research has shown that repeated applications of sodium chloride (NaCl) for deicing control on paved roads can lead to elevated concentrations of chloride and sodium in the surface waters adjacent to roads (Howard and Beck, 1993; Evans and Frick, 2001; Environment Canada and Health Canada, 2001; Fischel, 2001; Bossong et al, 2003; Godwin et al, 2003; Capesius et al, 2005; Kaushal et al, 2005; Panno et al, 2006; Collins and Russell, 2009). Dissolved salt may alter the physical properties of surface water by increasing the density, resulting in salt accumulation in deeper waters (Environment Canada and Health Canada, 2001; Fischel, 2001; Lewis, 1999).…”
mentioning
confidence: 99%
“…Natural chloride inputs to Colorado streams through precipitation are minor, with concentrations ranging from 0.05 to 0.20 mg/L (Bossong et al, 2003; Stevens, 2001; National Atmospheric Deposition Program/National Trends Network, 2007). In general, background concentrations of chloride in Colorado streams are <5.0 mg/L, depending on the geology of the area, but where human inputs have altered stream chemistry, concentrations have been measured up to 400 mg/L (Musselman et al, 1996; Bossong et al, 2003; Fischel, 2001; Stevens, 2001; Jassby and Goldman, 2003; Capesius et al, 2005). In other areas of North America, higher concentrations (more than 4000 mg/L chloride in winter months) have been measured in various watersheds, presumably from deicing salt inputs (Environment Canada and Health Canada, 2001; Kaushal et al, 2005).…”
mentioning
confidence: 99%