Research paperObserved mixing lengths in mountain streams
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A novel approach for selecting sampling points locations to river water quality monitoring in data-scarce regions
2019, Journal of HydrologyCitation Excerpt :Moreover, in order to use these procedures, reliable and long-term data collection of water quality must be in place, which is often not feasible in developing country (e.g. Iran). Do et al. (2012), in turn, proposed a new procedure based on Sanders’ procedure (Sanders, 1983) and taking river mixing length (Day, 1977) into account for removing the aforementioned problems. This modified approach was incorporated with pollution potential of each land-use by considering event mean concentration (EMC) and human activities.
Combining a thermal tracer with a transport model to estimate shallow flow velocities
2019, Physics and Chemistry of the EarthA cost-effective and efficient framework to determine water quality monitoring network locations
2018, Science of the Total EnvironmentCitation Excerpt :They proposed that the middle of each segment can be considered as sampling points. We first determined the mixing lengths for each branch or river only by using a single geometric parameter, the mean flow width, using a simple equation, L = 25 W (Day, 1977; Do et al., 2012). where Nj is the total number of segments of river j; lj is the total length of river j; Lj shows river's mixing length of each segment; Wj is the stream width, and N is the total number of potential sampling points of entire river system.
Comparison of thermal, salt and dye tracing to estimate shallow flow velocities: Novel triple-tracer approach
2018, Journal of HydrologyCitation Excerpt :Similar to the thermal tracer, the non-conservative aspect of the salt tracer decreases with flow velocity, since salt transport increases. A major concern when using salt tracers to measure flow velocity is how to ensure that the salt is completely dissolved in the flow so that it can be properly detected (Day, 1977). In the present study, salt was added as an aqueous solution with hot water, which greatly helped the salt to mix in the flow.