Jared Suchan

Permanent URI for this collectionhttps://hdl.handle.net/10294/14885

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Now showing 1 - 6 of 6
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    Using a network of core samples to explore hydroclimatic proxy relationships within the sediments of an alpine, glacier-fed lake
    (Copernicus Publications, 2015) Hodder, Kyle; Suchan, Jared
    The attached file is the open access abstract from (Geophysical Research Abstracts, Vol. 17, EGU2015-7224, 2015, EGU General Assembly 2015, © Author(s) 2015. Published by Copernicus Publications. This is open access abstract is available under the Creative Commons Attribution 3.0 License (CC BY 3.0) license (https://creativecommons.org/licenses/by/3.0/). This abstract is available at https://meetingorganizer.copernicus.org/EGU2015/EGU2015-7224.pdf.
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    Controlled photogrammetry system for determination of volume and surface features in soils
    (Elsevier, 2021-04-28) Suchan, Jared; Azam, Shahid
    Quantitative and qualitative determination of total volume and surface features of a soil specimen is important in geotechnical engineering. Available methods suffer from a variety of shortcomings such as sample disturbance, equipment calibration, and lack of precision. The Controlled Photogrammetry System (CPS) is based on Structure-from-Motion (SfM) to capture a series of photographs and transform the images into a referenced three-dimensional model.
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    Development of BAS2 for determination of evaporative fluxes
    (Elsevier, 2021-06-24) Suchan, Jared; Azam, Shahid
    Accurate determination of evaporative flux from water surfaces and liquid containing porous media is critical for geotechnical and geoenvironmental applications. Laboratory simulations can isolate the various parameters influencing evaporative fluxes. However, most simulators capture selected surface and atmospheric conditions, and published literature generally provide limited information on the development and operation of the instruments. The new simulator adequately captures a wide range of relevant field parameters, maintains controlled conditions over the required testing time, utilizes readily available components for modular fabrication, and facilitates operational efficiency between individual modules.
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    Determination of Evaporative Fluxes Using a Bench-Scale Atmosphere Simulator
    (Multidisciplinary Digital Publishing Institute, 2021-01-01) Suchan, Jared; Azam, Shahid
    An accurate determination of evaporative fluxes is critical for efficient water management in semi-arid climates such as in the Canadian Prairies. The main achievements of this research are the design and operation of a bench-scale atmosphere simulator, performance evaluation using selected weather scenarios pertaining to regional atmospheric conditions, validation using established empirical correlations, and estimation of evaporation rates and the amount for a typical local water body. Results indicate that the measured data achieved the target values for the various parameters and the data were found to be stable during the 3-h test duration. The vapour flux was found to have large variation during summer (0.120 g∙s−1∙m−2 during the day and 0.047 g∙s−1∙m−2 at night), low variation during spring (0.116 g∙s−1∙m−2 during the day and 0.062 g∙s−1∙m−2 at night), and negligible change during fall (0.100 g∙s−1∙m−2 during the day and 0.076 g∙s−1∙m−2 at night). The measured vapour flux was generally within one standard deviation of the equality line when compared with that predicted by both the mass-transfer equations and the combination equations. The average evaporation ranged from 4 mm∙d−1 to 8 mm∙d−1 during the day and decreased to 1 mm∙d−1 to 3 mm∙d−1 at night. The 24-h evaporation was found to be 8 ± 1 mm∙d−1 from late April through late October. Likewise, the cumulative annual evaporation was found to be 1781 mm, of which 82% occurs during the day and 18% at night.
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    Effect of Salinity on Evaporation from Water Surface in Bench-Scale Testing
    (Multidisciplinary Digital Publishing Institute, 2021-07-29) Suchan, Jared; Azam, Shahid
    Freshwater and hypersaline lakes in arid and semi-arid environments are crucial from agri- cultural, industrial, and ecological perspectives. The purpose of this paper was to investigate the effect of salinity on evaporation from water surfaces. The main achievement of this research is the successful capture of simulated climate–surface interactions prevalent in the Canadian Prairies using a custom-built bench-scale atmospheric simulator. Test results indicated that the evaporative flux has a large variation during spring (water/brine: 1452/764 10−4 g·s−1·m−2 and 613/230 × 10−4 g·s−1·m−2 night) and summer (1856/1187 × 10−4 g·s−1·m−2 day and 1059/394 × 10−4g·s−1·m−2 night), and small variation in the fall (1591/915 × 10−4 g·s−1·m−2 and 1790/1048 × 10−4 g·s−1·m−2 night). The primary theoretical contribution of this research is that the evaporation rate from distilled water is twice that of saturated brine. The measured data for water correlated well with mathematical estimates; data scatter was evenly distributed and within one standard deviation of the equality line, whereas the brine data mostly plotted above the equality line. The newly developed 2:1 water–brine correlation for evaporation was found to follow the combination equations with the Monteith model best matching the measurements.
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    Datasets for the Determination of Evaporative Flux from Distilled Water and Saturated Brine Using Bench-Scale Atmospheric Simulators
    (Multidisciplinary Digital Publishing Institute, 2021-12-22) Suchan, Jared; Azam, Shahid
    Evaporation from fresh water and saline water is critical for the estimation of water budget in the Canadian Prairies. Predictive models using empirical field-based data are subject to significant errors and uncertainty. Therefore, highly controlled test conditions and accurately measured experimental data are required to understand the relationship between atmospheric variables at water surfaces. This paper provides a comprehensive dataset generated for the determination of evaporative flux from distilled water and saturated brine using the bench-scale atmospheric simulator (BAS) and the subsequently improved design (BAS2). Analyses of the weather scenarios from atmospheric parameters and evaporative flux from the experimental data are provided.