Browsing Civil and Resource Engineering Faculty Research, Publications and Presentations by Author "ec342416-a32a-4721-bb3e-c5f4c767373b"
Now showing items 1-11 of 11
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Coastal groundwater model calibration using filtered and amplified hydraulic information retained in the freshwater–saltwater interface Postprint
Published Version: Pavlovskii I, Cantelon JA, Kurylyk BL. 2022. Coastal groundwater model calibration using filtered and amplified hydraulic information retained in the freshwater-saltwater interface, Hydrogeology Journal, 30, 1551–1567, DOI: 10.1007/s10040-022-02510-8.Coastal groundwater flow is driven by an interplay between terrestrial and marine forcings. One of the distinguishing features in these settings is the formation of a freshwater lens due to the density difference between ... -
Drone-based characterization of intertidal spring cold-water plume dynamics Postprint
Published Version: KarisAllen, J. J., & Kurylyk, B. L. (2021). Drone-based characterization of intertidal spring cold-water plume dynamics. Hydrological Processes, 35( 6), e14258. https://doi.org/10.1002/hyp.14258 -
Engineering challenges of warming
Kurylyk BL. 2019. Engineering challenges of warming. Nature Climate Change, 9, 807–808. DOI: 10.1038/s41558-019-0612-8. -
Heat: An overlooked tool in the practicing hydrogeologist's toolbox
Kurylyk, B.L. and Irvine, D.J. (2019), Heat: An Overlooked Tool in the Practicing Hydrogeologist's Toolbox. Groundwater, 57: 517-524. doi:10.1111/gwat.12910 -
Interpreting Repeated Temperature‐Depth Profiles for Groundwater Flow
Bense, V. F., Kurylyk, B. L., van Daal, J., van der Ploeg, M. J., & Carey, S. K. (2017). Interpreting repeated temperature‐depth profiles for groundwater flow. Water Resources Research, 53, 8639–8647. https://doi.org/10.1002/2017WR021496 -
Laboratory-scale assessment of a capillary barrier using fibre optic distributed temperature sensing (FO-DTS)
Wu R, Martin V, McKenzie JM, Broda S, Bussière B, Aubertin M, Kurylyk BL. 2020. Laboratory scale assessment of a capillary barrier using Fibre Optic Distributed Temperature Sensing (FO-DTS). Canadian Geotechnical Journal, 57(1): 115-126. DOI: 10.1139/cgj-2018-0283. -
Quantitative guidance for efficient vertical flow measurements at the sediment-water 4 interface using temperature-depth profiles
Irvine DJ, Kurylyk BL, Briggs MA. 2020. Quantitative guidance for efficient vertical flow measurements at the sediment-water interface using temperature-depth profiles. Hydrological Processes, 34(3): 649-661. DOI: 10.1002/hyp.13614. -
Rethinking the use of seabed sediment temperature profiles to trace submarine groundwater flow
Submarine groundwater fluxes across the seafloor facilitate important hydrological and biogeochemical exchanges between oceans and seabed sediment, yet few studies have investigated spatially distributed groundwater fluxes ... -
Snowmelt infiltration and macropore flow in frozen soils: overview, knowledge gaps, and a conceptual framework
Mohammed, A. A., B. L. Kurylyk, E. E. Cey, and M. Hayashi. 2018. Snowmelt Infiltration and Macropore Flow in Frozen Soils: Overview, Knowledge Gaps, and a Conceptual Framework. Vadose Zone J. 17:180084. doi:10.2136/vzj2018.04.0084Macropore flow in frozen soils plays a critical role in partitioning snowmelt at the land surface and modulating snowmelt-driven hydrological processes. Previous descriptions of macropore flow processes in frozen soil do ... -
Theory, tools, and multidisciplinary applications for tracing groundwater fluxes from temperature profiles
Kurylyk BL, Irvine DJ, Bense VF. 2019. Theory, tools, and multidisciplinary applications for tracing groundwater fluxes from temperature profiles. WIREs Water, 6(1): e1329. DOI: 10.1002/wat2.1329Quantifying groundwater fluxes to and from deep aquifers or shallow sediment is a critical task faced by researchers and practitioners from many environmental science disciplines including hydrology, hydrogeology, ecology, ... -
Tracking the subsurface signal of decadal climate warming to quantify vertical groundwater flow rates
Bense, V. F., & Kurylyk, B. L. (2017). Tracking the subsurface signal of decadal climate warming to quantify vertical groundwater flow rates. Geophysical Research Letters, 44, 12,244–12,253. https://doi.org/10.1002/2017GL076015