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Monitoring the effects of knickpoint erosion on bridge pier and abutment structural damage due to scour.

File Language:
English


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  • NTL Classification:
    NTL-HIGHWAY/ROAD TRANSPORTATION-Bridges and Structures
  • Abstract:
    The goal of this study was to conduct a field-oriented evaluation, coupled with advanced laboratory techniques, of channel ; degradation in a stream of the Deep Loess Region of western Iowa, namely Mud Creek. The Midwestern United States is ; an ideal place for such a study considering that ~$1 Billion of infrastructure and farmland has been lost recently to channel ; degradation. A common form of channel degradation in this region is associated with the formation of knickpoints, which ; naturally manifest as short waterfalls within the channel that migrate upstream. As flow plunges over a knickpoint face, ; scouring of the downstream bed creates a plunge pool. This downcutting increases bank height, facilitating bank failure, ; stream widening, and damage to critical bridge infrastructure. We conducted a state-of-the-art geotechnical analysis of the ; sediments from the knickpoint face, plunge pool, and adjacent stream banks to determine the areas of the streambed near ; the bridge infrastructure that favor knickpoint propagation. Soil characterization using particle size distributions and ; Gamma Spectroscopy identified a stratigraphic discontinuity at the elevation where the knickpoint forms. An automated ; surveillance camera was established to monitor the location of the knickpoint face relative to a fixed datum and provide a ; first-order approximation of its migration rate, which was approximately 0.9 m over a 248-day study period. Surveys ; conducted of the stream reach also facilitated information about knickpoint migration. Flow measurements using Largescale ; Particle Image Velocimetry were conducted during the study to understand the hydrodynamic conditions at the site. ; The results of this research will assist local and federal transportation agencies in better understanding the following: (1) ; principal geotechnical and hydrodynamic factors that control knickpoint propagation, (2) identify necessary data for ; extraction and analysis to predict knickpoint formation, (3) provide mitigation measures such as grade control structures ; (e.g., sheet-pile weirs, bank stabilization measures) near bridge crossings to control the propagation of knickpoints and ; prevent further damage to downstream infrastructure.
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    PDF
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    Filetype[PDF - 3.21 MB]
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    urn:sha-512:5c8572f4afe42ff3cbbd991b09ab0963dd53e2cf9bb559ea0f503c0b7396213e4d8d59123b61881c04dfe974269974c1e9f9d24446e8035662e4a7d194a1e127
File Language:
English
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