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Tag: Scour (Hydraulic engineering)
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  • Use of Chirp Sub-bottom Acoustic Profiling to Assess the Integrity of the Submerged Portion of the Jonesville Lock and Dam, Located at Jonesville, Louisiana

    Abstract: Jonesville Lock and Dam serves as a critical navigation conduit along the Black River in Louisiana. The structure has previously been impacted by localized scour, leading to concerns regarding the structure’s long-term integrity and an effort to stabilize the structure with targeted fill efforts. Despite these efforts, operators continued to observe localized water and sediment swirls and boils during high-flow events, suggesting that scour is still an ongoing concern. Recent research suggests that shallow acoustic sub-bottom mapping might be able to identify ongoing or historical scour along and underneath concrete structures, and that technique was evaluated at Jonesville. Sub-bottom profiles revealed density anomalies along the inside, eastern wall of the lock structure and underneath both the lock floor and the wall. These anomalies are interpreted to represent an erosional surface created by ephemeral scour events, with subsequent infilling of homogenous, fine-grained sand. The complex geology on which Jonesville is constructed likely contributes to the localized scour observed at this navigation facility.
  • Acoustic Doppler Current Profiler Study of Water and Sediment Movement through a Deep Scour Hole in the Lower Mississippi River

    Abstract: A series of acoustic Doppler current profiler (ADCP) transects were collected through a deep scour hole at the bend near River Mile 60 on the Lower Mississippi River. The measurements were collected during both a low and a high flow. The ADCP results show a 3D flow field through the deep bend. The backscatter intensity of the ADCP measurements indicates the majority of the sediment remains close to the inside of the bed and high in the water column, with minimal concentrations at the bottom of the bend. These findings have implications for numerical sediment transport models, which tend to deposit material at the bottom of deep scour holes like the one in this study
  • Evaluation of a Permeable Dam as an Erosion Control Structure on Coca River, Ecuador

    Abstract: The effort performed here describes the process to evaluate the scour-protection performance of the proposed permeable dam. The US Engineer Research and Development Center, Coastal and Hydraulics Laboratory, built a 1:50 Froude scaled movable bed section model of the permeable dam structure and tested in a specialized flume that simulates regressive erosion propagation. Profiles were collected at various times to track the progression of the scour. Tests evaluated variations of the proposed structure, which included tetrapods, riprap, bridge piers, and longitudinal piles. For the various proposed alternatives, a total of six tests were conducted. The collected profiles show the ability or inability of each alternative and its associated performance. From this analysis, untethered tetrapods could not effectively arrest the local scour around the structure. However, large rock along with invert control stopped the regressive erosion and held the upstream grade.
  • Waterborne Geophysical Investigation to Assess Condition of Grouted Foundation: Old River Control Complex – Low Sill Structure, Concordia Parish, Louisiana

    Abstract: The Old River Low Sill Structure (ORLSS) at the Old River Control Complex (ORCC) in Concordia Parish, LA, is a steel pile-founded, gated reinforced-concrete structure that regulates the flow of water into the Atchafalaya River to prevent an avulsion between the Mississippi River and the Atchafalaya River. A scour hole that formed on the southeast wall of ORLSS during the Mississippi River flood of 1973 was remediated with riprap placement and varied mixtures of self-leveling, highly pumpable grout. Non-invasive waterborne geophysical surveys were used to evaluate the distribution and condition of the grout within the remediated scour area. Highly conductive areas were identified from the surveys that were interpreted to consist mostly of grout. Resistive responses, likely representing mostly riprap and/or sediment, were encountered near the remediated scour area periphery. A complex mixture of materials in the remediated scour area is interpreted by the more gradual transitions in the geophysical response. Survey measurements immediately beneath ORLSS were impeded by the abundance of steel along with the structure itself. The survey results and interpretation provide a better understanding of the subsurface properties of ORLSS.