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Title: In-phase waves: Their behavior, internal stratification and fabric

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5722629
 [1];  [2]
  1. Brock Univ., St. Catharines, Ontario (Canada). Dept. of Earth Sciences
  2. Freiburg Univ. (Germany). Dept. of Geologie

Experiments were conducted in 0.305m wide, 9m long recirculating sediment flume on a bed of quartz sand (mean diameter of 0.18mm). The experiments included eight runs over the following range of conditions: 0.0605m [<=] depth [<=] 0.068m, 0.51m/s [<=] mean flow velocity [<=] 0.90m/s and 0.63 [<=] Froze Number (F) [<=] 1.1. For F < 0.83 dunes were the dominant bedform and these became longer and lower as F increased. At F = 0.83 the bed was nominally plane but locally and temporarily developed low in-phase waves or dunes. Post-run bed profiles showed symmetrical bedwaves with average length (L) of 0.26m and average height (H) of 0.005m. A complete cycle was characterized by: increased height of bed and water surface waves [r arrow] upstream migration [r arrow] breaking or decay [r arrow] planing of bed surface [r arrow] growth of new in-phase waves (initially migrating downstream and then remaining stationary during continued vertical growth). Each in-phase wave normally behaved independently of other waves although less commonly a breaking wave would trigger breaking of the next downstream wave. For F > 1.0 in-phase waves behaved as described above but a breaking wave would more commonly cause breaking of other waves. With increasing F it became more common for waves to break and rebuild quickly without complete planing of the bed surface. However, complete cycles occurred frequently with the following significant differences: (1) the upstream-migrating antidune developed upstream slopes that approached 25[degree]; (2) planing was accomplished by the rapid migration of a low, asymmetrical bedform through the antidune trough.

OSTI ID:
5722629
Report Number(s):
CONF-9303211-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:2; Conference: 28. annual Geological Society of America (GSA) Northeastern Section meeting, Burlington, VT (United States), 22-24 Mar 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English

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