From modern … Expand. The km long section of the Upper Yellow River at the First Great Bend is comprised of single channel and multiple channel systems that alternate among anastomosing, anabranching, meandering and … Expand. The pattern planform of a river can be considered at vastly different scales, depending upon both the size of the river and the part of the fluvial system that is under consideration Figure 1. Sedimentation in anastomosed river systems; examples from alluvial valleys near Banff, Alberta.
Each reach consists of an interconnected network of low-slope, narrow and deep, straight to sinuous, stable channels that transport coarse sand … Expand. Anastomosed river deposits: modern and ancient examples in Alberta, Canada. The anastomosed fluvial system is proposed as an environment of deposition for some over-bank deposits, coal, and coarse channel sediments sandstone and conglomerate in the Rocky Mountain molasse … Expand. Sinuosity of Alluvial Rivers on the Great Plains.
Data on the morphologic and sediment characteristics of stable alluvial rivers of the Great Plains were collected at 50 cross sections. The channel patterns of these rivers were classified into five … Expand. Anatomy of an avulsion. The Cumberland Marshes in east-central Saskatchewan, Canada, occupy over km2 and contain a variety of active and abandoned fluvial features, including straight to sinuous isolated channels, … Expand.
Contemporary and palaeo channel patterns and the late quaternary stratigraphy of Cooper Creek, Southwest Queensland, Australia. Braided and anastomosing channels make up two major coexistent networks in the mud-dominated fluvial system of Cooper Creek, Southwest Queensland.
The floodplain is characterized by a system of mud … Expand. Effect of vegetation on lateral migration of anastomosed channels of a glacier meltwater river. A series of experiments were performed on bank materials of anastomosed channels in flood-plain silt deposits in the Alexandra Valley in Banff Park, Alberta, to determine the effect of vegetation … Expand. Morphology and recent sediments of the lower anastomosing reaches of the Attawapiskat River.
The Attawapiskat River is one of the major low-gradient rivers which cross the flat wetlands of the Hudson Bay Lowland. It has a nival regime leading to strong, short-duration spring floods during … Expand. On the origin and characteristics of river channel patterns. Abstract A theory of the origin of channel patterns is developed and enables predictions of relationships and characteristics which are tested.
The reference scenario comprises one base station in Tx or Rx mode, a spatial random distribution of nodes resp. To derive the fundamental limits of this model, a spatial discretization is first proposed to obtain an equivalent BC or MAC. Then, a specific sequence of discretized spaces is defined to refine infinitely the approximation. The uniform capacity defined as the maximal symmetric achievable rate is also computed. Add Another. Standard Search Advanced Search. Limit to results with full text.
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Continuum-continuum coupling and polarization potentials for weakly bound systems. Canto, L. Abstract Abstract. For this purpose, we compare cross sections for complete fusion, breakup, and elastic scattering evaluated by continuum discretized coupled channel CDCC calculations, including and not including these couplings.
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