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Physical Modelling in Fluvial Geomorphology

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PHYSICAL MODELLING IN FLUVIAL GEOMORPHOLOGY 247<br />

1. Incorporation of more realistic model parameters <strong>in</strong>to FSM studies, such as flood<br />

hydrographs, f<strong>in</strong>e-gra<strong>in</strong>ed sediment and cohesion;<br />

2. Development and implementation of methodology to better quantify flow, sediment<br />

transport and morphological change;<br />

3. Additional and more complete test<strong>in</strong>g/verification of FSMs aga<strong>in</strong>st their prototype<br />

conditions.<br />

Although unscaled or 'analogue' models can shed much light on large temporal and<br />

spatial scale processes and products, these studies must always be considered <strong>in</strong> terms of<br />

their underly<strong>in</strong>g simplifications and drawbacks and must not be <strong>in</strong>terpreted as true scale<br />

models. Such 'analogue' models may <strong>in</strong>creas<strong>in</strong>gly be used to <strong>in</strong>vestigate the role of<br />

allocyclic factors on sedimentation, such as local tectonic and base level controls, but their<br />

departure from true scal<strong>in</strong>g perhaps demands more complete field verification than more<br />

rigidly scaled Froude scale models.<br />

ACKNOWLEDGEMENTS<br />

Many of the ideas expressed <strong>in</strong> this chapter have developed from work sponsored over the<br />

past six years by BP Exploration. We are grateful to BP for award of a Ph.D. studentship<br />

to Jeff Peakall and grants to establish the scale modell<strong>in</strong>g/aggradation facility at Leeds.<br />

This modell<strong>in</strong>g has also been supported by a grant from the Royal Society and more<br />

recently fund<strong>in</strong>g from NERC (GR9/01640) and ARCO Oil (USA) to Ashworth and Best.<br />

Marcelo Garcia and Bruce Rhoads provided helpful suggestions to improve the clarity of<br />

this contribution. Peter Ashmore k<strong>in</strong>dly supplied orig<strong>in</strong>al photographs of his flume<br />

experiments for Figures 9.9 and 9.11.<br />

REFERENCES<br />

Allen, J.R.L. 1982. Sedimentary Structures: Their Character and <strong>Physical</strong> Basis, Elsevier,<br />

Amsterdam, 539 pp..<br />

Anastasi, G. 1984. Simulaz<strong>in</strong>oe di regime torrentizio su modello fisico a fondo mobile mediante<br />

micro-computer, <strong>in</strong> Memorie XIX convegno di idraulica e construczioni idrauliche, Pavia, Italy,<br />

6-8 September 1984, Paper A9, 10 pp.<br />

ASCE 1942. Hydraulic Models, The American Society of Civil Eng<strong>in</strong>eers Manual of Practice, 25,<br />

American Society of Civil Eng<strong>in</strong>eers, New York, 110 pp.<br />

Ashmore, P.E. 1982. Laboratory modell<strong>in</strong>g of gravel braided stream morphology, Earth Surface<br />

Processes and Landforms, 7, 201-225.<br />

Ashmore, P.E. 1988. Bedload transport <strong>in</strong> braided gravel-bed stream models, Earth Surface<br />

Processes and Landforms, 13, 677-695.<br />

Ashmore, P.E. 1991a. Channel morphology and bed load pulses <strong>in</strong> braided, gravel-bed streams,<br />

Geografiska Annaler, 68, 361-371.<br />

Ashmore, RE. 1991b. How do gravel-bed rivers braid? Canadian Journal of Earth Sciences, 28,<br />

326-341.<br />

Ashmore, RE. 1993. Anabranch confluence k<strong>in</strong>etics and sedimentation processes <strong>in</strong> gravel-braided<br />

streams, <strong>in</strong> Braided Rivers, edited by J.L. Best and C.S. Bristow, Geological Society Special<br />

Publications, 75, pp. 129-146.<br />

Ashmore, RE., Ferguson, R.I., Prestegaard, K.L., Ashworth, P.J. and Paola, C. 1992. Secondary<br />

flow <strong>in</strong> anabranch confluences of a braided, gravel-bed stream, Earth Surface Processes and<br />

Landforms, 17, 299-311.

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