Downstream changes in bed meterial size and shape characteristics in a small upland stream: Cwm Treweryn, in South Wales

Bu çalışmanın amacı, Galler'in Brecon Beacons yöresinde küçük bir akarsu olan Cwm Treweryn'in yatağı boyunca yatak yükü (çakıl boyutundaki iri unsurlar (>32 mm)) malzemesinin şekil ve boyut özelliklerinin incelenmesidir, Bu amaçla, tali kollar dahil, yatak boyunca toplam 21 lokasyonda yatak yükünü oluşturan malzeme incelenmiştir. Her lokasyonda çapı (b-ekseni) 32 mm'den büyük olan toplam 100 çakıl örneği alınmıştır. Daha önce yapılan bir çok araştırma, aşınma ve seçici taşınmadan dolayı, akarsu yatağı boyunca (kaynaktan ağıza doğru) yatak yükünü oluşturan unsurların boyutlarının genellikle küçülme eğiliminde olduğu ve malzemenin yuvarlaklığının arttığını göstermiştir. Bununla birlikte, Cwm Treweryn nehrinde yapılan ölçümler, anılan modeldeki basitliğin aksine, yatak yükünü oluşturan unsurlar şekil ve boyut özellikleri bakımından daha karmaşık ve düzensiz bir değişim örneği göstermiştir. Yatak malzemesinin boyut özellikleri 21 lokasyonda oldukça geniş bir dağılım ve dolayısıyla zayıf bir seçici taşınma örneği göstermektedir. Bütün yatak boyunca, disk şekilli çakılların birinci ve bıçak sırtı şeklindeki çakılların da ikinci büyük oranda olması ise, havzada hakim litoloji olan Old Red kumtaşının yapısal ve litolojik özelliklerine bağlanmıştır. Sonuç olarak, önceki çalışmalarla karşılaştırıldığında, Cwm Traweryn nehrinde yatak yükünü oluşturan unsurların boyut ve şekilsel özelliklerinin (yuvarlaklık ve küresellik) akarsu yatağı boyunca küçük bir değişim gösterdiği saptanmıştır. Bu durum değişik faktörlerin biraradaki etkisine bağlanabilir. Bunlardan bazıları; yatak yükünü oluşturan malzemenin litolojik özellikleri (Old Red kumtaşı), akarsu boyunun kısalığı ve akarsuya yatak ve teraslardan eklenen yeni malzemedir.

Dağlık bir bölgede, kısa bir akarsu mecrası boyunca yatak malzemesi yükünün şekil ve boyut özelliklerinin değişimi: Cwm Treweryn Nehri, Güney Galler

The aim of this study is to investigate the downstream changes in bedload clast size and shape along the Cwm Treweryn stream, Brecon Beacons, South Wales. A total of 21 sites (including six tributary entry points) were used to evaluate Downstream changes in bedload size and shape (form, roundness and sphericity) characteristics. At each sites, 100 surface clasts with b axes (intermediate) greater than 32 mm were sampled. Many of the earlier studies found that, due to abrasion and sorting processes, particle size decreases and roundness increases in a downstreahl direction. However, in contrast to these studies, the Cwm Treweryn stream does not conform this simple dowhstream pattern, instead shows irregular and complex changes in both size and shape along the chan-nel. In terrflè of size characteristics, bed material at all 21 sites represented a wide range of size fractions and hence poor sorting. The dominance of disc-shaped clasts with blades the second most frequent shape along the entire channel length is attributed to the structural and lithological characteristics of the predominance of Old Red Sandstone. As a result, comparatively small downstream changes were determined in bedload clast size and shape (roundriëss, sphericity) and these changes are attributed to the combined effect of different factors, including the lithology of the bedload (Old Red Sandstone), the short river course, and occasional inputs of angular fresh material frorn the channel banks and bed.

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Adams, J., 1978. Data from New Zealand pebble ab rasion studies. New Zealand Journal of Scien ce, 21, 607-610.

Barclay, W.J., Taylor, K., and Thomas, L.P., 1988. Geology of the South Wales coalfield, Part V. The country around Merthyr Tydfil. Memoirs of the British Geological Survey, Her Majesty’s Stationery Office, London, pp. 3-6.

Cailleux, A., 1947. L’indice d’emousse: Definition et premiere application: Comptes Rendus de Science. Société Geologique de France, 250- 252.

Bradley, W. C., Fahnestock, R.K., and Rowekamp, E.T., 1972. Coarse sediment transport by flo od flow on Knik River, Alaska. Geological So ciety of America Bulletin, 83, 1261-1284.

Brierley, G.J., and Hickin, E.J., 1985, The downstre am gradiation of particle sizes in the Squ amish River, British Colombia. Earth Surface Processes and Landforms, 10, 597-606.

Carling, P.A., Kelsey, A., and Glaister, M.S., 1992, Ef fect of bed roughness, particle shape and ori entation on initial motion criteria. Dynamics of Gravel-bed Rivers, Billi, P., Hey, R.D., Thorne, C.R. & Taconni, P. (eds), Wiley, Chicester, 23- 39 pp.

Cui, Y., Parker, G., and Paola, C., 1996. Numerical simulation of aggradation and downstream fi ning. Journal of Hydraulic Research, 34, 185- 204.

Davis, W.M., 1899. The geographical cycle. Geog raphical Journal, 14, 481-504.

Dawson, M., 1988. Sediment size variation in a bra ided reach of the Sunwapta River, Alberta, Canada. Earth Surface Processes and Land forms, 13, 599-618.

Ergenzinger, P., Schmidt, K.H., and Busskamp, R., 1989. The Pebble Transmitter System (PETS) first result of a technique for studying coarse material erosion, transport and deposition. Ze itschrift fur Geomorphologie N.F., 33, 503- 508.

Ergenzinger, P., and Schmidt, K.-H., 1990. Stochas tic elements of bedload transport in a step-po ol mountain river. in Hydrology in Mountaino us Regions. II. Artificial Reservoirs; Water & slopes. Proc. of Symposia, Lausanne, August, IAHS Publication, 194, 39-46.

Ferguson, R.I., Hoey, T.B., Wathen, S.J., Werrity, A., Hardwick, R.I., and Sambrook Smith, G.H., 1998. Downstream fining of river gravels: in tegrated field, laboratory and modelling study. Gravel Bed Rivers in the Environment, Kinge man, P.C, Beschta, R.L., Komar, P.D. and Bradley, J.B. (eds), Water Resources Publica tions, Colorado, U.S.A. 85-113 pp.

Geode, A., 1975. Downstream changes in pebble morphometry of the Tambo River, Eastern Victoria. Journal of Sedimentary Petrology, 45, 704-718.

Gilbert, G.K., 1877. Report on the geology of the Henry Mountains. USGS Professional Paper, 160 pp.

Gilbert, G.K., 1914. The transportation of debris by flowing water. USGS Professional Paper 86. 263 pp.

Gregory, K.J., and Cullingford, R.A., 1974. Lateral va riation in pebble shape in northwest Yorkshire. Sedimentary Geology, 12, 237-248.

Helley, E.J., 1969. Field measurement of the initation of large motion in Blue Creek near Klamath, California. United States Geological Survey Professional paper 256-G.

Hoey, T.B., and Ferguson, R.I., 1994. Numerical mo delling of downstream fining by selective transport in gravel bed rivers: model develop ment and illustration. Water Resources Rese arch, 30, 2251-2260.

Hollerman, P., 1971. Zurundungsmessen an Ablage rungen in Hochgebirge: Zeitschrift fur Ge omorphologie, Supplementband, 205-237.

Hovermann, J., and Poser, H., 1951. Morphometrisc he und morphologische Scother-analysen. Proceedings of the 3rd International Congress on Sedimentation, 135-156.

Knighton, A.D., 1980. Longitudinal changes in size and sorting of stream-bed material in our Eng lish Rivers. Geological Society of American Bulletin, 91, 55-62.

Knighton, A.D., 1982. Longitudinal changes in the si ze and shape of stream bed material: eviden ce of variable transport conditions. Catena, 9, 25-34.

Knighton, D.A., 1984. Fluvial forms and processes. Edward Arnold, London, pp. 217.

Kodama, Y., 1992. Effect of abrasion on downstream gravel-size reduction in the Waterase River, Japan: fieldwork and laboratory experiments. Environmental Research Center Papers, The University of Tsukuba, Japan.

Komar, P.D., and Li, Z., 1986. Pivoting analyses of the selective entrainment of sediments by shape and size with application to gravel threshold. Sedimentology, 33, 425-436.

Krumbein, W.C. 1941. The effect of abrasion on the size, shape, and roundness of rock fragments. Journal of Geology, 64, 336-368.

Krumbein, W.C., 1942. Settling-velocity and flume behavior of non-spherical particles. Transacti ons of the America Geophysical Union, 23, 621-632.

Kuenen, P.H., 1956. Experimental abrasion of pebb les. 2. Rolling by current. Journal of Geology, 64, 336-368.

Mackin, J.H., 1948. Concept of the graded river. Ge ological Society of America Bulletin, 59, 463- 512.

McEwen, L.J., and Matthews, J.A., 1998. Channel form, bed material and sediment sources of the sprongdola, Southern Norway: evidence for a distinct periglacio-fluvial system. Geogra fiska Annaler, 80 A, 17-35.

Mills, H.H., 1979. Downstream rounding of pebbles-a quantitative review. Journal of Sedimentary Petrology, 49, 295-302.

Ouma, J.P.B.M., 1967. Fluviatile morphogenesis of roundness: the Hacking River, New South Wales, Australia: International Assocation. of Scientific Hydrology Publication, 75, 319-344.

Paola, C., and Seal, R., 1995. Grain size patchiness as a couse of selective deposition and downstream fining. Water Resources Rese- arch, 31, 1395-1407.

Parker, G., 1991. Selective sorting and abrasion of ri ver gravel, 1: Theory. Journal of Hydraulic En gineering, 117, 131-149.

Pizzuto, J.E., 1995. Downstream fining in a network of gravel-bedded rivers. Water Resources Re search, 31, 753-759.

Plumley, W.J., 1948. Blackhills terrace gravels: a study in sediment transport. Journal of Ge ology, 56, 526-577.

Rice, S., and Church, M., 1998. Grain size along two gravel-bed rivers: statistical variation, spatial pattern and sedimentary links. Earth Surface Processes and Landforms, 23, 345-363.

Russell, R. D., 1939. Effects of transportation on se dimentary particles, In P.D. Trask, (ed.) Re cent marine sediments. American Association of Petroleum Geologists, Tulsa, 32-37.

Schmidt, H.K. and Gintz, D., 1995. Results of bedlo- ad tracer experiments in a mountain river. Ri- ver Geomorphology. In E.J. Hickin (ed.), River Morphology, John Wiley & Sons Ltd, Chiches- ter.

Shaw, J., and Kellerhals, R., 1982. The composition of recent alluvial gravels in Alberta River beds. Alberta Research Council, Edmonton, Bulle- tin, 41, 151 pp.

Sneed, E.D., and Folk, R.L., 1958. Pebbles in the lo- wer Colorado River, Texas: a study in particle morphogenesis. Journal of Geology, 40, 443- 451.

Strenberg, H. 1875. Untersuchungen uber Langen- und Querprofil geschiebefuhrender Flusse. Zeitschrift fur Bauwesen, 25, 483-506.

Unrug, R., 1957. Recent transport and sedimentation of gravels in the Dunajec valley (western Car- pathians). Acta Geologica Polonica, 7, 217- 257.

Walsh, R.P.D., and Hudson, R.N., 1980. The floods of River Tawe of late December 1979. A report commissioned by Inco Europe Ltd, Clydach, Department of Geography, University College of Swansea, 184 pp.

Wentworth, C.K., 1919. A laboratory and field study of cobble abrasion. Journal of Geology, 27, 507- 522.

Wentworth, C.K., 1922. A field study of the shapes of river pebbles. U.S. Geological Survey Bulletin, 730-C, 103-114.

Werritty, A., 1992. Downstream fining in a gravel bed river in Southern Poland: lithological controls and the role of abrasion. In P. Billi, C.R. Thor- ne, and P. Taconni (eds), Dynamics of Gravel Bed Rivers, Wiley, Chichester, 333-346.

Wolman, M.G., 1954. A method of sampling coarse ri- ver-bed material. Transactions of the Ameri- can Geophysical Union, 35, 951-955.

Zingg, T.H., 1935. Beitrag zur Schotteranalyse: Schweizische Mineralogie und Petrographie Mitteilungen, 15, 39-140.
Yerbilimleri-Cover
  • ISSN: 1301-2894
  • Başlangıç: 1976
  • Yayıncı: Hacettepe Üniversitesi Yerbilimleri Uygulama ve Araştırma Merkezi