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  1. NTU Theses and Dissertations Repository
  2. 理學院
  3. 地理環境資源學系
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/28742
完整後設資料紀錄
DC 欄位值語言
dc.contributor.advisor李建堂(Cheing-Tung Lee)
dc.contributor.authorCheng-Wei Kuoen
dc.contributor.author郭鎮維zh_TW
dc.date.accessioned2021-06-13T00:20:24Z-
dc.date.available2007-07-31
dc.date.copyright2007-07-31
dc.date.issued2007
dc.date.submitted2007-07-25
dc.identifier.citation參考文獻
汪靜明 (1999) 大甲溪水資源環境教育,台北:經濟部水資局。
翁宇能 (1998) 自然生態河川低水流量斷面之合理型態研究,國立中興大學水土保持學系碩士論文。
張明雄 (2003) 台北縣坪林鄉北勢溪魚類資源保育利用芻議,溪流環境會訊,7: 1-10.
經濟部中央地質調查所 (2000) 五萬分之一地質圖-圖幅:新店。
經濟部水利署 (2006) 水文水資源資料管理供應系統,http://gweb.wra.gov.tw/wrweb/ [2006/4/5]。
賴建盛 (1996) 防砂壩對櫻花鉤吻鮭物理棲地影響之研究,國立台灣大學地理學研究所碩士論文。
Carling, P. A. (1991) An appraisal of the velocity-reversal hypothesis for stable riffle-pool sequences in the River Severn, England, Earth Surface Processes and Landforms, 16: 19-31.
Clifford, N. J. (1993) Differential bed sedimentology and the maintenance of riffle- pool sequences, Catena, 20: 447-468.
Clifford, N. J. and Richards, K. S. (1992) The reversal hypothesis and the main- tenance of riffle-pool sequence. Lowland rivers: geomorphological perspectives, Chichester: Wiley, 43-70.
Hirsch, P. J. and Abrahams, A. D. (1981) The properties of bed sediments in pools and riffles, Journal of Sedimentary Petrology, 51: 757–760.
Iseya, F. and Ikeda, H. (1987) Pulsations in bedload transport rates induced by a longitudinal sediment sorting: a flume study using sand and gravel mixtures, Geografiska Annaler, 69A: 15-27.
Keller, E. A. (1971) Areal sorting of bed load material; the hypothesis of velocity reversal, Geological Society America Bulletin, 82: 753-756.
Keller, E. A. and Melhorn, W. N. (1978) Rhythmic spacing and origin of pools and riffles, Geological Society of America Bulletin, 89: 723-730.
Leopold, L. B., Wolman, M. G. and Miller, J. P. (1964) Fluvial processes in geomorphology, San Francisco.
Lisle, T. S. (1982) Effects of aggradation and degradation on riffle-pool morphology in nature gravel channels, Northwestern California, Water Resources research, 18 (6): 1643-1651.
Lisle, T. S. and Hilton, S. (1992) The volume of fine sediment in pools: an index of sediment supply in gravel-bed stream, Water Resources Bulletin, 28(2): 371-383.
Miline, J. A. (1982) Bed-material size and the riffle-pool sequences, Sedimentology, 29:267-278.
Miline, J. A. (1982) Bed forms and bend-arc spacings of some coarse-bedload channels in Upland Britain, Earth Surface Processes and Land forms, 7: 227- 240.
Richards, K. S. (1976) The morphology of riffle-pool sequences, Earth Surface Processes and Land forms, 1: 71-88.
Richards, K. S. (1982) River: Form and process in alluvial channels, London, Methuen.
Robert, A. (1997) Characteristics of velocity profiles along riffle-pool sequences and estimates of bed shear stress, Geomorphology, 19: 89-98.
Robert, A. (2003) River Processes: an Introduction to Fluvial Dynamics, London, Arnold.
Rimmer, D. M., Paim, U. and Saunders, R. L. (1983) Changes in the selection of microhabitat by juvenile Atlantic salmon at the summer-autumn transition un a small river. Canadian Journal of Fisheries and Aquatic Science, 41: 469- 475.
Rosgen, D. L. (1985) A stream classification system, In: Riparian ecosystems and their management, Colorado, 91-95.
Sear, D.A. (1996) Sediment transport process in pool-riffle sequences, Earth surface processes and landforms, 21: 241-262.
Thompson, D. M., Wohl, E. E. and Jarrett, R. D. (1996) A revised velocity-reversal and sediment-sorting model for a high-gradient, pool-riffle stream, Physical Geography, 17: 142-156.
Thompson, D. M. and Hoffman, K. S. (2001) Equilibrium pool dimensions and sediment-sorting patterns in coarse-grained, New England channels, Geomorphology, 38: 301-316.
Wolman, M.G. (1954) A method of sampling coarse river-bed material, Transactions of the American, Geophysical Union, 35(6): 951-956.
Wohl, E. E., Vincent, K. R. and Merritts, D. J. (1993) Pool and riffle characteristics in relation to channel gradient. Geomorphology, 6: 99-110.
Yalin, M. S. (1971) Inception of sediment transport, Journal of the Hydraulic Division, American Society of Civil Engineers, 105: 1433-1443.
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/28742-
dc.description.abstract摘 要
淺瀨-深潭序列的研究近十幾年來因河川復育計畫而更加受到重視,在河床底質特性方面,一般認為淺瀨的粒徑較大且淘選度較佳,但並非所有研究都有此結論。台灣在這方面的基礎採樣研究較為缺乏,因此本文的目的是藉由採樣調查來比較淺瀨與深潭的河床底質特性,並討論底質分布與河床地形變化的關係,研究區選擇台北縣坪林鄉金瓜寮溪河段。本研究首先進行河段型態以及兩岸環境的調查,藉以探討兩岸環境對於淺瀨與深潭發育的影響。之後以數目網格採樣法於十個淺瀨-深潭對進行採樣,並同時測量河床地形,藉以探討河床縱剖面與粒徑分布的變化,並比較淺瀨與深潭在b軸粒徑、淘選度、圓度及扁平度等底質特性上的差異。
研究結果顯示兩岸環境局部性地影響了淺瀨-深潭的地形發育,特別是河岸岩盤或河道阻礙物,均有利於深潭的形成與發育。粒徑分布與河床縱剖面變化的結果,顯示潭心的粒徑通常較為細小,延伸至潭尾反而有略增的趨勢,而發育良好的淺瀨與深潭,其縱剖面變化與粒徑大小有較佳的對應關係。底質特性比較方面,有九個樣區的淺瀨粒徑大於深潭,其中有五個達顯著水準 (α=0.05);淘選度及扁平度則沒有一致的結論,圓度值則是淺瀨較深潭高。雙變數圖的分析結果,以粒徑平均數對應偏態值的圖最能區隔出淺瀨與深潭的特性。粒徑分布累積百分位數圖則顯示淺瀨的φ50分布明顯較深潭集中,顯示不同深潭間的河床底質粒徑分布有蠻大的差異。
zh_TW
dc.description.abstractAbstract
The studies of riffle-pool sequence have developed in the 1960s. In the last few years, because the ideas of river restoration start, the studies of riffle-pool become more important. In this research area, the river bed morphology of riffle-pool sequence and the differences in characteristics of bed materials always interest the researchers. There is concurrently academic and application value in bed materials research. The studies of streams in Taiwan comparatively lack the foundation investigations in bed materials, so this research hopes to understand the differences in bed materials characteristic between riffles and pools by sampling investigation. The purpose of this study is to compare the bed materials characteristic between riffles and pools, and to discuss the relationships between bed materials characteristic and the river bed morphology. The river bed materials characteristic contains the particle size, flatness and roundness. The research area - ChinKuaLiao stream - is in the PingLin Township in Taipei County.
The results reveal that the bed longitudinal variations and the particle size have better corresponding relations in well-growth riffle-pool morphology. By the T- test, particle sizes in pools are coarser than riffles in the five of ten sample zones. Flatness is varies along with the river channel characteristic, and roundness in most riffles is bigger than pool. In the bivariate scatter plots results, it is most clear to separate the characteristic of riffles and pools by the mean particle size vs. skewness. In the cumulative size frequency distributions plots, the φ50 distribution in riffles is obviously more convergence than pools. This reveals there are great differences in bed material size distribution between pools.
en
dc.description.provenanceMade available in DSpace on 2021-06-13T00:20:24Z (GMT). No. of bitstreams: 1
ntu-96-R92228007-1.pdf: 1440570 bytes, checksum: 469b6460b41d9db443e13519f9bcadf0 (MD5)
Previous issue date: 2007
en
dc.description.tableofcontents目 錄
口試委員審定書………………………………………………………………………i
謝辭…………………………………………………………………………………...ii
中文摘要……………………………………………………………………………..iii
英文摘要……………………………………………………………………………..iv
第一章 緒論 ............................................................................................................. 1
第一節 研究動機與目的 ..................................................................................... 1
第二節 研究區概述 ............................................................................................. 4
第二章 文獻回顧 ..................................................................................................... 9
第一節 河段型態的分類與定義 ......................................................................... 9
第二節 淺瀨與深潭生成的原因 ....................................................................... 11
第三節 淺瀨與深潭的河床底質特性 ............................................................... 16
第四節 河床底質採樣方法 ............................................................................... 20
第三章 研究方法 ................................................................................................... 23
第一節 研究流程 ............................................................................................... 23
第二節 野外測量方法 ....................................................................................... 24
第三節 資料分析方法 ....................................................................................... 30
第四章 結果與討論 ............................................................................................... 32
第一節 河段型態與兩岸環境的關係 ............................................................... 32
第二節 淺瀨-深潭底質分布與河床地形變化的關係 ...................................... 37
第三節 淺瀨-深潭河床底質之比較 .................................................................. 54
第五章 結論 ........................................................................................................... 59
參考文獻 ................................................................................................................... 62
dc.language.isozh-TW
dc.title淺瀨與深潭的河床底質特性研究—以金瓜寮溪中游河段為例zh_TW
dc.titleThe Study of Bed-Materials of Riffle and Pool-A Case Study in Chinkualiao Streamen
dc.typeThesis
dc.date.schoolyear95-2
dc.description.degree碩士
dc.contributor.oralexamcommittee林俊全(Jiun-Chuan Lin),徐美玲(Mei-Ling Hsu)
dc.subject.keyword淺瀨,深潭,河床底質,河床地形,zh_TW
dc.subject.keywordriffle,pool,bed materials,river bed morphology,en
dc.relation.page64
dc.rights.note有償授權
dc.date.accepted2007-07-27
dc.contributor.author-college理學院zh_TW
dc.contributor.author-dept地理環境資源學研究所zh_TW
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