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題名:花蓮溪河谷沖積扇之自然環境、土地利用及其土石災害之研究
書刊名:國立臺灣大學理學院地理學系地理學報
作者:陳紫娥 引用關係
作者(外文):Chen, Zue-er
出版日期:2000
卷期:27
頁次:頁55-69
主題關鍵詞:沖積扇自然環境土地利用土石災害Fluvial fansNatural environmentLand useDebris hazards
原始連結:連回原系統網址new window
相關次數:
  • 被引用次數被引用次數:期刊(3) 博士論文(1) 專書(0) 專書論文(0)
  • 排除自我引用排除自我引用:1
  • 共同引用共同引用:23
  • 點閱點閱:179
臺灣東部山多平地少,但有許多的沖積扇。沖積扇地勢低緩,居民取其耕作、水利之便,因此成為僅次於花蓮溪與卑南溪沖積平原外之精華區。然沖積扇依其自然發育階段可分為穩定、亞穩定與活動中的沖積扇,具有不同程度之土石災害的潛在危險性。 本研究調查東部花蓮溪河谷沖積扇之結果與發現,本河谷內之沖積扇皆為亞穩定~不穩定沖積扇。重要的聚落集中於兩大扇交會之河間區等沖積扇土砂災害陰影區,此為當地人世代從經驗中學到與自然災害安全相處之道。是以河間地為本河谷較安全可供發展的地區,未來開發必以此為是。沖積扇扇頂是土石易生區,故多為粗放型農作;扇端地下水面較高,喜水性作物如水田或荷池、漁塭等分布於此,但也有時有洪患。 沖積扇區上之河道位置與受災面具密切關連,河道位於扇緣者受災面較其位於扇央者廣。此因後者有較直而有效率之河道以疏解土石洪流之壓力。
In the mountainous eastern regions of Taiwan, there are many fluvial fans where, given their advantages of gentle sloping terrain and the availability of water, villages and arable lands have been developed. The importance of this land is second only to that of the alluvial plains of the Hualien and Peinan Rivers. According to their stages of development, there are three categories of fluvial fans: 'stable', 'meta-stable' and 'active', each having a different degree of potential debris hazard. The present study shows that all of the alluvial fans in the Hualien Valley fall into the meta-stable or active (unstable) categories, and the major towns or valleys are located in the interfluvial areas between large adjacent fans, right in the shadow fo the debris hazards. This natural development of settlements in the safer areas reflects the wisdom of the local people, who have learned from the experience of their ancestors how to cope with unavoidable natural hazards. These interfluvial areas are evidently the most suitable sites for further development in eastern Taiwan. In order for this development to take place, engineering works such as levees have been constructed to increase the safe areas, though there is still a certain level of risk. The central parts of the fans are hazard prone areas, and their land usage is limited to orchards, sugarcane, and betel. At the edges of the fans, where the ground water table is usually closer to surface level, fish ponds and rice paddies are found. These lowlands are also subject to flooding. This study also found that there is a close relationship between the location of the stream channel on the fan and the extent of area affected by debris hazards. The channels running along the flanks of the fans usually inflict damage on a larger area than those running through the center. This is because the latter has a straight and unhindered passage way in which the debris flood pressure is released.
期刊論文
1.張瑞津、石再添、楊淑君、林譽方、陳翰霖(19940300)。花東縱谷沖積扇的地形學研究。國立臺灣師範大學地理研究報告,21,43-74。new window  延伸查詢new window
2.Davis, W. M.(1899)。The geographical cycle。The Geographical Journal,1(14),481-504。  new window
3.Eckis, R.(1928)。Alluvial fans of the Cacamonga district Southern California。Journal of Geology,36,224-249。  new window
會議論文
1.張石角(1998)。颱風季的水土災害話題。沒有紀錄。1-4。  延伸查詢new window
2.陳紫娥(1997)。南投縣水里鄉郡坑二?、三?土石災害地學環境之比較研究。沒有紀錄。  延伸查詢new window
3.陳紫娥(1998)。美崙溪流域之自然環境與都市發展。臺北市:淑馨出版社。33.1-33.19。  延伸查詢new window
4.陳紫娥(1999)。花蓮縣鳳林鎮鳳義坑土石災害之研究。沒有紀錄。  延伸查詢new window
5.Brand, E. W.(1988)。Landslide risk assessment in Hong Kong。沒有紀錄。1059-1074。  new window
研究報告
1.張石角(1993)。臺灣過去二十年重大崩山災害及其對受影響地區之自然和社會環境之影響(五)。沒有紀錄:行政院國家科學委員會。  延伸查詢new window
2.張石角(1988)。臺灣過去二十年重大崩山災害及其對受影響之自然和社會環境之影響(一)。沒有紀錄:行政院國家科學委員會。  延伸查詢new window
3.謝正倫(1999)。花蓮縣鳳林鎮鳳義坑土石流災害整治工程規劃研究報告書。沒有紀錄:花蓮縣政府。  延伸查詢new window
學位論文
1.黃朝恩(1980)。臺灣島諸流域特徵及其相關性的研究(博士論文)。文化大學。new window  延伸查詢new window
圖書
1.刘希林、唐川(1995)。泥石流危险性评价。泥石流危险性评价。北京。  延伸查詢new window
2.富田芳郎(1972)。臺灣地形發達史。臺灣地形發達史。沒有紀錄:古今書院。  延伸查詢new window
3.Hails, J. R.(1977)。Applied Geomorphology。Applied Geomorphology。New York, NY:Elsevier。  new window
4.Hooke, R. LeB.(1987)。Mass movement in semi-arid environments and the morphology of alluvial fans。Slope Stability。沒有紀錄:John Wiley & Sons Ltd.。  new window
5.Judson, S.、Kauffman, M. E.(1990)。Physical Geology。Physical Geology。Englewood Cliffs, NJ:Prentice Hall。  new window
6.Kellerhals, R.、Church, M.(1990)。Hazard management on fans, with examples from British Columbia。Alluvial Fans: A Field Approach。New York, NY:John Wiley & Sons Ltd.。  new window
7.Lecce, S. A.(1990)。The alluvial fan problem。Alluvial Fans: A Field Approach。New York, NY:John Wiley & Sons Ltd.。  new window
8.Mukerji, A. B.(1990)。Alluvial Fan: The Chandigarh Dun Alluvial Fans: An Analysis of the Process - From Relationship。Alluvial Fan: The Chandigarh Dun Alluvial Fans: An Analysis of the Process - From Relationship。New York, NY:John Wiley & Sons Ltd.。  new window
9.Ollier, C.、Pain, C.(1996)。Regolith, Soils and Landforms。Regolith, Soils and Landforms。New York, NY:John Wiley & Sons Ltd.。  new window
10.Ono, Y.(1990)。Alluvial fans in Japan and South Korea。Alluvial Fans: A Field Approach。New York, NY:John Wiley & Sons Ltd.。  new window
11.Rachochi, A. H.、Church, A. H.(1990)。Alluvial Fan: A Field Approach。Alluvial Fan: A Field Approach。New York, NY:John Wiley & Sons Ltd.。  new window
12.Selby, M. J.(1982)。Processes on Rock Hillslopes, Hillslope Materials and processes。Processes on Rock Hillslopes, Hillslope Materials and processes。Oxford:Oxford University Press。  new window
13.Skinner, B. J.、Porter, S. C.(1995)。The Dynamic Earth: An Introduction to Physical Geology。The Dynamic Earth: An Introduction to Physical Geology。New York, NY:John Wiley & Sons Ltd.。  new window
圖書論文
1.林朝棨(1957)。台灣省通志稿。台灣地形。台灣省文獻委員會。  延伸查詢new window
 
 
 
 
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