埋積谷床地形特徵、作用與流域地形計測之探討：以新店平廣溪為例

The Study on Landform Feature, Process and Geomorphometric Analysis of Waste-filled Valleys: A Case Study of Ping Guang Stream, Xindian

10.6234/JGR.201905_(70).0006

林文毓(Wen-Yu Lin)；沈淑敏(Su-Min Shen)

埋積河谷 ； 地形判釋 ； 數值航測 ； 流域險峻值 ； 蘇迪勒颱風 ； waste-filled valleys ； landform identification ； digital aerial photogrammetry ； Melton's ratio ； Typhoon Soudelo

地理研究

70期（2019 / 05 / 01）

143 - 162

繁體中文

臺灣山區中小型河谷常見由沈積物淤埋而成的較平緩河段，當強颱豪雨驅動流域內沈積物搬運時，很可能造成谷床上建物、農地的災害，但對其地形變動的探討有限。本研究擬探討中小型埋積谷床地形特徵、地形作用和流域地形計測參數的關連，主要研究方法為數值航測地形判釋、流域地形計測，並結合前人現場調查和流域險峻值（Melton's ration）的分析結果，研究樣區為新店溪中游支流平廣溪，2015年8月蘇迪勒颱風時曾誘發較顯著的地形變化與造成災害。數值航測判釋結果顯示，平廣溪主流谷床以比高約2－3m的埋積階地為主要地形單元，中段並有多個支流扇狀地分布，顯示該溪谷主要受到土石流與洪水溢淹作用而建成，流域險峻值（MR值）估算結果亦大致符合。不過蘇迪勒颱風幾處特定地點之谷壁邊坡崩塌所供給的大量土砂，導致此次平廣溪土石流作用的河段比MR值推估的略向下游延伸，而且該溪流最下游的洪水溢淹與谷壁崩塌、新店溪水位高漲都有關係。由此可知，雖然每次降雨事件誘發的地形反應具有空間上的偶然性，但當代單一大規模事件（例如，蘇迪勒颱風）通常只是在其既有的地形單元上「再作用」，因為谷床地形特徵反映的是更長期無數次大規模事件作用的結果。臺灣山區類似平廣溪谷床地形的河段很多，結合判釋既有地形特徵、流域地形計測與現場實察，進行綜合評估，將有助於理解埋積谷床的災害風險評估。

In Taiwan, waste-filled valleys of small mountainous catchments imply that the valley floors are subject to geomorphic hazards triggered by debris flow, bank erosion and flooding. This study intends to demonstrate the spatial distribution of landform features and of geomorphic change by the major rainfall event in a waste-filled valley. The methods applied include digital aerial photogrammetry, geomorphometric analyse (Melton's ration, MR) and on-site investigation report analysis. The study area is the Ping Guang Stream (PS Stream), a tributary of the Xindian River in the northern Taiwan, which experienced the most significant geomorphic change during Typhoon Soudelo in August, 2015. The main landform unit of the valley bottom along the Ping Guang Stream is fill terraces with scarp 2-3 m and a few tributary fans locate in the mid-stream. During Typhoon Soudelo, the dominant geomorphic process in the upper streams was debris flow and turning into flooding in the downstream, which is in line with the result of MR. It is regarded as the reworking of geomorphic processes within the existent geomorphic framework of the Ping Guang Stream valley although the location of landslides and raising water level of the Xindian River, i.e., the spatial and temporal contingency, did increase the area of debris flow and flooding. There are numerous waste-filled valleys as the Ping Guang Stream in the mountainous Taiwan, a comprehensive investigation as demonstrated in this research will greatly benefit the future natural hazard assessment.

1. 翁毓穗, Y.S.,沈淑敏, S.M.,莊永忠, Y.C.(2010)。莫拉克颱風在楠梓仙溪誘發之洪水與土石流作用及其溢淹範圍的含意。中國地理學會會刊，45，59-74。
   連結：
2. Bovis, M.J.,Jakob, M.(1999).The role of debris supply conditions in predicting debris flow activity.Earth surface processes and landforms,24(11),1039-1054.
3. Coe, J.A.,Godt, J.W.,Parise, M.,Moscariello, A.(2003).Estimating debris-flow probability using fan stratigraphy, historic records, and drainage-basin morphology, Interstate 70 highway corridor, central Colorado, USA.USA Proceedings of the 3rd International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment,Davos (Switzerland):
4. Dadson, S.J.,Hovius, N.,Chen, H.,Dade, W.B.,Hsieh, M.L.,Willett, S.D.,Lague, D.(2003).Links between erosion, runoff variability and seismicity in the Taiwan orogen.Nature,426(6967),648.
5. De Scally, F.A.,Owens, I.F.(2004).Morphometric controls and geomorphic responses on fans in the Southern Alps, New Zealand.Earth Surface Processes and Landforms,29(3),311-322.
6. Harvey, A.M.(2001).Coupling between hillslopes and channels in upland fluvial systems: implications for landscape sensitivity, illustrated from the Howgill Fells, northwest England.Catena,42,225-250.
7. Hovius, N.,Stark, C.P.,Chu, H.T.,Lin, J.C.(2000).Supply and removal of sediment in a landslide-dominated mountain belt: Central Range, Taiwan.The Journal of Geology,108,73-89.
8. Jackson, L.E.,Kostaschuk, R.A.,MacDonald, G.M.(1987).Identification of debris flow hazard on alluvial fans in the Canadian Rocky Mountains.Debris Flows/Avalanches: Process, Recognition, and Mitigation, Reviews in Engineering Geology, 7
9. Schrott, L.,Hufschmidt, G.,Hankammer, M.,Hoffmann, T.,Dikau, R.(2003).Spatial distribution of sediment storage types and quantification of valley fill deposits in an alpine basin, Reintal, Bavarian Alps, Germany.Geomorphology,55(1-4),45-63.
10. Wilford, D.J.,Sakals, M.E.,Innes, J.L.,Sidle, R.C.,Bergerud, W.A.(2004).Recognition of debris flow, debris flood and flood hazard through watershed morphometrics.Landslides,1(1),61-66.
11. Wohl, E.(2000).Mountain Rivers.Washington, DC:American Geophysical Union.
12. 行政院農業委員會水土保持局（2015）：〈重大土石災情報告〉，《土石流防災資訊網》。https://246.swcb.gov.tw/Achievement/MajorDisasters。（2018/08/14 瀏覽）【Soil and Water Conservation Bureau(2015). Majon Disaster Events. Retrieved from https://www.afasi.gov.tw/aerial_search】
13. 行政院農業委員會水土保持局=Soil and Water Conservation Bureau(2015)。,南投=Nantou:行政院農業委員會水土保持局=Soil and Water Conservation Bureau。
14. 行政院農業委員會林務局農林航空測量所（2015）：〈航空攝影紀錄資料〉，《行政院農業委員會林務局農林航空測量所》。https://www.afasi.gov.tw/aerial_search。（2018/03/20 瀏覽）【Soil and Water Conservation Bureau(2015). Aerial photography Information. Retrieved from https://www.afasi.gov.tw/aerial_search】
15. 吳輝龍, H.L.,陳文福, W.F.,張維訓, W.S.(2004)。集水區地文特性因子與土石流發生機率間相關性之研究：以陳有蘭溪為例。中華水土保持學報，35(3)，251-259。
16. 李錫堤, C.T(1996)。從地形學的觀點看陳有蘭溪的賀伯風災。地工技術，57，17-24。
17. 沈淑敏, S.M.,葉懿嫻, I.H,黃健政, C.C.,張瑞津, J.C.,劉盈劭, Y.S.(2007)。花東縱谷北段的土石流扇和土石流溪溝的認定。中華水土保持學報，38(4)，311-324。
18. 周憲德, H.T.(2016)。行政院農業委員會水土保持局創新研究計畫成果報告行政院農業委員會水土保持局創新研究計畫成果報告,南投=Nantou:行政院農業委員會水土保持局=Soil and Water Conservation Bureau, COA。
19. 林昭遠, C.Y.,張力仁, L.(2000)。地文因子對土石流發生影響之研究─以陳有蘭溪為例。中華水土保持學報，31(3)，227-237。
20. 林朝宗, C.C.(2000).五萬分之一臺灣地質圖說明書─新店圖幅.新北=New Taipei:經濟部中央地質調查所=Central Geological Survey, Ministry of Economic Affairs.
21. 張志新, C.H.,王俞婷, Y.T.,傅鏸漩, H.X.,林又青, Y.C.,張駿暉, C.H.,劉哲欣, C.H.,呂喬茵, C.Y.,吳啟瑞, C.J.,蘇元風, Y.F.(2015)。,新北=New Taipei:國家災害防救科技中心=National Science and Technology Center for Disaster Reduction。
22. 張瑞津, J.C(1997)。陳有蘭溪流域的地形環境與自然災害之關係。中國地理學會會刊，25，43-64。
23. 陳宏宇, H.,蘇定義, D.I,陳琨銘, K.M.(1999)。土石流發生機制與地質環境之相關性。地工技術，74，5-20。
24. 游繁結, F.C.,陳重光, C.K.(1987)。豐丘土石流災害之探討。中華水土保持學報，18(1)，76-92。
25. 楊明德, M.D.,林基源, J.Y.,林蔚榮, W.J.,黃凱翔, K.S.,吳東諺, D.Y.(2009)。莫拉克颱風於陳有蘭溪流域之災害調查。中華水土保持學報，40(4)，345-358。
26. 詹錢登, C.D(2004)。豪雨造成的土石流。科學發展，374，14-23。
27. 鈴木隆介、松倉公憲(2017)。地形の辞典。東京=Tokyo:朝倉書店=Asakura Published Co., Ltd.。
28. 劉盈劭, Y.S.(2013)。臺北=Taipei，國立臺灣師範大學地理學系=Department of Geography, National Taiwan Normal University。