文學院
Permanent URI for this communityhttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/2
院成立於民國44年，歷經50餘年的銳意發展，目前設有國文、英文、歷史、地理、臺文等5個學系、翻譯和臺灣史2個獨立所，以及全球華人寫作中心和國際臺灣學研究中心。除臺史所僅設碩士班，其餘6個系所均設有碩、博士班；目前專兼任教師近250人，學生約2500餘人。
本院早期以培養優秀中學國文、英文、歷史和地理教師為鵠的，臺灣中學語文和史地教育的實踐與成功，本院提供不可磨滅的貢獻。近年來，本院隨師範體系轉型而調整發展方向，除維持中學師資培育的優勢外，也積極朝理論研究和實務操作等面向前進。目前，本院各系所師培生的教師檢定通過率平均在95%以上；非師培生在文化、傳播、文學、應用史學及環境災害、地理資訊系統等領域發展，也已卓然有成。
本院各系所教師的研究能量極為豐富，參與國內外學術活動相當活躍。根據論文數量、引用次數等指標所作的學術力評比，本院居人文領域全國第2名。各系所之間，無論是教師的教學與研究，或學生的生活與學習，都能相輔相成、榮辱與共，彼此渾然一體，足堪「為師、為範」而無愧。
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Item 花東縱谷沖積扇的地形學研究(地理學系, 1994-03-??) 張瑞津; 石再添; 楊淑君; 林譽方; 陳翰霖Huatung (Hualien-Taitung) Longitudinal Valley locates between Central Range and Coastal Range with a length of 183 km and width of 3-4km. With conspicuous fault scarps and abundant debris supply , alluvial fans are developed well in this valley. There are 31 fans with over 2 km2 in size and over 2[] in slope. Due to the continual uplift, most of the fans have been undercut into composite fans. There are 2-3 steps in southern fans whereas 1 step in northern fans, and also, the amounts of dissection of southern fans are greater than that of northern fans. These differences, thus, may provide an usable reference for differential uplift in Huatung area. By product-moment correlation, there are some relations between fan variables, such as a significant relation with fan area and fan width, slope and height. Further, the factors of drainage area, relief ratio, stream length and intermountain basin area have strong correlation with the variables of fan area, slope, width and degree of dissection. Based on the discriminant analysis, the sediment space, uplift rate, geologic age, precipitation, stream order and slope failure area are the dominating factors to the existence of fan. By factor analysis and canonical correlation analysis the results can be concluded that drainage area, stage of fan, sediment space, amount of uplift and relief ratio of drainage basins are the common factors which influence the fan morphology. It is difficult to examine the evolutionary hypothesis and climatic hypothesis in this area due to the insufficient chronologic and climatic data. But from the strong relation between fans and drainage basins, the fan development in this area can be interpretated by equilibrium hypothesis.Item 蘭陽地區沖積扇的地形學研究(地理學系, 1995-03-??) 張瑞津; 石再添; 楊淑君; 林譽方; 陳翰霖; 董德輝蘭陽地區是臺灣沖積扇發達地區之一，區內共有30個沖積扇，位於縱谷內13個，平原區者17個。縱谷上游諸扇呈四階複成扇，且扇項有逐次下移的現象，可推知本區現今山麓的河下切率，大於集水域的上升速率。另由扇體堆積的縱剖面呈凸透鏡狀，可推知沖積扇形成之同時，集水域的地盤仍持續隆升。由沖積扇的形態與堆積物特徵的相關分析，沖積扇面積愈大，流幅愈大，坡度愈緩，堆積物淘選度愈佳，圓度愈大。根據集水域的地形、地質、氣候各項特徵所作之判別分析，得知主流等級、起伏比、隆升率、年平均降雨量、面積高度積分、溪口距、山間盆地面積為決定沖積扇存在的要因。經因子分析地盤隆升率、集水域面積、起伏比，扇面時期為影響沖積扇形態的要因。由沖積扇特徵特徵與集水域各地形、地質、氣候諸要素的關係觀之，本區沖積扇的演育頗適合以侵蝕輪迴說及動態平衡說加以解釋均似合適。Item 高屏溪谷與潮州斷崖沖積扇的地形學研究(地理學系, 1995-10-??) 張瑞津; 石再添; 楊淑君; 林譽方; 陳翰霖; 董德輝Kaoping valley and Chaochou fault are lecated the southwestern part of Taiwan Island. With conspicuous fault scarps and abundant debris supply, alluvial fans are developed well in this area. There are 38 fans with area over 0.1 km each, 22 of them are distributed in the Laonung valley, 8 of them in Nantzuhsien valley, and the rest are in the piedmont along the Chaochou fault scarps. In the valley, most of the fans have been undercut to be composit fans. The fact of the fan head trench shifting down could reveal that the down cutting rate of stream channel is greater than the uplift rate of mountain area. By product-moment correlation, some fan variables are correlated closely, such as fan area has a significant relation with length, width, slope and roundness of sediments. Based on the discriminant analysis, the precipitation, geological period, the stream length, hypsometric integral and relief ratio are the dominating factors to the existence of the fan. By factor analysis, drainage area, uplift rate, relief ratio, geology of drainage basin, drainage length and evolution stage of fan are the main factors influencing the fan morphology. From the relation between fan and drainage basin, the evolution of the fan of the Nantzuhsien valley and Chaochou fault can be interpreted by the equillbrium model.