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。
News
Browse
11 results
Search Results
Item 台灣西南海岸的變遷(2006-01-01) 林宗儀; 陳翰霖; 張瑞津Item 台灣西南洲潟海岸的變遷(2006-01-01) 林宗儀; 張瑞津; 陳翰霖Item 臺江風華(經濟部中央地質調查所, 2010-12-01) 陳華玟; 吳樂群; 林宗儀; 陳翰霖; 張瑞津; 陳麒麟Item 花東縱谷國家風景區特殊地景景點開發、維護及旅遊路線規劃之研究(交通部觀光局花東縱谷國家風景區管理處, 2001-01-01) 張瑞津; 蔡文彩; 鄧國雄; 林雪美; 沈淑敏; 陳翰霖; 魏源金; 黃源城; 滕肇芸Item 曾文水庫對流量及輸沙量的影響(地理學系, 2003-11-??) 陳翰霖; 張瑞津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 臺灣西南部嘉南平原的海岸變遷研究(地理學系, 1998-05-??) 張瑞津; 石再添; 陳翰霖嘉南海岸平原形成於晚更新世，海岸線的變遷與海水進退相對應，近三百多年來整體呈現向西推移的趨勢，古笨港、魍港（蚊港）及倒風內海已逐漸淤填，並被大量圍墾開發為魚塭或鹽田。濱外沙洲西側海岸除河口地區外，均向內侵蝕，在海汕洲及王爺港汕西側最大侵蝕率約達 12mn/yr。 外傘頂洲整體向東南方陸地漂移， 沙洲北段漂移速率甚至達58mn/yr。 沙丘主要分布於新港、鹿草一線以西，其中北港地區因濁水溪供沙充足，較嘉義沿海發達。 北港以西的海岸沙丘，大致分布在 7mn 以下，呈四列南北帶狀分布，隱示不同時期的海岸線位置， 應形成於大湖期海侵（ 3500-4000yr B.P. ）之後。 比較 1904-1926及 1990 年各時期之沙丘，其規模大致逐漸減小，係受人類開發利用影響所致。海岸平原地區向為人口稠密地帶，地形變遷常造成洪患威脅、丘沙漂移、土地利用改變、沿岸聚落興衰、土地權屬爭議及行政區劃定等之衝擊。相反的，人類擴張聚落、興建水庫、修築堤防、開鑿渠道、圍墾海埔地、取直河道等作為，也造成天然地形之改變，地形變遷與人類生活息息相關，其研究正可提供為土地規劃與開發利用的參考。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 臺灣西南部臺南海岸平原地形變遷之研究(地理學系, 1996-11-??) 張瑞津; 石再添; 陳翰霖The Tainan coastal plain in southern Taiwan had been formed since late Pleistocene. The coast was marked by the offshore bars and lagoons, and have prograded to the west about 13 km since last three hundred years. The large lagoon was named as "paleo Taichiang Inland Sea" in Ching dynasty historical document had been filled up and reclaimed as fish ponds and salt pans due to the rapid sedimentation. However, the west coast of offshore bars have been eroded with a maxium rate about 14 m/yr in Tingtouerh bar in this century. The coastal dunes are distributed mainly in Salun, Tainan and Kunshen. Among them, Salun and Tainan dunes were deposited in Tahu Transgression stage (3500-4000 yr B.P.) where as the Kunshen dunes developed on offshore bars in last three centuries. Besides, a series of dunes is still exsited along the former Tsengwen River. Due to the expansions of the cultivated and built areas, all the dunes have decreased in magnitude. The river channel changed significantly both in hills and coastal plains. In the hills, 13 meander neck cutoffs can be observed in Erhjen River and Tsengwen River. On the coastal plain, river channel shifted by meandering and avulted suddenly in typhoon season because of epesodic sedimentation in the river bed. There were four big channel avulsions recorded since 19 century in Tsengwen River and the range of channel avulsion from north to south is about 25 km. However, the channel was confined after the dyke had been constructed in 1934. Overall, the geomorphological changes of Tainan coastal plain were caused by long term physical processes but modified strongly by human agency in the recent time. The geomorphological changes have induced some impacts on the human beings such as the decline of port, moving of village to prevent flooding, confusion of administrative boundary, etc.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.