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
13 results
Search Results
Item 戰後日本女性地形研究先驅--太田陽子教授(國立臺灣師範大學地理學系地理學會, 2009-06-01) 張瑞津; 沈淑敏; 黃美惠Item 臺灣東部河口地區之地形學研究(地理學系, 1995-10-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resources of this area more reasonably, the understanding of its geomorphological, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, runoff, sediments and monthly discharge, etc. are factors coming from land, while the wind, current, wave and tide etc. coming from the sea. This study focuses on eleven estuaries of the eastern coast of Taiwan. Based on the stream slope, number of channels, discharge, etc., these estuaries can be divided into straight and braided pattern. The former has sandbars or spurs, such as Hualien Hsi, Hsiukuluan Hsi and Kangkou Hsi, while the latter have braided channels, sandy-gravel sediments and changeable sandbars, such as Hoping Hsi, Liwu Hsi and the estuaries in Taitung coastal area. The eastern coast is classified as wave-dominated type according to average wave height and tidal range. The wave impacting upon the area between Hoping Hsi and Hsiukuluan Hsi is severer. The forms of the estuaries in eastern Taiwan have significant seasonal change due to the seasonal differences of discharge, monsoon and typhoon. In the summer, the channels usually become wider and the sandbars are gentler and extended seaward for most estuaries. In the winter, however, these sandbars become narrower, steeper and extend toward right bank. The mouth of channels will be narrowed or even closed when typhoon coming. The forms of estuaries are stable in the long-term scale. Eleven estuaries have only slight change during the period from 1904 to 1989, moving back and forth within the distance of 250m. The channel migration of most estuaries, however, is obvious.Item 臺灣西南部河口地區之地形學研究(地理學系, 1995-03-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resource of this area more reasonably, the understanding of geomorphogical, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, opening form, runoff, sediments, and monthly discharge etc. coming from the land. While the wind current, wave and tide etc. coming from the sea. This study area focuses on 20 estuaries of the south-western coast of Taiwan. The five of them are gravel estuaries and the rest are sandy. By correlation grain size of sandy estuaries has relationship with channel gradient below 100m, width of opening and shape factor. The forms of sand bar on estuaries are changed seasonly. Most of them has a tendency migrating southward due to northern moonsoon. The 20 estuaries can be classified into the wave dominated type, the tide dominated type and the runoff dominated type according average wave height, specific discharge and tidal range. Comparing the location of 20 estuaries during the period from 1904 to 1990(85 years). Most estuaries tend to migrate westward. The changes of estuaries are controlled by the intensity of wave and precipitation, the influence of reservior and hydraulic engineering and the changes of land use.Item 海岸山脈東坡河階的地形學研究(地理學系, 1991-03-??) 張瑞津; 石再添; 曾正雄; 高鵬飛; 陳美鈴Owing to the continuous uplift since Quaternary, rejuvenated terraces, gorges and raised alluvial fans are developed well in the eastern slope of Coastal Range. The river terraces in this area are distributed below 200 m generally. The scarps of higher level terrace are larger than that of lower level one. The gravel deposits in higher level terrace are thicker than that of lower level one. Comparing the terrace between six studied rivers, meander terraces are significant both in Mawuku River, Fengpin River, Shuilien Riverand Fanshuliao River whereas fan terraces are developed well in Sanhsien River. In contrary, the terrace in Shuimuting River is undeveloped due to down cutting into hard rock which restricts the widening of terrace. By correlating to marine terraces, most of the terraces in this area are formed in Holocene. The detailed correlation of each step or dating still needs more envidences.Item 臺灣西部海岸沙丘之地形學研究(地理學系, 1993-06-??) 石再添; 張瑞津; 張政亮; 林雪美; 連偵欽Coastal sand dunes are widely distributed along the western coast of Taiwan from Touchien Hsi to Erhjen Hsi. Based on maps work, airphoto interpretation, particle size analysis, field investigation, etc, the study results are summarized as follows: 1. The form and the magnitude of the western coastal sand dunes have close relationship with the source of 13 rivers' sand supply, alongshore current and wave action, power and direction of wind, terrains, rainfall, evaporation and vegetation. 2. The coastal dunes develop well on riversides of Chung Kang His, Holung Hsi, Choshui Hsi and offshore bars along Chianan coast. Two principal types of these dunefield may be distinguished, namely, active dunes and stabilized dunes. The two dunefield types contain a variety of dune features, such as transverse dunes, barchans, longitudinal dunes, and dome dune etc. 3. The grain sizes of beach and dune sand are quite uniform. The Md φ and δ φ on average of the dune sand is smaller than the beach sand. This shows that wave process is stronger than wind process. 4. Comparing the maps published in 1926 and 1984. the change of coastal dunes is clear. Because the dunefield was used as fishery or watermelon and sugarcane planting, most of the sand dunes were leveled off entirely. Some of the residual sand dune still exist at present fixed by windbreak forest. For sand dunes have the function of protecting coasts, they had better be well-planned and well-used so as to main-tain the sustainable utilization of land souces.Item 臺灣北部海岸沙丘之地形學研究(地理學系, 1992-03-??) 石再添; 張瑞津; 林雪美; 張政亮; 連偵欽Item 頭前溪階地之地形學研究(地理學系, 1999-11-??) 張瑞津; 鄧國雄; 劉明錡頭前溪階地群至今仍殘存之紅壤階地可分為六階，非紅壤階地為三階。紅壤高位階地分布於頭前溪兩岸，以南岸的竹東至新竹間之竹東丘陵區最為發達，紅壤最高面為竹東面，高度280~250公尺，比高約130 ~100公尺，對比為LH。其次為寶山北面、竹東西面、高峰面、仙宮面與關東橋面，前二者之紅壤階面多已侵蝕殆盡，僅餘丘頂殘面，高度為250~230公尺與220~200公尺，階崖均達20公尺，分別對比為LT1與LT2；後三者高度分別為110~100公尺、90~80公尺、70~50公尺，階崖為20公尺、15公尺與10公尺，對比為LT3、LT4與LT5面；北岸之飛鳳山丘陵區最高為飛鳳山，高度462公尺，殘面對此為LH，其次為犁頭山頂部賤留三塊向西緩降的高位紅壤階地，高度由230~150公尺，對比為LT1。非紅壤低位階地則分布於頭前溪南、北兩岸，可分為三段階地，其中南岸的員山面及麻園肚面較廣，高度為55~40公尺、45~30公尺，階崖為5公尺、3~5公尺，對比為FT2與FT3面，而FT1之員崠子面殘留甚少。北岸之穹林面與竹北面高度分別100~90公尺及80~20公尺，階崖5~10公尺與3~5公尺，對比為FT1與FT3。本區階地受到新期構造如新竹斷層、新城斷層、竹東斷層與寶山背斜、青草湖背斜等的影響，其中以新竹斷層及新城斷層對階地的影響最為明顯，例如新城斷層通過LT3、LT4與LT5，各造成40公尺、35公尺與25公尺之斷層崖，至於低位階地FT2則有數公尺的斷崖；新竹斷層通過LT5與FT2面，各造成10公尺與2公尺的斷崖，且影響LT5階面向南傾動。本研究根據階地分布、地形特徵及地形面對比推測，頭前溪地形演育如下：更新世中期頭前溪形成LH面，因受台灣島新期構造運動的隆升，造成頭前溪向北依次遷移下切，而新期構造運動中，斷層活動則至少持續至FT2。Item 新店溪河階之地形學研究(地理學系, 2000-11-??) 張瑞津; 鄧國雄; 劉明錡River terraces including six lateritic surfaces (LH、LT1-LT5) and three non-Iateritic surfaces (FT1-FT3) have been recognized along Hsin-tien River. Most of lateritic surfaces distributed concentrately at Ping-lin, Shen-chang-Pan and Hsin-tien. Comparatively speaking, surfaces LT4, LT5 and FT2 distributed more widely and continuously than the others. Under the effect of tilting, the channel tended to shift from south to north and became sinuos. Sinuosity increased to the maximum in the LT4 stage that imp1ied the river had a significant lateral erosion in relatively stable stage. FT terraces have been formed under the controlling effect eustatic fluctuation and subsidence of Taipei Basin. The meander cut occurred during the lowering base level stage (FT1-FT2). Referring the results of climatic and eustatic fluctuation, the LT5 and three FT surfaces have been formed respectively in high sea level around 40000, 10000, 6000 and 3000 years before present.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 臺灣活斷層的地形學研究(地理學系, 1986-03-??) 石再添; 鄧國雄; 張瑞津; 石慶得; 楊貴三