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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳宏宇(Hongey Chen) | |
| dc.contributor.author | Chen-Han Lin | en |
| dc.contributor.author | 林辰翰 | zh_TW |
| dc.date.accessioned | 2021-05-16T16:19:41Z | - |
| dc.date.available | 2019-01-09 | |
| dc.date.available | 2021-05-16T16:19:41Z | - |
| dc.date.copyright | 2013-08-09 | |
| dc.date.issued | 2013 | |
| dc.date.submitted | 2013-08-08 | |
| dc.identifier.citation | 中文部分：
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/6032 | - |
| dc.description.abstract | 本研究藉由分析花蓮和平溪流域2007年至2012年的四個山崩事件，探討崩塌地、河川化性，以及輸砂量間的相互對應關係。研究結果顯示，崩塌率與颱風的累積雨量及降雨強度有明顯正相關性，蘇拉颱風造成之山崩有最高的崩塌率、新生率與重現率，分別為2.1%、71.4%，以及58.2%。此外，岩體強度較低的廬山層和畢祿山層，占全區80%以上的崩塌率，顯示各地層之崩塌率與岩體強度有著負相關的趨勢。從崩塌地在坡體上的分布發現，大約有30%的崩塌地面積集中在靠近河道的位置，這些崩塌地在蘇拉颱風之後向上擴大，變成從河道延伸至山嶺的大型崩塌地，使得更多地質材料與碳酸鹽礦物等物質進入河川，除了提供颱風期間輸砂量增加的來源，也導致K+、Ca2+、溶解無機碳濃度，以及δ13CDIC急遽地上升。
由近30年的輸砂量計算結果顯示，本研究區之平均年輸砂量為14.45Mt，其中，颱風暴雨的沖刷與山崩事件為年輸砂量主要的供應來源，颱風期間的累積雨量越大，輸砂量占該年度輸砂量的比例也越大。而濕季的平均輸砂量為乾季的12.1倍，也顯示由於濕季雨量較充沛，造成乾濕季輸砂量的差異性。 從河水Gibbs圖得知，和平溪之河水離子濃度受到岩性影響，屬於「岩性控制」類型，約有40%至80%來自於碳酸鹽礦物。河川化性與流量的關係指出，Na+和Mg2+濃度和流量間屬於稀釋作用的關係，濕季時的濃度較低；Cl-濃度和流量間屬於水文常數平衡的關係，乾濕兩季的濃度沒有明顯之差異；Ca2+和K+濃度和流量間屬於潤濕作用的關係，在濕季時的濃度分別為乾季時的1.13倍和1.07倍；溶解無機碳濃度則是在流量大於20m3/sec時，和流量有明顯正相關的趨勢。 | zh_TW |
| dc.description.abstract | This research concerned the relationship among four typhoon-induced landslide events, river chemistry and sediment discharge in the catchment of the Heping River during 2007 to 2012. The analyzed results point out that higher rainfall intensity and cumulative rainfall would cause higher landslide ratios. Therefore, typhoon Saola triggered a highest landslide ratio of 2.1%, new generation ratio of 71.4%, and reactivated ratio of 58.2% among four typhoons. In addition, More than 80% landslides occurred in Lushan and Pilushan Formations because of the weak rock strength. About 30% of landslides located near the river and expanded to hilltop after typhoon Saola. Consequently, more deposits and carbonate minerals were transported into the river, causing the concentration of K+, Ca2+, dissolved inorganic carbon and δ13CDIC raised abruptly.
The average annual sediment discharge is 14.45 Mt and mainly resulted from the contribution of typhoon events. In comparison with sediment discharge and rainfall, the greater the cumulative rainfall during typhoon, the higher the proportion of typhoon-triggered sediment discharge to annual sediment discharge. The results also show that the average sediment discharge in wet season is 13.35 Mt, which is 12.1 times of dry season due to the difference of rainfall. The plot of the total dissolved salts versus Na+/ (Na++Ca2+) reflected that the chemical properties of Heping river belonged to rock-dominated type. Moreover, the relationship between water discharge and ionic concentrations indicate that the concentrations of Na+ and Mg2+ decreased with increasing discharge, the ionic concentrations were lower in wet season. In contrast, the concentrations of Ca2+ and K+ increased with increasing discharge, the concentrations in wet season were 1.13 and 1.07 times of the dry season, respectively. The concentrations of dissolved inorganic have apparently positive correlation with discharge when discharge is higher than 20 m3/sec. | en |
| dc.description.provenance | Made available in DSpace on 2021-05-16T16:19:41Z (GMT). No. of bitstreams: 1 ntu-102-R00224204-1.pdf: 9958381 bytes, checksum: ffb44563488cf967d46136ed8cbc9c5b (MD5) Previous issue date: 2013 | en |
| dc.description.tableofcontents | 致謝 I
摘要 II Abstract III 目錄 V 圖目錄 VIII 表目錄 XI 第一章 緒論 1 1.1研究動機與目的 1 1.2地理位置及交通概況 2 第二章 前人研究 4 2.1降雨和山崩之關係 4 2.2輸砂量估算與異重流特性 6 2.3河川化性與地質環境關係 9 2.4河水溶解無機碳 11 第三章 研究區域概況 13 3.1地形概況 13 3.2地質概況 16 3.3土壤概況 19 3.4氣候與水文概況 20 3.5颱風事件 21 第四章 研究方法 23 4.1野外調查工作 23 4.1.1樣品採集 23 4.1.2施密特錘試驗 25 4.2實驗室試驗 25 4.3崩塌地判釋 25 4.4輸砂量估算 31 4.5河川化學性質分析 33 4.5.1陰離子分析方法 34 4.5.2陽離子分析方法 34 4.5.3溶解無機碳分析方法 34 4.5.4岩石元素含量分析方法 35 4.5.5離子濃度與地質環境相關性分析 35 4.5.6溶解無機碳與地質環境相關性分析 39 第五章 研究結果 42 5.1地質材料性質試驗結果 42 5.1.1自然物理性質試驗 42 5.1.2岩石力學性質及消散耐久試驗 43 5.2崩塌地判釋結果 46 5.2.1崩塌地統計 46 5.2.2崩塌地在坡體分布狀況 50 5.2.3崩塌與岩體強度和颱風降雨之關係 53 5.3輸砂量估算結果 54 5.3.1歷年輸砂量統計 54 5.3.2輸砂量與乾濕季之關係 58 5.3.3花蓮群震對輸砂濃度之影響 60 5.4河川化學性質分析結果 63 5.4.1主要離子濃度分析結果 63 5.4.2溶解無機碳濃度與碳13同位素分析結果 67 5.5岩石元素含量分析結果 69 第六章 崩塌地與河川化性之關係 71 6.1崩塌地面積與離子濃度之關係 71 6.2離子濃度與岩性之相關性 73 6.3離子濃度與流量之相關性以及乾濕季變化 75 第七章 討論 79 7.1崩塌地面積機率分佈之比較 79 7.2碳酸鹽對河水陽離子的貢獻比例 83 7.3離子濃度與流量之回歸分析 85 7.4異重流事件之推估 87 第八章 結論 90 參考文獻 92 附錄一 河水採集與樣品前處理方法 106 附錄二 施密特錘單壓強度換算表 107 附錄三 自然物理性質試驗方法 108 附錄四 點荷重試驗方法 110 附錄五 消散耐久試驗方法 112 附錄六 陰離子分析方法 113 附錄七 陽離子分析方法 114 附錄八 溶解無機碳分析方法 115 | |
| dc.language.iso | zh-TW | |
| dc.title | 花蓮和平溪流域山崩作用與河川化性之相關性 | zh_TW |
| dc.title | The relationship between landslide and river chemistry in Heping River, Hualien | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 101-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 林曉武,董家鈞,侯秉承 | |
| dc.subject.keyword | 崩塌地,離子濃度,溶解無機碳,δ13CDIC,輸砂量, | zh_TW |
| dc.subject.keyword | landslide,ion concentration,dissolved organic carbon,δ13CDIC,sediment discharge, | en |
| dc.relation.page | 115 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2013-08-08 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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