請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/3847完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳尊賢 | |
| dc.contributor.author | Che-Yu Lin | en |
| dc.contributor.author | 林哲郁 | zh_TW |
| dc.date.accessioned | 2021-05-13T08:37:29Z | - |
| dc.date.available | 2017-08-24 | |
| dc.date.available | 2021-05-13T08:37:29Z | - |
| dc.date.copyright | 2016-08-24 | |
| dc.date.issued | 2016 | |
| dc.date.submitted | 2016-07-27 | |
| dc.identifier.citation | 中央氣象局。2016。氣候統計資料。http://www.cwb.gov.tw/V7/climate/monthlyMean/Taiwan_tx.htm。
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In K. Wada (ed.). 'Ando Soils in Japan'. Kyushu University Press. Zehetner, F., W. P. Miller, and L. T. West. 2003. Pedogenesis of volcanic ash soils in Andean Ecuador. Soil Sci. Soc. Am. J. 67: 1797-1809. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/3847 | - |
| dc.description.abstract | 烘爐山(Honglu Mountain, HL)屬於大屯火山亞群，約在40萬年前停止噴發，為一座由高鋁玄武岩所構成的截頂狀火山錐。由於母質特殊且尚未調查，根據地形土序在該地區山頂(HL-1)、上背坡(HL-2)與下背坡(HL-3)位置選擇土壤樣體，研究其土壤特性、化育作用與分類。土壤剖面呈現棕色，且不具有典型灰燼土具有的黑瘠表育層。研究區域屬亞熱帶氣候，茂盛的植被提供大量有機質來源，而豐富的可交換性鋁增加了土壤酸度，強烈的淋洗作用造成低鹽基飽和度。選擇性化學抽出指出，土壤中的活性鋁主要以鋁‒有機質複合物為主，而鋁英石在酸性環境下不易生成(pH < 5)。微形態特徵顯示樣體無明顯的黏粒洗入現象，再以質地分析結果判斷得知，研究樣體無黏聚層(argillic horizon, Bt)，B化育層均為火山灰土壤常見的變育層(cambic horizon, Bw)。礦物分析結果顯示黏土礦物以高嶺石、水鋁氧含量最多，石英次之，方矽石含量最少，HL-2及HL-3有中量的綠泥石及水化層間蛭石，HL-2及HL-3樣體有相對較多的2:1型礦物。研究區域土壤受母質影響為火山灰土化作用，且氣候與時間因素使得化育於火山母質的土壤逐漸脫離火山灰土壤性質，在此轉變的過程有鹽基離子流失、結晶性鐵氧化物變多、無定形物質減少、總體密度上升、黏粒含量變多、高嶺石等黏土礦物的生成等。地形對於本研究區域土壤化育的影響不大，但各樣體間受到坡度、坡向等微地形的影響，因此在物理及化學性質間仍有些許差異。所研究的三個樣體在物理及化學性質上皆未能完全符合美國土壤分類系統中火山灰土壤性質(andic soil properties)之定義，在海拔385–650 m間地形土序上的HL-1及HL-2其亞類為灰燼型低鹽基濕潤弱育土(Andic Dystrudepts)，HL-3所受的風化程度最大其亞類為典型低鹽基濕潤弱育土(Typic Dystrudepts)，地形土序上的變化不大，皆屬於弱育土(Inceptisols)。 | zh_TW |
| dc.description.abstract | Honglu Mountain belongs to Tatun volcano subgroup with the extinction of eruption approximate 0.4 million years ago. Previous studies have explored the pedogenesis and soil classification in most areas of Yangmingshan national park, but Honglu Mountain is not investigated and only an Al-enriched basalt composite cone in Tatun volcano group. Three soil pedons are selected along a toposequence including summit (HL-1), upper backslope (HL-2), and lower backslope (HL-3) landscape positions. The soil color is brown and the diagnostic epipedon is ochric epipedon for all the studied three pedons. Dense vegetation supplies large amounts of organic matter to the soils in this subtropical climate, but exchangeable cations were leached out of the soils due to the very high rainfall of 4800 mm per year. However, large amounts of exchangeable Al are generated in the soils to increase the soil acidity. The results of selective chemical extractions indicate that the active Al are dominantly formed as Al -humus complexes in the soils. Allophane is not identified in such an acidic condition (pH< 5). The soil micromorphology shows that clay illuviation is unobvious in B horizon and the particle-size analysis indicates that B horizon are cambic horizons (Bw). X-ray diffractometer analysis shows that the mineralogical compositions of the clay fractions are major with kaolinite and gibbsite, minor with quartz, and fewer with cristobalite. The pedogenesis processes of the studied soils are predominant andosolization and subsequent de-andosolization, which forming Inceptisols via the factors of climate and time. This implies the base loss, increases of crystalline iron oxides, bulk density, and clay contents, decreases of non-crystalline materials, and formation of kaolin minerals. The factor of topography did not significantly affect the pedogenesis, while the differences between physical and chemical properties of the three soil pedons can be attributed to micro-topography. The chemical and physical properties of the studied pedons can’t completely meet the criteria of andic soil properties of USDA Soil Taxonomy. The pedon HL-1 and HL-2 can be classified as Andic Dystrudepts, and pedon HL-3 can be classified as Typic Dystrudepts. The studied pedons are all classified as Inceptisols along the toposequence. | en |
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| dc.description.tableofcontents | 中文摘要 I
英文摘要 II 目 錄 III 圖目錄 VII 表目錄 VI 第一章 前言 1 第二章 前人研究概況 4 第一節、國外火山灰土壤之相關研究 4 一、灰燼土的轉變 4 二、環境因子對灰燼土化育之影響 6 第二節、台灣火山灰土壤之相關研究 7 一、環境因子對園區土壤的性質與分佈 7 二、園區灰燼土轉變之研究 8 第三節、研究區環境概況 11 一、氣候 11 二、植生 14 三、地形 17 四、母質 17 五、時間 19 第三章 材料與方法 25 第一節、土壤樣體之選擇與採樣 25 一、土壤樣體的選擇 25 二、土壤樣體之採樣與描述 25 三、土壤樣品的處理 25 四、微形態觀察所需樣品之採集 29 第二節、土壤分析方法 29 一、物理性質分析 29 二、化學性質分析 30 三、礦物組成份分析 34 四、土壤薄切片之製備與觀察 39 第三節、統計分析 39 第四章 結果與討論 41 第一節、土壤形態特徵 41 一、Honglu Mountain-1 (HL-1)樣體 41 二、Honglu Mountain-2 (HL-2)樣體 43 三、Honglu Mountain-3 (HL-3)樣體 43 第二節、土壤物理性質 46 一、總體密度 46 二、水分含量 49 三、土壤質地 52 第三節、一般土壤化學性質 55 一、pH值 55 二、有機質 59 三、陽離子交換容量、交換性鹽基與可交換性鋁 60 四、磷酸根吸持力 61 第四節、選擇性化學抽出 62 一、CBD試劑之抽出 62 二、酸性草酸銨(Acid oxalate)抽出 64 三、焦磷酸鈉抽出(Sodium pyrophosphate) 68 四、選擇性化學抽出性質之比值意義 68 五、鋁英石的生成與定量 69 第五節、土壤微形態特徵 72 一、HL-1樣體之微形態 73 二、HL-2樣體之微形態 74 三、HL-3樣體之微形態 80 第六節、礦物特徵 80 一、砂粒部分之礦物鑑定 82 二、黏土礦物的鑑定 82 (一) HL-1樣體之黏粒X光繞射分析 86 (二) HL-2樣體之黏粒X光繞射分析 86 (三) HL-3樣體之黏粒X光繞射分析 93 (四)礦物的生成與轉變 97 第七節、土壤化育作用 100 一、地形對研究樣體的影響 100 二、研究區域土壤的轉變 102 三、研究地區與其他大屯火山群地區之比較 103 第八節、土壤分類 104 第五章 結論 111 參考文獻 112 附錄 124 附錄1-1 124 附錄1-2 126 附錄1-3 128 | |
| dc.language.iso | zh-TW | |
| dc.subject | 地形土序 | zh_TW |
| dc.subject | 灰燼土 | zh_TW |
| dc.subject | 弱育土 | zh_TW |
| dc.subject | 土壤化育 | zh_TW |
| dc.subject | 火山灰土壤性質 | zh_TW |
| dc.subject | 玄武岩 | zh_TW |
| dc.subject | 安山岩 | zh_TW |
| dc.subject | 鋁–有機質複合物 | zh_TW |
| dc.subject | Pedogenesis | en |
| dc.subject | Al-humus complexes | en |
| dc.subject | Andisols | en |
| dc.subject | Inceptisols | en |
| dc.subject | Andic soil properties | en |
| dc.subject | Toposequence | en |
| dc.subject | Andesite | en |
| dc.subject | Basalt | en |
| dc.title | 台灣北部烘爐山森林土壤之特性化育與分類 | zh_TW |
| dc.title | Characteristics, Pedogenesis, and Classification of the Forest Soils in Honglu Mountain, Northern Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 104-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 許正一 | |
| dc.contributor.oralexamcommittee | 黃政恆,蔡呈奇,簡士濠 | |
| dc.subject.keyword | 灰燼土,弱育土,土壤化育,火山灰土壤性質,玄武岩,安山岩,鋁–有機質複合物,地形土序, | zh_TW |
| dc.subject.keyword | Pedogenesis,Andic soil properties,Inceptisols,Andisols,Al-humus complexes,Basalt,Andesite,Toposequence, | en |
| dc.relation.page | 129 | |
| dc.identifier.doi | 10.6342/NTU201601148 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2016-07-28 | |
| dc.contributor.author-college | 生物資源暨農學院 | zh_TW |
| dc.contributor.author-dept | 農業化學研究所 | zh_TW |
| 顯示於系所單位： | 農業化學系 | |
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