臺灣博碩士論文加值系統

土壤質量平衡研究，運用風化前後母質與土壤中化學元素組成、容積密度及土壤體積的改變，了解在土壤化育過程，剖面中不同元素的增添、流失與轉移情形，以提供一個土壤形成與外部環境的相關連結。
經測定台灣中部大肚台地與新社地區河階土壤的巨量與微量元素，藉由多變量主成分分析，發現新社地區HS-1b與大肚台地TD-b同屬大甲溪流域，但大肚台地TD-a與TD-c則為大肚溪流域混有不同程度之大甲溪沖積物質，顯示本區為一複雜的沉積環境，故後續進行土壤剖面質量平衡計算時，可能無法以現代河砂作為基準母質，因此採用土壤剖面的最底層作為假定之母質，進行計算；其次，並以在風化過程中相對不易移動的鋯元素，作為風化前後體積計算之基準，結果顯示剖面中各種元素流失與增添情形不同，鹽基陽離子中鉀元素流失量遠大於其他元素，鎂元素少量流失，而鈉元素則有增添的現象，應與外部輸入有關，再者，鐵、鋁、錳元素有發生粒徑轉移與剖面分布位置移動之現象，尤以鐵元素最為明顯，而鈦元素流失情形不顯著，呈現其相對穩定之特性。
藉由土壤元素之流失量評估土壤化育程度，大肚台地三個土壤剖面的化育程度應大於新社地區之土壤剖面，而由定年資料與元素流失總量推估新社HS-1b化學風化速率，得知鹽基陽離子的化學風化速率高於其他元素，最後，由元素化學風化速率回推大肚台地不同階地相對年代，發現TD-a與TD-b化育年代相當，至少應有200~210 ka。

第一章 緒論 1
第一節 研究動機與目的 1
第二節 前人研究 2
第二章 研究區概述 12
第一節 自然環境 12
第三章 材料與方法 19
第一節 土壤採樣與剖面描述 19
第二節 土壤理化性質分析 20
第三節 土壤質量平衡理論 23
第四節 長期化學風化速率推估 27
第四章 大肚台地與新社地區土壤性質與元素分析 28
第一節 土壤樣體形態特徵 28
第二節 土壤理化性質分析 37
第五章 紅土來源與質量平衡分析 56
第一節 土壤母質來源 56
第二節 土壤質量平衡計算 60
第三節 土壤化育程度與化學風化速率 76
第六章 結論 78
參考文獻 79
附錄 86

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