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題 名 | 金門島之紅土 |
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作 者 | 張仲民; | 書刊名 | 中華農學會報 |
卷 期 | 92 1975.12[民64.12] |
頁 次 | 頁112-126 |
關鍵詞 | 金門島; 紅土; |
語 文 | 中文(Chinese) |
中文摘要 | 金門島覆蓋最廣之土壤,主要為起源自更新世之沉積物,在本研究中所特別著重者為各土壤之徵斷層和其性質,藉以解決分類,生產力和土壤管理問題。各供試土壤之特徵為深厚、紅色、粘質、酸性與低鹽基含量狀況,粘粒部分主要由高領石類及變異數之粘粒雲母,水鋁氧,錯層礦物與無定型物所組成。自田間觀察與實驗室內分析結果判斷,各供試土皆可被分類為Rhodustult土壤。 |
英文摘要 | The most widespread soils of Chinmen Island are derived mainly from Pleistocene sediments. The special attention in this study was given to the diagnostic horizons and their properties to elucidate the problems of classification, productivity, and management of the soils under investigation. They are characterized by deep, red, clayey, acid and a very low base-status soils, clay separates of the soils consisted mainly of kaolinite minerals with varying amounts of clay-mica, gibbsite, mixed layers and amorphous materials. Judging from the results of field observations and laboratory analyses, they might be classified as Rhodustult soils. |
本系統中英文摘要資訊取自各篇刊載內容。