kaolinite minerals 中文意思是什麼
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Burial diagenesis can cause the kaolinite group of minerals to be neoformed, transformed or destroyed.
埋藏成巖作用能使高嶺石類礦物新生變形，轉化或消失。 -
Of these minerals, kaolinite, illite and chlorite are commonest.
在這些礦物中，高嶺石，伊利石和綠泥石最常見。 -
Abstract : starting from the crystal structural characteristics and through the theoretical calculation of the chemical bonds of diasporite and kaolinite structures and the study of the flotability of the flotation systems of anionic collector ( sodium oleate ) and cationic collector ( dodecylamine ), the relationship between the crystal structural characteristics and the flotability of diasporite and kaolinite and the main causes for the difference in their flotability are analysed by the crystal chemical theory of minerals
文摘:從一水硬鋁石和高嶺石的晶體結構特徵出發，通過對一水硬鋁石和高嶺石結構中化學鍵的理論計算及陰離子捕收劑（油酸鈉） 、陽離子捕收劑（十二胺）浮選體系中可浮性的研究，採用礦物晶體化學理論分析了礦物晶體結構特徵與可浮性之間的關系，以及產生一水硬鋁石和高嶺石可浮性差異的主要原因。 -
An experimental study of ecological restoration of mining wasted lands of kaolinite minerals in south china
南方高嶺土采礦廢棄地生態恢復試驗研究 -
Clay minerals are of illite, chlorite, kaolinite and smectite assemlblage. the content of illite is very high and its crystallinity index is high too, which indicate the cool and arid climate condition in the time of sediment conformation
粘土礦物組合為伊利石、綠泥石、高嶺石和蒙皂石，伊利石含量占絕對優勢，其結晶度指數（ hw ）較高，反映東海南部外陸架粘土形成於寒冷乾燥的氣候環境。 -
With the intermittent activity of hot fluid containing cc ^, ferrous carbonate minerals dissolved and precipitate repeatedly many times. in addition, dissolution of shells and feldspars, decrease of chlorite and increase of kaolinite could be found
隨著富co _ 2熱流體多次間歇性入侵導致了含鐵碳酸鹽礦物的反復多次溶解和沉澱、生物介殼大量溶蝕和長石鑄模孔的形成以及綠泥石消失、高嶺石增加等。 -
Kaolinite - organic intercalation has an important signification for researching the kaolinite structure and understanding reaction mechanism between natural organic matters and minerals
高嶺石有機插層反應對于探測高嶺石內部微結構特徵、了解環境中有機物與礦物的作用機制具有重要意義。 -
The research now mainly concentrate on polymer / montmorillonite nanocomposites. having typical layered structure, kaolinite and montmorillonite are all ideal host minerals for preparing polymer / layered silicate nanocomposites by intercalation composite method
高嶺土與蒙脫土同屬于層狀硅酸鹽，兩者都具有典型的層狀結構，是用插層復合法制備聚合物層狀硅酸鹽納米復合材料理想的主體礦物。
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