高嶺層 的英文怎麼說
中文拼音 [gāolǐngcéng]
高嶺層
英文
kandic horizon-
Different from potassium acetate, ammonium acetate intercalated into the inner layer of kaolinite more completely in buffer solution ( ph = 9 ) than under near dry condit ion
與乙酸鉀不同,乙酸銨與高嶺土的插層作用在ph = 9的緩沖溶液中,比在近干態下進行的完全。The i / s mixed layer and illite occur as pore lining and pore filling, while kaolinite occurs as pore filling
I s混層與伊利分佈於孔喉處或充填孔隙,而高嶺石主要充填于孔隙中。The kaolinite / acetate intercalation composites prepared by means mentioned in this paper can use as the intermedia for preparation of kaolinite / polymer nanocomposites directly
通過本法制備出的高嶺土乙酸鹽插層復合物,可以直接用作高嶺土聚合物納米復合物的中間體。Advances in kaolinite intercalation composites
高嶺石插層復合材料研究進展When the concentration of ammonium acetate is lomol / l, in
砒吒分子中的氮原子正對著高嶺土層面。Ammonium acetate can also directly insert between the inner layer of kaolinite by controlling ph strictly, but the intercalation rate is very low
在嚴格控制ph的條件下,乙酸銨也可以直接插入高嶺土層間,但插層率很低。Potassium acetate adsorbed on the surface of kaolinite particle can be eluted by absolute ethyl alcohol, while that intercalated between the inner layer of kaolinite may not be affected
用無水乙醇作洗滌液可以將吸附在高嶺土顆粒表面的乙酸鉀洗脫除去,而已經插入高嶺土層間的乙酸鉀則不受影響。The central concept of alfisols is that of soils that have an argillic, a kandic, or a nitric horizon and a base saturation of 35 % or greater
淋溶土的主要特性是有粘化層,高嶺層或氮化層和鹽基飽和度達35或以上。A fine clay used in ceramics and refractories and as a filler or coating for paper and textiles
高嶺土,瓷土一種細黏土,在制陶器和耐火材料時使用,也可用作紙張和紡織片的漿料或塗層。To join ( metals ) by applying heat, sometimes with pressure and sometimes with an intermediate or filler metal having a high melting point
高嶺土,瓷土一種細黏土,在制陶器和耐火材料時使用,也可用作紙張和紡織片的漿料或塗層。The xrd and sem indicate that the types clay consists of i / s mixed layer, illite and kaolinite. the i / s mixed layer is the most abundant mineral in the clay samples. the chlorite clay mineral has not been detected in the formation
Xrd與sem綜合分析證實,砂巖中粘土礦物由i s混層、伊利石與高嶺石組成,其中以i s混層為主,樣品中沒有發現綠泥石礦物。Kaolinite is a major host materials for the intercalation reaction
高嶺石是重要的插層反應主體。The result shows that dmso were intercalated into the interlayer of kaolinite and basal spacing was swelled from 0. 715nm to 1. 110nm, so the kaolinite - organic matter intercalation compound was formed
結果表明,二甲基亞碸進入了高嶺土的層間,層間距由0 . 715nm增加到1 . 110nm ,形成高嶺土有機插層材料。Study of kaolinite deposit within coal bed no. 11 in hancheng mining area, shaanxi
煤層中高嶺巖礦研究The employ kaolinite / polyacrylamide intercalation compound as a raw material to in - situ synthesize sialon was test by the carbothermal reduction and simultaneous nitridation ( crsn ) technique. this work was supported by the national natural science foundation of china ( grant no. 40072014 ), the natural science foundation of guangdong province ( grant no. 010496 ) and the foundation of state key laboratory for physical chemistry of solid surfaces in xiamen university ( grant no. 9911 )
研究工作得到國家自然科學基金項目《高嶺石礦物表面功能基及其反應活性研究》 (項目批準號: 40072014 ) 、廣東省自然科學基金項目《高嶺石有機插層原位合成- sialon納米材料》 (項目批準號: 010496 )和廈門大學固體表面物理化學國家重點實驗室開放基金項目(項目批準號: 9911 )的資助。Ft - ir spectrum show that water insert between the inner layer of kaolinite with potassium acetate, which form hydrogen bond with the inner surface hydroxyl of kaolinite
傅立葉變換紅外光譜顯示,水和乙酸鉀一同插入到高嶺土的層間,並與高嶺土的內表面羥基形成了氫鍵。The illite in the study area is characterized by, occurs as irregular flakes with short lath - like projection and this growth form can be confused with the mixed layer i / s, and formed in an alkaline environment. the i / s mixed layer in the study area occurs as irregular flakes with short lath - like projection
研究區伊利石形態特徵為不規則的片狀,並發育短絲,很容易與堿性環境中形成的i s混層混淆。自生高嶺石形態為片狀假六邊形或「手風琴」狀假六邊形集合體,是長石溶解或長石原地蝕變的產物。The results show that the kaolinite with low structure order degree and relative large particle size is more easily intercalated under well dispersed
具較低結構有序度、較大的顆粒粒度並充分分散的高嶺石有利於插層作用。Kaolinite - organic intercalation compound possesses not only the unique adsorptivity, dispersivity. porosity, rheological behaviour and surface acidity of the clay mineral but also the multivariate functional groups and the reactivity of the organic compound. as a new type of mineral materials, it has extensive potential application in catalysts, functional supporter, adsorbents and advance ceramics
高嶺石有機插層復合物既具有粘土礦物特有的吸附性、分散性、流變性、多孔性和表面酸性,又具有機化合物的多變功能團和反應活性,作為新型礦物材料,在催化劑、功能載體、吸附劑、先進陶瓷材料等方面具有廣闊的應用前景。Quality comparison among calcined coal - series kaolin products under different productive processes and their influences on properties of paper coating
煤系煅燒高嶺土不同生產工藝產品質量的比較及對紙張塗層性能的影響分享友人