高嶺石礦物 的英文怎麼說

中文拼音 [gāolǐngdànkuàngwù]
高嶺石礦物 英文
kaolinite minerals
  • 高 : Ⅰ形容詞1 （從下向上距離大; 離地面遠） tall; high 2 （在一般標準或平均程度之上; 等級在上的） above...
  • 嶺 : 名1. （頂上有路可通行的山） mountain; ridge 2. （高大的山脈） mountain range 3. （專指大庾嶺等五嶺） the five ridges
  • 石 : 石量詞（容量單位, 十斗為一石） dan, a unit of dry measure for grain （= l00 sheng）
  • 礦 : 名詞1. （礦床） ore [mineral] deposit 2. （礦石） ore 3. （開采礦物的場所） mine
  • 物 : 名詞1 （東西） thing; matter; object 2 （指自己以外的人或與己相對的環境） other people; the outsi...
  • 高嶺 : cao lamh
  • 礦物 : mineral
  1. The metallic mineral has very few content ( 1 % - 2 % ), the mineral of ore is mainly of pyrite, chalcopyrite, limonite, aurum and electrum etc. the gangue mineral is composed of chalcedony, micro grained quartz, calsite, sericite, adularia, aragonite, chlorite, laumontite, pyrophyuite, kaolinite and so on, which show the typical mineral assemblage of epithermal

    礦石為典型少硫化物型，金屬礦物含量極少（ 1 - 2 ） ，主要有黃鐵礦、黃銅礦、褐鐵礦和自然金、銀金礦等。主要脈石礦物有玉髓、微粒石英以及方解石、絹雲母、冰長石、文石、綠泥石、濁沸石、葉臘石、高嶺石等，屬典型低溫礦物組合。
  2. 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。
  3. 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。
  4. By being compared the adsorbent rate to tio2, the minerals ( diatomite, sepiolite, vermiculite, grammite, kaoline, bentonite ) has selected elementarily in the paper

    本文通過硅藻土、海泡石、蛭石、硅灰石、高嶺石、膨潤土等六種礦物對tio _ 2的吸附效果及吸附量的比較，對天然礦物進行了初步篩選。
  5. 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。
  6. 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。
  7. 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。
  8. 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。
  9. 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。
  10. Chemical analyses showed that the former was characterized by higher sio2, k2o and lower a12o3, tio2 than the later, as well as the content of fe varying on a great range with the deposit - forming parent racks and weatering conditions

    其結果表明，風化型高嶺土的化學成分一般屬硅高鋁低型，鉀含量偏高，鈦含量低，鐵含量則隨成礦母巖和風化條件的不同波動范圍大，礦物組成主要為結晶度較差的高嶺石、水雲母和石英，以及極少量的管狀埃洛石。
  11. 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。
  12. Abstract : the resource characteristics such as the composition, texture, structure and the prospects of industrial utilizations included white carbon black, alc13, 4a zeolite, al - si alloy and rubber filler of coal - series kaolinite in huainan and huaibei mining area were introduced

    文摘:在分析了兩淮煤系高嶺巖礦石的結構和構造、礦物成分、化學成分、熱變性等性質的基礎上，探討了兩淮煤系高嶺巖資源在白炭黑、氯化鋁、 4a沸石、鋁硅系列合金、功能性填料等工業應用前景。
  13. 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。
  14. Calculated mineral composition by chemical composition combined with x - ray powder diffraction analyses showed that the former generally consisted mainly of poorly - crystallized kaolinite and small amounts of illite and quartz, and the later contained well - crystallized predominent kaolinite ( over 95 % )

    含煤建造沉積型高嶺土一般屬鋁高硅低型，鉀含量低，鈦含量明顯偏高，礦物組成簡單，高嶺石含量95 % ，結晶度較好。
分享友人
分享到 Line

分享到臉書