| 单词 | 铝硅酸盐 |
| 释义 | 〔clay〕A fine-grained, firm earthy material that is plastic when wet and hardens when heated, consisting primarily of hydrated silicates of aluminum and widely used in making bricks, tiles, and pottery.粘土，泥土：一种磨细的、坚固的土质材料，潮湿时是可塑的而加热时变硬，主要由含氢铝硅酸盐组成，广泛用于砖、瓦和瓷器的制造中〔plagioclase〕Any of a common rock-forming series of triclinic feldspars, consisting of mixtures of sodium and calcium aluminum silicates. Also called oligoclase 斜长岩：三斜晶长石系列中一种普通的成岩石，由钠和钙铝硅酸盐组成 也作 oligoclase〔leucite〕A white or gray mineral of potassium aluminum silicate, KAlSi2O 6. 白榴石：一种白色或灰色的钾铝硅酸盐矿物，KAlSi2O 6 〔zeolite〕Any one of a family of hydrous aluminum silicate minerals, whose molecules enclose cations of sodium, potassium, calcium, strontium, or barium, or a corresponding synthetic compound, used chiefly as molecular filters and ion-exchange agents.沸石：水合的铝硅酸盐矿物的一种，它的分子包括钠、钾、钙、锶、钡的阳离子或相同的人工化合物，主要用于分子过滤和离子交换的催化剂〔feldspar〕Any of a group of abundant rock-forming minerals occurring principally in igneous, plutonic, and some metamorphic rocks, and consisting of silicates of aluminum with potassium, sodium, calcium, and, rarely, barium. About 60 percent of the earth's outer crust is composed of feldspar.长石：任何一组由大量岩石形成的矿物，主要存在于火成岩、深成岩以及一些变性的岩石中，含有钾、钠、钙及极少的钡的铝硅酸盐，地球的外层地壳中约百分之六十是长石〔sapphirine〕A rare light blue or green aluminum-magnesium silicate mineral.假蓝宝石：一种稀有的浅蓝色或绿色的镁-铝硅酸盐组成的矿物〔bentonite〕An absorbent aluminum silicate clay formed from volcanic ash and used in various adhesives, cements, and ceramic fillers.膨润土，斑脱土：由火山灰形成的一种具有吸附能力的铝硅酸盐粘土，用于各种粘合剂、水泥和陶瓷填料〔mica〕Any of a group of chemically and physically related aluminum silicate minerals, common in igneous and metamorphic rocks, characteristically splitting into flexible sheets used in insulation and electrical equipment.云母：化学上和物理上有联系的铝硅酸盐矿物群的总称，常见于火成岩和变质岩中，以易裂成柔软的薄片为特征，用于绝缘体及电气设备中〔pyrophyllite〕A silvery white or pale green aluminum silicate mineral, Al2Si 4O 10(OH) 2, occurring naturally in soft, compact masses. 叶腊石：一种银白色或浅绿色的铝硅酸盐矿石，Al2Si 4O 10(OH) 2，在松软紧密的矿堆中自然产生 |
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