水生成
- 与 水生成 相关的网络例句 [注:此内容来源于网络,仅供参考]
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A two-dimensional, two-phase and multi-component transport model was developed for the cathode of PEM fuel cell using interdigitated gas distributor.
对叉指型质子交换膜燃料电池阴极提出一个二维两相的多组分流体输运模型,应用连续性方程和Darcy定律以及组分扩散方程描述了反应气体和生成水的流动和传质。
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It is yellow of course; It is the most rudimentary to be blue and green, it is the color of common people's clothes.
这是一种存在于靛蓝草枝叶中的物质,经发酵后产生可溶性的白色溶液,将织物浸泡在这种溶液中后取出,在空气中氧气的氧化作用下生成不溶于水的青蓝色,它耐日晒水洗和加热。
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Typically, an acid and a base react to form a salt and water.
典型地,酸和碱反应生成盐和水。
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Hence, for the whole process, the reaction consumed equivalent of halogen acid and alcohol to produce halide and water.
反应实际消耗的是等当量的氢卤酸和醇生成卤代烃和水,是制备伯卤代烃非常有效和清洁的方法。
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It generated through the water, not only can directly drink, but is a measurable, to ensure that health and safety of health-weak alkaline water.
通过它生成的水,不但可直接饮用,而且是一种可计量,确保卫生安全的健康弱碱性离子水。
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In the samples containing aluminum sulphate, some ettringite crystalparticles are formed, which do not match with dihydrate gypsum crystals and increase thedefects in the hardened plaster. The strength decreases sharply with increase of aluminumsulphate amount.
硫酸铝的引入,使石膏浆体中生成部分钙矾石晶体,钙矾石晶体与二水石膏晶体不匹配,从而增加了硬化体内部的缺陷,因此,随着硫酸铝掺入量的增加,硬化体强度的降低比较严重。
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In general as long as the temperature reaches 90 ℃, the common E. coli, hepatitis B virus and other bacteria have already perished, but we still continue to boil water, this area is to allow water in the calcium carbonate, magnesium carbonate and other ingredients to fully precipitate impurities, and the other On the one hand, because I am using tap water is treated with chlorine, so a certain degree of residual chlorine in water, in the process of boiling water, chlorine and impurities in the water will generate harmful substances called chloroform.
在一般的长期的温度达90℃,普通大肠杆菌,乙型肝炎病毒和其他细菌已经死亡,但我们仍烧开水,这方面是允许的碳酸钙,碳酸镁和其他水成分,杂质充分沉淀,以及对其他一方面,因为我使用的自来水是用氯处理,因此在水中的余氯,在一定程度上开水,氯和水中杂质的过程中,将生成所谓有害物质氯仿。
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Methods IO(superscript - subscript 3) was prepared by quantitative oxidation of bromine water, with the excessive bromine removed with formic acid. In the presence of excessive iodide, I(superscript -) would be oxidized by I(superscript - subscript 3) to form 3 times of I(superscript - subscript 3) in mol, displaying maximal absorption at 286nm in ultraviolet zone and a slightly low apex at 345nm.ε286=1.3×10^5 Lmol^(-1)cm^(-1),ε345=8.1×10^4 Lmol^(-1)cm^(-1), with both showing high sensitivity.
利用溴水定量氧化I生成IO(上标-下标 3),再用甲酸除去过量的溴,IO(上标-下标 3)在过量碘化物存在下氧化I产生3倍摩尔量的I(上标-下标 3),在紫外光区的286nm具有最大吸收,并在345nm处另有一略低的吸收峰,ε286=1.3×10^5 Lmol^(-1)cm^(-1),ε345=8.1×10^4 Lmol^(-1)cm^(-1),均具有很高的灵敏度。
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Low levels of the crust, melting point 3180 ℃, boiling point 5627 ℃, the relative density of 2053, the external F electronic structure 5d56s2, reaction time will be lost 1-7 electronic, but also can capture an electron, so oxidation number of 0,± 1, 2 , 3, 4, 5, 6 and 7, rhenium with the halogen in the fluorine, chlorine, bromine reaction halides dissolved in water, can dissolve in nitric acid and ammonia hydrogen peroxide solution, but do not dissolve in hydrochloric acid.
地壳中含量很低,熔点3180℃,沸点5627℃,相对密度2053,外围F 电子结构5d56s2,反应时会丢失1—7个电子,也可捕获一个电子,所以氧化数为0、±1、+2、+3、+4、+5、+6和+7,铼能与卤素中的氟、氯、溴反应生成溶于水的卤化物,能溶于硝酸和含氨过氧化氢等溶液,但不溶于盐酸。
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The result shows that geopolymeric reaction is occurred when metakaolinte is activated by the compound solution of sodium silicate and sodium hydroxide, and the amorphous geopolymeric cement with layer structure and combination water is then formed.
结果表明:在氢氧化钠溶液和水玻璃的混合溶液的激发下偏高岭石发生了土壤聚合反应,生成了无定形的土聚水泥;该土聚水泥呈层状结构并含有非结合水
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。