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环己烷

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In the first part, the structures of two orthorhombic forms of trypsin crystals in cyclohexane were studied.

本论文的第一部分工作研究了胰蛋白酶正交晶系两种不同晶型的晶体在环己烷中的晶体结构。

To establish gas chromatography method for determination of methyl cyclohexane in workplace air.

目的 建立工作场所空气中甲基环己烷的气相色谱测定方法。

The influences of solvent, reaction temperature, and time on the conversion of cyclohexane were examined.

环己烷氧化为探针反应,考察了上述负载催化材料的催化性能并分析了不同金属离子或取代基对催化剂活性及选择性的影响。

The oxidation of cyclohexane is still one of the major challenges of modern catalysis.

因此,寻找温和、高效的环己烷氧化的方法,是一个非常有意义,且具有挑战性的难题。

The water used as extractor, ethanol aqueous solution and cyclohexane were obtained by means of extraction.

研究了物理化学二元液系相图实验中产生的乙醇-环己烷废液的回收利用方法。

The results showed that the crystals with high density form could bear long soaking time in cyclohexane.

实验表明,堆积密度高的胰蛋白酶晶体可以经受环己烷长时间的浸泡。

On the basis of production experience, the main reason for the system fouling during the oxidation of cyclohexane is discussed, and methods to prevent the fouling are introduced.

根据生产实践经验,论述了环己烷氧化过程中系统结渣的主要原因,及对结渣问题采取的措施。

It was proved through analysis by liquid chromatography that the strain could utilize cyclohexane.

通过液相色谱法分析代谢产物,也证明了该菌株可以利用环己烷

Their catalytic performances for the oxidation of cyclohexane in water under mild condition were also studied.

应用所得到的模拟酶在温和条件下以水作为溶剂、叔丁基过氧化氢为氧化剂,液相中催化环己烷的选择氧化反应。

By comparing the non-catalytic and catalytic oxidation of cyclohexane, the free radical mechanism of the oxidation was discussed in detail.

通过比较分析,讨论了环己烷液相氧化的链式反应机理。

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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。

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。

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。