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铀235的英文

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"铀235"怎么读用"铀235"造句

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  • uranium-235

例句与用法

  • It is necessary to enrich the fuel by increasing the percentage concentration of uranium-235 .
    必须提高铀235浓度的百分比,使燃料浓集。
  • A second prerequisite is that uranium 235 must be present in sufficient abundance
    第二个必要条件是,铀235的含量必须够充足。
  • Determination of the u isotopic content in uranium containing nuclear fuel solutions by spectrometry
    光谱分析测定含铀核燃料溶液中铀235同位素含量
  • Standard test method for analysis of urine for uranium - 235 and uranium - 238 isotopes by inductively coupled plasma - mass spectrometry
    用感应耦合等离子体质谱法分析铀235和铀238同位素用尿的标准试验方法
  • For in ordinary uranium there is much more of the u238 isotope than there is u235 and , as you know , u238 will not undergo fission easily
    因为在普通铀中,铀238同位素要比铀235多得多,而且正如你所知,铀238不易裂变。
  • Today even the most massive and concentrated uranium deposit cannot become a nuclear reactor , because the uranium 235 concentration , at less than 1 percent , is just too low
    今日,即使是最巨大、最精纯的铀矿,都无法成为核反应堆,因为其中铀235的含量小于1 % ,太低了。
  • But this isotope is radioactive and decays about six times faster than does uranium 238 , which indicates that the fissile fraction was much higher in the distant past
    但是,铀235是具放射性的,而且衰变的速度比铀238快六倍,表示在古代,这个易分裂同位素的比率,比现在高得多。
  • When the metal rods of cadmium were pushed all the way in , and stray neutrons that entered the pile were absorbed , and could not enter uranium ? 235 nuclei , and so there was no reaction at all
    当镉金属棒全部推入,进入反应堆的流动中子就被吸收,不能进入铀235原子核,因而完全没有反应。
  • Cowan described , for example , how some of the neutrons released during the fission of uranium 235 were captured by the more abundant uranium 238 , which became uranium 239 and , after emitting two electrons , turned into plutonium 239
    例如,柯文描述了某些铀235分裂所释放的中子,如何被含量更多的铀238捕捉而产生铀239 ,在放射出两个电子后又变成钸239 。
  • Most of earth ' s internal heat is generated by four long - lived radioisotopes ? potassium 40 , thorium 232 , uranium 235 and uranium 238 ? that release energy over billions of years as they decay into stable isotopes
    地球内部的热能主要来自半衰期较长的四种放射性同位素钾40 、钍232 、铀235与铀238 ,它们在几十亿年来逐渐衰变成稳定的同位素,同时释放能量。
  • 更多例句:  1  2
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