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首页> 外文期刊>Advances in space research >Experimental characterization of elastomeric O-rings as reusable seals for mass spectrometric measurements: Application to in situ K-Ar dating on Mars
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Experimental characterization of elastomeric O-rings as reusable seals for mass spectrometric measurements: Application to in situ K-Ar dating on Mars

机译:弹性O形圈作为可重复使用的密封件以进行质谱测量的实验特性:在火星上原位K-Ar测年中的应用

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摘要

Mass spectrometry has been widely used in lander missions to characterize the volatiles in rocks and soils on planetary surfaces. A good vacuum seal is very important for introducing such solid samples to a vacuum chamber and ejecting them. However, multiple measurements require many metal gaskets, leading to extra weight and complexity for the instruments. In this study, we investigate the capability of three kinds of elastomeric O-rings (Viton, Nexus-SLT, and Nexus-FV) as vacuum seals for mass spectrometric measurements, particularly for in situ K-Ar dating on Mars. First, thermal cycle tests revealed that low-temperature-resistant O-rings can maintain pressure <10~(−5) Pa at −60 °C under 1 bar ambient pressure, whereas Viton O-rings leaked at −25 °C. Then, the amount of ~(40)Ar due to outgassing from the O-rings and permeation under the ambient pressure of 650 Pa or 3 Pa was measured and compared with the amounts of ~(40)Ar that a flight-equivalent laser would liberate from potential target Martian rocks. The measured amounts were <1% of that a target rock with 5000 ppm K_2O and an age of 4.2 Ga would yield. These results suggest that a Viton O-ring can maintain the Ar blank low under the Mars atmospheric pressure when temperatures are higher than −25 °C. A double O-ring seal using the low-temperature-resistant elastomers would be an alternative approach at lower temperatures. The elastomeric O-rings would be useful for constructing a small and light-weighted mass spectrometric instrument for in situ K-Ar dating on Mars.
机译:质谱已广泛用于着陆任务,以表征行星表面岩石和土壤中的挥发物。良好的真空密封对于将此类固体样品引入真空室并将其排出非常重要。但是,多次测量需要许多金属垫片,从而导致仪器额外的重量和复杂性。在这项研究中,我们研究了三种弹性O形圈(Viton,Nexus-SLT和Nexus-FV)作为真空密封进行质谱测量的能力,尤其是对于火星上原位K-Ar测年的能力。首先,热循环测试表明,耐低温O型圈在1 bar环境压力下于-60°C时可保持压力<10〜(-5)Pa,而Viton O型圈在-25°C时泄漏。然后,测量由于从O形圈脱气和在650 Pa或3 Pa的环境压力下渗透而导致的〜(40)Ar量,并将其与飞行等效激光所产生的〜(40)Ar量进行比较。从潜在的目标火星岩石中解放出来。测得的量不到具有5000 ppm K_2O和4.2 Ga年龄的目标岩石的1%。这些结果表明,当温度高于-25°C时,Viton O形圈可以在火星大气压力下将Ar坯料保持在较低水平。使用较低温度的弹性体的双O形圈密封将是在较低温度下的替代方法。弹性体O形圈可用于构建小型轻质质谱仪,用于在火星上进行原位K-Ar测年。

著录项

  • 来源
    《Advances in space research》 |2017年第7期|1453-1462|共10页
  • 作者单位

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo, Japan;

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Department of Physics, Rikkyo University, 3-34-1 Nishi-Ikebukuro, Toshima, Tokyo, Japan;

    Earthquake Research Institute, The University of Tokyo, 1-1-1 Yayoi, Bunkyo, Tokyo, Japan;

    Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo, Japan;

    Department of Earth and Planetary Sciences, Kyushu University, 744 Motooka, Nishi, Fukuoka, Japan;

    Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo, Japan,Research Center for the Early Universe, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo, Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Elastomeric O-rings; In-situ K-Ar dating; Noble gas mass spectrometry; Outgassing; Permeation; Planetary missions;

    机译:弹性O型圈;原位K-Ar约会;稀有气体质谱法;放气;渗透行星任务;

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