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首页> 外文期刊>Geophysical Prospecting >Calibration shifts in Scintrex CG-3M gravimeters with an application to detection of microgravity changes at Iwo-tou caldera, Japan
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Calibration shifts in Scintrex CG-3M gravimeters with an application to detection of microgravity changes at Iwo-tou caldera, Japan

机译:Scintrex CG-3M重力仪的标定变化及其在日本硫磺破火山口微重力变化检测中的应用

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摘要

Calibration shift seriously influences gravity values measured using Scintrex CG-3M gravimeters. We calibrated three Scintrex CG-3M gravimeters three times (1999, 2003 and 2006) over eight years, using a calibration line with a gravity difference of 1.38 Gal. The scale factor correction coefficients (calibration factors) obtained here range from 0.9998-1.0005. The calibration factors vary with time by 89 ppm, -102 ppm and -126 ppm between the 1999-2003 surveys. The calibration shifts of two of the three gravimeters decreased to about 20 ppm or less in the second interval, the other remained about the same (142 ppm). The results indicate that they shifted at rates on the order of 10 ppm/year even several years after manufacturing. The large shift in calibration factors indicates that they must be corrected using calibrations done before and after the measurements to perform microgravity measurements when gravity differences between a reference gravity site and survey sites are on the order of a hundred milligals (mGal) or more. The results also indicate that the calibration factors change gradually with time, so their interpolation provides a good practical approximation for a specific survey time. We applied the time-dependent calibration factors to microgravity monitoring at the Iwo-tou caldera, Japan, where the gravity difference between the base site on the island and the reference site on Honshu (the mainland of Japan) is about 870 mGal mainly due to the 11° latitude difference. Gravity surveys were conducted every two years from 1998-2006. The correction of scale factors estimated from the repeated calibration surveys leads to satisfactory measurements, in which the average of the absolute differences between two Scintrex CG-3M instruments in five surveys is reduced from 207μGal to 19μGal; for three of those surveys, it is less than 10 μGal. This result demonstrates the importance of repeated calibration surveys.
机译:校准偏差会严重影响使用Scintrex CG-3M重力仪测量的重力值。我们使用重力差值为1.38 Gal的校准线在八年内对三台Scintrex CG-3M重力仪进行了三次校准(1999、2003和2006)。此处获得的比例因子校正系数(校正因子)范围为0.9998-1.0005。在1999-2003年的调查之间,校准因子随时间变化89 ppm,-102 ppm和-126 ppm。在第二时间间隔内,三个重力仪中的两个的校准位移降低到约20 ppm或更小,另一个保持相同(142 ppm)。结果表明,即使在制造后的几年内,它们的移动速率仍约为10 ppm /年。校准因子的较大变化表明,当参考重力站点和测量站点之间的重力差在100毫克(mGal)或更高的数量级时,必须使用在测量之前和之后进行的校准进行校正以执行微重力测量。结果还表明,校准因子随时间逐渐变化,因此它们的插值为特定的测量时间提供了良好的实用近似。我们将随时间变化的校准因子应用于日本硫磺火山口的微重力监测,该岛的基地站点与本州(日本大陆)参考站点之间的重力差约为870 mGal。 11°的纬度差。从1998年至2006年,每两年进行一次重力调查。通过重复校准调查估算出的比例因子的校正可得出令人满意的测量结果,其中五次调查中两台Scintrex CG-3M仪器之间的绝对差的平均值从207μGal降低至19μGal。对于其中三个调查,该值小于10μGal。该结果证明了重复校准调查的重要性。

著录项

  • 来源
    《Geophysical Prospecting》 |2010年第6期|p.1123-1132|共10页
  • 作者单位

    National Research Institute for Earth Science and Disaster Prevention, Tennodai 3-1, Tsukuba-shi, Ibaraki-ken 3005-0006, Japan;

    OYO Corporation, Miyukigaoka 43, Tsukuba-shi, Ibaraki-ken 3005-0841, Japan;

    rnNational Research Institute for Earth Science and Disaster Prevention, Tennodai 3-1, Tsukuba-shi, Ibaraki-ken 3005-0006, Japan;

    rnNational Research Institute for Earth Science and Disaster Prevention, Tennodai 3-1, Tsukuba-shi, Ibaraki-ken 3005-0006, Japan;

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

    gravimeter calibration; gravity;

    机译:重力仪校准重力;

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