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Abstract <p>X-ray photons (with an energy of more than 10 keV) have been detected using photometers-spectrometers developed at the Skobeltsyn Institute of Nuclear Physics, Moscow State University, similar to those used to detect X-rays from high-altitude discharges in orbital experiments, during the laboratory simulation using the Marx GROZA GIN-1MV generator installed at the Institute of Applied Physics, Russian Academy of Sciences. Several cases of the appearance of X-ray photons with an energy of ~20 to 160 keV have been detected, including those simultaneously in several detectors. Indications are received that it was possible to detect real X-ray photons during the laboratory experiments on the simulation of lightning discharges, which corresponds to the predictions of theoretical models and data of orbital and ground-based observations.</p>

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X-Ray Radiation of Long Spark Discharges in a Laboratory Experiment

  • 期刊论文

  • 发表日期：

    2025年2月1日

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  • E. A. Mareev,
  • Yu. V. Shlyugaev,
  • M. V. Shatalina,
  • F. G. Sarafanov,
  • A. A. Belov,
  • V. V. Bogomolov,
  • A. F. Iyudin,
  • P. A. Klimov,
  • N. A. Popov,
  • R. E. Saraev,
  • S. I. Svertilov,
  • I. V. Yashin

摘要

Abstract

X-ray photons (with an energy of more than 10 keV) have been detected using photometers-spectrometers developed at the Skobeltsyn Institute of Nuclear Physics, Moscow State University, similar to those used to detect X-rays from high-altitude discharges in orbital experiments, during the laboratory simulation using the Marx GROZA GIN-1MV generator installed at the Institute of Applied Physics, Russian Academy of Sciences. Several cases of the appearance of X-ray photons with an energy of ~20 to 160 keV have been detected, including those simultaneously in several detectors. Indications are received that it was possible to detect real X-ray photons during the laboratory experiments on the simulation of lightning discharges, which corresponds to the predictions of theoretical models and data of orbital and ground-based observations.