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首页> 外文期刊>Journal of Applied Geophysics >Detection of microwave emission due to rock fracture as a new tool for geophysics: A field test at a volcano in Miyake Island, Japan
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Detection of microwave emission due to rock fracture as a new tool for geophysics: A field test at a volcano in Miyake Island, Japan

机译:探测由于岩石破裂而产生的微波发射,这是地球物理的一种新工具:在日本三宅岛的一座火山上进行的现场测试

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This paper describes a field test to verify a newly discovered phenomenon of microwave emission due to rock fracture in a volcano. The field test was carried out on Miyake Island, 150. km south of Tokyo. The main objective of the test was to investigate the applicability of the phenomenon to the study of geophysics, volcanology, and seismology by extending observations of this phenomenological occurrence from the laboratory to the natural field.We installed measuring systems for 300. MHz, 2. GHz, and 18. GHz-bands on the mountain top and mountain foot in order to discriminate local events from regional and global events. The systems include deliberate data subsystems that store slowly sampled data in the long term, and fast sampled data when triggered. We successfully obtained data from January to February 2008. During this period, characteristic microwave pulses were intermittently detected at 300. MHz. Two photographs taken before and after this period revealed that a considerably large-scale collapse occurred on the crater cliff. Moreover, seismograms obtained by nearby observatories strongly suggest that the crater subsidence occurred simultaneously with microwave signals on the same day during the observation period.For confirmation of the microwave emission caused by rock fracture, these microwave signals must be clearly discriminated from noise, interferences, and other disturbances. We carefully discriminated the microwave data taken at the mountaintop and foot, checked the lightning strike data around the island, and consequently concluded that these microwave signals could not be attributed to lightning. Artificial interferences were discriminated by the nature of their waveforms. Thus, we inferred that the signals detected at 300. MHz were due to rock fractures during cliff collapses. This result may provide a useful new tool for geoscientists and for the mitigation of natural hazards.
机译:本文描述了一项现场测试,以验证新发现的因火山岩中的岩石破裂而引起的微波发射现象。现场测试是在东京以南150公里的三宅岛进行的。该测试的主要目的是通过将这种现象学现象的观察范围从实验室扩展到自然界,从而研究该现象在地球物理,火山学和地震学研究中的适用性。我们安装了300. MHz,2的测量系统。 GHz,以及在山顶和山脚的18 GHz频段,以便将本地事件与区域和全球事件区分开来。该系统包括蓄意的数据子系统,该子系统长期存储缓慢采样的数据,并在触发时存储快速采样的数据。我们成功获得了2008年1月至2008年2月的数据。在此期间,间歇性地在300. MHz处检测到了特征性的微波脉冲。在此之前和之后拍摄的两张照片显示,火山口悬崖发生了相当大的坍塌。此外,附近观测站获得的地震图强烈表明,在观测期间的同一天,陨石坑沉降与微波信号同时发生。为了确认岩石破裂引起的微波发射,必须将这些微波信号与噪声,干扰,和其他干扰。我们仔细区分了在山顶和山脚处采集的微波数据,检查了岛屿周围的雷击数据,因此得出结论,这些微波信号不能归因于闪电。人为干扰通过其波形的性质来区分。因此,我们推断在300 MHz处检测到的信号是由于悬崖倒塌期间的岩石破裂所致。这一结果可能为地球学家和减轻自然灾害提供有用的新工具。

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