auxiliary geophone

简明释义

1. 辅助检波器; 2. 备用检波器;

英英释义

例句

1.Using an auxiliary geophone can help in detecting smaller seismic events that might be missed by primary sensors.

使用辅助地震仪可以帮助检测到主要传感器可能遗漏的小型地震事件。

2.The seismic survey team deployed an auxiliary geophone to improve data collection in the field.

地震勘测小组部署了一个辅助地震仪以改善现场数据收集。

3.Researchers utilized an auxiliary geophone to monitor vibrations during the construction process.

研究人员利用辅助地震仪监测施工过程中的振动。

4.The data from the auxiliary geophone helped refine the geological model of the area.

来自辅助地震仪的数据有助于完善该地区的地质模型。

5.The installation of an auxiliary geophone near the drilling site provided valuable insights into subsurface conditions.

在钻探现场附近安装辅助地震仪提供了对地下条件的宝贵见解。

作文

In the field of geophysics, the use of various instruments is crucial for the accurate measurement and analysis of seismic activities. One such instrument that has gained significant importance is the auxiliary geophone. The term auxiliary geophone refers to a secondary device used alongside primary geophones to enhance the quality and reliability of seismic data collection. Typically, geophones are used to detect ground motion caused by seismic waves, and they play a pivotal role in oil and gas exploration, earthquake monitoring, and environmental studies.The primary purpose of an auxiliary geophone is to provide additional data points that can help in interpreting complex seismic signals. When deployed in conjunction with primary geophones, these auxiliary devices can improve the spatial resolution of the collected data. This is especially beneficial in areas where the geological conditions are complicated or when the primary geophones alone may not capture all the relevant seismic events.One of the advantages of using an auxiliary geophone is that it allows for the triangulation of seismic waves. By placing multiple geophones, both primary and auxiliary, at strategic locations, researchers can better determine the source and nature of seismic activities. This methodology not only enhances the accuracy of the data but also reduces the likelihood of misinterpretation that could arise from relying solely on a limited number of sensors.Moreover, the integration of auxiliary geophones into seismic surveys can significantly improve the signal-to-noise ratio. In environments where background noise is prevalent, the additional geophones can help filter out unwanted signals, allowing for clearer and more precise readings. This is particularly important in urban areas where human activities can generate substantial noise, potentially obscuring subtle seismic signals.In addition to their role in enhancing data quality, auxiliary geophones can also be used for specific applications such as monitoring landslides, assessing the stability of structures, and conducting research on subsurface geology. For instance, in landslide-prone regions, deploying a network of geophones, including auxiliary ones, can provide real-time data on ground movements, enabling timely warnings and preventive measures.Furthermore, the technological advancements in geophone design have led to the development of more sensitive and compact auxiliary geophones. These modern devices are often equipped with digital processing capabilities, allowing for real-time data analysis and transmission. This innovation has made it easier for researchers to monitor seismic activities continuously and respond promptly to any significant changes detected by the geophones.In conclusion, the auxiliary geophone plays a vital role in the field of geophysics by complementing primary geophones and enhancing the overall quality of seismic data collection. Its ability to improve data accuracy, increase spatial resolution, and filter out noise makes it an indispensable tool for researchers and professionals working in various geological and environmental contexts. As technology continues to evolve, the functionality and application of auxiliary geophones will likely expand, further contributing to our understanding of the Earth's dynamic processes and helping to mitigate risks associated with seismic events.

在地球物理学领域，各种仪器的使用对于准确测量和分析地震活动至关重要。其中一个日益重要的仪器是辅助地震仪。术语辅助地震仪指的是一种与主要地震仪一起使用的辅助设备，用于增强地震数据收集的质量和可靠性。通常，地震仪用于探测由地震波引起的地面运动，在石油和天然气勘探、地震监测和环境研究中发挥着关键作用。辅助地震仪的主要目的是提供额外的数据点，有助于解释复杂的地震信号。当与主要地震仪一起部署时，这些辅助设备可以提高所收集数据的空间分辨率。这在地质条件复杂或仅依靠主要地震仪可能无法捕捉到所有相关地震事件的区域尤为有利。使用辅助地震仪的一个优点是，它允许对地震波进行三角测量。通过在战略位置放置多个地震仪，包括主要和辅助地震仪，研究人员可以更好地确定地震活动的来源和性质。这种方法不仅提高了数据的准确性，还减少了仅依赖有限数量传感器可能导致的误解的可能性。此外，将辅助地震仪整合到地震调查中可以显著提高信噪比。在背景噪声普遍存在的环境中，额外的地震仪可以帮助过滤掉不必要的信号，从而获得更清晰、更精确的读数。这在城市地区尤其重要，因为人类活动会产生大量噪声，可能会掩盖微弱的地震信号。除了提高数据质量的作用外，辅助地震仪还可以用于特定应用，例如监测滑坡、评估结构的稳定性以及进行地下地质研究。例如，在滑坡易发区域，部署包括辅助地震仪在内的地震仪网络可以实时提供地面运动数据，从而实现及时预警和预防措施。此外，地震仪设计的技术进步导致了更灵敏和紧凑的辅助地震仪的开发。这些现代设备通常配备数字处理能力，允许实时数据分析和传输。这一创新使研究人员能够更轻松地持续监测地震活动，并迅速对检测到的任何重大变化做出反应。总之，辅助地震仪在地球物理学领域发挥着至关重要的作用，通过补充主要地震仪并增强整体地震数据收集的质量。它提高数据准确性、增加空间分辨率和过滤噪声的能力，使其成为研究人员和专业人士在各种地质和环境背景下不可或缺的工具。随着技术的不断发展，辅助地震仪的功能和应用可能会进一步扩展，为我们理解地球的动态过程作出更多贡献，并帮助减轻与地震事件相关的风险。