areal geophone array

简明释义

1. 面积检波器组合; 2. 面积组合检波;

英英释义

例句

1.By analyzing data from the areal geophone array, scientists can better understand wave propagation in different geological formations.

通过分析来自面状地震检波阵列的数据，科学家可以更好地理解不同地质构造中的波传播。

2.The areal geophone array helped identify potential earthquake hazards in the region.

该面状地震检波阵列帮助识别该地区潜在的地震危险。

3.Researchers used an areal geophone array to monitor the vibrations caused by nearby construction activities.

研究人员使用面状地震检波阵列监测附近施工活动引起的振动。

4.An areal geophone array was installed across the valley to capture seismic events more effectively.

在山谷中安装了一个面状地震检波阵列，以更有效地捕捉地震事件。

5.The deployment of an areal geophone array in the seismic survey allowed for high-resolution imaging of the subsurface.

在地震勘测中部署一个面状地震检波阵列，可以高分辨率成像地下结构。

作文

In the field of geophysics, understanding subsurface structures is crucial for various applications such as oil and gas exploration, mineral prospecting, and environmental studies. One of the key technologies employed in this endeavor is the use of an areal geophone array, which significantly enhances the ability to detect and analyze seismic waves generated by natural or artificial sources. An areal geophone array refers to a systematic arrangement of geophones across a specific area, designed to capture seismic data with high spatial resolution.Geophones are devices that convert ground motion into electrical signals, allowing researchers to study the characteristics of seismic waves. When these geophones are deployed in an areal geophone array, they work collaboratively to provide a comprehensive picture of the subsurface geology. The spatial distribution of the geophones in the array enables the collection of data from multiple angles, improving the accuracy and reliability of the seismic information gathered.The deployment of an areal geophone array involves careful planning and consideration of various factors, including the geological characteristics of the area, the type of seismic sources being used, and the desired resolution of the data. For instance, in areas with complex geological formations, a denser array may be necessary to capture the intricacies of the subsurface features. Conversely, in more homogeneous regions, a sparser array might suffice. This flexibility in design allows geophysicists to tailor their approach based on the specific objectives of their study.One of the primary advantages of using an areal geophone array is the enhancement of data quality through redundancy. Since multiple geophones are recording the same seismic event, any noise or interference affecting one geophone can often be mitigated by the data collected from others. This redundancy not only improves the signal-to-noise ratio but also provides a more robust dataset for analysis.Moreover, the data obtained from an areal geophone array can be processed using advanced algorithms and modeling techniques to create detailed images of the subsurface. Techniques such as seismic tomography and inversion methods allow geophysicists to interpret the data and visualize the geological structures beneath the surface. These interpretations are essential for making informed decisions in resource exploration and environmental assessments.In conclusion, the utilization of an areal geophone array represents a significant advancement in geophysical research. By enabling the collection of high-resolution seismic data, it facilitates a deeper understanding of subsurface geology, ultimately contributing to more effective exploration and management of natural resources. As technology continues to evolve, the capabilities of areal geophone arrays will likely expand, further enhancing our ability to explore and understand the Earth's subsurface dynamics.

在地球物理学领域，了解地下结构对石油和天然气勘探、矿产勘查以及环境研究等各种应用至关重要。为此，采用的关键技术之一是使用面状地震检波器阵列，它显著增强了探测和分析自然或人工源产生的地震波的能力。面状地震检波器阵列指的是在特定区域内系统性地排列的地震检波器，旨在以高空间分辨率捕捉地震数据。地震检波器是将地面运动转换为电信号的设备，使研究人员能够研究地震波的特性。当这些地震检波器在面状地震检波器阵列中部署时，它们协同工作，以提供地下地质的全面图像。阵列中地震检波器的空间分布使得从多个角度收集数据成为可能，从而提高了所收集地震信息的准确性和可靠性。部署面状地震检波器阵列需要仔细规划，考虑到多种因素，包括该区域的地质特征、使用的地震源类型以及所需的数据分辨率。例如，在地质构造复杂的地区，可能需要更密集的阵列以捕捉地下特征的复杂性。相反，在更均匀的区域，较稀疏的阵列可能就足够了。这种设计的灵活性使地球物理学家可以根据研究的具体目标量身定制他们的方法。使用面状地震检波器阵列的主要优点之一是通过冗余提高数据质量。由于多个地震检波器记录相同的地震事件，因此影响一个地震检波器的任何噪声或干扰通常可以通过其他地震检波器收集的数据来减轻。这种冗余不仅提高了信噪比，还为分析提供了更强大的数据集。此外，从面状地震检波器阵列获得的数据可以使用先进的算法和建模技术进行处理，以创建详细的地下图像。地震层析成像和反演方法等技术使地球物理学家能够解释数据并可视化地下结构。这些解释对于在资源勘探和环境评估中做出明智的决策至关重要。总之，利用面状地震检波器阵列代表了地球物理研究的重要进展。通过实现高分辨率地震数据的收集，它促进了对地下地质的更深入理解，最终有助于更有效地勘探和管理自然资源。随着技术的不断发展，面状地震检波器阵列的能力可能会进一步扩大，从而增强我们探索和理解地球地下动态的能力。