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首页> 外文期刊>Geoscientific Instrumentation, Methods and Data Systems >A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
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A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments

机译:低温晶体环境的时空电势测量监测系统

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Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures, non- or minimally invasive methods are required for inexpensive and timely characterization and monitoring of potential failure sites to allow in-time responses. These requirements can potentially be met by geophysical methods usually applied in near-surface geophysical settings, such as electrical resistivity tomography (ERT), ground-penetrating radar (GPR), various seismic methods, and self-potential (SP) measurements. While ERT and GPR have their primary uses in detecting lithological subsurface structure and liquid water/ice content variations, SP measurements are sensitive to active water flow in the subsurface. Combined, these methods provide huge potential to monitor the dynamic hydrological evolution of permafrost systems. However, while conceptually simple, the technical application of the SP method in high-alpine mountain regions is challenging, especially if spatially resolved information is required. We here report on the design, construction, and testing phase of a multi-electrode SP measurement system aimed at characterizing surface runoff and meltwater flow on the Schilthorn, Bernese Alps, Switzerland. Design requirements for a year-round measurement system are discussed; the hardware and software of the constructed system, as well as test measurements are presented, including detailed quality-assessment studies. On-site noise measurements and one laboratory experiment on freezing and thawing characteristics of the SP electrodes provide supporting information. It was found that a detailed quality assessment of the measured data is important for such challenging field site operations, requiring adapted measurement schemes to allow for the extraction of robust data in light of an environment highly contaminated by anthropogenic and natural noise components. Finally, possible short- and long-term improvements to the system are discussed and recommendations for future installations are developed.
机译:气候诱导的变暖越来越导致高高脂永久冻土的降解。为了开发用于迫在眉睫的坡度稳定的预警系统,迫切需要了解地下中的水文流程的知识。由于与斜率故障相关的快速动态,所需的廉价且及时表征和监测潜在故障站点所需的非动力学,以允许就时刻响应。这些要求可以通过通常应用于近表面地球物理设置的地球物理方法来满足,例如电阻率断层扫描(ERT),地面穿透雷达(GPR),各种地震方法和自电(SP)测量。虽然ERT和GPR在检测岩性地下结构和液体水/冰含量变化中具有它们的主要用途,但SP测量对地下的活性水流动敏感。结合,这些方法提供了监测永久冻土系统动态水文演化的巨大潜力。然而,在概念上简单的情况下,在高山山区SP方法的技术应用具有挑战性,特别是如果需要空间解决的信息。我们在这里报告了多电极SP测量系统的设计,结构和测试阶段,旨在表征Schilthorn,瑞士伯尔尼阿尔卑斯山脉的表面径流和熔体流动。讨论了全年测量系统的设计要求;提出了构造系统的硬件和软件以及测试测量,包括详细的质量评估研究。现场噪声测量和SP电极冷冻和解冻特性的一个实验室实验提供了支持信息。发现对测量数据的详细质量评估对于这种具有挑战性的场地,需要适应的测量方案,以允许鉴于受到人为和自然噪声分量高度污染的环境的鲁棒数据来提取鲁棒数据。最后,讨论了对系统的可能性短期和长期改进,并开发了未来安装的建议。

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