SmartSolo Bridge Health Monitoring System

Detailed Description

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The data logger in the SmartSolo bridge health monitoring system not only ensures reliability but also incorporates low-cost features. This allows researchers to realize the needs of large-scale and multi-network deployments on a limited budget. The observation system uses reliable, scientific research-grade sensors, which collect data more efficiently and simply. This is enabled through the data acquisition technology newly developed by SmartSolo.

The system consists of the following components: data logger M8000, three-channel seismic intelligent sensor IGU16-HR3C, Vaisala multi-parameter weather station WXT536, high precision atmospheric pressure sensor Setra 278, solar power supply module, and bracket. This system can achieve long-term unattended, automatic, and continuous data acquisition.

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The observation system is an integrated and fully configured system. In addition to ordering all the components of the observation system, you can also customize it according to your needs. You can add or replace sensors, peripheral measuring devices, or communication devices to meet your specific requirements. Please contact SmartSolo for details.

?#HighResolutionReceiver Function #Imaging Estimates the Dominance of Backwash and Pure Shear Mechanisms in Crustal Deformation of the Himalayan Tectonic Junction on the Eastern Tibetan Plateau ? Equipment Model: #SmartSolo IGU-16HR 3C ? Number of units: 200

? Research Overview: The question of how the crust deforms in the tectonics of the eastern Himalayas during the collision of the Indian and Asian plates remains unclear. For the first time, high-resolution receiver function images of crustal structures along a new NW-SE-trending dense array of stations crossing the Himalayan tectonic belt are shown. Two sets of low-velocity zones were observed, one below the western part of the Lhasa Massif and the High Himalayan region at a depth of 18 ~ 20 km, which is flat; and the other below the western part of the Yarlung Tsangpo Suture Belt at a depth of 10 ~ 30 km, displaying two westward-trending types. These low-velocity zones, caused by partially molten and aqueous fluids, are separated from each other and impede the formation of crustal flows. An eastward-dipping internal crustal discontinuity and a pronounced Moho dislocation with a length of 7 km were identified under the Ankiga-Motoro shear zone, suggesting that retrogression of the subducting crust beneath the Indian Plate and a pure shear mechanism dominate crustal deformation in the Eastern Himalayan tectonic belt.

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