SEISMIC DETECTION OF FROZEN SOIL SUBGRADE ON QINGHAI TIBET HIGHWAY
2025-11-21
Objective
To conduct precise geophysical exploration of the internal structure of permafrost roadbeds on the Qinghai Tibet Plateau, which can cause uneven settlement at the meter level due to thawing and settlement of permafrost roadbeds, leading to unevenness and cracking of the road surface. This will provide important basic data such as roadbed layer structure and artificial upper limit for the improvement and renovation project of Qinghai Tibet Highway;
Project Characteristics
The exploration area belongs to Qinghai Province and the Xizang Autonomous Region in terms of administrative division. It is a plateau peneplain landform area with the highest altitude and harsh climate conditions in the world, with an altitude of 5205 m, belonging to a low latitude and high altitude permafrost area;
Method
Joint detection method of active and passive seismic surface waves, and first arrival time tomography inversion technique;
Equipment
Ant-1C 5Hz 600 units, TB recorder, 80 kg acceleration hammer shock source;

Typical melting and sinking road sections
| Node layout | Explain the results |
Achievement: Interpreting the profile reveals the location, depth, thickness, and artificial upper limit depth of seasonal active layer subsidence.
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