By the end of the program, students will be able to conduct:
3D reconstruction using unmanned aerial vehicles
Geophysical/geotechnical assays: application of ground penetrating radar and superficial waves for archaeological and geotechnical engineering studies.
Ground penetrating radar
Surface waves
Non-destructive tests for structural characterization:
Modal analysis
Thermography
During the first week, students will attend classes at PUCP to give them a basic understanding of structure engineering principles, monumental architecture, geophysics, and non-destructive experimental techniques. Simultaneously, students will be conducting experiments in the campus laboratories.
For the following two weeks, students will be carrying out activities in the field. The first week will be spent in the archaeological site of Huaca de la Luna, while the second week will take place in the ruins of the colonial town of Zaña.
The activities have been developed in the following manner:
3D reconstruction using unmanned aerial vehicles:
The methodology for photogrammetric reconstruction work consists of the following steps:
Geophysics assays:
Application of ground penetrating radar and surface waves for archaeological and geotechnical engineering studies
Ground penetrating radar
The GPR equipment utilized for the measurement of subsurface conditions normally consists of a transmitter and receiver antenna since 10 MHz to 1.5 GHz, a radar control unit, and suitable data storage and display devices. A circuit within the radar control unit generates a train of trigger pulses that are sent to the transmitter and receiver electronics. The transmitter electronics produce output pulses that are radiated into the ground from the transmitting antenna. (ASTM-D6432).
Data acquisition for GPR surveys includes common offset and common midpoint profiling. Common midpoint profiles sample the same point in depth below the midpoint, and the reflection hyperbola which results from the varying source-receiver separation can be used to determine the velocity of the subsurface layer.
Surface waves test
The surface-waves test is widely used in geophysics to infer a shear wave velocity model of the subsoil for a wide variety of applications. The standard procedure for surface waves test can subdivided in three main steps:
Non-destructive tests for structural characterization: modal analysis and thermography
Modal analysis
The first step in this technique is to build a numerical model of structure in study. This model is used to determine the best location to install the accelerometers. Depending on the number of accelerometers different arrangements will be done, at least two. After installing the accelerometers for each arrangement vibration, data will be recorded. Collected data will be processed to identify modal forms and natural frequency of the structure using ARTEMIS software. If possible, a more detailed numerical model will be done and calibrated.
Thermography tests
Thermography tests are based on the thermal conductivity of a material and may be passive or active. The first step for survey with this technique is to locate the thermographic camera at the desired location and distance from the structure or specimen of interest. It is necessary to use an appropriate infrared imaging measurement to measure and compensate for the reflected temperature error incident upon the specimen. The test must be performed at least three times.
Trujillo – La Libertad, Perú
Time Period:3 weeks
Number of hours:135 hours
Credits:4
Professor:PhD. Rafael Aguilar
Associated Professors:PhD. Benjamin Castañeda
PhD. Renato Perucchio
PhD. Cynthia Ebinger
PhD. Miguel Pando
Msc. Guillermo Zavala