Principle Investigator: 
Jacobo Bielak, Carnegie Mellon University
Co-PIs: 
Dominic Assimaki, Loukas Kallivokas, Jamison Steidl, Letecia Velazquez

NEES Project Warehouse: http://nees.org/warehouse/project/391
NSF Award Abstract: http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=0619078
The main objective of this research is to develop the capability for estimating the geological structure and mechanical properties both of individual sites and of complete basins, and to demonstrate this capability on the nees@UCSB site at the Garner Valley. Specifically, this high-fidelity estimation will be based on integrating: 

  1. in-situ dynamic excitation using the NEES equipment at the University of Texas at Austin (nees@UTexas);
  2. earthquake records from new strong-motion and broadband sensor networks; and
  3. new inversion methods based on partial-differential-equation (PDE)-constrained optimization.

This project represents an unparalleled opportunity to couple state-of-the-art field experimentation with state-of-the-art computational tools for the purpose of imaging the subsurface at resolutions and length scales until recently unattainable.

Surface Wave Analysis

June, 2010. The University of Texas at Austin brought their Tri-Axial Vibroseis, T-REX, to Garner Valley to perform various surface wave tests. T-REX can produce sine wave and pulse shaped waves at a broad range of frequencies. The recordings are analyzed to determine subsurface features and soil properties.

Deployment at Garner Valley

The linear array deployed across Garner Valley was operational from April, 2008 until January of 2009. It captured hundreds of earthquakes, including the magnitude 5.4 Chino Hills event. The stations are spaced 50 meters (164 feet) apart.

November 2007 Test Deployment Near Austin, Texas

Tests were conducted at the Hornsby Bend biosolid facility in Austin Texas using equipment from both the NEES@UTexas and NEES@UCSB equipment sites. Seismic instruments were deployed along a grid at the surface, and the "liquidator" shaker was used to generate signals that would propagate out through the underlying soils and be recorded by the instruments. This initial test was conducted to improve our understanding of the shaker source capabilities within a range of frequencies from 0.5 to 16 Hz. These tests will help in planning of the future testing to be performed at the NEES@UCSB Garner Valley site.

NRC

The UCSB Geotechnical Array monitoring program is funded by the United States Nuclear Regulatory Commission (NRC)  under
Contract# NRC-HQ-60-15-C-0001 Project title: "Observations and Analysis of Geotechnical Array Data"

This site previously funded (2004 to 2014) by the Geoge E. Brown, Jr. Network for Earthquake Engineering Simulation (NEES) Program of the National Earthquake Hazards Reduction Program (NEHRP) of the National Science Foundation (NSF) under Award Number CMMI-0927178.