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GEOREF RECORD

Reference rock site condition for central and eastern North America

Youssef M. A. Hashash, Albert R. Kottke, Jonathan P. Stewart, Kenneth W. Campbell, Byungmin Kim, Cheryl Moss, Sissy Nikolaou, Ellen M. Rathje and Walter J. Silva
Reference rock site condition for central and eastern North America
Bulletin of the Seismological Society of America (April 2014) 104 (2): 684-701

Abstract

The reference rock site condition has two important applications for ground-motion prediction in the stable continental region of central and eastern North America (CENA). (1) It represents the site condition for which ground motions are computed using semiempirical ground-motion prediction equations. In addition, (2) it represents the site condition to which site amplification factors, which are used to modify ground-motion intensity measures for softer site condition, are referenced (i.e., site amplification is unity for reference rock). We define reference rock by its shear (S)- and compression (P)-wave velocities, as well as a site attenuation parameter (kappa (sub 0) ), which is used in stochastic ground-motion simulation methods. Prior definitions of reference rock conditions in CENA were based mostly on indirect large-scale crustal velocity inversions and judgment. We compile and interpret a unique database of direct velocity measurements to develop criteria for assessing the presence of reference rock site condition based on measured seismic velocities and their gradient with respect to depth. We apply the criteria to available profiles and perform rigorous statistical analysis from which we recommend S- and P-wave velocities of 3000 and 5500 m/s, respectively, for the reference rock condition. We recommend that, for practical applications, use ranges of reference S- and P-wave velocities of 2700-3300 m/s and 5000-6100 m/s, respectively. The ranges are based on a + or -5% change in amplification using quarter-wavelength theory. We do not find evidence for regional dependence of the reference velocities, which are derived principally from three general geographic regions: (1) Atlantic coast, (2) continental interior, and (3) Appalachian Mountains. Our data do not provide reference velocities for the Gulf Coast region. The recommended velocity-compatible reference rock site kappa is 0.006 s.


ISSN: 0037-1106
EISSN: 1943-3573
Coden: BSSAAP
Serial Title: Bulletin of the Seismological Society of America
Serial Volume: 104
Serial Issue: 2
Title: Reference rock site condition for central and eastern North America
Affiliation: University of Illinois at Urbana-Champaign, Department of Civil and Environmental Engineering, Urbana, IL, United States
Pages: 684-701
Published: 201404
Text Language: English
Publisher: Seismological Society of America, Berkeley, CA, United States
References: 62
Accession Number: 2014-036972
Categories: Seismology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 5 tables, sketch map
N33°00'00" - N47°30'00", W87°00'00" - W67°00'00"
Secondary Affiliation: Bechtel National, USA, United StatesUniversity of California at Los Angeles, USA, United StatesEQECAT, USA, United StatesRisk Management Solutions, USA, United StatesMueser Rutledge Consulting Engineers, USA, United StatesUniversity of Texas at Austin, USA, United StatesPacific Engineering and Analysis, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, Copyright, Seismological Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201423
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