Seismic hazard analysis in Santo Domingo City Team 4 Report.

Slides:



Advertisements
Similar presentations
Herrera Airport Group 2 Michael Ming Hei CalTech María C Araya RSN Cecilio Morales FUNVISIS Dorian Restrepo CMU Kenny García FUNVISIS Claude Jean-Poix.
Advertisements

An-Najah National University
Development of an In-Situ Test for Direct Evaluation of the Liquefaction Resistance of Soils K. H. Stokoe, II, E. M. Rathje and B.R. Cox University of.
J. Louie 9/5/2005 OutlineOutline 1.Refraction Microtremor for Shallow Vs 2.ReMi-Borehole Comparison 3.Los Angeles Transect 4.Las Vegas Transect 5.Effect.
PREDICTION OF RESPONSE SPECTRAL PARAMETERS FOR BHUJ EARTHQUAKE (26TH JANUARY 2001) USING COMPONENT ATTENUATION MODELLING TECHNIQUE By DR. SAROSH.H. LODI.
Multichannel Analysis of Surface Waves (MASW)
Kombineret inversion af MEP og seismik data med boringsoplysninger som á priori Combined inversion of MEP and seismic data with drilling data as prior.
Using 3D Seismic Imaging for Mine and Mineral Exploration G. Schuster University of Utah.
Near-Surface Geophysical Investigation of the 2010 Haiti Earthquake Epicentral Area Eray Kocel, Robert R. Stewart, Paul Mann, and Li Chang Eray Kocel,
Soil ConditionsRecordsStations Alluvium125 Rock2915 Stiff soil4615 Soft soil2213 Very soft soil147 Unknown3412 TOTAL15767 Period:
Tania Mukherjee Department of Earth And Atmospheric Sciences University of Houston April 28, 2010 Near-surface geophysical imaging in a highly structured.
Shallow Shear Velocity and Seismic Microzonation of the Urban Las Vegas Basinwww.seismo.unr.edu/hazsurv Rasmussen, Tiana; Smith, Shane B.; and Louie, John.
Probabilistic Seismic Hazard Maps - Inputs and Status Choi Yoon Seok Jennifer S. Haase Robert L. Nowack Purdue University.
Local Site Effects Seismic Site Response Analysis CEE 531/ESS 465.
Influence of Seismic Site Response on Landslide Reactivation during the Next Cascadia Earthquake Corina Cerovski-Darriau, Miles Bodmer, Joshua Roering,
Characterization of Glacial Materials Using Seismic Refraction and Multichannel Analysis of Surface Waves Glenn Larsen Ohio Department of Natural Resources.
1-D Zaid AlMusallam SAGE 2004 Synthetic Seismic Model.
Modeling Seismic Response for Highway Bridges in the St. Louis Area for Magnitude 6.0 to 6.8 Earthquakes J. David Rogers and Deniz Karadeniz Department.
SDC’s and Detailing Requirements Locations with Different Soils 1000 year return period Derrell Manceaux, FHWA.
Earthquake Hazard Assessment in the Pacific Northwest: Site Response Thomas L. Pratt U. S. Geological Survey School of Oceanography University of Washington.
Science for a changing world The USGS and the Development of the Nevada Great Basin Community Velocity Model.
J. Louie 2/24/2005 Refraction Microtremor for Shallow Shear Velocity in California Urban Basins John Louie, Nevada Seismological Lab UNR students: J. B.
WP-1-1: Methodological improvements for 3D reconstructions Contributors: Pierre Gouédard, Philippe Roux, Seiji Tsuno, Marc Wathelet.
Characterization of Ground Motion Hazard PEER Summative Meeting - June 13, 2007 Yousef Bozorgnia PEER Associate Director.
J. Louie 18/8/2005 Refraction Microtremor for Shallow Shear Velocity in Urban Basins John Louie, Nevada Seismological Lab (at GNS & VUW through July 2006–
The surface profiles in Grenoble area determined by the MASW measurements Seiji Tsuno, Cecile Cornou, Pierre-Yves Bard (LGIT) QSHA meeting, 1/Juin/2007,
ReMi Applied Geophysics Spring Break 2010 Fariha Islam Gretchen Schmauder.
Geology 492/692 Field Project Hoping to put Fernley and Hazen on the Fault Map ReMi Data.
Average properties of Southern California earthquake ground motions envelopes… G. Cua, T. Heaton Caltech.
Latin American Countries Map Review. Mexico Nicaragua Panama Colombia Haiti Puerto Rico Jamaica Honduras The Bahamas Cuba United States Belize Guatemala.
Ground Motion Parameters Measured by triaxial accelerographs 2 orthogonal horizontal components 1 vertical component Digitized to time step of
Downhole seismic and S-Waves Jacques JENNY Geo 2X Genève.
Seismic Hazard Assessment for the Kingdom of Saudi Arabia
University of Missouri - Columbia
Geomorphology Field Research Project: Mountain Front Faulting & Alluvial Fans San Gabriel Mountain Foothills, Southern, California Dr. Jeff Marshall -
Dominican Republic By Kerry, Craig and Ross.  Dominican Republic is in the Caribbean. It is located near Cuba, Puerto Rico and borders Haiti. Where is.
Web-based Class Project on Rock Mechanics
Earthquake Engineering GE / CEE - 479/679 Topic 13. Wave Propagation 2
Imaging Normal Faults in Alluvial fans using Geophysical Techniques: Field Example from the Coast of Aqaba, Saudi Arabia Sherif M. Hanafy 28 October 2014.
Where is Cuba? A B C D Where is Puerto Rico? A B C D.
Predicting Site Response. Based on theoretical calculations –1-D equivalent linear, non-linear –2-D and 3-D non-linear Needs geotechnical site properties.
Marine Resistivity: a Tool for Characterizing Sediment Zones.
NS/V noise NS/H noise NS/H earthquakes The use of a very dense seismic array to characterize the Cavola, Northern Italy, active landslide body. By P. Bordoni.
Translating the 2009 Provisions into ASCE 7-10: Ground Motions Maps
C. Guney Olgun Department of Civil and Environmental Engineering, Virginia Tech Thomas A. Barham, Morgan A. Eddy, Mark Tilashalski, Martin C. Chapman,
An E-W gravity profile across the La Bajada fault Zone in the Rio Grande Rift, North Central New Mexico Rajesh Goteti University of Rochester SAGE 2007.
Building and Housing Research Center
Tri-State Seismic Hazard Mapping -Kentucky Plan
Ground-Motion Attenuation Relationships for Cascadia Subduction Zone Megathrust Earthquakes Based on a Stochastic Finite-Fault Model Nick Gregor 1, Walter.
CodeClass 1 Course Title Interpretation of Reflection data & petroleum Exploration Credit Lecturer Kim, Ki Young Rm NS3-303 Office Hour By appointment.
NETWORK REPORT SRI LANKA Geological Survey & Mines Bureau Sri Lanka.
Microtremor method Saibi. Dec, 18, 2014.
Ground-roll Inversion for Near-surface Shear-Wave Velocity
Vertical electrical sounding (VES), also known as‘electrical drilling’ or ‘expanding probe’, is used mainly in the study of horizontal or near-horizontal.
Earthquake Site Characterization in Metropolitan Vancouver Frederick Jackson Supervisor – Dr. Sheri Molnar.
Servizio Sismico Nazionale
Site effect characterization of the Ulaanbaatar basin
Matteo Albano1, Marco Polcari1, Christian Bignami1, Marco Moro1, Michele Saroli2,1, Salvatore Stramondo1 1 - Istituto Nazionale di Geofisica a Vulcanologia,
An-Najah National University Faculty of Engineering
Mohammad Maher Jaradat Raghad Abdel-Salam Owaidat
Scott Callaghan Southern California Earthquake Center
WE PUT YOU ON SOLID GROUND
Structural Design for Host Mall
Latin American Countries Map Review
Creating a Conference Poster
of these basic elements
Assessments of Conditions at 70 Rock Sites Having Vs30 near the NEHRP B-C Boundary with Measures of Heterogeneity J.B. Scott1, J.N. Louie1, D. Pei1, K.
The Relationship between Uncertainty and Quality in Seismic Data
Cableless Seismograph Atom for engineering site investigation
Presentation transcript:

Seismic hazard analysis in Santo Domingo City Team 4 Report

Study area Geological setting HVSR technique ReMi, Masw and Spac techniques Final discussion Outline

Team Members PabloRocioFernando Venezuela Honduras Dominican Rep.

Team Members Junior Haiti Lidia Honduras Norberto Puerto Rico Heriberto Dominican Rep.

Study Area Profile 1 Profile 2 Profile 3 Profile 4 Profile 5 Profile 6

Geological setting of Santo Domingo Stratigraphic column

HVSR technique

H/V data acquisition

Geology (Team 4 HVSR study area)

H/V station deployments

H/V Results: 2.60 s Station SD03_p2-p3 (1508_9282_202) 4.02 s Station SD06_p3-p4 (1526_92F1_202) ? ? ?

H/V Results: Station SD02_p3-p4 (1349_92F1_202) Station SD03_p3-p4S (1410_949A_202) 4.32 Secs 3.70 Secs ? ?

H/V Results: Station SD07_p3-p4 (1550_949A_202) Station SD04_p2-p3 (1532_950C_202) 3.71 Secs 2.38 Secs ? ? ?

H/V Results: Station SD01A_p3-p4 (1300_92F1_202) Station SD01B_p3-p4 (1308_949A_202) 0.28 Hz 3.58 Secs 0.27 Hz 3.70 Secs ? ?

Isoperiods Map (seconds)

ReMi and Masw techniques

ReMi and Masw data acquisition

Location for ReMi, Spac and Masw surveys Mirador sur Av. Mirador del Sur park Remi and Masw Line 1 Remi Line 2 Spac 1 Spac 2 Remi Line 3

Remi velocity model Line 2

Dispersion model Line 2

Soil Characterization near to ReMi 2

Soil Classification DR Seismic Code

727 m Remi Model Line 3

Dispersion curve for Line 3

65.5 m Last 13.5 m Limestone! Borehole S-4 Vs = 2083 m/s Vs = 1261 m/s Vs = 978 m/s Vs = 795 m/s Dispersion curve RMS error: m/s Vs = m/s IBC class site B Line 3 Remi Model

MASW Line 1 results

Spac technique

Location for Spac survey No. 2 Mirador sur Av. Mirador del Sur park Remi and Masw Line 1 Remi Line 2 Spac 1 Spac 2 Remi Line 3

Spac survey No. 2 ground model

HVSR results have a good relationship with the geological environment of deposition (alluvial fal, prodelta), that is the reason because we got high predominant period peaks. Remi, Masw and Spac techniques revealed a high velocity layering structure, validated by 8 boreholes drilled near from the team’s study site. Remi line 2 could be defined as a Class C site ( m/s, Stiff Soil- standard designs - NERHP). Remi lines 3 could be defined as a Class B site ( m/s, Soft Rock- low-hazard design - NERHP). Conclusions

Thanks you so much!