Ground Penetrating Radar
GRORADAR™ by Gary R. Olhoeft, PhD
[ Home ] GRORADAR ] Tutorial ] Links ] Reading ] Bibliography ] Educational Software ] [ GRORADAR Ground Penetrating Radar Gary R. Olhoeft ]

http://www.g-p-r.com
Statistics  NetMechanic W3C HTML Validation Service  Eddy M. Elmer: Internet Help

Spot Gold Price    Spot Oil Prices   Bloomberg Futures   Weather

New & Used Equipment     Fraud & Virus Alerts

HEALTH/SAFETY/REGULATORY INFORMATION:
(check out FCC/NTIA restrictions on GPR)
(New NTIA UWB publications January 2001)
FCC/NTIA/IRAC/FDA/OSHA

    Ground penetrating radar (GPR, sometimes called ground probing radar, georadar or earth sounding radar or "radar terrestre penetrant") is a noninvasive electromagnetic geophysical technique for subsurface exploration, characterization and monitoring (history).  It is widely used in locating lost utilities, environmental site characterization and monitoring, agriculture, archaeological and forensic investigation, unexploded ordnance and land mine detection, groundwater, pavement and infrastructure characterization, mining, ice sounding, permafrost, void and tunnel detection, sinkholes, subsidence, karst, and a host of other applications.  It may be deployed from the surface by hand or vehicle, in boreholes, between boreholes, from aircraft and from satellites.  It has the highest resolution of any geophysical method for imaging the subsurface, with centimeter scale resolution sometimes possible.
    Resolution is controlled by wavelength of the propagating electromagnetic wave in the ground.   Resolution increases with increasing frequency (shorter wavelength).  Depth of investigation varies from less than one meter in mineralogical clay soils like montmorillonite to more than 5,400 meters in polar ice.  Depth of investigation increases with decreasing frequency but with decreasing resolution.  Typical depths of investigation in fresh-water saturated, clay-free sands are about 30 meters.  Depths of investigation (and resolution) are controlled by electrical properties through conduction losses, dielectric relaxation in water, electrochemical reactions at the mineralogical clay-water interface, scattering losses, and (rarely) magnetic relaxation losses in iron bearing minerals.  Scattering losses are the result of spatial scales of heterogeneity approaching the size of the wavelength in the ground (like the difference between an ice cube and a snowball in scattering visible light).  Detectability of objects in the ground depends upon their size, shape, and orientation relative to the antenna,  contrast with the host medium, as well as radiofrequency noise and interferences.  This is representative but greatly oversimplified: see tutorial.

GRORADAR™ data processing, modeling and display software.

Library, Bibliographic and Data Search Links

GPR Wiki

Search GRORADAR(tm) Site for:

Search "ground penetrating radar", "georadar" or "ground probing radar" on:
google25.jpg (3331 bytes)    Search IEEE Websites
AltaVista  or Yahoo! or HotBot or Government Information Xchange
Dogpile or Metacrawler Multiengine Search Tools
Search Adobe PDF Online

 

UXO/Countermine Forum
9-12 April 2001 New Orleans, Louisiana USA

Fourth International Conference on Electromagnetic Wave Interaction with Water and Moist Substances
13-16 May 2001 Weimar, Germany

Conference on the Geophysical Detection of Subsurface Water on Mars
6-10 August 2001 Houston, TX, USA

Ground Penetrating Radar (GPR) in Sediments
Applications and Interpretation
20-21 August 2001 London, UK

Information on the next sequences of the above conferences will be updated as soon as available.

AGU Geophysical Year Calendar

ASCE Events Calendar

IEEE Conference Search

SEG Meetings Calendar

 

Society of Exploration Geophysicists
Annual Meeting 9-14 September 2001 San Antonio, Texas USA
(10-15 October 2004 Denver)

Remote Sensing by Low-Frequency Radars
20-21 September 2001 Naples, Italy

Damage Prevention Convention
28-30 November 2001 Dallas, Texas USA

National Pavement Expo
30 Jan - 2 Feb 2002 Nashville, TN USA

Environmental and Engineering Geophysical Society
Symposium on the Application of Geophysics to Engineering and Environmental Problems
SAGEEP 2002 10-13 February 2002 Las Vegas, Nevada USA
Call for Papers 27 July 2001 extended abstract deadline

Applied Computational Electromagnetics Society
18-22 March 2002 Monterey, California, USA

IEEE Radar Conference
22-25 April 2002 Long Beach, CA USA

GPR2002
9th International Conference on Ground Penetrating Radar
April 29 to May 2, 2002 Santa Barbara, California USA
Steve Koppenjan, General Chair
12 October 2001 abstract deadline

IGARSS International Geoscience and Remote Sensing Symposium
24-28 June 2002 Toronto, Ontario, Canada

International Conference on Subsurface and Surface Sensing and Imaging Technologies and Applications
7-11 July 2002 Seattle, Washington USA

 

GRORADAR™ Contact Information:  
Postal address: P.O. Box 1520, Golden, CO  80402-1520  USA  
Shipping:
          1818 Smith Road, Golden, CO  80401-1756 USA
Phone:               303-279-7932    Fax:   303-273--9202                  
     Email: golhoeft@g-p-r.com  Resume and Publications of Gary R. Olhoeft

 

 
This web site is supported by sales of
GRORADAR™ data processing, modeling and display software.
Send mail to golhoeft@g-p-r.com with questions or comments about this web site.
Copyright © 1998-2001 Gary R. Olhoeft. All rights reserved.  Last modified: September 10, 2001.
All trademarks are owned by their respective companies. Copyright & Fair Use  Electronic Frontier Foundation
Please don't copy and redistribute anything without requesting permission.
Do freely make hyperlinks to these web pages through http://www.g-p-r.com