Webinar
The Basics of Interpreting GPR Data – Part 1
Webinar: The Basics of Interpreting GPR Data – Part 1
This webinar explores the basics of signals seen on GPR cross-sections. Understand responses from subsurface objects and boundaries. Learn that not everything you see in a GPR line is necessarily from the subsurface.
- GPR Interpretation Basics – Part 1
- 0:00 – Introduction
- 1:55 – What causes GPR Reflections?
- 4:25 – What controls the amount of GPR energy that reflects?
- 12:37 – GPR reflections from metallic and non-metallic utilities
- 16:17 – Geological reflections example
- 16:54 – Utility reflections example
- 18:50 – The shape of GPR signals
- 19:39 – Attenuation of GPR Signals
- 22:49 – Types of subsurface objects
- 24:20 – Hyperbolas in GPR images
- 27:00 – Tracking the path of a utility
- 28:32 – Crossing a utility at an angle
- 33:38 – Reflections from boundaries
- 34:20 – Direct air and ground arrivals at the top of all GPR images
- 37:24 – Direct arrivals change as surface conditions change
- 38:40 – Background radio frequency noise in GPR images
- 42:55 – Depth of GPR signal penetration
- 44:03 – GPR Interpretation Quiz
- 44:38 – Question 1 – Which target is likely non-metallic?
- 46:05 – Question 2 – What is the composition of the targets?
- 47:36 – Question 3 – Was this concrete data collected in the basement or on the second floor?
- 49:18 – Question 4 – What is the most plausible explanation of what happened to the pipe on Line 3?
- 51:22 – Question 5 – How do you interpret the vertical signals in the middle of this GPR line?
- 52:26 – Question 6 – Why is hyperbola 1 wider than hyperbola 2?
- 54:00 – Question 7 – Where is the gravel layer?
- 55:13 – Question 8 – What is happening in the concrete?
- 56:40 – Question 9 – Why are there no reflections here?
- 58:53 – Question 10 – What is causing the strong reflectors at about 1.6 meters?
- 1:00:15 – Summary
- 1:01:26 – Finish
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