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Title: | Appendix 1 : how ground penetrating radar (GPR) works |
Other Titles: | Temple landscapes : fragility, change and resilience of Holocene environments in the Maltese Islands |
Authors: | Ruffell, Alastair |
Keywords: | Ground penetrating radar Geophysics -- Methodology |
Issue Date: | 2020 |
Publisher: | McDonald Institute for Archaeological Research |
Citation: | Ruffell, A. (2020). Appendix 1 : how ground penetrating radar (GPR) works. In: C. French, C. O. Hunt, R. Grima, R. McLaughlin, S. Stoddart & C. Malone, Temple landscapes : fragility, change and resilience of Holocene environments in the Maltese Islands. Cambridge: McDonald Institute for Archaeological Research. 351-352. |
Abstract: | Ground penetrating radar (or GPR) uses the transmission and reflection of radio waves (typically 25 to 2 GHz) in imaging the subsurface. Radar waves, introduced in the ground, may reflect back to surface when they intersect objects or surfaces of varying dielectric permittivity. Thus a GPR system requires a source antenna and receiving antenna (built to measure the same frequency). *Note that the plural of electrical devices is antennas; antennae are exclusively for animals such as insects. The transmitting antenna generates a pulse of radiowaves that the receiver detects at a set time interval: the longer the time interval, (potentially) the deeper the waves will have travelled into the ground (or to a nearby surface object) and back again. When the ground has a slow radarwave velocity, so a buried object may appear deeper than in ground with a fast transmissive velocity. [excerpt] |
URI: | https://www.um.edu.mt/library/oar/handle/123456789/64162 |
Appears in Collections: | Temple landscapes: Fragility, change and resilience of Holocene environments in the Maltese Islands |
Files in This Item:
File | Description | Size | Format | |
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Appendix_1_how_ground_penetrating_radar_(GPR)_works.pdf | 200.2 kB | Adobe PDF | View/Open |
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