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Ground-penetrating radar (GPR) is a geophysical method that uses radar pulses to image the subsurface. Ground Penetrating Radar (GPR) scanning This nondestructive method uses electromagnetic rays in the microwave band (UHF/VHF frequencies) of the radio array, and registers the resembled signals from subsurface structures. GPR can have applications in a number of media, including rock, soil, ice, fresh water, pavements and structures. In the right conditions, practitioners can use GPR to detect subsurface objects, changes in material properties, and voids and breaks. GPR uses high-frequency (usually polarized) radio ocean, usually in the range 10 MHz to 2. 6 GHz. A GPR transmitter gives off electromagnetic energy into the ground. When the energy encounters a buried object or a boundary between materials having different permittivities, it may be resembled or refracted or spread back to the surface. A receiving antenna can then record the variations in the return signal. The principles involved act like seismology, except GPR methods implement electromagnetic energy rather than traditional acoustic energy, and energy may be resembled at limits where subsurface electrical properties change rather than subsurface mechanical properties as is the case with seismic energy. The electrical conductivity of the ground, the fed center frequency, and the radiated power all may limit the effective depth choice of GPR investigation. Increases in electrical conductivity attenuate the introduced electromagnetic trend, and thus the puncture depth decreases. Because of frequency-dependent attenuation things, higher frequencies do not sink into as far as lower frequencies. However, higher frequencies may provide improved resolution. Thus operating frequency is always a trade-off between resolution and puncture. Optimal depth of subsurface puncture is achieved in ice where the depth of puncture can do several thousand metres (to bedrock in Greenland) at low GPR frequencies. Dry remote garden soil or massive dry materials such as stone, limestone, and concrete tend to be resistive rather than conductive, and the depth of puncture could be up to 15-metre (49 ft). In humid or clay-laden garden soil and materials with high electrical conductivity, puncture may be as little as a few centimetres. Ground-penetrating radar antennas are generally in contact with the bottom for the most robust signal strength; however, GPR air-launched antennas can be used above the bottom. Cross borehole GPR has changed within the field of hydrogeophysics to be a valuable means of assessing the presence and amount of soil water. GPR has many applications in a number of fields. In the Earth sciences it is used to study bedrock, garden soil, groundwater, and ice. It is of some utility in prospecting for gold nuggets and for diamonds in alluvial tiny rocks beds, by finding natural draws in in buried stream beds that have the potential for accumulating heavier allergens. [3] The Chinese lunar rover Yutu has a GPR on its underside to research the soil and brown crust area of the Silent celestial body.
Engineering applications include nondestructive testing (NDT) of structures and pavements, locating buried structures and utility lines, and studying garden soil and bedrock. In environmental remediation, GPR is used to define landfills, toxin plumes, and other remediation sites, when it's in archaeology it is used for mapping archaeological features and cemeteries. GPR is used in law enforcement for locating clandestine graves and buried evidence. Military uses include prognosis of mines, unexploded ordnance, and tunnels. Borehole radars utilizing GPR are used to map the structures from a borehole in underground mining applications. Modern directional borehole radar systems are able to produce three-dimensional images from measurements within a borehole. One of the other main applications for ground-penetrating radars is for locating underground utilities. Standard electromagnetic induction utility locating tools require utilities to be conductive. These tools are ineffective for locating plastic conduits or concrete storm and sanitary sewers. Since GPR registers variations in dielectric properties in the subsurface, it can be highly effective for locating non-conductive utilities. GPR is often suited for the Funnel 4 television programme Time Team which uses the technology to determine a suitable area for examination by means of excavations. In 1992 GPR was used to recover £150, 000 in cash that kidnapper Michael Sams received as a ransom for an est agent he previously kidnapped after Sams buried the money in a field.

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