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In situ 2-D and 3-D measurements of radiation patterns of half-wave dipole GPR antennas
Institution:1. Center for Lithospheric Studies, The University of Texas at Dallas, P.O. Box 830688, 2601 N. Floyd Road, Richardson, TX 75083-0688, USA;2. Dip. ITS, Area Geofisica, Universitá di Roma La Sapienza, Via Eudossiana 18, 00184 Rome, Italy;1. Faculty of Engineering and Material Sciences, German University in Cairo, Egypt;2. Faculty of Engineering, Beni-Suef University, Beni-Suef, Egypt;1. Servicio de Ginecología, Centro Médico Teknon, Barcelona, España;2. Departamento de Ciencias Biomédicas (Área de Farmacología), Facultad de Medicina y Ciencias de la Salud, Universidad de Alcalá, Madrid, España;3. Departamento de Obstetricia y Ginecología, Universidad de Granada, Granada, España;4. Departamento Médico, E-C-BIO, S.L., Las Rozas, Madrid, España;1. Guelph Food Research Centre, Agriculture and Agri-Food Canada, Guelph, Ontario, Canada N1G 5C9;2. Advanced Pharmaceutics and Drug Delivery Laboratory, Leslie Dan Faculty of Pharmacy, University of Toronto, Toronto, Ontario, Canada M5S 3M2;1. National Laboratory for Civil Engineering, LNEC, Av. do Brasil 101, 1700-066 Lisbon, Portugal;2. Doctoral Programme in Geotechnologies Applied to Construction, Energy & Industry, University of Vigo, School of Mining Engineering, Campus Lagoas-Marcosende, 36310 Vigo, Spain;3. Defense University Center, Spanish Naval Academy, Plaza de España 2, 36920 Marín, Pontevedra, Spain;4. Applied Geotechnologies Research Group, University of Vigo, School of Mining Engineering, Campus Lagoas-Marcosende, 36310 Vigo, Spain
Abstract:Dipole antennas for ground-penetrating radar (GPR) radiate and receive electromagnetic waves with a strong directional dependence. Thus, experiments to measure in situ antenna radiation as functions of direction and polarization are of practical interest. Three field experiments were performed. One experiment was over a layered fluvial/eolian sequence; the other two used controlled targets (buried pipes and a metal ball). The radiation patterns were sampled by incrementally varying the antenna orientations and separations while recording reflections from the known targets. The results show qualitative, but systematic, correspondence with approximate theoretical far-field radiation patterns. Slow variations of amplitude with antenna azimuth and dip indicate that antenna orientations within 20° in the standard TE and TM acquisition geometries are adequate for most field applications, but not if detailed amplitude analysis is to be performed. Variations in antenna orientation or height (particularly for heights less than one-quarter wavelength) above the free surface introduce corresponding biases or uncertainties into recorded amplitudes. The variance within any suite of measurements is, in part, a consequence of differences in ground impedance at each antenna location. The theoretically predicted sensitivity to antenna height is mediated by surface roughness at high frequencies. It is necessary to include, or compensate for, the antenna radiation pattern in analysis of field data amplitudes, in experiment design, and in selecting appropriate antennas for specific applications.
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