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pro vyhledávání: '"Alan C. Tripp"'
Autor:
Alan C. Tripp
Publikováno v:
GEOPHYSICS. 70:25ND-31ND
Geophysics has proved to be an effective means of prospecting for the raw materials necessary for modern life. Electromagnetic techniques are the methods of choice when buried treasure has an anomalous electrical conductivity or dielectric permittivi
Autor:
A. A. Ekdale, Alan C. Tripp
Publikováno v:
Journal of Geoscience Education. 53:271-280
Sonification is the process of translating any type of data into sound. In paleontology, it is possible to render various aspects of fossil shapes, such as cephalopod suture patterns or brachiopod commissure lines, as a series of musical tones that c
Publikováno v:
GEOPHYSICS. 66:824-835
The finite‐difference time‐domain method is used for high‐resolution full‐wave analysis of cross‐borehole electromagnetic surveys of buried nickel sulfide deposits. The method is validated against analytical methods for simple cases, but is
Publikováno v:
IEEE Transactions on Antennas and Propagation. 48:1438-1441
Prof. James R. Wait (1951, 1953, 1967) examined electromagnetic (EM) wave propagation in many situations of interest to mining production, including propagation in tunnels, propagation along extended conductors such as cables and drill stems, and pro
Publikováno v:
Geophysical Prospecting. 46:589-601
Following previous work on bounds for complex dielectrics, bounds on the complex conductivity of a mixture of two isotropic components can be developed which are independent of any special assumption concerning the geometry of the mixture. If certain
Autor:
Zhongzhou Xiong, Alan C. Tripp
Publikováno v:
GEOPHYSICS. 62:1097-1106
Three‐dimensional electromagnetic (EM) modeling in the frequency range from 100 kHz to about 200 MHz using integral equations is examined. The modeling algorithm is formulated in the frequency domain. Time‐domain responses for ground‐penetratin
Autor:
Alan C. Tripp, Zhongzhou Xiong
Publikováno v:
GEOPHYSICS. 62:1127-1131
Ground‐penetrating radar (GPR) has been a very efficient tool for mapping shallow targets for applications such as those in geological engineering and environmental management (Fisher et al. 1992). Since the application of GPR depends on the comple
Publikováno v:
Journal of geomagnetism and geoelectricity. 49:1659-1676
We discuss in a simplified surface-to-borehole example the resolution of the coefficient of anisotropy λ for an anisotropic layer sandwiched in an isotropic half-space as a function of transmitter-receiver configuration and magnetic field components
Autor:
Elena Cherkaeva, Alan C. Tripp
Publikováno v:
Inverse Problems. 12:869-883
In order to determine the conductivity of a body or of a region of the Earth using electrical prospecting, currents are injected on the surface, surface voltage responses are measured, and the data are inverted to a conductivity distribution. In the
Autor:
Alan C. Tripp, Tsili Wang
Publikováno v:
GEOPHYSICS. 61:110-120
A finite‐difference, time‐domain solution to Maxwell’s equations has been developed for simulating electromagnetic wave propagation in 3-D media. The algorithm allows arbitrary electrical conductivity and permittivity variations within a model.