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By Richard D. Miller, John H. Bradford, Klaus Holliger

Published via the yankee Geophysical Union as a part of the Geophysical improvement sequence, quantity 15.

Advances in Near-surface Seismology and Ground-penetrating Radar (SEG Geophysical advancements sequence No. 15) is a suite of unique papers through well known and revered authors from around the globe. applied sciences utilized in the applying of near-surface seismology and ground-penetrating radar have obvious major advances within the final a number of years. either equipment have benefited from new processing instruments, elevated laptop speeds, and an increased number of applications.

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Extra resources for Advances in Near-surface Seismology and Ground-penetrating Radar, Volume 15

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Kauzmann, 1969, The structure and properties of water: Oxford University Press. Ernst, J. , A. G. Green, H. Maurer, K. Holliger, 2007, Application of a new 2D time-domain full-waveform inversion scheme to crosshole radar data: Geophysics, 72, no. 5, J53–J64. Farquharson, C. , 2008, Constructing piecewise-constant models in multidimensional minimum-structure inversions: Geophysics, 73, no. 1, K1–K9. Fine, R. , and F. J. Millero, 1973, Compressibility of water as a function of temperature and pressure: Journal of Chemical Physics, 59, 5529–5536.

Kowalsky, M. , S. Finsterle, J. Peterson, S. Hubbard, Y. Rubin, E. Majer, A. Ward, and G. Gee, 2005, Estimation of field-scale soil hydraulic parameters and dielectric parameters through joint inversion of GPR and hydrological data: Water Resources Research, 41, W11425. , K. Holliger, and D. E. : Geophysical Research Letters, 25, 2889–2892. Monteiro Santos, F. , S. A. Sultan, P. Represesas, and A. L. El Sorady, 2006, Joint inversion of gravity and geoelectrical data for groundwater and structural investigation: Application to the northwestern part of Sinai, Egypt: Geophysical Journal International, 165, 705–718.

Org/ Chapter 1: Joint Inversion of Crosshole GPR and Seismic Traveltime Data about the field site is very important. , salinity), such as in a coastal setting or at a contaminated site, as discussed in Linde et al. (2006). Access to geophysical logging data makes it possible to investigate structural similarity in the vertical direction at a few positions. Note that structural similarity is imposed at the resolution of the resulting models, not at the typically higher resolution of the logging data.

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