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@ARTICLE{Nyari:9456,
author = {Nyari, Z. and Kanli, AI. and Janos, S. and Tillmann, A.},
title = {{T}he use of non-conventional {CPT}e data in determination
of 3-{D} electrical resistivity distribution},
journal = {Journal of applied geophysics},
volume = {70},
issn = {0926-9851},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {PreJuSER-9456},
pages = {255 - 265},
year = {2010},
note = {This work is funded partly by the NATO Collaborative
Linkage Grant No. 979868. This paper presents partly the
results of research project GVOP-3.1.1-2004-05-0187/3.0
supported by the National Development Plan, the EU
co-financed part of the Europe Plan. This work was supported
by the Research Fund of Istanbul University, project number:
UDP-4295/23092009. We would like to thank Klaus Holliger
(Editor-in-Chief) and the reviewers for their constructive
remarks.},
abstract = {The spatial distribution of the electrical resistivity data
provides useful information for investigating and modeling
the fluid transport processes. 3D electrical resistivity
distribution provides information about water flow and
changes in electrical resistivity of the pore
fluid.Therefore, to assist in understanding and modeling of
the fluid transport process, 3D spatial distribution of the
electrical resistivity data with the corresponded 3D
geological section were mapped and interpreted in the test
site located in western Germany. A process of deriving
electrical resistivity values from the mechanical and
radioactive parameters of cone penetration tests (CPT) and
geological information of boreholes was presented. A
reliable method which gives accurate resistivity values in
cases of near surface sediments was introduced. Then a field
test was executed where the calculated resistivity values
were compared with the measured CPTe resistivity data. The
CPTe (cone penetration test with electrical extension) data
were also used in correlating to the ERT (electrical
resistivity tomography) data. Consequently, obtained dense
CPT surveys give us the possibility to determine a high
resolution resistivity distribution of the investigated
area. (C) 2010 Elsevier B.V. All rights reserved.},
keywords = {J (WoSType)},
cin = {ICG-4},
ddc = {620},
cid = {I:(DE-Juel1)VDB793},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Geosciences, Multidisciplinary / Mining $\&$ Mineral
Processing},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000276417700008},
doi = {10.1016/j.jappgeo.2010.01.008},
url = {https://juser.fz-juelich.de/record/9456},
}