Research output: Contribution to journal › Article
On the use of the Cole–Cole equations in spectral induced polarization. / Tarasov, A.; Titov, K.
In: Geophysical Journal International, 2013, p. 352-356.Research output: Contribution to journal › Article
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TY - JOUR
T1 - On the use of the Cole–Cole equations in spectral induced polarization
AU - Tarasov, A.
AU - Titov, K.
PY - 2013
Y1 - 2013
N2 - Two different equations, both of which are often called ‘the Cole–Cole equation’, are widely used to fit experimental Spectral Induced Polarization data. The data are compared on the basis of fitting model parameters: the chargeability, the time constant and the exponent. The difference between the above two equations (the Cole–Cole equation proposed by the Cole brothers and Pelton’s equation) is manifested in one of the fitting parameters, the time constant. The Cole–Cole time constant is an inverse of the peak angular frequency of the imaginary conductivity, while Pelton’s time constant depends on the chargeability and exponent values. The difference between the time constant values corresponding to the above two equations grows with the increase of the chargeability value, and with the decrease of the Cole–Cole exponent value. This issue must be taken into consideration when comparing the experimental data sets for high polarizability media presented in terms of the Cole–Cole parameters.
AB - Two different equations, both of which are often called ‘the Cole–Cole equation’, are widely used to fit experimental Spectral Induced Polarization data. The data are compared on the basis of fitting model parameters: the chargeability, the time constant and the exponent. The difference between the above two equations (the Cole–Cole equation proposed by the Cole brothers and Pelton’s equation) is manifested in one of the fitting parameters, the time constant. The Cole–Cole time constant is an inverse of the peak angular frequency of the imaginary conductivity, while Pelton’s time constant depends on the chargeability and exponent values. The difference between the time constant values corresponding to the above two equations grows with the increase of the chargeability value, and with the decrease of the Cole–Cole exponent value. This issue must be taken into consideration when comparing the experimental data sets for high polarizability media presented in terms of the Cole–Cole parameters.
KW - Electrical properties
KW - Electromagnetic theory
KW - Hydrogeophysics.
U2 - 10.1093/gji/ggt251
DO - 10.1093/gji/ggt251
M3 - Article
SP - 352
EP - 356
JO - Geophysical Journal International
JF - Geophysical Journal International
SN - 0956-540X
ER -
ID: 7378536