Abstract
Electrical impedance measurements in the laboratory on silicate melts are used to interpret magnetotelluric anomalies. On the basis of 2- and 4-electrode measurements, we show that the influence of the electrodes of the 2-electrode system on the measured resistivity can be of significant importance for low-resistivity melts and increases with temperature. At 1400 °C, the resistivity of very conductive melts measured with two electrodes can reach six times the resistivity value measured with four electrodes. A short-circuit experiment is needed to correct the 2-electrode data. Electrodes contribution is also estimated for samples from other studies, for which the resistance of the electrical cell can be as high as the resistance of the sample. A correction of the resistivity data from the literature is proposed and values of the corresponding Arrhenian parameters are recommended.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Brownleeite: A new manganese silicide mineral in an interplanetary dust particle
- Simulation of thermodynamic mixing properties of actinide-containing zircon solid solutions
- Multilevel modular mesocrystalline organization in red coral
- High-pressure behavior of 2M1 muscovite
- Chopinite-sarcopside solid solution, [(Mg,Fe)3□](PO4)2, in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
- Distribution of rare earth elements in lunar zircon
- Methodological re-evaluation of the electrical conductivity of silicate melts
- Site-specific infrared O-H absorption coefficients for water substitution into olivine
- High-pressure phase transition of a natural pigeonite
- Location and quantification of hydroxyl in wadsleyite: New insights
- Optical spectroscopic study of natural Fe-rich Pizzo Forno staurolite at different temperatures and pressures
- Metasideronatrite: Crystal structure and its relation with sideronatrite
- Optical absorption, luminescence, and electron paramagnetic resonance (EPR) spectroscopy of crystalline to metamict zircon: Evidence for formation of uranyl, manganese, and other optically active centers
- Factors responsible for crystal-chemical variations in the solid solutions from illite to aluminoceladonite and from glauconite to celadonite
- REE diffusion in olivine
- Phase transition induced by solid solution: The BCa-BMg substitution in richteritic amphiboles
- Aiolosite, Na2(Na2Bi)(SO4)3Cl, a new sulfate isotypic to apatite from La Fossa Crater, Vulcano, Aeolian Islands, Italy
- Gayite, a new dufrénite-group mineral from the Gigante granitic pegmatite, Córdoba province, Argentina
- Galliskiite, Ca4Al2(PO4)2F8·5H2O, a new mineral from the Gigante granitic pegmatite, Córdoba province, Argentina
- Description and crystal structure of liversidgeite, Zn6(PO4)4·7H2O, a new mineral from Broken Hill, New South Wales, Australia
- Evidence of dmisteinbergite (hexagonal form of CaAl2Si2O8) in pseudotachylyte: A tool to constrain the thermal history of a seismic event
- Partitioning of Eu between augite and a highly spiked martian basalt composition as a function of oxygen fugacity (IW-1 to QFM): Determination of Eu2+/Eu3+ ratios by XANES
- Density functional calculation of the infrared spectrum of surface hydroxyl groups on goethite (α-FeOOH)
- X-ray diffraction and Mössbauer spectroscopy of Fe3+-bearing Mg-silicate post-perovskite at 128–138 GPa