Register      Login
Soil Research Soil Research Society
Soil, land care and environmental research
RESEARCH ARTICLE

Effects of water content and temperature on the surface conductivity of bentonite clay

M. A. Mojid A C and H. Cho B
+ Author Affiliations
- Author Affiliations

A Department of Irrigation and Water Management, Bangladesh Agricultural University, Mymensingh – 2202, Bangladesh.

B Department of Agricultural Sciences, Saga University, Saga 840-8502, Japan.

C Corresponding author. Email: ma_mojid@yahoo.com

Soil Research 50(1) 44-49 https://doi.org/10.1071/SR11228
Submitted: 4 September 2011  Accepted: 21 December 2011   Published: 1 February 2012

Abstract

This study explored the effects of water content and temperature on the mobility of exchangeable cations (termed the surface ionic mobility and hereafter ionic mobility) in the hydration layers of bentonite clay. The ionic mobility directly governs the surface conductivity of the clay. The investigation was done by measuring the bulk electrical conductivity (EC) of four sand–bentonite mixtures of different proportions for a wide range of water contents under constant temperature, and three bentonite samples at different water contents over 5–90°C. The ionic mobility was determined from the surface conductivity at the mean ionic strength of the hydration layers. The ionic mobility in the sand–bentonite samples increased with an increase in hydration layer thickness. For a given thickness of the hydration layer, the greater the bentonite content of a sample, the smaller was the ionic mobility. The ionic mobility in the bentonite samples at different water contents also increased, at reduced rates, with a rise in temperature. Consequently, the surface conductivity of the samples increased non-uniformly, at two different rates, with an increase in temperature. The increasing rate of this conductivity depended on temperature; over the low temperature range which depended on the water content, the rate was 0.013 dS/m.K, and over higher temperature range, the rate decreased to 0.008 dS/m.K. The commonly used temperature correction factor, 0.019 dS/m.K, for EC therefore did not hold true for the bentonite samples.

Additional keywords: EDL, ionic mobility, surface conductivity, temperature, water content.


References

Bockris JOM, Reddy AKX (1972) ‘Modern aspects of electrochemistry.’ (Plenum: New York)

Bolt GH (Ed.) (1982) ‘Soil chemistry. Vol. B: Physico-chemical models.’ (Elsevier Science: Amsterdam)

Carrique F, Arroyo FJ, Jiménez ML, Delgado AV (2003) Influence of double-layer overlap on the electrophoretic mobility and DC conductivity of a concentrated suspension of spherical particles. Journal of Physical Chemistry (B 2003) 107, 3199–3206.

Cremers AE, Laudelout H (1966) Surface mobilities of cations in clays. Soil Science Society of America Proceedings 30, 570–576.
Surface mobilities of cations in clays.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaF2sXkvVegsQ%3D%3D&md5=81a93a0e4f3430946f8fdeda42eff641CAS |

Glover PWJ, Walker E (2009) Grain-size to effective pore-size transformation derived from electrokinetic theory. Geophysics 74, E17–E29.
Grain-size to effective pore-size transformation derived from electrokinetic theory.Crossref | GoogleScholarGoogle Scholar |

Gouy G (1910) Sur la constitution de la charge électrique à la surface d’um électrolyte. Annales de Physique (Paris) Série 4, 457–468.

Ito M Okamoto M Shibata M Sasaki Y Tanbara T Suzuki K Watanabe T (1993) Mineral composition analysis of bentonite. PNC TN8430, 93-003. Power Reactor and Nuclear Fuel Development Corporation, Japan.

Kan R, Sen PN (1987) Electrolytic conduction in periodic arrays of insulators with charges. The Journal of Chemical Physics 86, 5748–5756.
Electrolytic conduction in periodic arrays of insulators with charges.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaL2sXks1yku70%3D&md5=f72f23825d232c9abcf4aa62aa85f45bCAS |

Leroy P, Revil A (2004) A triple-layer model of the surface electrochemical properties of clay minerals. Journal of Colloid and Interface Science 270, 371–380.
A triple-layer model of the surface electrochemical properties of clay minerals.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD3sXpvFemtL4%3D&md5=39b11f5d5789fd08075d60a4c06b577bCAS |

McNeill JD (1980) ‘Electrical conductivity of soils and rocks.’ Technical Note TN-5. (Geonics Ltd: Mississauga, ON)

Mojid MA, Cho H (2006) Estimating the fully developed diffuse double layer thickness from the bulk electrical conductivity in clay. Applied Clay Science 33, 278–286.
Estimating the fully developed diffuse double layer thickness from the bulk electrical conductivity in clay.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD28XotFertbo%3D&md5=762d9f0413e271f5808c6c37fd31e8cbCAS |

Mojid MA, Cho H (2008) Wetting solution and electrical double layer contributions to bulk electrical conductivity of sand–clay mixtures. Vadose Zone Journal 7, 972–980.
Wetting solution and electrical double layer contributions to bulk electrical conductivity of sand–clay mixtures.Crossref | GoogleScholarGoogle Scholar |

Mojid MA, Wyseure GCL, Rose DA (1997) Extension of the measurement range of electrical conductivity by time-domain reflectometry (TDR). Hydrology and Earth System Sciences 1, 175–183.
Extension of the measurement range of electrical conductivity by time-domain reflectometry (TDR).Crossref | GoogleScholarGoogle Scholar |

Patchett JG (1975) An investigation of shale conductivity. In ‘SPWLA 16th Annual Logging Symposium’. New Orleans. Paper U. Society of Petrophysicists and Well Log Analysts.

Revil A, Glover PWJ (1997) Theory of ionic surface electrical conduction in porous media. Physical Review B: Condensed Matter and Materials Physics 55, 1757–1773.
Theory of ionic surface electrical conduction in porous media.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK2sXptFerug%3D%3D&md5=ad8df6ff0efee10b20c273db46e3dff4CAS |

Revil A, Cathles LM, Losh S, Nunn JA (1998) Electrical conductivity in shaly sands with geophysical applications. Journal of Geophysical Research 103, 23 925–23 936.
Electrical conductivity in shaly sands with geophysical applications.Crossref | GoogleScholarGoogle Scholar |

Revil A, Hermitte D, Spangenberg E, Cochemé JJ (2002) Electrical properties of zeolitized volcaniclastic materials. Journal of Geophysical Research 107, 2168
Electrical properties of zeolitized volcaniclastic materials.Crossref | GoogleScholarGoogle Scholar |

Schoch RB, Han J, Renaud P (2008) Transport phenomena in nanofluidics. Reviews of Modern Physics 80, 839–883.
Transport phenomena in nanofluidics.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD1cXhtFCku73O&md5=c139cb8a0ed8b393e3e89958f3a19ac6CAS |

Waxman MH, Smith LJM (1968) Electrical conductivities in oil-bearing shaly sand. Society of Petroleum Engineers Journal 8, 107–122.
Electrical conductivities in oil-bearing shaly sand.Crossref | GoogleScholarGoogle Scholar |