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Effects of orientation on the diffusive properties of fluid-filled grain boundaries during pressure solution

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Abstract

An unresolved issue in the study of pressure solution in rock materials is the dependence of grain boundary structure and diffusive properties on the mutual orientation of neighbouring grain lattices. We report electrical measurements yielding the diffusivity of differently oriented halite–glass and halite–halite contacts loaded in the presence of brine. The halite–glass contact experiments show pressure solution of the halite and an effect of halite lattice orientation on grain boundary transport. Post-mortem observations show an orientation-dependent grain boundary texture controlled by the periodic bond chains in the halite structure. It is inferred that this texture determines the internal grain boundary structure and properties during pressure solution. In the halite–halite experiments neck-growth occurred, its rate depending on twist-misorientation. The results imply that deformation by pressure solution may lead to lattice-preferred orientation development, and that polymineralic rocks may deform faster at lower stresses than monomineralic rocks.

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References

  • Atkins P, de Paula J (2002) Atkins’ physical chemistry, 7th edn. Oxford University Press, New York, p 1104

    Google Scholar 

  • Bos B, Spiers CJ (2002a) Frictional-viscous flow of phyllosilicate-bearing fault rock: microphysical model and implications for crustal strength profiles. J Geophys Res 107, B2, 10.1029/2001JB000301

  • Bos B, Spiers CJ (2002b) Fluid-assisted healing processes in gouge-bearing faults: insights from experiments on a rock analogue system. Pure Appl Geophys 159:2537–2566

    Article  Google Scholar 

  • Chester JS, Lenz SC, Chester FM, Lang RA (2004) Mechanisms of compaction of quartz sand at diagenetic conditions. Earth Planet Sci Lett 220:435–451

    Article  Google Scholar 

  • Cox SF, Paterson MS (1991) Experimental dissolution–precipitation creep in quartz aggregates at high temperatures. Geophys Res Lett 18:1401–1404

    Google Scholar 

  • De Meer S, Spiers CJ, Peach CJ, Watanabe T (2002) Diffusive properties of fluid-filled grain boundaries measured electrically during active pressure solution. Earth Planet Sci Lett 200:147–157

    Article  Google Scholar 

  • De Meer S, Spiers CJ, Nakashima S (2005) Structure and diffusive properties of fluid-filled grain boundaries: an in situ study using infrared (micro) spectroscopy. Earth Planet Sci Lett 232:403–414

    Article  Google Scholar 

  • Den Brok B (1998) Effect of microcracking on pressure-solution strain rate: the Gratz grain-boundary model. Geology 26:915–918

    Article  Google Scholar 

  • Den Brok B, Morel J, Sahid M (2002) In situ experimental study of roughness development at a stressed solid/fluid interface. In: De Meer S, Drury MR, de Bresser JHP, Pennock GM (eds) Deformation mechanisms, rheology and tectonics: current status and future perspectives. Geological Society Special Publications 200, London, pp 73–83

    Google Scholar 

  • Dysthe DK, Renard F, Porcheron F, Rousseau B (2002a) Fluid in mineral interfaces—molecular simulations of structure and diffusion. Geophys Res Lett 29, 7, 10.1029/2001GL013208

  • Dysthe DK, Podladchikov Y, Renard F, Feder J, Jamtveit B (2002b) Universal scaling in transient creep. Phys Rev Lett 89, 24, 10.1103/PhysRevLett89.246102

  • Dysthe DK, Renard F, Feder J, Jamtveit B, Meakin P, Jøssang T (2003) High resolution measurements of pressure solution creep. Phys Rev E Stat Nonlin Soft Matter Phys 68, PhysRevE.68.011603

  • Elliott D (1973) Diffusion flow laws in metamorphic rocks. Geol Soc Am Bull 84:2645–2664

    Article  Google Scholar 

  • Ghoussoub J, Leroy YM (2001) Solid–fluid phase transformation within grain boundaries during compaction by pressure solution. J Mech Phys Solids 49:2385–2430

    Article  Google Scholar 

  • Gratz AJ (1991) Solution-transfer compaction of quartzites: progress toward a rate law. Geology 19:901–904

    Article  Google Scholar 

  • Green HW (1984) “Pressure solution” creep: some causes and mechanisms. J Geophys Res 89:4313–4318

    Google Scholar 

  • Hartman P, Perdok WG (1955) On the relation between structure and morphology of crystals I. Acta Crystallogr 8:49–52

    Article  Google Scholar 

  • Hickman SH, Evans B (1991) Experimental pressure solution in halite: the effect of grain/interphase boundary structure. J Geol Soc London 148:549–560

    Google Scholar 

  • Hickman SH, Evans B (1992) Growth of grain contacts in halite by solution-transfer: implications for diagenesis, lithification, and strength recovery. In: Evans B, Wong TF (eds) Fault mechanics and transport properties of rocks. Academic, San Diego, pp 253–280

    Google Scholar 

  • Hickman SH, Evans B (1995) Kinetics of pressure solution at halite–silica interfaces and intergranular clay films. J Geophys Res 100(B7):13113–13132

    Article  Google Scholar 

  • Hickman SH, Sibson RH, Bruhn RL (1995) Introduction to special section: mechanical involvement of fluids in faulting. J Geophys Res 100(B7):12831–12840

    Article  Google Scholar 

  • Jin ZM, Green HW, Zhou Y (1994) Melt topology in partially molten mantle peridotite during ductile deformation. Nature 372:164–167

    Article  Google Scholar 

  • Karcz Z, Aharonov E, Ertas D, Polizotti R, Scholz CH (2006) Stability of a sodium chloride indenter contact undergoing pressure solution. Geology 34:61–63

    Article  Google Scholar 

  • Karner SL, Marone C, Evans B (1997) Laboratory study of fault healing and lithification in simulated fault gouge under hydrothermal conditions. Tectonophysics 277:41–55

    Article  Google Scholar 

  • Lehner FK (1995) A model for intergranular pressure solution in open systems. Tectonophysics 245:153–170

    Article  Google Scholar 

  • Niemeijer AR, Spiers CJ, Bos B (2002) Compaction creep of quartz sand at 400–600°C; experimental evidence for dissolution-controlled pressure solution. Earth Planet Sci Lett 195:261–275

    Article  Google Scholar 

  • Porter DA, Easterling KE (1992) Phase transformations in metals and alloys. Chapman and Hall, London

    Google Scholar 

  • Raj R (1982) Creep in polycrystalline aggregates by matter transport through a liquid phase. J Geophys Res 87(B6):4731–4739

    Google Scholar 

  • Renard F, Ortoleva P (1997) Water at grain–grain contacts: Debye–Hückel, osmotic model of stress, salinity, and mineralogy dependence. Geochim Cosmochim Acta 61:1963–1970

    Article  Google Scholar 

  • Renard F, Ortoleva P, Gratier JP (1997) Pressure solution in sandstones: influence of clays and dependence on temperature and stress. Tectonophysics 280:257–266

    Article  Google Scholar 

  • Revil A (2001) Pervasive pressure solution transfer in a quartz sand. J Geophys Res 106(B5):8665–8686

    Article  Google Scholar 

  • Rutter EH (1976) The kinetics of rock deformation by pressure solution. Philos Trans R Soc Lond A 283:203–219

    Google Scholar 

  • Rutter EH (1983) Pressure solution in nature, theory and experiment. J Geol Soc London 140:725–740

    Google Scholar 

  • Rutter EH, Wanten PH (2000) Experimental study of the compaction of phyllosilicate-bearing sand at elevated temperature and with controlled pore water pressure. J Sediment Res 70:107–116

    Google Scholar 

  • Schenk O, Urai J (2004) Microstructural evolution and grain boundary structure during static recrystallization in synthetic polycrystals of sodium chloride containing saturated brine. Contrib Mineral Petrol 146:671–682

    Article  Google Scholar 

  • Schenk O, Urai J, Evans B (2005) The effect of water on recrystallization behavior and grain boundary morphology in calcite—observations of natural marble mylonites. J Struct Geol 27:1856–1872

    Article  Google Scholar 

  • Schenk O, Urai J, Piazolo S (2006) Structure of grain boundaries in wet, synthetic polycrystalline, statically recrystallizing halite—evidence from cryo-SEM observations. Geofluids 6:93–104

    Article  Google Scholar 

  • Schutjens PMTM, Spiers CJ (1999) Intergranular pressure solution in NaCl: grain-to-grain contact experiments under the optical microscope. Oil Gas Sci Technol 54:729–750

    Article  Google Scholar 

  • Sleep NH, Blanpied ML (1992) Creep, compaction and the weak rheology of major faults. Nature 359:687–692

    Article  Google Scholar 

  • Spiers CJ, Schutjens PMTM, Brzesowsky RH, Peach CJ, Liezenberg JL, Zwart HJ (1990) Experimental determination of constitutive parameters governing creep of rock salt by pressure solution. In: Knipe RJ, Rutter EH (eds) Deformation mechanisms, rheology and tectonics. Geological Society Special Publications 54, London, pp 215–227

    Google Scholar 

  • Tada R, Maliva R, Siever R (1987) A new mechanism for pressure solution in porous quartzose sandstone. Geochim Cosmochim Acta 51:2295–2301

    Article  Google Scholar 

  • Vanýsek P (2006) Ionic conductivity and diffusion at infinite dilution. In: Lide DR (ed) CRC handbook of chemistry and physics, internet version 2007, 87th edn, chap 5. Taylor & Francis, Boca Raton, pp 76–78

    Google Scholar 

  • Vigil G, Xu Z, Steinberg S, Israelachvili J (1994) Interactions of silica surfaces. J Colloid Interface Sci 165:367–385

    Article  Google Scholar 

  • Wang JH (1951) Self-diffusion and structure of liquid water. II. Measurement of self-diffusion of liquid water with O18 as tracer. J Am Chem Soc 73:4181–4183

    Article  Google Scholar 

  • Weyl PK (1959) Pressure solution and the force of crystallization—a phenomenological theory. J Geophys Res 64:2001–2025

    Article  Google Scholar 

  • Wintsch RP, Yi K (2002) Dissolution and replacement creep: a significant deformation mechanism in mid-crustal rocks. J Struct Geol 24:1179–1193

    Article  Google Scholar 

  • Zubtsov S, Renard F, Gratier JP, Guiguet R, Dysthe DK, Traskine V (2004) Experimental pressure solution compaction of synthetic halite/calcite aggregates. Tectonophysics 385:45–57

    Article  Google Scholar 

Download references

Acknowledgments

This research and the position of RvN were funded by the The Netherlands Organisation for Scientific Research, grant number 814.01.001. The authors would like to thank Eimert de Graaff for his outstanding technical support and Peter van Krieken for his help with the SEM.

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Authors and Affiliations

  1. High Pressure and Temperature Laboratory, Faculty of Geosciences, Department of Earth Sciences, Utrecht University, P.O. Box 80.021, 3508 TA, Utrecht, The Netherlands

    R. van Noort, C. J. Spiers & C. J. Peach

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  1. R. van Noort
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  2. C. J. Spiers
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  3. C. J. Peach
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Correspondence to R. van Noort.

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van Noort, R., Spiers, C.J. & Peach, C.J. Effects of orientation on the diffusive properties of fluid-filled grain boundaries during pressure solution. Phys Chem Minerals 34, 95–112 (2007). https://doi.org/10.1007/s00269-006-0131-9

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  • DOI: https://doi.org/10.1007/s00269-006-0131-9

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