Metakaolin

Metakaolin is a dehydroxylated form of the clay mineral kaolinite.

Stone that are rich in kaolinite are known as china clay or kaolin, traditionally used in the manufacture of porcelain. The particle size of metakaolin is smaller than cement particles, but not as fine as silica fume.

Kaolinite sources

The quality and reactivity of metakaolin is strongly dependent of the characteristics of the raw material used. Metakaolin can be produced from a variety of primary and secondary sources containing kaolinite:

Forming metakaolin

The T-O clay mineral kaolinite does not contain interlayer cations or interlayer water. The temperature of dehydroxylation depends on the structural layer stacking order. Disordered kaolinite dehydroxylates between 530 and 570 °C, ordered kaolinite between 570 and 630 °C. Dehydroxylated disordered kaolinite shows higher pozzolanic activity than ordered.[1] The dehydroxylation of kaolin to metakaolin is an endothermic process due to the large amount of energy required to remove the chemically bonded hydroxyl ions. Above the temperature range of dehydroxylation, kaolinite transforms into metakaolin, a complex amorphous structure which retains some long-range order due to layer stacking.[2] Much of the aluminum of the octahedral layer becomes tetrahedrally and pentahedrally coordinated.[3] In order to produce a pozzolan (supplementary cementitious material) nearly complete dehydroxylation must be reached without overheating, i.e., thoroughly roasted but not burnt. This produces an amorphous, highly pozzolanic state, whereas overheating can cause sintering, to form a dead burnt, nonreactive refractory, containing mullite and a defect Al-Si spinel.[4] Reported optimum activation temperatures vary between 550 and 850 °C for varying durations, however the range 650-750 °C is most commonly quoted.[5] In comparison with other clay minerals kaolinite shows a broad temperature interval between dehydroxylation and recrystallization, much favoring the formation of metakaolin and the use of thermally activated kaolin clays as pozzolans. Also, because the octahedral layer is directly exposed to the interlayer (in comparison to for instance T-O-T clay minerals such as smectites), structural disorder is attained more easily upon heating.

High-reactivity metakaolin

High-reactivity metakaolin (HRM) is a highly processed reactive aluminosilicate pozzolan, a finely-divided material that reacts with slaked lime at ordinary temperature and in the presence of moisture to form a strong slow-hardening cement. It is formed by calcining purified kaolinite, generally between 650–700 °C in an externally fired rotary kiln. It is also reported that HRM is responsible for acceleration in the hydration of ordinary portland cement (OPC), and its major impact is seen within 24 hours. It also reduces the deterioration of concrete by Alkali Silica Reaction (ASR), particularly useful when using recycled crushed glass or glass fines as aggregate.[6] The amount of slaked lime that can be bound by metakaolin is measured by the modified Chapelle test.[7][8]

Adsorption properties

The adsorption surface properties of the metakaolins can be accomplished by inverse gas chromatography analysis.[9]

Concrete application

Considered to have twice the reactivity of most other pozzolans, metakaolin is a valuable admixture for concrete/cement applications. Replacing portland cement with 8–20% (by weight) metakaolin produces a concrete mix, which exhibits favorable engineering properties, including: the filler effect, the acceleration of OPC hydration, and the pozzolanic reaction. The filler effect is immediate, while the effect of pozzolanic reaction occurs between 3 and 14 days.[10]

Advantages

Uses

See also

References

  1. ↑ Kakali, G.; Perraki T.; Tsivilis S.; Badogiannis E. (2001). "Thermal treatment of kaolin: the effect of mineralogy on the pozzolanic activity". Applied Clay Science. 20: 73–80. doi:10.1016/s0169-1317(01)00040-0.
  2. ↑ Bellotto, M.; Gualtieri A.; Artioli A.; Clark S.M. (1995). "Kinetic study of the kaolinite-mullite reaction sequence". Physics and Chemistry of Minerals. 22: 207–217. doi:10.1007/bf00202254.
  3. ↑ Fernandez, R.; Martirena F.; Scrivener K.L. (2011). "The origin of the pozzolanic activity of clay minerals: A comparison between kaolinite, illite and montmorillonite.". Cement and Concrete Research. 41: 113–122. doi:10.1016/j.cemconres.2010.09.013.
  4. ↑ "High Reactivity Metakaolin (HRM)". Advanced Cement Technologies, LLC. Metakaolin. Retrieved May 7, 2010.
  5. ↑ Snellings, R.; Mertens G.; Elsen J. (2012). "Supplementary cementitious materials". Reviews in Mineralogy and Geochemistry. 74: 211–278. doi:10.2138/rmg.2012.74.6.
  6. ↑ "High Reactivity Metakaolin (HRM)". Alkali-Silica Reaction (ASR). Metakaolin. Retrieved Oct 22, 2010.
  7. ↑ modified Chapelle test,
  8. ↑ Ferraz, E.; et al. (2015). "POZZOLANIC ACTIVITY OF METAKAOLINS BY THE FRENCH STANDARD OF THE MODIFIED CHAPELLE TEST: A DIRECT METHOLOGY". Acta Geodynamica et Geometerialia Aspects. 12: 289–298. doi:10.13168/AGG.2015.0026.
  9. ↑ Gamelas, J.; Ferraz, E.; Rocha, F. (2014). "An insight into the surface properties of calcined kaolinitic clays: the grinding effect". Colloids and Surfaces A: Physicochemical and Engineering Aspects. 455: 49–57. doi:10.1016/j.colsurfa.2014.04.038.
  10. ↑ filler effect,
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