Magnesium hydroxychloride

Short description: Class of chemical compounds

Magnesium hydroxychloride[1] is the traditional term for several chemical compounds of magnesium, chlorine, oxygen, and hydrogen whose general formula xMgO·yMgCl2·zH2O, for various values of x, y, and z; or, equivalently, Mgx+y(OH)2xCl2y(H2O)z−x . The simple chemical formula that is often used is MgClOH, which appears in high school subject, for example.Other names for this class are magnesium chloride hydroxide,[2] magnesium oxychloride, and basic magnesium chloride.[3] Some of these compounds are major components of Sorel cement.

## Contents

* 1 Compounds
* 2 History
* 3 Properties
* 3.1 Solubility
* 3.2 Decomposition and degradation
* 4 Structure
* 5 Preparation
* 5.1 From MgO or Mg(OH)2 and MgCl2
* 5.2 From MgO or Mg(OH)2 and HCl
* 5.3 From MgCl2 and NaOH
* 5.4 Other
* 6 References

## Compounds

Phase diagram for the ternary system MgO – MgCl2 – H2O at ~ 23 °C.[4] The stable oxychloride phases are P5 (Phase 5, 5:1:8) and P3 (phase 3, 3:1:8). The dark blue region is clear solution. The triple equilibrium points of the saturated solution are S1 (Sol:Mg(OH)2:P5), S2 (Sol:P5:P3), and S3 (Sol:P3:MgCl2·6H2O). The light blue region is the approximate range of compositions of homogeneous metastable gels.

The ternary diagram of the system MgO – MgCl2 – H2O has the following well-defined and stable phases:[4][5][6]

* Mg(OH)2 (magnesium hydroxide, the mineral brucite)
* 2Mg(OH)2·MgCl2·4H2O = Mg3(OH)4Cl2·4H2O ("phase 2", "2:1:4")
* 3Mg(OH)2·MgCl2·8H2O = 2Mg2(OH)3Cl·4H2O ("phase 3", "3:1:8")
* 5Mg(OH)2·MgCl2·8H2O = 2Mg3(OH)5Cl·4H2O ("Phase 5", "5:1:8")
* 9Mg(OH)2·MgCl2·5H2O = Mg10(OH)18Cl2·5H2O ("Phase 9", "9:1:5")
* MgCl2·6H2O (magnesium chloride hexahydrate)

Phase 3 and phase 5 may exist at ambient temperature, whereas the phase 2 and phase 9 are stable only at temperatures above 100 °C.[5] All these compounds are colorless crystalline solids.

At ambient temperature, there are also gel-like homogeneous phases that form initially when the reagents are mixed, and eventually crystallize as phase 5, phase 3, or mixtures with Mg(OH)2 or MgCl2·6H2O.[4]

There are also other lower hydrates that can be obtained by heating the "natural" phases:[7]

* 2Mg(OH)2·MgCl2·2H2O (phase 2 dihydrate; ~230 °C)
* 3Mg(OH)2·MgCl2·5H2O (phase 3 pentahydrate; ~110 °C)
* 3Mg(OH)2·MgCl2·4H2O (phase 3 tetrahydrate; ~140 °C)
* 5Mg(OH)2·MgCl2·4H2O (phase 5 tetrahydrate; ~120 °C)
* 5Mg(OH)2·MgCl2·3H2O (phase 5 trihydrate; ~150 °C)
* 9Mg(OH)2·MgCl2·2H2O (phase 9 dihydrate; ~190 °C)

In addition, a heptahydrate of phase 5, 5Mg(OH)2·MgCl2·7H2O, can be obtained by washing the natural octahydrate with ethanol.[7]

All four stable phases have anhydrous versions, such as 3Mg(OH)2·MgCl2 (anhydrous phase 3) and 5Mg(OH)2·MgCl2 (anhydrous phase 5), with the crystal structure of Mg(OH)2. They can be obtained by heating them to about 230 °C (phases 3 and 5) about 320 °C (phase 2), and about 260 °C (phase 9).[7]

## History

These compounds are the primary components of matured magnesia cement, invented in 1867 by the French chemist Stanislas Sorel.[8]

In the late 19th century, several attempts were made to determine the composition of set Sorel's cement, but the results were not conclusive.[9][10][11][12] Phase 3 was properly isolated and described by Robinson and Waggaman in 1909,[9] and phase 5 was identified by Lukens in 1932.[13]

## Properties

### Solubility

The oxychlorides are only very slightly soluble in water.[14]

In the system MgO – MgCl2 – H2O at about 23 °C, the completely liquid region has vertices at the following triple equilibrium points (as mass fractions, not molar fractions):[4]

S1 = 0.008 MgO + 0.170 MgCl2 \+ 0.822 H2O (Sol:Mg(OH)2:P5)
S2 = 0.010 MgO + 0.222 MgCl2 \+ 0.768 H2O (Sol:P5:P3)
S3 = 0.012 MgO + 0.345 MgCl2 \+ 0.643 H2O (Sol:P3:MgCl2·6H2O)

The other vertices are pure water, magnesium chloride hexahydrate, and the saturated Mg(OH)2 solution (0.0044 MgO + 0.9956 H2O by mass).[4]

### Decomposition and degradation

The anhydrous forms decompose when heated above 450-500 °C by decomposition of the hydroxide and chloride anions, releasing water and hydrogen chloride and leaving a magnesium oxide residue, by the reactions:[7]

2HO− → O2− \+ H2O
H2O \+ 2Cl− → O2− \+ 2HCl

Extended exposure of magnesium oxychlorides to water leaches out the soluble MgCl2, leaving hydrated brucite Mg(OH)2.[15]

On exposure to the atmosphere, the oxychlorides will slowly react with carbon dioxide CO2 from the air to form magnesium chlorocarbonates. Anhydrous and partially hydrated forms also absorb water, turning into phase 5 and then phase 3 on the way to the chlorocarbonate. The exceptions are the dihydrate and hexahydrate of phase 9, that remain unchanged for many months.[7]

## Structure

The crystal structure of phase 3 is triclinic with space group P1¯ and z = 2.[16] The solid consists polymeric aquohydroxo cations, in the form of double chains of magnesium atoms surrounded and bridged by the oxygen atoms in hydroxy groups and complexed water molecules. These linear cations are interleaved and neutralized by chloride anions and some unbound water molecules, yielding the general formula [(Mg2(OH)3(H2O)3)n]n+ ·nCl− · nH2O.[17][16][7]

The structure of phase 5 is believed to be similar, with generic formula [(Mg3(OH)5(H2O)x)n]n+·nCl− · n(4-x)H2O.[17]

The anhydrous forms of phase 3 and phase 5 have the same structure as Mg(OH)2: namely, layers of magnesium cations, each sandwiched between two layers of hydroxy or chloride anions.[7]

Phase 5 crystals form as long needles consisting of rolled-up sheets.[18]

The Raman spectrum of phase 3 has peaks at 3639 and 3657 cm−1, whereas phase 5 has peaks at 3608 and 3691 cm−1, and brucite has a peak at 3650 cm−1. These peaks are attributed to stretching vibrations of the OH groups. Phase 3 has also a peak at 451 cm−1, attributed to the stretching of Mg–O bonds.[6][16]

## Preparation

### From MgO or Mg(OH)2 and MgCl2

Phases 3 and 5 can be prepared by mixing powdered magnesium oxide MgO with a solution of magnesium chloride MgCl2 in water H2O, in molar ratios 3:1:11 and 5:1:13, respectively, at room temperature. This is the common method of preparing Sorel magnesia cement.[16] Magnesium hydroxide Mg(OH)2 can also be used instead of the oxide, with adjusted amount of water.

For best results, the magnesium oxide should have small particle size and large surface area. It can be prepared by calcination of magnesium hydroxycarbonate Mg5(OH)2(CO3)4·4H2O at about 600 °C. Higher temperatures increase particle size leading to slower reaction rate.[19]

It is believed that, during the reaction, the magnesium oxide is continuously hydrated and dissolved, helped by the slightly acidic character of the magnesium chloride solution.[17] The acidity is attributed to hydrolysis of the magnesium hexahydrate cations:

[Mg(H2O)6]2+ ↔ [Mg(OH)(H2O)5]+ \+ H+

The protons (which are actually hydrated, e.g. as H3O+) make the solution acidic; the pH varies from 6.5 to 4.7 as the concentration of MgCl2 increases from 30% to 70% (weight basis).[17] The protons then react with and dissolve the nearly insoluble oxide or hydroxide, by such reactions as[17]

MgO \+ 2H+ \+ 5H2O → [Mg(H2O)6]2+
Mg(OH)2 \+ H+ \+ 4H2O → [Mg(OH)(H2O)5]+

The ions [Mg(H2O)6]2+ and [Mg(OH)(H2O)5]+ in solution then combine into complex cations with multiple magnesium atoms, bridged by hydroxide anions and water molecules (magnesium aquohydroxo complexes), with general formula [Mgx(OH)y(H2O)z](2x−y)+.[17] This process involves additional hydrolysis, turning some H2O ligands into OH− and freeing more H+, which keeps dissolving more oxide. With enough magnesium chloride, the dissolution of the oxide is relatively fast, and a clear solution of magnesium aquohydroxo cations can be obtained by filtration.[13][12]

Over a period of several hours, those cations keep combining into larger complexes, becoming less soluble as they grow. After a few hours (at room temperature), those cations and the chloride anions precipitate as (or turn the solution into) a hydrogel, which then gradually crystallizes into a mixture of phase 3, phase 5, solid magnesium oxide and/or chloride, and/or some residual solution.[17] Depending on the proportion of the reagents, phase 5 may form at first, but then will react with excess chloride to form phase 3.[16]

The magnesium oxide can also react with water to form the hydroxide, which, being poorly soluble, would coat the oxide grains and stop further hydration. The acidity provided by hydrolysis of the cations in solution dissolves this coating, and thus allows the process to run continuously until one of the reagents is exhausted.[17]

### From MgO or Mg(OH)2 and HCl

The compounds can also be prepared from magnesium oxide or hydroxide and hydrochloric acid. The MgO – H2O – MgCl2 phase diagram is contained in the MgO – H2O – HCl diagram.[4]

### From MgCl2 and NaOH

The difficulties of preparing the magnesium oxide and ensuring its full reaction can be avoided by using NaOH instead of MgO or Mg(OH)2, so that all reagents are solutions. However, sodium chloride NaCl may also precipitate for certain concentrations of the reagents.

With this route, stable phase 5 precipitates in a rather narrow range of conditions, namely when the concentration [Cl] of chloride anions in solution is 2.02 ± 0.03 mol/L, the concentration [Mg] of magnesium (as Mg2+ and other cations) is 1.78 ± 0.07 mol/L, and the pH is 7.65 ± 0.05. Stable phase 3 precipitates in a broader range of cases, namely when [Cl] is 6.48 ± 2.17 mol/L, [Mg] is 3.14 ± 1.12 mol/L, and the pH is 6.26 ± 0.14[14][19]

### Other

A short note from 1872 reported the formation a solid with approximate formula 5MgO·MgCl2·13H2O, as a mass of fine needles, from a solution of magnesium ammonium chloride Mg(NH4)Cl3 with excess ammonia left standing for several months.[10]

G. André claimed in 1882 the preparation of anhydrous oxychlorides by fusing anhydrous magnesium chloride with powdered magnesium oxide.[12]

## References

1. ↑ Bodine, M. W. Jr. (1976): "Magnesium hydroxychloride: A possible pH buffer in marine evaporite brines?" Geology, volume 4, issue 2, pages 76-80. doi:10.1130/0091-7613(1976)4<76:MHAPPB>2.0.CO;2
2. ↑ Yongliang Xiong, Haoran Deng, Martin Nemer, and Shelly Johnsen (2010): "Experimental determination of the solubility constant for magnesium chloride hydroxide hydrate (Mg3Cl(OH)5·4H2O, phase 5) at room temperature, and its importance to nuclear waste isolation in geological repositories in salt formations". Geochimica et Cosmochimica Acta, volume 74, issue 16, pages 4605–4611. doi:10.1016/j.gca.2010.05.029
3. ↑ JianSong Wu, YingKai Xiao, JingYun Su, TingTing Deng, JieRong Feng, YuYing Mo, and Mei Zeng (2011): "The growth mechanism of the basic magnesium chloride whisker". Science China Technological Sciences, volume 54, issue 3, pages 682–690. doi:10.1007/s11431-011-4300-9
4. ↑ 4.0 4.1 4.2 4.3 4.4 4.5 Ladawan Urwongse and Charles A, Sorrell (1980): "The System MgO‐MgCl2‐H2O at 23°C". Journal of the American Ceramic Society, volume 63, issue 9-10, pages 501-504. doi:10.1111/j.1151-2916.1980.tb10752.x
5. ↑ 5.0 5.1 Zongjin Li and C. K. Chau (2007): "Influence of molar ratios on properties of magnesium oxychloride cement". Cement and Concrete Research, volume 37, issue 6, pages 866-870. doi:10.1016/j.cemconres.2007.03.015
6. ↑ 6.0 6.1 Ronan M. Dorrepaal and Aoife A. Gowen (2018): "Identification of Magnesium Oxychloride Cement Biomaterial Heterogeneity using Raman Chemical Mapping and NIR Hyperspectral Chemical Imaging". Scientific Reports, volume 8, article number 13034. doi:10.1038/s41598-018-31379-5
7. ↑ 7.0 7.1 7.2 7.3 7.4 7.5 7.6 W. F. Cole and T. Demediuk (1955): "X-Ray, thermal, and Dehydration studies on Magnesium oxychlorides". Australian Journal of Chemistry, volume 8, issue 2, pages 234-251. doi:10.1071/CH9550234
8. ↑ Stanislas Sorel (1867): "Sur un nouveau ciment magnesién". Comptes rendus hebdomadaires des séances de l'Académie des sciences, volume 65, pages 102–104.
9. ↑ 9.0 9.1 W. O. Robinson and W. H. Waggaman (1909): "Basic magnesium chlorides". Journal of Physical Chemistry, volume 13, issue 9, pages 673–678. doi:10.1021/j150108a002
10. ↑ 10.0 10.1 J. W. C. Davis (1872): "Composition of Crystalline Deposit from a Solution of Magnesium and Ammonium Chloride". The Chemical News and Journal of Physical Science, volume 25, page 258.
11. ↑ Otto Krause (1873): "Ueber Magnesiumoxychlorid". Annalen der Chemie und Pharmacie, volume 165, pages 38–44.
12. ↑ 12.0 12.1 12.2 G. M. André (1882): "Sur les oxychlorures de magnésium". Comptes rendus hebdomadaires des séances de l'Académie des sciences, volume 94, pages 444–446.
13. ↑ 13.0 13.1 H. S. Lukens (1932): "The composition of magnesium oxychloride". Journal of the American Chemical Society, volume 54, issue 6, pages 2372–2380. doi:10.1021/ja01345a026
14. ↑ 14.0 14.1 Carmen Mažuranić, Halka Bilinski, and Boris Matković (1982): "Reaction Products in the System MgCl2‐NaOH‐H2O". Journal of the American Ceramic Society, volume 65, issue 10, pages 523-526. doi:10.1111/j.1151-2916.1982.tb10346.x
15. ↑ Amal Brichni, Halim Hammi, Salima Aggoun, and M'nif Adel (2016): "Optimization of magnesium oxychloride cement properties by silica glass". Advances in Cement Research (Springer conference proceedings). doi:10.1680/jadcr.16.00024
16. ↑ 16.0 16.1 16.2 16.3 16.4 Isao Kanesaka and Shin Aoyama (2001): "Vibrational spectra of magnesia cement, phase 3". Journal of Raman Spectroscopy, volume 32, issue 5, pages 361-367. doi:10.1002/jrs.706
17. ↑ 17.0 17.1 17.2 17.3 17.4 17.5 17.6 17.7 Deng Dehua and Zhang Chuanmei (1999): "The formation mechanism of the hydrate phases in magnesium oxychloride cement". Cement and Concrete Research, volume 29, issue 9, pages 1365-1371. doi:10.1016/S0008-8846(98)00247-6
18. ↑ B. Tooper and L. Cartz (1966): "Structure and Formation of Magnesium Oxychloride Sorel Cements". Nature, volume 211, pages 64–66. doi:10.1038/211064a0
19. ↑ 19.0 19.1 Halka Bilinski, Boris Matković, Carmen Mažuranić, and Toncci Balić Žunić (1984): "The Formation of Magnesium Oxychloride Phases in the Systems MgO‐MgCl2‐H2O and NaOH‐MgCl2‐H2O". Journal of the American Ceramic Society, volume 67, issue 4, pages 266-269. doi:10.1111/j.1151-2916.1984.tb18844.x

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