Water of crystallization

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Short description: Water molecules present inside crystals

In chemistry, water(s) of crystallization or water(s) of hydration are water molecules that are present inside crystals. Water is often incorporated in the formation of crystals from aqueous solutions.[1] In some contexts, water of crystallization is the total mass of water in a substance at a given temperature and is mostly present in a definite (stoichiometric) ratio. Classically, "water of crystallization" refers to water that is found in the crystalline framework of a metal complex or a salt, which is not directly bonded to the metal cation.

Upon crystallization from water, or water-containing solvents, many compounds incorporate water molecules in their crystalline frameworks. Water of crystallization can generally be removed by heating a sample but the crystalline properties are often lost.

Compared to inorganic salts, proteins crystallize with large amounts of water in the crystal lattice. A water content of 50% is not uncommon for proteins.

Applications

Knowledge of hydration is essential for calculating the masses for many compounds. The reactivity of many salt-like solids is sensitive to the presence of water. The hydration and dehydration of salts is central to the use of phase-change materials for energy storage.[2]

Position in the crystal structure

File:H-bondingFeSO47aq.tif A salt with associated water of crystallization is known as a hydrate. The structure of hydrates can be quite elaborate, because of the existence of hydrogen bonds that define polymeric structures.[3] [4] Historically, the structures of many hydrates were unknown, and the dot in the formula of a hydrate was employed to specify the composition without indicating how the water is bound. Per IUPAC's recommendations, the middle dot is not surrounded by spaces when indicating a chemical adduct.[5] Examples:

  • CuSO
    4
     · 5H2O
    – copper(II) sulfate pentahydrate
  • CoCl
    2
     · 6H2O
    – cobalt(II) chloride hexahydrate
  • SnCl
    2
     · 2H2O
    – tin(II) (or stannous) chloride dihydrate

For many salts, the exact bonding of the water is unimportant because the water molecules are made labile upon dissolution. For example, an aqueous solution prepared from CuSO
4
 · 5H2O
and anhydrous CuSO
4
behave identically. Therefore, knowledge of the degree of hydration is important only for determining the equivalent weight: one mole of CuSO
4
 · 5H2O
weighs more than one mole of CuSO
4
. In some cases, the degree of hydration can be critical to the resulting chemical properties. For example, anhydrous RhCl
3
is not soluble in water and is relatively useless in organometallic chemistry whereas RhCl
3
 · 3H2O
is versatile. Similarly, hydrated AlCl
3
is a poor Lewis acid and thus inactive as a catalyst for Friedel-Crafts reactions. Samples of AlCl
3
must therefore be protected from atmospheric moisture to preclude the formation of hydrates. File:Ca(aq)6 improved image.tif

Crystals of hydrated copper(II) sulfate consist of [Cu(H
2
O)
4
]2+
centers linked to SO2−
4
ions. Copper is surrounded by six oxygen atoms, provided by two different sulfate groups and four molecules of water. A fifth water resides elsewhere in the framework but does not bind directly to copper.[6] The cobalt chloride mentioned above occurs as [Co(H
2
O)
6
]2+
and Cl
. In tin chloride, each Sn(II) center is pyramidal (mean O/Cl–Sn–O/Cl angle is 83°) being bound to two chloride ions and one water. The second water in the formula unit is hydrogen-bonded to the chloride and to the coordinated water molecule. Water of crystallization is stabilized by electrostatic attractions, consequently hydrates are common for salts that contain +2 and +3 cations as well as −2 anions. In some cases, the majority of the weight of a compound arises from water. Glauber's salt, Na
2
SO
4
(H
2
O)
10
, is a white crystalline solid with greater than 50% water by weight.

Consider the case of nickel(II) chloride hexahydrate. This species has the formula NiCl
2
(H
2
O)
6
. Crystallographic analysis reveals that the solid consists of [trans-NiCl
2
(H
2
O)
4
]
subunits that are hydrogen bonded to each other as well as two additional molecules of H
2
O
. Thus one third of the water molecules in the crystal are not directly bonded to Ni2+, and these might be termed "water of crystallization".

Analysis

The water content of most compounds can be determined with a knowledge of its formula. An unknown sample can be determined through thermogravimetric analysis (TGA) where the sample is heated strongly, and the accurate weight of a sample is plotted against the temperature. The amount of water driven off is then divided by the molar mass of water to obtain the number of molecules of water bound to the salt.

Other solvents of crystallization

Water is particularly common solvent to be found in crystals because it is small and polar. But all solvents can be found in some host crystals. Water is noteworthy because it is reactive, whereas other solvents such as benzene are considered to be chemically innocuous. Occasionally more than one solvent is found in a crystal, and often the stoichiometry is variable, reflected in the crystallographic concept of "partial occupancy". It is common and conventional for a chemist to "dry" a sample with a combination of vacuum and heat "to constant weight".

For other solvents of crystallization, analysis is conveniently accomplished by dissolving the sample in a deuterated solvent and analyzing the sample for solvent signals by NMR spectroscopy. Single crystal X-ray crystallography is often able to detect the presence of these solvents of crystallization as well. Other methods may be currently available.

Table of crystallization water in some inorganic halides

In the table below are indicated the number of molecules of water per metal in various salts.[7][8]

Hydrated metal halides
and their formulas
Coordination sphere
of the metal
Equivalents of water of crystallization
that are not bound to M
Remarks
Calcium chloride
CaCl
2
(H
2
O)
6
[Ca(μ-H
2
O)
6
(H
2
O)
3
]2+
none example of water as a bridging ligand[9]
Titanium(III) chloride
TiCl
3
(H
2
O)
6
trans-[TiCl
2
(H
2
O)
4
]+
[10]
two isomorphous with VCl
3
(H
2
O)
6
Titanium(III) chloride
TiCl
3
(H
2
O)
6
[Ti(H
2
O)
6
]
3+[10]
none isomeric with [TiCl
2
(H
2
O)
4
]Cl
.2H2O[11]
Zirconium(IV) fluoride
ZrF
4
(H
2
O)
3
(μ–F)
2
[ZrF
3
(H
2
O)
3
]
2
none rare case where Hf and Zr differ[12]
Hafnium tetrafluoride
HfF
4
(H
2
O)
3
(μ–F)
2
[HfF
2
(H
2
O)
2
]
n(H2O)n
one rare case where Hf and Zr differ[12]
Vanadium(III) chloride
VCl
3
(H
2
O)
6
trans-[VCl
2
(H
2
O)
4
]+
[10]
two
Vanadium(III) bromide
VBr
3
(H
2
O)
6
trans-[VBr
2
(H
2
O)
4
]+
[10]
two
Vanadium(III) iodide
VI
3
(H
2
O)
6
[V(H
2
O)
6
]3+
none relative to Cl
and Br
, I
competes poorly
with water as a ligand for V(III)
Nb
6
Cl
14
(H
2
O)
8
[Nb
6
Cl
14
(H
2
O)
2
]
four
Chromium(III) chloride
CrCl
3
(H
2
O)
6
trans-[CrCl
2
(H
2
O)
4
]+
two dark green isomer, aka "Bjerrums's salt"
Chromium(III) chloride
CrCl
3
(H
2
O)
6
[CrCl(H
2
O)
5
]2+
one blue-green isomer
Chromium(II) chloride
CrCl
2
(H
2
O)
4
trans-[CrCl
2
(H
2
O)
4
]
none square planar/tetragonal distortion
Chromium(III) chloride
CrCl
3
(H
2
O)
6
[Cr(H
2
O)
6
]3+
none violet isomer. isostructural with aluminium compound[13]
Aluminum trichloride
AlCl
3
(H
2
O)
6
[Al(H
2
O)
6
]3+
none isostructural with the Cr(III) compound
Manganese(II) chloride
MnCl
2
(H
2
O)
6
trans-[MnCl
2
(H
2
O)
4
]
two
Manganese(II) chloride
MnCl
2
(H
2
O)
4
cis-[MnCl
2
(H
2
O)
4
]
none cis molecular, the unstable trans isomer has also been detected[14]
Manganese(II) bromide
MnBr
2
(H
2
O)
4
cis-[MnBr
2
(H
2
O)
4
]
none cis, molecular
Manganese(II) iodide
MnI
2
(H
2
O)
4
trans-[MnI
2
(H
2
O)
4
]
none molecular, isostructural with FeCl2(H2O)4.[15]
Manganese(II) chloride
MnCl
2
(H
2
O)
2
trans-[MnCl
4
(H
2
O)
2
]
none polymeric with bridging chloride
Manganese(II) bromide
MnBr
2
(H
2
O)
2
trans-[MnBr
4
(H
2
O)
2
]
none polymeric with bridging bromide
Iron(II) chloride
FeCl
2
(H
2
O)
6
trans-[FeCl
2
(H
2
O)
4
]
two
Iron(II) chloride
FeCl
2
(H
2
O)
4
trans-[FeCl
2
(H
2
O)
4
]
none molecular
Iron(II) bromide
FeBr
2
(H
2
O)
4
trans-[FeBr
2
(H
2
O)
4
]
none molecular,[16] hydrates of FeI2 are not known
Iron(II) chloride
FeCl
2
(H
2
O)
2
trans-[FeCl
4
(H
2
O)
2
]
none polymeric with bridging chloride
Iron(III) chloride
FeCl
3
(H
2
O)
6
trans-[FeCl
2
(H
2
O)
4
]+
two one of four hydrates of ferric chloride,[17] isostructural with Cr analogue
Iron(III) chloride
FeCl
3
(H
2
O)
2.5
cis-[FeCl
2
(H
2
O)
4
]+
two the dihydrate has a similar structure, both contain FeCl
4
anions.[17]
Cobalt(II) chloride
CoCl
2
(H
2
O)
6
trans-[CoCl
2
(H
2
O)
4
]
two
Cobalt(II) bromide
CoBr
2
(H
2
O)
6
trans-[CoBr
2
(H
2
O)
4
]
two
Cobalt(II) iodide
CoI
2
(H
2
O)
6
[Co(H
2
O)
6
]2+
none[18] iodide competes poorly with water
Cobalt(II) bromide
CoBr
2
(H
2
O)
4
trans-[CoBr
2
(H
2
O)
4
]
none molecular[16]
Cobalt(II) chloride
CoCl
2
(H
2
O)
4
cis-[CoCl
2
(H
2
O)
4
]
none note: cis molecular
Cobalt(II) chloride
CoCl
2
(H
2
O)
2
trans-[CoCl
4
(H
2
O)
2
]
none polymeric with bridging chloride
Cobalt(II) chloride
CoBr
2
(H
2
O)
2
trans-[CoBr
4
(H
2
O)
2
]
none polymeric with bridging bromide
Nickel(II) chloride
NiCl
2
(H
2
O)
6
trans-[NiCl
2
(H
2
O)
4
]
two
Nickel(II) chloride
NiCl
2
(H
2
O)
4
cis-[NiCl
2
(H
2
O)
4
]
none note: cis molecular[16]
Nickel(II) bromide
NiBr
2
(H
2
O)
6
trans-[NiBr
2
(H
2
O)
4
]
two
Nickel(II) iodide
NiI
2
(H
2
O)
6
[Ni(H
2
O)
6
]2+
none[18] iodide competes poorly with water
Nickel(II) chloride
NiCl
2
(H
2
O)
2
trans-[NiCl
4
(H
2
O)
2
]
none polymeric with bridging chloride
Platinum(IV) chloride
[Pt(H
2
O)
2
Cl
4
](H
2
O)
3
[19]
trans-[PtCl
4
(H
2
O)
2
]
3 octahedral Pt centers; rare example of non-first row chloride-aquo complex
Platinum(IV) chloride
[Pt(H
2
O)
3
Cl
3
]Cl(H
2
O)
0.5
[20]
fac-[PtCl
3
(H
2
O)
3
]+
0.5 octahedral Pt centers; rare example of non-first row chloride-aquo complex
Copper(II) chloride
CuCl
2
(H
2
O)
2
[CuCl
4
(H
2
O)
2
]
2
none tetragonally distorted
two long Cu-Cl distances
Copper(II) bromide
CuBr
2
(H
2
O)
4
[CuBr
4
(H
2
O)
2
]
n
two tetragonally distorted
two long Cu-Br distances[16]
Zinc(II) chloride
ZnCl
2
(H
2
O)
1.33
[21]
2 ZnCl
2
+ ZnCl
2
(H
2
O)
4
none coordination polymer with both tetrahedral and octahedral Zn centers
Zinc(II) chloride
ZnCl
2
(H
2
O)
2.5
[22]
Cl
3
Zn(μ-Cl)Zn(H
2
O)
5
none tetrahedral and octahedral Zn centers
Zinc(II) chloride
ZnCl
2
(H
2
O)
3
[21]
[ZnCl
4
]2− + Zn(H
2
O)
6
]2+
none tetrahedral and octahedral Zn centers
Zinc(II) chloride
ZnCl
2
(H
2
O)
4.5
[21]
[ZnCl
4
]2− + [Zn(H
2
O)
6
]2+
three tetrahedral and octahedral Zn centers

Hydrates of metal sulfates

Substructure of MSO4(H2O), illustrating presence of bridging water and bridging sulfate (M = Mg, Mn, Fe, Co, Ni, Zn).

Transition metal sulfates form a variety of hydrates, each of which crystallizes in only one form. The sulfate group often binds to the metal, especially for those salts with fewer than six aquo ligands. The heptahydrates, which are often the most common salts, crystallize as monoclinic and the less common orthorhombic forms. In the heptahydrates, one water is in the lattice and the other six are coordinated to the ferrous center.[23] Many of the metal sulfates occur in nature, being the result of weathering of mineral sulfides.[24][25] Many monohydrates are known.[26]

Formula of
hydrated metal ion sulfate
Coordination
sphere of the metal ion
Equivalents of water of crystallization
that are not bound to M
mineral name Remarks
MgSO4(H2O) [Mn(μ-H2O)(μ4,-κ1-SO4)4][26] none kieserite see Mn, Fe, Co, Ni, Zn analogues
MgSO4(H2O)4 [Mg(H2O)4(κ′,κ1-SO4)]2 none sulfate is bridging ligand, 8-membered Mg2O4S2 rings[27]
MgSO4(H2O)6 [Mg(H2O)6] none hexahydrate common motif[24]
MgSO4(H2O)7 [Mg(H2O)6] one epsomite common motif[24]
TiOSO4(H2O) [Ti(μ-O)2(H2O)(κ1-SO4)3] none further hydration gives gels
VSO4(H2O)6 [V(H2O)6] none Adopts the hexahydrite motif[28]
VOSO4(H2O)5 [VO(H2O)41-SO4)4] one
Cr(SO4)(H2O)3 [Cr(H2O)31-SO4)] none resembles Cu(SO4)(H2O)3[29]
Cr(SO4)(H2O)5 [CR(H2O)41-SO4)2] one resembles Cu(SO4)(H2O)5[30]
Cr2(SO4)3(H2O)18 [Cr(H2O)6] six One of several chromium(III) sulfates
MnSO4(H2O) [Mn(μ-H2O)(μ4,-κ1-SO4)4][26] none szmikite see Fe, Co, Ni, Zn analogues
MnSO4(H2O)4 [Mn(μ-SO4)2(H2O)4][31] none Ilesitepentahydrate is called jôkokuite; the hexahydrate, the most rare, is called chvaleticeite with 8-membered ring Mn2(SO4)2 core
MnSO4(H2O)5 ? jôkokuite
MnSO4(H2O)6 ? Chvaleticeite
MnSO4(H2O)7 [Mn(H2O)6] one mallardite[25] see Mg analogue
FeSO4(H2O) [Fe(μ-H2O)(μ41-SO4)4][26] none see Mn, Co, Ni, Zn analogues
FeSO4(H2O)7 [Fe(H2O)6] one melanterite[25] see Mg analogue
FeSO4(H2O)4 [Fe(H2O)4(κ′,κ1-SO4)]2 none sulfate is bridging ligand, 8-membered Fe2O4S2 rings[27]
FeII(FeIII)2(SO4)4(H2O)14 [FeII(H2O)6]2+[FeIII(H2O)41-SO4)2]2 none sulfates are terminal ligands on Fe(III)[32]
CoSO4(H2O) [Co(μ-H2O)(μ41-SO4)4][26] none see Mn, Fe, Ni, Zn analogues
CoSO4(H2O)6 [Co(H2O)6] none moorhouseite see Mg analogue
CoSO4(H2O)7 [Co(H2O)6] one bieberite[25] see Fe, Mg analogues
NiSO4(H2O) [Ni(μ-H2O)(μ41-SO4)4][26] none see Mn, Fe, Co, Zn analogues
NiSO4(H2O)6 [Ni(H2O)6] none retgersite One of several nickel sulfate hydrates[33]
NiSO4(H2O)7 [Ni(H2O)6] morenosite[25]
(NH4)2[Pt2(SO4)4(H2O)2] [Pt2(SO4)4(H2O)2]2- none Pt-Pt bonded Chinese lantern structure[34]
CuSO4(H2O)5 [Cu(H2O)41-SO4)2] one chalcantite sulfate is bridging ligand[35]
CuSO4(H2O)7 [Cu(H2O)6] one boothite[25]
ZnSO4(H2O) [Zn(μ-H2O)(μ41-SO4)4][26] none see Mn, Fe, Co, Ni analogues
ZnSO4(H2O)4 [Zn(H2O)4(κ′,κ1-SO4)]2 none sulfate is bridging ligand, 8-membered Zn2O4S2 rings[27][36]
ZnSO4(H2O)6 [Zn(H2O)6] none see Mg analogue[37]
ZnSO4(H2O)7 [Zn(H2O)6] one goslarite[25] see Mg analogue
CdSO4(H2O) [Cd(μ-H2O)21-SO4)4] none bridging water ligand[38]

Hydrates of metal nitrates

Transition metal nitrates form a variety of hydrates. The nitrate anion often binds to the metal, especially for those salts with fewer than six aquo ligands. Nitrates are uncommon in nature, so few minerals are represented here. Hydrated ferrous nitrate has not been characterized crystallographically.

Formula of
hydrated metal ion nitrate
Coordination
sphere of the metal ion
Equivalents of water of crystallization
that are not bound to M
Remarks
Cr(NO3)3(H2O)9 [Cr(H2O)6]3+ three octahedral configuration[39] isostructural with Fe(NO3)3(H2O)9
Mn(NO3)2(H2O)4 cis-[Mn(H2O)41-ONO2)2] none octahedral configuration
Mn(NO3)2(H2O) [Mn(H2O)(μ-ONO2)5] none octahedral configuration
Mn(NO3)2(H2O)6 [Mn(H2O)6] none octahedral configuration[40]
Fe(NO3)3(H2O)9 [Fe(H2O)6]3+ three octahedral configuration[41] isostructural with Cr(NO3)3(H2O)9
Fe(NO3)3)(H2O)4 [Fe(H2O)32-O2NO)2]+ one pentagonal bipyramid[42]
Fe(NO3)3(H2O)5 [Fe(H2O)51-ONO2)]2+ none octahedral configuration[42]
Fe(NO3)3(H2O)6 [Fe(H2O)6]3+ none octahedral configuration[42]
Co(NO3)2(H2O)2 [Co(H2O)21-ONO2)2] none octahedral configuration
Co(NO3)2(H2O)4 [Co(H2O)41-ONO2)2 none octahedral configuration
Co(NO3)2(H2O)6 [Co(H2O)6]2+ none octahedral configuration.[43]
α-Ni(NO3)2(H2O)4 cis-[Ni(H2O)41-ONO2)2] none octahedral configuration.[44]
β-Ni(NO3)2(H2O)4 trans-[Ni(H2O)41-ONO2)2] none octahedral configuration.[45]
Pd(NO3)2(H2O)2 trans-[Pd(H2O)21-ONO2)2] none square planar coordination geometry[46]
Cu(NO3)2(H2O) [Cu(H2O)(κ2-ONO2)2] none octahedral configuration.
Cu(NO3)2(H2O)1.5 uncertain uncertain uncertain[47]
Cu(NO3)2(H2O)2.5 [Cu(H2O)21-ONO2)2] one square planar[48]
Cu(NO3)2(H2O)3 uncertain uncertain uncertain [49]
Cu(NO3)2(H2O)6 [Cu(H2O)6]2+ none octahedral configuration[50]
Zn(NO3)2(H2O)4 cis-[Zn(H2O)41-ONO2)2] none octahedral configuration.

Photos

See also

References

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