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], ], Norway. Size: 8.4 x 5.2 x 4.1 cm.]] | ], ], Norway. Size: 8.4 x 5.2 x 4.1 cm.]] | ||
'''Layered double hydroxides''' ('''LDH''') comprise an unusual class of layered materials with positively charged layers and weakly bound, often ], charge-balancing anions located in the interlayer region. This is unusual in solid state chemistry: many more materials have negatively charged layers and cations in the interlayer spaces. Examples include ] silicates such as ]. | '''Layered double hydroxides''' ('''LDH''') comprise an unusual class of layered materials with positively charged layers and weakly bound, often ], charge-balancing anions located in the interlayer region. This is unusual in solid state chemistry: many more materials have negatively charged layers and cations in the interlayer spaces.<ref>Evans, David G.; Slade, Robert C. T. "Structural aspects of layered double hydroxides" Structure and Bonding 2006, vol. 119, 1-87. </ref> Examples include ] silicates such as ]. LDH's are of interest for their ] properties.<ref>Khan, Aamir I.; O'Hare, Dermot "Intercalation chemistry of layered double hydroxides: recent developments and applications" Journal of Materials Chemistry (2002), 12(11), 3191-3198. {{DOI| 10.1039/b204076j}}</ref> | ||
LDHs are commonly represented by the formula <sup>q+</sup>(X<sup>n-</sup>)<sub>q/n</sub>·''y''H<sub>2</sub>O. | LDHs are commonly represented by the formula <sup>q+</sup>(X<sup>n-</sup>)<sub>q/n</sub>·''y''H<sub>2</sub>O. | ||
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LDHs may be formed with a wide variety of anions X (e.g. Cl<sup>-</sup>, Br<sup>-</sup>, NO<sub>3</sub><sup>-</sup>, CO<sub>3</sub><sup>2-</sup>, SO<sub>4</sub><sup>2-</sup> and SeO<sub>4</sub><sup>2-</sup>). | LDHs may be formed with a wide variety of anions X (e.g. Cl<sup>-</sup>, Br<sup>-</sup>, NO<sub>3</sub><sup>-</sup>, CO<sub>3</sub><sup>2-</sup>, SO<sub>4</sub><sup>2-</sup> and SeO<sub>4</sub><sup>2-</sup>). | ||
==Applications== | |||
The anions located in the ] regions can be replaced easily, in general. A wide variety of anions may be incorporated, ranging from simple inorganic anions (e.g. CO<sub>3</sub><sup>2-</sup>) through organic anions (e.g. benzoate, succinate) to complex biomolecules, including DNA. This has led to an intense interest in the use of LDH ] for advanced applications. Drug molecules such as ] may be intercalated; the resulting ]s have potential for use in controlled release systems, which could reduce the frequency of doses of medication needed to treat a disorder. Further effort has been expended on the intercalation of agrochemicals, such as the chlorophenoxyacetates, and important organic ]s, such as terephthalate and nitrophenols. Agrochemical intercalates are of interest because of the potential to use LDHs to remove agrochemicals from polluted water, reducing the likelihood of ]. | The anions located in the ] regions can be replaced easily, in general. A wide variety of anions may be incorporated, ranging from simple inorganic anions (e.g. CO<sub>3</sub><sup>2-</sup>) through organic anions (e.g. benzoate, succinate) to complex biomolecules, including DNA. This has led to an intense interest in the use of LDH ] for advanced applications. Drug molecules such as ] may be intercalated; the resulting ]s have potential for use in controlled release systems, which could reduce the frequency of doses of medication needed to treat a disorder. Further effort has been expended on the intercalation of agrochemicals, such as the chlorophenoxyacetates, and important organic ]s, such as terephthalate and nitrophenols. Agrochemical intercalates are of interest because of the potential to use LDHs to remove agrochemicals from polluted water, reducing the likelihood of ]. | ||
LDHs |
LDHs exhibit shape-selective intercalation properties. For instance, treating LiAl<sub>2</sub>-Cl with a 50:50 mixture of terephthalate (1,4-benzenedicarboxylate) and phthalate (1,2-benzenedicarboxylate) results in intercalation of the 1,4-isomer with almost 100% preference. The selective intercalation of ions such as benzenedicarboxylates and ]s has importance because these are produced in isomeric mixtures from crude oil residues, and it is often desirable to isolate a single form, for instance in the production of polymers. | ||
Naturally occurring (i.e., mineralogical) examples of LDH are classified as members of the Hydrotalcite Supergroup, named after the Mg-Al carbonate ], which is the longest-known example of a natural LDH phase. More than 40 mineral species are known to fall within this supergroup.<ref name=Report/> The dominant divalent cations, M<sup>2+</sup>, that have been reported in hydrotalcite supergroup minerals are | Naturally occurring (i.e., mineralogical) examples of LDH are classified as members of the Hydrotalcite Supergroup, named after the Mg-Al carbonate ], which is the longest-known example of a natural LDH phase. More than 40 mineral species are known to fall within this supergroup.<ref name=Report/> The dominant divalent cations, M<sup>2+</sup>, that have been reported in hydrotalcite supergroup minerals are | ||
Mg, Ca, Mn, Fe, Ni, Cu and Zn; the dominant trivalent cations, M<sup>3+</sup>, are Al, Mn, Fe, Co and Ni. The | Mg, Ca, Mn, Fe, Ni, Cu and Zn; the dominant trivalent cations, M<sup>3+</sup>, are Al, Mn, Fe, Co and Ni. The | ||
most common intercalated anions are <sup>2-</sup>, <sup>2-</sup> and Cl<sup>-</sup>; OH<sup>-</sup>, S<sup>2-</sup> and <sup>-</sup> have also been reported. Some species contain intercalated cationic or neutral complexes such as <sup>+</sup> or <sup>0</sup>. The International Mineralogical Association's 2012 report on hydrotalcite supergroup nomenclature defines eight groups within the supergroup on the basis of a combination of criteria. These groups are: | most common intercalated anions are <sup>2-</sup>, <sup>2-</sup> and Cl<sup>-</sup>; OH<sup>-</sup>, S<sup>2-</sup> and <sup>-</sup> have also been reported. Some species contain intercalated cationic or neutral complexes such as <sup>+</sup> or <sup>0</sup>. The International Mineralogical Association's 2012 report on hydrotalcite supergroup nomenclature defines eight groups within the supergroup on the basis of a combination of criteria. These groups are: | ||
# the ], with M<sup>2+</sup>:M<sup>3+</sup> = 3:1 (layer spacing ~7.8 Å); | # the ] group, with M<sup>2+</sup>:M<sup>3+</sup> = 3:1 (layer spacing ~7.8 Å); | ||
# the ], with M<sup>2+</sup>:M<sup>3+</sup> = 2:1 (layer spacing ~7.8 Å); | # the ] group, with M<sup>2+</sup>:M<sup>3+</sup> = 2:1 (layer spacing ~7.8 Å); | ||
# the ] of natural ']' phases, with M<sup>2+</sup> = Fe<sup>2+</sup>, M<sup>3+</sup> = Fe<sup>3+</sup> in a range of ratios, and with O<sup>2-</sup> replacing OH<sup>-</sup> in the brucite module to maintain charge balance (layer spacing ~7.8 Å); | # the ] group of natural ']' phases, with M<sup>2+</sup> = Fe<sup>2+</sup>, M<sup>3+</sup> = Fe<sup>3+</sup> in a range of ratios, and with O<sup>2-</sup> replacing OH<sup>-</sup> in the brucite module to maintain charge balance (layer spacing ~7.8 Å); | ||
# the ], with variable M<sup>2+</sup>:M<sup>3+</sup> and interlayer <sup>2-</sup>, leading to an expanded layer spacing of ~8.9 Å; | # the ] group, with variable M<sup>2+</sup>:M<sup>3+</sup> and interlayer <sup>2-</sup>, leading to an expanded layer spacing of ~8.9 Å; | ||
# the ], with interlayer <sup>-</sup> and a layer spacing of ~9.7 Å; | # the ] group, with interlayer <sup>-</sup> and a layer spacing of ~9.7 Å; | ||
# the ], with interlayer <sup>2-</sup> as in the woodwardite group, and with additional interlayer H<sub>2</sub>O molecules that further expand the layer spacing to ~11 Å; | # the ] group, with interlayer <sup>2-</sup> as in the woodwardite group, and with additional interlayer H<sub>2</sub>O molecules that further expand the layer spacing to ~11 Å; | ||
# the ], with a layer spacing of ~11 Å, in which cationic complexes occur with anions between the brucite-like layers; and | # the ] group, with a layer spacing of ~11 Å, in which cationic complexes occur with anions between the brucite-like layers; and | ||
# the ], with M<sup>2+</sup> = Ca<sup>2+</sup> and M<sup>3+</sup> = Al, which contains brucite-like layers in which the Ca:Al ratio is 2:1 and the large cation, Ca<sup>2+</sup>, is coordinated to a seventh ligand of ‘interlayer’ water. | # the ] group, with M<sup>2+</sup> = Ca<sup>2+</sup> and M<sup>3+</sup> = Al, which contains brucite-like layers in which the Ca:Al ratio is 2:1 and the large cation, Ca<sup>2+</sup>, is coordinated to a seventh ligand of ‘interlayer’ water. | ||
The IMA Report <ref name=Report/> also presents a concise systematic nomenclature for synthetic LDH phases that are not eligible for a mineral name. This uses the prefix LDH, and characterises components by the numbers of the octahedral cation species in the chemical formula, the interlayer anion, and the Ramsdell ] symbol (number of layers in the repeat of the structure, and crystal system). For example, the 3''R'' polytype of Mg<sub>6</sub>Al<sub>2</sub>(OH)<sub>12</sub>(CO<sub>3</sub>).4H<sub>2</sub>O (] ''sensu stricto'') is described by "LDH 6Mg2Al·CO3-3''R''". This simplified nomenclature does not capture all the possible types of structural complexity in LDH materials. Elsewhere, the Report discusses examples of: | The IMA Report <ref name=Report/> also presents a concise systematic nomenclature for synthetic LDH phases that are not eligible for a mineral name. This uses the prefix LDH, and characterises components by the numbers of the octahedral cation species in the chemical formula, the interlayer anion, and the Ramsdell ] symbol (number of layers in the repeat of the structure, and crystal system). For example, the 3''R'' polytype of Mg<sub>6</sub>Al<sub>2</sub>(OH)<sub>12</sub>(CO<sub>3</sub>).4H<sub>2</sub>O (] ''sensu stricto'') is described by "LDH 6Mg2Al·CO3-3''R''". This simplified nomenclature does not capture all the possible types of structural complexity in LDH materials. Elsewhere, the Report discusses examples of: | ||
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# the wide variety of ''c'' periodicities that can occur due to relative displacements or rotations of the brucite-like layers, producing multiple ]s with the same compositions, intergrowths of polytypes and variable degrees of stacking disorder; | # the wide variety of ''c'' periodicities that can occur due to relative displacements or rotations of the brucite-like layers, producing multiple ]s with the same compositions, intergrowths of polytypes and variable degrees of stacking disorder; | ||
# different periodicities arising from order of different interlayer species, either within an interlayer or by alternation of different anion types from interlayer to interlayer. | # different periodicities arising from order of different interlayer species, either within an interlayer or by alternation of different anion types from interlayer to interlayer. | ||
==See also== | |||
* ], an iron-bearing LDH mineral that is an example of a ']' phase. | |||
* ], a LDH mineral. | |||
==Citations== | ==Citations== | ||
<references /> | |||
{{reflist|refs= | |||
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== |
==Other references== | ||
* | * | ||
* | |||
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{{Commons category|Hydrotalcite}} | {{Commons category|Hydrotalcite}} | ||
Revision as of 07:09, 23 July 2014
Layered double hydroxides (LDH) comprise an unusual class of layered materials with positively charged layers and weakly bound, often exchangeable, charge-balancing anions located in the interlayer region. This is unusual in solid state chemistry: many more materials have negatively charged layers and cations in the interlayer spaces. Examples include clay mineral silicates such as kaolinite. LDH's are of interest for their intercalation properties.
LDHs are commonly represented by the formula (X)q/n·yH2O.
Most commonly, z = 2, and M = Ca, Mg, Mn, Fe, Co, Ni, Cu or Zn; hence q = x. Fixed-composition phases have been shown to exist over the range 0.2 ≤ x ≤ 0.33. However, phases with variable x hare also known, and in some cases, x > 0.5.
Examples are also known with z = 1, where M = Li and M = Al. In this case, q = 2x - 1. The latter family of materials can be described by the formula X∙yH2O (LiAl2-X)). X represents a generic anion and the value of y is normally found to be between 0.5 – 4.
LDHs may be formed with a wide variety of anions X (e.g. Cl, Br, NO3, CO3, SO4 and SeO4).
Applications
The anions located in the interlayer regions can be replaced easily, in general. A wide variety of anions may be incorporated, ranging from simple inorganic anions (e.g. CO3) through organic anions (e.g. benzoate, succinate) to complex biomolecules, including DNA. This has led to an intense interest in the use of LDH intercalates for advanced applications. Drug molecules such as ibuprofen may be intercalated; the resulting nanocomposites have potential for use in controlled release systems, which could reduce the frequency of doses of medication needed to treat a disorder. Further effort has been expended on the intercalation of agrochemicals, such as the chlorophenoxyacetates, and important organic synthons, such as terephthalate and nitrophenols. Agrochemical intercalates are of interest because of the potential to use LDHs to remove agrochemicals from polluted water, reducing the likelihood of eutrophication.
LDHs exhibit shape-selective intercalation properties. For instance, treating LiAl2-Cl with a 50:50 mixture of terephthalate (1,4-benzenedicarboxylate) and phthalate (1,2-benzenedicarboxylate) results in intercalation of the 1,4-isomer with almost 100% preference. The selective intercalation of ions such as benzenedicarboxylates and nitrophenols has importance because these are produced in isomeric mixtures from crude oil residues, and it is often desirable to isolate a single form, for instance in the production of polymers.
Naturally occurring (i.e., mineralogical) examples of LDH are classified as members of the Hydrotalcite Supergroup, named after the Mg-Al carbonate hydrotalcite, which is the longest-known example of a natural LDH phase. More than 40 mineral species are known to fall within this supergroup. The dominant divalent cations, M, that have been reported in hydrotalcite supergroup minerals are Mg, Ca, Mn, Fe, Ni, Cu and Zn; the dominant trivalent cations, M, are Al, Mn, Fe, Co and Ni. The most common intercalated anions are , and Cl; OH, S and have also been reported. Some species contain intercalated cationic or neutral complexes such as or . The International Mineralogical Association's 2012 report on hydrotalcite supergroup nomenclature defines eight groups within the supergroup on the basis of a combination of criteria. These groups are:
- the hydrotalcite group, with M:M = 3:1 (layer spacing ~7.8 Å);
- the quintinite group, with M:M = 2:1 (layer spacing ~7.8 Å);
- the fougèrite group of natural 'green rust' phases, with M = Fe, M = Fe in a range of ratios, and with O replacing OH in the brucite module to maintain charge balance (layer spacing ~7.8 Å);
- the woodwardite group, with variable M:M and interlayer , leading to an expanded layer spacing of ~8.9 Å;
- the cualstibite group, with interlayer and a layer spacing of ~9.7 Å;
- the glaucocerinite group, with interlayer as in the woodwardite group, and with additional interlayer H2O molecules that further expand the layer spacing to ~11 Å;
- the wermlandite group, with a layer spacing of ~11 Å, in which cationic complexes occur with anions between the brucite-like layers; and
- the hydrocalumite group, with M = Ca and M = Al, which contains brucite-like layers in which the Ca:Al ratio is 2:1 and the large cation, Ca, is coordinated to a seventh ligand of ‘interlayer’ water.
The IMA Report also presents a concise systematic nomenclature for synthetic LDH phases that are not eligible for a mineral name. This uses the prefix LDH, and characterises components by the numbers of the octahedral cation species in the chemical formula, the interlayer anion, and the Ramsdell polytype symbol (number of layers in the repeat of the structure, and crystal system). For example, the 3R polytype of Mg6Al2(OH)12(CO3).4H2O (hydrotalcite sensu stricto) is described by "LDH 6Mg2Al·CO3-3R". This simplified nomenclature does not capture all the possible types of structural complexity in LDH materials. Elsewhere, the Report discusses examples of:
- long-range order of different cations within a brucite-like layer, which may produce sharp superstructure peaks in diffraction patterns and a and b periodicities that are multiples of the basic 3 Å repeat, or short-range order producing diffuse scattering;
- the wide variety of c periodicities that can occur due to relative displacements or rotations of the brucite-like layers, producing multiple polytypes with the same compositions, intergrowths of polytypes and variable degrees of stacking disorder;
- different periodicities arising from order of different interlayer species, either within an interlayer or by alternation of different anion types from interlayer to interlayer.
Citations
- Evans, David G.; Slade, Robert C. T. "Structural aspects of layered double hydroxides" Structure and Bonding 2006, vol. 119, 1-87.
- Khan, Aamir I.; O'Hare, Dermot "Intercalation chemistry of layered double hydroxides: recent developments and applications" Journal of Materials Chemistry (2002), 12(11), 3191-3198. doi:10.1039/b204076j
- ^ Cite error: The named reference
Report
was invoked but never defined (see the help page).
Other references
- LDH, DNA and Hydrothermal Vents - Science Daily
- Mindat entry for Hydrotalcite Supergroup
- IMA Nomenclature Report
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