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Salt (chemistry)
Salt (chemistry)
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The crystal structure of sodium chloride, NaCl, a typical salt. The purple spheres represent sodium cations, Na+, and the green spheres represent chloride anions, Cl. The yellow stipples show the electrostatic forces.

In chemistry, a salt or ionic compound is a chemical compound consisting of an assembly of positively charged ions (cations) and negatively charged ions (anions),[1] which results in a compound with no net electric charge (electrically neutral). The constituent ions are held together by electrostatic forces termed ionic bonds.

The component ions in a salt can be either inorganic, such as chloride (Cl), or organic, such as acetate (CH
3
COO
). Each ion can be either monatomic, such as sodium (Na+) and chloride (Cl) in sodium chloride, or polyatomic, such as ammonium (NH+
4
) and carbonate (CO2−
3
) ions in ammonium carbonate. Salts containing basic ions hydroxide (OH) or oxide (O2−) are classified as bases, such as sodium hydroxide and potassium oxide.

Individual ions within a salt usually have multiple near neighbours, so they are not considered to be part of molecules, but instead part of a continuous three-dimensional network. Salts usually form crystalline structures when solid.

Salts composed of small ions typically have high melting and boiling points, and are hard and brittle. As solids they are almost always electrically insulating, but when melted or dissolved they become highly conductive, because the ions become mobile. Some salts have large cations, large anions, or both. In terms of their properties, such species often are more similar to organic compounds.

History of discovery

[edit]
X-ray spectrometer developed by W. H. Bragg

In 1913 the structure of sodium chloride was determined by William Henry Bragg and his son William Lawrence Bragg.[2][3][4] This revealed that there were six equidistant nearest neighbours for each atom, demonstrating that the constituents were not arranged in molecules or finite aggregates, but instead as a network with long-range crystalline order.[4] Many other inorganic compounds were also found to have similar structural features.[4] These compounds were soon described as being constituted of ions rather than neutral atoms, but proof of this hypothesis was not found until the mid-1920s, when X-ray reflection experiments (which detect the density of electrons), were performed.[4][5]

Principal contributors to the development of a theoretical treatment of ionic crystal structures were Max Born, Fritz Haber, Alfred Landé, Erwin Madelung, Paul Peter Ewald, and Kazimierz Fajans.[6] Born predicted crystal energies based on the assumption of ionic constituents, which showed good correspondence to thermochemical measurements, further supporting the assumption.[4]

Formation

[edit]
White crystals form a mineral sample of halite, shown against a black background.
Halite, the mineral form of sodium chloride, forms when salty water evaporates leaving the ions behind.
Solid lead(II) sulfate (PbSO4)

Many metals such as the alkali metals react directly with the electronegative halogens gases to form salts.[7][8]

Solid salts can form upon evaporation of solvent from their solutions once the solution is supersaturated and the solid compound nucleates.[9] This process occurs widely in nature and is the means of formation of the evaporite minerals.[10]

Insoluble salts can be precipitated by mixing two solutions, one containing the cation and one containing the anion. Because all solutions are electrically neutral, the two solutions mixed must also contain counterions of the opposite charges. To ensure that these do not contaminate the precipitated salt, it is important to ensure they do not also precipitate.[11] If the two solutions have hydrogen ions and hydroxide ions as the counterions, they will react with one another in what is called an acid–base reaction or a neutralization reaction to form water.[12] Alternately the counterions can be chosen to ensure that even when combined into a single solution they will remain soluble as spectator ions.[11]

If the solvent is water in either the evaporation or precipitation method of formation, in many cases the ionic crystal formed also includes water of crystallization, so the product is known as a hydrate, and can have very different chemical properties compared to the anhydrous material.[13]

Molten salts will solidify on cooling to below their freezing point.[14] This is sometimes used for the solid-state synthesis of complex salts from solid reactants, which are first melted together.[15] In other cases, the solid reactants do not need to be melted, but instead can react through a solid-state reaction route. In this method, the reactants are repeatedly finely ground into a paste and then heated to a temperature where the ions in neighboring reactants can diffuse together during the time the reactant mixture remains in the oven.[8] Other synthetic routes use a solid precursor with the correct stoichiometric ratio of non-volatile ions, which is heated to drive off other species.[8]

In some reactions between highly reactive metals (usually from Group 1 or Group 2) and highly electronegative halogen gases, or water, the atoms can be ionized by electron transfer,[16] a process thermodynamically understood using the Born–Haber cycle.[17]

Salts can be formed through a variety of reaction types, such as those between:

Bonding

[edit]
A schematic electron shell diagram of sodium and fluorine atoms undergoing a redox reaction to form sodium fluoride. Sodium loses its outer electron to give it a stable electron configuration, and this electron enters the fluorine atom exothermically. The oppositely charged ions – typically a great many of them – are then attracted to each other to form a solid.

Ions in salts are primarily held together by the electrostatic forces between the charge distribution of these bodies, and in particular, the ionic bond resulting from the long-ranged Coulomb attraction between the net negative charge of the anions and net positive charge of the cations.[18] There is also a small additional attractive force from van der Waals interactions which contributes only around 1–2% of the cohesive energy for small ions.[19] When a pair of ions comes close enough for their outer electron shells (most simple ions have closed shells) to overlap, a short-ranged repulsive force occurs,[20] due to the Pauli exclusion principle.[21] The balance between these forces leads to a potential energy well with minimum energy when the nuclei are separated by a specific equilibrium distance.[20]

If the electronic structure of the two interacting bodies is affected by the presence of one another, covalent interactions (non-ionic) also contribute to the overall energy of the compound formed.[22] Salts are rarely purely ionic, i.e. held together only by electrostatic forces. The bonds between even the most electronegative/electropositive pairs such as those in caesium fluoride exhibit a small degree of covalency.[23][24] Conversely, covalent bonds between unlike atoms often exhibit some charge separation and can be considered to have a partial ionic character.[22] The circumstances under which a compound will have ionic or covalent character can typically be understood using Fajans' rules, which use only charges and the sizes of each ion. According to these rules, compounds with the most ionic character will have large positive ions with a low charge, bonded to a small negative ion with a high charge.[25] More generally HSAB theory can be applied, whereby the compounds with the most ionic character are those consisting of hard acids and hard bases: small, highly charged ions with a high difference in electronegativities between the anion and cation.[26][27] This difference in electronegativities means that the charge separation, and resulting dipole moment, is maintained even when the ions are in contact (the excess electrons on the anions are not transferred or polarized to neutralize the cations).[28]

Although chemists classify idealized bond types as being ionic or covalent, the existence of additional types such as hydrogen bonds and metallic bonds, for example, has led some philosophers of science to suggest that alternative approaches to understanding bonding are required. This could be by applying quantum mechanics to calculate binding energies.[29][30]

Structure

[edit]
The unit cell of the zinc blende structure

The lattice energy is the summation of the interaction of all sites with all other sites. For unpolarizable spherical ions, only the charges and distances are required to determine the electrostatic interaction energy. For any particular ideal crystal structure, all distances are geometrically related to the smallest internuclear distance. So for each possible crystal structure, the total electrostatic energy can be related to the electrostatic energy of unit charges at the nearest neighboring distance by a multiplicative constant called the Madelung constant[20] that can be efficiently computed using an Ewald sum.[31] When a reasonable form is assumed for the additional repulsive energy, the total lattice energy can be modelled using the Born–Landé equation,[32] the Born–Mayer equation, or in the absence of structural information, the Kapustinskii equation.[33]

Using an even simpler approximation of the ions as impenetrable hard spheres, the arrangement of anions in these systems are often related to close-packed arrangements of spheres, with the cations occupying tetrahedral or octahedral interstices.[34][35] Depending on the stoichiometry of the salt, and the coordination (principally determined by the radius ratio) of cations and anions, a variety of structures are commonly observed,[36] and theoretically rationalized by Pauling's rules.[37]

Common ionic compound structures with close-packed anions[36]
Stoichiometry Cation:anion
coordination
Interstitial sites Cubic close packing of anions Hexagonal close packing of anions
Occupancy Critical radius
ratio
Name Madelung constant Name Madelung constant
MX 6:6 all octahedral 0.4142[34] sodium chloride 1.747565[38] nickeline <1.73[a][39]
4:4 alternate tetrahedral 0.2247[40] zinc blende 1.6381[38] wurtzite 1.641[4]
MX2 8:4 all tetrahedral 0.2247 fluorite 5.03878[41]
6:3 half octahedral (alternate layers fully occupied) 0.4142 cadmium chloride 5.61[42] cadmium iodide 4.71[41]
MX3 6:2 one-third octahedral 0.4142 rhodium(III) bromide[b][43][44] 6.67[45][c] bismuth iodide 8.26[45][d]
M2X3 6:4 two-thirds octahedral 0.4142 corundum 25.0312[41]
ABO3 two-thirds octahedral 0.4142 ilmenite Depends on charges
and structure[e]
AB2O4 one-eighth tetrahedral and one-half octahedral rA/rO = 0.2247,
rB/rO = 0.4142[f]
spinel, inverse spinel Depends on cation
site distributions[48][49][50]
olivine Depends on cation
site distributions[51]

In some cases, the anions take on a simple cubic packing and the resulting common structures observed are:

Common ionic compound structures with simple cubic packed anions[44]
Stoichiometry Cation:anion
coordination
Interstitial sites occupied Example structure
Name Critical radius
ratio
Madelung constant
MX 8:8 entirely filled cesium chloride 0.7321[52] 1.762675[38]
MX2 8:4 half filled calcium fluoride
M2X 4:8 half filled lithium oxide

Some ionic liquids, particularly with mixtures of anions or cations, can be cooled rapidly enough that there is not enough time for crystal nucleation to occur, so an ionic glass is formed (with no long-range order).[53]

Defects

[edit]
Diagram of charged ions with a positive ion out of place in the structure
Frenkel defect
Diagram of charged ions with a positive and negative missing from the structure
Schottky defect

Within any crystal, there will usually be some defects. To maintain electroneutrality of the crystals, defects that involve loss of a cation will be associated with loss of an anion, i.e. these defects come in pairs.[54] Frenkel defects consist of a cation vacancy paired with a cation interstitial and can be generated anywhere in the bulk of the crystal,[54] occurring most commonly in compounds with a low coordination number and cations that are much smaller than the anions.[55] Schottky defects consist of one vacancy of each type, and are generated at the surfaces of a crystal,[54] occurring most commonly in compounds with a high coordination number and when the anions and cations are of similar size.[55] If the cations have multiple possible oxidation states, then it is possible for cation vacancies to compensate for electron deficiencies on cation sites with higher oxidation numbers, resulting in a non-stoichiometric compound.[54] Another non-stoichiometric possibility is the formation of an F-center, a free electron occupying an anion vacancy.[56] When the compound has three or more ionic components, even more defect types are possible.[54] All of these point defects can be generated via thermal vibrations and have an equilibrium concentration. Because they are energetically costly but entropically beneficial, they occur in greater concentration at higher temperatures. Once generated, these pairs of defects can diffuse mostly independently of one another, by hopping between lattice sites. This defect mobility is the source of most transport phenomena within an ionic crystal, including diffusion and solid state ionic conductivity.[54] When vacancies collide with interstitials (Frenkel), they can recombine and annihilate one another. Similarly, vacancies are removed when they reach the surface of the crystal (Schottky). Defects in the crystal structure generally expand the lattice parameters, reducing the overall density of the crystal.[54] Defects also result in ions in distinctly different local environments, which causes them to experience a different crystal-field symmetry, especially in the case of different cations exchanging lattice sites.[54] This results in a different splitting of d-electron orbitals, so that the optical absorption (and hence colour) can change with defect concentration.[54]

Properties

[edit]
[BMIM]+[PF6]−, an ionic liquid

Acidity/basicity

[edit]

Ionic compounds containing hydrogen ions (H+) are classified as acids, and those containing electropositive cations[57] and basic anions ions hydroxide (OH) or oxide (O2−) are classified as bases. Other ionic compounds are known as salts and can be formed by acid–base reactions.[58] Salts that produce hydroxide ions when dissolved in water are called alkali salts, and salts that produce hydrogen ions when dissolved in water are called acid salts, e.g. sodium hydrogen selenite (NaHSeO3).[59] If the compound is the result of a reaction between a strong acid and a weak base, the result is an acid salt. If it is the result of a reaction between a strong base and a weak acid, the result is a base salt. If it is the result of a reaction between a strong acid and a strong base, the result is a neutral salt.[citation needed] Weak acids reacted with weak bases can produce ionic compounds with both the conjugate base ion and conjugate acid ion, such as ammonium acetate.

Some ions are classed as amphoteric, being able to react with either an acid or a base.[60] This is also true of some compounds with ionic character, typically oxides or hydroxides of less-electropositive metals (so the compound also has significant covalent character), such as zinc oxide, aluminium hydroxide, aluminium oxide and lead(II) oxide.[61]

Solubility

[edit]
The aqueous solubility of a variety of salts as a function of temperature. Some compounds exhibiting unusual solubility behavior have been included.

When simple salts dissolve, they dissociate into individual ions, which are solvated and dispersed throughout the resulting solution. Salts do not exist in solution.[62] In contrast, molecular compounds, which includes most organic compounds, remain intact in solution.

The solubility of salts is highest in polar solvents (such as water) or ionic liquids, but tends to be low in nonpolar solvents (such as petrol/gasoline).[63] This contrast is principally because the resulting ion–dipole interactions are significantly stronger than ion-induced dipole interactions, so the heat of solution is higher. When the oppositely charged ions in the solid ionic lattice are surrounded by the opposite pole of a polar molecule, the solid ions are pulled out of the lattice and into the liquid. If the solvation energy exceeds the lattice energy, the negative net enthalpy change of solution provides a thermodynamic drive to remove ions from their positions in the crystal and dissolve in the liquid. In addition, the entropy change of solution is usually positive for most solid solutes like salts, which means that their solubility increases when the temperature increases.[64] There are some unusual salts such as cerium(III) sulfate, where this entropy change is negative, due to extra order induced in the water upon solution, and the solubility decreases with temperature.[64]

The lattice energy, the cohesive forces between these ions within a solid, determines the solubility. The solubility is dependent on how well each ion interacts with the solvent, so certain patterns become apparent. For example, salts of sodium, potassium and ammonium are usually soluble in water. Notable exceptions include ammonium hexachloroplatinate and potassium cobaltinitrite. Most nitrates and many sulfates are water-soluble. Exceptions include barium sulfate, calcium sulfate (sparingly soluble), and lead(II) sulfate, where the 2+/2− pairing leads to high lattice energies. For similar reasons, most metal carbonates are not soluble in water. Some soluble carbonate salts are: sodium carbonate, potassium carbonate and ammonium carbonate.

Strength

[edit]

Strong salts or strong electrolyte salts are chemical salts composed of strong electrolytes. These salts dissociate completely or almost completely in water. They are generally odorless and nonvolatile.

Strong salts start with Na__, K__, NH4__, or they end with __NO3, __ClO4, or __CH3COO. Most group 1 and 2 metals form strong salts. Strong salts are especially useful when creating conductive compounds as their constituent ions allow for greater conductivity.[citation needed]

Weak salts or weak electrolyte salts are composed of weak electrolytes. These salts do not dissociate well in water. They are generally more volatile than strong salts. They may be similar in odor to the acid or base they are derived from. For example, sodium acetate, CH3COONa, smells similar to acetic acid CH3COOH.

Electrical conductivity

[edit]
Edge-on view of portion of crystal structure of hexamethyleneTTF/TCNQ charge transfer salt.[65]

Salts are characteristically insulators. Although they contain charged atoms or clusters, these materials do not typically conduct electricity to any significant extent when the substance is solid. In order to conduct, the charged particles must be mobile rather than stationary in a crystal lattice. This is achieved to some degree at high temperatures when the defect concentration increases the ionic mobility and solid state ionic conductivity is observed. When the salts are dissolved in a liquid or are melted into a liquid, they can conduct electricity because the ions become completely mobile. For this reason, molten salts and solutions containing dissolved salts (e.g., sodium chloride in water) can be used as electrolytes.[66] This conductivity gain upon dissolving or melting is sometimes used as a defining characteristic of salts.[67]

In some unusual salts: fast-ion conductors, and ionic glasses,[53] one or more of the ionic components has a significant mobility, allowing conductivity even while the material as a whole remains solid.[68] This is often highly temperature dependent, and may be the result of either a phase change or a high defect concentration.[68] These materials are used in all solid-state supercapacitors, batteries, and fuel cells, and in various kinds of chemical sensors.[69][70]

Melting and boiling points

[edit]

Electrostatic forces between particles are strongest when the charges are high, and the distance between the nuclei of the ions is small. In such cases, the compounds generally have very high melting and boiling points and a low vapour pressure.[71] Trends in melting points can be even better explained when the structure and ionic size ratio is taken into account.[72] Above their melting point, salts melt and become molten salts (although some salts such as aluminium chloride and iron(III) chloride show molecule-like structures in the liquid phase).[73] Inorganic compounds with simple ions typically have small ions, and thus have high melting points, so are solids at room temperature. Some substances with larger ions, however, have a melting point below or near room temperature (often defined as up to 100 °C), and are termed ionic liquids.[74] Ions in ionic liquids often have uneven charge distributions, or bulky substituents like hydrocarbon chains, which also play a role in determining the strength of the interactions and propensity to melt.[75]

Even when the local structure and bonding of an ionic solid is disrupted sufficiently to melt it, there are still strong long-range electrostatic forces of attraction holding the liquid together and preventing ions boiling to form a gas phase.[76] This means that even room temperature ionic liquids have low vapour pressures, and require substantially higher temperatures to boil.[76] Boiling points exhibit similar trends to melting points in terms of the size of ions and strength of other interactions.[76] When vapourized, the ions are still not freed of one another. For example, in the vapour phase sodium chloride exists as diatomic "molecules".[77]

Brittleness

[edit]

Most salts are very brittle. Once they reach the limit of their strength, they cannot deform malleably, because the strict alignment of positive and negative ions must be maintained. Instead the material undergoes fracture via cleavage.[78] As the temperature is elevated (usually close to the melting point) a ductile–brittle transition occurs, and plastic flow becomes possible by the motion of dislocations.[78][79]

Compressibility

[edit]

The compressibility of a salt is strongly determined by its structure, and in particular the coordination number. For example, halides with the caesium chloride structure (coordination number 8) are less compressible than those with the sodium chloride structure (coordination number 6), and less again than those with a coordination number of 4.[80]

Colour

[edit]
a pile of red granules on white paper
Cobalt(II) chloride hexahydrate,
CoCl2·6H2O

The colour of a salt is often different from the colour of an aqueous solution containing the constituent ions,[81] or the hydrated form of the same compound.[13]

The anions in compounds with bonds with the most ionic character tend to be colorless (with an absorption band in the ultraviolet part of the spectrum).[82] In compounds with less ionic character, their color deepens through yellow, orange, red, and black (as the absorption band shifts to longer wavelengths into the visible spectrum).[82]

The absorption band of simple cations shifts toward a shorter wavelength when they are involved in more covalent interactions.[82] This occurs during hydration of metal ions, so colorless anhydrous salts with an anion absorbing in the infrared can become colorful in solution.[82]

Salts exist in many different colors, which arise either from their constituent anions, cations or solvates. For example:

Some minerals are salts, some of which are soluble in water.[dubiousdiscuss][clarification needed] Similarly, inorganic pigments tend not to be salts, because insolubility is required for fastness. Some organic dyes are salts, but they are virtually insoluble in water.

Taste

[edit]

Salts can elicit all five basic tastes, e.g., salty (sodium chloride), sweet (lead diacetate, which will cause lead poisoning if ingested), sour (potassium bitartrate), bitter (magnesium sulfate), and umami or savory (monosodium glutamate).

Odor

[edit]

Salts of strong acids and strong bases ("strong salts") are non-volatile and often odorless, whereas salts of either weak acids or weak bases ("weak salts") may smell like the conjugate acid (e.g., acetates like acetic acid (vinegar) and cyanides like hydrogen cyanide (almonds)) or the conjugate base (e.g., ammonium salts like ammonia) of the component ions. That slow, partial decomposition is usually accelerated by the presence of water, since hydrolysis is the other half of the reversible reaction equation of formation of weak salts.

Uses

[edit]

Salts have long had a wide variety of uses and applications. Many minerals are ionic.[83] Humans have processed common salt (sodium chloride) for over 8000 years, using it first as a food seasoning and preservative, and now also in manufacturing, agriculture, water conditioning, for de-icing roads, and many other uses.[84] Many salts are so widely used in society that they go by common names unrelated to their chemical identity. Examples of this include borax, calomel, milk of magnesia, muriatic acid, oil of vitriol, saltpeter, and slaked lime.[85]

Soluble salts can easily be dissolved to provide electrolyte solutions. This is a simple way to control the concentration and ionic strength. The concentration of solutes affects many colligative properties, including increasing the osmotic pressure, and causing freezing-point depression and boiling-point elevation.[86] Because the solutes are charged ions they also increase the electrical conductivity of the solution.[87] The increased ionic strength reduces the thickness of the electrical double layer around colloidal particles, and therefore the stability of emulsions and suspensions.[88]

The chemical identity of the ions added is also important in many uses. For example, fluoride containing compounds are dissolved to supply fluoride ions for water fluoridation.[89]

Solid salts have long been used as paint pigments, and are resistant to organic solvents, but are sensitive to acidity or basicity.[90] Since 1801 pyrotechnicians have described and widely used metal-containing salts as sources of colour in fireworks.[91] Under intense heat, the electrons in the metal ions or small molecules can be excited.[92] These electrons later return to lower energy states, and release light with a colour spectrum characteristic of the species present.[93][94]

In chemical synthesis, salts are often used as precursors for high-temperature solid-state synthesis.[95]

Many metals are geologically most abundant as salts within ores.[96] To obtain the elemental materials, these ores are processed by smelting or electrolysis, in which redox reactions occur (often with a reducing agent such as carbon) such that the metal ions gain electrons to become neutral atoms.[97][98]

Nomenclature

[edit]

According to the nomenclature recommended by IUPAC, salts are named according to their composition, not their structure.[99] In the most simple case of a binary salt with no possible ambiguity about the charges and thus the stoichiometry, the common name is written using two words.[100] The name of the cation (the unmodified element name for monatomic cations) comes first, followed by the name of the anion.[101][102] For example, MgCl2 is named magnesium chloride, and Na2SO4 is named sodium sulfate (SO2−
4
, sulfate, is an example of a polyatomic ion). To obtain the empirical formula from these names, the stoichiometry can be deduced from the charges on the ions, and the requirement of overall charge neutrality.[103]

If there are multiple different cations and/or anions, multiplicative prefixes (di-, tri-, tetra-, ...) are often required to indicate the relative compositions,[104] and cations then anions are listed in alphabetical order.[105] For example, KMgCl3 is named magnesium potassium trichloride to distinguish it from K2MgCl4, magnesium dipotassium tetrachloride[106] (note that in both the empirical formula and the written name, the cations appear in alphabetical order, but the order varies between them because the symbol for potassium is K).[107] When one of the ions already has a multiplicative prefix within its name, the alternate multiplicative prefixes (bis-, tris-, tetrakis-, ...) are used.[108] For example, Ba(BrF4)2 is named barium bis(tetrafluoridobromate).[109]

Compounds containing one or more elements which can exist in a variety of charge/oxidation states will have a stoichiometry that depends on which oxidation states are present, to ensure overall neutrality. This can be indicated in the name by specifying either the oxidation state of the elements present, or the charge on the ions.[109] Because of the risk of ambiguity in allocating oxidation states, IUPAC prefers direct indication of the ionic charge numbers.[109] These are written as an arabic integer followed by the sign (... , 2−, 1−, 1+, 2+, ...) in parentheses directly after the name of the cation (without a space separating them).[109] For example, FeSO4 is named iron(2+) sulfate (with the 2+ charge on the Fe2+ ions balancing the 2− charge on the sulfate ion), whereas Fe2(SO4)3 is named iron(3+) sulfate (because the two iron ions in each formula unit each have a charge of 3+, to balance the 2− on each of the three sulfate ions).[109] Stock nomenclature, still in common use, writes the oxidation number in Roman numerals (... , −II, −I, 0, I, II, ...). So the examples given above would be named iron(II) sulfate and iron(III) sulfate respectively.[110] For simple ions the ionic charge and the oxidation number are identical, but for polyatomic ions they often differ. For example, the uranyl(2+) ion, UO2+
2
, has uranium in an oxidation state of +6, so would be called a dioxouranium(VI) ion in Stock nomenclature.[111] An even older naming system for metal cations, also still widely used, appended the suffixes -ous and -ic to the Latin root of the name, to give special names for the low and high oxidation states.[112] For example, this scheme uses "ferrous" and "ferric", for iron(II) and iron(III) respectively,[112] so the examples given above were classically named ferrous sulfate and ferric sulfate.[citation needed]

Common salt-forming cations include:

Common salt-forming anions (parent acids in parentheses where available) include:

Salts with varying number of hydrogen atoms replaced by cations as compared to their parent acid can be referred to as monobasic, dibasic, or tribasic, identifying that one, two, or three hydrogen atoms have been replaced; polybasic salts refer to those with more than one hydrogen atom replaced. Examples include:

Non-salt

[edit]

Zwitterion

[edit]

Zwitterions contain an anionic and a cationic centre in the same molecule, but are not considered salts. Examples of zwitterions are amino acids, many metabolites, peptides, and proteins.[113]

See also

[edit]

Notes

[edit]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
In chemistry, a salt is an ionic compound formed by the combination of a positively charged cation and a negatively charged anion, held together by strong electrostatic forces. These compounds typically result from the neutralization reaction between an and a base, in which the cation derives from the base and the anion from the acid, producing a neutral product. Salts encompass a vast array of substances beyond common table salt, including both simple binary compounds like sodium chloride (NaCl) and more complex ones involving polyatomic ions. Salts are characteristically crystalline solids at room temperature, exhibiting high melting and boiling points due to the robust ionic bonding within their lattice structures. Many salts are highly soluble in water, where they dissociate completely into free ions, enabling the resulting solutions to conduct electricity effectively. For instance, sodium chloride dissociates into Na⁺ and Cl⁻ ions in aqueous solution, while other salts like copper(II) sulfate form distinctive colored crystals and solutions. The physical form of salt crystals can vary, often appearing as cubic or octahedral structures depending on the specific ions involved. Salts play a fundamental role in biological systems, serving as essential electrolytes that regulate , function, and levels in organisms. Industrially, they are critical raw materials in chemical manufacturing, such as the production of and via the chlor-alkali process, as well as in detergents, production, and . Additionally, specialized salts like molten nitrates are utilized in , metal processing, and applications due to their thermal stability. Their versatility underscores their importance across natural, biological, and technological contexts.

Definition and Classification

Definition

In chemistry, a salt is defined as an ionic formed through the neutralization reaction of an and a base, resulting in a substance composed of cations derived from the base and anions from the , while excluding oxides and water-soluble hydroxides. This distinguishes salts from other ionic species, emphasizing their role as products of acid-base interactions where the resulting compound dissociates completely into ions in aqueous solutions. The general formula for a simple salt is \ceM+X\ce{M^{+} X^{-}}, where \ceM+\ce{M^{+}} represents a metal cation and \ceX\ce{X^{-}} an anion, though this extends to more complex structures involving polyatomic ions such as \ceSO42\ce{SO4^{2-}} or \ceNH4+\ce{NH4^{+}}. Salts typically exhibit high melting points, often exceeding 600°C, due to the strong electrostatic forces within their ionic lattices. Many are soluble in , forming crystalline solids at , and they conduct electricity when molten or dissolved because the ions are free to move. A classic example is (\ceNaCl\ce{NaCl}), the archetypal salt, which forms an ionic lattice of \ceNa+\ce{Na^{+}} and \ceCl\ce{Cl^{-}} ions, demonstrating these properties with a of 801°C and high solubility in . This structure underscores the crystalline nature and conductivity of salts in solution or melt states.

Types of Salts

Salts in chemistry are classified based on their composition, the extent of neutralization in their formation, and their behavior in solution. This categorization helps in understanding their properties and applications. The primary types include normal salts, acid salts, basic salts, double salts, and complex salts, each distinguished by the nature of their ions and structural features. Normal salts are formed by the complete neutralization of an acid with a base, resulting in the replacement of all ionizable hydrogen ions from the acid or hydroxyl ions from the base. These salts typically exhibit neutral behavior in aqueous solutions when derived from strong acids and strong bases. A representative example is sodium chloride (\ceNaCl\ce{NaCl}), produced from hydrochloric acid and sodium hydroxide. Acid salts arise from the partial neutralization of polyprotic acids, retaining one or more replaceable hydrogen ions in their structure. These salts often produce acidic solutions due to the hydrolysis of the hydrogen-containing anion. For instance, sodium bisulfate (\ceNaHSO4\ce{NaHSO4}) forms from sulfuric acid and sodium hydroxide, where only one hydrogen is replaced. Basic salts result from the incomplete neutralization of polyacidic bases, incorporating one or more replaceable hydroxyl groups. Such salts tend to yield basic solutions through the hydrolysis of the hydroxyl-bearing cation. An example is basic lead chloride (\cePb(OH)Cl\ce{Pb(OH)Cl}), derived from lead hydroxide and hydrochloric acid. Double salts contain more than one type of cation or anion and form when solutions of two different simple salts are mixed and crystallized together; they dissociate into their constituent ions in solution but exhibit distinct properties in the solid state. Mohr's salt (\ceFeSO4(NH4)2SO46H2O\ce{FeSO4 \cdot (NH4)2SO4 \cdot 6H2O}) is a classic example, combining iron(II) sulfate and ammonium sulfate. Complex salts involve coordination compounds where a central metal ion is bound to ligands, forming a complex ion that acts as a single unit; these do not fully ionize into simple ions in solution. Potassium ferrocyanide (\ceK4[Fe(CN)6]\ce{K4[Fe(CN)6]}) exemplifies this, with the ferrocyanide ion [\ceFe(CN)6]4[ \ce{Fe(CN)6]^{4-} } coordinated around iron. Salts can also be classified by their solubility in water, which depends on the interacting ions and follows general empirical rules. Soluble salts include those of metals (e.g., , \ceNaCl\ce{NaCl}) and , nitrates, most halides (except silver, lead, and mercury(I) halides), and most sulfates (except barium, , lead, and calcium sulfates). Insoluble salts encompass most carbonates, phosphates, sulfides, hydroxides (except and some group 2), and silver halides like (\ceAgCl\ce{AgCl}).

History

Early Observations and Uses

The earliest evidence of systematic salt extraction dates back to around 3000 BCE in ancient , where communities harvested sodium chloride from brine springs and lake beds in regions like province, primarily for and as a seasoning to enhance flavor and extend . In , similar practices emerged by approximately 3000 BCE, with salt derived from evaporated or natural deposits used to cure and meats, preventing spoilage in the hot climate and supporting long-distance trade. These empirical applications underscored salt's role in enabling surplus , which was crucial for the growth of early agricultural societies. Ancient Egyptians further observed salt's preservative qualities around 2600 BCE during the , incorporating —a naturally occurring sodium salt mixture—into mummification rituals to dehydrate bodies and inhibit bacterial decay, a practice detailed in later accounts by Greek historian . This recognition of salt's desiccating properties marked one of the earliest documented uses beyond , transforming it into a cornerstone of funerary customs that preserved thousands of remains for the . In the , salt's economic importance was evident in the term salarium, an allowance provided to officials and soldiers for procuring salt, reflecting its status as a vital commodity essential for health, preservation, and military logistics, though not as direct payment. Medicinal applications of salt appeared in around 400 BCE, with advocating its use in treatments such as inhaling salt vapors for respiratory ailments and applying saline solutions to wounds for their antibacterial effects, based on observations of salt's ability to draw out fluids and purify tissues. Ritual significance is highlighted in biblical texts, such as Leviticus 2:13, which mandates seasoning grain offerings with salt as a symbol of enduring covenants with God, emphasizing its incorruptible nature in religious practices across ancient Near Eastern cultures. By medieval , () was produced through leaching wood ashes, initially for soap-making and glass production, expanding the practical repertoire of salt-like compounds derived from natural sources.

Modern Chemical Understanding

In the late , advanced the understanding of salts by classifying them as products of reactions between acids and bases, a concept outlined in his seminal 1789 treatise Traité élémentaire de chimie. This work shifted chemistry toward a systematic , viewing salts not as mysterious essences but as stable compounds formed by the combination of acidic and basic substances, laying the groundwork for quantitative analysis in chemical reactions. John Dalton's atomic theory, introduced in 1808, further revolutionized salt chemistry by proposing that salts consist of indivisible atoms combining in fixed proportions, which directly led to the development of stoichiometric formulas for compounds like (NaCl). Published in A New System of Chemical Philosophy, this theory explained the observed in salt formation, enabling chemists to predict and balance reactions based on atomic weights. A pivotal advancement came in 1887 with Svante Arrhenius's theory of electrolytic dissociation, which posited that salts dissociate into ions when dissolved in water, accounting for their conductive properties as electrolytes. This idea, detailed in his doctoral thesis and later elaborated in publications, resolved discrepancies in solution behavior and earned Arrhenius the in 1903 for its profound impact on . In the 20th century, , pioneered by and William Lawrence Bragg in the 1910s and applied to salts in the 1920s, revealed the ionic lattice structures of crystals like NaCl, confirming their ordered atomic arrangements. Complementing this, Linus Pauling's scale, developed in the 1930s and published in his 1939 book The Nature of the Chemical Bond, provided a quantitative tool to analyze bonding in salts, distinguishing purely ionic interactions from partial covalency based on differences. Since 2000, computational modeling, particularly simulations, has refined insights into salt solutions by simulating ion-water interactions at the atomic level, improving predictions of and dynamics without introducing major new paradigms. These approaches, as reviewed in recent perspectives, build on classical theories to address complex behaviors in concentrated electrolytes.

Formation

Reaction of Acids and Bases

The formation of salts primarily occurs through acid-base neutralization reactions, in which an acid reacts with a base to produce a salt and water. This process involves the transfer of a proton (H⁺) from the acid to the base, resulting in the combination of the acid's anion with the base's cation to form the salt. The general equation for such a reaction is HA + MOH → MA + H₂O, where HA represents the acid, MOH the base, MA the salt, and H₂O water. Stoichiometry in these reactions requires balancing the equation based on the number of protons donated by the acid and accepted by the base. For monoprotic acids and monobasic bases, the reaction is 1:1, as exemplified by the neutralization of with : HCl + NaOH → NaCl + H₂O. Polyprotic acids, which can donate multiple protons, necessitate multiple equivalents of base for complete neutralization; for instance, reacts with two moles of : H₂SO₄ + 2NaOH → Na₂SO₄ + 2H₂O. These balanced equations ensure that the reaction proceeds to form the neutral salt without excess reactants. Neutralization reactions typically occur in aqueous solutions at , allowing ions to dissociate and react efficiently. For the formation of insoluble salts, gentle heating may be applied to promote and improve yield by enhancing limits or driving the reaction forward. An illustrative example is the formation of , where acts as a weak acid (forming in water) reacting with : Ca(OH)₂ + CO₂ → CaCO₃ + H₂O; this reaction produces the insoluble CaCO₃ precipitate, commonly observed in processes like limewater . When strong acids and strong bases are involved, the neutralization reaction goes to completion, yielding nearly 100% of the salt under stoichiometric conditions due to the highly favorable of formation. This complete conversion contrasts with reactions involving weak acids or bases, where equilibrium considerations may limit yield. The resulting salts can vary in type, such as normal or acidic salts, depending on the reactants.

Other Synthetic Methods

Salts can be synthesized through direct combination of elemental metals and non-metals, often requiring high temperatures to facilitate the reaction. For instance, reacts vigorously with gas to form , as represented by the equation 2Na+Cl22NaCl2\text{Na} + \text{Cl}_2 \rightarrow 2\text{NaCl}. This method is particularly useful for preparing binary salts like halides in settings, where the exothermic nature of the reaction drives the formation of the ionic lattice. Metathesis reactions, also known as double displacement reactions, involve the exchange of ions between two ionic compounds, typically in , to yield new salts. A classic example is the reaction between and , producing precipitate and solution: AgNO3(aq)+NaCl(aq)AgCl(s)+NaNO3(aq)\text{AgNO}_3(\text{aq}) + \text{NaCl}(\text{aq}) \rightarrow \text{AgCl}(\text{s}) \downarrow + \text{NaNO}_3(\text{aq}). This process is driven by the low solubility of one product, such as the formation of an insoluble salt, making it a common technique for isolating specific salts like silver halides. Salts can also be prepared from metal oxides or carbonates via reactions that avoid direct neutralization, including pathways. For example, heating decomposes it to and oxygen gas: 2NaNO32NaNO2+O22\text{NaNO}_3 \rightarrow 2\text{NaNO}_2 + \text{O}_2, yielding a new salt that can be further reacted if needed. Similarly, group 2 nitrates like decompose upon heating to form the corresponding , , and oxygen: 2Ca(NO3)22CaO+4NO2+O22\text{Ca(NO}_3)_2 \rightarrow 2\text{CaO} + 4\text{NO}_2 + \text{O}_2, providing a route to intermediates for subsequent salt formation. These thermal methods are valuable for producing salts or for recycling components in synthetic sequences. Electrochemical methods, such as , enable the synthesis of salts from molten salts or aqueous s by applying an to drive separation and recombination. In the , of produces , gas, and : overall reaction 2NaCl+2H2OCl2+H2+2NaOH2\text{NaCl} + 2\text{H}_2\text{O} \rightarrow \text{Cl}_2 + \text{H}_2 + 2\text{NaOH}, with anodic oxidation of ions and cathodic reduction of . This industrial-scale technique, using cells for efficiency, generates high-purity NaOH as a key salt product while minimizing energy use at around 2,200–2,500 kWh per ton of . For complex salts, employs high-pressure, high-temperature conditions in non-aqueous solvents to promote reactions that form intricate ionic structures. This method, developed prominently since the , involves sealing precursors in a solvent like and heating to 100–200°C, facilitating the assembly of polyselenidoarsenate salts with complex cations, such as [Ni(phen)₃][As₂Se₂(μ-Se₃)(μ-Se₅)]. approaches excel in producing crystalline materials with controlled morphology, offering advantages over conventional methods for like or coordination compounds.

Bonding

Ionic Bonding

Ionic bonding in salts is characterized by the electrostatic attraction between oppositely charged ions, typically a cation and an anion, which form when atoms transfer electrons to achieve stable electron configurations. This attraction is governed by Coulomb's law, which states that the force FF between two point charges q1q_1 and q2q_2 separated by distance rr is given by
F=kq1q2r2,F = k \frac{q_1 q_2}{r^2},
where k=14πϵ0k = \frac{1}{4\pi\epsilon_0} is the Coulomb constant, with ϵ0\epsilon_0 being the permittivity of free space. In ionic compounds like salts, this force holds the ions together in a lattice, with the strength increasing as the charges q1q_1 and q2q_2 grow in magnitude and decreasing with larger interionic distances rr.
The stability of ionic salts arises from the , which is the energy released when gaseous combine to form the solid lattice per mole of compound. Lattice energy can be estimated using the Born-Landé equation, which accounts for the attractive electrostatic interactions and short-range repulsions between . The basic form for the attractive contribution is
U=NAkZ+Ze24πϵ0r0,U = -\frac{N_A k Z_+ Z_- e^2}{4\pi\epsilon_0 r_0},
where NAN_A is Avogadro's constant, Z+Z_+ and ZZ_- are the charges, ee is the , and r0r_0 is the equilibrium interionic distance; the full equation incorporates a for lattice geometry and a repulsion term (11/n)(1 - 1/n), with nn as the Born exponent (typically 5–12 for ionic solids). Higher lattice energies correspond to stronger , favored by small sizes and high charge magnitudes.
To understand the energetics of salt formation, the Born-Haber cycle provides a stepwise thermodynamic pathway linking the to measurable quantities, exemplified by (NaCl). The cycle includes: (1) sublimation of solid Na to gaseous Na atoms (ΔH>0\Delta H > 0); (2) of Na(g) to Na⁺(g) + e⁻ (ΔH>0\Delta H > 0, first ); (3) dissociation of ½ Cl₂(g) to Cl(g) (ΔH>0\Delta H > 0); (4) addition of e⁻ to Cl(g) forming Cl⁻(g) (ΔH<0\Delta H < 0, electron affinity); and (5) combination of Na⁺(g) and Cl⁻(g) to form NaCl(s), releasing the lattice energy (ΔH<0\Delta H < 0). By Hess's law, the sum of these steps equals the overall formation enthalpy, allowing indirect calculation of lattice energy when other values are known. While the ionic model assumes complete electron transfer and pure electrostatic interactions, ideal ionic bonding is most closely approached in alkali metal halides like NaCl and KBr, where large electronegativity differences and simple +1/-1 charges minimize deviations. In contrast, transition metal salts, such as those of or , often exhibit deviations from ideality due to variable oxidation states and d-electron involvement, leading to partial covalent character that reduces lattice energies compared to predictions from purely ionic models.

Covalent and Other Interactions

While ideal ionic bonding in salts assumes complete electron transfer between cations and anions, real salts often exhibit deviations due to partial covalent character and secondary interactions that influence bond polarity and lattice stability. Fajans' rules describe how the polarizing power of a cation—determined by its small size and high charge—can distort the electron cloud of an anion, inducing covalent character in the bond. A small, highly charged cation like Al³⁺ polarizes the Cl⁻ anion more effectively than a larger, low-charge cation like Na⁺, leading to greater covalency in AlCl₃ compared to NaCl. This polarization effect increases with higher cation charge density and larger anion polarizability, shifting the bond from predominantly ionic toward hybrid ionocovalent. The degree of covalent character can also be assessed using electronegativity differences on the Pauling scale, where atoms with similar electronegativities (ΔEN < 1.7) form bonds with significant covalent contributions, while larger differences (ΔEN > 1.7) favor ionic character typical of many salts. For instance, the Na–Cl bond has ΔEN = 2.1, supporting its ionic nature, but compounds like AlCl₃ (ΔEN ≈ 1.5 for Al–Cl) show partial covalency due to the lower difference. In hydrated salts, hydrogen bonding provides an additional interaction where molecules bridge cations and anions, enhancing structural cohesion beyond primary ionic forces. In CuSO₄·5H₂O, four molecules coordinate directly to Cu²⁺, while the fifth forms bonds that link the complex to SO₄²⁻ ions, creating a networked lattice stabilized by these directional O–H···O interactions. All atoms in the molecules participate in such bonding, as confirmed by low-temperature studies. Van der Waals forces, though weak compared to ionic attractions, contribute to the cohesion of ionic lattices, particularly in salts with large, polarizable anions like I⁻, where dispersion interactions between anions supplement the primary electrostatic binding. These forces arise from temporary dipoles and become more significant in crystals with softer, larger anions that allow greater cloud distortion. Ammonium salts such as exemplify coordinate covalent bonding within the cation, where the ammonium ion () features three conventional N–H covalent bonds and one dative bond from nitrogen's to a proton, resulting in a tetrahedral held ionically to Cl⁻. This hybrid bonding underscores how salts can incorporate covalent elements internally while maintaining overall ionic character between polyatomic ions.

Structure

Crystal Lattices

In ionic crystals, salts form extended three-dimensional lattices composed of alternating cations and anions, held together by electrostatic forces, resulting in a repeating pattern that defines the 's and stability. A common is the rock salt type, exemplified by (NaCl), which adopts a face-centered cubic (FCC) lattice with a 1:1 cation-to-anion ratio. In this arrangement, each Na⁺ ion is octahedrally coordinated to six Cl⁻ ions ( 6:6), and the unit cell contains four formula units, with ions occupying octahedral sites in the lattice. Another prevalent lattice is the cesium chloride (CsCl) structure, a primitive cubic arrangement where cations and anions form two interpenetrating simple cubic sublattices. Here, each Cs⁺ ion is cubically coordinated to eight Cl⁻ ions ( 8:8), with one per and no direct contact between like-charged ions to minimize repulsion. For salts with more covalent character, such as (ZnS) in its form, the structure is a cubic close-packed FCC lattice of anions with cations occupying half the tetrahedral voids, yielding tetrahedral coordination (4:4). The unit cell includes four Zn²⁺ and four S²⁻ ions, maintaining a 1:1 . The specific coordination geometry in these lattices is governed by the radius ratio rule, which relates the ratio of cation radius (r⁺) to anion radius (r⁻) to the stable : for 0.414 ≤ r⁺/r⁻ < 0.732, octahedral (6) coordination predominates, as in NaCl (r⁺/r⁻ ≈ 0.56); for r⁺/r⁻ ≥ 0.732, cubic (8) coordination occurs, as in CsCl; and for 0.225 ≤ r⁺/r⁻ < 0.414, tetrahedral (4) coordination is favored, as in ZnS (r⁺/r⁻ ≈ 0.39). Unit cells in ionic lattices vary in volume and packing efficiency depending on the structure; for example, the NaCl FCC unit cell has a volume of a³ (where a is the lattice parameter) and achieves a packing efficiency of approximately 74% when treating ions as hard spheres in close-packed arrangements, reflecting efficient space utilization in the lattice. Some salts exhibit polymorphism, where the same composition forms distinct lattice types under different conditions; (TiO₂), for instance, occurs as (tetragonal, with Ti⁴⁺ in octahedral 6-coordination to O²⁻ and each O²⁻ bonded to three Ti⁴⁺) or (also tetragonal but with distorted octahedral coordination, leading to a less compact structure).

Structural Defects

Structural defects in ionic crystals, such as salts, represent deviations from the periodic arrangement of ions in the lattice, arising during , thermal processes, or external stresses. These imperfections include point, line, and plane defects, as well as non-stoichiometric compositions, which occur to maintain charge neutrality in the ionic structure. Point defects are zero-dimensional imperfections localized at atomic sites. Vacancies, where an ion is missing from its lattice position, are common in salts like (NaCl), forming Schottky defects that involve equal numbers of cation and anion vacancies to preserve electroneutrality. Interstitial defects occur when an ion occupies a site between regular lattice positions, though they are less frequent in highly coordinated ionic structures due to space constraints. In contrast, Frenkel defects combine a vacancy and an interstitial, typically involving smaller cations; for example, in (AgCl), silver ions displace to interstitial sites, leaving cation vacancies behind. Line defects, or , extend in one dimension and disrupt the continuity of lattice planes. Edge dislocations feature an extra half-plane of ions inserted into the lattice, causing local compression or tension, while screw dislocations involve a shear displacement along the dislocation line, resulting in a helical arrangement of lattice planes. These dislocations influence in salts by providing sites for attachment or hindering perfect layer formation. Plane defects are two-dimensional disruptions across lattice layers. Stacking faults arise when the of ionic layers is interrupted, such as an ABCABC in close-packed structures shifting to ABCACBC. Grain boundaries form in polycrystalline salts, separating regions of differing crystallographic orientation and consisting of mismatched lattice planes. Non-stoichiometry in salts refers to compositions deviating from ideal 1:1 cation-anion ratios, often due to excess vacancies. In (Fe1-xO, ), cation vacancies predominate, with each vacancy cluster compensating for charge imbalance by associating with neighboring iron ions in higher oxidation states. Detection of these defects typically involves techniques that reveal deviations from ideal lattice periodicity. identifies line broadening in diffraction patterns caused by strain from dislocations or small grain sizes at boundaries. Conductivity measurements indirectly detect point defects by assessing enhanced mobility through vacancies or interstitials.

Physical Properties

Solubility and Hydration

The solubility of salts in varies widely depending on the specific s involved, governed by empirical rules that predict whether a given ionic compound will dissolve appreciably. Salts containing cations (such as Na⁺ and K⁺) or (NH₄⁺) are generally soluble, as are nitrates (NO₃⁻). In contrast, carbonates (CO₃²⁻) and phosphates (PO₄³⁻) are typically insoluble except when paired with or Group 2 cations (such as Ca²⁺ for some phosphates). These rules arise from the balance between , which holds the ions in the solid , and the released upon in , with highly soluble salts like NaCl dissolving to concentrations exceeding 6 M at 25°C. When salts dissolve, the process involves the formation of hydration shells around the s through ion-dipole interactions between the charged s and the polar molecules. The hydration (ΔH_hyd) quantifies this stabilization and is approximated by the relation ΔHhydconstantq2r\Delta H_{\text{hyd}} \approx -\frac{\text{constant} \cdot q^2}{r}, where qq is the ion charge and rr is the ; smaller s like Li⁺ (with r76r \approx 76 pm) exhibit more negative (exothermic) hydration energies, around -519 kJ/mol, due to stronger electrostatic attraction. This energy offsets the endothermic lattice dissociation, favoring dissolution for salts with low lattice energies or high hydration energies, such as halides. For sparingly soluble salts, equilibrium is described by the product constant (K_sp), the product of concentrations at saturation. For example, (AgCl) has Ksp=[\ceAg+][\ceCl]=1.8×1010K_{\text{sp}} = [\ce{Ag+}] [\ce{Cl-}] = 1.8 \times 10^{-10} at 25°C, indicating very low of about 1.3 × 10⁻⁵ M. Solubility can be influenced by external factors like and . For (CaSO₄), solubility increases modestly with temperature, from about 0.20 g/100 mL at 0°C to 0.24 g/100 mL at 40°C, due to the endothermic nature of its dissolution. pH affects solubility through or ; for instance, CaSO₄ becomes less soluble at higher pH values above 7, as hydroxide ions can form less soluble complexes or alter ionic equilibria. The further modulates solubility by Le Châtelier's principle: adding an ion shared with the salt shifts the dissolution equilibrium leftward, reducing overall solubility. In , with its high Na⁺ (≈0.47 M) and Cl⁻ (≈0.55 M) concentrations, the solubility of additional NaCl is suppressed compared to pure , aiding processes like salt in .

Melting and Boiling Points

Ionic salts exhibit notably high melting points compared to molecular compounds, primarily due to the strong electrostatic attractions in their ionic lattices, which require substantial energy to disrupt. For instance, sodium chloride (NaCl) has a melting point of 801 °C, while magnesium oxide (MgO) reaches 2852 °C, reflecting the robust ionic bonding that holds the crystal structure together. These elevated temperatures underscore the thermal stability of ionic compounds, where the lattice energy—the energy released when gaseous ions form the solid—directly correlates with the melting point, as higher lattice energies demand more heat to overcome the interionic forces. The melting points of salts increase with greater , which is influenced by the sizes and charges of the constituent . Smaller and those with higher charges pack more closely, enhancing electrostatic interactions; for example, aluminum fluoride (AlF₃), with its Al³⁺ cation, has a of 1291 °C, significantly higher than (NaF) at 993 °C. Similarly, ion size plays a role: as cation or anion radii decrease, the rises, strengthening bonds and elevating melting points across . However, deviations occur when covalent character increases, as in (AgCl), which melts at 455 °C due to partial polarization of the by the large, polarizable Ag⁺ cation, weakening the purely ionic lattice. Boiling points of ionic salts are typically even higher than their melting points, as vaporization involves further separation of ions into the gas phase, but many salts decompose before reaching this stage. , for example, boils at 1413 °C without . In contrast, (CaCO₃) decomposes at 825 °C into and , preventing observation of a true . Crystalline salts upon form ionic liquids—molten states composed of discrete ions that retain conductivity and differ from amorphous structures by maintaining ordered fluidity at high temperatures.

Density, Brittleness, and Compressibility

Ionic salts possess densities determined by the arrangement and packing of ions within their crystal lattices, which can be precisely calculated using lattice parameters, the number of formula units per unit cell, and molar masses. For sodium chloride (NaCl), adopting the rock salt structure with a lattice parameter of approximately 5.64 Å, the theoretical density is 2.16 g/cm³, reflecting efficient cubic close-packing of Na⁺ and Cl⁻ ions. Variations in density across different salts arise from differences in ionic radii and charges, which affect the overall volume occupied by ions in the lattice; for instance, denser packing occurs in salts with smaller, higher-charged ions. The brittleness of ionic salts stems from their lattice structure and electrostatic interactions. Under mechanical stress, such as , the layers of ions in the shift, positioning ions of the same charge adjacent to one another, which generates intense repulsive forces that cause the to shatter rather than deform plastically. This lack of contrasts with metallic solids, where delocalized electrons enable layer sliding without repulsion. Hardness in salts, measured on the , is generally low due to weak interionic forces relative to covalent materials, with (NaCl) rating 2.5, meaning it can be scratched by a fingernail. However, hardness tends to increase with the charge of the ions, as higher charges strengthen electrostatic attractions and improve resistance to indentation or scratching; for example, salts like MgO exhibit greater than NaCl owing to divalent ions. Compressibility of salts is low, attributable to the rigid ionic bonds that resist volume changes under pressure. The of NaCl, quantifying this resistance, is about 24 GPa, indicating that substantial force is required to alter its volume by 1%. This property underscores the stability of salt lattices under compressive loads, though extreme pressures can induce phase transitions in some cases. Certain salts exhibit mechanical anisotropy, where properties like elasticity and strength depend on the direction relative to the crystal axes. In (CaCO₃), a rhombohedral salt, stress-strain behavior and patterns vary significantly along different crystallographic orientations, reflecting the underlying lattice asymmetry.

Sensory Properties

Salts exhibit a range of sensory properties that are primarily determined by their ionic composition and physical form, allowing for direct human observation without specialized equipment. The of salts varies depending on the cations and anions involved; for instance, (NaCl) produces a characteristic salty taste when dissolved, as the sodium ions (Na⁺) interact with epithelial sodium channels on the tongue's , while ions (Cl⁻) contribute to the overall perception. In contrast, (KCl) is perceived as salty at low concentrations but imparts a bitter aftertaste at higher levels, due to the potassium ions (K⁺) poorly activating the same sodium channels and stimulating bitter taste receptors. Acid salts, such as , elicit a sour sensation stemming from the partial release of hydrogen ions (H⁺) that activate acid-sensitive taste receptors. Most inorganic salts are odorless in their solid or aqueous forms, as they lack volatile components under normal conditions. However, certain ammonium salts, like ammonium carbonate, release pungent ammonia gas (NH₃) upon exposure to moisture or heat, producing a sharp, irritating odor detectable even at low concentrations. Similarly, some thiocyanate salts, such as those involving hydrogen thiocyanate (HSCN), can emit a stinking, sulfur-like odor resembling that of thiocyanic acid. The color of salts is typically white or colorless in pure crystalline form, as seen in NaCl, which appears transparent and colorless due to its ionic lattice lacking electronic transitions in the visible spectrum. Salts containing transition metal ions, however, display vivid colors; for example, copper(II) chloride (CuCl₂) forms blue solutions or solids from the presence of Cu²⁺ ions. Structural defects, such as F-centers in alkali halide crystals, can also induce coloration—irradiated NaCl, for instance, develops a yellow tint from electron-trapped anion vacancies. In terms of transparency, single of salts like NaCl are optically clear, allowing to pass through without significant , which highlights their ordered ionic . When ground into , however, the same salts become opaque and , as the irregular particle surfaces diffuse in all directions. Hygroscopicity is a notable sensory trait in many salts, where they visibly absorb atmospheric moisture; highly hygroscopic salts like (CaCl₂) exhibit deliquescence, dissolving into a pool over time as they draw in until saturation. This process is observable as a gradual and of the solid, distinguishing it from less reactive salts.

Chemical Properties

Acidity and Basicity

Salts in exhibit acidity, basicity, or neutrality based on the relative strengths of the parent and base from which they are derived, primarily through the of their ions. This behavior arises because the anions or cations of the salt can react with to produce H₃O⁺ or OH⁻ ions, shifting the away from neutrality unless both ions are from strong acids and bases. The classification avoids full exploration of hydrolysis mechanisms but focuses on the resulting effects, which require the salt to be soluble for observable changes. Neutral salts form from a strong acid and a strong base, such as (NaCl) derived from (HCl) and (NaOH); their aqueous solutions have a of approximately 7 at 25°C, as neither hydrolyzes significantly. For example, a 0.1 M NaCl solution maintains near-neutral due to the negligible interaction of Na⁺ and Cl⁻ with water. Acidic salts result from a strong acid and a , like (NH₄Cl) from HCl and (NH₃); the NH₄⁺ cation hydrolyzes to produce H₃O⁺, yielding solutions with less than 7. The equilibrium is NH₄⁺ + H₂O ⇌ NH₃ + H₃O⁺, where the for NH₄⁺ is given by Ka=KwKb(\ceNH3)K_a = \frac{K_w}{K_b(\ce{NH3})}, with KwK_w being the ion product of (1.0 × 10⁻¹⁴ at 25°C). A typical 0.5 M solution has a around 5, reflecting the weak basicity of NH₃ (Kb1.8×105K_b \approx 1.8 \times 10^{-5}). Basic salts arise from a weak and a strong base, such as (NaCH₃COO) from acetic (CH₃COOH) and NaOH; the CH₃COO⁻ anion hydrolyzes to produce OH⁻, resulting in greater than 7. The equilibrium is CH₃COO⁻ + H₂O ⇌ CH₃COOH + OH⁻, with the base dissociation constant Kb=KwKa(\ceCH3COOH)K_b = \frac{K_w}{K_a(\ce{CH3COOH})}, where Ka(\ceCH3COOH)1.8×105K_a(\ce{CH3COOH}) \approx 1.8 \times 10^{-5}. For instance, a 0.1 M solution exhibits a near 9, due to the weak acidity of CH₃COOH. Salts from a weak acid and a weak base, like (NH₄CH₃COO), have values that depend on the relative magnitudes of the parent KaK_a and KbK_b; if comparable, the solution is approximately neutral ( ≈ 7). In , the acidic of NH₄⁺ balances the basic of CH₃COO⁻, often yielding a close to 7 in dilute solutions, as seen in 1 M preparations adjusted to neutrality. The of salt solutions is determined experimentally using pH indicators, which change color in response to H⁺ concentration, or more precisely with meters equipped with electrodes that measure potential differences proportional to pH. meters provide accurate readings to 0.01 units, essential for quantifying subtle shifts in salt solutions, while indicators like are suitable for rough estimates in the basic range.

Hydrolysis Reactions

of salts refers to the chemical reactions in which the constituent ions of a dissolved salt interact with molecules, resulting in the production of ions (H₃O⁺) or ions (OH⁻), which thereby alter the of the solution. This process occurs primarily with salts derived from weak acids or weak bases, as the ions from strong acids or strong bases do not significantly hydrolyze due to their negligible tendency to accept or donate protons. In cases of acidic hydrolysis, such as with salts like aluminum chloride (AlCl₃), the metal cation acts as a weak by coordinating with molecules to form a hydrated complex that partially dissociates. For instance, the hexaaquaaluminum(III) undergoes according to the equilibrium: [\ceAl(H2O)63+]+\ceH2O[\ceAl(H2O)5OH2+]+\ceH3O+[\ce{Al(H2O)6^{3+}}] + \ce{H2O} \rightleftharpoons [\ce{Al(H2O)5OH^{2+}}] + \ce{H3O^{+}} with an Ka=1.4×105K_a = 1.4 \times 10^{-5}. This reaction exemplifies amphoteric behavior in certain metal salts, where the cation's high promotes proton release, leading to an acidic solution. Basic hydrolysis is observed in salts of weak acids, such as carbonate salts like (Na₂CO₃), where the anion accepts a proton from . The reacts as follows: \ceCO32+H2OHCO3+OH\ce{CO3^{2-} + H2O \rightleftharpoons HCO3^{-} + OH^{-}} This equilibrium shifts the solution toward basicity, with the extent depending on the base dissociation constant of the anion. The degree of , denoted as hh, quantifies the fraction of salt that react with at equilibrium and is particularly relevant for salts of weak bases with strong acids. For such systems, under dilute conditions where h1h \ll 1, the approximate formula is hKaCh \approx \sqrt{\frac{K_a}{C}}
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