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Caesium hydroxide

Caesium hydroxide (CsOH) is an consisting of cations and anions, recognized as the strongest base among the hydroxides. It appears as a colorless to crystalline solid with a molecular weight of 149.91 g/mol and a of 272 °C. Highly hygroscopic and deliquescent, it readily absorbs from the air to form , which often contaminates commercial samples. Chemically, caesium hydroxide is extremely reactive and corrosive, neutralizing acids violently to produce salts and while reacting with certain metals like aluminum and to generate gas and metal oxides or hydroxides. It attacks and many metals, making it suitable for applications requiring strong , such as dissolving samples for analytical purposes when fused at high temperatures. With exceptional in —up to 395 g/100 mL at 15 °C—it forms a highly concentrated alkaline solution that is miscible with . Caesium hydroxide is primarily produced through the of aqueous solutions or by reacting caesium sulfate with , followed by to remove . Alternatively, hydrothermal leaching of using at 200–280 °C under yields a low-purity product that can be purified further. Notable applications include its use as an in alkaline storage batteries, particularly effective at subzero temperatures, and as a catalyst in , reactions, and the production of polyols for . It also serves as a precursor for other caesium salts, in , heavy oil desulfurization, and specialty glass manufacturing. Due to its (LD50 100 mg/kg in rats via ) and severe irritant effects on skin and eyes, handling requires strict safety precautions.

Properties

Physical properties

Caesium hydroxide appears as a colorless to yellowish deliquescent crystalline solid that is highly hygroscopic, rapidly absorbing moisture from the air to form hydrates. Due to this property, it is typically handled and stored as the monohydrate (CsOH·H₂O) in settings to prevent or unwanted reactions with atmospheric . The of anhydrous caesium hydroxide is 149.91 g/mol. Its is 3.68 g/cm³ at 25 °C. The form has a of 272 °C and decomposes upon strong heating without reaching a . Caesium hydroxide exhibits extreme in , dissolving at rates up to 300 g per 100 mL at 30 °C, reflecting the trend of increasing solubility down the hydroxide group. It is also soluble in and lower alcohols. The monohydrate form adopts a monoclinic crystal structure at low temperatures, transitioning to hexagonal above 229 K, characterized by layered polyanionic arrangements.

Chemical properties

Caesium hydroxide, with the chemical formula CsOH in its anhydrous form, dissociates completely in water to yield Cs⁺ and OH⁻ ions, behaving as a strong electrolyte. Among hydroxides, it exhibits the greatest basic strength owing to the large of Cs⁺ (167 pm), which leads to low and reduced of the cation in , thereby enhancing the reactivity of the OH⁻ ion. This results in a very low pK_b value of -1.76, indicative of nearly complete . Unlike certain metal hydroxides such as those of aluminum, caesium hydroxide shows minimal amphoteric tendencies and functions predominantly as a . As a strong base, it readily neutralizes acids to produce caesium salts and water; for instance, \ce{CsOH + HCl -> CsCl + H2O} This reaction exemplifies typical acid-base neutralization behavior. Caesium hydroxide also reacts with silica components in glass, leading to silicate formation: \ce{SiO2 + 2CsOH -> Cs2SiO3 + H2O} Such reactions occur under elevated temperatures, such as around 600–800 °C in hydrogen-steam atmospheres. Upon heating to high temperatures, it undergoes to caesium oxide and water: \ce{2CsOH -> Cs2O + H2O} This process highlights its instability at elevated temperatures. Although stable toward reactions in dry air, caesium hydroxide reacts with atmospheric CO₂ to form : \ce{2CsOH + CO2 -> Cs2CO3 + H2O} This carbonation contributes to its gradual degradation upon prolonged exposure to air.

Production

Industrial production

Caesium hydroxide is primarily derived from extracted from ore (CsAlSi₂O₆·0.5H₂O), the principal commercial source of the element, through processes such as or alkaline treatment. One key industrial process involves with to produce , followed by of the aqueous solution to directly yield caesium hydroxide solution, hydrogen gas, and chlorine gas:
$2\mathrm{CsCl} + 2\mathrm{H_2O} \rightarrow 2\mathrm{CsOH} + \mathrm{H_2} + \mathrm{Cl_2}
Subsequent filtration steps remove impurities, including compounds often co-extracted from the ore.
An alternative method employs direct reaction of with :
\mathrm{Cs_2CO_3} + \mathrm{Ca(OH)_2} \rightarrow 2\mathrm{CsOH} + \mathrm{CaCO_3}
This can be achieved via hydrothermal alkaline leaching of with at 200–280 °C under , yielding a low-purity caesium aluminate solution that is further processed to isolate caesium hydroxide.
High-purity caesium hydroxide is manufactured in small quantities, with global production of caesium compounds—including caesium hydroxide—limited to 5–10 metric tons per year due to the element's scarcity in economically viable deposits. Modern industrial approaches incorporate ion-exchange purification from or concentrates to achieve high purity, often followed by caustic fusion or alkaline decomposition to facilitate extraction and conversion to the form.

Laboratory synthesis

Caesium hydroxide can be prepared in the laboratory on a small scale by reacting caesium metal with under an inert atmosphere, such as , to control the highly and prevent oxidation of the metal prior to use. The reaction proceeds according to : $2\mathrm{Cs}(s) + 2\mathrm{H_2O}(l) \rightarrow 2\mathrm{CsOH}(aq) + \mathrm{H_2}(g) This process generates significant heat and hydrogen gas, necessitating cooling baths and proper ventilation to manage the vigorous evolution of gas and potential ignition risks. An alternative laboratory method involves the neutralization of caesium carbonate with barium hydroxide, leveraging the low solubility of barium carbonate to drive the metathesis reaction: \mathrm{Cs_2CO_3}(aq) + \mathrm{Ba(OH)_2}(aq) \rightarrow 2\mathrm{CsOH}(aq) + \mathrm{BaCO_3}(s) The barium carbonate precipitate is removed by filtration, yielding a caesium hydroxide solution suitable for further processing; this approach is particularly useful when starting from commercially available caesium salts. The monohydrate form, CsOH·H₂O, is obtained by dissolving anhydrous caesium hydroxide in water to form a concentrated solution, followed by controlled cooling or evaporation to induce crystallization; this hydrate is the stable form under ambient conditions and is commonly isolated as colorless crystals. Purity of the synthesized caesium hydroxide is verified using spectroscopic techniques, such as ¹³³Cs NMR, which confirms the characteristic for the hydroxide environment and detects potential impurities through comparison with reference spectra, as rubidium often co-occurs in caesium sources. Yields from the caesium metal reaction are near-quantitative, approaching 100% based on the , though practically limited by the scarcity and cost of pure caesium metal.

Uses

Industrial applications

Caesium hydroxide plays a key role in the and ceramics industry, where its strong basicity enables the of silica components at elevated temperatures, facilitating the formation of caesium silicates through fusion processes around 750 °C. This property is useful for analytical of samples, such as reference glasses used in testing. Additionally, it is incorporated into optical formulations to enhance such as electrical reduction and thermal stability, supporting applications in fiber optics and specialty ceramics. In chemical manufacturing, caesium hydroxide serves as a potent for reactions, including the promotion of chemoselective N-alkylation to produce secondary amines and the initiation of of oxiranes for production. Its superior basicity compared to makes it effective for in specialty chemical processes. It also acts as a key in the of other salts used in high-value intermediates for pharmaceuticals and . Furthermore, as a base , it supports the production of polyols essential for foams. It is used in developers. Within the , caesium hydroxide is utilized in molten form to desulfurize , removing sulfur compounds to meet standards and reduce environmental emissions. Its high contributes to formulations of fluids, where it helps control and in high-pressure environments, often as a precursor to cesium brines that enable stable wellbore conditions during . Due to the rarity and high cost of , the industrial consumption of caesium hydroxide remains confined to niche sectors. Annual production is closely linked to limited caesium mineral supplies, primarily from deposits (as of the early ), restricting broader adoption despite its specialized efficacy.

Research and niche uses

Caesium hydroxide serves as an anisotropic etchant in , particularly for fabricating (MEMS) from substrates. It exhibits high selectivity, preferentially etching p-doped over n-doped , which enables precise control in device structuring. Etching rates reach up to approximately 1 μm/min at elevated temperatures around 70–80 °C in concentrated solutions (50-65 wt% CsOH), with optimal selectivity ratios around 200:1 for specific crystal orientations under these conditions. In electrochemistry, caesium hydroxide functions as an electrolyte component in specialized batteries, including alkaline storage systems designed for subzero temperatures, where it supports ionic transport in aqueous configurations. Additionally, it acts as a precursor for synthesizing caesium-based ionic conductors, such as hydrated forms exhibiting superprotonic conductivity, with values approaching 10^{-2} S/cm at elevated temperatures above 100 °C. These properties stem from its ability to form proton-conducting phases in hydroxide hydrates, facilitating applications in solid-state electrochemical devices. In , caesium hydroxide promotes reactions such as the Favorskii rearrangement of α-halo ketones to carboxylic acids under conditions, leveraging its strong nucleophilicity. It also facilitates of weakly acidic compounds, including those with pK_a > 20, enabling additions and other carbon-carbon formations that weaker bases cannot achieve. Isotope studies utilize the ¹³³Cs nucleus (100% natural abundance, spin 7/2) in NMR spectroscopy of hydroxide solutions, where caesium hydroxide provides a reference for probing pairing, complexation, and dynamics in alkaline media, such as CsOH/H₂O systems at high (>13).

Safety and handling

Health hazards

Caesium hydroxide is a strong base that poses significant risks primarily due to its corrosivity and the toxicity of the caesium ion. It is classified under the Globally Harmonized System (GHS) as "Danger" with hazard statement H314, indicating it causes severe skin burns and eye damage upon contact. Exposure through skin or eye contact results in immediate , chemical burns, and potential tissue , while inhalation irritates the upper and mucous membranes. Its deliquescent nature allows it to absorb atmospheric moisture readily, forming concentrated solutions that heighten the risk of accidental exposure in humid environments. Ingestion of caesium hydroxide is harmful, with an oral LD50 of 570 mg/kg in rats, classifying it under GHS code H302 as harmful if swallowed. Symptoms typically include severe nausea, vomiting, abdominal pain, and diarrhea due to its caustic action on the gastrointestinal tract. Additionally, the caesium ions can interfere with potassium channels in cardiac cells, potentially leading to arrhythmias such as prolonged QT syndrome or ventricular tachyarrhythmias, as observed in cases of caesium compound ingestion. Inhalation of caesium hydroxide dust or mist irritates the lungs and , with the National Institute for Occupational Safety and Health (NIOSH) recommending a (REL) of 2 mg/m³ as a time-weighted average (TWA). Higher exposures can cause chemical burns to the , coughing, , and in severe cases, —a potentially life-threatening accumulation of fluid in the lungs. Chronic or repeated exposure to caesium hydroxide may result in organ , classified under GHS H373, with potential effects on the , adrenal glands, and testes. Long-term exposure has been linked to kidney through accumulation and interference with renal function. It is also suspected of causing (GHS H361), including reduced and effects on the unborn child, based on studies of compounds showing impacts on reproductive systems such as decreased counts. First aid for exposure requires immediate action to minimize damage. For skin or eye contact, flush the affected area with copious amounts of water for at least 15 minutes to dilute and remove the chemical; for skin exposure, a weak acid such as vinegar may then be applied to neutralize residual base after initial flushing. In cases of ingestion, do not induce vomiting; seek immediate medical attention. For inhalation, move the person to fresh air and provide respiratory support if breathing is difficult, followed by professional medical evaluation.

Environmental considerations

Caesium hydroxide (CsOH) is highly soluble in water, dissociating into caesium ions (Cs⁺) and hydroxide ions (OH⁻), which results in high mobility and rapid dispersion in aquatic environments. The Cs⁺ exhibits low adsorption to particles and sediments due to its large and weak binding affinity, facilitating its transport through and without significant retention. This persistence in the dissolved phase contributes to widespread distribution but limits long-term accumulation in sediments compared to less mobile metals. Caesium ions bioaccumulate in aquatic and terrestrial organisms, primarily because Cs⁺ mimics (K⁺) in biological uptake pathways, leading to incorporation into plant tissues and animal cells. In freshwater systems, factors for Cs in typically range from 100 to 1,000, depending on potassium concentrations and trophic levels, with higher uptake in low- waters. plants and algae show similar accumulation, serving as vectors for transfer through food webs, though (Cs-133) poses lower risks than radioactive isotopes like Cs-137. Ecotoxicity of caesium hydroxide to aquatic life is primarily driven by its rather than the itself, with low observed for dilute solutions. Studies indicate an LC50 of approximately 97 mg/L (96 h) for Danio rerio (zebra fish). Chronic exposure can disrupt potassium-dependent balances in organisms, potentially affecting and growth. like exhibit similar low sensitivity to Cs⁺, though elevated from OH⁻ can cause indirect stress in sensitive ecosystems. Under the European Union's REACH regulation, caesium hydroxide is registered with EC number 244-344-1 and classified as corrosive to metals (category 1) and skin/eye irritant, with specific handling requirements for environmental release. Disposal mandates neutralization to a pH of 7-9 using dilute acids before discharge into waterways, in compliance with local wastewater treatment standards; releases are monitored particularly for potential radioactive caesium isotopes from contaminated sources, though stable CsOH itself is not radioactive. In the United States, the EPA regulates caesium compounds under general hazardous waste guidelines, emphasizing containment to prevent alkaline runoff. For spill response, caesium hydroxide spills should be isolated immediately to at least 25-50 meters, contained with inert absorbents like or , and neutralized with non-reactive acids such as acetic acid, followed by dilution with . The compound is not flammable but reacts exothermically with , generating heat and potentially increasing hazards during cleanup. Global environmental impact from caesium hydroxide remains minimal owing to its low volume. As of 2024, U.S. consumption of cesium chemicals is estimated at no more than a few thousand kilograms annually, with global of cesium compounds on the order of tens of metric tons per year derived from limited pollucite ore . However, localized concerns arise in mining regions, such as Bernic Lake in , where of caesium-bearing ores can lead to alkaline and potential leaching into nearby aquatic systems if not properly managed. Overall, non-radioactive caesium use has negligible broad-scale ecological effects compared to more abundant industrial chemicals.

History and occurrence

Discovery and early development

The element caesium was discovered in 1860 by German chemists and through flame applied to from Dürkheim, where they observed a characteristic pair of blue spectral lines. This marked the first identification of an element using spectroscopy, a technique they had developed the previous year. Shortly thereafter, in 1861, Bunsen and Kirchhoff isolated small quantities of caesium salts, including the chloride, from the evaporated residues of the mineral water, laying the groundwork for subsequent compound preparations. Caesium hydroxide was first synthesized in the early 1860s by reacting caesium sulfate or with or , producing the highly soluble CsOH as a colorless crystalline solid. Limited early studies focused on its basic properties and reactivity, with initial applications centered on spectroscopic due to 's distinct lines. In 1882, Carl Setterberg isolated pure metal for the first time via of molten cyanide, providing a direct route for synthesizing purer hydroxide by with . Following , interest in compounds surged due to the prevalence of in products, prompting research into their chemical behavior for and reactor applications. Commercial production of began in the 1950s, derived from ore mined at Bernic Lake, Manitoba, , where the deposit contains up to 34% by weight. By the , ion-exchange methods were developed for purifying from complex mixtures, enhancing hydroxide yield for specialized uses. Early scientific investigations into caesium hydroxide's properties were documented in J.W. Mellor's 1936 supplement to his Comprehensive Treatise on Inorganic and , which summarized its , hygroscopic nature, and reactivity with , noting the scarcity of data owing to the element's rarity. In the 1970s, precise determination of its value (approximately 15.76 for the conjugate acid) confirmed caesium hydroxide as the strongest among common alkali hydroxides in , based on and studies.

Natural occurrence

Caesium is a relatively rare element in the Earth's crust, ranking as the 45th most abundant with an average concentration of approximately 3 parts per million (ppm). While caesium hydroxide (CsOH) itself is not stable under typical natural conditions due to its high reactivity and solubility, trace amounts of caesium ions (Cs⁺) can form transient hydroxide species in highly alkaline environments such as certain soils or waters, where pH exceeds 10 and hydroxide ions are abundant. These formations are fleeting, as CsOH readily dissociates or reacts further with atmospheric CO₂ to form carbonates. No direct deposits of caesium hydroxide exist in nature, as it does not precipitate stably from geological processes. The primary natural sources of caesium are concentrated in specific minerals, predominantly pollucite (Cs[AlSi₂O₆]·0.5H₂O), a rare zeolite found in lithium-rich granitic pegmatites. Notable deposits include the Bernic Lake (Tanco Mine) in Manitoba, Canada, and the Bikita pegmatite in Zimbabwe, which together represent the world's largest known accumulations of this mineral. Lepidolite, a lithium-bearing mica, serves as a minor source, containing up to several percent caesium oxide (Cs₂O) as an impurity substituting within its structure. Approximately 90% of the global supply of caesium is derived from pollucite mining, underscoring its geochemical concentration in these specialized igneous environments. Geochemically, behaves similarly to due to their comparable ionic radii (Cs⁺: 1.67 Å; K⁺: 1.33 Å, but effective in lattice substitution), allowing Cs⁺ to substitute for K⁺ in common minerals like feldspars (e.g., ) and micas (e.g., , ). This substitution disperses widely but at low levels in the continental crust. In and hydrothermal processes, soluble caesium species leach from these minerals into , brines, and hot springs, particularly in alkaline or saline settings where mobility increases. Trace caesium is ubiquitous in natural waters, with concentrations in seawater averaging about 0.3 parts per billion (ppb) as Cs⁺, derived from riverine input and oceanic circulation. Volcanic and geothermal hot springs, such as those in the southern Qinghai-Xizang Plateau, can exhibit elevated caesium levels (up to several ppb) due to alkali metal reactions with host rocks and magmatic fluids, potentially forming transient CsOH in highly basic conditions. These occurrences highlight caesium's role as a fluid-mobile element in Earth's geochemical cycles, though always at dilute concentrations far below those of industrial sources.