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Ammonium oxalate

Ammonium oxalate is an consisting of cations and anions in a 2:1 ratio, with the (NH₄)₂C₂O₄. It typically occurs as a colorless or white, odorless crystalline solid, often in the monohydrate form ((NH₄)₂C₂O₄·H₂O), and is highly soluble in at approximately 4.5 g/100 mL at 20°C. The compound has a molecular weight of 124.1 g/mol for the form and 142.11 g/mol for the monohydrate, a of 1.5 g/cm³, and decomposes upon heating at around 70°C without a distinct . As a and , ammonium oxalate is widely used in settings to precipitate calcium ions as insoluble for of calcium in samples. In , it serves to extract iron and aluminum from poorly crystalline minerals, aiding in geochemical assessments. Industrially, it finds applications in and processing, metal and removal, electrolytic detinning of iron, and the manufacture of explosives and other oxalates. Ammonium oxalate is considered hazardous, being due to its potential to disrupt calcium balance and affect the kidneys, and it acts as an irritant to the skin, eyes, and . It reacts with strong oxidants and may form combustible dust in air, necessitating careful handling with protective equipment and storage away from incompatible materials. Despite its , its role in precise analytical and underscores its importance in chemistry and .

Physical and chemical properties

Physical characteristics

Ammonium oxalate typically exists as a monohydrate, (NH₄)₂C₂O₄·H₂O, appearing as a colorless or white, odorless crystalline powder or solid. The monohydrate form has a of 142.11 g/mol and a of 1.50 g/cm³. It does not melt upon heating but undergoes initial incomplete in the range of 105–130 °C, with rapid decomposition initiating around 215 °C and completing by 265 °C, releasing gases such as , , , and . Ammonium oxalate monohydrate exhibits high solubility in , approximately 4.5 g per 100 mL at 20 °C, while it is only slightly soluble in and insoluble in . The crystal structure of the monohydrate is orthorhombic, belonging to the P2₁2₁2₁, characterized by hydrogen-bonded networks involving ions, ions, and molecules. Thermodynamically, the (ΔH_f°) for ammonium oxalate monohydrate is -1425.5 kJ/mol.

Chemical reactivity

Ammonium oxalate is stable under normal storage and handling conditions, remaining unchanged at in dry environments. However, it decomposes in the presence of strong acids or bases; in strong acidic media, the component can protonate and release , while in strong basic conditions, occurs gradually, leading to the formation of and species. Upon heating, ammonium oxalate undergoes , releasing gas (NH₃), (CO), (CO₂), and (H₂O). The overall reaction for the monohydrate can be represented as: \ce{(NH4)2C2O4 \cdot H2O -> 2NH3 + CO + CO2 + 2H2O} This process typically initiates around 215°C and completes by 265°C, with the gaseous products confirming the breakdown of both the ammonium and oxalate moieties. In aqueous solutions, ammonium oxalate undergoes complete dissociation into ammonium cations (NH₄⁺) and oxalate anions (C₂O₄²⁻), as expected for an ionic of a and . Subsequent partial occurs, where the oxalate acts as a (derived from with pKₐ values of 1.25 and 4.14) and the ammonium as a (pKₐ = 9.25), resulting in a near-neutral solution around 6.5–7.0. The compound exhibits reducing properties primarily due to the oxalate ion, which can donate electrons in reactions, often generating as a byproduct; for instance, it reacts rapidly with oxidizing agents like . Ammonium oxalate participates in precipitation reactions with various metal ions to form insoluble oxalates, such as (CaC₂O₄) upon addition to solutions containing Ca²⁺, a key step in qualitative inorganic analysis for identifying calcium.

Synthesis and production

Laboratory synthesis

Ammonium oxalate is commonly synthesized in the laboratory through the neutralization of with an , typically ammonium hydroxide. The reaction proceeds as follows: \mathrm{H_2C_2O_4 + 2NH_3 \rightarrow (NH_4)_2C_2O_4} To perform this synthesis, approximately 0.5 g of is weighed and dissolved in water, then gently heated to around 50°C. Concentrated is added dropwise with stirring, using an indicator such as to monitor the endpoint until the solution turns pink, indicating neutralization. The mixture is then filtered to remove any undissolved impurities. An alternative laboratory method involves reacting with . The balanced equation for this process is: \mathrm{(NH_4)_2CO_3 + H_2C_2O_4 \rightarrow (NH_4)_2C_2O_4 + H_2O + CO_2} In practice, 100 g of is dissolved in 800 mL of and gently warmed, followed by the addition of about 83 g of until neutralization is achieved, often monitored by pH adjustment to approximately 7 using a or suitable indicator. gas evolves during the reaction, which is vented safely. The solution is filtered, and the filtrate is concentrated by to promote . Following by either method, the crude ammonium oxalate is purified by recrystallization from hot to isolate the monohydrate form, (NH₄)₂C₂O₄·H₂O, as colorless . The solid is dissolved in the minimum volume of boiling , filtered while hot to remove insoluble impurities, and then slowly cooled to or below to allow formation. The are collected by , washed with or , and dried. This step enhances purity by exploiting the compound's , which is higher in hot than in (about 4.3 g/100 mL at 20°C). These procedures are typically conducted at after initial warming, with controlled to neutrality (around 7) to ensure complete reaction and avoid excess acidity or basicity. Yields are generally high, ranging from 80-90%, depending on the precision of neutralization and purification steps.

Commercial production

Ammonium oxalate is commercially produced on an industrial scale primarily through the neutralization of with gas or ammonium hydroxide solution in large-scale reactors, following the reaction \mathrm{H_2C_2O_4 + 2NH_3 \rightarrow (NH_4)_2C_2O_4}, with the monohydrate (NH₄)₂C₂O₄ · H₂O formed upon subsequent , , , and optional recrystallization for purification. , the key precursor, is mainly manufactured via microbial using the fungus on carbohydrate substrates such as glucose or , yielding up to several grams per liter under optimized conditions, though chemical oxidation methods like treatment of are also employed in some facilities. This process is scaled up from methods but emphasizes continuous reactors and automation for efficiency, often integrated into oxalic acid production plants rather than as a direct byproduct of unrelated ammonia-based processes. Although ammonium oxalate occurs naturally in plants such as , , and , where it forms as a metabolic product, commercial extraction from these sources is limited and not economically viable due to low yields and complex purification requirements. Historically, processing of deposits—rich in including ammonium oxalate as the oxammite—provided a source of such salts for and chemical applications in the , but this has been superseded by synthetic methods. Global production is handled by specialized chemical manufacturers, primarily in regions like and , with major suppliers including companies that distribute to industrial and laboratory markets. Commercial ammonium oxalate is available in several purity grades tailored to end-use requirements: technical grade at approximately 98-99% purity for general applications, analytical (AR) grade at ≥99.5% for precise chemical analyses, and trace-metal-free variants at ≥99.99% purity to minimize contamination in sensitive processes. The monohydrate form, (NH₄)₂C₂O₄ · H₂O, predominates in commercial products due to its stability and ease of handling.

Uses

Analytical applications

Ammonium oxalate plays a key role in , particularly for the quantitative determination of calcium in various samples. The procedure involves adding a of ammonium oxalate to a neutral or slightly acidic sample containing calcium ions, which precipitates as monohydrate (CaC₂O₄·H₂O), an insoluble compound with low that ensures complete . The white precipitate is then filtered, washed to remove impurities, dried at 100–110°C, and weighed; the mass is used to calculate calcium content based on the stoichiometric ratio. This method achieves high accuracy, with typical recoveries exceeding 99% when performed under controlled conditions to avoid co-precipitation of other ions. Ammonium oxalate is used as an in sample collection and preservation, where it binds calcium ions to inhibit the clotting cascade, allowing for analysis of components without . In qualitative analysis, ammonium oxalate serves as a for detecting specific metals through reactions. For calcium, it produces a white, crystalline precipitate of that is insoluble in acetic acid, distinguishing it from other alkaline earth metals like magnesium. Similarly, lead forms a white precipitate of lead(II) , useful in identifying lead in complex mixtures after separation from interfering ions. For rare earth elements, ammonium oxalate precipitates them as insoluble oxalates, enabling their isolation and subsequent quantification in samples. These tests leverage the selective insolubility of metal oxalates, often performed in ammoniacal solutions to control and enhance specificity. Ammonium oxalate is also employed in for extracting amorphous and poorly crystalline forms of iron and aluminum oxides, which are critical for understanding and . The method, known as Tamm's acid ammonium oxalate extraction, uses a buffered of 0.2 M ammonium oxalate and 0.2 M adjusted to pH 3.0–3.3, which selectively dissolves these non-crystalline phases without significantly affecting crystalline minerals like or . The extract is analyzed by or to quantify Fe and Al contents, providing insights into pedogenic processes; for example, high oxalate-extractable Fe indicates active in podzolic soils. This technique minimizes interference from when performed in the dark to prevent photochemical reduction. The analytical applications of ammonium oxalate originated in the 19th century, coinciding with the development of systematic gravimetric and qualitative methods in by chemists such as , who refined techniques for accurate elemental quantification. By the mid-1800s, had become a standard for calcium in geological and biological samples, evolving into modern protocols like Tamm's method in the early for studies.

Industrial applications

Ammonium oxalate serves as a versatile compound in various , particularly where its chelating and reducing properties facilitate material treatment and synthesis. In the , it functions as a to enhance fixation on fabrics, improving colorfastness and binding strength during operations. This application leverages its ability to form stable complexes with metal ions, aiding in the even distribution and permanence of on fibers. In , ammonium oxalate is incorporated into formulations to remove , scale, and oxidation from surfaces, restoring metallic luster through its rust-complexing action. It is particularly effective in electrolytic detinning processes for iron and in general metal surface treatments, where it dissolves iron oxides without excessive abrasion. The compound plays a role in explosives manufacturing as an in the production of safety explosives and as a burn rate moderator in ammonium-based propellants and detonators. Its reducing properties contribute to controlled combustion rates in solid rocket formulations. Additionally, ammonium oxalate finds application in leather processing as an agent in tanning and treatment stages, helping to stabilize hides and improve finish quality. Its chelating effects assist in removing impurities and enhancing the penetration of tanning agents into leather matrices.

Biological and geological occurrence

Biological role

Soluble oxalates, such as sodium and oxalates, occur naturally in , synthesized from . These accumulate particularly in vegetables like (Spinacia oleracea), (Rheum rhabarbarum), and sorrel (Rumex acetosa), where they contribute to a defense mechanism against herbivory by deterring feeding through toxicity and crystal formation. In these , total oxalate concentrations can reach up to 1% of dry weight, with exhibiting levels as high as 2350 mg per 100 g fresh weight, predominantly as insoluble but including soluble variants that enhance overall antinutritional effects. In vertebrates, oxalate is produced endogenously through the metabolism of glyoxylate, a key intermediate derived from pathways such as degradation or from the breakdown of ascorbic acid (). Glyoxylate is primarily converted to oxalate by enzymes like in the liver and other tissues. This oxalate is not further metabolized but is primarily eliminated via the kidneys, often forming various salts, with normal urinary levels of total oxalate ranging from 10 to 40 mg per day in humans, reflecting a balance between endogenous synthesis and dietary intake. Excess urinary contributes to the formation of crystals, a primary component of stones in vertebrates, particularly when exceeds limits influenced by factors like urinary and calcium concentration. Ammonium oxalate is not a primary metabolic intermediate in mammals, which detoxify via the . High concentrations of ammonium oxalate are also prominent in , the accumulated excrement of birds and bats, arising from their uric acid-based where oxalate combines with ammonium during waste processing. In deposits, such as those from , ammonium oxalate comprises up to 17.7% of the composition, while bat guano similarly features elevated levels reaching several percent, supporting nutrient-rich ecological roles in and fertilization.

Mineral forms

Oxammite, with the chemical formula (NH₄)₂C₂O₄·H₂O, is the primary natural mineral form of ammonium oxalate, recognized as an derived from deposits. It was first described in 1870 from guano in the Virú Province, La Libertad Region, , marking its initial identification in subfossil eggs and on subfossil birds. This rare typically forms through precipitation in ammonia-rich environments created by the decomposition of bat or guano under arid conditions, often in caves or dry deposits where accumulates without significant alteration. It is commonly associated with other ammonium-bearing minerals such as mascagnite ((NH₄)₂SO₄), reflecting shared origins in guano-derived geochemical systems. Physically, oxammite occurs as colorless to pale yellow crystals, transparent in transmitted light, with a white streak. It exhibits distinct on {001}, belongs to the , and has a Mohs hardness of 2.5, making it relatively soft. The specific gravity is measured at 1.5, consistent with its hydrated, low-density structure. Occurrences of oxammite are exceedingly rare and limited to specific -rich sites in arid or settings. The type locality remains the Guañape Islands off , with additional verified finds in bat at the Murra Mine, , , and , , , . It has also been reported from the near , . As a pre-1959 description, oxammite holds grandfathered status under International Mineralogical Association (IMA) guidelines, without a formal approval process post-1959. Its biological origin traces to the breakdown in , leading to formation in hyperarid conditions.

Health and safety

Toxicity profile

Ammonium oxalate exhibits moderate upon , with an oral LD50 value of 375 mg/kg in female rats, determined by analogy to similar compounds. Exposure can cause gastrointestinal distress, including , , and , as well as systemic effects such as leading to muscle cramps and . In severe cases, it may result in convulsions, , or due to renal impairment from crystal formation in the kidneys. Dermal and routes also pose risks, with potential for and absorption contributing to overall , though dermal LD50 exceeds 2,000 mg/kg in rats; no specific LD50 is available for . Chronic exposure to ammonium oxalate primarily manifests as , potentially progressing to renal failure through repeated deposition of crystals in the renal tubules. It acts as an irritant to the skin, causing redness and upon prolonged contact; to the eyes, leading to corneal and severe ; and to the , where of dust may induce coughing, , and in high concentrations. Long-term effects may also include disruptions in , exacerbating cardiovascular and neurological issues. The primary mechanism of toxicity involves oxalate ions chelating calcium to form insoluble calcium oxalate crystals, which precipitate in the kidneys and impair , leading to acute and renal damage. The component contributes additional irritation to mucous membranes and respiratory tissues, potentially releasing upon decomposition and enhancing local corrosive effects. Solubility in aqueous media facilitates gastrointestinal absorption, influencing the rate of systemic exposure. Under the Globally Harmonized System (GHS), ammonium oxalate is classified as harmful if swallowed (, Oral, Category 4; H302). No specific OSHA (PEL) exists for ammonium oxalate; the general PEL for nuisance dust is 5 mg/m³ (respirable fraction) as an 8-hour time-weighted average.

Handling and environmental considerations

Ammonium oxalate should be stored in tightly closed containers in a cool, dry, and well-ventilated area to prevent and potential , which could release gas; it must be kept away from incompatible materials such as strong oxidizers, acids, and metals like iron or lead to avoid violent reactions or . Safe handling requires the use of , including gloves, safety goggles, and protective clothing to prevent skin and eye contact; respiratory protection with a P2 filter is recommended when dust is generated to avoid inhalation, and work should be conducted under a . In case of exposure, measures include immediately flushing affected eyes or skin with plenty of water for at least 15 minutes and removing contaminated clothing, while necessitates rinsing the mouth, if conscious, and seeking immediate medical attention. For spills, the area should be evacuated, ventilated, and the material collected using non-sparking tools into sealed containers for disposal, followed by washing the site with water; disposal must follow local, state, and federal regulations, treating it as due to its , potentially under the (RCRA) if it exhibits characteristic hazards, without allowing entry into sewers or waterways. Environmentally, ammonium oxalate has low persistence in soil due to rapid microbial biodegradation, with up to 89% degradation observed within 20 days, primarily through oxalotrophic and fungi that mineralize to ; however, its high allows of ions into and surface waters, where it may affect aquatic organisms by chelating metals and altering , though is relatively low (EC50 >33 mg/L for ).

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