General Information
Cobalt (Co) is found with minerals containing a possible variety of elements (Ni, As, S, Fe, Cr, Cu, Pb, and Mn) as the oxide, sulfide, or arsenide, but is not found naturally occurring as the metal. Co is not mined directly, but is produced as a byproduct (mostly from Ni and Cu mining) of mining operations in Africa, the former Soviet Union, and North America.
Cobalt is an element that is low to moderately abundant in the earth's crust. Its abundance is roughly equal to that of scandium. Cobalt and scandium are the less abundant of the first row transition elements, making them both candidates as internal standard (IS) elements. Cobalt is not favored for its use as an IS for its complex spectrum, but rather for its compatibility with all of the common mineral acids and fluxes used in sample preparation.
The chemistry of cobalt allows for the use of a wide variety of preparation techniques and is typically included in methods intended for a large number and variety of elements. For example, it is easily included in EPA Method 3052 "Microwave Assisted Acid Digestion of Siliceous and Organically Based Matrices," which uses combinations of nitric, hydrochloric, and hydrofluoric acids heated in a Teflon bomb up to temperatures of around 180 °C; acid digestions in quartz or borosilicate glass using combinations of HNO₃, HCl, H₂SO₄, and H₂O₂; as well as in dry ashing and fusions using a wide variety of crucible materials, ashing aids, and fluxes. The main, and possibly only, thing to avoid with sample preparations is formation of the oxide in dry ashing procedures.
Cobalt is one of the ferrous metals (Fe, Co, Ni, from old Table Group VIII of the extended periodic table), having properties that are very similar to Fe and Ni. Co can have oxidation states of -1, 0, +1, +2, +3, and +4. The -1 oxidation state is encountered, for example, in "oxo process" catalysts [Co(CO)₄⁻], where Co is in a high-temperature reducing atmosphere. The 0 oxidation state will be found in a variety of alloys, such as high-speed steels (for example, steels used for cutting and drilling), cemented carbides (WC is cemented with either Co or Ni metal to make it less brittle), and Co-based super alloys. Cobalt metal is rapidly dissolved at room temperature by nitric acid, which is not the case for Fe and Ni, which both require heat. The +1 and +4 oxidation states are uncommon. Cobalt is most commonly found in the +2 oxidation state. The +2 state is the final oxidation state after sample preparation and acidification of samples containing Co in any of the possible oxidation states, using conventional sample methods. The +3 oxidation state is more stable when complexed, but uncomplexed is very unstable, with a high (1.4V) reduction potential, making it a very powerful oxidizing agent. In general, sample preparations for Co are similar to those for Fe and Ni and are relatively simple compared to the rest of the Group VIII elements (i.e., the precious metals). Sample preparations for ICP measurements typically take Co in the 0 or +2 oxidation states to solutions of Co²⁺ in dilute nitric acid matrices. Further discussion will be confined to these oxidation states.
The Oxides
Cobalt has two oxides that are more commonly encountered in conventional sample preparation schemes, namely CoO and Co₃O₄. CoO, which is grey-green, can be obtained by heating the sample to temperatures in excess of 1000 °C. This temperature is generally considered unnecessarily high in sample dry ashing preparations. More commonly, samples are ashed at temperatures in the 450 to 500 °C range, typically described as a dull red heat. Under these conditions, the black Co₃O₄, which is the most stable of the oxides, is formed. The cobalt(II, III) oxide, or cobalt tetraoxide, is refractory toward dissolution in dilute acids at room temperature or with heating.
Compounds and Salts of Co(II)
Co(II) arsenate, carbonate, hydroxide, iodate, phosphate, sulfide, borate, oxalate, and cyanide are insoluble in water, whereas the chloride, nitrate, fluoride, and sulfate are all quite soluble. Consequently, typical acid digestions are not hampered by samples containing large amounts of cobalt in moderate to small volumes.
The hydroxide is commonly encountered in sample preparations of Co. The Co²⁺ ion has been shown to form mononuclear hydrolysis products ranging from Co(OH)⁺ to Co(OH)₄²⁻. The solubility product of Co(OH)₂↓ is ~10⁻¹⁵. Precipitation doesn't begin until a pH of 6.4. The use of EDTA is most effective in keeping Co²⁺ in solution at pHs of 6.5 to 13 (Log K_CoEDTA = 16.3). Other common ligands and chelates that extend the solubility pH range, although not as effectively as EDTA, are acetylacetonate, ammonia, citrate, ethylenediamine, and tartrate.
Sampling and Handling
Co is used in alloys to impart wear resistance and high-temperature hardness, but there is not a great risk of contamination when using stainless steel. However, it is always advised that the analyst know the composition of the steel or alloy coming in contact with the sample. For example, grinding equipment and WC mills may use Co as a binding agent. For the most part, clean rooms or special handling equipment are not required. Biological materials with ultra-trace amounts of cobalt may be handled with stainless steel or other metallic devices, such as spatulas and scalpels. The composition of any biological materials should be known before approval for use in the sample handling/preparation apparatus/device. The following considerations apply:
- If the tools that you plan to use to pulverize, mix, cut, etc., contain Co or have an unknown composition, then attempt to use devices made of ceramics, silica/quartz, and polymers where possible.
- Many polymers, such as Teflon, have been exposed to alloys (cutting/pulverizing) prior to molding. As a precaution, new plastic and Teflon containers should always be acid-leached to remove possible contamination from a variety of elements.
- The collection of biological samples is also at risk of contamination, due to the very low (ppt) levels of Co sought. The use of steel needles, scalpels, or any metallic object that may contain Co should be avoided.
For more on sample contamination risks, see chapters eight, nine, and ten of the Inorganic Ventures Trace Analysis Guide.
For general information on sampling and subsampling, see Sampling and Subsampling.
The Metal and Alloys
Metal
Unlike Fe and Ni, Co metal dissolves readily at room temperature using 1:1 nitric acid. Heating is never required and, in fact, may cause the reaction to get out of control. If the metal is a powder, exercise caution, since the reaction will be quite vigorous.
Alloys
The use of dilute 1:1 nitric acid is commonly used for cobalt alloys. Heating is typically required, and the use of a microwave can greatly speed the reaction. An impressive 1:1:1 mixture of HNO₃ + HF + H₂O is used to dissolve high-temperature alloys of Fe/Co/Cr/Ti/Al/Mo/Ta/Hf (use 10 mL mixture/0.2 grams sample).
Oxides and Ores
Oxides
As a general rule, both grey and black cobalt oxides are soluble in hot HCl, if they have not been ignited. If the oxides are insoluble in HCl, then fusion with potassium bisulfate or sodium carbonate in a Pt crucible is required. The following is a general guide for carbonate fusions:
- Make certain that the sample is well mixed with the sodium carbonate.
- A 5-9's pure sodium carbonate is recommended and available from E.M. Science.
- Mix the sample with the flux at no more than a 1:20 ratio. Typical sample-to-flux ratios are in the 1:10 area.
- If organic matter is present, either initially mix the sample with the flux and heat slowly to 500 °C for ~2 hours before bringing up to full temperature, or pre-ash the sample at 500 °C and then mix the ash with the flux.
- Use Pt as the crucible container material.
- Perform the fusion at 1000 °C in a muffle furnace. Avoid flames, since this fusion is difficult to perform in a flame due to the high melting point of the sodium carbonate.
- Most fusions are complete in 15 minutes, but some require up to 45 minutes.
- Dissolve the fuseate in dilute HCl (1:1).
Ores
The ores containing cobalt vary widely in their chemical nature, making it difficult to present a method for all types. All sample types should be pulverized to pass an 80 to 100 mesh sieve. Sulfides and ores containing organic matter can be mixed with sodium carbonate and ashed in a Pt crucible at 500 °C for one hour, prior to bringing to a temperature of 1000 °C, as described below. If the ore has already been strongly ignited, you can go directly to 1000 °C with sodium carbonate (see above procedure). When a sodium carbonate fusion is performed, HF is not needed, unless silica content is high (silicates formed from the carbonate fusion are soluble, but do not heat the fuseate to dissolve, since this will bring about the formation of polysilicic acid, which is a gelatinous precipitate). This approach is applicable to many types of ores, including sulfides, ores containing organic matter, oxides, and ores containing silica.
Organic Matrices
Ashing of organic materials, foodstuffs, plant, and blood and sewage sludge, as a preliminary decomposition step, is not suggested for samples containing Co, unless an ashing aid such as sodium carbonate is used and the crucible material is Pt. If magnesium nitrate is used as the ashing aid, then porcelain or quartz crucibles are acceptable. Conventional dry ashing procedures will result in the formation of a refractory form of cobalt oxide, unless there is a significant amount of one or more elements from Groups I, II, or III. If ashing is used, it is suggested to keep the temperature low (400 to 450 °C max) and to use an ashing aid, such as high-purity sodium carbonate or magnesium nitrate. If the sample is high in silica, subsequent fusion of the ash with sodium carbonate (see above for procedure), or heating of the ash to fumes with sulfuric and hydrofluoric acids, is suggested.
The acid digestion of organic samples containing Co is also very common. Co does not offer any unusual challenges over the other elements. There are numerous oxidative acid digestion procedures available that are tailored to the matrix.
For more on acid digestion, please see the following paper: Acid Digestions of Organic Samples