Actinium
minorActinium is measurable in water only as the natural radionuclide Ac-227 at attograms per kilogram, released from deep sea sediments and used as a tracer of deep ocean mixing; it has no guideline of its own and no treatment role, and falls under gross alpha in drinking water rules.
Typical wastewaters
- uranium ore refining raffinate (pitchblende digestion residues, St. Louis airport site and Weldon Spring raffinate pits) Ac-227 with Pa-231 and Th-230 in the raffinate, the filtered solids and slurry left after uranium extraction, stored as AM-7 cake and in raffinate pits source term for ore in equilibrium: Pa-231 and Ac-227 each at 0.02 of the uranium activity, 0.01 of total alpha; for raffinate work the non-uranium alpha is apportioned 94.6 percent Th-230 and 5.4 percent Ac-227; a residue slurry rather than a discharged liquid, and no activity per litre was read
1 · Identity
- Symbol, number
- Ac, 89
- Oxidation states in water
- +3 only (Ac³⁺), a heavier lanthanum; only radioactive isotopes
- Note
- Ac-227 (half-life 21.8 years) is the actinium of natural water, produced by decay of Pa-231 (half-life 32,760 years), itself from U-235; Pa-231 adsorbs to particles and settles, then its Ac-227 daughter is released to the overlying water because actinium is the more soluble of the two.
2 · Occurrence in water
- Natural sources
- Ac-227 in the ocean: at secular equilibrium with dissolved Pa-231 in mid water, in excess near the seafloor from sediment release (an excess reaching 1.0 dpm/m₃ in the North Atlantic section), and from hydrothermal vents (up to 1.44 dpm/m₃ in a neutrally buoyant plume). Activities are low: below 0.4 dpm/m₃ along the North Atlantic GA₀₁ section, 0.02 to 0.4 dpm/m₃ for most samples, 0.6 and 1.1 dpm/m₃ near the seafloor; 0.05 to 2.68 dpm/m₃ in other basins and 0.1 to 4.8 dpm/m₃ in the compilations cited. In mass terms: below the detection limit of about 0.5 ag/kg in South China Sea surface water, 3.4 ag/kg at 2760 m, 4.2 to 10.9 ag/kg in the Weddell Gyre; 4.1 to 6.1 ag/kg in the Vienne river, France. Actinium also follows uranium into ore, tailings and phosphate rock (book entry).
- Anthropogenic sources
- None read; Ac-225 and Ac-227 medical and research uses are in the book entry, without a water pathway.
| matrix | typical range | note |
|---|---|---|
| seawater, North Atlantic (GA₀₁ section) | 0.02 to 0.4 dpm/m3 activity, not mass; 2014 section | most samples; 0.6 and 1.1 dpm/m₃ near the seafloor; excess over Pa-231 up to 1.0 dpm/m₃ |
| seawater, South China Sea and Weddell Gyre | below 0.5 to 10.9 ag/kg | below detection at the surface, 3.4 ag/kg at 2760 m in the South China Sea; 4.2 to 10.9 ag/kg in the Weddell Gyre |
| river water (Vienne, France) | 4.1 to 6.1 ag/kgone river, two samples | duplicates used as a method quality control |
3 · Speciation
Ac³⁺ behaves as a soluble trivalent cation, more soluble than its parent Pa-231, which is particle reactive; that difference is the source of the excess Ac-227 in bottom water. No speciation model for actinium in natural water was read.
| condition | dominant species | note |
|---|---|---|
| deep ocean, near the seafloor | dissolved Ac-227 released from sediment Pa-231 decay | excess over the water column Pa-231 support up to about 500 m above the bottom |
- Solubility
- Ac(OH)₃ is precipitated by ammonia and is less soluble than radium hydroxide (book entry); at ag/kg no solid controls it in nature.
- Hydrolysis
- Ac³⁺ hydrolyses to Ac(OH)₃ (book entry); no constant read.
- Complexation
- not read
- Precipitates
- none at natural levels; co-precipitated with manganese oxide in the analytical method
4 · Role in treatment
Not relevant or not given for this element.
5 · Removal and control
Not relevant or not given for this element.
6 · Analytics
| method | standard | detection limit | note |
|---|---|---|---|
| radium delayed coincidence counting (RaDeCC) of Ac-227 via its Rn-219 and Po-215 daughters after manganese fibre or cartridge adsorption | research method (Shaw and Moore 2002, as applied by Le Roy et al. 2023) | not stated as a number; hundreds of litres pumped at 3 to 6 L/min through 0.8 µm filters then manganese cartridges | Pa-231 must be measured or interpolated to compute the excess |
| isotope dilution MC-ICP-MS with an Ac-225 spike milked from Th-229, manganese co-precipitation and chromatographic purification | research method (Levier et al. 2021) | about 0.5 ag/kg for 30 L; sample size 10 to 30 L | measures Pa-231 from the same sample |
- Sampling pitfalls
- Volume: tens of litres at least, hundreds for counting methods. Separate Ac-227 supported by dissolved Pa-231 from the excess released by sediments; near-bottom and hydrothermal samples carry the excess.
7 · Regulatory limits
Limits change, and many are set locally. Treat these as the published values to start from, not as your compliance target: check the standard in force at your site and the numbers written into your own permit.
| body | limit | note |
|---|---|---|
| US EPA National Primary Drinking Water Regulations | not regulated | no actinium entry; Ac-227 and its alpha emitting daughters count toward the gross alpha MCL of 15 pCi/L |
8 · Health and environmental effects
- Toxicity
- Radiological only; about 150 times as active as radium (book entry). No chemical toxicity data were read.
- Bioaccumulation
- not read
- Ecotoxicity
- not read
Flags
- Seawater activities are from one North Atlantic section (2014) and a few Pacific and Southern Ocean stations; the river figure is two quality control duplicates.
- Geibert 2002 and Nozaki 1984 are cited by title only, through the two papers read.
Gaps
- No actinium measurement in groundwater, mine water or uranium mill effluent was read.
- WHO GDWQ radiological screening and EU DWD Annex I Part D were not read this session.
- No removal data for actinium in water treatment were read.
Sources
Le Roy, E. et al., The distribution of 227Ac along the GA01 section in the North Atlantic, Marine Chemistry 248 (2023) 104207 (author manuscript, Archimer)
Levier, M. et al., Determination of low level of actinium 227 in seawater and freshwater by isotope dilution and mass spectrometry, Marine Chemistry 233 (2021) 103986 (abstract via Semantic Scholar)
Geibert, W. et al., Actinium-227 as a deep-sea tracer: sources, distribution and applications, Earth and Planetary Science Letters 198 (2002) 147 to 165 (title only; not read)
Nozaki, Y., Excess 227Ac in deep ocean water, Nature 310 (1984) 486 to 488 (title only; not read)
US EPA, National Primary Drinking Water Regulations (table of regulated contaminants; no lanthanide, rare earth or actinium entry; gross alpha 15 pCi/L)
ORAU Team Dose Reconstruction Project for NIOSH, Basis for Development of an Exposure Matrix for the Mallinckrodt Chemical Company St. Louis Downtown Site and the St. Louis Airport Site, St. Louis, Missouri, ORAUT-TKBS-0005 Rev. 03 (2010), sections 1 to 2 (raffinate residues) and Appendix A total alpha source term factors
Identity
- Name and symbol
- Actinium, Ac
- Atomic number
- 89 protons
- Position
- no group (f-block) · period 7 · f-block · actinide
- CAS number
- 7440-34-8
Atomic structure
- Atomic mass
- 227 u
- Electron configuration
- 1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹⁴ 5d¹⁰ 6p⁶ 7s² 6d¹
[Rn] 7s²⁶d¹ - Electrons per shell
- 2, 8, 18, 32, 18, 9, 2
- Valence electrons
- 3 ns, (n-1)d and (n-2)f
| nuclide | half-life | decay |
|---|---|---|
| 227Ac | 21.772 y | β-=98.62±3.6%; α=1.38±3.6% |
| 225Ac | 9.9190 d | α=100%; 14C=5.3e-10±1.3% |
| 226Ac | 29.37 h | β-=83±0.3%; ε=17±0.3%; α=0.006±0.2% |
| 228Ac | 6.15 h | β-=100% |
Physical properties
- State at room temperature
- Solid
- Melting point
- 1,324 K (1,050.85 °C)
- Boiling point
- 3,471 K (3,197.85 °C)
- Density
- 10.07 g/cm3
- Appearance
- silvery-white, glowing with an eerie blue light; sometimes with a golden cast
- Thermal conductivity
- 12 W/(m·K)
- Electrical resistivity
- not in sources
- Electrical conductivity
- not in sources
- Crystal structure
- face-centered cubic
- Molar heat capacity
- 27.2 J/(mol·K)
Chemical properties
- Oxidation states
- +3
- Electronegativity
- 1.1 (Pauling Scale)
- Ionisation energy
- 5.17 eV
1st 499, 2nd 1,170 kJ/mol - Electron affinity
- not in sources
- Atomic radius
- empirical 215, covalent 215, van der Waals 260 pm
- Ionic radius
- not in sources
- Reactivity
- The first actinide, chemically a heavier lanthanum: +3 in every known compound, colourless Ac3+ in solution, and lattice constants within a few percent of the lanthanum analogues; its intense radioactivity (it is about 150 times as active as radium) limits the number of compounds that have been characterised.
- with water
- Reacts rapidly with moisture, the air-exposed metal growing a white oxide coating; in solution Ac3+ hydrolyses to the hydroxide Ac(OH)3, which ammonia precipitates and which is less soluble than radium hydroxide.
- with oxygen, air
- Reacts rapidly with oxygen in air to a white coating of the sesquioxide: , which protects the metal from further oxidation.
- with acids
- Dissolves in hydrochloric and nitric acid to Ac3+ solutions, from which the chloride AcCl3, the nitrate Ac(NO3)3 and the insoluble phosphate are obtained; nitric acid solutions serve the ion exchange separation from radium.
- with halogens
- No direct reaction of the metal with a halogen is reported; the trihalides AcF3, AcCl3 and AcBr3 and the oxyhalides AcOF, AcOCl and AcOBr are known, made from the oxide or hydroxide with the hydrogen halide.
- Typical compounds
- Ac₂O₃ actinium(III) oxide white protective coating on the metal
- AcF₃ actinium(III) fluoride reduced with lithium vapour to make the metal
- AcCl₃ actinium(III) chloride from hydrochloric acid solutions
- Ac(NO₃)₃ actinium(III) nitrate soluble salt of the nitric acid separations
- AcPO₄ actinium(III) phosphate white insoluble hemihydrate from phosphate solutions
- Ac₂S₃ actinium(III) sulfide black, from the oxalate and hydrogen sulfide at 1400 C
Occurrence, production and use
- Crustal abundance
- 5.5×10-10 milligrams per kilogram
- Oceanic abundance
- Not Applicable
- Occurrence and sources
- actinium-227 in uranium ores (pitchblende) about 150 mg per tonne of pitchblende, from the decay of uranium-235
- Extraction, production
- Neutron bombardment of radium-226
no equation printed
- Uses
Actinium has no significant commercial applications, although it is used in the production of neutrons.
- Safety, toxicity
- not in sources
Discovery and name
- Discovered by
- Friedrich Oskar Giesel
- Discovered
- 1902
- First isolated
- Joseph G. Stites, Murrell L. Salutsky, Bob D. Stone
- Named by
- André-Louis Debierne
- Origin of the name
- from the Ancient Greek ακτίς, "beam" or "ray"
Actinium-227, a decay product of uranium-235, is a beta emitter with a 21.6-year half-life. Its principal decay products are thorium-227 (18.5-day half-life), radium-223 (11.4-day half-life), and a number of short-lived products including radon, bismuth, polonium, and lead isotopes. In equilibrium with its decay products, it is a powerful source of alpha particles. Actinium metal has been prepared by the reduction of actinium fluoride with lithium vapor at about 1100 to 1300-degrees C. The chemical behavior of actinium is similar to that of the rare earths, particularly lanthanum. Purified actinium comes into equilibrium with its decay products at the end of 185 days, and then decays according to its 21.6-year half-life. It is about 150 times as active as radium, making it of value in the production of neutrons.
In April of 2012, Los Alamos National Laboratory announced a new medical isotope project that shows promise for rapidly producing major quantities of a new cancer-treatment agent, actinium 225 (Ac-225). Both a press release and a video are available.
Conventions
Valence electrons are counted by the usual convention: the outer shell for s- and p-block elements, ns and (n-1)d for the d-block, ns, (n-1)d and (n-2)f for the f-block. Lanthanides and actinides are placed in the f-block with no group number. Electrical conductivity is the reciprocal of the printed resistivity. Ionic radii are Shannon effective radii, six-coordinate unless noted. Where a field reads “not in sources” the value was not found; it is a gap, not a zero. Regulatory limits are the published values and change often, so check the standard in force at your site and the numbers written into your own permit before you design to them.
Data
Element records, isotopes, radii and the descriptive text come from PubChem (NCBI), the Los Alamos National Laboratory periodic table, IUPAC CIAAW and the IAEA Atomic Mass Data Center. Appearance, thermal conductivity, electrical resistivity, crystal structure, discovery and the origin of each name come from Wikipedia and Periodic-Table-JSON, used under CC BY-SA 4.0. Hazard classifications come from the ECHA C&L inventory via PubChem. Ionic radii follow R. D. Shannon (1976). The water chapters cite their own sources at the foot of each entry, and are written to the level of Snoeyink and Jenkins, Stumm and Morgan, MWH's Water Treatment and Metcalf and Eddy.