Actinium

    no group (f-block) · period 7 · f-block · actinide

    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.
    matrixtypical rangenote
    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 Gyrebelow 0.5 to 10.9 ag/kgbelow 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 samplesduplicates 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.

    conditiondominant speciesnote
    deep ocean, near the seafloordissolved Ac-227 released from sediment Pa-231 decayexcess 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

    methodstandarddetection limitnote
    radium delayed coincidence counting (RaDeCC) of Ac-227 via its Rn-219 and Po-215 daughters after manganese fibre or cartridge adsorptionresearch 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 cartridgesPa-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 purificationresearch method (Levier et al. 2021)about 0.5 ag/kg for 30 L; sample size 10 to 30 Lmeasures 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.

    drinking water
    bodylimitnote
    US EPA National Primary Drinking Water Regulationsnot 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

    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.