Protactinium

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

    fullProtactinium is not relevant to ordinary water treatment: protactinium-231, the only long lived isotope, is a trace daughter of uranium-235 present at attograms per litre in seawater and is so strongly hydrolysed and particle reactive that it is used as a scavenging tracer of ocean circulation; it has a WHO guidance level of 0.1 Bq/L, the lowest in the annex, is caught by gross alpha screening, and appears in water only at uranium mill and legacy nuclear sites.

    Typical wastewaters

    • uranium ore refining raffinate (pitchblende, St. Louis airport site and Weldon Spring raffinate pits) Pa-231 following Th-230 into the raffinate solids and slurry left after ether extraction of uranium, with Ac-227 growing in from it source term for ore in equilibrium: Pa-231 at 0.02 of the uranium activity, 0.01 of total alpha; NIOSH found dose reconstruction for raffinate workers exposed to Th-230, Pa-231 and Ac-227 not feasible; a residue slurry rather than a discharged liquid, and no activity per litre was read

    1 · Identity

    Symbol, number
    Pa, 91
    Oxidation states in water
    +5 as hydrolysed hydroxo oxo species that adsorb to vessel walls and particles at any pH above strong acid; +4 under strongly reducing conditions (element entry). Protactinium-231 (half life 32,500 years, alpha, uranium-235 chain) and the short lived protactinium-234 and -233 are the isotopes; the element has no stable form.
    Note
    The element entry covers the discovery and the fluoro complexes. This chapter says only that Pa(V) is among the most particle reactive actinides and how it is regulated.

    2 · Occurrence in water

    Natural sources
    Decay of uranium-235 in uranium ores and in seawater, where protactinium-231 is present at tens of attograms per litre in filtered water and is detectable in about 2 L of surface seawater for the particulate fraction (Shen 2003); it is removed onto sinking particles and is used together with thorium-230 as a tracer of ocean circulation.
    Anthropogenic sources
    Uranium mill tailings and spent fuel; neptunium-237 in waste decays to protactinium-233, which was removed from solution together with neptunium by bioprecipitation in one laboratory study (EPA Kd volume III). No effluent figure was read.
    matrixtypical rangenote
    seawatertens of attograms per litre ag/Lanalytical paper, not a surveyprotactinium-231 in filtered (below 0.4 µm) seawater; detection limits 38 and 49 ag in particulate and dissolved fractions by isotope dilution TIMS; 1 ag is 10⁻18 g

    3 · Speciation

    Pa(V) hydrolyses at once to hydroxy oxide species that stick to vessel walls, so aqueous protactinium is kept only in strong acid or as fluoride complexes such as PaF₈³⁻ (element entry). In natural water it is therefore almost entirely on particles and is removed from the water column by scavenging; the dissolved remainder is a hydrolysed Pa(V) species whose formula was not given by any source read.

    conditiondominant speciesnote
    natural water, any pHhydrolysed Pa(V) hydroxo oxo species, mostly particulateparticle reactive; measured in both dissolved and particulate fractions (Shen 2003)
    hydrofluoric acidPaF₈³⁻ and other fluoro complexeselement entry; the only way to hold it in solution
    Solubility
    Pa₂O₅ and the hydrous oxide are insoluble; the dioxide resists nitric, hydrochloric and sulfuric acid and dissolves in hydrofluoric acid (element entry).
    Hydrolysis
    Immediate and complete in dilute acid and above (element entry).
    Complexation
    Fluoride; nothing sourced for carbonate or organics.
    Precipitates
    Hydrous protactinium oxide on any surface or particle.

    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
    isotope dilution thermal ionisation mass spectrometry after chemical separationresearch method (Shen 2003)38 to 49 ag per sample; 100 to 1000 ag needed for 4 to 12 percent uncertaintythe only way to see natural levels; blank 16 plus or minus 15 ag
    gross alpha screeningISO 9696, ISO 10704; WHO Table 9.30.02 to 0.1 Bq/L; Euratom 0.04 Bq/Lprotactinium-231 counts in gross alpha; WHO screening level 0.5 Bq/L, Euratom 0.1 Bq/L, US 15 pCi/L
    Sampling pitfalls
    Protactinium adsorbs to every surface it meets; samples must be acidified hard at collection and spiked with tracer before any handling, and filtration separates a particulate fraction that holds most of it.

    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
    WHO GDWQ Annex 6, Table A₆.10.1 (protactinium-231); 100 (protactinium-230 and -233) Bq/Lguidance levels; protactinium-231 is marked natural and shares the lowest level in the table with lead-210, polonium-210, radium-228 and thorium-229; not in the chapter 9 short table
    EU Directive 2013/51/Euratom, Annex IIInot set no protactinium isotope in the derived concentration table; caught by the 0.1 Bq/L gross alpha screening level
    US EPA NPDWR15 pCi/Lgross alpha MCL excluding radon and uranium; no protactinium specific MCL

    8 · Health and environmental effects

    Toxicity
    Toxic through its radioactivity (element entry); an alpha emitter with no chemical toxicity relevant at these masses. No dose coefficient was read.
    Bioaccumulation
    Not addressed in the sources read.
    Ecotoxicity
    Not addressed in the sources read.

    Flags

    • The seawater level is quoted from an analytical method paper, not a survey.
    • Speciation is qualitative from the element entry; no hydrolysis constants or a formula for the dissolved species were read.
    • The Euratom table was read from the retained UK copy on legislation.gov.uk.

    Gaps

    • No source read gives protactinium in fresh water, groundwater, drinking water, wastewater or uranium mill effluent.
    • No removal study exists in the sources read; the removal list is empty on purpose.
    • No dose coefficient or toxicity value for protactinium-231 was read.
    • The CWW BAT conclusions have no radioactivity parameter; no discharge row is written.
    • The relative particle reactivity of protactinium and thorium, the basis of the protactinium-231 to thorium-230 circulation tracer, was not read this session and is not stated.
    • No balanced equation is written: protactinium hydrolysis is described qualitatively in the sources read; no constant or stoichiometry was printed.

    Sources

    Shen, C.-C., Cheng, H., Edwards, R. L., Moran, S. B., Edmonds, H. N., Hoff, J. A. and Thomas, R. B., Measurement of attogram quantities of 231Pa in dissolved and particulate fractions of seawater by isotope dilution thermal ionization mass spectroscopy, Analytical Chemistry 75 (2003) 1075 to 1079 (abstract via Europe PMC)
    WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first and second addenda (2022), Annex 6 Supporting information on radionuclides, Table A6.1 (NCBI Bookshelf)
    WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first addendum, chapter 9 Radiological aspects (screening levels, Table 9.3)
    Council Directive 2013/51/Euratom, Annex III (screening levels, derived concentrations, limits of detection), read in the retained UK copy on legislation.gov.uk
    US EPA, National Primary Drinking Water Regulations (table of MCLs and MCLGs, radionuclides)
    US EPA, Understanding Variation in Partition Coefficient, Kd, Values, Volume III: Review of Geochemistry and Available Kd Values for Americium, Arsenic, Curium, Iodine, Neptunium, Radium and Technetium, EPA 402-R-04-002C (July 2004), section 5.6.2 (protactinium-233 bioprecipitation with neptunium)
    The Element Book, element entry and reference text for Pa (data/elements/Pa.json, data/reference/text/Pa.json)
    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

    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.