Aguato

    Technetium

    group 7 · period 5 · d-block · transition metal

    full Most contaminants are slowed on their way through an aquifer because something holds them back: a charge, a surface, a mineral that will take them in. Technetium-99 is one of the most mobile radionuclides in water precisely because almost nothing does. In oxic water it is the pertechnetate anion TcO₄⁻, large, singly charged and weakly hydrated, and so barely sorbed at the pH of ordinary groundwater that it is carried at very nearly the speed of the water itself; decay is no help either, because the half life is far longer than the time any plume takes to move. That is why the isotope defines the groundwater plumes under Hanford and the other fuel cycle sites. Anything done about it has to change either the charge or the oxidation state: reduce it with Fe(II) or sulfide to a Tc(IV) oxide of very low solubility, remembering that the return of oxygen can undo that, or catch the anion on an exchanger against the nitrate, sulfate and chloride competing for the same site. Technetium has no stable isotope and no chemical limit, so what stands in place of one is radiological: a WHO guidance level of 100 Bq/L and a US derived concentration of 900 pCi/L.

    Typical wastewaters

    • nuclear fuel reprocessing and uranium enrichment plant discharges
      technetium-99 as pertechnetate TcO₄⁻, weakly sorbed and mobile
    • nuclear site groundwater pump and treat (Hanford tank leaks and disposal cribs)
      pertechnetate TcO₄⁻ in oxic groundwater above the 900 pCi/L standard in plume areas
    • alkaline nuclear tank waste streams (Hanford, Savannah River)
      TcO₄⁻ in 1 M sodium hydroxide with nitrate, sulfate and chloride competing
      removal work uses perrhenate as the surrogate
    • hospital effluent and sewage (radiopharmaceuticals)
      technetium-99m from medical imaging, decaying with a 6 hour half-life; species not given by the source

    1 · Identity

    Symbol, number
    Tc, 43
    Oxidation states in water
    +7 as pertechnetate TcO₄⁻ in oxic water; +4 as TcO₂ hydrate (and Tc(IV) sulfides) under reducing conditions
    Note
    The element chapter covers the isotopes and the pertechnetate chemistry. Tc-99 is a pure beta emitter with a 210,000 year half-life; Tc-99m (6 h) from medical imaging reaches hospital effluent and sewage but decays away.

    2 · Occurrence in water

    Natural sources
    Negligible: traces from spontaneous fission of uranium (element chapter); the EPA fact sheet notes very small natural amounts in the crust and very low concentrations in air, seawater, soils and biota from fallout.
    Anthropogenic sources
    Fission product of uranium and plutonium in reactors; atmospheric weapons tests; fuel reprocessing and uranium enrichment plant discharges; groundwater beneath uranium processing facilities at US federal sites; Tc-99m in hospital and laboratory effluent. At Hanford the isotope is present in the vadose zone and groundwater from tank leaks and disposal cribs.
    matrixtypical rangenote
    contaminated groundwater, Hanfordabove the 900 pCi/L standard in plume areas pCi/Lone site; maxima not quotedWashington Ecology lists Tc-99 among the eight main Hanford groundwater contaminants, water soluble and highly mobile, with limited methods to capture it in the environment
    contaminated vadose zone sediment, Hanford34 to 3800 pCi/gsediment, not waterrange of the sediments used in the PNNL gas-phase treatment tests

    3 · Speciation

    In oxic water technetium is pertechnetate, TcO₄⁻, a large weakly hydrated anion that is weakly sorbed at neutral and alkaline pH and moves with the water. Under anoxic conditions Fe(II) and sulfide reduce Tc(VII) to Tc(IV), which precipitates as a hydrous TcO₂ phase (and sulfides where sulfide is present) of very low solubility; re-oxidation on return of oxygen remobilises it, so immobilisation may not be permanent. Organic rich soils retain it.

    conditiondominant speciesnote
    oxic groundwater and surface water, pH 6 to 9TcO₄⁻highly mobile; radioactive decay does not attenuate a plume over any practical time
    anoxic, Fe(II) or sulfide bearing sedimentTcO₂.nH₂O (s), Tc(IV) sulfidesimmobilised; the basis of reductive treatment
    organic rich soilretained Tc, not characterised in the fact sheetEPA: retained and not highly mobile
    Solubility
    Pertechnetate salts are freely soluble; TcO₂ hydrate is very insoluble.
    Hydrolysis
    None for TcO₄⁻; Tc(IV) is fully hydrolysed.
    Complexation
    No complexation with natural ligands is described here; on an exchanger the anion competes with nitrate, sulfate and chloride.
    Precipitates
    TcO₂.nH₂O, Tc(IV) sulfide.
    TcOX4X−+4 HX++3 eX−→TcOX2(s)+2 HX2O\ce{TcO4^- + 4 H+ + 3 e- -> TcO2 (s) + 2 H2O}
    the Tc(VII) to Tc(IV) half reaction that every reductive treatment rests on; it runs once the redox potential falls into the iron reducing and sulfate reducing range of an anoxic aquifer, and reverses when air returns; written as the electron balance of the reduction the PNNL report describes, which prints no standard potential
    TcOX4X−+3 FeX2++7 HX2O→TcOX2(s)+3 Fe(OH)X3(s)+5 HX+\ce{TcO4^- + 3 Fe^2+ + 7 H2O -> TcO2 (s) + 3 Fe(OH)3 (s) + 5 H+}
    reduction of pertechnetate by aqueous or mineral Fe(II) to a hydrous Tc(IV) oxide, the reaction described for anoxic Hanford sediments and cited by the PNNL report (Zachara et al. 2007); balanced statement of that redox pair, the hydration water of the oxide omitted
    4 TcOX2(s)+3 OX2+4 OHX−→4 TcOX4X−+2 HX2O\ce{4 TcO2 (s) + 3 O2 + 4 OH^- -> 4 TcO4^- + 2 H2O}
    re-oxidation of the reduced solid when oxygen returns, the reason reductive immobilisation may not be permanent; alkaline to circumneutral water; electron balance of the re-oxidation the PNNL report names, not printed there

    4 · Role in treatment

    as a problem
    pertechnetate plumes in groundwater
    weak sorption of the anion, no decay, so the plume travels at groundwater velocity
    Hanford 200 Area groundwater is pumped and treated; the vadose zone is the long term source

    5 · Removal and control

    in situ reductive immobilisation with hydrogen sulfide and ammonia gases (vadose zone)
    hydrogen sulfide reduces Tc(VII) to Tc(IV); ammonia vapour dissolves sediment aluminosilicates so that precipitates coat and enclose the reduced technetium
    laboratory tests on Hanford sediments at 34 to 3800 pCi/g, 1 to 8 percent moisture, gas delivery of minutes to hours, sequential or parallel gases
    Efficiency
    a large fraction of the treated Tc-99 resisted leaching in saturated column tests
    Interferences
    re-oxidation on return of air; alkaline co-contaminants
    anion exchange and selective anion sorbents (pump and treat, waste streams)
    TcO₄⁻ exchanges onto quaternary ammonium, imidazolium or other cationic frameworks; perrhenate is the non-radioactive surrogate in development work
    RCl+TcOX4X−→RTcOX4+ClX−\ce{RCl + TcO4^- -> RTcO4 + Cl^-}
    a cationic polymer sorbent reached 1052 mg/g perrhenate after 24 h in 1 M sodium hydroxide and removed TcO4^- rapidly from simulated Hanford and Savannah River waste; a zinc oxide biochar composite took 25,916 mg/kg perrhenate with selectivity over iodide, nitrite, nitrate, sulfate and phosphate; the exchange is written in the usual resin notation (R a quaternary ammonium site) for a chloride form bed, the sources describe the sorbents and capacities rather than the exchange step
    Efficiency
    as quoted for the surrogate; no plant performance figure read
    Interferences
    nitrate, sulfate and chloride compete; radiolysis and high alkalinity degrade organic resins
    zero valent iron and Fe(II) reduction in reactive barriers
    reduction to Tc(IV) oxide and sulfide on iron surfaces
    3 Fe(s)+2 TcOX4X−+8 HX+→3 FeX2++2 TcOX2(s)+4 HX2O\ce{3 Fe (s) + 2 TcO4^- + 8 H+ -> 3 Fe^2+ + 2 TcO2 (s) + 4 H2O}
    anoxic; sulfidised iron holds the reduced technetium longer; the stoichiometry is the electron balance for the reduction to Tc(IV) oxide that the PNNL report describes, not printed there
    Efficiency
    not recorded
    Interferences
    oxygen re-mobilises Tc(IV)

    6 · Analytics

    methodstandarddetection limitnote
    liquid scintillation counting after separationISO 22125-1:2019about 5 to 20 Bq/kg with 30 min counting of 14 to 40 mLall water types: drinking, rain, surface, ground, cooling, industrial and domestic wastewater
    ICP-MS after separationISO 22125-2:2019not recordedcatalogue entry only; the separation chemistry and the handling of interferences are not described here
    Sampling pitfalls
    Keep the sample oxic: pertechnetate is dissolved and passes filters, but a sample that goes anoxic in the bottle loses technetium to the walls as Tc(IV). Ruthenium and molybdenum isobars must be separated before ICP-MS.

    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 Table A₆.1100 Bq/Ltechnetium-99 guidance level at 0.1 mSv per year; Tc-99m is not listed in the rows read
    US EPA NPDWR900 pCi/Lderived concentration of Tc-99 assumed to yield the 4 mrem per year beta and photon MCL when Tc-99 is the only such nuclide (33 Bq/L, the writer's conversion); with other beta emitters the summed dose applies
    US EPA 40 CFR 141.664 mrem per yearMCL for beta particle and photon radioactivity from man-made radionuclides; the section read lists tritium 20,000 and strontium-90 8 pCi/L, not technetium
    EU 10.1 mSv per yearindicative dose parametric value; gross beta screening 1.0 Bq/L; Tc-99 is not among the derived concentrations listed in the annex read
    EU DWD 2020/2184not set radioactivity is left to Directive 2013/51/Euratom
    discharge
    bodylimitnote
    EU CWW BREF BAT-AEL 2, BAT 12not set radionuclides are outside the CWW BAT conclusions

    8 · Health and environmental effects

    Toxicity
    Radiological, not chemical: Tc-99 is a weak beta emitter, so external exposure is minimal and ingestion of contaminated water and plants is the route; once absorbed it concentrates in the thyroid and gastrointestinal tract and is excreted steadily (half in about 60 hours, Washington Ecology). Risk is an increased chance of cancer.
    Bioaccumulation
    Under aerobic conditions technetium in soil transfers readily to plants; brown algae concentrate Tc-99 from seawater and it transfers to marine animals 3.

    Read these with care

    • Hanford groundwater maxima were not read; only the standard and the qualitative plume statements are quoted.
    • The pertechnetate sorbent capacities are perrhenate surrogate figures from laboratory materials, not plant performance.
    • The Fe(II) reduction equation is the writer's balanced statement of the redox pair described in the PNNL report; the original paper was not read.
    • The 900 pCi/L to 33 Bq/L conversion is the writer's arithmetic.

    What this chapter does not cover

    • Tc-99 concentrations in groundwater (pCi/L) at Hanford or any other site were not read from a primary source.
    • Kd values for pertechnetate were not read.
    • Tc-99m in hospital effluent and sewage was not read.
    • The Euratom Annex III list read did not include Tc-99; the full annex may.
    • No GCC standard was read.
    • The oxidation product of hydrogen sulfide in the gas phase reduction of pertechnetate is not stated by the PNNL report, so no equation is written for that step.
    • Complexation of pertechnetate with natural ligands, the separation chemistry behind the mass spectrometric method, and any ecotoxicity test for technetium were not read.
    • Ecotoxicity: No ecotoxicity data for technetium are quoted in this chapter.

    Notes

    1. Euratom Directive 2013/51
    2. Decision 2016/902
    3. EPA fact sheet

    Sources

    US EPA, EPA Facts About Technetium-99 4: sources, half-life 210,000 years, environmental behaviour, 4 mrem per year MCL and the 900 pCi/L derived concentration
    Washington State Department of Ecology, Hanford cleanup: groundwater contaminants (technetium-99 entry: 900 pCi/L standard, mobility, half-life, health effects)
    Truex, M. J., Szecsody, J. E., Zhong, L. and Qafoku, N., Gas-Phase Treatment of Technetium in the Vadose Zone at the Hanford Site Central Plateau, PNNL-23665 / RPT-DVZ-AFRI-023 (September 2014), summary and introduction
    Creation of cationic polymeric nanotrap featuring high anion density and exceptional alkaline stability for highly efficient pertechnetate removal from nuclear waste streams, ACS Central Science (2024) (open access, PMC10906250); and Synthesis of ZnO nanoparticle-anchored biochar composites for the selective removal of perrhenate, a surrogate for pertechnetate, Journal of Hazardous Materials (2020) (abstract, PubMed 31761646)
    ISO 22125-1:2019, Water quality. Technetium-99. Part 1: Test method using liquid scintillation counting (scope and detection limit from the catalogue abstract)
    ISO 22125-2:2019, Water quality. Technetium-99. Part 2: Test method using inductively coupled plasma mass spectrometry (catalogue entry)
    40 CFR 141.66 Maximum contaminant levels for radionuclides (beta particle and photon radioactivity 4 mrem/year; gross alpha 15 pCi/L; combined radium 5 pCi/L; uranium 30 µg/L)
    WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first and second addenda (2022), Annex 6 Table A6.1 guidance levels for radionuclides in drinking-water (individual dose criterion 0.1 mSv per year, levels rounded to the nearest order of magnitude)
    Council Directive 2013/51/Euratom on radioactive substances in water intended for human consumption, Annex I (radon 100 Bq/l, tritium 100 Bq/l, indicative dose 0.1 mSv), Annex III screening (gross alpha 0.1 Bq/l, gross beta 1.0 Bq/l) and derived concentrations (annexes read on legislation.gov.uk)
    Directive (EU) 2020/2184 on the quality of water intended for human consumption (recast), Annex I Parts B, C and D (annexes read on legislation.gov.uk)
    US EPA, National Primary Drinking Water Regulations (table of MCLs; inorganic chemicals and radionuclides; beta particle and photon emitters 4 millirem per year)
    Commission Implementing Decision (EU) 2016/902 establishing BAT conclusions for common waste water and waste gas treatment/management systems in the chemical sector (CWW), BAT 12 Tables 1 to 3 (TOC, COD, TSS, TN, Ninorg, TP, AOX, Cr, Cu, Ni, Zn) (annex read on legislation.gov.uk)
    The Element Book, element chapter and reference text for Tc (isotopes, pertechnetate chemistry, medical Tc-99m, corrosion inhibition)

    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.