Rhenium

    group 7 · period 6 · d-block · transition metal

    minorRhenium has no drinking water guideline and no effluent limit, but it is the one heavy metal that behaves like an anion in oxic water: the perrhenate ion ReO₄⁻ is soluble across the whole pH range of oxic water, is not sorbed, and is the stable chemical analogue of pertechnetate TcO₄⁻, which is why rhenium stands in for technetium-99 in sorption and barrier tests; rivers carry it from black shale and pyrite weathering and, increasingly, from people, and molybdenum roasters are the industrial source.

    Typical wastewaters

    • molybdenite roasting (scrubber liquor) perrhenate ReO₄⁻ in the flue dust scrubber liquor of molybdenum roasters, from which it is recovered as perrhenic acid or ammonium perrhenate on strong base resin a recovery liquor rather than a discharge; no concentration in mine, mill or scrubber water was read

    1 · Identity

    Symbol, number
    Re, 75
    Oxidation states in water
    +7 as perrhenate ReO₄⁻ in oxic water, mobile and conservative; +4 as insoluble ReO₂ and as rhenium taken into sulfide and organic rich sediment under reducing conditions. The lower states are not stable in water.
    Note
    The element entry covers the metal, the superalloy and catalyst markets and recovery from molybdenite roaster dust as ammonium perrhenate. This chapter is about ReO₄⁻ as a conservative tracer and technetium analogue.

    2 · Occurrence in water

    Natural sources
    Oxidative weathering of black shales and of pyrite in basalts releases rhenium as perrhenate (Rahaman 2012); it stays dissolved through estuaries and the oxic ocean and is removed only into anoxic sediment, which is why the marine rhenium budget is used to read past ocean anoxia.
    Anthropogenic sources
    Indian Peninsular rivers carry a large anthropogenic rhenium load that accounts for most of their rhenium and about 70 percent of the total rhenium supply from Indian rivers to the sea, most of it in the Godavari (Rahaman 2012); the study does not name the industries. Molybdenite roasting sends rhenium to flue dust and scrubber liquor from which it is recovered as perrhenic acid or ammonium perrhenate (element entry); molybdenum and copper mine and mill waters are the expected point sources, but none was read.
    matrixtypical rangenote
    surface water, rivers1.4 to 72.7 (Himalayan rivers, mean 7.8); 0.5 to 122 (Peninsular India, mean 15) pmol/kg
    one region; the high Peninsular values are largely anthropogenic
    dissolved rhenium; the pre-anthropogenic global river average is estimated at about 3 pmol/kg from the rhenium to potassium correlation
    seawater0.000004 mg/L
    compilation value, not a measured profile read this session
    PubChem compilation figure carried in the element entry, about 20 pmol/L; rhenium is conservative in the oxic ocean

    3 · Speciation

    In oxic water rhenium is the tetrahedral oxyanion perrhenate ReO₄⁻, the conjugate base of the strong acid HReO₄, so it carries a single negative charge at any pH, forms no hydroxide, is not sorbed by oxides or clays and travels with the water. Under sulfidic or organic rich reducing conditions it is reduced to Re(IV) and fixed in sediment, the same behaviour as technetium, uranium and molybdenum. The element entry gives the formation of perrhenic acid from the heptoxide; no stability constants were read.

    conditiondominant speciesnote
    oxic water, any pHReO₄⁻conservative; the technetium analogue
    sulfidic, organic rich sedimentRe(IV) in sulfide or organic phases, ReO₂removal term of the marine budget; not sourced beyond the river paper's framing
    Solubility
    Perrhenates of the alkali metals and ammonium are soluble; ReO₂ is insoluble (element entry).
    Hydrolysis
    None; ReO₄⁻ is a stable oxyanion.
    Complexation
    Negligible; the anion does not pair strongly with the major cations.
    Precipitates
    None in natural water; ammonium perrhenate crystallises from concentrated recovery liquors.
    ReX2OX7+HX2O2HReOX4\ce{Re2O7 + H2O -> 2 HReO4}
    the heptoxide dissolves in water to perrhenic acid (element entry)
    HReOX4HX++ReOX4X\ce{HReO4 -> H+ + ReO4^-}
    strong acid, fully dissociated at natural pH

    4 · Role in treatment

    as a problem
    not removed by conventional treatment
    a monovalent anion that is neither hydrolysed nor sorbed
    the same problem technetium-99 poses at nuclear sites; rhenium is used as its non-radioactive stand-in in column and barrier tests

    5 · Removal and control

    anion exchange
    ReO₄⁻ is held on strong base resin, which is how rhenium is recovered from roaster scrubber liquor
    recovery chemistry stated by the element entry only in outline; no water treatment study read
    Efficiency
    not read
    Interferences
    sulfate, chloride and molybdate compete

    6 · Analytics

    methodstandarddetection limitnote
    ICP-MSresearch methods (Rahaman 2012 used ICP-MS on river water); not an analyte of EPA 200.8not readrhenium at masses 185 and 187; osmium-187 interferes at 187
    Sampling pitfalls
    Rhenium is conservative and easy to keep in solution; filter and acidify as for any trace metal. The risk is contamination from tungsten and molybdenum alloys in sampling hardware.

    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 GDWQno guideline rhenium does not appear in the Annex 3 chemical summary tables; Annex 6 gives a guidance level of 100 Bq/L for rhenium-186, a medical isotope
    US EPA NPDWRnot regulated no entry in the table of regulated contaminants
    discharge
    bodylimitnote
    EU CWW BREF BAT-AEL (Decision 2016/902)not set BAT 12 metals are Cr, Cu, Ni and Zn only

    8 · Health and environmental effects

    Toxicity
    No known biological role (element entry); no drinking water assessment exists.
    Bioaccumulation
    Not addressed in the sources read.
    Ecotoxicity
    Not addressed in the sources read.

    Flags

    • The river concentrations are Indian rivers only; the pre-anthropogenic global average is a model estimate in the same paper.
    • The seawater figure is a compilation value from the element entry, not a measured profile.
    • The anion exchange removal row is inferred from the recovery route in the element entry, not from a treatment study.

    Gaps

    • No molybdenum or copper mine water, roaster scrubber liquor or tailings groundwater rhenium concentration was read; the industrial row is therefore missing.
    • No source read gives rhenium in groundwater, drinking water or municipal wastewater.
    • EU DWD 2020/2184 Annex I was not read this session.
    • The technetium analogue statement rests on the element entry; no sorption study comparing ReO₄⁻ and TcO₄⁻ was read.
    • No GCC discharge standard was 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.