Holmium

    no group (f-block) · period 6 · f-block · lanthanide

    minorHolmium has no water regulation, no treatment role and no known point source; beyond the shared heavy lanthanide chemistry the only holmium specific water number read is a field bioconcentration factor.

    Typical wastewaters

    • rare earth separation and processing (saponification wastewater) Ho³⁺ carried with the whole lanthanide row in ammonia rich separation plant wastewater (ammonia nitrogen 300 to 5,000 mg/L in Chinese saponification wastewater, 2005 estimate) no holmium specific concentration read
    • coal mine drainage (acid) Ho³⁺ and the HoSO₄⁺ ion pair dissolved at low pH in sulfate rich drainage; total rare earths averaged 282 µg/L over 141 Appalachian sites, per-element values not read co-precipitates into the iron, aluminium and manganese hydroxide sludge when the drainage is neutralised

    1 · Identity

    Symbol, number
    Ho, 67
    Oxidation states in water
    +3 only (Ho³⁺)
    Note
    The metal's reactions are in the book entry; in water holmium shares the trivalent carbonate and phosphate chemistry of the lanthanide row.

    2 · Occurrence in water

    Natural sources
    Weathering of monazite, bastnaesite and xenotime; heavy lanthanide, carbonate complexed in neutral to alkaline water.
    Anthropogenic sources
    None read. Ho-166 is used in medicine (not read this session); rare earth separation wastewater carries the whole row.
    matrixtypical rangenote
    seawater0.31 to 2.23 pmol/Lone stationwestern Pacific, 3 to 5663 m; concentrations rise with depth
    acid mine drainage (total rare earth elements)282 average µg/L
    sum of all REE, not this element
    total REE in coal mine drainage of the northern and central Appalachian basins, 141 sites; per-element values not read
    groundwater (total rare earth elements)0.36 to 1.66 µg/L
    sum of all REE, not this element
    sum of REE at a pH 5.1 to 6.1 site; 973 µg/L mean at a pH 3.1 to 3.4 site; per-element values not read

    3 · Speciation

    Trivalent Ho³⁺ throughout the natural pH and Eh range. Below about pH 6, and in sulfate rich water such as mine drainage, the free ion and the HoSO₄⁺ ion pair dominate (sulfate complexes above 90 percent at pH 3.1 to 3.4 in the EPA groundwater study). From neutral to alkaline pH the carbonate complexes HoCO₃⁺ and Ho(CO₃)₂⁻ take over, and they bind the heavy lanthanides more strongly than the light ones (at pH 5.1 to 6.1 the carbonate share rose from 5.0 percent for La to 19.2 percent for Lu). Phosphate, carbonate and fluoride solids and sorption to iron and manganese oxides cap the dissolved concentration at ng/L in oxic neutral water, and the light lanthanides ride partly on colloids.

    conditiondominant speciesnote
    acid mine drainage and acidic groundwater, pH below 5Ho³⁺, HoSO₄⁺the most mobile state; dissolved total REE in coal mine drainage averaged 282 µg/L (Part 2 survey), against ng/L in neutral water
    neutral to alkaline groundwater and river water, pH 7 to 9HoCO₃⁺, Ho(CO₃)₂⁻; a small free ion fraction; part of the load on colloids below 0.2 µmthe carbonate complexes keep the element in solution and make the heavy lanthanides relatively more mobile
    phosphate rich water, treated lake sedimentsHoPO₄ (s) as a hydrated phosphateREE phosphate solubility products can be as low as 10⁻25 (RIVM report citing Liu and Byrne 1997)
    Solubility
    Controlled by the phosphate, carbonate and fluoride solids and by sorption; the RIVM report puts total dissolved lanthanum and cerium in Dutch surface water at about 1 µg/L or less and the free ion fraction at 0.3 fM to 9 pM. No solubility product for a holmium solid was read this session.
    Hydrolysis
    Hydrolysis of Ho³⁺ is minor in natural water; the hydroxide Ho(OH)₃ forms only at high pH, so lime or caustic neutralisation of acid mine water strips the element with the iron and aluminium hydroxides rather than as its own hydroxide (no hydrolysis constant read this session).
    Complexation
    Sulfate at low pH, carbonate at neutral to alkaline pH (the sources read); humic substances compete for the element in organic rich water and are out-competed by carbonate in alkaline water. No stability constants were read this session.
    Precipitates
    HoPO₄ (hydrated phosphate), Ho₂(CO₃)₃, HoF₃ near fluoride rich discharges, Ho(OH)₃ at high pH; co-precipitated on iron, aluminium and manganese hydroxides.
    HoX3++COX3X2HoCOX3X+\ce{Ho^3+ + CO3^2- -> HoCO3^+}
    circumneutral pH; the first carbonate complex
    HoX3++2COX3X2Ho(COX3)X2X\ce{Ho^3+ + 2 CO3^2- -> Ho(CO3)2^-}
    alkaline pH; the dicarbonate anion, strongest for the heavy lanthanides
    HoX3++SOX4X2HoSOX4X+\ce{Ho^3+ + SO4^2- -> HoSO4^+}
    acid, sulfate rich water; above 90 percent of the dissolved element at pH 3.1 to 3.4
    HoX3++POX4X3HoPOX4(s)\ce{Ho^3+ + PO4^3- -> HoPO4 (s)}
    phosphate present; the solid that caps solubility and that phosphate binders rely on

    4 · Role in treatment

    Not relevant or not given for this element.

    5 · Removal and control

    neutralisation of acid mine drainage (lime, caustic or passive alkaline systems)
    co-precipitation with iron, aluminium and manganese hydroxides and hydroxysulfates as pH rises
    coal mine drainage precipitates carry about 724 g REE per tonne (Part 2 survey, 141 sites)
    Efficiency
    not quoted as a percentage
    zero-valent iron permeable reactive barrier
    REE drop below detection within the iron treatment zone
    groundwater remediation sites
    Efficiency
    to below 2 to 4 ng/L

    6 · Analytics

    methodstandarddetection limitnote
    ICP-MSISO 17294-2:2023not read; the standard covers drinking, surface, ground and waste waterholmium is in the element list of ISO 17294-2 (catalogue abstract)
    ICP-MS after preconcentrationresearch methods: chelating resin columns or magnesium hydroxide co-precipitation, then quadrupole or high resolution ICP-MS0.012 to 0.98 pmol/L (procedural blanks 0.041 to 3.60 pmol/L) for the 14 lanthanides pooled, magnesium hydroxide co-precipitation with a factor of about 200; terbium has been measured at 7 fmol/kg in recycled waterthe only way to reach the ng/L and sub-ng/L levels of rivers and seawater; the shale-normalised pattern, not the single concentration, is what the geochemists read
    Sampling pitfalls
    Filtration defines the result: 0.2 or 0.45 µm filtrates still carry colloid bound lanthanides, and only ultrafiltration (10 kDa) separates the truly dissolved pool, which matters most for the light lanthanides. Acidify after filtration. Report the shale-normalised pattern so that anthropogenic anomalies (gadolinium, lanthanum, samarium) are visible.

    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 lanthanide or rare earth element in the NPDWR table
    discharge
    bodylimitnote
    EU CWW BAT-AEL (Decision 2016/902), BAT 12not set Tables 1 to 3 carry TOC, COD, TSS, TN, Ninorg, TP, AOX, Cr, Cu, Ni, Zn; no rare earth element

    8 · Health and environmental effects

    Toxicity
    No human health guideline anywhere read; no acute or chronic human toxicity data for this element were read this session.
    Bioaccumulation
    Field bioconcentration factors in Rhine estuary amphipods fall from the light to the heavy lanthanides (La 28,840 to Lu 4,786; Ho 8,511); carp muscle takes up little (BCF 0.22 to 1.10 for Ce, La, Nd, Pr, Sm) while internal organs reach 634 to 978. Anthropogenic La and Sm in the Rhine are taken into mussel shells, anthropogenic Gd is not, so speciation decides bioavailability.
    Ecotoxicity
    No MPC was derived for holmium: the RIVM report set risk limits only for Y, La, Ce, Pr, Nd, Sm, Gd and Dy. The one holmium number it carries is a field bioconcentration factor in amphipods of 8,511 (porewater basis).

    Flags

    • The RIVM MPCs, where they exist, are environmental risk limits from a 2000 report (LC₅₀ divided by 1000, background at the detection limit), not permit limits.
    • The seawater range is one western Pacific station.

    Gaps

    • WHO GDWQ and EU DWD 2020/2184 Annex I were not read this session (eur-lex returned the articles without the annexes), so their absence of a rare earth parameter is not asserted here; only the US EPA table was read.
    • No GCC discharge standard was read; no GCC row is written.
    • World average river water concentrations (Gaillardet et al. 2003) were not reachable; river figures come from the Rhine and Dutch waters only.
    • No source read this session gives municipal wastewater concentrations for this element beyond the gadolinium literature.
    • ICP-MS oxide interference corrections between lanthanides are standard practice but no method text describing them was read, so none is written.
    • No stability constants or solubility products for this element's carbonate, phosphate or hydroxide were read; the speciation is qualitative, taken from the EPA groundwater study and the RIVM report.
    • No holmium specific river, groundwater or wastewater concentration was read, and no toxicity test.

    Sources

    The Element Book, holmium entry (data/elements/Ho.json and data/reference/text/Ho.json)
    Sneller, F. E. C., Kalf, D. F., Weltje, L. and Van Wezel, A. P., Maximum Permissible Concentrations and Negligible Concentrations for Rare Earth Elements (REEs), RIVM report 601501 011 (Bilthoven, 2000), Tables I, II, 2.2 and 4.1, section 5.1 and Appendices 1 to 3
    Rare earth element geochemistry characteristics of seawater and porewater from deep sea in western Pacific, Scientific Reports 7 (2017), Table 1 (Pigafetta basin, 3 to 5663 m)
    Rare-Earth Elements as Natural Tracers for In Situ Remediation of Groundwater (open access, PMC7868090); REE speciation and concentrations at three US groundwater remediation sites
    The occurrence and concentration of rare earth elements in acid mine drainage and treatment byproducts, Part 2: regional survey of northern and central Appalachian coal basins, Mining, Metallurgy and Exploration (OSTI 1577122)
    Lawrence, M. G. et al., Removal of magnetic resonance imaging contrast agents through advanced water treatment plants, Water Science and Technology 61 (2010) 685 to 692 (abstract via Crossref)
    Hatje, V., Bruland, K. W. and Flegal, A. R., Increases in anthropogenic gadolinium anomalies and rare earth element concentrations in San Francisco Bay over a 20 year record, Environmental Science and Technology 50 (2016) 4159 to 4168 (abstract via Europe PMC)
    Kulaksiz, S., Rare earth elements as emerging contaminants in the Rhine River, Germany and its tributaries, PhD thesis, Jacobs University Bremen (2012), chapters III to V (the Environment International 2011, Applied Geochemistry 2011 and EPSL 2013 papers)
    ISO 17294-2:2023, Water quality. Application of ICP-MS. Part 2: Determination of selected elements including uranium isotopes (element list from the ISO catalogue abstract)
    US EPA, National Primary Drinking Water Regulations (table of regulated contaminants; no lanthanide, rare earth or actinium entry; gross alpha 15 pCi/L)
    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
    US EPA, Rare Earth Elements: A Review of Production, Processing, Recycling, and Associated Environmental Issues, EPA 600/R-12/572 (December 2012), sections 4.5.1, 4.5.2 and 6.1.1

    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.