Holmium
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.
| matrix | typical range | note |
|---|---|---|
| seawater | 0.31 to 2.23 pmol/Lone station | western 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.
| condition | dominant species | note |
|---|---|---|
| acid mine drainage and acidic groundwater, pH below 5 | Ho³⁺, 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 9 | HoCO₃⁺, Ho(CO₃)₂⁻; a small free ion fraction; part of the load on colloids below 0.2 µm | the carbonate complexes keep the element in solution and make the heavy lanthanides relatively more mobile |
| phosphate rich water, treated lake sediments | HoPO₄ (s) as a hydrated phosphate | REE 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.
4 · Role in treatment
Not relevant or not given for this element.
5 · Removal and control
- Efficiency
- not quoted as a percentage
- Efficiency
- to below 2 to 4 ng/L
6 · Analytics
| method | standard | detection limit | note |
|---|---|---|---|
| ICP-MS | ISO 17294-2:2023 | not read; the standard covers drinking, surface, ground and waste water | holmium is in the element list of ISO 17294-2 (catalogue abstract) |
| ICP-MS after preconcentration | research methods: chelating resin columns or magnesium hydroxide co-precipitation, then quadrupole or high resolution ICP-MS | 0.012 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 water | the 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.
| body | limit | note |
|---|---|---|
| US EPA National Primary Drinking Water Regulations | not regulated | no lanthanide or rare earth element in the NPDWR table |
| body | limit | note |
|---|---|---|
| EU CWW BAT-AEL (Decision 2016/902), BAT 12 | not 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
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
Identity
- Name and symbol
- Holmium, Ho
- Atomic number
- 67 protons
- Position
- no group (f-block) · period 6 · f-block · lanthanide
- CAS number
- 7440-60-0
Atomic structure
- Atomic mass
- 164.93 u
- Electron configuration
- 1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹¹
[Xe] 6s²⁴f¹¹ - Electrons per shell
- 2, 8, 18, 29, 8, 2
- Valence electrons
- 13 ns, (n-1)d and (n-2)f
| isotope | mass (u) | abundance |
|---|---|---|
| 165Ho | 164.930 329(5) | 100 % |
Physical properties
- State at room temperature
- Solid
- Melting point
- 1,747 K (1,473.85 °C)
- Boiling point
- 2,973 K (2,699.85 °C)
- Density
- 8.8 g/cm3
- Appearance
- silvery white
- Thermal conductivity
- 16.2 W/(m·K)
- Electrical resistivity
- poly: 814 nΩ·m
- Electrical conductivity
- 1.23 MS/m
- Crystal structure
- hexagonal close packed
- Molar heat capacity
- 27.15 J/(mol·K)
Chemical properties
- Oxidation states
- +3
- Electronegativity
- 1.23 (Pauling Scale)
- Ionisation energy
- 6.022 eV
1st 581, 2nd 1,140, 3rd 2,204 kJ/mol - Electron affinity
- not in sources
- Atomic radius
- empirical 192, covalent 192, van der Waals 216 pm
- Ionic radius
- Ho³⁺ 90 pm
- Reactivity
- A late lanthanide (4f11 6s2, electronegativity 1.23) that is trivalent in essentially all its compounds; the metal is fairly corrosion resistant in dry air but oxidises quickly in moist air or when heated and reacts with water and acids.
- with water
- Reacts slowly with cold water and quickly with hot water to the hydroxide and hydrogen: , like the other heavy lanthanides.
- with oxygen, air
- Stable in dry air at room temperature but tarnishes in moist air to a yellowish oxide film and burns readily on heating: , the pale yellow sesquioxide.
- with acids
- Dissolves readily in dilute sulfuric acid to yellow Ho3+ solutions with evolution of hydrogen: , the sulfate.
- with halogens
- Reacts with all the stable halogens to the trihalides: , yellow, while the fluoride is pink.
- Typical compounds
- Ho₂O₃ holmium(III) oxide holmia, yellow oxide that colours glass and cubic zirconia
- HoCl₃ holmium(III) chloride yellow, soluble trihalide
- HoF₃ holmium(III) fluoride pink trihalide, reduced to make the metal
- Ho(OH)₃ holmium(III) hydroxide product of the metal with water
- Ho₂(SO₄)₃ holmium(III) sulfate yellow salt from sulfuric acid
Occurrence, production and use
- Crustal abundance
- 1.3 milligrams per kilogram
- Oceanic abundance
- 2.2×10-7 milligrams per liter
- Occurrence and sources
- monazite and bastnaesite a minor component; recovered from ores processed for yttrium
- Extraction, production
- not in sources
- Uses
- not in sources
- Safety, toxicity
- GHS classification, signal word Danger
- H228 Flammable solid Flammable solids
Discovery and name
- Discovered by
- Per Theodor Cleve, Jacques-Louis Soret and Marc Delafontaine
- Discovered
- 1878
- First isolated
- Heinrich Bommer
- Named by
- not in sources
- Origin of the name
- from Holmia, the Latin name for the city of Stockholm, home town of its discoverer
Pure holmium has a metallic to bright silver luster. It is relatively soft and malleable and is stable in dry air at room temperature but rapidly oxidizes in moist air and at elevated temperatures. The metal has unusual magnetic properties. Few uses have yet been found for the element. The element, as with other rare earths, seems to have a low acute toxic rating.
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.