Aguato

    Neodymium

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

    minor Neodymium is a light lanthanide, trivalent across the natural range of pH and redox condition, and it is the light lanthanide geochemists report most often, so its seawater profile stands as the reference against which the others are read. In acid sulfate water it travels as the free ion and a sulfate ion pair; from neutral pH upwards the carbonate complexes take over, and phosphate, carbonate and fluoride solids together with sorption on iron and manganese oxides keep the dissolved concentration very low. None of that asks anything of a treatment works, and neodymium has no water regulation and no treatment role. What the element does have is a point source and a toxicity number. Phosphogypsum discharge carried 75 t a year of it into the Rhine estuary, and among the eight rare earths the Dutch risk assessment tested, neodymium gave the lowest Daphnia EC₅₀ and hence the lowest freshwater MPC, 1.8 µg/L.

    Typical wastewaters

    • phosphate fertiliser manufacture (phosphogypsum slurry)
      Nd³⁺ precipitating as fluoride and phosphate near the outfall
      75 t of Nd to the Rhine estuary in 1994 from one plant and 11 t from a second; sediment near the outfall 80 ppm
    • mine drainage (coal)
      Nd³⁺ and the NdSO₄⁺ ion pair in acid sulfate water; total REE averaged 282 µg/L over 141 sites

    1 · Identity

    Symbol, number
    Nd, 60
    Oxidation states in water
    +3 only (Nd³⁺)
    Note
    The metal's reactions are in the element chapter; in water neodymium shares the trivalent carbonate and phosphate chemistry of the lanthanide row.

    2 · Occurrence in water

    Natural sources
    Weathering of monazite and bastnaesite; the light lanthanide most often reported by geochemists, so its seawater profile (rising with depth from scavenging at the surface and release at depth) is the reference for the row: 2.62 to 26.66 pmol/kg in the Northwest Pacific, 4.45 pmol/kg in subtropical surface water and 22.70 pmol/kg at 2000 m in the mixed water region.
    Anthropogenic sources
    Phosphogypsum slurry: 75 t of Nd to the Rhine estuary in 1994 from one plant and 11 t from a second, sediment near the outfall 80 ppm Nd; neodymium-iron-boron magnet manufacture and recycling effluent is not described by any source read.
    matrixtypical rangenote
    seawater7.21 to 36.1 pmol/Lone stationwestern Pacific, 3 to 5663 m; concentrations rise with depth
    seawater, Northwest Pacific2.62 to 26.66 pmol/kg13 to 40 N along 150 E, surface to 2000 m
    drinking waterbelow detection to 8 to 14 µg/L1994 dataDutch drinking water normally below detection; Y, La, Ce and Nd reached 8 to 14 µg/L at three works in 1994, called exceptional
    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; the survey reports the sum, not the neodymium share
    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; the study reports the sum, not the neodymium share

    3 · Speciation

    Trivalent Nd³⁺ 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 NdSO₄⁺ ion pair dominate 1. From neutral to alkaline pH the carbonate complexes NdCO₃⁺ and Nd(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 5Nd³⁺, NdSO₄⁺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 9NdCO₃⁺, Nd(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 sedimentsNdPO₄ (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 neodymium solid was read.
    Hydrolysis
    Hydrolysis of Nd³⁺ is minor in natural water; the hydroxide Nd(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).
    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.
    Precipitates
    NdPO₄ (hydrated phosphate), Nd₂(CO₃)₃, NdF₃ near fluoride rich discharges, Nd(OH)₃ at high pH; co-precipitated on iron, aluminium and manganese hydroxides.
    NdX3++COX3X2−→NdCOX3X+\ce{Nd^3+ + CO3^2- -> NdCO3^+}
    circumneutral pH; the first carbonate complex
    NdX3++2 COX3X2−→Nd(COX3)X2X−\ce{Nd^3+ + 2 CO3^2- -> Nd(CO3)2^-}
    alkaline pH; the dicarbonate anion, strongest for the heavy lanthanides
    NdX3++SOX4X2−→NdSOX4X+\ce{Nd^3+ + SO4^2- -> NdSO4^+}
    acid, sulfate rich water; above 90 percent of the dissolved element at pH 3.1 to 3.4
    NdX3++POX4X3−→NdPOX4(s)\ce{Nd^3+ + PO4^3- -> NdPO4 (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 recorded
    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 waterneodymium 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 2, 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.
    Bioaccumulation
    Field bioconcentration factors in Rhine estuary amphipods fall from the light to the heavy lanthanides (La 28,840 to Lu 4,786; Nd 29,512); 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
    RIVM (2000) environmental risk limits, not discharge limits: MPC 1.8 µg/L in fresh surface water and 0.86 µg/L in salt water (negligible concentrations 0.40 and 0.009 µg/L), derived as lowest LC₅₀ divided by 1000; the Daphnia EC₅₀ of 1.4 mg/L is the lowest of the eight elements tested plus a background set at the detection limit (0.39 µg/L). Acute data behind it: Daphnia magna 48 h EC₅₀ 1.4 mg/L, zebrafish 96 h LC₅₀ 21 mg/L; chronic: Daphnia magna 21 d NOEC 1.6 mg/L (mortality and reproduction). Field bioconcentration factor in amphipods (porewater basis) 29,512.

    Read these with care

    • 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.

    What this chapter does not cover

    • WHO GDWQ and EU DWD 2020/2184 Annex I were not read (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 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 neodymium specific river concentration was read; the Rhine estuary survey reports Nd only in sediment (80 ppm near the outfall).

    Notes

    1. sulfate complexes above 90 percent at pH 3.1 to 3.4 in the EPA groundwater study
    2. Decision 2016/902

    Sources

    The Element Book, neodymium entry
    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
    Dissolved rare earth elements in the Northwest Pacific: sources, water mass tracing and cross-shelf fluxes, Frontiers in Marine Science 10 (2023) 1135113

    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.