Lanthanum

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

    minorLanthanum is not regulated in drinking water or effluent anywhere read, but it is the one lanthanide that is dosed on purpose into water bodies (lanthanum-modified bentonite as a phosphate binder) and the first rare earth shown to contaminate a large river from an industrial point source (the Rhine, from a refinery catalyst plant).

    Typical wastewaters

    • fluid catalytic cracking catalyst manufacture (Rhine, river-km 447.4) dissolved La³⁺ and its carbonate complexes at up to 49 mg/kg in the effluent (total REE 52 mg/kg) raised dissolved La in the Rhine from 1.91 to 338 ng/kg; about 1.5 t a year to the North Sea
    • phosphate fertiliser manufacture (phosphogypsum slurry) La³⁺ precipitating as LaF₃ near the outfall and as phosphate further away 93 t of La emitted to the Rhine estuary in 1994 by the larger of two plants
    • mine drainage (coal) La³⁺ and the LaSO₄⁺ ion pair in acid sulfate water; total REE averaged 282 µg/L over 141 sites leaves solution with the Fe, Al and Mn hydroxides on neutralisation

    1 · Identity

    Symbol, number
    La, 57
    Oxidation states in water
    +3 only (La³⁺); no redox chemistry in water
    Note
    The metal's reaction with water is in the book entry; in natural water lanthanum is a large, hard trivalent cation that pairs with carbonate, phosphate and fluoride.

    2 · Occurrence in water

    Natural sources
    Weathering of monazite and bastnaesite and of the accessory phosphates in ordinary rock; released most where water is acid. Dutch groundwater carried up to 2 µg/L at pH at or above 6.2 and up to 105 µg/L below pH 6.2 (RIVM, citing Stuyfzand 1991).
    Anthropogenic sources
    Effluent of a fluid catalytic cracking catalyst plant on the Rhine at river-km 447.4 (dissolved La up to 49 mg/kg in the effluent, total REE 52 mg/kg), which raised dissolved La from 1.91 ng/kg upstream at Mannheim to 338 ng/kg at Mainz and still 46.6 ng/kg (94 percent anthropogenic) 400 km downstream at the Dutch border, about 1.5 t of anthropogenic La a year to the North Sea; phosphogypsum slurry from phosphate fertiliser plants in the Rhine estuary (93 t of La emitted to water in 1994 by the larger of two plants, the REE precipitating as fluorides near the outfall and as phosphates further away); lanthanum-modified bentonite applied to about 200 lakes and reservoirs; rare earth processing wastewater.
    matrixtypical rangenote
    groundwaterbelow detection to 2 µg/Lregion-dependent; 1991 dataDutch groundwater at pH 6.2 or above; up to 105 µg/L in acidic groundwater below pH 6.2
    surface water, rivers1.91 to 338 ng/kg
    one river with a point source; geogenic Rhine La is of order 2 ng/kg
    dissolved (below 0.2 µm) in the Rhine, upstream of Mannheim to Mainz below the catalyst plant; 46.6 ng/kg at Xanten near the Dutch border
    seawater8.57 to 50.2 pmol/Lone stationwestern Pacific, 3 to 5663 m; concentrations rise with depth
    drinking waterbelow detection to 8 to 14 µg/L
    1994 data, treatment may have changed
    Dutch drinking water normally below detection; Y, La, Ce and Nd reached 8 to 14 µg/L at three works in 1994, called exceptional
    industrial wastewater49 mg/kgone plant, one samplingeffluent of the Rhine catalyst plant, dissolved La (total REE 52 mg/kg); 0.14 mg/kg total REE and Y in the plume downstream
    treated lakes after lanthanum-modified bentonite0.026 to 2.30 mg/Lmaxima, not meanspost-application maximum total La in surface water across 16 lakes; filterable La 0.002 to 0.14 mg/L; below 0.001 mg/L before treatment; back to baseline in 3 to 12 months

    3 · Speciation

    Trivalent La³⁺ 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 LaSO₄⁺ 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 LaCO₃⁺ and La(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. For lanthanum specifically, the RIVM report names lanthanum fluoride, carbonate and phosphate as the solubility controlling solids, the carbonate mattering most at high pH, and puts the free La³⁺ fraction at 0.3 fM to 9 pM.

    conditiondominant speciesnote
    acid mine drainage and acidic groundwater, pH below 5La³⁺, LaSO₄⁺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 9LaCO₃⁺, La(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 sedimentsLaPO₄ (s) as a hydrated phosphateREE phosphate solubility products can be as low as 10⁻25 (RIVM report citing Liu and Byrne 1997)
    lake water after lanthanum-modified bentonite, alkalinity above 0.8 meq/LLa³⁺ below 0.0004 mg/L (modelled); La bound as rhabdophane LaPO₄.nH₂O in the sedimentin very low alkalinity lakes modelled La³⁺ reached 0.12 mg/L, which is where the ecotoxicity concern sits
    Solubility
    Lanthanum fluoride, carbonate and phosphate control solubility (carbonate most at high pH); total dissolved La in Dutch surface water about 1 µg/L or less; free ion 0.3 fM to 9 pM (RIVM citing Maas and Botterweg 1993). REE phosphate solubility products can be as low as 10⁻25.
    Hydrolysis
    Hydrolysis of La³⁺ is minor in natural water; the hydroxide La(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
    LaPO₄.nH₂O (rhabdophane, confirmed by NMR and EXAFS in treated lake sediments, with monazite LaPO₄ in the oldest), LaF₃ near fluoride rich discharges, La₂(CO₃)₃ at high pH, La(OH)₃ only under lime.
    LaX3++COX3X2LaCOX3X+\ce{La^3+ + CO3^2- -> LaCO3^+}
    circumneutral pH; the first carbonate complex
    LaX3++2COX3X2La(COX3)X2X\ce{La^3+ + 2 CO3^2- -> La(CO3)2^-}
    alkaline pH; the dicarbonate anion, strongest for the heavy lanthanides
    LaX3++SOX4X2LaSOX4X+\ce{La^3+ + SO4^2- -> LaSO4^+}
    acid, sulfate rich water; above 90 percent of the dissolved element at pH 3.1 to 3.4
    LaX3++POX4X3LaPOX4(s)\ce{La^3+ + PO4^3- -> LaPO4 (s)}
    phosphate present; the solid that caps solubility and that phosphate binders rely on
    LaX3++3FXLaFX3(s)\ce{La^3+ + 3 F^- -> LaF3 (s)}
    fluoride rich phosphogypsum discharge; the first solid to form near the outfall, phosphate taking over as pH rises further away

    4 · Role in treatment

    as a problem
    river contamination from catalyst manufacture
    spent or off-specification fluid catalytic cracking catalyst effluent carries dissolved La at mg/kg level; the Rhine's REE inventory became dominated by anthropogenic La
    the Rhine plant effluent La was above concentrations at which ecotoxicological effects have been observed; 1 L of effluent in 100,000 L of river water reproduces the downstream signal
    lanthanum release after in-lake dosing
    lanthanum-modified bentonite (about 5 percent La in a clay matrix) sheds filterable La for weeks; humic substances and competing oxyanions reduce its phosphate binding, and low alkalinity water leaves more free La³⁺
    saline waters need a separate risk evaluation because of possible La release (Copetti review)
    as a reagent
    phosphate inactivation in lakes and reservoirs: lanthanum-modified bentonite
    La³⁺ held in the clay binds filterable reactive phosphate as rhabdophane; the clay settles and caps sediment phosphorus release
    LaX3++POX4X3LaPOX4(s)\ce{La^3+ + PO4^3- -> LaPO4 (s)}
    about 200 environments treated worldwide; La to P molar ratio in treated sediments generally above 1; phosphorus retention held 2 to 9 years after treatment in 8 of 10 European lakes; efficiency limited by humic substances and competing oxyanions
    phosphate adsorbents for wastewater polishing: lanthanum oxide, hydroxide and carbonate on carbon, clay, silica, polymer and industrial waste carriers
    ligand exchange, electrostatic attraction, Lewis acid-base interaction and surface precipitation of lanthanum phosphate; Langmuir isotherms, pseudo second order kinetics
    regeneration with acid, alkali or salt-alkali; spent adsorbent proposed as slow release fertiliser

    5 · Removal and control

    neutralisation of acid mine drainage (lime, caustic or passive alkaline systems)
    La leaves solution with the iron, aluminium and manganese hydroxides and hydroxysulfates as pH rises
    coal mine drainage precipitates carry about 724 g of 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
    conventional drinking water treatment
    Dutch works reduced raw groundwater REE to below detection in nearly all cases
    1990s data
    Efficiency
    to below detection, with the three exceptions at 8 to 14 µg/L

    6 · Analytics

    methodstandarddetection limitnote
    ICP-MSISO 17294-2:2023not read; the standard covers drinking, surface, ground and waste waterlanthanum 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. A positive La anomaly (La normalised to shale against its neighbours) of more than 1.5 was the thesis's conservative threshold for calling La anthropogenic.

    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. Kulaksiz and Bau note that the catalyst plant effluent La exceeds concentrations with reported ecotoxicological effects; Herrmann et al. (2016) found no regulatory thresholds for REE anywhere and made preliminary water and sediment quality suggestions (values not read). Anthropogenic La is bioavailable to freshwater mussels.
    Bioaccumulation
    Field bioconcentration factors in Rhine estuary amphipods fall from the light to the heavy lanthanides (La 28,840 to Lu 4,786; La 28,840); 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 10.1 µg/L in fresh surface water and 1.01 µg/L in salt water (negligible concentrations 0.18 and 0.02 µg/L), derived as MPA 10 µg/L from the lowest NOEC divided by 10 (fresh); lowest LC₅₀ divided by 1000 (salt) plus a background set at the detection limit (0.08 µg/L). Acute data behind it: Daphnia magna 48 h EC₅₀ 24 mg/L, zebrafish 96 h LC₅₀ 23 mg/L, alga 72 h EC₅₀ 1.3 mg/L; chronic: Daphnia magna 21 d NOEC 0.1 mg/L, carp 21 d NOEC 0.26 mg/L, alga 72 h NOEC 1.4 mg/L. Field bioconcentration factor in amphipods (porewater basis) 28,840. Lanthanum concentrations during lanthanum-modified bentonite applications are generally below acute thresholds except in low alkalinity waters (Copetti review).

    Flags

    • Dutch groundwater and drinking water figures are 1991 to 1994 data compiled by RIVM in 2000.
    • The Rhine figures are single sampling campaigns with a point source; they are not a river background.
    • The RIVM MPCs are environmental risk limits from a 2000 report, mostly LC₅₀ divided by 1000, with background set at the detection limit; they are not permit limits.
    • The lanthanum-modified bentonite figures are maxima across 16 lakes; the modelled La³⁺ values depend on the speciation code used.
    • The Spears 2013 title carries a product name; it is not written here.
    • The 5 percent lanthanum content of the modified bentonite comes from a search summary of the Copetti review, not from the abstract read.

    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.
    • Lanthanum carbonate as an oral phosphate binder (a pharmaceutical) was not read; its excretion route into sewage is not described.
    • No removal percentage for lanthanum in activated sludge was read.
    • Herrmann et al. 2016 proposed water and sediment quality criteria for lanthanum; the values are in the full text, which was not read.

    Sources

    The Element Book, lanthanum entry (data/elements/La.json and data/reference/text/La.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
    Kulaksiz, S. and Bau, M., Rare earth elements in the Rhine River, Germany: first case of anthropogenic lanthanum as a dissolved microcontaminant in the hydrosphere, Environment International 37 (2011) 973 to 979 (abstract read via PubMed 21458860)
    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)
    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)
    Spears, B. M. et al., Lake responses following lanthanum-modified bentonite clay application: an analysis of water column lanthanum data from 16 case study lakes, Water Research 47 (2013) 5930 to 5942 (abstract, PubMed 23911225)
    Dithmer, L. et al., Responses in sediment phosphorus and lanthanum concentrations and composition across 10 lakes following applications of lanthanum modified bentonite, Water Research 97 (2016) 101 to 110 (abstract, PubMed 26971297)
    Copetti, D. et al., Eutrophication management in surface waters using lanthanum modified bentonite: a review, Water Research 97 (2016) 162 to 174 (abstract, PubMed 26706125)
    Phosphate removal and recovery by lanthanum-based adsorbents: a review for current advances, Chemosphere (2022) (abstract, PubMed 35597457)
    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)
    Merschel, G. and Bau, M., Rare earth elements in the aragonitic shell of freshwater mussel Corbicula fluminea and the bioavailability of anthropogenic lanthanum, samarium and gadolinium in river water, Science of the Total Environment 533 (2015) 91 to 101 (abstract via Europe PMC)
    Herrmann, H., Nolde, J., Berger, S. and Heise, S., Aquatic ecotoxicity of lanthanum: a review and an attempt to derive water and sediment quality criteria, Ecotoxicology and Environmental Safety 124 (2016) 213 to 238 (abstract, PubMed 26528910)
    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)
    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

    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.