Lanthanum
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.
| matrix | typical range | note |
|---|---|---|
| groundwater | below detection to 2 µg/Lregion-dependent; 1991 data | Dutch groundwater at pH 6.2 or above; up to 105 µg/L in acidic groundwater below pH 6.2 |
| surface water, rivers | 1.91 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 |
| seawater | 8.57 to 50.2 pmol/Lone station | western Pacific, 3 to 5663 m; concentrations rise with depth |
| drinking water | below 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 wastewater | 49 mg/kgone plant, one sampling | effluent 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 bentonite | 0.026 to 2.30 mg/Lmaxima, not means | post-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.
| condition | dominant species | note |
|---|---|---|
| acid mine drainage and acidic groundwater, pH below 5 | La³⁺, 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 9 | LaCO₃⁺, La(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 | LaPO₄ (s) as a hydrated phosphate | REE 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/L | La³⁺ below 0.0004 mg/L (modelled); La bound as rhabdophane LaPO₄.nH₂O in the sediment | in 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.
4 · Role in treatment
5 · Removal and control
- Efficiency
- not quoted as a percentage
- Efficiency
- to below 2 to 4 ng/L
- Efficiency
- to below detection, with the three exceptions at 8 to 14 µg/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 | lanthanum 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. 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.
| 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. 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
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
Identity
- Name and symbol
- Lanthanum, La
- Atomic number
- 57 protons
- Position
- no group (f-block) · period 6 · f-block · lanthanide
- CAS number
- 7439-91-0
Atomic structure
- Atomic mass
- 138.905 u
- Electron configuration
- 1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 5d¹
[Xe] 6s²⁵d¹ - Electrons per shell
- 2, 8, 18, 18, 9, 2
- Valence electrons
- 3 ns, (n-1)d and (n-2)f
| isotope | mass (u) | abundance |
|---|---|---|
| 138La | 137.907 12(2) | 0 % |
| 139La | 138.906 36(2) | 99.9 % |
Physical properties
- State at room temperature
- Solid
- Melting point
- 1,191 K (917.85 °C)
- Boiling point
- 3,737 K (3,463.85 °C)
- Density
- 6.15 g/cm3
- Appearance
- silvery white
- Thermal conductivity
- 13.4 W/(m·K)
- Electrical resistivity
- α, poly: 615 nΩ·m
- Electrical conductivity
- 1.63 MS/m
- Crystal structure
- double hexagonal close packed
- Molar heat capacity
- 27.11 J/(mol·K)
Chemical properties
- Oxidation states
- +3
- Electronegativity
- 1.1 (Pauling Scale)
- Ionisation energy
- 5.577 eV
1st 538.1, 2nd 1,067, 3rd 1,850.3 kJ/mol - Electron affinity
- 0.5 eV
- Atomic radius
- empirical 207, covalent 207, van der Waals 240 pm
- Ionic radius
- La³⁺ 103 pm
- Reactivity
- One of the most reactive of the rare-earth metals, soft enough to cut with a knife: it tarnishes within hours in air, the oxide spalls off so a small piece corrodes completely in a year, and it reacts directly with water, the halogens and most non-metals.
- with water
- Attacked slowly by cold water and much faster by hot water, giving lanthanum hydroxide and hydrogen: .
- with oxygen, air
- Oxidises rapidly in air, turning dark within hours, and burns readily to the strongly basic sesquioxide: .
- with acids
- Dissolves readily in dilute acids to colourless La3+ salts and hydrogen: ; hydrofluoric acid forms a protective LaF3 layer instead.
- with halogens
- Reacts with the halogens even at room temperature to the trihalides: .
- Typical compounds
- La₂O₃ lanthanum(III) oxide optical glass for camera and telescope lenses
- LaF₃ lanthanum fluoride reduced with calcium for the metal; fluoride electrodes
- LaCl₃ lanthanum chloride typical trihalide, deliquescent
- La(OH)₃ lanthanum hydroxide product of the water reaction
- LaNi₅ lanthanum nickel hydrogen-storage alloy in NiMH batteries
- La₂(CO₃)₃ lanthanum carbonate phosphate binder drug for kidney disease
Occurrence, production and use
- Crustal abundance
- 3.9×101 milligrams per kilogram
- Oceanic abundance
- 3.4×10-6 milligrams per liter
- Occurrence and sources
Lanthanum is found in rare-earth minerals such as cerite, monazite, allanite, and bastnasite. Monazite and bastnasite are principal ores in which lanthanum occurs in percentages up to 25 percent and 38 percent respectively. Misch metal, used in making lighter flints, contains about 25 percent lanthanum.
The availability of lanthanum and other rare earths has improved greatly in recent years. The metal can be produced by reducing the anhydrous fluoride with calcium.
- monazite, a rare earth phosphate (about 25 percent lanthanum) heavy-mineral-sand concentrates, stockpiled as a separated concentrate or an accessory mineral in the southeastern United States; the principal thorium mineral
- bastnaesite, a rare earth fluorocarbonate (about 38 percent lanthanum) mined as a primary product at Mountain Pass, California; the main Chinese deposits are not itemised by the source
- rare earth metals (mainly lanthanum, cerium, praseodymium, neodymium) carried with phosphate rock into wet-process phosphoric acid and discharged with phosphogypsum reported emission to water on disposal of phosphogypsum: 2,200 g and 360 g of rare earth metals per tonne P2O5 at two plants (HDH-1 and HDH-2 processes, 1996/97 data, plants since closed because of the discharge to sea); Table 5.8 of the LVIC-AAF BREF, PDF p253, printed p225; the ledger's chemical chapter holds this under the phosphoric-acid hub
- Extraction, production
- Separation of the rare earths from monazite or bastnaesite concentrates by ion exchange and solvent extraction
no balanced equation is printed by the sources; the oxide and chloride are the traded intermediates
Reduction of anhydrous lanthanum fluoride with calcium to the metalthe usual route to lanthanum metal; stoichiometry not printed by the source, so no equation is written
- Uses
Lanthanum is one of the rare earth elements used to make carbon arc lights which are used in the motion picture industry for studio lighting and projector lights. Lanthanum also makes up about 25% of Misch metal, a material that is used to make flints for lighters. Lanthana (La2O3) is used to make the glass used in camera lenses and in other special glasses.
Rare-earth compounds containing lanthanum are extensively used in carbon lighting applications, especially by the motion picture industry for studio lighting and projection. This application consumes about 25 percent of the rare-earth compounds produced. La2O3 improves the alkali resistance of glass, and is used in making special optical glasses. Small amounts of lanthanum, as an additive, can be used to produce nodular cast iron.
There is current interest in hydrogen sponge alloys containing lanthanum. These alloys take up to 400 times their own volume of hydrogen gas, and the process is reversible. Every time they take up the gas, heat energy is released; therefore these alloys have possibilities in an energy conservation system.
- Petroleum refining catalysts: lanthanum salts in catalysts for petroleum refining catalysts were the estimated leading United States end use of rare earths in 2024 (usgs-mcs2025, PDF p148, printed p144)
- Batteries and hydrogen storage: lanthanum-nickel alloy anodes of nickel metal hydride batteries in hybrid cars; lanthanum-nickel alloy for storing hydrogen gas limited quantities of rare earths were recovered from batteries in the United States in 2024 (usgs-mcs2025)
- Glass and optics: lanthanum(III) oxide in special optical glass, raising the refractive index and alkali resistance for camera and telescope lenses ceramics and glass were among the United States end uses of rare earths in 2024 (usgs-mcs2025)
- Steel and metallurgy: mischmetal (about 20 percent lanthanum in the RSC account; 65 percent cerium and 35 percent lanthanum in the USGS price grade) for lighter flints and pyrophoric alloys; small additions to iron and steel to reduce brittleness and to tungsten for arc-welding electrodes mischmetal averaged about 5 dollars per kilogram in 2024 (usgs-mcs2025, PDF p148, printed p144)
- Rare earth mining and separation: mined as bastnaesite (a rare-earth fluorocarbonate) at Mountain Pass, California, and as monazite (a phosphate) in heavy-mineral-sand concentrates; separated from the other rare earths by ion exchange and solvent extraction world mine production of rare earths 390,000 t of rare-earth-oxide equivalent in 2024 (USGS estimate), of which China 270,000 t (production quota), the United States 45,000 t, Burma 31,000 t, Australia, Nigeria and Thailand 13,000 t each; reserves over 90 million t, China 44 million t, Brazil 21 million t (usgs-mcs2025, PDF p149, printed p145)
- Safety, toxicity
Lanthanum and its compounds have a low to moderate acute toxicity rating; therefore, care should be taken in handling them.
GHS classification, signal word Danger- H228 Flammable solid Flammable solids
- H260 In contact with water releases flammable gases which may ignite spontaneously Substances and mixtures which in contact with water, emit flammable gases
Discovery and name
- Discovered by
- Carl Gustaf Mosander
- Discovered
- 1838
- First isolated
- not in sources
- Named by
- not in sources
- Origin of the name
- from the Greek λανθάνειν, "to lie hidden", for 'hiding' in cerite
Lanthanum is silvery white, malleable, ductile, and soft enough to be cut with a knife. It is one of the most reactive of the rare-earth metals. It oxidizes rapidly when exposed to air. Cold water attacks lanthanum slowly, while hot water attacks it much more rapidly.
The metal reacts directly with elemental carbon, nitrogen, boron, selenium, silicon, phosphorus, sulfur, and with halogens.
At 310°C, lanthanum changes from a hexagonal to a face-centered cubic structure, and at 865°C it again transforms into a body-centered cubic structure.
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.