Thorium
fullThorium is regulated only through its radioactivity, with WHO guidance levels of 1 Bq/L for thorium-228, -230 and -232 and the gross alpha screen in the US and EU, and in practice it is never the problem: Th(IV) hydrolyses above pH 3, hydrous thorium oxide holds dissolved thorium below about 1 µg/L, and sorption to iron and manganese oxides and humics takes the rest, so fresh water rarely exceeds 1 µg/L (0.1 pCi/L of thorium-232) while acidic uranium tailings leachate can carry milligrams per litre; the industrial sources are uranium and rare earth processing, monazite sands and phosphate.
Typical wastewaters
- uranium and thorium mining, milling and tailings (acid leachate) Th⁴⁺ with ThSO₄²⁺ and fluoro complexes at low pH; up to 38 mg/L thorium, probably thorium-230, in acidic uranium tailings water and milligrams per litre of thorium-232 in high acid groundwater beneath tailings thorium-230, not thorium-232, is the isotope to measure near uranium mills
- phosphate rock processing and phosphate fertiliser manufacture Th(IV), hydrolysed and particulate at neutral pH; named by ATSDR among the major industrial releases to surface water no concentration read
- tin processing Th(IV), hydrolysed and particulate; named by ATSDR among the major industrial releases to surface water no concentration read
- monazite and zircon sand processing (legacy sites) particulate and sorbed Th(IV) in surface water and groundwater at Superfund and NRC decommissioning sites thorium contamination identified at 21 of 45 Superfund NPL sites and 23 of 38 NRC decommissioning sites
- drinking water treatment residuals (NORM scale, softening and iron removal sludge) thorium and its daughters trapped in solids depositing on sediment and pipe walls, building up over time; radium-228 and thorium-228 join radium-226 in the sludge on the solids rather than in a liquid effluent
1 · Identity
- Symbol, number
- Th, 90
- Oxidation states in water
- +4 only, as Th⁴⁺ below pH 3.5, then the hydroxo complexes Th(OH)₂²⁺, Th(OH)₃⁺ and Th(OH)₄ (aq), and above pH 7.5 the carbonate complex Th(OH)₃CO₃⁻ (EPA Kd volume II). Natural thorium is essentially thorium-232 (half life 1.41 x 10^10 years); thorium-230 (8.0 x 10^4 years) and thorium-234 (24.1 days) come from the uranium-238 chain and thorium-228 (1.913 years) from the thorium-232 chain.
- Note
- The element entry covers monazite, thoria and the reactor hopes. This chapter is about why Th⁴⁺ stays in the sediment and what the radiological limits are.
2 · Occurrence in water
- Natural sources
- Thorite, thorianite, monazite and zircon resist weathering and do not dissolve at low temperature; what dissolves is capped by hydrous thorium oxide and by sorption (EPA Kd volume II). Fresh water rarely exceeds 1 µg/L; the US population weighted averages in community supplies were below 0.01 pCi/L thorium-232 and below 0.04 pCi/L thorium-230 (ATSDR, citing Cothern). Thorium-232 rarely exceeds 0.1 pCi/L in natural waters and thorium-230 can reach 0.4 pCi/L; Austrian surface water carried 1.24 to 2.90 µg/L and Austrian groundwater 0.5 to 2.90 µg/L; alkaline Mono Lake reached 1.02, 1.41 and 0.7 pCi/L of thorium-228, -230 and -232 (ATSDR).
- Anthropogenic sources
- Uranium and thorium mining, milling and processing, tin processing, phosphate rock processing and phosphate fertiliser production are the major industrial releases to surface water (ATSDR); acidic leaching of uranium tailings mobilises thorium-230 and thorium (probably thorium-230) has reached 38 mg/L in low pH tailings water (ATSDR), with milligram per litre thorium-232 in high acid groundwater beneath tailings (EPA Kd volume II). Thorium contamination of soil, surface water or groundwater was identified at 21 of 45 Superfund NPL sites and 23 of 38 NRC decommissioning sites, some from monazite and zircon sand processing (EPA Kd volume II). The MWEI BREF data collection had no operator monitoring thorium in extractive waste water (element entry).
| matrix | typical range | note |
|---|---|---|
| fresh water, general | 0.01 to 1 µg/L | Hem 1985 range quoted by EPA; rarely exceeds 1 µg/L, about 0.1 pCi/L thorium-232 |
| drinking water, US community supplies | below 0.01 (thorium-232); below 0.04 (thorium-230) pCi/L1980s data | population weighted averages, surface and groundwater derived (Cothern 1986, 1987 via ATSDR) |
| surface water and groundwater, Austria | 1.24 to 2.90 (surface); 0.5 to 2.90 (groundwater) µg/Lregion-dependent; 1980 data | Harmsen and De Haan 1980 via ATSDR; isotope undefined |
| seawater | 0.00004 to below 0.5 µg/kg old compilation; the low end is the modern measured level | world average 0.05 µg/L (Harmsen and De Haan 1980 via ATSDR); dissolved thorium in seawater about 1.3 x 10⁻5 dpm/L against up to 4.9 dpm/L in an alkaline lake |
| acidic uranium tailings water | up to 38 mg/Lextreme low pH case | isotope undefined but probably thorium-230 (Harmsen and De Haan 1980 via ATSDR); mg/L thorium-232 in high acid groundwater beneath tailings (Langmuir and Herman 1980 via EPA) |
3 · Speciation
Th⁴⁺ is the largest tetravalent cation and hydrolyses above pH 3: in pure water the uncomplexed ion dominates below pH 3.5 and then Th(OH)₂²⁺, Th(OH)₃⁺ and Th(OH)₄ (aq) in turn, the last two over the widest pH range. In a typical river water fluoride complexes dominate below pH 5, phosphate complexes between 5 and 7 (constants suspect), and above pH 7.5 more than 95 percent of dissolved thorium is Th(OH)₃CO₃⁻ (EPA Kd volume II). Hydrous thorium oxide caps dissolved thorium at about 10⁻8.5 to below 10⁻9 mol/L (0.0007 to 0.0002 mg/L) between pH 5 and 10 in 0.1 M perchlorate, rising to about 600 mg/L as pH falls from 5.0 to 3.2, and its solubility rises by two to three orders of magnitude in 3 M chloride and dramatically in high carbonate (EPA Kd volume II). Goethite and manganese dioxide sorb thorium from 0 percent at pH 2.5 to 3.5 to 90 to 100 percent at pH 5 to 6.5; sulfate lowers sorption and 100 meq/L carbonate alkalinity or EDTA lifts it off again, so carbonate rich alkaline water and organic rich water are where thorium moves (EPA Kd volume II). Humic and citrate, oxalate and EDTA complexes can dominate in organic rich water; ThEDTA (aq) dominates from pH 2 to 8 at the concentrations Langmuir and Herman considered.
| condition | dominant species | note |
|---|---|---|
| acid, below pH 3.5, tailings leachate | Th⁴⁺, ThSO₄²⁺, ThF³⁺, ThF₂²⁺ | the mobile case; hydrous oxide solubility hundreds of mg/L at pH 3.2 |
| river water, pH 5 to 7 | thorium phosphate complexes such as Th(HPO₄)₃²⁻ (constants suspect), Th(OH)₃⁺, Th(OH)₄ (aq) | sorbed to Fe and Mn oxides and humics |
| pH above 7.5, carbonate bearing water | Th(OH)₃CO₃⁻, Th(CO₃)₅⁶⁻ | more than 95 percent as the hydroxo carbonate; carbonate desorbs thorium from goethite |
| organic rich water | thorium humate, ThEDTA (aq), citrate and oxalate complexes | organic complexes likely predominate over inorganic ones |
- Solubility
- Hydrous thorium oxide about 10⁻8.5 to below 10⁻9 mol/L at pH 5 to 10 in 0.1 M NaClO₄, up to 10⁻2.6 mol/L (600 mg/L) at pH 3.2; higher in brines and in carbonate; crystalline ThO₂, thorite and monazite far lower and kinetically inert (EPA Kd volume II).
- Hydrolysis
- Begins above pH 3; polynuclear species Th₂(OH)₂⁶⁺, Th₄(OH)₈⁸⁺ and Th₆(OH)₁₅⁹⁺ are believed to matter at higher concentration (EPA Kd volume II).
- Complexation
- Fluoride, phosphate, sulfate, chloride weak, carbonate strong at high pH, humics and chelants strongest (EPA Kd volume II).
- Precipitates
- Hydrous thorium oxide, ageing to ThO₂; thorium phosphate in phosphate rich water; thorium carried in Fe and Mn oxide sludge.
4 · Role in treatment
5 · Removal and control
- Efficiency
- not read for thorium specifically
- Interferences
- high carbonate alkalinity, sulfate, EDTA and humics keep thorium dissolved
- Efficiency
- not read
- Interferences
- the sludge is NORM
6 · Analytics
| method | standard | detection limit | note |
|---|---|---|---|
| ICP-MS, mass 232 | EPA 200.8 (thorium is a listed analyte); ISO 17294-2 | estimated instrument detection limit 0.03 µg/L scanning and 0.005 µg/L selected ion monitoring (EPA 200.8 Table 1) | measures thorium-232 mass, which can be converted to activity; thorium-230 and -228 need alpha spectrometry |
| gross alpha screening | ISO 9696, ISO 10704; WHO Table 9.3 | 0.02 to 0.1 Bq/L; Euratom 0.04 Bq/L | thorium isotopes count in gross alpha; the WHO screening level is 0.5 Bq/L, Euratom 0.1 Bq/L, US 15 pCi/L |
| isotopic thorium by alpha spectrometry after separation | method number not read | not read | needed to separate thorium-230 (uranium chain) from thorium-228 and -232 |
- Sampling pitfalls
- Thorium sorbs to bottle walls and particles within minutes at neutral pH: acidify at collection, and filter first only if dissolved thorium is the question. Old thorium Kd values were inflated by precipitation of hydrous thorium oxide during the test (EPA), and the same happens in a spiked sample.
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 |
|---|---|---|
| WHO GDWQ chapter 9 Table 9.2 and Annex 6 Table A₆.1 | 1 (thorium-228, -230, -232); 10 (thorium-227); 100 (thorium-234); 0.1 (thorium-229) Bq/L | guidance levels; dose coefficients 7.2 x 10⁻8 (Th-228), 2.1 x 10⁻7 (Th-230) and 2.3 x 10⁻7 Sv/Bq (Th-232); screening levels 0.5 Bq/L gross alpha and 1 Bq/L gross beta; thorium is not a chemical parameter in Annex 3; the isotopes beyond the chapter 9 table are from Annex 6 Table A₆.1 |
| EU Directive 2013/51/Euratom, Annex III | not set | no thorium isotope in the derived concentration table; caught by the recommended 0.1 Bq/L gross alpha screening level |
| US EPA NPDWR | 15 pCi/L | gross alpha MCL excluding radon and uranium, MCLG zero; no thorium specific MCL and EPA does not require thorium to be measured (ATSDR) |
| body | limit | note |
|---|---|---|
| EU CWW BREF BAT-AEL (Decision 2016/902) | not set | no radioactivity or thorium parameter |
8 · Health and environmental effects
- Toxicity
- Radiological: bone seeking alpha emitters with ingestion dose coefficients of 7.2 x 10⁻8 to 2.3 x 10⁻7 Sv/Bq (WHO Table 9.2); chemical toxicity is not the basis of any limit. Thorium compounds are not readily absorbed by the body and intakes from water are very low (ATSDR).
- Bioaccumulation
- Plant to soil transfer ratio below 0.01 (ATSDR); thorium concentrates in sediment (0.5 to 31 pCi/g of the three isotopes) rather than in water.
- Ecotoxicity
- Not addressed in the sources read.
Flags
- Most concentration data are 1980s compilations quoted by ATSDR and EPA; no modern survey of thorium in water was read.
- The thorium phosphate constants are suspect and may over predict those complexes, as EPA itself notes.
- The hydrolysis equations are net reactions written from the species distribution, with constants from Stumm and Morgan chapter 6 not re-read.
- The Euratom values were read from the retained UK copy of the directive on legislation.gov.uk.
- EPA 200.8 gives an instrument detection limit for thorium, not a method detection limit; Table 7 was not located in the text read.
Gaps
- No measured thorium concentration in municipal wastewater, rare earth processing effluent or monazite plant effluent was read; the ledger's mining chapter and the MWEI BREF note that no operator monitored it.
- No thorium specific removal efficiency was read; WHO Table 9.4 has no thorium row.
- Alpha spectrometry method numbers for isotopic thorium were not read.
- No aquatic toxicity value was read.
- No GCC discharge standard was read; radioactive waste is prohibited to sewer in Abu Dhabi per the Ra chapter, not re-read here.
- No surface species or surface complexation constants for thorium on goethite or manganese dioxide were read, so the coagulation row carries no equation.
Sources
ATSDR, Toxicological Profile for Thorium (2019), chapter 5 Potential for human exposure (NCBI Bookshelf NBK591328)
WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first addendum, chapter 9 Radiological aspects (Tables 9.2 to 9.4, section 9.6) and Annex 6 Table A6.1 of the 2022 edition
WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first and second addenda (2022), Annex 6 Supporting information on radionuclides, Table A6.1 (NCBI Bookshelf)
Council Directive 2013/51/Euratom, Annex III (screening levels, derived concentrations, limits of detection), read in the retained UK copy on legislation.gov.uk
US EPA, National Primary Drinking Water Regulations (table of MCLs and MCLGs, radionuclides)
US EPA Method 200.8, Revision 5.4 (1994), Determination of trace elements in waters and wastes by ICP-MS, Table 1 estimated instrument detection limits
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
Stumm, W. and Morgan, J. J., Aquatic Chemistry, 3rd ed. (Wiley, 1996), chapter 6 (hydrolysis of metal ions)
The Element Book, element entry and reference text for Th (data/elements/Th.json, data/reference/text/Th.json)
Identity
- Name and symbol
- Thorium, Th
- Atomic number
- 90 protons
- Position
- no group (f-block) · period 7 · f-block · actinide
- CAS number
- 7440-29-1
Atomic structure
- Atomic mass
- 232.0377 u
- Electron configuration
- 1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹⁴ 5d¹⁰ 6p⁶ 7s² 6d²
[Rn] 7s²⁶d² - Electrons per shell
- 2, 8, 18, 32, 18, 10, 2
- Valence electrons
- 4 ns, (n-1)d and (n-2)f
| isotope | mass (u) | abundance |
|---|---|---|
| 230Th | 230.033 132(8) | 0.02 % |
| 232Th | 232.038 05(1) | 99.98 % |
Physical properties
- State at room temperature
- Solid
- Melting point
- 2,023 K (1,749.85 °C)
- Boiling point
- 5,061 K (4,787.85 °C)
- Density
- 11.72 g/cm3
- Appearance
- silvery
- Thermal conductivity
- 54.0 W/(m·K)
- Electrical resistivity
- 157 nΩ·m at 0 °C
- Electrical conductivity
- 6.37 MS/m
- Crystal structure
- facecentredcubic
- Molar heat capacity
- 26.23 J/(mol·K)
Chemical properties
- Oxidation states
- +4
- Electronegativity
- 1.3 (Pauling Scale)
- Ionisation energy
- 6.08 eV
1st 587, 2nd 1,110, 3rd 1,930 kJ/mol - Electron affinity
- not in sources
- Atomic radius
- empirical 206, covalent 206, van der Waals 237 pm
- Ionic radius
- Th⁴⁺ 94 pm
- Reactivity
- A highly reactive, electropositive actinide (Th4+/Th at -1.90 V, more electropositive than zirconium) that behaves like a heavier zirconium or hafnium: +4 in essentially all its chemistry, colourless diamagnetic Th4+, and a metal that is slow to corrode when pure and bulk but pyrophoric when powdered.
- with water
- Slowly attacked by water at ordinary temperature, and more quickly by steam, giving the dioxide and hydrogen: , the oxide film then slowing further attack.
- with oxygen, air
- Pure bulk thorium keeps its lustre for months in air, but oxide-contaminated metal tarnishes grey then black, turnings ignite when heated and burn with a brilliant white light: , and the powder is pyrophoric.
- with acids
- Does not dissolve readily in most common acids; hydrochloric acid is the exception and dissolves it: , while nitric acid passivates it unless a little fluoride is present.
- with halogens
- Reacts with the halogens on heating to the tetrahalides: , the fluoride ThF4 being the compound reduced with calcium to make the metal.
- Typical compounds
- ThO₂ thorium dioxide thoria, highest melting oxide (3300 C), gas mantles and crucibles
- ThF₄ thorium tetrafluoride reduced with calcium to give the metal
- ThCl₄ thorium tetrachloride from the metal and chlorine or hydrochloric acid
- Th(NO₃)₄ thorium nitrate soluble salt of the monazite processing route
- ThSiO₄ thorium silicate the mineral thorite
Occurrence, production and use
- Crustal abundance
- 9.6 milligrams per kilogram
- Oceanic abundance
- 1×10-6 milligrams per liter
- Occurrence and sources
Thorium-232 is a primordial nuclide, having existed in its current form for over 4.5 billion years, a half-life is comparable to the age of the Universe and thus predating the formation of the Earth. Thorium was forged in the cores of dying stars through the r-process and scattered across the galaxy by supernovas. Thorium is found in small amounts in most rocks and soils. Soil commonly contains an average of around 6 parts per million (ppm) of thorium. Thorium occurs in several minerals including thorite (ThSiO4), thorianite (ThO2 + UO2) and monazite. Thorianite is a rare mineral and may contain up to about 12% thorium oxide. Monazite contains 2.5% thorium, allanite has 0.1 to 2% thorium and zircon can have up to 0.4% thorium.[66] Thorium-containing minerals occur on all continents. Thorium is now thought to be about three times as abundant as uranium and about as abundant as lead or molybdenum. Thorium is recovered commercially from the mineral monazite, which contains from 3 to 9% ThO2 along with rare-earth minerals.
- monazite, a rare earth and thorium phosphate the world's primary source of thorium, in heavy-mineral-sand placers, carbonatites and veins; recovered for rare earths, with thorium a by-product mostly left unrecovered; China was the leading importer of monazite, supplied by Nigeria, Madagascar, Thailand and Indonesia (usgs-mcs2025, PDF p186 to 187, printed p182 to 183)
- thorite (thorium silicate), uranothorite and thorianite primary thorium minerals; thorite was the mineral of discovery from Brevig
- trace thorium in phosphate rock reporting to phosphogypsum phosphogypsum from wet-process phosphoric acid is stored indefinitely because of weak radioactivity from naturally occurring uranium and thorium and their daughters radium, radon and polonium; the ledger's chemical chapter holds phosphogypsum under the phosphoric-acid hub
- thorium in mine water no operator reported the monitoring of thorium in extractive waste influenced water in the MWEI BREF data collection (PDF p184, printed p156)
- Extraction, production
- By-product recovery from monazite concentrates; the source does not print the leach chemistry
world production and reserves are associated with monazite recovery in heavy-mineral-sand deposits; thorium consumption worldwide is small compared with most mineral commodities (usgs-mcs2025)
Thorium metal by reducing thorium oxide with calcium, or by electrolysis of the fluorideno balanced equation printed by the source
- Uses
Thorium is used as an alloying agent to improve magnesium's strength at high temperatures. Thorium is also used to coat tungsten filaments used in electronic devices, such at television sets. When bombarded with neutrons, thorium-232 becomes thorium-233, which eventually decays into uranium-233 through a series of beta decays. Uranium-233 is a fissionable material and can be used as a nuclear fuel.
Thorium oxide (ThO2), one of thorium's compounds, has many uses. It is primarily used in a type of lantern mantel known as a Welsbach mantle. This mantle, which also contains about 1% cerium oxide, glows with a bright white light when it is heated in a gas flame. Thorium oxide has a very high melting point, about 3300°C, and is used to make high temperature crucibles. Thorium oxide is also used to make glass with a high index of refraction that is used to make high quality camera lenses. Thorium oxide is used as a catalyst in the production of sulfuric acid (H2SO4), in the cracking of petroleum products and in the conversion of ammonia (NH3) to nitric acid (HNO3).
Thorium's most stable isotope, thorium-232, has a half-life of about 14,050,000,000 years. It decays into radium-228 through alpha decay or decays through spontaneous fission.
The principal historic use of thorium has been in the preparation of the Welsbach mantle, used for portable gaslights. These mantles, consisting of thorium oxide with about 1% cerium oxide and other ingredients, glow with a dazzling light when heated in a gas flame. Thorium is an important alloying element in magnesium, imparting high strength and creep resistance at elevated temperatures. Because thorium has a low work-function and high electron emission, it is used to coat tungsten wire used in electronic equipment. The oxide is also used to control the grain size of tungsten used for electric lamps; it is also used for high-temperature laboratory crucibles. Glasses containing thorium oxide have a high refractive index and low dispersion. Consequently, they find application in high quality lenses for cameras and scientific instruments. Thorium oxide has also found use as a catalyst in the conversion of ammonia to nitric acid, in petroleum cracking, and in producing sulfuric acid. Thorium metal is a source of nuclear power. There is probably more energy available for use from thorium in the minerals of the earth's crust than from both uranium and fossil fuels. Any sizable demand from thorium as a nuclear fuel is still several years in the future. Work has been done in developing thorium cycle converter-reactor systems. Several prototypes, including the HTGR (high-temperature gas-cooled reactor) and MSRE (molten salt converter reactor experiment), have operated. While the HTGR reactors are efficient, they are not expected to become important commercially for many years because of certain operating difficulties.
- Nuclear: candidate fuel for a new generation of reactors; research and development programmes reported in Australia, Belgium, Brazil, Canada, China, Czechia, Denmark, Finland, France, Germany, India, Israel, Italy, Japan, the Republic of Korea, the Netherlands, Norway, Russia, the United Kingdom and the United States; nuclear medicine India and China are developing thorium reactor plants but the technology is still very new (rsc-element-90)
- Electrical and lighting products: magnetrons in microwave ovens; metal-halide lamps; tungsten filaments; welding electrodes domestic (United States) demand for thorium alloys, compounds and metals was limited in 2024 (usgs-mcs2025, PDF p187, printed p183)
- Catalysts, ceramics and coatings: thorium oxide as an industrial catalyst; high-temperature ceramics; optical coatings (thorium fluoride, now largely replaced by yttrium fluoride and proprietary materials); formerly thoriated glass for high-quality camera lenses
- Metallurgy: alloying agent in magnesium for strength and creep resistance at high temperature (a magnesium alloy with lanthanides, yttrium and zirconium now substitutes in aerospace)
- Heavy-mineral-sand and rare earth mining: none as a product: thorium is a by-product of monazite recovered for rare earths and is the reason monazite residues are radioactive exports of unspecified thorium compounds from the United States were 44,100 kg through August 2024 at a unit value of 73 dollars per kilogram (usgs-mcs2025)
- Phosphoric acid and phosphate fertilisers: none as a product: thorium is a trace constituent of phosphate rock that reports to phosphogypsum, listed for the ledger link
- Safety, toxicity
- GHS classification, signal word Danger
- H272 May intensify fire; oxidizer Oxidizing liquids; Oxidizing solids
- H302 Harmful if swallowed Acute toxicity, oral
- H315 Causes skin irritation Skin corrosion/irritation
- H319 Causes serious eye irritation Serious eye damage/eye irritation
- H335 May cause respiratory irritation Specific target organ toxicity, single exposure; Respiratory tract irritation
- H373 May causes damage to organs through prolonged or repeated exposure Specific target organ toxicity, repeated exposure
Discovery and name
- Discovered by
- Jöns Jakob Berzelius
- Discovered
- 1829
- First isolated
- not in sources
- Named by
- not in sources
- Origin of the name
- after Thor, the Norse god of thunder
When pure, thorium is a silvery-white metal that is air-stable and retains its luster for several months. When contaminated with the oxide, thorium slowly tarnishes in air, becoming gray and finally black. The physical properties of thorium are greatly influenced by the degree of contamination with the oxide. The purest specimens often contain several tenths of a percent of the oxide. High-purity thorium has been made. Pure thorium is soft, very ductile, and can be cold-rolled, swaged, and drawn. Thorium is dimorphic, changing at 1400°C from a cubic to a body-centered cubic structure. Thorium oxide has a melting point of 3300°C, which is the highest of all oxides. Only a few elements, such as tungsten, and a few compounds, such as tantalum carbide, have higher melting points. Thorium is slowly attacked by water, but does not dissolve readily in most common acids, except hydrochloric. Powdered thorium metal is often pyrophoric and should be handled carefully. When heated in air, thorium turnings ignite and burn brilliantly with a white light.
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.