Calcium
fullCalcium is hardness: the ion behind carbonate scale, the Langelier index, lime softening and the stabilisation of desalinated water, and, as lime and calcium hypochlorite, the cheapest base and the commonest solid chlorine of the trade; it has no health based limit anywhere.
Typical wastewaters
- lime softening plant residuals calcium carbonate and magnesium hydroxide sludge, plus the lime added; some plants regenerate lime from it
- ion exchange softener regenerant Ca²⁺ and Mg²⁺ in spent brine
- reverse osmosis concentrate and cooling water Ca²⁺ concentrated toward calcium carbonate and gypsum saturation, held off with antiscalant or acid
- lime treated acid effluent and mine water Ca²⁺ with sulfate, capped by gypsum near 2 g/L, so lime treatment leaves 1.5 to 2 g/L sulfate
1 · Identity
- Symbol, number
- Ca, 20
- Oxidation states in water
- +2 only, as the hydrated Ca²⁺ ion and its ion pairs with bicarbonate, carbonate and sulfate; the solids CaCO₃ (calcite, aragonite), CaSO₄.2H₂O (gypsum), Ca(OH)₂ (portlandite, slaked lime), Ca₅(PO₄)₃OH (hydroxyapatite) and CaF₂ (fluorite) set its solubility.
- Note
- The element entry covers limestone, lime burning and the narrative on solubility. This chapter is the carbonate system in practice: when calcium carbonate precipitates, how a saturation index is read, what lime does at pH 10 and 11, and what a desalination plant has to put back.
2 · Occurrence in water
- Natural sources
- Dissolution of limestone, chalk, dolomite and gypsum by carbon dioxide charged rainwater; calcium concentrations up to and exceeding 100 mg/L are common in natural sources, particularly groundwater, and calcium hardness usually predominates over magnesium (WHO hardness document).
- Anthropogenic sources
- Lime and calcium hypochlorite dosing; lime neutralisation of acid effluent and mine water; gypsum from flue gas desulfurisation and phosphoric acid (phosphogypsum) in the ledger's chemical chapter; road salt (calcium chloride); concrete leaching.
| matrix | typical range | note |
|---|---|---|
| groundwater and natural sources | up to and exceeding 100 mg/L as Ca qualitative range, region-dependent | magnesium usually negligible to about 50 mg/L and rarely above 100 mg/L |
| hardness classes (calcium plus magnesium) | soft below 60; moderately hard 60 to 120; hard 120 to 180; very hard above 180 mg/L as CaCO3 | the classification quoted by WHO |
| seawater | 412 mg/Lsingle figure | estimated oceanic abundance, Jefferson Lab figure via PubChem |
3 · Speciation
Calcium is Ca²⁺ at every pH, and its story is the solids it can form. In natural water it sits close to calcium carbonate saturation: warming the water, stripping carbon dioxide or raising pH pushes it over and calcite deposits on heaters, pipes and membranes; cooling, adding acid or carbon dioxide dissolves it. The Langelier saturation index (pH minus the pH at which the water would be saturated with CaCO₃) reads which way the water is tending, positive for scaling and negative for dissolving, and Standard Methods 2330 pairs it with the calcium carbonate precipitation potential, the mass that would actually precipitate. Sulfate rich water is capped instead by gypsum near 2 g/L. Lime softening deliberately drives the water far past saturation at pH 10 to 11.
| condition | dominant species | note |
|---|---|---|
| natural water, pH 6.5 to 8.5 | Ca²⁺ with CaHCO₃⁺, CaCO₃ (aq) and CaSO₄ (aq) ion pairs; calcite at or near saturation | carbonate (temporary) hardness is the calcium matched by bicarbonate, non carbonate (permanent) hardness the rest |
| heated or carbon dioxide stripped water | CaCO₃ (s) scale | the boiler, kettle and heat exchanger deposit |
| lime softening, pH 10 to 11 | CaCO₃ (s) and Mg(OH)₂ (s) sludge; residual Ca²⁺ at the practical solubility limit | recarbonation with CO₂ brings the water back to stability |
| demineralised or desalinated water | almost no calcium; aggressive to cement and metals | stabilised before distribution with lime, limestone or calcium chloride plus carbon dioxide |
| sulfate rich water, brines, reverse osmosis concentrate | gypsum CaSO₄.2H₂O (s) at saturation | a recovery limit alongside silica and calcium carbonate |
- Solubility
- Calcite: log Ks₀ about minus 8.48 at 25 C (Stumm and Morgan chapter 7, from the chapter, not re-read); solubility falls with rising temperature, which is why calcium carbonate scales hot surfaces. Gypsum about 2 g/L. Calcium hydroxide about 1.7 g/L, enough to make lime water a strong base but too little to dose lime as a clear solution at scale, hence lime slurry. Fluorite and hydroxyapatite far less soluble, the basis of fluoride and phosphate removal with lime.
- Hydrolysis
- Negligible; Ca²⁺ is a hard, weakly hydrolysing cation. Quicklime hydrates exothermically to slaked lime, a strong base.
- Complexation
- Ion pairs with bicarbonate, carbonate and sulfate; strong complexes with EDTA and with phosphonate antiscalants (the basis of EDTA titration for hardness and of threshold scale inhibition); calcium binds humic substances and bridges them into floc.
- Precipitates
- CaCO₃ (calcite, aragonite, vaterite), CaSO₄.2H₂O gypsum, Ca(OH)₂ in lime slurry, Ca₅(PO₄)₃OH hydroxyapatite, CaF₂ fluorite, calcium arsenate, calcium silicate and ettringite in lime treated water.
4 · Role in treatment
5 · Removal and control
- Efficiency
- to about 30 to 40 mg/L as CaCO₃ calcium hardness and about 10 mg/L magnesium hardness practical limits (MWH chapter 20, from the chapter, not re-read)
- Interferences
- carbon dioxide demand, sludge volume, post-precipitation if recarbonation is skipped
- Efficiency
- to near zero hardness until breakthrough
- Interferences
- iron and manganese foul the resin; brine disposal; sodium or potassium added
- Efficiency
- not quoted
- Interferences
- scaling limits recovery
- Efficiency
- not quoted
- Interferences
- magnesium is not removed
6 · Analytics
| method | standard | detection limit | note |
|---|---|---|---|
| EDTA titration | Standard Methods 3500-Ca B (calcium) and 2340 C (total hardness); ISO 6059 (calcium plus magnesium) | not read | total hardness is the sum of calcium and magnesium expressed as CaCO₃; EDTA combines first with calcium (method abstracts) |
| ICP-OES | EPA 200.7 (315.887 nm); ISO 11885 | EPA 200.7 instrument detection limit 30 µg/L, total recoverable method detection limit 0.01 mg/L | calcium is not an analyte of EPA 200.8; hardness by calculation from calcium and magnesium (Standard Methods 2340 B) |
| calcium carbonate saturation indices | Standard Methods 2330 | not applicable | Langelier saturation index and calcium carbonate precipitation potential from pH, temperature, alkalinity, calcium and ionic strength |
- Sampling pitfalls
- Calcium is stable in a sample, but the saturation index is not: pH and temperature must be measured in the field, and a supersaturated sample will precipitate calcite in the bottle so that calcium, alkalinity and pH all fall. Acidify samples for total calcium; do not acidify the aliquot used for alkalinity.
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 4th ed. with addenda (2022), hardness | no guideline | not of health concern at levels found; may affect acceptability; insufficient data to propose minimum or maximum mineral concentrations; assessment 1993, revised 2011 |
| EU DWD 2020/2184 | not set | calcium and hardness are not in Annex I; Annex I Part C note allows Member States to set minimum calcium and magnesium or TDS in softened or demineralised water; Annex IV lists calcium among the minerals reported to consumers |
| US EPA | not regulated | absent from the primary and secondary standards |
| body | limit | note |
|---|---|---|
| EU CWW BREF BAT-AEL (Decision 2016/902) | not set | not a BAT 12 parameter |
| Abu Dhabi ADS 23/2017 (marine) and DoE Trade Effluent Control Regulations 2022 (sewer) | not set region-dependent | calcium and hardness are not listed in either table; pH ranges apply |
| sector | body | limit | note |
|---|---|---|---|
| textile | ZDHC Wastewater Guidelines v₂.1 (2022) | not set | calcium and hardness are not ZDHC parameters |
8 · Health and environmental effects
- Toxicity
- Non toxic and essential (about 1 kg in an adult, the element entry); drinking water can be a useful contributor to calcium and magnesium intake, and WHO advises adding calcium and magnesium back to demineralised supplies to the levels the population had before (hardness background document).
- Bioaccumulation
- Not applicable.
- Ecotoxicity
- Calcium is a nutrient; its practical ecotoxicological role is that hardness reduces the toxicity of metals, which is why the US EPA freshwater criteria for chromium(III), nickel and other metals are expressed as functions of hardness.
Flags
- The calcite solubility product, gypsum and lime solubilities, the lime softening equations and the practical softening limits are cited to textbook chapters (Stumm and Morgan 7, Snoeyink and Jenkins 6, MWH 20) from memory, not re-read.
- The fluoride residual after lime treatment is from Metcalf and Eddy chapter 6 by memory and is not quoted as a number in a source read.
- The seawater figure is a single PubChem abundance figure.
- The hardness classes are one classification quoted by WHO; other bodies use different bands.
- No calcium discharge limit exists in any document read; pH limits do the work.
Gaps
- No source read gives calcium in surface water, municipal or industrial wastewater as numbers.
- No Langelier index worked example or calcium carbonate precipitation potential figure was read; Standard Methods 2330 is cited by title.
- Lime doses, softening sludge quantities and recarbonation doses were not read; MWH chapter 20 has them.
- Detection limits for the EDTA titrations were not read.
- Remineralisation targets for desalinated water (calcium, alkalinity, index) were not read; WHO states the principle only.
- Other GCC standards were not read.
- The Langelier index itself is an index, not a reaction: it is written here as the calcite solubility and the carbonate dissociation that fix pHs; no worked example or activity correction was read.
- The hydroxyapatite, gypsum neutralisation and EDTA titration stoichiometries are cited to Metcalf and Eddy chapter 6 and Standard Methods 2340 by chapter and method number, not re-read.
Sources
WHO, Hardness in Drinking-water, background document, WHO/HSE/WSH/10.01/10/Rev/1 (2011), sections 1.1 to 1.3, 2.1, 4.2 and 4.3
Directive (EU) 2020/2184 on the quality of water intended for human consumption (recast), recital and Annex I Part C note on calcium and magnesium in softened water, Annex IV
US EPA, National Primary Drinking Water Regulations (table of MCLs and treatment techniques)
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 and 2
Abu Dhabi Specification ADS 23/2017, Environmental Specifications for Land-Based Liquid Discharges to the Marine Environment (Environment Agency Abu Dhabi), Table 1
ZDHC Wastewater Guidelines Version 2.1 (November 2022), conventional parameters, anions and metals tables and sludge Table 4A
US EPA, National Recommended Water Quality Criteria, Aquatic Life Criteria Table (hardness dependent metal criteria)
Standard Methods (online edition), 2330 Calcium Carbonate Saturation (Langelier saturation index, calcium carbonate precipitation potential)
Standard Methods (online edition), 2340 Hardness (C. EDTA titrimetric method)
Standard Methods (online edition), 3500-Ca Calcium (B. EDTA titrimetric method)
ISO 6059:1984, Water quality. Determination of the sum of calcium and magnesium. EDTA titrimetric method
US EPA Method 200.7, Revision 4.4 (1994), Determination of metals and trace elements in water and wastes by ICP-AES, Table 1 (wavelengths and instrument detection limits), Table 4 (method detection limits) and Table 5 (argon plasma conditions)
ISO 11885:2007, Water quality. Determination of selected elements by inductively coupled plasma optical emission spectrometry (ICP-OES)
PubChem element summary for calcium; estimated oceanic abundance 4.12 x 10^2 mg/L (PUG View, reference 5, Jefferson Lab)
The Element Book, layer 1 entry for calcium (data/elements/Ca.json and data/reference/text/Ca.json)
The Element Book, water chapter for chlorine (data/water/Cl.json), calcium hypochlorite hydrolysis
Stumm, W. and Morgan, J. J., Aquatic Chemistry, 3rd ed. (Wiley, 1996), chapter 7 (precipitation and dissolution: calcite, gypsum)
Snoeyink, V. L. and Jenkins, D., Water Chemistry (Wiley, 1980), chapter 6 (precipitation and dissolution: the carbonate system, saturation index, lime softening)
Crittenden, J. C. et al., MWH's Water Treatment: Principles and Design, 3rd ed. (Wiley, 2012), chapter 20 (removal of selected constituents: lime softening) and chapter 17 (reverse osmosis: scaling)
Metcalf and Eddy, Wastewater Engineering: Treatment and Resource Recovery, 5th ed. (McGraw-Hill, 2014), chapter 6 (lime precipitation of phosphate and fluoride) and chapter 14 (lime stabilisation of sludge)
Identity
- Name and symbol
- Calcium, Ca
- Atomic number
- 20 protons
- Position
- group 2 · period 4 · s-block · alkaline earth metal
- CAS number
- 7440-70-2
Atomic structure
- Atomic mass
- 40.078 u
- Electron configuration
- 1s² 2s² 2p⁶ 3s² 3p⁶ 4s²
[Ar] 4s² - Electrons per shell
- 2, 8, 8, 2
- Valence electrons
- 2 outer shell
| isotope | mass (u) | abundance |
|---|---|---|
| 40Ca | 39.962 5909(2) | 96.9 % |
| 42Ca | 41.958 618(1) | 0.6 % |
| 43Ca | 42.958 766(2) | 0.1 % |
| 44Ca | 43.955 482(2) | 2 % |
| 46Ca | 45.953 69(2) | 0 % |
| 48Ca | 47.952 5229(6) | 0.1 % |
Physical properties
- State at room temperature
- Solid
- Melting point
- 1,115 K (841.85 °C)
- Boiling point
- 1,757 K (1,483.85 °C)
- Density
- 1.54 g/cm3
- Appearance
- dull gray, silver; with a pale yellow tint
- Thermal conductivity
- 201 W/(m·K)
- Electrical resistivity
- 33.6 nΩ·m at 20 °C
- Electrical conductivity
- 29.76 MS/m
- Crystal structure
- face-centered cubic
- Molar heat capacity
- 25.929 J/(mol·K)
Chemical properties
- Oxidation states
- +2
- Electronegativity
- 1 (Pauling Scale)
- Ionisation energy
- 6.113 eV
1st 589.8, 2nd 1,145.4, 3rd 4,912.4 kJ/mol - Electron affinity
- 0 eV
- Atomic radius
- empirical 176, covalent 176, van der Waals 231 pm
- Ionic radius
- Ca²⁺ 100 pm
- Reactivity
- A typical heavy alkaline earth metal ([Ar] 4s2), reactive enough that it is never found free; it tarnishes rapidly in air, reacts with water faster than magnesium and more slowly than strontium, and is a strong reducing agent used to win other metals.
- with water
- Reacts steadily with cold water to calcium hydroxide and hydrogen, faster than magnesium:
- with oxygen, air
- Forms a dark oxide-nitride coating in air; heated it is reluctant to start but then burns with an intense yellow-red flame to calcium oxide and nitride, and the fine powder burns spontaneously:
- with acids
- Reacts readily with dilute hydrochloric acid to the chloride and hydrogen; with sulfuric acid a coating of sparingly soluble calcium sulfate slows the reaction, and very dilute nitric acid gives hydrogen contaminated with nitrogen oxides:
- with halogens
- Reacts with the halogens to the ionic dihalides such as calcium chloride:
- Typical compounds
- CaCO₃ calcium carbonate limestone, chalk, marble; building stone and cement
- CaO calcium oxide quicklime, from roasting limestone
- Ca(OH)₂ calcium hydroxide slaked lime; mortar and plaster
- CaSO₄.2H₂O calcium sulfate dihydrate gypsum; plaster
- CaC₂ calcium carbide from lime and carbon; gives acetylene with water
- CaF₂ calcium fluoride fluorite; lowers the melting point in calcium electrolysis
Occurrence, production and use
- Crustal abundance
- 4.15×104 milligrams per kilogram
- Oceanic abundance
- 4.12×102 milligrams per liter
- Occurrence and sources
Calcium, a metallic element, is fifth in abundance in the earth's crust, of which it forms more than 3%. It is an essential constituent of leaves, bones, teeth, and shells. Never found in nature uncombined, it occurs abundantly as limestone, gypsum, and fluorite. Apatite is the fluorophosphate or chlorophosphate of calcium.
- limestone and chalk (CaCO3), gypsum (CaSO4), fluorite (CaF2), apatite (calcium fluoro and chlorophosphate) sedimentary rock worldwide; limestone and dolomite suitable for lime manufacture are very large resources in every producing country
- dissolved calcium bicarbonate hard groundwater and surface water; it precipitates as stalactites and scale when carbon dioxide is lost
- calcium phosphate the main component of bone, teeth and shells
- Extraction, production
- Lime burning (calcination of limestone)
Limestone heated in kilns gives off carbon dioxide and leaves quicklime; balanced from the reactants and products stated by the source. World lime production about 420 million tonnes in 2024 (estimate), 73 quicklime plants and 10 hydrating plants in the United States (USGS). Large quantities of lime are regenerated by paper mills and some water treatment plants regenerate lime from softening sludge.
Slaking (hydration of quicklime)Quicklime reacts vigorously with a controlled amount of water in a hydrator to give hydrated (slaked) lime, a dry calcium hydroxide powder used in chemical, construction and environmental applications; balanced from the reactants and product stated by the sources.
Calcium metal by aluminothermic reduction of limeThe metal is prepared commercially by heating lime with aluminium under vacuum, or by electrolysis of fused calcium chloride with calcium fluoride added to lower the melting point. The sources name the reducing agent but not the aluminium bearing product, so no equation is written; demand for the metal is small (reducing agent for thorium, uranium and zirconium, deoxidiser and desulphuriser for alloys).
- Uses
Due to its high reactivity with common materials, there is very little demand for metallic calcium. It is used in some chemical processes to refine thorium, uranium and zirconium. Calcium is also used to remove oxygen, sulfur and carbon from certain alloys. Calcium can be alloyed with aluminum, beryllium, copper, lead and magnesium. Calcium is also used in vacuum tubes as a getter, a material that combines with and removes trace gases from vacuum tubes.
Calcium carbonate (CaCO3) is one of the common compounds of calcium. It is heated to form quicklime (CaO) which is then added to water (H2O). This forms another material known as slaked lime (Ca(OH)2) which is an inexpensive base material used throughout the chemical industry. Chalk, marble and limestone are all forms of calcium carbonate. Calcium carbonate is used to make white paint, cleaning powder, toothpaste and stomach antacids, among other things. Other common compounds of calcium include: calcium sulfate (CaSO4), also known as gypsum, which is used to make dry wall and plaster of Paris, calcium nitrate (Ca(NO3)2), a naturally occurring fertilizer and calcium phosphate (Ca3(PO4)2), the main material found in bones and teeth.
The metal is used as a reducing agent in preparing other metals such as thorium, uranium, zirconium, etc., and is used as a deoxidizer, desulfurizer, or decarburizer for various ferrous and nonferrous alloys. It is also used as an alloying agent for aluminum, beryllium, copper, lead, and magnesium alloys, and serves as a "getter" for residual gases in vacuum tubes, etc.
- Steel: lime as the flux that removes impurities from molten iron and steel; steelmaking is the largest lime market in the United States steelmaking was the leading United States lime market in 2024 (USGS, ranking only)
- Food and beverage: lime and carbon dioxide for beet juice purification (carbonatation), leaving carbonatation lime cake as a residue; sugar companies burn lime for their own use; calcium salts as additives (calcium carbonate E170, propionate, lactate, phosphates)
- Chemicals: calcium ammonium nitrate fertiliser, made by mixing ammonium nitrate solution with dolomite, limestone or calcium carbonate; phosphate rock (apatite) as the calcium phosphate feed of wet process phosphoric acid and superphosphates, with phosphogypsum and calcium fluoride sludge as co product and waste stream
- Glass, pulp and paper: lime for glass, pulp and paper manufacture and for precipitated calcium carbonate; paper mills regenerate large quantities of lime
- Mining: lime, quicklime, hydrated lime and limestone for neutralisation and metal precipitation in mine water treatment, including the high density sludge lime process for base metal mine water
- Water treatment: slaked lime to reduce acidity, lime softening of hard water, flue gas desulphurisation
- Construction: cement, lime mortar and lime plaster; gypsum plaster and plasterboard
- Safety, toxicity
- not in sources
Discovery and name
- Discovered by
- Humphry Davy
- Discovered
- 1808
- First isolated
- not in sources
- Named by
- not in sources
- Origin of the name
- from the Latin word for lime, calx
The metal has a silvery color, is rather hard, and is prepared by electrolysis of fused chloride and calcium fluoride (to lower the melting point).
Chemically it is one of the alkaline earth elements; it readily forms a white coating of nitride in air, reacts with water, burns with a yellow-red flame.
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.