Calcium

    group 2 · period 4 · s-block · alkaline earth metal

    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
    In the ledger's plant and process records, discharged by: Sugar beet extraction (Food and beverage)

    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.
    matrixtypical rangenote
    groundwater and natural sourcesup 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 CaCO3the classification quoted by WHO
    seawater412 mg/Lsingle figureestimated 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.

    conditiondominant speciesnote
    natural water, pH 6.5 to 8.5Ca²⁺ with CaHCO₃⁺, CaCO₃ (aq) and CaSO₄ (aq) ion pairs; calcite at or near saturationcarbonate (temporary) hardness is the calcium matched by bicarbonate, non carbonate (permanent) hardness the rest
    heated or carbon dioxide stripped waterCaCO₃ (s) scalethe boiler, kettle and heat exchanger deposit
    lime softening, pH 10 to 11CaCO₃ (s) and Mg(OH)₂ (s) sludge; residual Ca²⁺ at the practical solubility limitrecarbonation with CO₂ brings the water back to stability
    demineralised or desalinated wateralmost no calcium; aggressive to cement and metalsstabilised before distribution with lime, limestone or calcium chloride plus carbon dioxide
    sulfate rich water, brines, reverse osmosis concentrategypsum CaSO₄.2H₂O (s) at saturationa 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.
    CaCOX3(s)+COX2+HX2OCaX2++2HCOX3X\ce{CaCO3 (s) + CO2 + H2O <=> Ca^2+ + 2 HCO3^-}
    the carbonate equilibrium of natural water; runs right as limestone dissolves and left as scale forms when CO2 is lost or the water is heated
    CaCOX3(s)CaX2++COX3X2\ce{CaCO3 (s) <=> Ca^2+ + CO3^2-}
    calcite solubility, log Ks0 about minus 8.48 at 25 C and falling as the water warms; with the carbonate dissociation below it fixes pHs, the pH at which the water would be saturated, and the Langelier saturation index is pH minus pHs: positive water scales, negative water dissolves calcite and cement (Standard Methods 2330 pairs the index with the calcium carbonate precipitation potential, the mass that would actually come out)
    HCOX3XCOX3X2+HX+\ce{HCO3^- <=> CO3^2- + H+}
    the second dissociation of carbonic acid, pK2 about 10.33 at 25 C; it is what converts a measured pH and alkalinity into the carbonate activity in the saturation index, and it is why raising pH with lime precipitates calcite without adding any carbonate; Snoeyink and Jenkins chapter 4, from the chapter, not re-read
    CaX2++2HCOX3XCaCOX3(s)+COX2+HX2O\ce{Ca^2+ + 2 HCO3^- -> CaCO3 (s) + CO2 + H2O}
    scale formation on heating; the element entry says hard water deposits scale when bicarbonate loses carbon dioxide
    CaO+HX2OCa(OH)X2\ce{CaO + H2O -> Ca(OH)2}
    lime slaking, strongly exothermic; slaked lime is the base of softening, neutralisation and sludge stabilisation (the element entry)
    COX2+Ca(OH)X2CaCOX3(s)+HX2O\ce{CO2 + Ca(OH)2 -> CaCO3 (s) + H2O}
    first lime demand in softening: free carbon dioxide is neutralised before any hardness precipitates (MWH chapter 20, from the chapter, not re-read)
    Ca(HCOX3)X2+Ca(OH)X22CaCOX3(s)+2HX2O\ce{Ca(HCO3)2 + Ca(OH)2 -> 2 CaCO3 (s) + 2 H2O}
    calcium carbonate hardness removal at pH about 10.3; one mole of lime per mole of calcium bicarbonate
    Mg(HCOX3)X2+2Ca(OH)X22CaCOX3(s)+Mg(OH)X2(s)+2HX2O\ce{Mg(HCO3)2 + 2 Ca(OH)2 -> 2 CaCO3 (s) + Mg(OH)2 (s) + 2 H2O}
    magnesium carbonate hardness needs excess lime and pH about 11
    CaSOX4+NaX2COX3CaCOX3(s)+NaX2SOX4\ce{CaSO4 + Na2CO3 -> CaCO3 (s) + Na2SO4}
    non carbonate hardness needs soda ash; lime alone cannot remove it
    CaSOX42HX2O(s)CaX2++SOX4X2+2HX2O\ce{CaSO4.2H2O (s) <=> Ca^2+ + SO4^2- + 2 H2O}
    gypsum saturation, about 2 g/L at 25 C; the sulfate ceiling of lime treatment
    5CaX2++3POX4X3+OHXCaX5(POX4)X3OH(s)\ce{5 Ca^2+ + 3 PO4^3- + OH- -> Ca5(PO4)3OH (s)}
    phosphorus removal with lime above pH 10; hydroxyapatite is the stable solid, so the calcium demand is set by the pH reached rather than by the phosphorus alone; Metcalf and Eddy chapter 6, from the chapter, not re-read
    Ca(OH)X2+HX2SOX4CaSOX42HX2O(s)\ce{Ca(OH)2 + H2SO4 -> CaSO4.2H2O (s)}
    lime neutralisation of acid mine drainage and of spent sulfuric acid; the sulfate leaves as gypsum, which saturates near 2 g/L, so lime alone cannot take sulfate below about 1.5 to 2 g/L; Metcalf and Eddy chapter 6, from the chapter, not re-read
    CaX2++CX10HX14NX2OX8X2CaCX10HX12NX2OX8X2+2HX+\ce{Ca^2+ + C10H14N2O8^2- -> CaC10H12N2O8^2- + 2 H+}
    the EDTA titration of hardness at pH 10 in an ammonia buffer, written with the disodium EDTA anion; the indicator gives up its magnesium (Eriochrome Black T in Standard Methods 2340 C) or its calcium (murexide in 3500-Ca B) to the stronger chelate at the end point, and the protons released are why the buffer is needed; cited by method number, not re-read

    4 · Role in treatment

    as a problem
    carbonate scale
    calcite deposits where water is heated, degassed or concentrated: heat exchangers, boilers, hot water systems, membranes, cooling towers
    WHO: hard water causes scale in distribution and heated applications, reducing heat exchanger efficiency; the Langelier index and calcium carbonate precipitation potential (Standard Methods 2330) quantify the tendency
    soap consumption and acceptability
    calcium and magnesium precipitate soap
    WHO: hardness is the traditional measure of the capacity to react with soap; taste threshold for calcium 100 to 300 mg/L; hardness above about 200 mg/L as CaCO₃ is a scaling nuisance, below 100 mg/L the water tends to be corrosive (the WHO fact sheet reads that hardness may affect acceptability)
    corrosion of soft and demineralised water
    water with little calcium and alkalinity dissolves cement linings and metals (lead, copper, cadmium, zinc) instead of laying down a carbonate film
    WHO: desalinated water is highly aggressive and must be stabilised by lime and carbon dioxide before distribution; the EU DWD allows Member States to set minimum calcium and magnesium in softened or demineralised water
    post-precipitation after lime softening
    water leaving the softener is supersaturated with CaCO₃ and deposits it in filters and mains unless recarbonated
    WHO hardness document: softened waters are balanced to minimise post-precipitation of lime and stabilised to control corrosivity
    gypsum scaling and sulfate ceiling
    calcium sulfate saturates in reverse osmosis concentrate, cooling water and lime treated mine water
    about 2 g/L gypsum, so lime treatment leaves 1.5 to 2 g/L sulfate
    Ca(OH)X2+HX2SOX4CaSOX42HX2O(s)\ce{Ca(OH)2 + H2SO4 -> CaSO4.2H2O (s)}
    lime treated acid mine drainage and any concentrated sulfate stream; gypsum saturation near 2 g/L is the floor, and in a membrane concentrate the same solid is the recovery limit
    lime sludge
    every mg/L of hardness removed leaves calcium carbonate and magnesium hydroxide sludge, plus the lime added
    the element entry: some plants regenerate lime from softening sludge
    as a reagent
    lime (quicklime, hydrated lime) for softening, pH control, coagulation and neutralisation
    strong base that raises pH, precipitates carbonate hardness, magnesium, phosphate, fluoride and metals, neutralises acid mine drainage and industrial acid, and conditions sludge
    Ca(HCOX3)X2+Ca(OH)X22CaCOX3(s)+2HX2O\ce{Ca(HCO3)2 + Ca(OH)2 -> 2 CaCO3 (s) + 2 H2O}
    water treatment is one of the listed uses of the 420 million tonnes of lime made a year (the element entry); softening to pH 10.3 for calcium, 11 for magnesium; the practical residual is about 30 to 40 mg/L as CaCO3 (MWH chapter 20, from the chapter)
    lime for phosphorus and fluoride precipitation
    hydroxyapatite above pH 10 and fluorite
    CaX2++2FXCaFX2(s)\ce{Ca^2+ + 2 F^- -> CaF2 (s)}
    the element narrative: lime drops phosphate, fluoride and metals out of effluent; fluorite leaves about 8 mg/L fluoride at its own solubility (figure not read this session, from Metcalf and Eddy chapter 6 by memory)
    calcium hypochlorite as solid chlorine
    dissolves to hypochlorous acid and hydroxide; raises pH and adds calcium hardness
    Ca(OCl)X2+2HX2O2HOCl+CaX2++2OHX\ce{Ca(OCl)2 + 2 H2O -> 2 HOCl + Ca^2+ + 2 OH^-}
    typically 65 percent available chlorine; the equation as in the book's chlorine entry
    limestone contactors, lime and calcium chloride for remineralisation
    desalinated and soft water is given calcium and alkalinity so that it is neither corrosive nor tasteless
    CaCOX3(s)+COX2+HX2OCaX2++2HCOX3X\ce{CaCO3 (s) + CO2 + H2O -> Ca^2+ + 2 HCO3^-}
    WHO: addition of lime is a common and low cost stabilisation; target bicarbonate equilibrium and suitable pH and alkalinity; calcium and magnesium salts may be added to conditioned water to reduce corrosiveness and improve taste (EU DWD Annex I Part C note)
    lime stabilisation of sludge
    lime to pH 12 kills pathogens and stops odour
    Metcalf and Eddy chapter 14 (from the chapter, not re-read); no dose quoted

    5 · Removal and control

    lime and lime soda softening
    precipitation of CaCO₃ and Mg(OH)₂ at pH 10 to 11 in a reactor clarifier or solids contact unit, followed by recarbonation and filtration; excess lime for magnesium; soda ash for non carbonate hardness
    Ca(HCOX3)X2+Ca(OH)X22CaCOX3(s)+2HX2O\ce{Ca(HCO3)2 + Ca(OH)2 -> 2 CaCO3 (s) + 2 H2O}
    the WHO hardness document: central softening usually involves lime or lime soda; the treated water is balanced and stabilised
    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
    ion exchange softening
    sodium (or potassium) form strong acid cation resin takes calcium and magnesium and gives back sodium; regenerated with brine
    point of entry devices and central plants; softened water is not necessarily corrosive since it keeps its alkalinity (WHO hardness document)
    Efficiency
    to near zero hardness until breakthrough
    Interferences
    iron and manganese foul the resin; brine disposal; sodium or potassium added
    nanofiltration and reverse osmosis
    divalent calcium is rejected by nanofiltration and reverse osmosis; membrane softening
    antiscalant or acid to hold calcium carbonate and gypsum below saturation in the concentrate
    Efficiency
    not quoted
    Interferences
    scaling limits recovery
    pellet softening
    caustic or lime dosed into a fluidised sand bed on which calcium carbonate crystallises as dry pellets instead of sludge
    CaX2++2HCOX3XCaCOX3(s)+COX2+HX2O\ce{Ca^2+ + 2 HCO3^- -> CaCO3 (s) + CO2 + H2O}
    MWH chapter 20 (from the chapter, not re-read)
    Efficiency
    not quoted
    Interferences
    magnesium is not removed

    6 · Analytics

    methodstandarddetection limitnote
    EDTA titrationStandard Methods 3500-Ca B (calcium) and 2340 C (total hardness); ISO 6059 (calcium plus magnesium)not readtotal hardness is the sum of calcium and magnesium expressed as CaCO₃; EDTA combines first with calcium (method abstracts)
    ICP-OESEPA 200.7 (315.887 nm); ISO 11885EPA 200.7 instrument detection limit 30 µg/L, total recoverable method detection limit 0.01 mg/Lcalcium is not an analyte of EPA 200.8; hardness by calculation from calcium and magnesium (Standard Methods 2340 B)
    calcium carbonate saturation indicesStandard Methods 2330not applicableLangelier 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.

    drinking water
    bodylimitnote
    WHO GDWQ 4th ed. with addenda (2022), hardnessno 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 2020/2184not 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 EPAnot regulated absent from the primary and secondary standards
    discharge
    bodylimitnote
    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-dependentcalcium and hardness are not listed in either table; pH ranges apply
    industry thresholds
    sectorbodylimitnote
    textileZDHC 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 GDWQ 4th ed. with addenda (2022), chapter 12 fact sheet, Hardness (pp. 408 to 409)
    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)

    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.