Barium

    group 2 · period 6 · s-block · alkaline earth metal

    fullBarium carries a WHO guideline of 1.3 mg/L and a US MCL of 2 mg/L, occurs at milligram levels in deep groundwater and at gram levels in oil and gas produced water, and its sulfate is at once the tightest scale in the oilfield, the carrier that co-precipitates radium, and the reason barium is easy to remove.

    Typical wastewaters

    • oil and gas produced water and flowback Ba²⁺ at 815 mg/L average in shale gas water and 25 mg/L in coal bed methane water, kept dissolved by the absence of sulfate; BaSO₄ with radium precipitates on mixing with sulfate water downstream of a discharge dissolved barium fell from 13.4 to 0.93 mg/L over 20 to 300 m
    • drilling wastes (barite mud) and metal refineries barite BaSO₄ solids in drilling waste; Ba²⁺ in refinery effluent, capped by BaSO₄ where sulfate is present US EPA source list for the barium MCL
    • radium removal residuals (barium chloride dosing, barium sulfate impregnated media) Ba(Ra)SO₄ filter solids and spent media carrying radium every barium removal step concentrates the radium
    • water softening residuals (cation exchange brine, lime softening sludge) Ba²⁺ in the spent regenerant brine; BaCO₃ in lime sludge; both carry any radium
    • textile wet processing total barium, a sample and report only ZDHC parameter; sludge threshold 200 mg/kg
    In the ledger's plant and process records, discharged by: Speciality inorganic pigments (iron oxide, chromium oxide, CIC, zinc sulphide, lithopone) (Chemicals) · Base metal ores (Cu, Ni, Pb, Sn, Zn) (Mining) · Coal, lignite and peat (Mining) · Industrial minerals (potash, salt, kaolin, magnesite and others) (Mining) · Precious metal ores (Au, Ag, Pt): gold and silver extraction (Mining) · Uranium ore (Mining)

    1 · Identity

    Symbol, number
    Ba, 56
    Oxidation states in water
    +2 only, as the large, weakly hydrated Ba²⁺ ion; it forms few complexes and behaves as a heavier calcium that is stopped by sulfate rather than by carbonate.
    Note
    The element entry gives the metal's reactions and the barite and witherite minerals. This chapter is about Ba²⁺ in solution and BaSO₄ in pipes, filters and sludges.

    2 · Occurrence in water

    Natural sources
    Leaching and erosion of barite and witherite deposits and of igneous and sedimentary rocks; barium enters water primarily from natural sources, and deep rock and drift wells can hold milligram levels (WHO). Solubility rises as pH falls and falls where sulfate or carbonate are high, because BaSO₄ and BaCO₃ precipitate (WHO background document). Deep formation waters are sulfate free and therefore carry barium in quantity.
    Anthropogenic sources
    Drilling wastes (barite mud) and metal refineries, the sources the US EPA lists; industrial emissions and uses; produced water from unconventional gas, where barium averages 815 mg/L in shale gas and 25 mg/L in coal bed methane waters (Willems 2025); barium chloride dosed deliberately to precipitate radium as Ba(Ra)SO₄ (Clifford).
    matrixtypical rangenote
    drinking watergenerally below 100 µg/Lregion-dependentconcentrations above 1 mg/L have been measured in drinking water derived from groundwater (WHO fact sheet); US public supply wells median 46.7 µg/L, 90th percentile 164.1 µg/L, maximum 11 mg/L in 630 samples (USGS 2010 via WHO); Canada median 18 µg/L, range 5 to 600; Sweden 1 to 20; Norway median 9 µg/L
    groundwater0.23 mean, 2.5 maximum mg/Lregion-dependent60 Dutch locations; 16 cities in northern Illinois have sources at 1.1 to 10.0 mg/L from deep rock and drift wells; Tuscany groundwater supplies 700 to 1160 µg/L
    raw water treated for barium, USA0.4 to 8.5 mg/Ltreatment study, not a surveyaverage 5.32 mg/L in the Krause and Stover study quoted by WHO
    produced and flowback water, unconventional gas815 average (shale gas); 25 average (coal bed methane) mg/L
    averages from a toxicity paper, not a survey
    dissolved barium downstream of a discharge fell from 13.4 to 0.93 mg/L over 20 to 300 m as sulfate precipitated it
    seawaternot read no figure read this sessionseawater is sulfate rich (about 28 mmol/L) and therefore barium poor; mixing it with formation water is the classic barite scaling event

    3 · Speciation

    Barium is Ba²⁺ across the whole pH range of natural water, with minor BaSO₄ and BaCO₃ ion pairs; it hydrolyses only above pH 13. The solid that controls it is barite: with 0.003 g/L solubility (WHO background document) any water carrying both barium and sulfate at more than a few milligrams per litre is supersaturated, so barium is either low and sulfate rich, or high and sulfate free, never both. Carbonate takes over as the control only in sulfate free alkaline water (witherite, 0.0014 g/L).

    conditiondominant speciesnote
    oxic or anoxic fresh water with sulfate, pH 6 to 9Ba²⁺ capped by BaSO₄ (s)the usual case; barium stays at tens of micrograms per litre
    sulfate free deep groundwater and formation brinesBa²⁺ at milligram to gram levels; BaCl⁺ ion pairing in brinessulfate has been reduced to sulfide, so barite cannot form; radium rides with barium
    high pH softening (pH above 10)BaCO₃ (s) with the calcium carbonate sludgethe lime softening route to removal (WHO: lime softening removes barium to below 1 mg/L)
    mixing of barium brine with sulfate water (seawater injection, produced water into a sulfate bearing stream)BaSO₄ (s) precipitates at once, carrying Ra²⁺ and Sr²⁺the scaling and NORM event of the oilfield; downstream of a discharge dissolved barium fell from 13.4 to 0.93 mg/L (Willems 2025)
    Solubility
    BaSO₄ 0.003 g/L at 20 C and BaCO₃ 0.0014 g/L at 20 C, against 370 g/L for BaCl₂ and 49 g/L for Ba(OH)₂ (WHO background document Table 2). The solubility product of barite is about 10⁻10 in the Stumm and Morgan table (from the chapter, not re-read), so 1 mg/L barium is at saturation with about 1 mg/L sulfate at low ionic strength, and brine ionic strength raises it several fold.
    Hydrolysis
    Negligible: Ba²⁺ is the least hydrolysed of the common divalent cations and BaOH⁺ matters only above pH 13 (Stumm and Morgan chapter 6, from the chapter). Barium hydroxide is a strong base and fully dissociated.
    Complexation
    Weak ion pairs with sulfate, carbonate and chloride; no significant organic complexation. Barium is carried instead by adsorption onto suspended solids and sediment (WHO background document).
    Precipitates
    BaSO₄ barite (the scale, the drilling mud and the radium carrier), BaCO₃ witherite (softening sludge), Ba(Ra)SO₄ solid solution. Barium chromate and barium phosphate are analytical, not treatment, solids.
    BaX2++SOX4X2BaSOX4(s)\ce{Ba^2+ + SO4^2- -> BaSO4 (s)}
    any pH; solubility 0.003 g/L at 20 C; the reaction that scales injection wells and pipelines when barium formation water meets sulfate rich seawater, and the reaction used deliberately to strip barium and radium
    BaX2++COX3X2BaCOX3(s)\ce{Ba^2+ + CO3^2- -> BaCO3 (s)}
    lime softening pH above 10; witherite solubility 0.0014 g/L; barium leaves with the calcium carbonate sludge
    BaX2++RaX2++2SOX4X2BaSOX4RaSOX4(s)\ce{Ba^2+ + Ra^2+ + 2 SO4^2- -> BaSO4.RaSO4 (s)}
    excess barium chloride added to sulfate bearing water before filtration; trace radium enters the barite lattice because RaSO4 is far less soluble than barite (Rowan 2011); Clifford writes it as excess Ba^2+ plus trace Ra plus sulfate giving Ba(Ra)SO4
    2RNa+BaX2+RX2Ba+2NaX+\ce{2 RNa + Ba^2+ -> R2Ba + 2 Na^+}
    strong acid cation exchange in sodium form, the same softening reaction as for calcium and radium (Clifford writes it for radium); regenerated with brine
    BaX2++ClXBaClX+\ce{Ba^2+ + Cl^- <=> BaCl^+}
    chloride ion pairing in formation brines; it is part of why a brine holds far more barium than the low ionic strength solubility product suggests, and why a barite saturation index calculated without activity corrections underpredicts scale
    Ba(OH)X2(s)BaX2++2OHX\ce{Ba(OH)2 (s) -> Ba^2+ + 2 OH-}
    barium hydroxide is a strong base and dissolves at 49 g/L at 20 C, against 0.003 g/L for barite; the contrast is the whole of barium water chemistry, one anion caps it and the others do not

    4 · Role in treatment

    as a problem
    barite scale in oil and gas systems
    barium rich formation water meets sulfate rich seawater or another sulfate water; BaSO₄ precipitates instantly and is nearly insoluble in acid, so unlike carbonate scale it cannot be dissolved away
    the oilfield answers are low sulfate injection water, scale inhibitors and mechanical removal; none of the sources read prints scale rates, so this row is the chemistry, not a figure
    BaCOX3(s)+2HX+BaX2++COX2(g)+HX2O\ce{BaCO3 (s) + 2 H+ -> Ba^2+ + CO2 (g) + H2O}
    the contrast that defines the problem: witherite and calcite scale dissolve in acid by this reaction, barite does not, so an acid wash that clears a carbonate scale leaves a barite scale untouched and it has to be milled or jetted out
    NORM in barite scale and sludge
    radium co-precipitates in BaSO₄, so barite scale, filter cake and treatment sludges from produced water are radioactive
    Marcellus produced water radium runs to 18,000 pCi/L (Rowan 2011); every barium removal step concentrates it
    health limit exceedance in deep groundwater supplies
    sulfate free aquifers carry barium above 1 mg/L
    16 cities in northern Illinois at 1.1 to 10 mg/L (WHO background document); nephropathy is the WHO end point
    interference with sulfate analysis and with softening capacity
    barium competes with calcium and magnesium for cation resin sites; in ICP-MS it needs sulfate free acid to stay in solution
    EPA 200.8 warns that nitric acid solubilises only minimal barium in the presence of free sulfate
    RX2Ca+BaX2+RX2Ba+CaX2+\ce{R2Ca + Ba^2+ -> R2Ba + Ca^2+}
    R is a strong acid cation exchange site; barium sits above calcium in the selectivity sequence, so it is taken preferentially and elutes late, and a softener run set by hardness breakthrough still holds its barium, which then leaves in the brine
    as a reagent
    barium chloride for radium removal
    excess Ba²⁺ precipitates BaSO₄ that carries radium; removed by filtration
    BaX2++SOX4X2BaSOX4(s)\ce{Ba^2+ + SO4^2- -> BaSO4 (s)}
    added to the feed before filtration; 50 to 95 percent radium removal (Clifford); needs sulfate in the water
    barium sulfate impregnated media for radium
    radium exchanges into BaSO₄ held on cation resin or activated alumina
    BaSOX4(s)+RaX2+RaSOX4(s)+BaX2+\ce{BaSO4 (s) + Ra^2+ -> RaSO4 (s) + Ba^2+}
    single column with 10 pCi/L radium in the feed leaves 510 pCi/g on spent resin and 220 pCi/g on spent alumina (Clifford); the exchange runs because radium sulfate is less soluble than barite, so the radium enters the solid and an equivalent of barium leaves it, which is why a spent medium is a NORM waste and why a little barium appears in the product water
    gravimetric sulfate analysis
    sulfate is weighed as BaSO₄
    BaX2++SOX4X2BaSOX4(s)\ce{Ba^2+ + SO4^2- -> BaSO4 (s)}
    the classical sulfate method; barium is the reagent

    5 · Removal and control

    cation exchange softening
    Ba²⁺ exchanges for sodium on strong acid resin with the hardness; brine regeneration
    2RNa+BaX2+RX2Ba+2NaX+\ce{2 RNa + Ba^2+ -> R2Ba + 2 Na^+}
    run to hardness breakthrough; barium is held more strongly than calcium
    Efficiency
    to below 1 mg/L from 0.4 to 8.5 mg/L raw water (Krause and Stover via WHO); to below 2 mg/L (USEPA 2014 via WHO)
    Interferences
    hardness consumes capacity; spent brine carries barium and any radium
    lime softening
    barium precipitates as BaCO₃ with calcium carbonate at high pH
    BaX2++COX3X2BaCOX3(s)\ce{Ba^2+ + CO3^2- -> BaCO3 (s)}
    pH above 10 with lime and soda ash
    Efficiency
    to below 1 mg/L (WHO)
    Interferences
    sludge carries barium and radium
    direct filtration with chemical precipitation (sulfate addition)
    sulfate precipitates BaSO₄, removed on the filter
    BaX2++SOX4X2BaSOX4(s)\ce{Ba^2+ + SO4^2- -> BaSO4 (s)}
    the third method Krause and Stover found effective
    Efficiency
    to below 1 mg/L (WHO)
    Interferences
    fine barite passes filters without coagulant
    reverse osmosis and electrodialysis
    divalent cation rejection
    effective to below 2 mg/L (USEPA 2014 via WHO); point of use RO and point of entry cation exchange are available for homes but costly
    Efficiency
    to below 2 mg/L
    Interferences
    barite scaling of the membrane concentrate when sulfate is present; antiscalant needed

    6 · Analytics

    methodstandarddetection limitnote
    ICP-MSEPA 200.8; ISO 17294-20.004 to 0.8 µg/L (WHO fact sheet); EPA 200.8 Table 7 MDL 0.8 µg/L scanning mode, 0.04 µg/L selected ion monitoringthe ZDHC method for barium is EPA 200.8, 6010C, 6020A
    ICP-AESEPA 200.71.0 µg/L (WHO fact sheet)
    atomic absorptionStandard Methods 3111 D (nitrous oxide flame)detection limits reported for barium range from 0.2 to 132 µg/L depending on method (ATSDR via WHO)flame AAS is the insensitive end
    Sampling pitfalls
    Acidify with nitric acid, never sulfuric; EPA 200.8 notes that nitric acid holds only minimal barium in solution when free sulfate is present, so a sulfate rich sample that is concentrated or evaporated loses barium as barite. Total versus dissolved barium differ where barite particles are suspended; filter in the field for the dissolved figure.

    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)1.3 mg/LTDI 0.21 mg/kg body weight per day from a BMDL₀₅ of 63 mg/kg for nephropathy in mice with an uncertainty factor of 300; 20 percent allocation to water, 60 kg, 2 L/day; two significant figures kept because rounding matters at mg/L; assessment 2016
    EU DWD 2020/2184not set barium is not an Annex I parameter
    US EPA NPDWR2 mg/LMCL and MCLG both 2 mg/L; sources listed as discharge of drilling wastes, discharge from metal refineries, erosion of natural deposits
    discharge
    bodylimitnote
    EU CWW BREF BAT-AEL (Decision 2016/902)not set barium is not among the BAT 12 parameters
    US EPA effluent guidelines (40 CFR)not regulated part 435 not read this sessionno barium limitation found in the parts read (423, 433, 440); the oil and gas category regulates oil and grease and TSS, not barium
    Abu Dhabi ADS 23/2017, discharge to the marine environment (EAD)2.0 mg/L
    region-dependent; marine discharge only
    Table 1 maximum allowable concentration at the point of discharge
    Abu Dhabi DoE Trade Effluent Control Regulations 2022, discharge to sewer10 mg/L
    region-dependent; sewer discharge, not receiving water
    Table A₄ maximum allowable concentration for trade effluent to the sewer network
    industry thresholds
    sectorbodylimitnote
    textileZDHC Wastewater Guidelines v₂.1 (2022)sample and report only mg/Lno limit value; sludge threshold 200 mg/kg (textile) in Table 4A

    8 · Health and environmental effects

    Toxicity
    Not carcinogenic or genotoxic; soluble salts cause hypertension, arrhythmia and skeletal muscle paralysis in acute poisoning; nephropathy in animals is the guideline end point; a human study found no effect on hypertension at 10 mg/L but was small and short (WHO). Insoluble barite is essentially non toxic, which is why it is the X-ray contrast meal (element entry).
    Bioaccumulation
    Not addressed as such in the sources read; barium follows calcium into bone and is retained there, and the dissolved fraction is what matters because BaSO₄ is not bioavailable (Willems 2025).
    Ecotoxicity
    Chronic Ceriodaphnia dubia reproduction EC₂₀ 0.95 mg/L and EC₅₀ 10.1 mg/L dissolved barium; with 410 mg/L NaCl the EC₂₀ was 10.1 mg/L; toxicity is governed by solubility, since BaSO₄ (0.0025 g/L in that paper) is not bioavailable and hardness raises tolerance (Willems 2025). No EPA aquatic life criterion or EU EQS was read for barium.

    Flags

    • Occurrence figures are national compilations in the WHO 2016 background document (Netherlands, Canada, Sweden, Norway, Italy, USA); the Illinois 1.1 to 10 mg/L supplies are the extreme, not the norm.
    • The produced water barium averages (815 and 25 mg/L) come from the introduction of a toxicity paper, not from a produced water database.
    • No seawater barium figure was read; the sulfate rich seawater argument is chemistry, not a measured number.
    • The barite solubility product and the hydrolysis statement are cited to Stumm and Morgan chapters from memory of the text, not re-read.
    • The Ba(Ra)SO₄ co-precipitation and cation exchange equations are written from Clifford's slide notation; the radium removal percentages are his ranges.
    • Abu Dhabi values cover two media (marine 2.0 mg/L, sewer 10 mg/L); other GCC states were not read.
    • No quantitative barite scaling source (rates, saturation indices, inhibitor doses) was read; the scaling row is descriptive.

    Gaps

    • No source read gives barium in seawater, surface water as a survey range, municipal wastewater or industrial wastewater other than produced water.
    • Barite scaling kinetics, saturation index practice and low sulfate seawater treatment were not sourced; they belong with the oilfield chapter of the ledger.
    • Barium in drilling mud discharges and the offshore barite rules (OSPAR, 40 CFR 435) were not read.
    • Barium removal percentages are given by WHO as achievable residuals, not as percentages.
    • Sorption of barium on iron and manganese oxides and its behaviour in RO concentrate were not sourced.
    • EPA aquatic life criteria and EU EQS were not checked for barium beyond noting none in the tables read.
    • The chloride ion pairing, the barium hydroxide dissolution and the radium for barium exchange on impregnated media are written as the mass balances behind statements the WHO background document and the EPA radionuclides manual make in words; no stability constants, solubility products or exchange constants beyond the barite value were read.

    Sources

    WHO Guidelines for Drinking-water Quality, 4th ed. incorporating the first and second addenda (2022), chapter 12 chemical fact sheet, Barium (pp. 346 to 347)
    WHO, Barium in Drinking-water, background document for development of WHO Guidelines for Drinking-water Quality, WHO/FWC/WSH/16.48 (2016), sections 1, 2.2, 7.2 and 7.3
    Directive (EU) 2020/2184 on the quality of water intended for human consumption (recast), Article 11, Annex I Part B, Annex II Part D and Annex III
    US EPA, National Primary Drinking Water Regulations (table of MCLs and MCLGs, inorganic chemicals and radionuclides)
    Clifford, D., Fundamentals of Radium and Uranium Removal from Drinking Water Supplies, US EPA radionuclides treatment workshop slides (University of Houston)
    Rowan, E. L., Engle, M. A., Kirby, C. S. and Kraemer, T. F., Radium content of oil- and gas-field produced waters in the northern Appalachian basin (USA): summary and discussion of data, USGS Scientific Investigations Report 2011-5135
    Willems, D. J., Kumar, A. and Nugegoda, D., Chronic toxicity of dissolved barium and sodium chloride to the water flea Ceriodaphnia dubia: implications for unconventional gas flowback-produced waters, Environmental Toxicology and Chemistry (2025), doi 10.1093/etojnl/vgae019
    US EPA Method 200.8, Revision 5.4 (1994), Determination of trace elements in waters and wastes by ICP-MS, Table 7 (method detection limits)
    ISO 17294-2:2023, Water quality. Application of ICP-MS. Part 2: Determination of selected elements including uranium isotopes
    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
    Abu Dhabi Department of Energy, Trade Effluent Control Regulations 2022 (DoE/PD/R01/005, effective 1 January 2022), Appendix Tables A2 and A4
    ZDHC Wastewater Guidelines Version 2.1 (November 2022), Table 2 heavy metals and Table 4 sludge parameters
    Stumm, W. and Morgan, J. J., Aquatic Chemistry, 3rd ed. (Wiley, 1996), chapter 6 (metal ions in aqueous solution, hydrolysis and complex formation) and chapter 7 (precipitation and dissolution, solubility products)
    The Element Book, element entry and reference text for Ba (data/elements/Ba.json, data/reference/text/Ba.json)

    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.