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Extraction · Water

Water for coffee

Why brewing water matters, where its minerals come from, how hardness and alkalinity shape flavour and machines, which targets are published, and how water is measured and treated.

Across the chain: Science · Equipment

Source-checkedby Coffearium verification pass· Last source-checked 10 Oct 2026· Prepared with AI assistance· 21 sources (19 tier A)· 6 contested· Updated 20 Oct 2026
Reading depth
Contents

In brief

  • Water is the main ingredient of brewed coffee. Its minerals affect flavour and how long machines last.1
  • Two numbers describe most waters for coffee – total hardness (calcium plus magnesium) and alkalinity (the capacity to neutralise acid, mostly bicarbonate).1,3,4
  • High alkalinity neutralises coffee acids and flattens the cup, more in filter coffee than in espresso, because filter uses far more water per gram of coffee.1
  • The SCA recommends total hardness of 50–175 ppm and alkalinity of 40–75 ppm as CaCO₃, pH 6–8, odour-free and hygienic; alkalinity below 40 ppm raises the risk of corrosion.1
  • pH and “TDS” meter readings alone say little about how a water will brew.1

Why water matters#

Water is the main ingredient of brewed coffee; everything else is the coffee solids it extracts.1 Its quality can mask a coffee’s flavour. In dilute brews such as filter coffee, unsuitable water can overpower acidity and leave the cup dull.1 Water carries tastes and odours of its own, and some of its dissolved substances change how brewing proceeds.2

Water also decides how long machines last. Even with treatment, many espresso machines break down through scale that blocks valves and jets, or, more rarely, through corrosion.1 Water treatment for coffee has long been aimed mainly at protecting equipment; the SCA handbook also sets out to treat water for flavour.1

Drinking-water rules are written for safety, not for coffee. Tap water that meets them can still make poor coffee.2

Where the minerals come from#

Rain is slightly acidic: carbon dioxide from the air dissolves in it and forms weak carbonic acid.5 More carbon dioxide is taken up from organic matter in the soil, and this acidic water partly dissolves carbonate rocks such as limestone.6 It leaves with calcium, magnesium and hydrogen carbonate (bicarbonate) ions.1 Silicate rocks such as granite, feldspar or quartz barely dissolve, so water from them stays soft.1,2

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  1. Rain. Carbon dioxide from the air dissolves in it and forms weak carbonic acid5: CO2 + H2O ⇌ H2CO3.1 Normal rain is about pH 5.6.5
  2. Soil. The water takes up more carbon dioxide from organic matter in the soil.6
  3. Limestone and chalk. The acidic water partly dissolves carbonate rock6; limestone and chalk are the most common sources of calcium and magnesium.7 CaCO3 + CO2 + H2O ⇌ Ca2+ + 2 HCO3−.1
  4. Granite. Silicate rocks such as granite, feldspar or quartz barely dissolve, so water from them stays soft.1,2
  5. Groundwater. Carries calcium, magnesium and hydrogen carbonate ions.1 Ca2+ and Mg2+ make up total hardness1,3; HCO3− is most of the alkalinity.1 Longer contact with the rock makes it usually harder than river or lake water.1
  6. Boiler. Heat drives off the carbon dioxide and the reaction runs backwards: Ca2+ + 2 HCO3− → CaCO3 (scale) + CO2 + H2O.1,3 At most, the lower of total hardness and alkalinity can leave as scale.1
  7. Cup. Hydrogen carbonate neutralises coffee acids and releases carbon dioxide1,2; the higher the alkalinity, the lower the perceived acidity.1
How carbon dioxide links rain, limestone, hardness, alkalinity, boiler scale and the cup. Schematic, not to scale.

How much dissolves depends on the rock, on how long the water stays in contact with it and on the grain size of the minerals.1 Groundwater is therefore usually harder than river or lake water.1 Calcium and magnesium are the two principal ions of hardness, and limestone and chalk are their most common sources.7

Other rocks add other ions. Gypsum (calcium sulfate) raises hardness without adding alkalinity; intruding sea water adds sodium and bicarbonate, which raise alkalinity without adding hardness.1

Hardness and alkalinity#

Most of what matters in coffee water comes down to two numbers.1

  • Total hardness is the amount of dissolved calcium and magnesium.1,3 It is what forms scale with carbonate when water is heated.3
  • Alkalinity is the water’s ability to neutralise acids.2,4 It is measured as the amount of acid needed to bring a sample down to a low end point – between about pH 4.5 and 4.0 in the USGS field method,21 pH 4.3 in the SCA handbook – and in most waters it is mostly bicarbonate.1

In the cup, alkalinity is the more important of the two. The higher the alkalinity, the lower the perceived acidity.1 At high alkalinity, bicarbonate neutralising coffee acids releases much carbon dioxide, which can slow the flow and lead to over-extraction.1 Older trials found that coffees brewed with water containing carbonates were the most bitter and tasted flat, and that more carbonates lengthened the brewing time.2 A review of espresso brewing discusses the role of alkalinity and of individual cations in its sensory properties.9

Hardness affects flavour balance and aroma.1 Whether it also raises how much coffee is extracted is disputed (see Contested).1,8,15

Carbonate hardness is not the same as alkalinity. Carbonate hardness is the part of the hardness that can leave as scale. It equals whichever of total hardness and alkalinity is lower.1 In most tap waters hardness is slightly higher than alkalinity, so the two terms happen to coincide. In softened or salt-influenced water they do not.1 Many test kits sold as “carbonate hardness” kits actually measure alkalinity.1

Why pH misleads. pH tells how acidic or basic the water is at that moment.4 It does not tell how much acid the water can absorb, just as a room’s temperature does not tell how much heat it takes to warm it.2 The pH of most tap waters is set largely by excess dissolved carbon dioxide; left standing in an open container for a day, such water loses carbon dioxide and its pH rises markedly.1 Even a little alkalinity buffers far more acid than the difference between pH 5 and pH 7.1 Our own arithmetic: 25 ppm as CaCO₃ is 0.5 mmol/L of acid-neutralising capacity, while going from pH 7 to pH 5 adds only about 0.01 mmol/L of hydrogen ions – about 50 times less.

Why TDS meters mislead. A “TDS meter” measures electrical conductivity and converts it with an assumed factor.1 The factor depends on which salts are dissolved, and the reading says nothing about what they are.1 Conductivity is still useful to check that a supply or a treatment stays stable.1

Units#

Hardness and alkalinity are usually given as if all the ions were calcium carbonate: ppm (mg/L) as CaCO₃, or as German, French or English degrees.1 These units count ions, not their weight. Bottled-water labels instead give each ion in mg/L, which cannot simply be added up.1

To convert Multiply by To get Source
German degree (°dH) 17.85 ppm as CaCO₃ SCA1, United Utilities20
French degree (°fH) 10 ppm as CaCO₃ SCA1, United Utilities20
Grains per US gallon (gpg) 17.12 ppm as CaCO₃ SCA1, SCAA18
English (Clark) degree (°e) 14.25 ppm as CaCO₃ SCA1, United Utilities20
German degree (°dH) 1.8 French degree (°fH) SVGW13
Calcium, mg/L 2.497 ppm as CaCO₃ (hardness) SCA1, United Utilities20
Magnesium, mg/L 4.118 ppm as CaCO₃ (hardness) SCA1
Hydrogen carbonate, mg/L 0.8202 ppm as CaCO₃ (alkalinity) SCA1
Total hardness, mmol/L 100.1 ppm as CaCO₃ SCA1

The factors follow from atomic masses and the definitions of each degree.1 The UK utility factsheet rounds the same conversions (×0.056 to German, ×0.1 to French, ×0.07 to Clark degrees, ×0.4 to calcium);20 the SCAA standard equates 4 grains with 68 mg/L.18 We checked the magnesium, hydrogen carbonate and mmol/L factors from molar masses (CaCO₃ 100.09, Mg 24.305, HCO₃⁻ 61.02 g/mol; one hydrogen carbonate neutralises half as much acid as one carbonate). A shortcut from the SCA: ppm as CaCO₃ divided by 20, plus ten per cent, gives °dH;1 by our arithmetic it is within about 2% of the exact factor. Example from a bottle label: 50 mg/L calcium, 10 mg/L magnesium and 100 mg/L hydrogen carbonate give a total hardness of 166 ppm and an alkalinity of 82 ppm as CaCO₃ (SCA example,1 checked with the factors above).

Published targets#

SCAA standard (2009). The SCAA standard “Water for Brewing Specialty Coffee” gives a target and an acceptable range for each characteristic; the target is the most desirable point, and any value within the range meets the standard.18 It asks for clean, fresh, odour-free and clear water without chlorine, with TDS 150 mg/L (acceptable 75–250 mg/L), calcium hardness 68 mg/L or 4 grains (acceptable 17–85 mg/L, 1–5 grains), total alkalinity 40 mg/L (acceptable at or near 40 mg/L), pH 7.0 (acceptable 6.5–7.5) and sodium 10 mg/L (at or near 10 mg/L).18 It specifies calcium hardness, not total hardness. The standard specifies TDS measured with a ‘4-4-2’ conversion.18 The SCAA handbook traces the standards to testing at the former Coffee Brewing Center; its own table of them gives some different values (see Contested).2

SCA Water Quality Handbook (2018). The handbook by Wellinger, Smrke and Yeretzian, uses total hardness and alkalinity as the key parameters, and treats TDS as not meaningful on its own.1 It recommends water that is odour-free and hygienic, with total hardness 50–175 ppm as CaCO₃, alkalinity 40–75 ppm (2.2–4.2 °dH) and pH 6–8.1 The handbook gives the hardness range as 2.9–9.8 °dH; by its own factor, 50 ppm is 2.8 °dH. For espresso machines and boilers it recommends a narrower “core zone”, bounded by the corrosion limits and by a maximum of 12 mg/L of scale in a brew boiler or 30 mg/L in a steam boiler at 130 °C.1

Other published views. Recommendations collected by the SCA differ widely on hardness – the softest from a World Brewers Cup recommendation, the hardest from Colonna-Dashwood and Hendon – but agree much more closely on alkalinity; the SCA’s own range, 40–75 ppm, reflects this.1 All of them put total hardness above alkalinity.1 Most were made for espresso.1

These are recommendations, not laws of nature. The SCA stresses that the sensory part of the target is largely subjective and that too few data exist to describe the effect of hardness and alkalinity across origins, roasts and brew methods.1

Treatment#

No single filter suits every water. Each treatment moves a water in its own direction on the water chart (see Check your water).1

Treatment How it works Hardness Alkalinity Source
Activated carbon Removes chlorine, chloramines and organic off-flavours – – SCA1, SCAA2
Softener Ion exchange: calcium and magnesium for sodium or potassium Down Unchanged SCA1
Decarboniser (weak-acid cation exchanger) Calcium and magnesium for H⁺; H⁺ turns bicarbonate into carbonic acid Down Down by the same amount SCA1
Buffered decarboniser Mostly decarboniser resin with some softener resin Down Down, leaving some alkalinity SCA1
Reverse osmosis or deioniser Removes almost all dissolved substances; often blended back with tap water Towards zero Towards zero SCA1
Dealkaliser Ion exchange or strong acid Unchanged Down SCA1
Hardener Adds calcium or magnesium as sulfate or chloride Up Unchanged SCA1
Carboniser Dissolves magnesium carbonate Up Up by the same amount SCA1
Alkaliser Dissolves sodium or potassium hydrogen carbonate Unchanged Up SCA1
Calcium-for-magnesium exchanger Swaps one hardness ion for the other Unchanged Unchanged SCA1

Mixing two waters gives any composition on the straight line between them; mixing three gives any point inside their triangle.1 Where no single method reaches the target, the SCA suggests a decarboniser plus hardener, or full demineralisation followed by remineralisation.1 Only reverse osmosis and deionisation fully remove unwanted ions such as iron and lead.1

Softened water is a special case. Softening leaves the alkalinity, now paired with sodium. The SCAA handbook reports that this slowed the flow of water through the coffee bed in Coffee Brewing Center trials and advises against softened water for brewing.2

Check your water#

Enter the total hardness and alkalinity from your water supplier’s report or a bottle label, or pick a sample water. The chart shows where it sits against the published targets and corrosion limits, and which treatments would move it towards the SCA range. The calculations use only the numbers cited on this page.

Tool

Water chart

Enter the hardness and alkalinity of your water, or a bottle label: see where it sits against published targets and which treatment would help.

Or pick a sample water

Water chart

Water chart: alkalinity (horizontal) against total hardness (vertical), both in ppm as calcium carbonate, with published targets, corrosion-risk zones and your water.
Unit

ppm as CaCO₃

Key and notes

Key: amber box = SCA 2018 range (hardness 50–175, alkalinity 40–75 ppm) · black square on thin bar = SCAA 2009 target, calcium hardness 68 at alkalinity 40 (bar: acceptable calcium hardness 17–85); the SCAA standard gives calcium hardness, not total hardness, so it is not directly comparable on this axis · hatched = corrosion risk (alkalinity below 40; hardness above 1.8 × alkalinity) · dotted line = hardness equals alkalinity (limestone) · dashed line = 150 ppm alkalinity, up to which espresso shows no clear buffering.

Treatment directions: ↓ softener · ↙ decarboniser · towards zero: reverse osmosis + blending · ← dealkaliser · ↑ hardener · ↗ carboniser · → alkaliser (bicarbonate). Hover an arrow for its name.

Arrows show the direction each treatment moves a water, not how far. Amber arrows move this water towards the SCA range. Sample waters are worked examples from the SCA handbook.

Keeps your inputs, result and chart. Nothing is stored online.
Alkalinity against total hardness, both in ppm as CaCO₃, with the SCA 2018 recommendation, the SCAA 2009 standard (plotted as calcium hardness), the corrosion limits and the direction in which each treatment moves a water.1,18 Enter your own water or pick a sample. Sample waters are worked examples from the SCA handbook.1

Your local water#

Tap water differs from town to town. How hard it is depends on where it comes from: rain picks up lime from the rock it seeps through, so groundwater and spring water tend to be harder than treated lake water.12 Bottled waters differ just as much.

The numbers you need are usually published. Water suppliers report hardness in their water analyses, and bottle labels list calcium, magnesium and hydrogen carbonate in mg/L, which can be converted to ppm as CaCO₃.1 The tool above does this conversion.

Countries report hardness in different units and sort it into different classes. These classes were written for households and appliances, not for coffee, so a water called “soft” locally may still be too hard or too alkaline for brewing:

Where Unit used Classes, converted to ppm as CaCO₃ Source
United States mg/L (ppm) as CaCO₃; grains per gallon Soft 0–60; moderately hard 61–120; hard 121–180; very hard above 180 USGS3
Germany mmol/L of calcium carbonate Soft below 150; medium 150–250; hard above 250 (law: below 1.5, 1.5–2.5, above 2.5 mmol/L) Detergents law (WRMG §9)17
Switzerland French degrees (°fH; 1 °fH = 10 ppm) Soft below 150; medium hard 150–250; fairly hard 250–320; hard 320–420; very hard above 420 Kanton Zürich12, SVGW13

In these terms the SCA range for total hardness, 50–175 ppm,1 starts in the softest class everywhere. It ends in the medium class in Germany and Switzerland, but its upper part (121–175 ppm) already counts as hard in the US classes.3,12,13,17 Alkalinity, the more important number for coffee, is often not in these classes at all; look for it in the full water analysis.1

Household softening follows its own rules. In Switzerland, for example, the SVGW advises against softening drinking water below a certain hardness and sets a minimum residual hardness for softened water.13 Such rules protect pipes and appliances; for coffee, the SCA puts the most weight on alkalinity.1

Carbonate chemistry#

Four equilibria tie carbon dioxide, alkalinity and scale together.1

  1. CO₂ (dissolved) + H₂O ⇌ H₂CO₃ (carbonic acid)
  2. H₂CO₃ ⇌ HCO₃⁻ + H⁺
  3. HCO₃⁻ ⇌ CO₃²⁻ + H⁺ (only relevant in strongly basic water)
  4. Taken together with limestone: CaCO₃ + CO₂ + H₂O ⇌ Ca²⁺ + 2 HCO₃⁻

Equations 1–3 are given in the SCA handbook, which lumps dissolved CO₂ and carbonic acid together, as is customary in water chemistry.1 Equation 4 is the sum of dissolution and protonation that the handbook describes in words: acidic water dissolves carbonate rock and acquires calcium and hydrogen carbonate.1 Read forwards, it explains how limestone becomes hardness and alkalinity. Read backwards, it is scale: heating drives off CO₂, and calcium carbonate precipitates.1,3

Normal rain has a pH of about 5.6 because carbon dioxide from the air dissolves in it;5 the SCA handbook explains the slight acidity of pure water in contact with air the same way.1 Most tap water carries carbon dioxide in excess of that equilibrium, which strongly influences its pH.1 Water in equilibrium with air holds much less. Our own calculation from Henry’s law gives about 0.7 mg/L: with a solubility constant of 3.4 × 10⁻⁴ mol/(m³·Pa) at 25 °C and a temperature coefficient of 2,300 K,19 air with 400–420 ppm CO₂ (40.5–42.6 Pa) gives 0.69–0.73 mg/L at 20 °C. The SCA handbook gives a lower value (see Contested). Stirred in an open container for a day, a hard tap water in one of the handbook’s examples lost most of its excess carbon dioxide and its pH rose markedly.1

Charge must balance. Calcium carbonate removed as scale takes one calcium ion but two hydrogen carbonate ions, because each calcium carries two charges.1 This is why units based on equivalents, such as ppm as CaCO₃, make hardness, alkalinity and scale directly comparable.1

Why filter needs less alkalinity than espresso#

Filter coffee uses far more water per gram of coffee than espresso, so the same water brings far more buffer into contact with the same acids.1 The SCA assumes a ratio of coffee to beverage of about 1:15 for filter and 1:2 for espresso (see Brew ratio and strength for the different ratios).1 It concludes that espresso tolerates up to about 150 ppm alkalinity before buffering becomes apparent, while filter needs less.1

Our own arithmetic, from these cited numbers: 1 g of coffee brewed at 1:15 with water of 50 ppm alkalinity meets 0.75 mg of acid-neutralising capacity (as CaCO₃), or about 0.015 mmol of bicarbonate. At 1:2 it meets 0.10 mg – 7.5 times less. Espresso brewed with 150 ppm water still meets only 0.30 mg per gram. This simple calculation uses beverage weight and ignores water held back in the grounds.

Hardness behaves differently. The SCA finds that total hardness has less impact than alkalinity and that even hard water can give a high-quality filter brew.1

Scale and corrosion#

Scale. Scale forms where calcium meets carbonate and heat, mostly as calcium carbonate; at very high pH magnesium hydroxide can form too.1 It lowers heat transfer and clogs valves and jets, especially in hot-water sections.1 Gypsum-rich water forms scale of a different kind.1 Silica scales regardless of pH and alkalinity, and is hard to remove.2 Lower pH means less scale.1

The SCA estimates maximum scale from a modified Langelier index and turns it into a yearly amount from the number of drinks.1 Our own arithmetic, following its example: at 100 drinks a day and 0.1 L per drink including flushing, a machine uses about 3,650 L a year, so water able to deposit 30, 100 or 200 mg/L of scale can leave about 110, 365 or 730 g. The estimate holds best when the machine stands hot for hours; at high throughput the water does not stay hot long enough for all of it to form.1

Corrosion. The SCA lists the conditions that make corrosion likely:1

  • alkalinity below 40 ppm as CaCO₃, which leaves too little buffer;
  • pH below 6 or above 8;
  • chloride, sulfate or nitrate above about 80% of the alkalinity in equivalents (a Larson–Skold index above 0.8). For gypsum waters this becomes: total hardness no more than 80% higher than alkalinity;
  • for salt-influenced waters, electrical conductivity (µS/cm) more than three times the alkalinity (ppm as CaCO₃). The SCA derives this rule from measured waters, among them tap waters near Barcelona.

Chloride is a particular concern. The SCA advises calcium or magnesium sulfate rather than chlorides for hardening water used in espresso machines, because chlorides increase the chance of corrosion; espresso machine makers often advise against water with significant amounts of chloride.1 Soft water that is not stabilised tends to corrode pipes in general.7

Decarboniser limits. A decarboniser turns bicarbonate into carbonic acid. In an open kettle the CO₂ escapes when the water is heated, but in a closed espresso system it stays.1 Removing a large amount of alkalinity therefore leaves much dissolved CO₂; the water turns acidic, corrosion risk rises, and espresso can foam with large, short-lived bubbles.1 Our own arithmetic: removing 250 ppm of alkalinity (as CaCO₃) converts 5 mmol/L of hydrogen carbonate into 5 mmol/L of CO₂, about 220 mg/L. The SCA therefore advises setting the bypass so that output alkalinity is 40–70 ppm for waters up to 250 ppm, and so that alkalinity falls by no more than 200 ppm for harder waters.1

The SCAA handbook adds that corrosion in brewers is rarely caused by natural water: acid flux from soldered copper pipe joints is a more usual culprit.2

Off-flavours and contaminants#

  • Chlorine and chloramines used for disinfection give unpleasant flavours and should be removed, most simply with activated carbon.1,2 Chlorine can react with coffee phenols to form chlorophenols, which have a medicinal taste.2
  • Iron turns coffee greenish. In a 1955 study, a difference could be seen side by side at 1 ppm, and above 7 ppm coffee with cream had a clearly unpleasant greenish cast.14
  • Lead is toxic. Only reverse osmosis and deionisation remove it completely.1
  • Taste thresholds. In water, the taste threshold for calcium is 100–300 mg/L, depending on the anion.7 In the 1955 study, coffee made with water containing single ions at their thresholds in water could not be told apart from coffee made with distilled water.14

Measuring water#

Drop titration. Outside a laboratory, hardness and alkalinity are measured by titration, as two separate tests.1 Hardness is titrated with EDTA; alkalinity with a strong acid such as hydrochloric acid.1 Reagent is added drop by drop until the colour changes completely, and the drops are counted.1 The SCA recommends a resolution of at least 20 ppm (1 °dH). Doubling the sample volume halves the value of each drop, which helps with low-mineral treated waters.1

Conductivity meters. Electrical conductivity depends on temperature: depending on the salts present, it rises by about 1–3% per °C.10 Measurements are therefore referred to a standard temperature, typically 25 °C, and field meters often correct with a fixed coefficient of 0.019–0.020 per °C.10 The SCA handbook uses 20 °C as its reference and warns that many cheap meters do not correct at all.1

Converting conductivity to TDS adds a second uncertainty. In the natural waters studied by Hem of the US Geological Survey, the ratio of dissolved solids (mg/L) to conductivity (µS/cm) ranged from 0.54 to 0.96.11 It is much higher for dissolved calcium carbonate than for table salt.1 The heritage SCAA standard assumed one fixed factor, but many meters use another or a variable factor.1 The SCA therefore treats a TDS estimate as rough, with large deviations possible.1

Daily checks. Once a treatment is set, a conductivity meter can track it. For decarbonisation, conductivity falls roughly in proportion to the alkalinity removed, which the SCA confirmed on Swiss tap waters.1 A softener barely changes conductivity, so conductivity cannot track it.1

Making water from salts#

Recipe waters start from almost pure water and add salts in known amounts.1 Sodium hydrogen carbonate raises alkalinity only; magnesium or calcium sulfate or chloride raises hardness only.1 As an example, the SCA dissolves 3 g of pure sodium bicarbonate in 1 L of reverse-osmosis water to make a concentrate of 100 °dH alkalinity; 10 g of it in 1 L of water adds 1 °dH.1 We checked the arithmetic from molar masses: 3 g of NaHCO₃ is about 35.7 mmol, 35.7 mmol/L of hydrogen carbonate is about 100 °dH, and diluting about 10 g in a litre is roughly a hundredfold dilution.

Mixing follows a lever rule. For a target alkalinity, the share of water 1 is (alkalinity of water 2 − target) ÷ (alkalinity of water 2 − alkalinity of water 1); the same formula works for hardness.1 The SCA’s worked example mixes a water of 5 ppm alkalinity with one of 150 ppm to reach 60 ppm.1 The handbook prints 64.1% of the soft water, but its own formula gives 62.1% (our own arithmetic): (150 − 60) ÷ (150 − 5) = 90 ÷ 145 = 0.621, and 0.621 × 5 + 0.379 × 150 = 60 ppm.

Reference values#

Parameter Value reported Source
Total hardness, SCA recommendation 50–175 ppm as CaCO₃ (2.8–9.8 °dH by the factor above; printed as 2.9–9.8) SCA 20181
Alkalinity, SCA recommendation 40–75 ppm as CaCO₃ (2.2–4.2 °dH) SCA 20181
Alkalinity titration end point About pH 4.5–4.0 (USGS field method); pH 4.3 (SCA) USGS21, SCA 20181
pH, SCA recommendation 6–8 SCA 20181
Alkalinity tolerable for espresso Up to about 150 ppm before buffering becomes apparent SCA 20181
SCAA target (2009) TDS 150 mg/L; calcium hardness 68 mg/L (4 grains); total alkalinity 40 mg/L; pH 7.0; sodium 10 mg/L; chlorine 0 mg/L SCAA 200918
SCAA acceptable range (2009) TDS 75–250 mg/L; calcium hardness 17–85 mg/L (1–5 grains); total alkalinity at or near 40 mg/L; pH 6.5–7.5; sodium at or near 10 mg/L SCAA 200918
Corrosion: minimum alkalinity 40 ppm as CaCO₃ SCA 20181
Corrosion: gypsum waters Total hardness < 1.8 × alkalinity SCA 20181
Corrosion: salt-influenced waters Conductivity (µS/cm) ≤ 3 × alkalinity (ppm) SCA 20181
Core-zone scale limit 12 mg/L (brew boiler); 30 mg/L (steam boiler, 130 °C) SCA 20181
Decarboniser output, espresso 40–70 ppm alkalinity (input ≤ 250 ppm); reduce by ≤ 200 ppm (input > 250 ppm) SCA 20181
Hardness classes, USGS Soft 0–60; moderately hard 61–120; hard 121–180; very hard > 180 mg/L as CaCO₃ USGS3
Hardness classes, Switzerland Soft < 15; medium hard 15–25; fairly hard 25–32; hard 32–42; very hard > 42 °fH Kanton Zürich12, SVGW13
Normal rain pH about 5.6 EPA5
Dissolved CO₂ at equilibrium with air, 20 °C About 0.7 mg/L (our Henry’s law calculation; the SCA gives 0.4 mg/L, see Contested) Calculated from Henry’s law19
Conductivity temperature effect About 1–3% per °C McCleskey10
TDS/conductivity ratio 0.54–0.96 (natural waters studied by Hem) Singh & Kalra11
Calcium taste threshold in water 100–300 mg/L WHO7
050100150200250300350400450ppm as CaCO₃SCA 2018 – total hardness50–175 ppm1 SCA 2018 – alkalinity40–75 ppm1 SCAA 2009 target – calciumhardness68 mg/L (4 grains)18 SCAA 2009 acceptable –calcium hardness17–85 mg/L (1–5 grains)18 SCAA 2009 target – totalalkalinity40 mg/L (acceptable: at or near 40)18 Soft0–60 mg/L3 Moderately hard61–120 mg/L3 Hard121–180 mg/L3 Very hard> 180 mg/L3 Soft< 1.5 mmol/L17 Medium1.5–2.5 mmol/L17 Hard> 2.5 mmol/L17 Soft< 15 °fH12,13 Medium hard15–25 °fH12,13 Fairly hard25–32 °fH12,13 Hard32–42 °fH12,13 Very hard> 42 °fH12,13
Data table
ppm as CaCO₃Source
SCA 2018 – total hardness50–175 ppm1
SCA 2018 – alkalinity40–75 ppm1
SCAA 2009 target – calcium hardness68 mg/L (4 grains)18
SCAA 2009 acceptable – calcium hardness17–85 mg/L (1–5 grains)18
SCAA 2009 target – total alkalinity40 mg/L (acceptable: at or near 40)18
Soft0–60 mg/L3
Moderately hard61–120 mg/L3
Hard121–180 mg/L3
Very hard> 180 mg/L3
Soft< 1.5 mmol/L17
Medium1.5–2.5 mmol/L17
Hard> 2.5 mmol/L17
Soft< 15 °fH12, 13
Medium hard15–25 °fH12, 13
Fairly hard25–32 °fH12, 13
Hard32–42 °fH12, 13
Very hard> 42 °fH12, 13
Coffee targets and general hardness classes on one scale, in ppm as CaCO₃: SCA 2018 and SCAA 2009 recommendations (SCAA values are calcium hardness),1,18 US Geological Survey classes,3 German classes converted from mmol/L17 and Swiss classes converted from °fH.12,13

Sample waters#

The water chart under Check your water offers sample waters. They are worked examples from the SCA handbook: points used to show how mixing and treatment move a water, not measurements of real supplies.1

Water Ca (mg/L) Mg (mg/L) HCO₃⁻ (mg/L) Alkalinity (ppm CaCO₃) Total hardness (ppm CaCO₃) Source
Bottle-label example 50 10 100 82 166 SCA1
Almost pure (RO-like) – – – 5 10 SCA1
Medium-hard (example) – – – 150 200 SCA1
Hard mineral water (example) – – – 300 320 SCA1
Epsom salt concentrate – – – 10 450 SCA1

Real waters can sit far from the limestone diagonal: gypsum adds hardness without alkalinity, and sea-water intrusion adds alkalinity without hardness.1

Open questions#

  • Calcium versus magnesium. Theory and preliminary experiments suggest magnesium extracts slightly more than calcium, but its effect on sensory properties remains unclear.1,8 The total-hardness concept treats the two as one.1
  • Brew ratio, temperature and pressure. The SCA expects the optimum to shift with brew ratio and with temperature and pressure, and calls for correction factors or separate zones.1
  • Roast style. Anecdotal evidence suggests that harder, more alkaline water can partly compensate for underdeveloped roasts.1 No study opened for this entry tested it.
  • Local taste. Where tap water is very soft, preferences and roasting styles may have adapted to it.1
  • The evidence behind TDS 150 mg/L. The SCAA target rests partly on a small blind tasting by committee members, which the handbook itself says cannot be considered statistically valid.2

Key studies#

Hendon et al., 2014 – Cations and extraction. Uses density functional theory to calculate how strongly sodium, magnesium and calcium ions bind to five coffee acids, caffeine and the aroma compound eugenol. The calculations are meant to explain the mechanism of extraction and suggest an ideal mineral composition; they are a model, not a brewing trial.

Journal of Agricultural and Food Chemistry 62(21), 4947–4950 · doi:10.1021/jf501687c

Navarini & Rivetti, 2010 – Water quality for espresso. Reviews what was known about how water and coffee components interact during espresso brewing. It discusses the role of alkalinity and of selected cations in the sensory properties of espresso.

Food Chemistry 122(2), 424–428 · doi:10.1016/j.foodchem.2009.04.019

Lockhart et al., 1955 – Water impurities and flavour. Determined taste thresholds of common ions in water with experienced panels, then brewed coffee with water at those levels. Coffee made with water containing single ions at their water thresholds could not be told apart from coffee made with distilled water; iron also gave the coffee a greenish colour.

Journal of Food Science 20(6), 598–605

Bratthäll et al., 2024 – Divalent cations and coffee acids. Added magnesium and calcium salts before or after brewing and measured citric, malic, lactic and quinic acids by GC–MS and NMR. At drinking-water concentrations the acids varied little; only ten-fold higher concentrations gave clearer differences.

Heliyon 10(5), e26625 · doi:10.1016/j.heliyon.2024.e26625

Dadalı & Elmacı, 2021 – Hardness and filter coffee. Brewed filter coffee with four waters – bottled, purified, medium hard and hard – and compared volatile compounds and sensory intensities. Sourness was strongest with soft water and weakest with hard water; bitterness was reported as the dominant taste only for hard water (3.63). Medium-hard water gave the most volatile compounds, which is why the authors recommend it; the study did not measure preference.

Turkish Journal of Agriculture – Food Science and Technology 9(2), 312–320 · doi:10.24925/turjaf.v9i2.312-320.3885

Contested
  • Does hardness raise extraction? A density-functional model of how sodium, magnesium and calcium bind coffee compounds8 is read by the SCA handbook as implying higher extraction with harder water, but laboratory tests reported in the handbook found no effect measurable with a coffee refractometer, only on flavour balance and aroma.1 Adding magnesium and calcium salts at drinking-water levels changed four coffee acids little.15 The SCAA handbook reports an older study in which water with sodium bicarbonate gave a stronger brew than water with calcium chloride.2
  • How soft is too soft: suggested hardness optima collected by the SCA range widely, from a World Brewers Cup recommendation at the soft end to Colonna-Dashwood and Hendon at the hard end.1 Some cuppers use water with hardness and alkalinity far below the SCA range; the SCA advises strongly against such water in espresso machines because of corrosion.1 A study of filter coffee recommended medium-hard water because it gave the most volatile compounds, not on grounds of sensory preference; bitterness dominated only in coffee made with hard water.16
  • TDS versus hardness and alkalinity: the SCAA standard is built around a TDS of 150 mg/L,2,18 while the SCA 2018 handbook calls TDS on its own not meaningful for coffee extraction.1 The SCAA standard also sets a pH target of 7.0 with an acceptable range of 6.5–7.5, narrower than the SCA’s 6–8,1,18 and the SCAA handbook’s text and table disagree on sodium (20 mg/L in the list, 10 mg/L in the table).2 The table in the 2011 SCAA handbook, credited to the 2009 committee, also differs from the standard document: calcium hardness target 3–4 grains (51–68 mg/L), pH target 7–8 with an adequate range of 6.5–7.5, total alkalinity adequate at 10–100 mg/L and sodium adequate below 30 mg/L.2,18
  • Carbon dioxide in water at equilibrium with air: the SCA handbook gives 0.4 mg/L at 20 °C (a single trade source);1 our own calculation from published Henry’s law constants gives about 0.7 mg/L (see Carbonate chemistry).19
  • Softened water: the SCAA handbook advises against brewing with softened water, citing slower flow through the coffee bed;2 the SCA 2018 handbook lists the softener as a standard treatment that lowers hardness but leaves alkalinity unchanged.1
  • Conductivity reference temperature: the SCA handbook uses 20 °C;1 a USGS study gives 25 °C as the typical reference.10 Readings from meters with different reference temperatures or conversion factors are not directly comparable.1
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Sources

  1. AWellinger, M.; Smrke, S.; Yeretzian, C. (2018). The SCA Water Quality Handbook, edition 2 (ISBN 978-0-9995807-3-8). Specialty Coffee Association.
  2. ABeeman, D.; Songer, P.; Lingle, T. (ed. Everage, L.) (2011). The Water Quality Handbook (ISBN 978-1-882552-08-5). Specialty Coffee Association of America.
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  9. ANavarini, L.; Rivetti, D. (2010). Water quality for Espresso coffee. Food Chemistry 122(2), 424–428. doi:10.1016/j.foodchem.2009.04.019 · other copies
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  15. ABratthäll, T.; Figueira, J.; Nording, M. L. (2024). Influence of divalent cations on the extraction of organic acids in coffee determined by GC-MS and NMR. Heliyon 10(5), e26625. doi:10.1016/j.heliyon.2024.e26625 · other copies
  16. ADadalı, C.; Elmacı, Y. (2021). The Effect of Water Hardness on Volatile Compounds and Flavour of Filter Coffee. Turkish Journal of Agriculture – Food Science and Technology 9(2), 312–320. doi:10.24925/turjaf.v9i2.312-320.3885 · other copies
  17. ABundesrepublik Deutschland (2007). Gesetz über die Umweltverträglichkeit von Wasch- und Reinigungsmitteln (Wasch- und Reinigungsmittelgesetz – WRMG), § 9 Angabe der Wasserhärtebereiche. Federal law; § 9 text as reproduced by the Umweltbundesamt (Kennzeichnung von Wasch- und Reinigungsmitteln).
  18. ASpecialty Coffee Association of America (2009). SCAA Standard: Water for Brewing Specialty Coffee (version 21NOV2009A). Specialty Coffee Association of America (copy of the standard hosted by a water-treatment retailer).
  19. ASander, R. (2023). Compilation of Henry’s law constants (version 5.0.0) for water as solvent – carbon dioxide (CAS RN 124-38-9). Atmospheric Chemistry and Physics 23, 10901–12440. doi:10.5194/acp-23-10901-2023 · other copies
  20. BUnited Utilities Water Limited (2025). Water hardness (factsheet 09/25/SD/10586-6335). United Utilities Water Limited.
  21. AU.S. Geological Survey, Office of Water Quality NFM 6.6.4.B: Alkalinity and ANC field determination by Inflection Point Titration (method summary). U.S. Geological Survey National Field Manual, via the National Environmental Methods Index (NEMI).

Tier A · authoritative · B · trade and expert · C · general. Supporting quotes for every source are in the data version of this entry. If a publisher’s site refuses access, try the doi link or “other copies”.

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