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Borehole Water Problems

Borehole water usually looks clean from the tap, but groundwater is chemically complex and almost never ready to use untreated. Because the water sits in an oxygen-free aquifer, it carries dissolved metals, gases, hardness and sometimes pathogens that only reveal themselves — as stains, scale, smell, fouled membranes or failed samples — once it reaches the surface. This page explains every common borehole water problem: what it is, why it happens, and what it does to your plant.

The Anoxic Aquifer Problem

Almost every borehole problem traces back to one fact: the water has no oxygen.

Deep groundwater is typically anoxic — it has been isolated from the air for years. In that reducing, often slightly acidic, environment, metals stay dissolved and invisible, carbon dioxide builds up, and sulphate can reduce to hydrogen sulphide. The water looks crystal clear at the wellhead. The moment it meets air — in your tank, pipe, membrane or sample bottle — the chemistry reverses: metals oxidise and precipitate, gases come out of solution, and the “clean” water turns orange, black, scaly or smelly. Understanding this is the key to treating it: most borehole treatment is about controlling that oxidation deliberately, instead of letting it happen where you don’t want it.

Common Borehole Contaminants & What They Do

Each one needs a specific treatment step — there is no single “borehole filter”.

Dissolved Iron (Fe²⁺)

Invisible in the aquifer; precipitates as orange/brown deposits on contact with air. Stains fixtures and laundry, fouls RO membranes, blocks pipework. Needs oxidation then filtration.

Fe/Mn Removal

Dissolved Manganese (Mn²⁺)

Black staining, harder to oxidise than iron — needs a higher pH or a catalyst. Often the parameter that defeats a simple plant. Tiny limits (0.05 mg/L potable).

Fe/Mn Removal

Carbon Dioxide & Aggressive Water

Excess dissolved CO₂ makes water acidic and corrosive (low Langelier index), attacking pipes and concrete. Stripped out by aeration, then pH corrected.

Aeration Towers

Hydrogen Sulphide (H₂S)

Rotten-egg smell, corrosive, toxic at the wellhead. Formed by sulphate-reducing bacteria in the aquifer. Removed by aeration/stripping and oxidation.

Aeration Towers

Hardness & Scaling

Calcium and magnesium scale boilers, cooling systems and RO membranes. Managed by softening or antiscalant depending on end use.

Hardness & Softening

Colloids & Turbidity (SDI)

Sub-micron 1–3 µm colloids pass straight through sand filters and drive the Silt Density Index that fouls RO. Needs ultrafiltration.

RO Pre-Treatment

Ammonia & Nitrate

Ammonia consumes disinfectant and feeds nitrification; nitrate breaches potable limits. Removed biologically, by ion exchange or RO.

Ammonia Treatment

Bacteria & Pathogens

Even deep boreholes can suffer ingress (E. coli, coliforms). A potable supply needs a disinfection barrier and a sampling regime.

Disinfection

Salinity & TDS

Coastal or deep boreholes can be brackish. High TDS/chloride needs reverse osmosis to reach potable or process quality.

RO Pre-Treatment

Typical Borehole Parameters & Limits

Indicative figures — only a treatability assessment of your water is definitive.

ParameterOften found in borehole waterUK/EU potable limitMain impact
Iron (Fe)0.5–15 mg/L0.2 mg/LStaining, fouling
Manganese (Mn)0.1–3 mg/L0.05 mg/LBlack staining
Hardness150–500 mg/L CaCO₃(indicator)Scaling
Ammonium0–3 mg/L0.5 mg/LDisinfection demand
Nitrate0–100 mg/L50 mg/LHealth limit
Turbidity0.5–20 NTU4 NTU (1 at works)RO fouling, aesthetics
H₂S0–5 mg/Lnone detectableOdour, corrosion

Solve Each Problem

Not sure what’s in your borehole?

Send us a water analysis — or let us sample it — and we will identify exactly which of these problems you have, what each one will cost you untreated, and the treatment train that fixes them.

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