Water Quality Fundamentals & Indicators
Learn water-quality fundamentals and the physical, chemical, and biological indicators operators use to evaluate source water, treatment performance, finished water, and changing process conditions.
Water quality describes the physical, chemical, and biological characteristics of water. Operators use water-quality data to understand the source, control treatment processes, verify finished-water performance, and recognize developing problems before they become serious.
No single measurement describes overall water quality. Operators should interpret related parameters together, compare current results with normal baseline conditions, and understand whether a change began in the source, treatment process, storage system, or distribution system.
Three Major Water-Quality Categories
Water-quality characteristics are commonly grouped as:
- physical;
- chemical;
- biological.
Physical Water-Quality Indicators
Important physical indicators include:
- temperature;
- turbidity;
- color;
- taste;
- odor;
- visible solids.
Chemical Water-Quality Indicators
Important chemical indicators include:
- pH;
- alkalinity;
- hardness;
- conductivity;
- dissolved oxygen;
- iron;
- manganese;
- nutrients;
- disinfectant residual.
Biological Water-Quality Indicators
Biological indicators include microorganisms such as:
- bacteria;
- viruses;
- protozoa;
- algae.
Water Quality Depends on Location
The meaning of a result depends on where the sample was collected.
Operators may compare:
- raw source water;
- individual treatment stages;
- finished water;
- storage facilities;
- distribution-system locations.
Water Quality Depends on Time
Water quality can change over:
- hours;
- days;
- seasons;
- years.
Trend data are often more useful than a single isolated result.
Temperature
Temperature affects many treatment and water-quality processes.
It can influence:
- chemical reaction rates;
- coagulation;
- settling;
- disinfection;
- biological activity;
- gas solubility.
Cold Water
Cold water can slow:
- chemical reactions;
- floc formation;
- microbial activity.
Warm Water
Warm water can increase:
- biological activity;
- algal growth;
- disinfectant decay;
- taste and odor concerns.
Turbidity
Turbidity describes the cloudiness of water caused by suspended or colloidal material that scatters light.
Turbidity can result from:
- clay;
- silt;
- organic matter;
- microorganisms;
- precipitates.
Why Turbidity Matters
Turbidity can indicate:
- changing source conditions;
- poor coagulation;
- clarifier carryover;
- filter breakthrough;
- distribution-system disturbance.
Turbidity and Microorganisms
Particles can shield microorganisms from disinfectants.
Good particle removal therefore supports effective disinfection.
Raw-Water Turbidity
Raw-water turbidity can rise quickly after:
- rainfall;
- snowmelt;
- erosion;
- reservoir turnover;
- intake disturbance.
Finished-Water Turbidity
Unexpected finished-water turbidity should prompt review of:
- coagulation;
- settling;
- filter performance;
- instrument condition;
- sample location.
pH
pH indicates how acidic or basic water is.
The pH scale is logarithmic.
This means a one-unit pH change represents a tenfold change in hydrogen-ion activity.
Why pH Matters
pH affects:
- coagulation;
- disinfection;
- corrosion;
- chemical solubility;
- biological processes.
pH Is Not the Same as Alkalinity
pH describes the current acid-base condition of water.
Alkalinity describes the water's ability to neutralize added acid.
Alkalinity
Alkalinity is the acid-neutralizing capacity of water.
It is commonly associated with:
- bicarbonate;
- carbonate;
- hydroxide.
Why Alkalinity Matters
Alkalinity helps stabilize pH and is important in:
- coagulation;
- corrosion control;
- biological treatment;
- chemical-feed calculations.
Low Alkalinity
Low-alkalinity water can experience larger pH changes when acids or treatment chemicals are added.
Hardness
Hardness is mainly associated with dissolved calcium and magnesium.
Hard water can contribute to:
- scale;
- higher soap consumption;
- mineral deposits.
Hardness and Source Water
Groundwater often has higher hardness than surface water because it remains in contact with mineral formations for longer periods.
Conductivity
Conductivity measures the ability of water to conduct electrical current.
Conductivity generally increases as dissolved ionic material increases.
What Conductivity Can Tell an Operator
Conductivity is useful for identifying changes in:
- source water;
- source blending;
- road-salt influence;
- industrial discharge;
- dissolved mineral content.
Conductivity Does Not Identify the Chemical
A conductivity change indicates that ionic conditions changed, but it does not identify which dissolved substance caused the change.
Total Dissolved Solids
Total dissolved solids represent dissolved material remaining in water after suspended matter is removed.
Higher dissolved-solids levels can affect:
- taste;
- conductivity;
- corrosion;
- scaling.
Color
Color can result from:
- natural organic matter;
- iron;
- manganese;
- industrial contamination;
- distribution-system deposits.
True Color Versus Apparent Color
Apparent color can include suspended material.
True color refers more specifically to color remaining after suspended material is removed.
Taste and Odor
Taste and odor can originate from:
- algae;
- organic matter;
- chlorine;
- stagnation;
- industrial chemicals;
- distribution-system conditions.
Taste and Odor Are Operational Clues
An unusual taste or odor can provide early evidence of:
- source-water change;
- algal activity;
- chemical contamination;
- distribution-system water age.
Do Not Identify Chemicals by Smell
Operators should not deliberately inhale concentrated vapors or unknown chemicals to identify them.
Iron
Iron can occur naturally in groundwater and may also enter water through corrosion.
Iron can contribute to:
- red or brown color;
- staining;
- sediment;
- taste complaints.
Manganese
Manganese can produce:
- dark staining;
- black particles;
- deposits;
- consumer complaints.
Iron and Manganese Can Change with Oxidation State
Dissolved forms can become insoluble after oxidation.
This can create particles that must be removed through treatment.
Dissolved Oxygen
Dissolved oxygen, or DO, is oxygen dissolved in water.
DO can influence:
- corrosion;
- biological activity;
- iron and manganese chemistry;
- odor formation.
Low DO in Reservoirs
Low dissolved oxygen in deep reservoir water can promote reducing conditions and increased soluble iron or manganese.
Chlorine Residual
Chlorine residual is an important finished-water and distribution-system indicator where chlorine is used.
Residual trends can help identify:
- changing chlorine demand;
- water age;
- storage conditions;
- possible contamination or loss of disinfectant protection.
Microbiological Water Quality
Microbiological monitoring is essential because disease-causing organisms may not change water appearance, taste, or odor.
Clear water should never be assumed microbiologically safe based on appearance alone.
Indicator Organisms
Indicator organisms are used to provide information about microbiological water quality without testing for every possible pathogen.
Source-Water Microbiology
Surface-water microbial quality can change rapidly after:
- storms;
- wastewater releases;
- agricultural runoff;
- wildlife activity.
Finished-Water Microbiology
Finished-water microbiological quality depends on multiple barriers such as:
- source protection;
- particle removal;
- disinfection;
- distribution-system integrity.
Algae
Algae can affect water quality through:
- taste and odor;
- pH changes;
- organic matter;
- filter loading;
- disinfectant demand.
Nutrients
Nutrients such as nitrogen and phosphorus can support biological growth.
Excess nutrients in source water can contribute to:
- algal blooms;
- taste and odor;
- source-water variability.
Natural Organic Matter
Natural organic matter comes from sources such as:
- soil;
- vegetation;
- wetlands;
- runoff.
Why Organic Matter Matters
Organic matter can increase:
- coagulant demand;
- chlorine demand;
- color;
- disinfection byproduct precursor load.
Water Quality and Treatment Demand
Changes in raw-water quality frequently change treatment requirements.
For example:
- higher turbidity may require more coagulation effort;
- higher organic matter may increase coagulant and disinfectant demand;
- lower alkalinity may make pH less stable;
- higher iron or manganese may increase oxidation and filtration demand.
Source Water Versus Process Water
When treatment performance changes, compare raw-water data with process data.
If raw water changed first, the treatment process may simply be responding to a new load.
Finished Water Versus Raw Water
Comparing source and finished water helps determine how effectively treatment is changing key parameters.
Trend Relationships
Useful relationships include:
- raw turbidity versus coagulant dose;
- raw organic matter versus chlorine demand;
- temperature versus chemical demand;
- finished-water pH versus corrosion-control feed;
- distribution residual versus water age.
Baseline Conditions
A baseline describes normal water-quality behavior under typical conditions.
Baselines should account for:
- season;
- source;
- flow;
- normal treatment configuration.
One Number Is Not a Trend
An isolated result may reflect:
- temporary change;
- sampling error;
- instrument error;
- real process change.
Operators should compare the result with related data.
Rate of Change Matters
A parameter moving gradually over several days may suggest a different cause than the same parameter changing sharply within minutes.
Example: Gradual Conductivity Increase
Possible explanations include:
- changing source blend;
- seasonal groundwater influence;
- increasing road-salt impact.
Example: Sudden Conductivity Increase
Possible explanations include:
- source switch;
- chemical release;
- instrument problem.
Example: Raw Turbidity Rises but Finished Turbidity Remains Stable
This suggests treatment is successfully handling the increased source-water particle load.
Example: Raw Turbidity Stable but Filter Turbidity Rises
This points more strongly toward a treatment-process or filter problem.
Example: Finished-Water pH Changes
Review:
- raw-water pH;
- alkalinity;
- chemical-feed rate;
- chemical strength;
- pH instrument calibration.
Example: Chlorine Residual Falls
Review:
- chlorine dose;
- flow;
- organic matter;
- ammonia where relevant;
- water age;
- analyzer condition.
Sampling Location
A sample is meaningful only if the operator understands what the location represents.
Examples include:
- raw source;
- post-coagulation;
- filter effluent;
- clearwell;
- distribution-system endpoint.
Representative Sampling
A representative sample should reflect the actual water or process being evaluated.
Problems can result from:
- stagnant sample lines;
- incorrect sample point;
- contaminated container;
- poor flushing.
Instrument Calibration
Reliable water-quality interpretation requires reliable instruments.
Operators should follow appropriate procedures for:
- calibration;
- verification;
- cleaning;
- maintenance.
Bad Instrument Data Can Cause Bad Process Changes
An incorrect analyzer can cause an operator or automatic control system to change treatment unnecessarily.
Cross-Check Important Results
When a result is unexpected, compare it with:
- a second instrument;
- laboratory analysis;
- another sampling location;
- related process variables.
Correlations Are Useful but Not Proof
If two parameters change together, the relationship can help identify a cause, but correlation alone does not prove causation.
Water Quality and Consumer Complaints
Customer complaints can provide clues about:
- color;
- odor;
- taste;
- sediment;
- localized distribution-system conditions.
Complaint Location Matters
A complaint from one building may indicate a local premise-plumbing problem.
Similar complaints across a large area may indicate a broader system condition.
Water Age
Water age can affect:
- disinfectant residual;
- taste and odor;
- biological activity;
- corrosion;
- disinfection byproducts.
Storage and Water Quality
Poor tank turnover can create:
- high water age;
- low disinfectant residual;
- temperature increase;
- sediment problems.
Distribution Disturbances
Main breaks, valve operation, hydrant use, and flow reversals can disturb deposits and create temporary:
- turbidity;
- color;
- iron or manganese particles.
Look for Patterns, Not Just Limits
Operators should understand both:
- whether a value is acceptable;
- whether the trend is moving in an unfavorable direction.
Operational Limits Versus Regulatory Limits
An operational target can be tighter than a regulatory requirement because operators need time to respond before treatment performance becomes unacceptable.
Common Water-Quality Interpretation Mistakes
- Relying on one measurement.
- Ignoring sample location.
- Ignoring seasonal source changes.
- Confusing pH with alkalinity.
- Assuming clear water is microbiologically safe.
- Using conductivity to identify a specific contaminant.
- Ignoring instrument calibration.
- Changing chemical feed before verifying unexpected data.
- Ignoring relationships among related parameters.
- Looking only at total chemical use without considering flow or source quality.
A Practical Raw-Water Quality Review
- Confirm the active source or source blend.
- Review temperature and turbidity.
- Review pH and alkalinity.
- Review conductivity.
- Review organic-matter indicators where available.
- Review iron and manganese where relevant.
- Compare with recent weather and source conditions.
- Compare with historical seasonal trends.
A Practical Treatment-Performance Review
- Compare raw-water and finished-water conditions.
- Review chemical feed rates.
- Review coagulation and clarification performance.
- Review filter performance.
- Review disinfectant residual.
- Verify instruments and sample locations.
- Identify whether the change began upstream or within treatment.
A Practical Unexpected-Result Review
- Verify the sample location.
- Repeat or confirm the measurement.
- Check instrument calibration.
- Compare related parameters.
- Review source-water conditions.
- Review recent process changes.
- Review historical trend.
- Take corrective action based on the confirmed cause.
What to Remember for the Exam
- Water quality includes physical, chemical, and biological characteristics.
- No single parameter describes overall water quality.
- Temperature affects chemical reactions, biological activity, settling, and disinfection.
- Turbidity measures light scattering caused by suspended or colloidal material.
- High turbidity can interfere with particle removal and disinfection.
- pH describes acid-base condition, while alkalinity describes acid-neutralizing capacity.
- Hardness is mainly associated with calcium and magnesium.
- Conductivity increases with dissolved ionic material but does not identify the specific dissolved chemical.
- Color, taste, and odor can provide important operational clues.
- Iron and manganese can produce staining, particles, and deposits.
- Dissolved oxygen affects biological processes and oxidation-reduction conditions.
- Microbiological safety cannot be judged by appearance alone.
- Natural organic matter can increase coagulant and disinfectant demand.
- Source-water changes can change treatment requirements even when plant flow remains constant.
- Trend data are usually more useful than isolated measurements.
- Sampling location must be considered when interpreting a result.
- Instrument calibration and QA/QC are essential to reliable water-quality decisions.
- Raw-water and process data should be compared to distinguish source changes from treatment problems.
- Operational trends can provide warning before a serious treatment problem develops.
- Good water-quality interpretation combines measurements, source conditions, treatment data, sampling quality, and historical trends.