Water is vital for life, animals, and the environment.
Maintaining water quality is essential for various purposes like human consumption and industrial use.
Determining water quality requires more than just visual inspection.
Water quality parameters are grouped into three types:
Chemical
Physical
Biological
Basic chemical characteristics include:
pH
Dissolved Oxygen (DO)
Hardness
Nitrates
Phosphates
pH represents the acidity or alkalinity (basicity) of water.
The pH scale ranges from 0 to 14.
pH < 7: Acidic
pH > 7: Basic (alkaline)
pH = 7: Neutral (pure distilled water)
pH is related to the balance between hydrogen ions (H+) and hydroxide ions (OH-).
More H+ than OH-: Acidic
More OH- than H+: Basic (alkaline)
Equal H+ and OH-: Neutral
The pH scale is logarithmic; a one-step change implies a tenfold change in H+ concentration.
Example: Water with a pH of 4 is ten times more acidic than water with a pH of 5.
Aquatic organisms may be harmed by water with a pH of less than 4.8 or greater than 9.2.
Most freshwater fish prefer a pH of 6.5 to 8.4.
WHO standards for drinking water: 6.5 to 8.5.
DO is the amount of free oxygen (O2) dissolved in water.
It's critical for aquatic plants and animals.
Measured using a dissolved oxygen meter or DO meter (optical or electrochemical sensor).
Ways oxygen gets into water:
Wind blowing over water surfaces
Aquatic plants and algae during photosynthesis
Water movement (splashing waves)
Rivers and streams typically have higher DO concentrations than lakes due to faster aeration.
Oxygen's solubility in water is poor.
DO is affected by:
Temperature: Cold water holds more DO than warm water.
At 4 °C, pure water can hold about y13.2 ppm DO at 100 percent saturation.
4
{}^
{o}C = 13.2 ppm
At 25 °C, pure water can hold about 8.4 ppm at 100 percent saturation.
25
{}^
{o}C = 8.4 ppm
Salinity: Waters with high salt concentrations retain less DO than pure water.
Impacts of DO concentration (ppm = parts per million):
5-6 ppm: Sufficient for most aquatic species
< 3 ppm: Stressful to most aquatic species
< 2 ppm: Fatal to most species
Terms:
Hypoxia: Low dissolved oxygen levels in water (from 2 ppm down to 0.5 ppm)
Anoxia: Absence of oxygen; dissolved oxygen levels in water below 0.5 ppm
Phosphates (PO4 3-) are naturally occurring forms of phosphorus (P) in rivers, but usually in small quantities.
Lower phosphate levels are generally better.
Total phosphates include organic (part of living plants and animals) and inorganic phosphates (ions bonded to soil particles and phosphates present in laundry detergents).
ppm (parts per million) is used to express small concentrations of dissolved substances:
1 ppm = 1 \frac{mg}{L}
ppb (parts per billion) is an even smaller concentration:
1 ppb = 1 \frac{\mu g}{L}
Phosphates are required nutrients for plant growth.
Excess can cause eutrophication (excessive plant and algae growth), decreasing water transparency.
When plants and algae die, aerobic bacteria consume DO, potentially causing death to fish and other aquatic organisms.
Excess phosphates in water may come from erosion, agricultural, storm water, residential, and industrial runoff.
Phosphate Level Limits:
River draining into a natural lake: 0.05 ppm
Natural lake: 0.025 ppm
River that is not flowing into a lake: 0.1 ppm
Nitrates (NO3 –) are naturally occurring forms of nitrogen and are more abundant than phosphates.
Like phosphates, excess nitrates can cause algal bloom and reduce water transparency.
The nitrogen cycle balances nitrate levels naturally.
Excess nitrates come from agricultural and industrial runoff.
Philippine National Standards for Drinking Water (PNSDW) of 2017 limits nitrate concentration to 50 ppm for drinking water.
High nitrate concentrations may cause methemoglobinemia (blue baby syndrome) in bottle-fed infants.
Water hardness measures the concentration of dissolved minerals like calcium, magnesium, strontium, iron, and manganese.
Water containing these minerals is referred to as “hard” because it requires more soap/detergent to create a lather.
Hard water is usually alkaline or basic.
Total hardness is represented as ppm of calcium carbonate (CaCO3).
Hardness Level as a measure of CaCO3 concentrations:
Soft: 0 – 60 ppm
Moderately Hard: 60 – 120 ppm
Hard: 120 – 180 ppm
Very Hard: Greater than 180 ppm
TDS indicates the amount of material dissolved in water.
These materials are often inorganic solids with a small amount of organic content, both natural and anthropogenic.
The PNSDW limit for TDS in drinking water is 300 ppm.
High TDS levels can cause undesirable tastes and laxative effects, making water unsuitable for aquatic life and crop irrigation.
Physical characteristics of water include:
Temperature
Color
Taste and Odor
Turbidity
Solids
Water temperature affects:
Rates of biological processes (metabolic rates of aquatic organisms, sensitivity to pollution, parasites, and diseases)
Chemical processes (rate of photosynthesis, gas solubility)
Increase in water temperature can:
Reduce dissolved oxygen capacity.
Promote biological activities.
Increase the activity of cellular enzymes, increasing metabolic functions in most aquatic organisms.
Increase photosynthetic activity in most algae.
Changes in water temperature are influenced by:
Changes in season and weather
Industrial discharge
Removal of shading vegetation
Groundwater influx
Turbidity represents the amount of light scattered in water due to suspended particles.
It determines how far light can travel through the water.
Suspended particles include clay, silt, fine organic and inorganic substances, soluble colored organic compounds, planktons, and other microorganisms.
A sudden increase in turbidity may be caused by runoff from land.
Relative turbidity can be measured using a Secchi disk.
Low turbidity: the disk is visible far below the surface.
Accurate measurement is done using a turbidimeter (nephelometer) and is expressed in nephelometric turbidity units (NTUs).
The PNSDW maximum allowable level of turbidity for drinking water is 5.0 NTU.
Conductivity is the ability of water to conduct electricity.
It is connected to the concentration of dissolved solids: the more dissolved solids, the more ions present, which means the more electrical current can be conducted.
Measured using a conductivity meter and is expressed in microsiemens per centimeter (µS/cm).
The target water quality range is 0 to 70 µS/cm.
Pure water is colorless.
The presence of color indicates suspended particles and organic matter.
Color can be reported as:
Apparent color: Color of the whole water sample (dissolved and suspended components).
True color: Measured after filtering the water sample to remove all suspended material.
Color is graded on a scale of 0 (clear) to 70 color units.
Pure water has 0 color units.
Possible Water Colors and Their Cause:
Blue: transparent; low level of accumulated dissolved materials; low rate of productivity
Yellow/brown: significant amount of dissolved organic materials, humic substance from soil, peat, or decaying plant material
Red: certain algae
Green: presence of phytoplankton and other algae
Mixture of colors: soil runoff
Pure water has no taste, but substances like zinc or foaming agents can give it a taste.
Chemical Component and Their Corresponding Taste:
Chloride, sulfate: salty taste
Copper, iron, zinc: metallic taste
Foaming agent: bitter taste
Manganese: bitter metallic taste
Pure water is odorless.
Dissolved substances influence the odor.
Decayed organic substances: fouling smell
Inorganic substances: earthy smell
Biological parameters are the organisms found in water such as fecal coliform bacteria.
Most bacteria are useful, but some are harmful, causing diseases.
Coliforms and fecal streptococci are used to test for disease-causing microorganisms.
They are called “fecal” indicators because they live in the intestinal tract of humans and other warm-blooded animals.
Fecal coliform bacteria are not harmful themselves, but their presence indicates the water might contain harmful microorganisms.
Large amounts of fecal coliform bacteria can give water a murky appearance, bad smell, and lowers DO level.
Sources of fecal coliform bacteria include wastewater treatment plants, domestic and wild animal manure, and storm runoff.
The USEPA standard for drinking water is 0 coliform per 100 mL (0 col./100 mL) of water.
Water quality assessment involves checking physical, chemical, and biological parameters against regulatory standards.
It is important to maintain water quality for various uses.
pH: Acidity or alkalinity of water.
Dissolved oxygen (DO): Amount of free oxygen (O2) in water.
Total phosphates (PO43–): Total amount of phosphates in water.
Nitrates (NO3 –): Total amount of nitrates in water.
Hardness: Concentration of dissolved minerals in water.
Total dissolved solids: Total amount of materials contained in water.
Temperature: How hot or cold the water is.
Turbidity: Cloudiness or murkiness of water.
Conductivity: Ability of water to conduct electrical current.
Color: Indicates the presence of suspended particles and dissolved matter.
Odor: Indicates the presence of organic and inorganic substances.
Fecal coliform bacteria: Indicates the presence of pathogens in water.