Water Quality Analysis

  Physical, Chemical and Biological Analysis


Physical parameters : Colour, Temperature, Transparency, Turbidity and Odour

Chemical parameters: pH, Electrical Conductivity (EC), Total Solids (TS), Total Dissolved Solids (TDS), Total Suspended Solids (TSS), Total Hardness, Calcium Hardness, Magnesium Hardness, Nitrates, Phosphates, Sulphates, Chlorides, Dissolved Oxygen (D.O), Biological Oxygen Demand (BOD), Chemical Oxygen Demand (COD), Fluorides, Free Carbon-di-oxide, Potassium and Sodium

Heavy metals: Lead, Copper, Nickel, Iron, Chromium, Cadmium and Zinc

Biological parameters: The biological parameters involved the qualitative analyses of planktons (zooplankton and phytoplankton).

Field measurement: The field parameters measured include pH, conductivity, dissolved oxygen, temperature and transparency

  Physical Parameters


Colour

In natural water, colour is due to the presence of humic acids, fulvic acids, metallic ions, suspended matter, plankton, weeds and industrial effluents

Visual comparison: take about 20ml of the sample and 20ml of distilled water in two separate wide mouthed test tubes. The results are tabulated (as clear, greenish, greyish, brownish, blackish, etc) by comparing the colour of the sample with distilled water

Temperature

Impinging solar radiation and atmospheric temperature brings about spatial and temporal changes in temperature, setting up convection currents and thermal stratification. Temperature plays a very important role in wetland dynamism affecting the various parameters such as alkalinity, salinity, dissolved oxygen, electrical conductivity etc. In an aquatic system, these parameters affect the chemical and biological reactions such as solubility of oxygen, carbon-di-oxide-carbonate-bicarbonate equilibrium, increase in metabolic rate and physiological reactions of organisms, etc. Water temperature is important in relation to fish life. The temperature of drinking water has an influence on its taste 

Apparatus required: Thermometer

Procedure: Temperature measurement is made by taking a portion of the water sample (about 1litre) and immersing the thermometer into it for a sufficient period of time (till the reading stabilizes) and the reading is taken, expressed as °C

Transparency (Light Penetration)

Solar radiation is the major source of light energy in an aquatic system, governing the primary productivity. Transparency is a characteristic of water that varies with the combined effect of colour and turbidity. It measures the light penetrating through the water body and is determined using Secchi disc

Apparatus required: Secchi disc, a metallic disc of 20cm diameter with four quadrats of alternate black and white on the upper surface. The disc with centrally placed weight at the lower surface, is suspended with a graduated cord at the center

Procedure: Transparency is measured by gradually lowering the Secchi disc at respective sampling points. The depth at which it disappears in the water (X1) and reappears (X2) is noted. The transparency of the water body is computed as follows:

                          Transparency (Secchi Disc Transparency) =  (X1 + X2 )/2

                                

Turbidity

Turbidity is an expression of optical property; wherein light is scattered by suspended particles present in water (Tyndall effect) and is measured using a nephelometer. Suspended and colloidal matter such as clay, silt, finely divided organic and inorganic matter; plankton and other microscopic organisms cause turbidity in water. Turbidity affects light scattering, absorption properties and aesthetic appearance in a water body. Increase in the intensity of scattered light results in higher values of turbidity

Apparatus required: Nephelometer

Principle: Nephelometric measurement is based on comparison of the intensity of scattered light of the sample with the intensity of light scattered by a standard reference suspension (Formazin polymer) under similar conditions. Turbidity is measures in unit NTU.

Procedure: The nephelometer is calibrated using distilled water (Zero NTU) and a standard turbidity suspension of 40NTU. The thoroughly shaken sample is taken in the nephelometric tube and the value is recorded

                Turbidity (NTU) = (Nephelometer readings) (Dilution factor*)

* If the turbidity of the sample is more than 40 NTU, then the sample is diluted and the dilution factor is accounted in final calculations

Turbidity can also be measured by Jackson Turbidity Meter. It is a visual method, where a flame of candle is seen till its view is obscured by the turbidity of water. 

 

  Chemical Parameters : pH


pH:

The effect of pH on the chemical and biological properties of liquids makes its determination very important. It is one of the most important parameter in water chemistry and is defined as -log [H+], and measured as intensity of acidity or alkalinity on a scale ranging from 0-14. If free H+ are more it is expressed acidic (i.e. pH<7), while more OH- ions is expressed as alkaline (i.e. pH> 7).

In natural waters pH is governed by the equilibrium between carbon dioxide/bicarbonate/carbonate ions and ranges between 4.5 and 8.5 although mostly basic. It tends to increase during day largely due to the photosynthetic activity (consumption of carbon-di-oxide) and decreases during night due to respiratory activity. Waste water and polluted natural waters have pH values lower or higher than 7 based on the nature of the pollutant. The parameter need to checked in field to avoid any changes.

 

Colorimetric method

Electrometric method

  Solids in Water


Total Solids (TS)

Total solids is the term applied to the material residue left in the vessel after evaporation of the sample and its subsequent drying in an oven at a temperature of 103-105 degree C.

Total solids include Total Suspended Solids (TSS) and Total Dissolved Solids (TDS)

Principle: A known volume (50 ml) of well-mixed sample is evaporated in a pre-weighed dish and dried to constant weight in an oven at 103-105C. The increase in weight over that of the empty dish gives the total solids

Total Dissolved Solids (TDS)

Dissolved solids are solids that are in dissolved state in solution. Waters with high dissolved solids generally are of inferior palatability and may induce an unfavourable physiological reaction in the transient consumer

Principle: The difference in the weight of total solids and the total suspended solids expressed in the same units gives the total dissolved solids.

Total Suspended Solids (TSS)

Suspended solids are the portions of solids that are retained on a filter of standard specified size (generally 2.0 µ) under specific conditions. Water with high-suspended solids is unsatisfactory for bathing, industrial and other purposes

Principle: A well – mixed sample is filtered through a weighed standard glass fibre filter and the residue that is retained on the filter is dried to a constant weight at 103-105 C. The increase in the weight of the filter determines the total suspended solids. This is called Gravimetric Method, however these days Electronic Methods are also used for TDS. You might have seen your home RO service provider always bring a small electronic device to check and adjust TDS of water.

Calculation:                                          

 

Where; W1 and W2 are initial and final weight respectively.

  Nitrates


Nitrates are the most oxidized forms of nitrogen and the end product of the aerobic decomposition of organic nitrogenous matter. The significant sources of nitrates are chemical fertilizers from cultivated lands, drainage from livestock feeds, as well as domestic and industrial sources. Natural waters in their unpolluted state contain only minute quantities of nitrates.

The stimulation of plant growth by nitrates may result in eutrophication, especially due to algae. The subsequent death and decay of plants produces secondary pollution. Nitrates are most important for biological oxidation of nitrogenous organic matter. Certain nitrogen fixing bacteria and algae have the capacity to fix molecular nitrogen in nitrates. The main source of polluting nitrates is domestic sewage. Nitrates may find their way into ground water through leaching from soil and at times by contamination. They can be measured by the phenoldisulphonic method.

Principle: Nitrates react with phenoldisulphonic acid and produce a nitrate derivative, which in alkaline solution develops yellow colour due to rearrangement of its structure. The colour produced is directly proportional to the concentration of nitrates present in the sample.Instrument used is Spectrophotometer.

Calculation:

The high concentration of nitrate in water is indicative of pollution.

  Phosphates


Phosphates occur in natural or wastewaters as orthophosphates, condensed phosphates and naturally found phosphates. Their presence in water is due to detergents, used boiler waters, fertilizers and biological processes. They occur in solution in particles or as detritus. They are essential for the growth of organisms and a nutrient that limits the primary productivity of the water body. Inorganic phosphorus plays a dynamic role in aquatic ecosystems; when present in low concentration is one of the most important nutrients, but in excess along with nitrates and potassium, causes algal blooms.

Principle: In acidic conditions orthophosphate reacts with ammonium molybdate forming Molybdophosphoric acid, reduced further to molybdenum blue by stannous chloride. The intensity of the blue colour is directly proportional to the concentration of phosphate. The absorbance is noted at 690nm using spectrophotometer. It is calculated by the stannous chloride method

Calculation:

High phosphorus content causes increased algal growth till nitrogen becomes limiting, although blue green algae continues to dominate because of its ability to utilize molecular nitrogen. Besides sedimentation, high uptake by phytoplankton is one of the reasons for fast depletion of phosphorus in water.

  Sulphates


Sulphates are found appreciably in all natural waters, particularly those with high salt content. Besides industrial pollution and domestic sewage, biological oxidation of reduced sulphur species also add to sulphate content. Soluble in water, it imparts hardness with other cations. Sulphate causes scaling in industrial water supplies, and odour and corrosion problems due to its reduction to hydrogen sulphide.

Principle: Sulphate ions are precipitated in acetic acid medium with barium chloride to form barium sulphate crystals of uniform size. The scattering of light by the precipitated suspension (barium sulphate) is measured by a Nephelometer and the concentration is recorded.It is measured by turbidometric method

Calculation:

 

  Chlorides


The presence of chlorides in natural waters can mainly be attributed to dissolution of salt deposits in the form of ions (Cl-). Otherwise, high concentrations may indicate pollution by sewage, industrial wastes, intrusion of seawater or other saline water. It is the major form of inorganic anions in water for aquatic life. High chloride content has a deleterious effect on metallic pipes and structures, as well as agricultural plants.

Principle: In alkaline or neutral solution, potassium chromate indicates the endpoint of the silver nitrate titration of chlorides. Silver chloride is quantitatively precipitated before the red silver chromate is formed. They are calculated by Argentometric method 

  Dissolved Oxygen (DO)


Oxygen dissolved in water is a very important parameter in water analysis as it serves as an indicator of the physical, chemical and biological activities of the water body. The two main sources of dissolved oxygen are diffusion of oxygen from the air and photosynthetic activity. Diffusion of oxygen from the air into water depends on the solubility of oxygen, and is influenced by many other factors like water movement, temperature, salinity, etc. Photosynthesis, a biological phenomenon carried out by the autotrophs, depends on the plankton population, light condition, gases, etc. Oxygen is considered to be the major limiting factor in water bodies with organic materials. It is one of the most important parameter and is also required for testing BOD so discussed in details.

Measurement:

Either electronically by Membrane electrode method or by titration through Winkler’s Iodometric method.

Principle: Oxygen present in the sample oxidizes the dispersed divalent manganous hydroxide to the higher valency to precipitate as a brown hydrated oxide after addition of potassium iodide and sodium hydroxide. Upon acidification, manganese reverts to its divalent state and liberates iodine from potassium iodide, equivalent to the original dissolved oxygen content of the sample. The liberated iodine is titrated against N/80 sodium thiosulphate using fresh iodine as an indicator

Reagents: Manganese sulphate, Alkaline iodide-azide reagent, Conc. sulphuric acid, Starch indicator, Stock sodium thiosulphate

Procedure: Take BOD Bottles add 2ml of manganous sulphate and 2ml of potassium iodide This is mixed well and the precipitate allowed to settle down. At this stage 2ml of conc. sulphuric acid is added, and mixed well until all the precipitate dissolves. 203ml of the sample is measured into the conical flask and titrated against 0.025N sodium thiosulphate using starch as an indicator. The end point is the change of colour from blue to colourless

Calculations:

                           

where:
V = mL thiosulphate solution used
M = molarity of thiosulphate titrant

 203ml because (200) (300)/ (300-4=296) = 203ml (202.7ml)

 

  Biological Oxygen Demand (BOD)


Biological Oxygen Demand (BOD) is the amount of oxygen required by microorganisms for stabilizing biologically decomposable organic matter (carbonaceous) in water under aerobic conditions. The test is used to determine the pollution load of wastewater, the degree of pollution and the efficiency of wastewater treatment methods. 5-Day BOD test being a bioassay procedure (involving measurement of oxygen consumed by bacteria for degrading the organic matter under aerobic conditions) requires the addition of nutrients and maintaining the standard conditions of pH and temperature and absence of microbial growth inhibiting substances.

Principle: The method consists of filling the samples in airtight bottles of specified size and incubating them at specified temperature 20 degree C for 5 days or else 27 degree for 3 days. The difference in the dissolved oxygen measured initially and after incubation gives the BOD of the sample.

Reagents: all are same as that for DO but need to prepare dilution water in BOD testing.

Preparation of dilution water: To 1000ml of water, 1ml each of phosphate buffer, magnesium sulphate, calcium chloride and ferric chloride solution is added, before bringing it to 20 C and aerating it thoroughly. 

Procedure: The sample having a pH of 7 is determined for first day DO. Various dilutions (at least 3) are prepared to obtain about 50% depletion of D.O. using sample and dilution water. The samples are incubated at 20 C for 5 days and the 5th day D.O is noted using the oximeter. A reagent blank is also prepared in a similar manner.

Calculation:

Where;

  • D initial - 1st day D.O of diluted sample
  • Dfinal  - 5th day D.O of diluted sample
  • p – Dilution
  • p = Vol of ww/ vol of DO bottle

Types of BOD

  • Aerobic decomposition : CO2, Orthophosphate, Sulfate, Nitrate
  • Anaerobic Decomposition : H2S, NH3, CH4 Swamp Gas

BOD in two parts

CBOD – Carbonaceous (OC to CO2); NBOD – Nitrogenous (Ammonia to Nitrate)(ON to Amm to Nitrite to Nitrate) – does not exert till 5-8 days

Ultimate BOD (UBOD)= 4.57 X TKN

5 Day BOD

Total amount of oxygen consumed by microorganism in initial 5 days;No light – keep algae away which can add O2 by photosynthesis and air tight;DO should be above zero at the end of experiment. Seeding to provide sufficient microorganism. In this case it is necessary to subtract OD caused by seed from mixed sample OD (one seeded dilution water other with sample)

where:

      D1 =  DO of diluted sample immediately after preparation, mg/L,
      D2=  DO of diluted sample after 5 d incubation at 20°C, mg/L,
      P=  decimal volumetric fraction of sample used,
      B1=  DO of seed control before incubation, mg/L,
      B2=  DO of seed control after incubation mg/L, and

f =  ratio of seed in diluted sample to seed in seed control = (% seed in diluted sample)/(% seed in seed control).
If seed material is added directly to sample or to seed control bottles: f = (volume of seed in diluted sample)/(volume of seed in seed control)

 

  Potassium and Sodium


Potassium

Potassium ranks seventh among the elements in order of abundance, behaves similar to sodium and remains low. Though found in small quantities (<20mg/L) it plays a vital role in the metabolism.

Principle: Trace amount of potassium can be determined by direct reading of flame photometer at a specific wavelength of 766.5nm by spraying the sample into the flame. The desired spectral lines are then isolated by the use of interference filters or suitable slit arrangements. The intensity of light is measured by the phototube.

Working principle of Flame photometer: The emission of characteristic radiations by alkali and alkaline earth metals and the correlation of the emission intensity with the concentration of the element form the basis of flame photometry. The principle of the flame photometer depends on the "Emission Spectroscopy" in which the electrons of the metals after absorbing energy get excited from ground state to higher energy level and return back to the ground state with emission of light. The sample under test is introduced into flame in solution by means of atomizer. The radiation from the flame enters a dispersing device and isolates it (radiation) from the flame to the desired region of the spectrum. The phototube measures the intensity of isolated radiation, which is proportional to the concentration of the element present in the sample. 

Sodium

Sodium is one of the most abundant elements and is a common constituent of natural waters. The sodium concentration of water is of concern primarily when considering their solubility for agricultural uses or boiler feed water. The concentration ranges from very low in the surface waters and relatively high in deep ground waters and highest in the marine waters. It is calculated by flame photometric method.

Prev  

Top