Results

Date

S1

S2

S3

Limits (Inland)

Permissible
750-2000

Excessive
>2000

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

 TOTAL DISSOLVED SOLIDS (TDS)

4

TDS : The substances that would pass through the filter paper but will remain as residue when the water evaporates which includes dissolved minerals and salts, humic, tannin and pyrogens. A constant level of minerals in the water is necessary for aquatic life. Changes in the amounts of dissolved solids can be harmful because the density of total dissolved solids determines the flow of water in and out of an organism’s cells. Many of these dissolved solids contain chemicals, such as nitrogen, phosphorous, and sulfur, which are the building blocks of molecules for life. Concentration of total dissolved solids that are too high or too low may limit the growth and may lead to the death of many aquatic organisms. High concentrations of total dissolved solids may reduce water clarity, which contributes to a decrease in photosynthesis and lead to an increase in water temperature. Many aquatic organisms cannot survive in high temperatures. The conductivity in water is affected by the presence of inorganic dissolved solids such as chloride, nitrate, sulfate, and phosphate anions or sodium, magnesium, calcium, iron, and aluminum cations. These particles contribute the dissolved solids of the water. Waters with high dissolved solids generally are of inferior palatability and may induce an unfavourable physiological reaction.

Procedure

Clean the pH-TDS-EC probe with distilled water and fill the container with water sample. Then the total dissolved solids is determined by dipping the pH-TDS-EC probe into sample and express in parts per million (ppm).

Apparatus: pH-TDS-EC probe, 100ml Beaker

Do’s and Dont’s:

• Clean the meters with distilled water and wipe properly using tissue paper, before and after usage.
• Calibrate the meters prior to each field trip.
• Ensure that all the instructions on use, maintenance and storage of the pH-TDS-EC probe has been followed.
• Note down the TDS readings of each sample.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
500

Excessive
1500

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

TRANSPARENCY (LIGHT PENETRATION)

5

TRANSPARENCY: 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.

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                               
Where, X1 = Depth at which Secchi disc disappears
X2 = Depth at which Secchi disc reappears

Apparatus: 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.

Do’s and Dont’s:

• Clean the secchi disc before and after usage.
• Handle the secchi disc with care.
• Note down the readings of each sample.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible

Excessive

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

6

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. Any substance having a particle size more than 10‑9 will produce turbidity in water. 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 appearance in a water body. Increase in the intensity of scattered light results in higher values of turbidity. Turbidity makes the water unfit for domestic purposes, food and beverage industries, and many other industrial purposes. In natural waters, turbidity restricts light penetration for photosynthesis.
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.

Procedure: The nephelometer is calibrated using distilled water (Zero NTU) and a standard turbidity suspension of 40 NTU. 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.

Apparatus:Nephelometer (It detects scattered light at 90o to the incident beam of light. It consists of a light source for illuminating the sample. One or more photoelectric detectors with a display unit indicate the intensity of light scattered at 90o to the path of incident light.), sample cells, lab-glass wares.

Do’s and Dont’s:

• Collect the sample directly into the sampling cuvet (cell).
• Do not leave the sample cell in the meter so as to avoid scratches.
• Empty the sample at each site and rinse properly.
• Note down the Turbidity readings of each sample.
• Wipe the cell properly with tissue paper and ensure that the outside of the cell is clean and dry before placing the cell in to the meter.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
5 NTU
Excessive
25 NTU

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

DISSOLVED OXYGEN (DO)

7

DISSOLVED OXYGEN: Oxygen is essential to all forms of aquatic life. DO depend upon the physical, chemical and biochemical activities in the water body. The analysis of DO is a key test in water pollution and waste treatment control. The two main sources of dissolved oxygen are diffusion of oxygen from the air and photosynthetic activity. Low levels of DO frequently indicate a high concentration of decaying organic matter in the water. As bacteria digest organic matter, they use up oxygen, leaving little for the other aquatic creatures. The factors affecting the DO are (1) temperature: as temperature increases, the amount of oxygen (or any gas) dissolved in water decreases. (2) Partial pressure of O2 in contact with water: at high altitudes, less oxygen is dissolved in water because the partial pressure of oxygen in the atmospheric is low (3) Salinity: the solubility of gases O2 and CO2 decreases with increasing salinity.

Winkler’s 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.

Calculation:  NIVI = N2V2 (Molar equivalence formula)

                                                 (ml*N) of sodium thiosulphate * 8 * 1000
Dissolved oxygen, mg/L =
V2 [(V1 - V)/V1]

Where,     V1 = Volume of sample bottle
V2 = Volume of contents titrated
V = Volume of MnSO4 and KI added (2ml)

Procedure

The samples are collected in BOD bottles, to which 1ml of manganous sulphate and 1ml of potassium iodide are added and sealed. This is mixed well and the precipitate is allowed to settle down. Then, 1ml of concentrated sulphuric acid is added, and mixed well until all the precipitate dissolves. 25 ml 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.

Apparatus: BOD bottle-125ml, measuring cylinder, conical flask, 1ml glass pipette etc.

Reagents:

Manganous sulphate solution: Dissolved 100 g of manganous sulphate in 200ml of distilled water and heated to dissolve salt and filtered after cooling.

• Alkaline potassium iodide solution: Dissolved 100 g of KOH and 50 g of KI in 200ml of pre-boiled distilled water.
• Starch indicator:1g of starch is dissolved in 100 ml of warm distilled water and added few drops of formaldehyde solution.
• Stock sodium thiosulphate (0.1 N):24.82g of sodium thiosulphate pentahydrate (Na2S202. 5H2O) is dissolved in distilled water and made up to 1000ml.

• Standard sodium thiosulphate (0.025N): 250ml of the stock sodium thiosulphate pentahydrate is made up to 1000ml with distilled water to give 0.025N.

Do’s and Dont’s

• Label the BOD bottle with waterproof pen before collecting sample.
• Ensure that no air bubble enters the BOD bottle while filling it with water sample.
• Clean and different microtips should be used for each reagent.
• Handle the reagents and acids with extreme care. Wear disposable gloves if possible.
• Don’t keep the BOD under direct sunlight while doing experiment as it will interfere with the results.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
3

Excessive
6

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

FREE CARBON-DIOXIDE

10

FREE CARBON-DIOXIDE: The important source of free carbon-dioxide in surface water bodies is mainly respiration and decomposition by aquatic organisms. It reacts with water partly to form calcium bicarbonate and in the absence of bicarbonates gets converted to carbonates releasing carbon-dioxide.

Procedure

A known volume (25ml) of the sample was measured into a conical flask. 2-3 drops of phenolphthalein indicator was added and titrated against 0.22N sodium hydroxide till the pink colour persisted indicating the end point.
If the pink colour appears on adding phenolphthalein it indicates the absence of free carbon-dioxide.

Apparatus: Lab glassware - measuring cylinder, pipette, conical flask, etc.

Reagents:

• Sodium hydroxide solution (0.22N):1g of sodium hydroxide was dissolved    in 100ml of distilled water and made up to 1000ml to give 0.22N.
•  Phenolpthalein indicator: Dissolve 0.5 g of phenolphthalein in 50 ml of 95% ethanol and add 50 ml of distilled water. Add 0.05 N CO2 free NaOH solution dropwise, until the solution turns faintly pink.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.

• Handle the reagents and acids with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible

Excessive

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

ALKALINITY

11

ALKALINITY: In natural water, that are not highly polluted alkalinity is more commonly found than acidity. Alkalinity is the good indicator of presence of dissolved inorganic carbon (bicarbonates and carbonate anions). Some of the minor contributions to alkalinity come from ammonia, phosphates, borates, silicates and other basic substances.

Alkalinity is beneficial to aquatic animals and plants, because it buffers both the natural and human induced pH changes. Water with high alkalinity generally have a high concentration of dissolved inorganic carbon (in the form of HCO3- and CO32-), which can be converted to biomass by photosynthesis.
Titrating a basic water sample with acid to pH 8.3 measures phenolphthalein alkalinity. Phenolphthalein alkalinity primarily measures the amount of carbonate ion (CO32-) present in the sample. Titrating with acid to pH 3.7 measures methyl orange alkalinity or total alkalinity. Total alkalinity measures the neutralizing effects of all the bases present.
Calculate total phenolphthalein and methyl orange alkalinity as follows and express in mg/L as CaCO3,
A*1000
P Alkalinity m mg/L as CaCO3 =
ml sample

                                                              B*1000
T Alkalinity m mg/L as CaCO3 =
ml sample
Where,
A= ml of H2SO4 required to raise pH up to 8.3
B= ml of H2SO4 required to raise pH up to 4.5

Procedure

Measure a suitable volume of sample in 250 ml conical flask. Add 2-3 drops of phenolphthalein indicator. If the pink colour develops titrate against 0.02 N H2SO4, till the colour disappears, which is the characteristic of pH 8.3.Note down the volume of H2SO4 consumed. Add 2-3 drops of methyl orange and continue titration with H2SO4 till the yellow colour changes to orange, which is the characteristic of pH 4.5. Note down the additional amount of H2SO4 required. In case pink colour does not appear after addition of phenolphthalein, continue with addition of methyl orange.

Apparatus: Lab glassware - measuring cylinder, pipette, conical flask, etc.

Reagents

1. Standard sulphuric acid (0.02N):  Dilute 200 ml of 0.1N H2SO4 with distilled water to 1000ml to obtain standard 0.02N H2SO4.
2. Phenolphthalein indicator: Dissolve 0.5g phenolphthalein in 1:1 of 95 % ethanol and distilled water. Add 0.05 N CO2 free NaOH solution drop wise until faint pink colour appears.
3. Methyl orange indicator: Dissolve 0.5 g of methyl orange in 1000ml CO2 free distilled water.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.

• Handle the reagents and acids with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible

Excessive
500

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

TOTAL HARDNESS

12

TOTAL HARDNESS: Water hardness is the traditional measure of the capacity of water to react with soap, hard water requiring a considerable amount of soap to lather.Hardness is predominantly caused by divalent cations such as calcium, magnesium and alkaline earth metals such as iron, manganese, strontium, etc. The total hardness is defined as the sum of calcium and magnesium concentrations, both expressed as CaCO3 in mg/L. Carbonates and bicarbonates of calcium and magnesium cause temporary hardness. Sulphates and chlorides cause permanent hardness.
In alkaline conditions EDTA (Ethylene-diamine tetra acetic acid) and its sodium salts react with cations forming a soluble chelated complex when added to a solution. If a small amount of dye such as Eriochrome black-T is added to aqueous solution containing calcium and magnesium ions at alkaline pH of 10.0 ± 0.1, it forms wine red colour. When EDTA is added as a titrant, all the calcium and magnesium ions in the solution get complexed resulting in a sharp colour change from wine red to blue, marking the end point of the titration. Hardness of water prevents lather formation with soap rendering the water unsuitable for bathing and washing. It forms scales in boilers, making it unsuitable for industrial usage. At higher pH >12, Mg++ ion precipitates with only Ca++ in solution. At this pH, murexide indicator forms a pink color with Ca++ ion. When EDTA is added Ca++ gets complexed resulting in a change from pink to purple indicating end point of the reaction.
METAL + INDICATOR            METAL-INDICATOR COMPLEX (WINE RED COLOUR)

METAL-INDICATOR COMPLEX + EDTA                   METAL-EDTA COMPLEX  +
INDICATOR (BLUE COLOUR)
 Calculation:
Total hardness (mg/L)   =  (T) (1000) /  V
Where, T = Volume of titrant
V = Volume of sample
                              Hardness Chart (for drinking water):

Procedure

The complete titration should be completed within 5 minutes after addition of the buffer. Take 25 ml of the sample (dilute it with distilled water if required) and add 1-2 ml of the buffer solution and 1-2 g of EBT indicator. Then titrate against the EDTA, with continuous stirring; until the last reddish tinge disappears. At the end point the solution gives blue colour.

Apparatus: Lab glassware-burette, pipette, conical flask, beakers etc.

Reagents:

1. Buffer solution: (a) 16.9 g of ammonium chloride was dissolved in 143ml of concentrated ammonium hydroxide. (b) Dissolve 1.179 g of disodium EDTA and 0.780 g of MgSO4. 7H2O in 50 ml distilled water. Mix both (a) and (b) and dilute to 250ml with distilled water
2. Standard EDTA indicator: (0. 01 M) Weigh 3.723 g of EDTA and dissolve in 1000 ml of distilled water and standardize against standard calcium solution.
3. EBT Indicator: Mix 0.40 g of Eriochrome Black T with 100 g NaCl (AR) and grind.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.
• Don’t keep the reagent bottle open.
• Handle the reagents and acids with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
150

Excessive
500

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

CALCIUM HARDNESS

13

CALCIUM HARDNESS: The presence of calcium (fifth most abundant) in water results from passage through or over deposits of limestone, dolomite, gypsum and such other calcium bearing rocks. Calcium is present in all waters as Ca2+ and is readily dissolved from rocks rich in calcium minerals, particularly as carbonates and sulphates. Calcium carbonate solubility is controlled by pH and dissolved CO2. The salts of calcium, together with those of magnesium are responsible for hardness of water. Calcium is an important element for all organisms and is incorporated in to the shells of many aquatic invertebrates, as well as the bones of vertebrates. Calcium concentrations in natural waters are typically <15 mg/l. For water associated with carbonate rich rocks, concentrations may reach 30-100 mg/l. Salt waters have concentrations of several hundred milligrams per litre or more.
When EDTA (Ethylene-diamine tetra acetic acid) is added to the water containing calcium and magnesium, it combines first with calcium. Calcium can be determined directly with EDTA when pH is made sufficiently high such that the magnesium is largely precipitated as hydroxyl compound (by adding NaOH and iso-propyl alcohol). When murexide indicator is added to the solution containing calcium, all the calcium gets complexed by the EDTA at pH 12-13. The end point is indicated from a colour change from pink to purple.

Calculation

                                                            A*B*1000
Calcium hardness as CaCO3 =                                       * Dilution factor (If diluted)
ml of sample taken

Where, A = ml titrant for sample and B = mg Caco3 equivalent to 1.0 ml EDTA titrant.

Procedure

A known volume (25ml) of the sample is pipetted into a clean conical flask, to which 1ml of sodium hydroxide is added. A pinch of murexide indicator is added to this mixture and titrated against EDTA until the pink color turns purple.

Apparatus: Burettes, pipette, conical flask, beakers and droppers

Reagents:

• Sodium hydroxide (8%):8g of sodium hydroxide is dissolved in 100ml of distilled water.
• Murexide indicator (ammonium purpurate):0.2 g of murexide is ground well with 100g of sodium chloride.
• Standard EDTA titrant, 0.01M:3.723 g of EDTA (disodium salt) is dissolved in distilled water and made up to 100ml with the same.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.
• Don’t keep the reagent bottle open.
• Handle the reagents and acids with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
75

Excessive
200
*Calcium (as Ca) mg/l

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

MAGNESIUM HARDNESS

14

MAGNESIUM HARDNESS: Magnesium is a relatively abundant element in the earth's crust, ranking eighth in abundance among the elements. It is found in all natural waters and its source lies in rocks, generally present in lower concentration than calcium. It is also an important element contributing to hardness and a necessary constituent of chlorophyll. Its concentration greater than 125 mg/L can influence cathartic and diuretic actions.
Magnesium hardness can be calculated from the determined total hardness and calcium hardness.
Magnesium  =  (T - C) x 0.243 (as mg/L)
 where, T = Total hardness mg\L (as CaCO3)
C = Calcium hardness mg\L (as CaCO3)
 High concentration of magnesium proves to be diuretic and laxative, and reduces the utility of water for domestic use while a concentration above 500 mg/L imparts an unpleasant taste to water and renders it unfit for drinking. Chemical softening, reverse osmosis and electro dialysis or ion exchange reduces the magnesium hardness to acceptable levels.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
50

Excessive
150
*Magnesium  (as Mg) mg/l

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

17

 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.

Procedure

The filter of the flame photometer is set to 589nm (marked for Sodium, Na). By feeding distilled water the scale is set to zero and maximum using the standard of highest value. A standard curve between concentration and emission is prepared by feeding the standard solutions. The sample is filtered through filter paper and fed into the flame photometer and the concentration is found from graph or by direct readings.

Apparatus: Flame photometer, lab glassware and Whattman filter paper.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.
• Don’t keep the reagent bottle open.
• Handle the reagents and acids and gas of flame photometer with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible

Excessive

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

NITRATES

18

  NITRATES: Nitrate ion (NO3¯) is the common form of combined nitrogen found in natural waters. It may be bio chemically reduced to nitrite (NO2¯) by denitrification processes, usually under anaerobic conditions. The nitrite ion is rapidly oxidized to nitrate. Natural sources of nitrate to surface water include igneous rocks, domestic sewage, land drainage and plant growth and decay. The natural concentration of nitrate is 0.1mg/L; it may be enhanced by sewage, industrial effluents and nitrate fertilizers.

           
Ammonia and other nitrogenous material in natural waters tend to be oxidized by aerobic bacteria first to nitrite and then nitrates. So all organic compounds containing nitrogen are potential source of nitrates. It is first oxygenated to nitrite (NO2¯) and is rapidly oxidized to nitrate (NO3¯) so normally the amount of nitrite is very low. High concentrations (>1-2 mg/L) of nitrate or nitrite in surface or ground water generally indicate agricultural contamination from fertilizers and manure.

NITRIFICATION
(O)                               (R)
Ammonia                        Nitrite                           Nitrates
ADB                           FAB
           
ADB = Aerobic Denitrifying Bacteria.  Ex: Nitrosomes
FAB = Facultative Anaerobic Denitrifying Bacteria. Eg: Pseudomonas

Estimation of nitrates by electrode screening method

The NO3¯ ions electrode is a selective sensor that develops a potential across a thin, porous, inert membrane that holds in a place a water-immiscible liquid ion exchanger. The electrode responds only to NO3¯ ion activity between about 10¯5 and 10¯1 M (0.14 to 1400 mg NO3¯ -N/L). The lower limit of detection is determined by the small but finite solubility of the liquid ion exchanger.

Procedure

A known volume (50ml) of the sample is pipetted into a porcelain dish and evaporated to dryness on a hot water bath. 2ml of phenol disulphonic acid is added to dissolve the residue by constant stirring with a glass rod. Concentrated solution of sodium hydroxide or conc. ammonium hydroxide and distilled water is added with stirring to make it alkaline. This is filtered into a Nessler's tube and made up to 50ml with distilled water. The absorbance is read at 410nm using a spectrophotometer after the development of colour. The standard graph is plotted by taking concentration along X-axis and the spectrophotometric readings (absorbance) along Y-axis. The value of nitrate is found by comparing absorbance of sample with the standard curve and expressed in mg/L.

Apparatus: Porcelain dishes, pipettes, standard flasks, beakers, spectrophotometer, cuvettes, measuring jar and hot water bath.

Reagents:
 Phenol disulphonic acid:25 g of phenol is dissolved in 150 ml of concentrated sulphuric acid, to which 85ml of sulphuric acid is further added and heated for about 90 min on a water bath and stored in dark bottles upon cooling.
 Sodium hydroxide:About 50g of sodium hydroxide is dissolved in 150-200 ml of water and cooled.
  Conc. Ammonium hydroxide (Liquid ammonia)
Nitrate solution:

• Stock nitrate solution:721.8 mg (0.722g) of AR potassium nitrate is dissolved in distilled water and made up to 100ml for stock solution.
•  Standard nitrate solution:Standard nitrate solution is prepared by evaporating 50ml of the stock solution to dryness in the water bath. The obtained residue is dissolved in 2ml of phenol disulfonic acid and diluted to 500ml, to give 1ml = 10 mg. The solution of various strengths ranging from 0.0 (blank) to 1.0 mg/L at the intervals of 0.2 mg/L is prepared by diluting stock solution with distilled water.

Do’s and Dont’s

• Ensure that the Erlenmeyer flasks to be used are washed properly and labeled.
• Don’t keep the reagent bottle open.
• Handle the reagents and acids with extreme care.

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
45

Excessive

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

Results

Date

S1

S2

S3

Limits (Inland)

Permissible
2

Excessive
5

Inference

References

APHA (1998); Trivedi R. K. and Goel P. K. (1986); Ramachandra T. V. and Ahalya N. (2001)

BIOLOGICAL PARAMETERS

PLANKTON ANALYSIS: The physical and chemical characteristics of water affect the abundance, species composition, stability and productivity of the indigenous populations of aquatic organisms. The biological methods used for assessing water quality includes collection, counting and identification of aquatic organisms; biomass measurements; measurements of metabolic activity rates; toxicity tests; bioaccumulation; biomagnifications of pollutants; and processing and interpretation of biological data. The work involving plankton analysis would help in:

1. Explaining the cause of colour and turbidity and the presence of objectionable odour, tastes and visible particles in waters.
2. The interpretation of chemical analyses.
3. Identifying the nature, extent and biological effects of pollution.
4. Providing data on the status of an aquatic system on a regular basis.

Plankton:A microscopic community of plants (phytoplankton) and animals (zooplankton), found usually free floating, swimming with little or no resistance to water currents, suspended in water, non-motile or insufficiently motile to overcome transport by currents, are called "Plankton". 
Phytoplankton (microscopic algae) usually occurs as unicellular, colonial or filamentous forms and is mostly photosynthetic and is grazed upon by the zooplankton (microscopic protozoans, rotifers, cladocerans and copepods) and other organisms occurring in the same environment.

The structure of photosynthetic populations in the aquatic ecosystems is dynamic and constantly changing in species composition and biomass distribution. An understanding of the community structure is dependent on the ability to understand the temporal distribution of the different species. Changes in species composition and biomass may affect photosynthetic rates, assimilation efficiencies, rates of nutrient utilization, grazing, etc.
Plankton, particularly phytoplankton, has long been used as indicators of water quality. Because of their short life spans, planktons respond quickly to environmental changes. They flourish both in highly eutrophic waters while a few others are very sensitive to organic and/or chemical wastes. Some species have also been associated with noxious blooms causing toxic conditions apart from the tastes and odour problems.

Plankton net:The plankton net is a field-equipment used to trap plankton. It has a polyethylene filter of a defined mesh size and a graduated measuring jar attached to the other end. A handle holds the net. The mesh size of the net determines the size range of the plankton trapped. The mesh number 30 of size 60 mm was used for collecting samples.

Sampling Procedure:The manner in which sampling is done should conform to the objectives of the study. The “surface samples” (samples collected from the surface) are collected as close to the water surface as possible, mostly towards the center of the lake at regular monthly intervals. A known volume of the sample, 5L to 50 L is filtered and planktons are filtered and preserved for further analysis.

Labels:The sample label has the date, time of sampling, study area-lake name and the volume measured and pasted on the containers of 50 ml capacity.

Preservation:The samples are collected into 100 ml polyethylene vials and  are preserved by adding suitable amounts of 1ml chloroform to act as the narcotizing agent and 2 ml of 2% formalin for preservation and analyses.

Concentration technique: The plankton nets are used to collect samples for the qualitative and quantitative estimation of the plankton, by filtering a known volume of water (5-50 liters) through the net depending on the plankton density of the tanks. 

Qualitative and quantitative evaluation of plankton:Detailed analyses of phytoplankton populations are done by estimating the numbers in each species. The phytoplankton consisting of individual cells, filaments and colonies are counted as individual cells. When colonies of species are counted, the average number of cells per colony is counted, and in filamentous algae, the average length of the filament has to be determined.

Sedimentation and enumeration by microscope:Preserved samples in bottles are mixed uniformly by gentle inversion and then exactly 1ml of the sample is pipetted out into the S-C cell for analysis.

Microscope
Compound microscope: A monocular compound microscope is used in the counting of plankton with different eyepieces such as 4X, 10X and 40X. The microscope is calibrated using plankton-counting squares.

Counting

Counting cell- Sedgwick-Rafter (S-R) cell: The Sedgwick-Rafter cell is a devise used for plankton counting and is about 50mm long by 20mm wide and 1mm deep. The cell is covered by a relatively thick cover slip and is calibrated to contain exactly 1.0 ml. 

Method

Filling the cell:The cover slip is placed diagonally across the S-R cell and filled with the sample carefully without air bubbles with a large bore pipette. The sample is allowed to settle for about 5 minutes before the actual counting begins.

  Note: Since the configuration of the S-R cell does not allow the use of high power microscope objectives, the identification of organisms smaller than 10 – 15 mm is difficult or impossible, limiting the usage to only larger forms of relatively dense populations.

  Strip counting: A "strip" is the length of the cell that constitutes a volume approximately 50 mm long, 1-mm deep accounting to the volume of 25mm3 or 1/40 (2.5%) of the total cell volume. By moving the mechanical stage from left to right, the organisms can be examined in a systematic manner. By knowing the surface area of the portion counted in relation to that of the total, a factor is determined to expand the average counts of the plankton to the total area of the counting surface. This total area represents the number of organisms present per given volume of the sample. This volume expanded to an appropriate factor yields the organisms per litre of water for the lake.

  The total number of planktons in the S-R cell is obtained by multiplying actual count in the strip by the number (enumeration factor) representing the portion of the S-R cell counted. The number of the strips counted is a function of the precision desired and the number of units (cells, colonies) for the strips measured. In this study, 500 cells were counted for estimation. 

The plankton count in the S-R cell is got from the following,
C X 1000 mm            
Number/ml =      -------------------------
L X D X W X S
Where
C = Number of organisms counted
L = Length of each strip (S-R cell length) mm
D = Depth of a strip (S-R cell depth) mm
W = Width of a strip in mm
S = Number of strips counted
                       V1   = (50)(1)(W)
=            mm3          
 The plankton counts per strip are then determined by multiplying the actual count by the factor representing the counted portion of the whole S-R cell volume.
                        Number/ml = (C) (1000 mm3) / (L) (D) (W) (S)
  Where
C = Number of organisms counted.
L = Length of each strip in mm (of S-R cell)
D = Depth of the strip in mm (S-R cell)
W = Width of the strip in mm (Whipple grid image width)
S = Number of strips counted.
Phytoplankton Counting Units: Some plankton are unicellular while others are multicellular (colonial), posing a problem for enumeration. For analysis, a colony of plankton is accounted as a single count. The large forms that cross two or more boundaries of the grid are counted separately at lower magnification and their number included in the total count.

COMMONLY FOUND ALGAL GROUPS IN LAKES

Bacillariophytes: They occur in fresh water, salt water, and terrestrial ecosystems. They are single-celled algae with shells constructed of two overlapping valves composed of pectin and impregnated with silica. Amorphous silica is the form of silicon in diatom cell walls. The diatoms are single-celled or unicellular organisms, but some can form colonies and filaments. They may occur as plankton or periphyton, with most brownish-green films on substrates such as rocks or aquatic plants being composed of attached diatoms. The Bacillariophytes comprises two main types: centric and pennate. Centric diatoms are radially symmetrical and pennate diatoms that are bilaterally symmetrical. Many diatoms have conspicuous oil droplets within the cell, which is the photosynthetic food reserve, chrysolaminarin. The diatoms contain the pigments chlorophyll a and b, alpha and beta carotene, and several xanthophylls.
Example: Nitzschia sp., Cymbella sp., Melosira sp., Navicula sp., Gomphonema sp., Cyclotella sp., Pinnularia sp., Gyrosigma sp., etc.

Euglenoids: Typically green and unicellular, euglenoid flagellates occur in most freshwater habitats: puddles, ditches, ponds, streams, lakes, and rivers, particularly waters contaminated by animal pollution or decaying organic matter. Most are photosynthetic, but many, lacking chloroplasts are heterotrophs. Most do not reproduce sexually. Euglenoids lack a cellulose cell wall; instead, they have a proteinaceous pellicle just inside the plasmalemma. Euglenoids are characterized by chlorophylls a, b, beta carotene, and xanthophylls, one membrane of chloroplast endoplasmic reticulum, a mesokaryotic nucleus, two emergent flagella with fibrillar hairs in one row and paramylon or chrysolaminarin as the storage product in the cytoplasm. They have eyespot (stigma) which is a collection of orange-red lipid droplets. If placed in the dark over the course of several divisions, the chloroplasts of Euglena gracilis will become colorless. When returned to the light, the plastid structure is reformed and the green color returns. All euglenoid species with an eyespot and flagellar swelling exhibit phototaxis, usually swimming away from bright light (negative phototaxis) and away from darkness toward subdued light (positive photoaxis) to accumulate in a region of low light intensity.
Example: Euglena sp., Phacus sp., Trachelomonas sp., etc.

Blue-Green Algae (Cyanobacteria): The cyanophytes are the only prokaryotic algae and lack membrane bound organelles. Cyanobacteria are aerobic phototrophic organisms that can perform photosynthesis as they possess chlorophyll a and photosystem II. They are ubiquitous in nature and are found in every type of environment including terrestrial, freshwater, and marine habitats. Blue green algae are very common in waters of a great range of salinity and temperature, and they occur in and on the soil and also on rocks and in their fissures. However, the external structure can range from unicellular or colonial to branched or unbranched and filamentous. The cyanobacterial cells possess a number of cell inclusion bodies like include phycobilisomes, carboxysomes, glycogen granules, polyphosphate granules, poly-β –hydroxybutyrate granules, cyanophycin granules and gas vesicles. The cyanophytes possess no flagellated or cilliated cells at any stage of their lifecycle, although, simple movements such as bending and swaying are made possible by internal pressure changes exerted on the cell wall. They are heavily pigmented with chlorophyll a, beta carotene, and several xanthophylls. The presence of several phycobiliproteins gives the cyanophyta their unique blue-green coloration. Food is stored in the form of glycogen. Example: Microcystis sp., Merismopedia sp., Phormidium sp., Anabaena sp., etc.

Green Algae (Chlorophytes): Chlorophytes are a diverse group and are common in fresh water, salt water, and soil. The chlorophyta are primarily freshwater; only about 10% of the algae are marine, whereas 90% are freshwater. Green algae have unicellular or multicellular thalli. Some are flagellates, and others produce reproductive cells, the majority of which are biflagellate. Chlorophyte reproduction varies greatly, from asexual division to isogamy and heterogamy to oogamy. Cell walls are constructed of cellulose and pectin. The food storage product is true starch, the same as plants. Green algae possess true chloroplasts, which contain the same pigments found in higher plants: chlorophyll a and b, alpha and beta carotene, and many xanthophylls.
Example: Chlorella sp., Ankistrodesmus sp., Chlamydomonas sp., Pandorina sp., Eudorina sp., Chlorogonium sp., Actinastrum sp., Pediastrum sp., Scenedesmus sp., etc.