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MAGNESIUM AND ALKALINITY

5)  Calculating Magnesium Content: A Simple yet Logical Approach


Now that we've determined the calcium content in our water sample, let's move on to calculating the magnesium content. But wait, why aren't we using a separate test for magnesium? Well, here's the thing: magnesium and calcium are both alkaline earth metals that contribute to the overall hardness of water. By subtracting the calcium content from the total hardness content, we can indirectly determine the magnesium content.

Think of it like a simple math problem:

Total Hardness (CaCO3) = Calcium Content (CaCO3) + Magnesium Content (CaCO3)

To find the magnesium content, we simply rearrange the equation:

Magnesium Content (CaCO3) = Total Hardness (CaCO3) - Calcium Content (CaCO3)

By using this approach, we can accurately determine the magnesium content in our water sample without needing a separate test. It's a logical and efficient way to get the information we need

6) Unraveling the Mystery of Alkalinity: A Tale of Three Titration

Alkalinity is a crucial parameter in water quality analysis, as it helps us understand the capacity of water to neutralize acids. But did you know that alkalinity is not a single entity? In fact, there are different types of alkalinity, each requiring a unique approach to determination.

So, how do we determine these different types of alkalinity? The answer lies in the world of titration, where a carefully calibrated acid is used to neutralize the alkaline substances in the water sample.

Titration 1: Phenolphthalein Indicator
In the first titration, we use phenolphthalein as an indicator. This indicator changes color from pink to colorless when the pH of the solution drops below 8.3. By using phenolphthalein, we can determine the hydroxide alkalinity, which is caused by the presence of hydroxide ions (OH-) in the water.

Titration 2: Methyl Orange Indicator
In the second titration, we switch to methyl orange as an indicator. This indicator changes color from yellow to red when the pH of the solution drops below 4.4. By using methyl orange, we can determine the total alkalinity, which includes both hydroxide and bicarbonate alkalinity.

Titration 3: Phenolphthalein after Barium Chloride Addition
In the third titration, we add a twist to the phenolphthalein method. After adding barium chloride to the water sample, we perform the titration with phenolphthalein again. This time, we're determining the bicarbonate alkalinity, which is caused by the presence of bicarbonate ions (HCO3-) in the water.

So, why do we need to perform three separate titrations to determine alkalinity? The reason lies in the different types of alkaline substances present in water. By using different indicators and techniques, we can selectively determine the different types of alkalinity, providing a more comprehensive picture of the water's chemical properties.

The Reagent Team: Uncovering Alkalinity Secrets


When it comes to determining alkalinity, we need a team of specialized reagents let's meet them and explore why they're chosen for this task.

1. Phenolphthalein Indicator

Phenolphthalein is our first team member. This indicator is incredibly sensitive to changes in pH, especially around pH 8.3. When the pH drops below 8.3, phenolphthalein changes color from pink to colorless. This color change is like a signal, telling us that the alkalinity has been neutralized.

2. Std HCl Acid – 0.02N

Next up is our standardized hydrochloric acid (HCl) solution, with a concentration of 0.02N. This acid is used to neutralize the alkalinity in the water sample. The reaction between HCl and alkalinity is like a game of chemical tag:

  • HCl (acid) + OH- (alkalinity) → H2O (water) + Cl- (chloride ion)

3. Barium Chloride Solution – 10%

Now, let's introduce barium chloride, our third team member. This reagent is used to precipitate out sulfate ions, which can interfere with our alkalinity determination. The reaction between barium chloride and sulfate ions is like a chemical filter:

  • BaCl2 (barium chloride) + SO42- (sulfate ion) → BaSO4 (barium sulfate precipitate) + 2Cl- (chloride ion)

4. Methyl Orange Indicator

Last but not least, we have methyl orange, our fourth team member. This indicator changes color from yellow to red when the pH drops below 4.4. Methyl orange is used to determine the total alkalinity, which includes both hydroxide and bicarbonate alkalinity.

By combining these reagents, we can determine the different types of alkalinity in a water sample. Phenolphthalein helps us detect hydroxide alkalinity, while methyl orange indicates total alkalinity. Barium chloride ensures that sulfate ions don't interfere with our results, and standardized HCl acid provides a precise way to neutralize the alkalinity.

There you have it – the reagent team that helps us uncover the secrets of alkalinity!

Determining Alkalinity: A Step-by-Step Guide


Step 1: Phenolphthalein Titration

  1. Take 100ml of the sample and place it in a porcelain basin. Make sure the basin is clean and free of any contaminants that could affect the results.
  2. Add 1ml of phenolphthalein indicator. If the solution turns pink, it's time to titrate! The pink color indicates the presence of hydroxide ions (OH-), which are a key component of alkalinity.
  3. Slowly add standardized HCl acid while stirring with a glass rod until the pink color disappears. The acid will react with the hydroxide ions to form water and chloride ions, causing the pink color to fade.
  4. Preserve the titrated solution for future reference. This solution will be used as a reference point for the next steps.

Step 2: Methyl Orange Titration

  1. Add 3 drops of methyl orange indicator to the same solution. Methyl orange is a pH indicator that changes color in response to changes in pH.
  2. Continue the titration with standardized HCl acid until the color changes from yellow to orange. The color change indicates that the pH of the solution has dropped below 4.4, which is the endpoint for this titration.
  3. Note down the volume of HCl acid used for this titration. This volume will be used to calculate the total alkalinity of the sample.

Step 3: Determining Alkalinity to Phenolphthalein (Modified)

  1. Take another 100ml aliquot of the sample and add a crystal of sodium sulphate. Sodium sulphate is added to precipitate out any sulfate ions that may be present in the sample.
  2. Add 10ml of barium chloride solution and stir well for 2 minutes. Barium chloride is used to precipitate out any sulfate ions that may be present in the sample.
  3. Add 1ml of phenolphthalein indicator and titrate with standardized HCl acid until the pink color disappears. This titration is used to determine the alkalinity to phenolphthalein, which is a measure of the hydroxide ion concentration.
  4. Disregard any reappearance of the pink color. The reappearance of the pink color is likely due to the presence of other ions that are not relevant to the alkalinity determination.

Calculation of Alkalinity


The alkalinity of a water sample is calculated based on the volume of standardized acid used to neutralize the alkaline substances present.

Alkalinity to phenolphthalein (p) is calculated using the following formula:

  • p (mg/L) = 10 × V1

where V1 is the volume in milliliters (mL) of standardized acid used to neutralize the hydroxide ions (OH-) present in the sample.

Proof

The reaction between hydroxide ions (OH-) and standardized acid (HCl) is as follows:

  • OH- + HCl → H2O + Cl-

The equivalent weight of hydroxide ions (OH-) is 1/2 of the molecular weight of calcium carbonate (CaCO3), which is 50 mg/mmol. Therefore, 1 mmol of hydroxide ions (OH-) is equivalent to 50 mg of CaCO3.

Since 1 mL of 0.02 N standardized acid is equivalent to 1 mmol of acid, the amount of CaCO3 equivalent to 1 mL of acid is:

  • 50 mg/mmol × 1 mmol/mL = 50 mg/mL

However, the formula uses a factor of 10 instead of 50. This is because the alkalinity is expressed in terms of CaCO3, and the equivalent weight of CaCO3 is 50 mg/mmol.

But the standardized acid is 0.02 N, which means it is 1/50 of the normality. Therefore, the factor of 10 is used instead of 50:

  • p (mg/L) = 10 × V1



Alkalinity to methyl orange (m) is calculated using the following formula:

m (mg/L) = 10 × V2

where V2 is the volume in milliliters (mL) of standardized acid used to neutralize the bicarbonate ions (HCO3-) present in the sample.

Proof

The reaction between bicarbonate ions (HCO3-) and standardized acid (HCl) is as follows:

  • HCO3- + HCl → H2O + CO2 + Cl-

The equivalent weight of bicarbonate ions (HCO3-) is also 1/2 of the molecular weight of calcium carbonate (CaCO3), which is 50 mg/mmol. Therefore, 1 mmol of bicarbonate ions (HCO3-) is equivalent to 50 mg of CaCO3.

Using the same logic as before, the formula for alkalinity to methyl orange is:

  • m (mg/L) = 10 × V2


Alkalinity to phenolphthalein after the addition of barium chloride is calculated using the following formula:

Alkalinity (mg/L) = 10 × V3

where V3 is the volume in milliliters (mL) of standardized acid used to neutralize the hydroxide ions (OH-) present in the sample after the addition of barium chloride.

Its Proof

The addition of barium chloride precipitates out the sulfate ions (SO42-) present in the sample:

  • BaCl2 + SO42- → BaSO4 + 2Cl-

The resulting solution contains only hydroxide ions (OH-), which are then neutralized by the standardized acid:

  • OH- + HCl → H2O + Cl-

Using the same logic as before, the formula for alkalinity to phenolphthalein after addition of barium chloride is:

  • Alkalinity (mg/L) = 10 × V3