Tuesday, July 9, 2013

Literature Review

Research Title
 Investigation on how dissolving chemicals in water changes the freezing point of a solution.

Hypothesis
 The higher amount of dissolving chemicals in water, the lower the freezing point of water.

Salt, also known as sodium chloride (CaCl2), lowers the freezing point of water. This process is called the freezing point depression. The freezing point depression can occur as long as there is a solution. Adding a solute, like salt, to a solvent, like water, lowers the freezing point of the solvent. However, the freezing point of the solvent varies in different conditions: the molality of the solution, the van't Hoff factor of the solute, and the molal freezing-point-depression constant of the solvent.


Molality, is defined as shown below:

Molality (moles/kg) = Moles (mol) of Solute/Kilograms (kg) of Solvent


Freezing point depression is a colligative property, a property that depends on the number of solute particles are in the solvent. The van't Hoff factor on the other hand, is how a molecule of a solute dissociates, or breaks apart, in the solvent. Covalent compounds, like sucrose (C12H22O11), do not dissociate in solution. These compounds have van't Hoff factors i = 1. Ionic compounds, like table salt (NaCl), dissociate when in solution. Table salt (NaCl) has a van't Hoff factor i = 2 because it dissociates into two ions in solution Na+ and Cl-. The third factor, the molal freezing-point-depression constant, Kf, is different for every solvent. It has units of (° C/m), and it tells indicates how much 1 mol of solute added to 1 kg of solvent will lower the solvent's freezing point. For pure water, Kf = 1.86° C/m. Combining these three factors—molality, m, van't Hoff factor, i, and molal freezing-point-depression constant, Kf—into an equation that predicts how much the freezing point of a solvent will decrease, ΔT, when a certain amount of solute is added.

The freezing point depression formula is defined as shown below:

Degrees Freezing Point is Depressed (° C) = Molal Freezing-Point-Depression Constant (° C/m)
× molality of solution (mol solute/kg solvent) × van't Hoff Factor (unitless)

In terms of symbols, the freezing point depression formula is stated below with what the symbols stands for:

ΔT = Kf m i

ΔT - freezing point in degrees Celsius (° C)
Kf - molal freezing point depression constant in degrees Celsius per molal (° C/m)
m - molality of the solution in moles per kilogram (mol/kg)
i - van't Hoff factor of the solute

The equation below shows the formula for the freezing point of a solution:

Solution Freezing Point (° C) = Solvent Freezing Point (° C) - Degrees Freezing Point is Depressed (° C)

In terms of symbols, the freezing point of a solution is as stated below:

Tn = Tf - ΔT

Tn - freezing point of the solution in degrees Celsius (° C)
Tf - freezing point of the solvent in degrees Celsius (° C)
ΔT i- freezing point depression in degrees Celsius (° C)


Bibliography

Eli, Todd & Keith. (n.d.). "Colligative Properties," Chemworld, ThinkQuest Library, Oracle Education Foundation. Retrieved July 10, 2013, from http://library.thinkquest.org/C006669/data/Chem/colligative/colligative.html?tqskip1=1.

Lachish, U. (2000). Avogadro's Number, Atomic and Molecular Weight. Retrieved July 10, 2013, from http://urila.tripod.com/mole.htm.

MacQuade, J., et al. (1986). It's Getting Colder (Freezing Point Depression). Retrieved July 10, 2013, from http://www.woodrow.org/teachers/chemistry/institutes/1986/exp9.html.

Science Buddies Organization. (n.d.). Chemistry of Ice-Cream Making: Lowering the Freezing Point of Water. Retrieved July 11, 2013 from http://www.sciencebuddies.org/science-fair-projects/project_ideas/FoodSci_p013.shtml#summary.




Monday, July 8, 2013

Literature Review 2: Investigation on the pH level of rainwaters collated around SST

Project Title 2: Investigation on the pH level of rainwaters collated around SST.
Hypothesis: The more polluted the air is in a location that the rainwater is located in SST, the lower the pH level.
Done by: Ain Nuha

Rainwater is water in form of droplets that are condensed from atmospheric water vapour and precipitated until it is heavy enough to fall because of gravity. Rain is important to the water cycle as it deposits the most fresh water on Earth. Also, rain provides a lot of suitable condition for the eco-system. Rainwater varies in terms of the pH level, mostly due to its origin. The places of where rainwater is from affects the pH level of it. For an example,  rain that is collected from the Atlantic Ocean has a pH level of 5.0 to 5.6. (Whereas, rain that is collected across the continental from the west has a pH level of 3.8 to 4.8. With that, we want to know on how the location of where the rainwater is collected affects the pH level and what are the factors that would change the pH level of the rainwater collected in SST. 

Bibliography
Willey, J. D. (1998) "Effect of storm type on rainwater composition in southeastern North Carolina"  Retrieved July 9, 2013 from http://en.wikipedia.org/wiki/Rain

Literature Review 3: Investigation on how dissolving chemicals in water changes the freezing point of a solution.

Project Title 3: Investigation on how dissolving chemicals in water changes the freezing point of a solution.
Hypothesis:  The higher amount of dissolving chemicals in water, the lower the freezing point of water.
Done by: Liew Yee Theng

Through some research, salt, otherwise known as sodium chloride (CaCl2), lowers the freezing point of water. This process is known as freezing point depression and it can occur as long as we have a solution. Adding a solute, like salt, to a solvent, like water, lowers the freezing point of the solvent. The answer to how much the freezing point of the solution depends on three things: the molality of the solution, the van't Hoff factor of the solute, and the molal freezing-point-depression constant of the solvent. 

Molalitym, is defined as moles (mol) solute per kilograms (kg) solvent, as shown in Equation 1, below: 

Equation 1:
Molality (moles/kg) = Moles (mol) of Solute/Kilograms (kg) of Solvent
Freezing point depression is a colligative property, a property that depend on how many solute particles are in the solvent, not the kind of solute particles. Molality, m, is one piece of this "how many solute particles are present?" question. The van't Hoff factor is the second part of the "how many solute particles are present?" question.
The van't Hoff factori, deals with how a molecule of solute dissociates, or breaks apart, in the solvent. Covalent compounds, like sucrose (C12H22O11), do not dissociate in solution. These compounds have van't Hoff factors i = 1. Ionic compounds, like table salt (NaCl), dissociate when in solution. Table salt (NaCl) has a van't Hoff factor i = 2 because it dissociates into two ions in solution, Na+ and Cl-.
The third factor, the molal freezing-point-depression constantKf, is different for every solvent. It has units of (° C/m), and it tells us how much 1 mol of solute added to 1 kg of solvent will lower the solvent's freezing point. For pure water, Kf = 1.86° C/m.
Combining these three factors—molality, m, van't Hoff factor, i, and molal freezing-point-depression constant, Kf—into an equation that predicts how much the freezing point of a solvent will decrease, ΔT, when a certain amount of solute is added. Equation 2, below, is the freezing point depression equation:

Equation 2:

Degrees Freezing Point is Depressed (° C) = Molal Freezing-Point-Depression Constant (° C/m)
× molality of solution (mol solute/kg solvent) × van't Hoff Factor (unitless)
ΔT = Kf m i
  • ΔT is the freezing point depression in degrees Celsius (° C)
  • Kf is the molal feezing-point-depression constant in degrees Celsius per molal (° C/m)
  • m is the molality of the solution in moles per kilogram (mol/kg)
  • i is the van't Hoff factor of the solute, which does not have units
In order to find out the new freezing point of a solution, Tn, subtract the change in temperature, ΔT, from the original freezing point, Tf, as shown in Equation 3, the solution freezing point equation:

Equation 3:

Solution Freezing Point (° C) = Solvent Freezing Point (° C) - Degrees Freezing Point is Depressed (° C)
Tn = Tf - ΔT
  • Tn is the freezing point of the solution in degrees Celsius (° C)
  • Tf is the freezing point of the solvent in degrees Celsius (° C)
  • ΔT is the freezing point depression in degrees Celsius (° C)


Bibliography
This idea for this Project Idea came from this source.




Wednesday, July 3, 2013

Hypothesis

Project Title 1: Investigation on how the pH level affects copper corrasion 
Hypothesis: The lower the pH level, the rate of corrasion will be higher.

Project Title 2: Investigation on the pH level of rainwaters collated around SST.
Hypothesis: The more polluted the air is in a location that the rainwater is located in SST, the lower the pH level.

Project Title 3: Investigation on how dissolving chemicals in water changes the freezing point of a solution.
Hypothesis: The higher amount of dissolving chemicals in water, the lower the freezing point of water.

Tuesday, July 2, 2013

Project Titles

Project Title 1:
Investigation on how the pH level affects copper corrasion 

Project Title 2:
Investigation on the pH level of rainwaters collated around SST.

Project Title 3:
Investigation on how dissolving chemicals in water changes the freezing point of a solution.


Monday, July 1, 2013

What is Scientific Method?

Scientific Methods are techniques or procedures that one would do in order to attain a certain result or a new knowledge using methods based on the principles of science. Scientific methods consists of making up a hypothesis by asking a relevant question, and to conduct an experiment to find out a conclusion as to the question asked in the first place. Scientific methods may vary.