Topic: Water as the Biological Solvent, pH, and Buffers
Referenced Text: Campbell Chapter 3
Water is essential for all living organisms.
Most cells are composed of 70-95% water.
The prevalence of water contributes significantly to Earth's habitability.
Water molecules interact through hydrogen bonds, which occur due to polar covalent bonds.
Visual representation of bonds:
δ− (negative charge on oxygen) and δ+ (positive charge on hydrogen).
Four critical properties that enhance Earth’s suitability for life:
Cohesive/Adhesive Properties: Water molecules stick to each other (cohesion) and to other substances (adhesion).
Temperature Moderation: Water can absorb and retain heat, regulating temperature.
Expansion upon Freezing: Water expands and becomes less dense as it freezes, allowing ice to float.
Solvent Versatility: Water dissolves a wide range of substances, supporting metabolic processes.
Water in conducting cells moves due to:
Cohesion: Water molecules stick together.
Adhesion: Water molecules stick to other materials.
Defined as the energy required to break the surface of a liquid.
High surface tension in water is due to hydrogen bonds, allowing for phenomena like water striders walking on water.
Specific Heat: Amount of heat needed to raise the temperature of 1 g of water by 1°C, approximately 1 cal/g°C.
Compared to ethanol (0.55 cal/g°C).
Water’s high specific heat moderates temperature changes in environments.
Heat of vaporization refers to the heat required to convert 1 g of water from liquid to gas.
Evaporative cooling occurs as the fastest molecules escape as gas, cooling the remaining liquid.
Water expands upon freezing due to the formation of stable hydrogen bonds in a crystalline structure (ice) similar to a hexagonal lattice.
This open structure makes ice less dense than liquid water; hence, ice floats.
Practical impacts include the potential for frozen water to break containers.
Solution: Homogeneous mixture of substances where a solvent dissolves the solute.
Aqueous Solutions: Solutions in which water acts as the solvent.
Water, as a polar solvent, effectively dissolves other polar and ionic substances.
Molecules do not have to be ionic to dissolve in water; they can be polar as well.
Molecular Mass: Sum of the masses of all atoms in a molecule calculated in daltons.
Molarity (M): Number of moles of solute per liter of solution.
Sucrose (C12H22O11) has a molecular mass of 342 daltons.
1 mol = 342 g in 1 liter of water.
pH Scale: Measures the acidity/basicity of a solution based on [H+] and [OH-].
Pure water has [H+] = [OH-] at 10^-7 M, defining neutrality (pH = 7).
Buffers: Substances that minimize changes in pH, essential for cellular function and metabolism.
Buffers often consist of an acid-base pair that interact with H+. E.g., H2CO3 ↔ HCO3- + H+.
CO2 emissions lead to ocean acidification, impacting marine life and calcification processes.
The reaction of CO2 with seawater to form carbonic acid decreases pH.
The pH scale is logarithmic, where a change of 1 unit represents a tenfold change in [H+] concentration.
Comparison questions can assess understanding of the relationship between different pH values.
Water's polarity allows it to form hydrogen bonds, making it crucial for life.
Key concepts covered include the role of H+ and OH- ions, the pH scale, and buffer systems.