Water and Life

Introduction

Water is essential for all known forms of life. Its unique chemical and physical properties make it indispensable for biological processes, from cellular structure to environmental regulation. This section explores the molecular basis of water's properties, their biological significance, and the role of hydrogen bonding and pH in living systems.

Properties of Water

Polarity of Water Molecules

Water (H2O) is a polar molecule, meaning it has an uneven distribution of electrical charge.

• Oxygen atom: Carries a partial negative charge (δ−).

• Hydrogen atoms: Each carries a partial positive charge (δ+).

• This polarity arises because oxygen is more electronegative than hydrogen, pulling shared electrons closer.

Hydrogen Bonding in Water

The polarity of water molecules enables them to form hydrogen bonds with each other.

• The partial positive charge of hydrogen in one water molecule is attracted to the partial negative charge of oxygen in another water molecule.

• Hydrogen bonds are relatively weak individually but collectively confer significant structure and stability to liquid water.

• Hydrogen bonds constantly form and break, allowing water to flow while maintaining cohesion.

Four Emergent Properties of Water Critical for Life

Cohesion and Adhesion

Water molecules exhibit strong cohesion due to hydrogen bonding, and can also adhere to other substances.

• Cohesion: The attraction between like molecules (water to water), leading to phenomena such as surface tension.

• Adhesion: The attraction between water molecules and different substances (e.g., water to plant cell walls).

• Together, cohesion and adhesion enable water transport in plants against gravity.

Surface Tension

Surface tension is a measure of how difficult it is to break the surface of a liquid.

• Water has a high surface tension due to the collective strength of hydrogen bonds at the surface.

• This allows small insects to walk on water and supports the formation of droplets.

Moderation of Temperature

Water moderates temperature through its high specific heat and ability to absorb and release heat with minimal temperature change.

• Specific heat: The amount of heat required to raise the temperature of 1 gram of a substance by 1°C.

• Water's specific heat:

• Hydrogen bonding requires extra energy to break, so water heats and cools slowly, stabilizing environments and organisms.

• Evaporative cooling: As water evaporates, the remaining liquid cools, helping regulate temperature in organisms and ecosystems.

Expansion Upon Freezing

Unlike most substances, water expands as it freezes, making ice less dense than liquid water.

• Hydrogen bonds arrange water molecules in a crystalline structure, spacing them further apart.

• This property allows ice to float, insulating aquatic life in cold environments.

Versatility as a Solvent

Water is known as the universal solvent due to its ability to dissolve a wide variety of substances.

• Polar molecules and ions readily dissolve in water, forming hydration shells.

• Nonpolar substances (hydrophobic) do not dissolve well in water.

• Water's solvent properties are crucial for biochemical reactions and transport of nutrients and waste.

Acids, Bases, and pH

Dissociation of Water

Water molecules can dissociate into ions:

• Hydronium ion:

• Hydroxide ion:

• In pure water, the concentration of and is mol/L, making it neutral.

Acids and Bases

• Acid: A substance that increases the hydrogen ion () concentration in a solution. Example: HCl dissociates into and .

• Base: A substance that reduces the hydrogen ion concentration, often by accepting or donating . Example: NaOH dissociates into and .

The pH Scale

The pH scale measures the concentration of hydrogen ions in a solution, ranging from 0 (most acidic) to 14 (most basic).

• pH is defined as the negative logarithm (base 10) of the hydrogen ion concentration:

• Each pH unit represents a tenfold change in concentration.

• Acidic solutions: pH < 7; Neutral: pH = 7; Basic solutions: pH > 7.

Buffers

Buffers are solutions that minimize changes in pH by absorbing excess or ions.

• Example: The carbonic acid-bicarbonate buffer system in blood maintains pH near 7.4.

• Carbonic acid () can donate to become bicarbonate (), or accept to revert to carbonic acid, buffering blood pH.

Environmental Impact: Ocean Acidification

Increased atmospheric CO2 leads to more CO2 dissolving in oceans, forming carbonic acid and lowering ocean pH.

• This process, called ocean acidification, threatens marine life by altering carbonate availability for shell formation.

Summary Table: Properties of Water

Additional info: Academic context and definitions have been expanded for clarity and completeness.