Water
- 65% of the human body is composed of water
- 70% of the Earth is the ocean
- 98% of water on Earth is in oceans (saltwater) whereas 2% is freshwater, most often found in lakes
water’s polarity and hydrogen bonding
- water is a polar molecule, meaning that it has both positive and negative charges
- non-polar molecules cannot bond with other molecules of their kind as they only have one charge; bonds must be formed with different charges
- can form non-hydrogen bonds
- water can bond with up to four other water molecules
- each individual hydrogen bond is relatively weal, but collectively, the structure is strong
- water bonds with other molecules through hydrogen bonds
the properties of water
cohesion—allows water to defy gravity and scale trunks/stems of plants
versatile solvent—polar-opposite molecules form bonds (easy to break apart), beneficial for digestion
less dense—water has low density and will often float when combined with other substances
high specific heat—lots of energy necessary to break water’s hydrogen bonds (hard for temperature to change)
- specific heat: the amount of heat absorbed or lost due to a change in temperature
- high specific heat stabilizes ocean temperatures
- water absorbs and stores heat from the sun during the day while barely warming, and gradually cools during the night and colder months, warming the air above it
evaporative cooling—the hottest molecules have more kinetic energy and are the first to evaporate, leaving the cooler ones behind
the fastest (hottest) molecules evaporate
helps protect terrestrial organisms from overheating and contributes to the stability of temperatures in lakes and ponds
- people are not cooled by sweat itself—we’re cooled by the evaporation that follows