topic 1 >-< Flashcards
ocean water
Know the freezing point of freshwater and saltwater
- freshwater: 0C / 32 F
- saltwater: -2C / 28.4F
Be able to explain the change in molecular speed with increased temperature
As temperature increases molecular speed increases according to the kinetic particle theory
Be able to explain what the hydrogen bonds look like when ice forms
lattice structure/ crystalline structure
Be able to define the kinetic particle theory
describes all matter as a collection of particles that are in constant, random motion (even if the movements are only small vibrations)
Understand how the spacing and movement of molecules changes with state (SOLID)
Solid: arranged in a lattice structure fixed in position (ice)
When ice is heated water molecule are given more energy, resulting in them vibrating faster until the forces holding the molecules together start to break. (Breaking of hydrogen bonds)
The water molecules nearest the outer surfaces of the ice crystals break free and flow away taking shape of the container they are in.
Understand how the spacing and movement of molecules changes with state (LIQUID)
Liquid: water molecules are closely packed to each other in a liquid but are able to move freely past each other (cannot be compressed and take shape of the contained they are in)
When liquid water is heated, the particles gain more energy, making them move faster and slightly further from each other.
Understand how the spacing and movement of molecules changes with state (GAS)
Gas: Water vapour (vapor) term given to the gaseous water (both from evaporation and boiling)
Boiling is 100 degrees Celsius at 1 atmospheric Pressure
Be able to identify a covalent bond
Covalent bond: two atoms share a pair of electrons (Covalent bonding occurs in most non-metal elements and in compounds formed between nonmetals)
Be able to identify a hydrogen bond
Hydrogen bonding is a special type of dipole-dipole attraction between molecules, not a covalent bond to a hydrogen atom.
It results from the attractive force between a hydrogen atom covalently bonded to a very electronegative atom such as a N, O, or F atom and another very electronegative atom.
Know what the atomic number of an element is, and be able to determine the number of electrons from it
atomic number: the number of protons contained in the nucleus of an atom
Electron: a negatively charged subatomic particle that orbits the nucleus of an atom
An atom has an equal number of protons as electrons, so they are neutral, but….
An ION is an atom or a molecule that has lost or gained one or more electrons creating an electrical charge. (Cations- lost electrons, Anions- gained electrons)
Be able to determine how many shells an atom has based on its electron count
1st Shell: nearest to nucleus can hold 2 electrons (only shell present in hydrogen and helium)
2nd Shell: holds up to 8 electrons
3rd Shell: holds up to 18 electrons
4th Shell: holds up to 32 electrons
Know the definition of the term polar molecule
A polar molecule is a molecule in which one end of the molecule is slightly positive, while the other end is slightly negative. Examples: H2O, HF, NH3, SO2
Know the difference between Halocline, thermocline, and Pycnocline. (Significant Changes in abiotic factors happen at these locations)
Thermocline: a layer between two layers of water with different temperatures
Halocline: a layer of water below the mixed surface layer where a rapid change in salinity can be measured as depth increases
The Surface layer (0-200m) is the best-mixed area of the ocean. (Turbulence is created from wind and currents so this layer is typically uniform across the ocean. Mixing of layers are typically density driven. For example, if the surface of the ocean cools, density of water will increase and the water will sink carrying all the nutrients and gaseous contained in that surface layer.
Pycnocline: a layer of water between two layers of water with different densities
Pressure increases with depth compressing the water molecules together, forcing more molecules into smaller volumes. Also as salinity increases, density also increases. This indicates that the saltiest water is at the seabed. However, there is one exception, the tropical seas (between 30 N and 30 S latitudes) high evaporation rates equals high salinity.
Tropical region (temperature)
decreases w/ depth
Surface layer could be 25 degrees celsius or more but experiences a drastic decline with depth.
tropical region (salinity)
decreases w/ depth
High evaporation = high salinity at surface, followed by a steep decrease, followed by a slow increase
If it rains a lot, salinity may increase w/ depth slightly after the surface layer
tropical region (density)
increases w/ depth
Defined pycnocline: surface water density is a lot less dense than the lower layers
polar region (temperature)
decrease w/ depth (less dramatic)
Surface is close to freezing and remains constant with increasing depth.
No mixed layer or pycnocline exists in the highest latitudes since sm heat is lost to the cold atmosphere that the temp cools very quickly to a similar temp to the bottom water
, i.e. no temp gradient.
polar region (salinity)
increases w/ depth
Lower salinities at the surface and increases as you go deeper.
Cold and fresh water in the surface mixed layer is separated from a layer of warm saline Atlantic water by a cold and stable layer, the cold halocline.