A layer of gases surrounding Earth, held by gravity, protecting life by absorbing UV radiation, retaining heat, and moderating temperature extremes.
The atmosphere has a mass of 5 quintillion kilograms, with 75% within 11 km of the surface.
It has no definitive boundary, but 100 km altitude (the Kármán Line) is commonly used as a reference.
The part of the atmosphere used for breathing and photosynthesis, found near Earth's surface.
Nitrogen (78%), Oxygen (21%), Argon (0.9%).
Gases that make up 0.1% of the atmosphere, including carbon dioxide, methane, water vapor, nitrous oxide, and ozone.
Natural substances include dust, pollen, volcanic ash, and sea spray. Industrial pollutants include chlorine compounds, fluorine compounds, mercury, and sulfur compounds.
Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere.
The lowest layer, containing 80% of atmospheric mass and 99% of its water vapor.
From Earth's surface to 7 km at the poles and 20 km at the equator.
* Temperature decreases from 15°C at ground level to -75°C at the top.
* Air pressure decreases from 101.3 kPa to about 10 kPa.
Nearly all weather phenomena, including clouds and storms.
It contains the ozone layer, which absorbs UV radiation.
Rises from -50°C at the bottom to 0°C at the top due to solar radiation absorption.
The ozone layer, about 1 cm thick, absorbs 97-99% of UV radiation.
* Temperatures drop to as low as -100°C, making it the coldest atmospheric layer.
* Meteors burn up here due to collisions with gas particles.
* Temperatures can reach up to 1500°C.
* Low air density prevents significant heat transfer to objects.
The aurora borealis, caused by ionization of gas particles.
The outermost layer, extending from the thermosphere to about 190,000 km, halfway to the Moon.
Mostly hydrogen and helium, with particles spaced so far apart they rarely collide.
From volcanic gases, primarily carbon dioxide, water vapor, ammonia, and methane. Photosynthetic bacteria began producing oxygen, increasing its levels while reducing carbon dioxide.
* Early: 95% CO2, 4% O2, high temperatures (~400°C).
* Today: 78% N2, 21% O2, moderate temperatures (~20°C).
It broke down into nitrogen and hydrogen, with hydrogen escaping into space.
The temperature at which particle motion ceases (-273°C or 0 K).
A barometer, invented by Evangelista Torricelli in 1643.
101.3 kPa or 760 mmHg.
At constant temperature, pressure and volume are inversely proportional: P1V1=P2V2. the plot results in a downwards curve.
At constant pressure, volume and temperature are directly proportional: V1/T1=V2/T2. the plot results in a straight line..
At constant volume, pressure and temperature are directly proportional: P1/T1=P2/T2. the plot results in multiple straight lines, where every line represents the relationship between pressure and temperature for a different gas.
Combines all three laws: the relationship among pressure, volume, and temperature of a fixed amount of gas. P1V1/T1=P2V2/T2
The total pressure of a gas mixture equals the sum of partial pressures in a gas mixture. the components act independently of each other: Ptotal=P1+P2+P3…
Mercury adjusts in a tube to balance atmospheric pressure, with normal atmospheric pressure at 760 mmHg. the weight of mercury creates a vacuum in the top of the tube.
Measuring gas pressure in closed systems by comparing mercury levels in a U-shaped tube. has a known pressure (possibly vacuum) on one side and the unknown pressure on the other. calculated based on the difference in height between the two sides.
* Anything that has mass and occupies space. Mass is the amount of matter in an object.
* Solid: Has a definite shape and volume, with tightly packed particles that vibrate in place and strong intermolecular forces (IMFs).
* Liquid: Has a definite volume but no definite shape, particles move freely, are moderately attracted to each other, and take the shape of the container.
* Gas: Has no definite shape or volume, particles are far apart with weak or no attraction, and is highly compressible.
* Plasma: ionized gas
1. Crystalline Solids
* Particles have a regular repeating pattern (e.g., ionic compounds like salt).
2. Amorphous Solids
* Particles are arranged randomly (e.g., plastic, glass).
* Slightly compressible, particles have translational motion, and liquids can flow.
* Highly compressible, particles move by diffusion (high to low concentration) and effusion (high to low pressure through an opening). Gases, like liquids, are fluids, meaning they can flow.
* Result of gas particles colliding with container walls; calculated as force per unit area.
Measured with a barometer; mercury is used due to its high density, which allows a measurable column at sea level (760 mmHg or 1 atm)
* Has a fixed composition and properties, cannot be separated by physical processes.
* Element: Pure substance with one type of atom.
* Compound: Two or more elements chemically combined, with unique properties.
* Variable composition and properties, can be separated by physical processes.
* Characteristics that don’t change the substance’s composition (e.g., density, color, melting point).
* Characteristics describing how a substance reacts with other substances, changing composition (e.g., flammability, reactivity).
* Change that doesn’t alter the substance's composition and is often reversible (e.g., melting, dissolving).
* Change that forms new substances and alters composition; generally not reversible (e.g., burning, rusting).
* Thermal energy transferred due to a temperature difference between two bodies.
* Measures average kinetic energy of particles in a substance (K.E. = ½ mv²).
* Flows from high to low temperature and can occur by:
* Conduction: Heat transfer through direct contact.
* Convection: Heat transfer by motion of fluids.
* Radiation: Heat transfer without a medium (e.g., sunlight).
* Gases consist of tiny, fast-moving particles with little attraction.
* The distance between particles is large, so the actual volume of particles is minimal.
* Particles move in straight lines, with elastic collisions causing pressure.
* Average kinetic energy of particles is directly proportional to temperature.
* Shows the number of particles at various speeds in a sample at a certain temperature; higher temperatures increase the average speed and kinetic energy of particles.
* Occurs when matter absorbs or releases energy without changing temperature (e.g., melting, boiling).
* Absorbing energy: Solid → Liquid (melting), Liquid → Gas (evaporation).
* Releasing energy: Gas → Liquid (condensation), Liquid → Solid (freezing).
* During phase changes, energy overcomes IMFs rather than raising temperature, resulting in a constant temperature until the phase change completes.
* Pressure of a vapor in equilibrium with its liquid or solid in a closed container.
* Higher temperature increases vapor pressure, allowing more particles to escape into the vapor phase.
* Stronger IMFs in a liquid lower vapor pressure as fewer molecules can escape.
1. Boiling Point
* Temperature at which vapor pressure of a liquid equals atmospheric/ barometric pressure, allowing bubbles to form and rise within the liquid.
2. Evaporation
* Surface-only process of liquid turning into gas at temperatures below boiling point.
* Graphical representation of a substance's phases under varying temperatures and pressures.
* Triple Point: Where all three phases coexist in equilibrium.
* Critical Point: Beyond which a substance becomes a supercritical fluid, with no distinction between liquid and gas.
* Fusion (Melting) Curve: Transition between solid and liquid.
* Vaporization Curve: Transition between liquid and gas.
* Sublimation Curve: Transition between solid and gas.
* Moving vertically (upward) increases density, while moving horizontally (rightward) increases kinetic energy.
the gaseous state of a substance that is solid or liquid at room temperature
The smallest unit of an element that retains its chemical properties, made of protons, neutrons, and electrons.
The number of protons in the nucleus, also known as the atomic number.
The number of protons in the nucleus of an atom, which identifies the element.
The total number of protons and neutrons in an atom's nucleus.
Atoms of the same element that have the same number of protons but different numbers of neutrons.
Isotopes with more neutrons have a greater mass.
Chemical properties depend only on the number of electrons, which isotopes have in common.
By adding the mass number to the element’s name, e.g., potassium-39.
Number of neutrons = A - Z (mass number - atomic number)
The central part of an atom, containing protons and neutrons, and accounting for most of the atom's mass.
Positively charged subatomic particles located in the nucleus.
Subatomic particles with no charge, located in the nucleus, that add to the atom's mass.
Negatively charged subatomic particles orbiting the nucleus, with negligible mass compared to protons and neutrons.
Electrons are about 1/5000 the mass of a proton, or approximately negligible.
A unit of mass equal to 1/12 the mass of a carbon-12 atom, approximately 1.6611x10^-24 grams.
Carbon-12 is a common element and ensures atomic masses are represented as whole numbers for most elements.
The weighted average mass of an element's isotopes, as shown on the periodic table, measured in atomic mass units (amu).
It’s a weighted average of all naturally occurring isotopes of the element.
6.02x10^23. he number of representative particles in one mole of a substance.
The metric unit for measuring the amount of substance, defined as the number of atoms in exactly 12 grams of carbon-12.
The mass in grams of one mole of a substance, numerically equal to its atomic or formula mass in g/mol.
* Element: Atoms
* Ion: Ions
* Ionic compound: Formula units
* Molecular compound: Molecules
The sum of the average atomic masses of all atoms in the formula of an ionic compound.
The sum of the average atomic masses of all atoms in the formula of a molecular compound.
* Moles to mass: moles x molar mass = g
* Mass to moles: g / molar mass = moles
* Mass → Moles → Particles
* Particles → Moles → Mass
The percentage by mass of each element in a compound, calculated as (mass of element / mass of compound) x 100
The ratio of elements in a compound does not change, regardless of sample size.
Draw a line from 1 atmosphere to the liquid-gas boundary, then drop to the corresponding temperature.
Evaporation and condensation occur at equal rates, maintaining equilibrium.
The mass remains constant.