Unit 1 Study Sheet Test PDF
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Esther Starkman School
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This document is a study sheet for a chemistry test, covering topics such as particle theory, classifying matter, physical and chemical properties, and climate change. It provides definitions and equations related to these topics and includes sections on the history of the atom and isotopes.
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2.7 to 2.13 are mainly focused on the unit test Particle Theory 2.1 - Everything is made up of particles. Classifying Matter 2.2 - Pure substances: have 1 type of atom - Compounds: 2 or more atoms that are different from each other and are chemically bonded. - Mol...
2.7 to 2.13 are mainly focused on the unit test Particle Theory 2.1 - Everything is made up of particles. Classifying Matter 2.2 - Pure substances: have 1 type of atom - Compounds: 2 or more atoms that are different from each other and are chemically bonded. - Molecule: 2 or more atoms from elements or compounds. - Mixture:Two or more different pure substances that are NOT chemically combined. - Homogeneous: Not seeable (one phase) - Heterogeneous: Seeable (two or more phases) Physical and Chemical Properties 2.3 - Physical Properties: Without changing one substance and turning it into another. Most physical properties can be identified from our senses. - Qualitative: Using 5 senses and no numerical value. - Quantitative:Involving numbers for measurement. - Chemical Properties: The ability of a substance to react to another substance to create a new substance. - Chemical reactions must take place to see a chemical property. Density 2.4 - Equations: - DxV=M - M/V=D - M/D=V - (Make sure when you get the volume(ex.10 by 3 by 6) make sure to multiply and for the end add a 3 because it’s cubed.) Physical and Chemical Changes 2.5 - Physical Change: No new substances, different form, and most likely reversible. - Chemical Change: Two substances react to create a new substance with new properties and most likely is irreversible. History of the Atom 2.6 - Democritus - Aristotle - John Dalton - J.J Thomson - Ernest Rutherford - made the foil - James Chadwick - Niels Bohr - made the model of the atom Structure of the Atom/Periodic Table 2.7 - Atoms are made up of 3 subatomic particles: protons, neutrons, and electrons. - Atoms are neutral due to the equal amount of protons and electrons. Drawing Atoms 2.8 - (Already know how to do this) Periodic Table Patterns 2.9 - Groups are down and up - Periods are across - Period = the amount of shells - Groups = the amount of valence electrons - Group 18 = will always have an equal amount of valence electrons. Counting Atoms 2.10 - H,O,F,Br,I,N,Cl are the diatomic elements. - If there is a comma in the chemical equation, that means it’s a mixture. If there is no comma, that means it’s a compound that is chemically bonded. - (ex. C2, HO) - C = 2 atoms - H = 1 atom Molecules? = 1 molecule - O = 1 atom Isotopes 2.11 - Isotope - An element atom with the same number of protons but different amounts of neutrons. - The elements that you see on the periodic table are the common version of that element. - The more neutrons, the heavier the isotope will be. - Isotopes of an element will have different weights, but the same chemical properties. - Can be identified by the element name and the new mass number or through standard atomic notation. - Carbon-14 is made from nitrogen and is converted to carbon-14 by using cosmic rays from the sun. - To turn back into its original element, it takes 5730 years. - It can break-down over time because of how radioactive it is. - We can see how old a thing is based on how much carbon-14 is in that thing. Ions 2.12 - A chemical reaction is from 2 substances that transfer electrons to create a new substance. - Most atoms are unstable, but are still neutral. - Ions are overly charged particles - The less electrons the elements need to lose or gain, means it’s going to be more reactive. - Group 18 will always remain unreactive because of its full valence shells of electrons. Climate Change 2.13 - Weather is day to day - Climate is long-term using patterns over years. - Greenhouse effect: When greenhouse gasses trap heat from the sun in the earth’s atmosphere. - Ice cores were used to see how much carbon dioxide was in the past. - We can see that ice cores showed us that the amount of CO2 has increased over the past 70 years. - How to know CO2 is human caused: Carbon reservoirs have different percentages for each of the 3 carbon isotopes. (isotopic fingerprint) - The things we burn are C12, not C14. - C14 does not come from fossil fuels. - Suess Effect: The amount of CO2 is increasing, but the ratio of carbon-14 is decreasing. The carbon that is increasing is C-12, which is the type of isotope that comes from burning fossil fuels.