Science Chemistry - Atomic Structure Yr10

Year 10 Chemistry unit - looking at:Atomic Structure
Electronic StructureChemical BondingMacro Molecules

9 cards   |   Total Attempts: 189
  

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What is the atomic mass
The atomic mass is the weight of and element. Calculated by the total mass of protons and neutrons(as electrons weight 2000 times less than either)
What is the atomic numberwhat does this, combined with the atomic mass allow us to calculate?
The atomic number is the neutron number.As the number of neutrons is equal to the number of protons, we therefore know the number of electrons. also, this means that: the atomic mass - the atomic number = number of neutrons
What is an isotope
An isotope is where the element has the same electronic configuration as usual, but the mass has changed (due to a different number of protons)
What is the top number of an isotope, and what it the bottom number
The top number is always the bigger of the two - the atomic mass (this is what changes in different isotopes)the bottom number is the atomic number which remains the same
What is the relative atomic mass of an element?How do we calculate it?
This is taking into account all of the isotopes f that element, and forming a new mass. E.g.To calculate the relative atomic mass we see:
. Ar Ag = 107 + 109 = 108 2 Ar Br = 79 + 81 = 80 2
Define relative atomic mass:
THE RELATIVE ATOMIC MASS OF AN ELEMENT, IS THE MASS OF AN ATOM OF THIS ELEMENT, COMPARED WITH THE MASS OF ONE ATOM OF CARBON ISOTOPE 12 (12C). (WHICH HAS A MASS OF 12.000 EXACTLY).
What is the difference between a stable and non stable isotope?
Non-stable isotopes are radioactive. Nucleus will split up and give off subatomic energy.From element 84 in the periodic table, ALL ELEMENTS ARE THEN RADIOACTIVE.
How log does it take an atom to decay?
The time taken for half the atoms in the sample to decay is a constant property of the isotope. This property is called the half life t½.What it means is this. If I have a sample of 14C, then after t½ , half the atoms present will have decayed. After a further t½ half of the remaining atoms will have also decayed, and so on. This means that t½ does not depend on the number of atoms in the sample. Whatever this is, half of them will have decayed after t½. For example 14C has t½ = 5730 years. This is very convenient for archeologists, who use 14C dating as a way of finding the age of objects they find. (For instance the Shroud of Turin was proved to be a medieval cloth by carbon dating).
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