Lecture Notes: Atoms, Conservation Laws, and Isotopes

What is an Atom?

  • Originally thought of as the smallest, indivisible unit of matter.
  • 99.9999% empty space.
  • Currently, 118 known atoms, potentially more stable ones up to around 126.
  • Changing chemical composition involves rearrangement of atoms.
  • Originally, there was no method to determine the size or appearance of an atom or identify individual elements.

Conservation Laws in Chemical Reactions

  • During a chemical reaction, mass cannot be created or destroyed (Law of Conservation of Mass).
  • Proposed by scientists through observation of elements combining, noting no mass change during heating.
  • Consistent Mixture of Components: When materials are made, the ratio of components is consistent.
  • Proust's experiment with copper carbonate showed that lab-made and naturally occurring samples have the same composition.
  • Chemical synthesis has multiple pathways to a product, but the final composition remains the same.
  • Ratios were originally worked out based on mass (e.g., water as a one:eight ratio of hydrogen to oxygen).

Law of Definite Proportions

  • If a substance contains specific amounts of elements, the same ratio applies even with different masses.
  • Example provided: Given 2 grams of a substance with 0.93 grams of iron and 1.07 grams of sulfur, calculate the amount of sulfur in 4.19 grams of iron in the same material based on proportion.
  • Application: Determining how much iron can be extracted from a ton of ore to estimate potential profit.

Dalton's Atomic Theory

  • Matter consists of tiny atoms, each unique for each element.
  • Atoms are considered indestructible (though nuclear fission can split them).
  • Changing material nature involves rearranging atom interactions.
  • In a pure element, all atoms are identical (with caveats).
  • Atoms of different elements differ in mass.
  • Atoms combine in consistent ratios (e.g., H2O, O2, O3).

Shorthand Notation in Chemistry

  • Chemists use chemical equations as shorthand notation.
  • Starting materials (reactants) are on the left, products on the right, with an arrow indicating the transformation.
  • Symbols for elements (H for hydrogen, O for oxygen), some Greek in origin (Pb for lead - plumbonium)

Importance of Chemical Grammar

  • Position of numbers (subscripts and superscripts) is critical.
  • O2 indicates two oxygen atoms joined together, while 2O indicates two individual oxygen atoms.
  • Chemical equations must be balanced, reflecting the conservation of mass.
  • Example: Splitting water (H2O) to form hydrogen (H2) and oxygen (O2) requires balancing: 2H<em>2O2H</em>2+O22H<em>2O \rightarrow 2H</em>2 + O_2

Anomalies and Further Investigations

  • Sulfur dioxide (SO2) is a gas, while sulfur trioxide (SO3) is a solid, suggesting different atomic arrangements.
  • In SO2, one gram of sulfur interacts with one gram of oxygen, while in SO3, the ratio is one:1.5.
  • Different properties indicate that the arrangement of atoms affects chemical properties.

Discoveries Regarding the Atom's Structure

  • Experiments showed that something could change photographic plates at a distance, suggesting the atom is not the end-all.
  • Cathode ray experiments showed the emission of negatively charged particles (electrons) from a heated source.
  • If negatively charged particles are ejected from an atom, what remains must be positively charged to maintain electrical neutrality.

Atomic Models

  • Plum Pudding Model: original belief that the atom was basically a pudding and the positive charges were spread out in there and the electrons were spread out in there.

Millikan's Oil Drop Experiment

  • In 1909, Millikan calculated the charge on an electron: 1.5924×10191.5924 \times 10^{-19} coulombs (current value is 1.6×10191.6 \times 10^{-19} coulombs).
  • The mass of an electron is 103110^{-31} kg.

Rutherford's Gold Foil Experiment

  • Alpha particles fired at a thin gold foil.
  • Most particles passed straight through, but a small fraction (0.0125%) bounced back.
  • This suggested that all positive charge is concentrated in the middle of the atom, with the rest being empty space.
  • The electrons orbit the nucleus like planets around the sun (although quantum mechanics provides a more nuanced picture).

Composition of the Nucleus

  • The nucleus contains positively charged protons.
  • To balance the mass, there must also be neutrons.
  • Atoms are made up of electrons, protons, and neutrons.
  • Electrons are in different levels, which is significant because electrons in an atom are different depending on where they actually are.
  • The mass of the neutron and the mass of the proton is pretty much exactly the same.

Atomic Mass

  • Carbon is the element of life. It crops up everywhere.
  • Atomic mass is defined relative to carbon, with carbon-12 assigned a mass of 12.
  • This simplifies calculations, as it's easier to work with 12 rather than 102710^{-27}.
  • Atomic number (Z) is the number of protons in the nucleus; mass number (A) is the total number of protons and neutrons.
  • For oxygen (atomic number 8), the mass number is typically 16 (8 protons + 8 neutrons).

Isotopes

  • Different forms of the same element with varying numbers of neutrons.
  • Hydrogen exists as hydrogen, deuterium (one neutron), and tritium (two neutrons).
  • Isotopes have different chemical properties (e.g., deuterium oxide (D2O) is denser than H2O).
  • Most elements have multiple isotopes, making calculation of molecular weight complex.

Carbon Isotopes Example

  • Carbon-12 (six protons, six neutrons) is the standard.
  • Carbon-13 (six protons, seven neutrons) is used in resonance spectroscopy.
  • Carbon-14 (six protons, eight neutrons) is radioactive and used for radiodating.

Atomic Mass Units (amu)

  • Defined based on carbon-12.
  • One amu is one-twelfth of the mass of carbon-12.
  • The actual atomic weight of carbon is 12.0107 due to the presence of carbon-13.

Practical Importance

  • Knowing the exact mass of materials is crucial for chemical synthesis.
  • Calculations must account for the contribution of each isotope to the overall mass of an element.