Atomic Theorists and their Contributions

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Presentation transcript:

Atomic Theorists and their Contributions ATOMIC THEORY Atomic Theorists and their Contributions

Atomic Theory: Timeline 460 BC: Democritus 1803: Dalton 1897: Thomson 1900: Planck 1909: Millikan 1911: Rutherford 1913: Bohr 1924: de Broglie 1927: Heisenberg

Democritus 460 BC another Greek philosopher student of Leucippus “atoms cannot be changed or destructed and everything we see is made of clusters of atoms” his ideas lacked experimental support because scientific testing was unknown at that time

John Dalton 1766-1844 English schoolteacher developed the first useful atomic theory of matter (in1803) Dalton’s atomic theory includes four main assumptions…

Dalton’s Atomic Theory 1. All elements are composed of tiny indivisible (cannot be separated) particles called atoms. Atoms of the same element are identical. Atoms of different elements are different. Atoms of different elements can physically mix together or can chemically combine with one another in simple whole number ratios to form compounds. 4. Chemical reactions occur when atoms are separated, joined, or rearranged. Atoms of one element, however, are never changed into atoms of another element as a result of a chemical reaction.

Dalton’s Table of Elements and their Combinations

Sir J.J. Thomson English physicist discovered the electron (in 1897) used a cathode-ray tube to show that there are particles smaller than atoms (electrons) created the “plum pudding model”

Thomson’s Plum Pudding Model atoms are made of a sphere which is positively charged, with negatively-charged electrons “swimming” in this sphere electrons = plums positive interior = pudding

Thomson’s Cathode Ray Experiment Thomson used cathode-ray tubes in his experiments: 1. gases under low pressure were sealed into glass tubes fitted at both ends with metal disks called electrodes 2. the electrodes were connected to a source of high-voltage electricity 3. one electrode, the anode, became positively charged; the other electrode, the cathode, became negatively charged 4. a glowing beam formed between the electrodes – this beam, which traveled from the cathode to the anode is called the cathode ray

Thomson’s Experiment (cont.) Thomson found that the cathode rays were attracted to the positively-charged metal plates – plates that were negatively-charged repelled the cathode rays Thomson knew that opposite charges attract and like charges repel SO he proposed that a cathode ray is a stream of tiny negatively-charged particles moving at high speed 7. these negatively-charged particles were then named electrons he concluded that electrons must be parts of the atoms of all elements by 1900, Thomson and others had determined that an electron’s mass is about 1/2000 the mass of a hydrogen atom

Ernest Rutherford in 1911, discovered the atomic nucleus a New Zealand physicist “atoms have a positively-charged nucleus which is surrounded by negatively-charged particles” suggested the so called planetary model, which claims electrons orbit the nucleus just like planets orbit the Sun performed his famous experiment with a thin golden foil

Rutherford’s Experiment aimed a beam of alpha particles (+ charge) at a sheet of gold foil surrounded by a fluorescent screen found that most of the particles passed through the foil with no deflection at all a few particles were greatly deflected CONCLUSION: most of the alpha particles pass through the gold foil because the atom is mostly empty space the mass and positive charge are concentrated in a small region of the atom called the nucleus particles that approach the nucleus closely are greatly deflected

Robert Millikan found the quantity of charge carried by an electron (in 1909) determined the ratio of the charge to the mass of an electron found the values for electron charge and mass (in 1916) American scientist performed the famous “oil-drop” experiment

Niels Bohr Danish physicist improved the “planetary model” by suggesting that electrons only orbit the nucleus in well-defined paths (in 1913) depicted the atom as a small, positively-charged nucleus surrounded by electrons in orbit “electrons travel in discrete orbits around the nucleus” electrons orbiting an atom can only exist at certain energy levels (distances) from the nucleus, not at continuous levels as might be expected from Rutherford’s model

Max Planck discovered the quantum nature of energy (in 1900) “energy does not flow in a steady continuum, but is delivered in discrete packets called quanta” “quantum” is the amount of energy for an electron to jump to an energy level

Werner Heisenberg discovered the “uncertainty principle” (in 1927) – we really don’t know where electrons are at any time electrons may exist in certain orbits (Bohr), but we cannot pinpoint where they will be at a certain time German physicist

Louis de Broglie discovered the wave nature of electrons – (in 1924) electrons act not only as a particle, but as a wave thus, electrons can have stable configurations in an orbit