the atomic theories
The atomic theory has evolved over time through several key stages:
Dalton's Atomic Theory (1803): John Dalton introduced the first scientific atomic theory, which stated:
Elements are made of atoms, which are indivisible and indestructible.
All atoms of a given element are identical in mass and properties.
Compounds are formed by a combination of different atoms.
A chemical reaction rearranges atoms.
Thomson's Model (1897): J.J. Thomson discovered the electron and proposed the "plum pudding" model, the cathode ray tube experiment, suggesting that atoms were a uniform sphere of positive charge with scattered electrons.
Rutherford's Model (1911): Ernest Rutherford conducted the gold foil experiment, leading to the nuclear model of the atom, where most of the mass is concentrated in a small, dense nucleus, surrounded by orbiting electrons.
Bohr Model (1913): Niels Bohr refined Rutherford's model by introducing quantized orbits for electrons, explaining the stability of atoms and their emission spectra. higher the energy level faster the e- orbit.
Note: Chadwick discovered the neutrons.
neutron>proton>electron
the orbits around the nucleus are labeled as n=1, n=2, n=3… or K,L,M,N…
the n=1 orbit is called the ground state
an electron in the ground state has the lowest energy and the greatest stability.
the n=2 and higher states are called excited states.
electrons in the excited states have more energy but less stability.
more energy=greater distance from the nucleus
an electron that absorbs energy will move to a higher orbit
an electron that loses energy will move to a lower orbit