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Chapter 4 Atomic Structure Section 4.1, Studying Atoms Timeline of Atomic Models Ancient Greek Models of Atoms About 540 B.C., the Greek scientist Democritus proposed the first model of the atom. All matter is made of small invisible, indivisible particles called atomos, which later became our word atom. His theory was rejected by the Greek scientific community. Section 4.1, Studying Atoms Timeline of Atomic Models John Dalton’s Atomic Theory (1803) Dalton was an English scientist born in 1766. Section 4.1, Studying Atoms Timeline of the Atomic Model Dalton’s atomic theory had four main parts 1. All Elements are composed of atoms. 2. All atoms of the same atom have the same mass and different elements have different masses. 3. Compounds contain elements of more than one type of atom. Section 4.1, Studying Atoms Timeline of the Atomic Model Dalton’s atomic theory (continued) 4. In a particular compound, atoms of different elements always combine in the same proportion (ratio). Also known as the law of definite proportions. Daltons model of the atom was a sphere. He was not sure how the spheres (atoms) were connected, but knew that they did combine in definite ratios or proportions. Section 4.1, Studying Atoms Timeline of the Atomic Model J. J. Thomason Model (1909) J.J. Thomason (1856 – 1940), an English born scientist developed a model of the atom composed of positively and negatively charged particles. He had a partner named Nagayoka which your book doesn’t mention. Section 4.1, Studying Atoms J.J. Thomason Model (1909) Thomason’s model showed us the following: 1. Atoms were made of smaller (subatomic particles. 2. The sub-atomic particles carried positive and negative charges. 3. Overall atomic charge is neutral. 4. Negative charges balance the positive charges. Thomason-Nagaoka Model 1909 Section 4.1, Studying Atoms J.J. Thomason Model (1909) Thomason had the nucleus (positively charged area) and the electrons (negatively charged particles) in one spherical mass. The model had several nicknames: The Plum Pudding Model, The Watermelon Model, and The Raisin Cookie Model. Section 4.1, Studying Atoms Rutherford’s Atomic Theory (1911) Ernest Rutherford was an Australian born physicist. His first major discovery was the alpha particles given off in the radioactive decay of Uranium. Alpha particles are very small and consist of 2 protons and 2 neutrons (a helium nucleus) and carry a positive charge. Section 4.1, Studying Atoms Rutherford’s Atomic Theory It shows that there is a lot of empty space in atoms between the nucleus and electrons. It also (unlike Thomason-Nagaoka) places the electrons outside the nucleus. The Gold Foil Experiment Rutherford used Polonium (Po), another radioactive substance to direct a beam of alpha (α) particles at a thin sheet of gold foil. Section 4.1, Studying Atoms The Gold Foil Experiment (continued) Rutherford predicted that the mass and charge of the gold atoms in the foil would not be great enough to deflect the α particles and they would travel straight through. As the diagram shows, many of the alpha particles were deflected to varying degrees. Rutherford felt that the deflection was caused by the α particles coming close to a positively charged particle. Section 4.1, Studying Atoms The Gold Foil Experiment (Continued) This evidence led Rutherford to the following conclusions: Deflected α particles had come close to a positively charged particle. + and – charges are not equally distributed in an atom. The nucleus is dense and positively charged. Electrons are located outside the nucleus. Notice, that in Rutherford’s Atomic Model, the electrons (negatively charged particles) are located outside the nucleus, located in the center of the atom. Section 4.1, Studying Atoms The Gold Foil Experiment (Continued) From the time of Democritus (540 BC) to The Gold Foil Experiment (1911), we have the classical development and study of our atomic model. From this point forward, we will study modern atomic theory, which will begin with Neils Bohr (a student of Rutherford’s), but first we will learn of a few of the sub-atomic particles that we have discovered. Section 4.2, The Structure of an Atom Properties of Sub-Atomic Particles (cont) The three sub-atomic particles we will study are: Protons, Neutrons, and Electrons. Electrons charged (-1 per electron e-) Found outside the nucleus Low mass low density particles Outer e- are involved in chemical bonding Negatively Section 4.2, The Structure of an Atom Properties of Sub-Atomic Particles Protons charged (+1 per proton p+) Found in the nucleus of the atom Very dense, high mass particles (equal to the density/mass of a neutron) Positively Section 4.2, The Structure of an Atom Properties of Sub Atomic Particles (cont.) Neutrons Carries a “0” or neutral charge (symbol n) Found inside the nucleus Very dense, high mass particle Discovered by the English physicist James Chadwick in 1932. Differences in numbers of neutrons in the same type of atoms account for isotopes. Section 4.2, The Structure of an Atom Section 4.2, The Structure of an Atom Section 4.2, The Structure of an Atom Atomic Number and Mass Number Atomic Number The atomic number of an atom equals the number of protons in its nucleus. Atoms of the same element have the same number of protons. Each proton has a charge of +1. The number of protons is balanced by an equal number of electrons, giving the atom an overall charge of “0”. Section 4.2, The Structure of an Atom Atomic Number and Mass Number (cont.) Mass Number The mass number of an atom is the sum of the number of protons and neutrons in the nucleus (#Protons + #Neutrons = Mass #) All atom of an element must have the same number of protons, but they can have different numbers of neutrons. Most mass numbers are fractional due to the presence of isotopes. Section 4.2, The Structure of an Atom Atomic Number and Mass Number (cont.) Isotopes Isotopes are atoms of a specific element with the same number of protons and electrons, but different numbers of neutrons. Different isotopes have different mass numbers. Different isotopes can have different chemical and physical properties. Section 4.3, Modern Atomic Theory Bohr’s Neils Model of the Atom Bohr (1885 – 1962) was a former student of Ernest Rutherford. Unlike Rutherford’s model, Bohr’s model of the atom focused more on the electrons. Where individual electrons were located around the nucleus. How the electrons moved in their orbits. Section 4.3, Modern Atomic Theory Bohr’s Model of the Atom (1913) Bohr’s model had electrons in fixed orbitals (energy levels) around the nucleus. The Bohr model was sometimes referred to as the “Planetary Model”. Section 4.3, Modern Atomic Theory The Bohr Model of the Atom (1913) Energy levels closest to the nucleus are considered to be the lower energy levels and those farther away are higher energy levels. By absorbing or releasing energy, an electron can change its energy level Electrons can’t stay between energy levels. Section 4.3, Modern Atomic Theory Electron Cloud Model (also referred to as the Quantum-Mechanical Model). Electrons do not have fixed orbits as in the Bohr model. Electron movement is based on probable areas around the nucleus where electrons might be found (the electron cloud). Current Quantum-Mechanical Section 4.3, Modern Atomic Theory Atomic An Orbitals orbital is an area in space around an atomic nucleus in which an electron is most likely to be found. There are different types and shapes of orbitals. An electron cloud is a good approximation of how electrons behave in their orbits. Shape of a Typical S – Orbital Shapes of typical P - Orbitals Shape of Typical d - Orbitals Comparison s, p, andAtomic d Orbital Shapes Section 4.3,ofModern Theory Notice how each of the different orbitals have different shapes. Element Atomic Number Number of Electrons Number of Protons Atomic Mass Number of Neutrons Elemental Symbol Section 4.3, Modern Atomic Theory Section 4.3, Modern Atomic Theory Section 4.3, Modern Atomic Theory Electron Energy Levels and Configurations Electrons in the lowest energy levels have the least energy. When possible, electrons travel in pairs. The most stable electron configuration of an atom is when the outer orbital is filled. This is called the octet rule. The noble gases are an example of this rule. All atoms that don’t have complete outer orbits try to complete them by bonding with other atoms Flame Photometry Comparison of Protons, Neutrons and Electrons