The smallest particle of matter that still retains its properties is called an atom.
In the fifth century B.C., the Greek philosopher Democritus proposed that matter is composed of a finite number of discrete particles, named atomos (meaning uncuttable or indivisible)
Democritus
In 1808, John Dalton, built on ideas of Democritus, and formulated a precise definition of the building blocks of matter.
Dalton's model represented the atom as a featureless ball of uniform density.
John Dalton
This model is referred to as the "soccer ball" model.
DALTON'S ATOMIC THEORY
Dalton's Atomic Theory consisted of three parts:
Each element is composed of tiny indestructible particles called atoms.
All atoms of a given element are similar to one another, but different from atoms of other elements.
Atoms combine in simple, whole-number ratios to form compounds.
DISCOVERY OF THE ELECTRON
In 1897, J.J. Thomson performed experiments with a cathode ray tube. Negatively charged particles from cathode were pulled towards positively charged plate, anode, and allowed to pass through and be detected on a fluorescent screen.
In absence of a magnetic field, the cathode rays were not deflected.
In presence of a magnetic and electric fields, the cathode rays were deflected towards the positive plate, indicating a negative charge.
The cathode rays were later named electrons.
Based on these findings, Thomson proposed an atomic model composed of negatively charged electrons embedded in a uniform positively charged sphere.
This model is called the "plum pudding" model.
NUCLEAR MODEL OF THE ATOM
In 1910, Ernest Rutherford carried out a number of experiments to further probe the nature of the atom.
In these experiments he bombarded a thin sheet of gold foil with -particles (large, positively charged) emitted from a radioactive source.
The majority of the particles were observed to pass through undeflected or slightly deflected.
Some of the particles were observed to be deflected at large angles.
Few of the particles were observed to be turned back towards the direction they came from.
Thomson's model of the atom could not account for these results.
Based on these observations, Rutherford proposed a model of the atom consisting of a small, massive positive center (nucleus), surrounded by electrons in mostly empty space.
This model is called the nuclear model.
THE STRUCTURE OF THE ATOM
In 1932, James Chadwick discovered the existence of a second nuclear particle. This neutral particle was named neutron.
Current Model of the Atom:
The atom is an electrically neutral spherical entity.
It is composed of a positively charged center surrounded by negatively charged electrons.
The electrons (e) move rapidly through the atomic volume, held by the attractive forces to the nucleus.
The atomic nucleus consists of positively charged protons ( ) and neutrally charged neutrons ( ).
The modern atom consists of 3 subatomic particles:
TABLE 4.1 Subatomic Particles
Mass
Mass
Charge
proton
1.0073
neutron
1.0087
0
electron
0.00055
Mass Relationships in the Atom:
The number of protons in an atom determines its identity, and is called atomic number (Z).
In a neutral atom, the number of protons (+) are equal to the number of electrons ( - ).
Almost all the mass of the atom rests in the nucleus.
The number of protons and neutrons in an atom is called the mass number (A).
The number of neutrons in an atom can be determined by the difference between mass number (A) and atomic number (Z):
ELEMENTS & THE PERIODIC TABLE
The number of protons in an atom identify it as a particular element, and is called atomic number.
Elements are arranged on the periodic table according to their atomic number.
Over time some elements have been named for planets, mythological figures, minerals, colors, geographic locations and famous people. Some examples are shown below:
Element
Source of Name
Uranium
The planet Uranus
Titanium
Titans (mythology)
Chlorine
Chloros, "greenishyellow"(Greek)
Iodine
Ioeides, "violet" (Greek)
Magnesium
Magnesia, a mineral
Californium
California
Curium
Marie and Pierre Curie
The symbol for most elements is the one- or two-letter abbreviation of the name of the element. Only the first letter of an elements symbol is capitalized. If the symbol has a second letter, it is written as lowercase.
Co (cobalt)
CO(carbon and oxygen)
Although most of the symbols use letters from current names, some of the symbols of the elements are based on their Latin names.
K potassium (kalium)
Na sodium (natrium)
Fe iron (ferrum)
Some elements have formulas that are not single atoms. Seven of these elements have diatomic (2-atoms) molecules.
Hydrogen
Chlorine
Oxygen
Fluorine
Nitrogen
Bromine
Iodine
ELEMENTS & THE PERIODIC TABLE
Arrangement of elements based on their atomic masses was first proposed by the Russian chemist, Dmitri Mendeleev in 1869.
The elements are generally classified as metals, nonmetals and metalloids.
Metalloids are elements that possess some properties of metals and some of non-metals. The most important metalloids are silicon (Si) and germanium (Ge) which are used extensively in computer chips.
ELEMENTS & THE PERIODIC TABLE
The periodic table is composed of periods (rows) and groups or families (columns).
Elements in the same family have similar properties, and are commonly referred to by their traditional names.
Elements in groups 1-2 and 13-18 are referred to as main-group or representative elements.
Group 1 elements are called alkali metal. These are soft metals that are very reactive, and often react explosively with other elements.
Group 8 elements are called noble gases. These are un-reactive gases that are commonly used in light bulbs.
Group 7 elements are called halogens. These are the most reactive nonmetals, and occur in nature only as compounds.
Group 2 elements are called alkaline-earth metals. These metals are less reactive than alkali metals.
The group of metals in-between the main group elements are called the transition metals.
FORMATION OF IONS
When reacting, atoms often lose or gain electrons to form charged particles, called ions.
For example, when reacting, lithium atom (3 protons and 3 electrons) loses one electron to form a ion:
The charge of an ion is determined by the imbalance of the number of protons and electrons in the atom. Therefore, for lithium ion, the charge is determined as follows:
Similarly, when reacting, fluorine atom (9 protons and 9 electrons) gains an electron to form a ion:
Positive ions are called cations. Cations are formed when a neutral atom loses electrons.
Negative ions are called anions. Anions are formed when a neutral atom gains electrons.
In nature, cations and anions occur together so that matter remains charge-neutral. For example, in table salt, sodium cations ( ) occur together with chloride anions ( ).
Atoms of the same element that posseess different number of neutrons are called isotopes.
Isotopes of an element have the same atomic number (Z), but different mass number (A).
Ne-20
(90.48%)
Ne-21
(0.27%) Ne
Ne-22
(9.25%)
For a given element, the relative amount of each isotope in a naturally occurring sample of that element is always the same.
The mass of an atom is measured relative to the mass of a chosen standard (carbon-12 atom), and is expressed in atomic mass units (amu).
The average atomic mass of an element-called atomic mass- is the mass of that element's natural occurring isotopes weighted according to their abundance. Therefore the atomic mass of an element is closest to the mass of its most abundant isotope.
Examples:
Determine the number of protons, neutrons and electrons in .
Which two of the following are isotopes of each other?
Based on the information below, which is the most abundant isotope of boron (atomic mass )?
Isotope
Mass (amu)
10.0
11.0
CALCULATING ATOMIC MASSES FROM ISOTOPIC DATA
The atomic mass of an element can be calculated from the mass and abundance of its isotopes as shown below:
Examples:
Calculate the average atomic mass of silver from the following isotopic data:
Isotope
Mass (amu)
Abundance (%)
106.90509
51.84
108.90476
48.16
Atomic mass of
Calculate the average atomic mass of gallium from the following isotopic data:
Isotope
Mass (amu)
Abundance (%)
Ga-69
68.9256
60.11
Ga-71
70.9247
39.89
A fictitious element is composed of isotopes A and B with masses of 61.9887 and 64.9486 amu, respectfully. The atomic mass of the element is 64.52 amu. What can you conclude about the natural abundances of the two isotopes? Briefly explain your answer.