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1 Chapter 4: jectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass and charge; dissect the atom into its component parts; explain the role of atomic number in determining the identity of an atom; define an isotope and explain why atomic masses are not whole numbers; calculate the number of protons, electrons and neutrons in an atom given the mass number and atomic number; explain the relationship between unstable nuclei and radioactive decay; characterize alpha, beta, and gamma radiation in terms of mass and charge; interconnect the changes in the theory of the atom with the idea of the scientific method
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1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

Jan 21, 2016

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Piers Watkins
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Page 1: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Chapter 4:

Objectives: the student will be able to:

compare and contrast early atomic models; distinguish between subatomic particles in terms of mass and charge; dissect the atom into its component parts; explain the role of atomic number in determining the identity of an atom; define an isotope and explain why atomic masses are not whole numbers; calculate the number of protons, electrons and neutrons in an atom given the mass number and atomic number;explain the relationship between unstable nuclei and radioactive decay; characterize alpha, beta, and gamma radiation in terms of mass and charge;interconnect the changes in the theory of the atom with the idea of the scientific method

Page 2: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Dalton’s Atomic Theory (1808 A.D.)-very similar to ideas of Democritus (~400 B.C.)

• Each element is made up of tiny particles called atoms that can not be broken down into smaller particles.

• The atoms of a given element are identical; the atoms of different elements are different in some fundamental way or ways.

• Chemical compounds are formed when atoms combine with each other. A given compound always has the same relative numbers and types of atoms.

• Chemical reactions involve reorganization of the atoms - changes in the way they are bound together. The atoms themselves are not changed in a chemical reaction.

Page 3: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Cathode Ray: stream of charged particles produced by an electric field. The green “glow” in the picture.

The particles move from the cathode (negatively charged plate) to the anode (positively charged plate).

Page 4: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Cathode “rays” are influenced by both magnetic and electric fields (electric field shown in the diagram).

Opposite charges are known to attract each other. Since the cathode “ray” was deflected towards the positively charged plate,

what must the charge be of the particles in the cathode “ray”?

Page 5: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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The negatively charged particles produced by the electric field were named electrons.

J.J Thompson (~1890)-measured the charge to mass ratio of the electron. He discovered that an electron

must be smaller than the smallest known atom.

Whoops! There goes part of Dalton’s theory of the atom-an atom is not the smallest particle of matter.

However, Dalton was correct that an atom is the smallest particle of matter that can still be recognized

as a specific element.

Page 6: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Robert Millikan (1909)-measured the charge of an electron.

Knowing the charge to mass ratio of an electron from Thompson, Millikan can use the charge he has measured to calculate the mass of an electron!

Mass of e1 = 9.11X1028 g Mass of H atom = 1.676X1024 g

(1.676X1024 g)/(9.11X1028 g) = 1840

A Hydrogen atom is 1840 times more massive than an electron.

Page 7: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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After Thompson’s and Millikan’s work, a new “model” of an atom must be produced. In the old one an atom was much like a ball bearing because it was the same throughout.

The new model must: 1) allow electrons to be removed from the atom; 2) must explain why an atom is neutral; 3) must explain where most of the mass of an atom is located.

Plum Pudding Model:

Electrons are evenly distributed throughout a uniform positive charge equal to the negative

charge of all of the electrons. The part with the positive

charge is where most of the

mass of an atom is located.

Page 8: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Ernest Rutherford (1911) “gold foil” experiment

Large, high energy particles (alpha particles, +2 charge) do not always pass straight through a thin sheet of matter. The alpha particle being deflected or reflected is like having a 30-06 bullet bounce off of a sheet of tissue paper.

Page 9: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Rutherford’s experiment does not fit with the Plum Pudding Model (a) because not all of the alpha particles do not pass straight through.

Rutherford proposed a nuclear model of the atom.

The small, dense nucleus contains virtually all the mass of the atom and all of the positive charge while the negatively charged electrons exist apart from the nucleus (b).

How does this model fit Rutherford’s results?

Page 10: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Rutherford called the positive particle in the nucleus a proton.

In 1932, James Chadwick discovered a neutral particle in the nucleus and called it a neutron.

Summary of Subatomic Particles (mid 1900’s)

RelativeMass

1/1840~1~1

Page 11: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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If all atoms contain the same types of particles, what makes one atom hydrogen

and another carbon?

Nuclear Model of an Atom

The number of protons in the nucleus determine what element an atom is. Remember that in normal atoms, the

number of protons is equal to the number of electrons (they are neutral-a

total charge of zero).

How many times bigger is the atom compared to the nucleus? ______________

________________________________________________________________

Small, very dense nucleus containing massive protons and neutrons, surrounded by small rapidly moving electrons

Page 12: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Atomic Number:

Atomic number is the number of protons in the nucleus of an element. Since in neutral atoms the number of protons is equal to the number of electrons, atomic number also indicates the number of electrons in an element.

The Periodic Table is arranged according to atomic number.

For example, hydrogen is element 1 and has 1 proton in its nucleus.

Similarly, helium is element 2 and has 2 protons in its nucleus.

How many protons does element number 25 contain? What is the name of this element? How many electrons does element 25 contain? What is the charge of one atom of element 25?

Page 13: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Isotopes are atoms with the same number of protons (same element) but with a different number of neutrons.

Na-23 (11 + 12 = 23) Na-24 (11 + 13 = 24)

Page 14: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Mass Number:

Mass Number is the number of protons plus the number of neutrons in the nucleus of an atom.

Mass # = # Protons + # Neutrons

Remember: Atomic # = # Protons

Therefore: Mass # = Atomic # + # Neutrons

If you have Mass # and Atomic #, you can find # Neutrons.

From Algebra:a = b + c therefore if you are given a and b, you can find c using this equation: c = a b

Page 15: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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XAZ

Element Symbol

Mass Number

Atomic Number

# Neutrons = Mass # Atomic # or

# Neutrons = A Z

Since: Mass # = Atomic # + # Neutrons

Remember that the mass number must be the largest number in the problem!

X-A is another way to identify an isotope

Identifying Specific Isotopes

Page 16: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Examples: Three Isotopes of Carbon (atomic number = 6)

C126

C136 C14

6

How many Protons, Electrons, and Neutrons are in each atom?

C126

C136 C14

6

Protons

Electrons

Neutrons

6 6 6 From Atomic #

6 6 6 From Atomic #

6 7 8 Mass # Atomic #

C-12 C-13 C-14

Page 17: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Isotope Atomic # Mass # # Protons # Neutrons137Ba

14 14207 80

Use a periodic table to help you complete the following table.

Isotope Atomic # Mass # # Protons # NeutronsK-42

13 14207 82

Page 18: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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AMU: Atomic Mass Unit is a unit of mass based on 12C.

By Definition: the mass of one atom of 12C = 12 amu,

so 1 amu = 1/12 of the mass of one atom of 12C

On this scale, 1 proton = 1.007276 amu 1 neutron = 1.008668 amu 1 electron = 0.000549 amu

The Mass of “C” on the periodic table is 12.011 amu because pure carbon is made up of both 12C (12 amu exactly) and 13C (close to 13 amu).

The mass of “C” is a weighted average of all isotopes of C!

Page 19: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Weighted Average:

Average Mass = [(% abundance of isotope one)*(mass of isotope one)

+ (% abundance of isotope two)*(mass of isotope two)]

Average Mass of Mg: (78.99%)*(23.985 amu) + (10.00%)*(24.986 amu) + (11.01%)*(25.982 amu)

24.3049697 amu

24Mg25Mg26Mg

Isotope Abundance Mass

78.99%

10.00%

11.01%

23.985 amu

24.986 amu

25.982 amu

Data for the known isotopes of Magnesium

24.30 amu

Page 20: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Estimating the abundance of isotopes in an element.

The atomic mass (numbers in black beneath the element symbols on the periodic table in the classroom) are weighted averages of all stable isotopes of that element. If we know the atomic mass we can make a guess about which isotope may be most abundant.

Example: Carbon is 12.011 amu. Since this is very nearly 12, we would guest that most of the carbon atoms in the world are C-12 and that there is very little of other isotopes.

This method will not always work, but it can be used to get an idea.

If we know which isotopes are present in an element and its atomic mass, we can start to estimate the abundance of the isotopes.

Example: Cl-35 and Cl-37 are the only stable isotopes of chlorine. The atomic mass of Cl is 35.45 amu. Since 35.45 is closer to 35 than to 37, there is going to be a greater abundance of Cl-35 than of Cl-37.

Using math to estimate: 50%*35 + 50%*37 = 36 and 75%*35 + 25%*37 = 35.5

Page 21: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Hg20180 Tl201

81 e01+

Beta Decay (-particle is produced)

A high energy electron is a -particle

Cf25298 He4

2Cm24896 0

0+ +

Alpha Decay (-particle is produced)

A helium nucleus is an -particle

High energy “light” is -radiation

Gamma Radiation (-ray is produced)

Types of Radioactive decay: occur because the nucleus of an isotope is not stable.

Page 22: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Alpha Radiation has +2 charge and mass of 4 amu

Beta radiation has 1 charge and mass of (1/1840 amu)

Gamma radiation has 0 charge and mass of 0 amu

(+)

()

Electrically charged plates

Lead Block

Source of radiation is

inside.target screen

Why should we expect that beta would bend more than alpha?

Page 23: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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Radioactive decay is dangerous because the particles have very high energy compared to “normal” matter, and it damages “normal” matter when it hits it.

Gamma has the most energy and is the hardest to block out. It can penetrate several feet of concrete because it has no mass (it is really just a high energy form of “light”).

Beta has less energy than gamma but more that alpha. Because of its small mass, it can penetrate more matter than alpha does.

Alpha has the least energy of the three and can be blocked by just an inch or two of concrete. It has a large mass and will “hit” other atoms more easily than the much smaller beta particle.

The danger in being exposed to radiation increases as you are exposed to more and more of it. Too much can cause death quickly. Smaller amounts may cause cancer or other diseases.

Page 24: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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He42 W187

74

Zr9340

e01

Since nuclear reactions create and destroy atoms, we do not balance the number of atoms on both sides of the equation.

Nuclear Equations must balance mass number and atomic number!

+Os19176

+Nb9341

Examples:

Radioactive decay is a nuclear reaction and is not like chemical reaction!

Page 25: 1 Chapter 4: Objectives: the student will be able to: compare and contrast early atomic models; distinguish between subatomic particles in terms of mass.

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