chapter 21 nuclear chemistry

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Prentice Hall © 2003 Chapter 21 Chapter 21 Chapter 21 Nuclear Chemistry Nuclear Chemistry CHEMISTRY The Central Science 9th Edition David P. White

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CHEMISTRY The Central Science 9th Edition. Chapter 21 Nuclear Chemistry. David P. White. Radioactivity. Nuclear Equations Nucleons: particles in the nucleus: p + : proton n 0 : neutron. Mass number: the number of p + + n 0 . Atomic number: the number of p + . - PowerPoint PPT Presentation

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Page 1: Chapter 21 Nuclear Chemistry

Prentice Hall © 2003 Chapter 21

Chapter 21Chapter 21Nuclear ChemistryNuclear Chemistry

CHEMISTRY The Central Science

9th Edition

David P. White

Page 2: Chapter 21 Nuclear Chemistry

Prentice Hall © 2003 Chapter 21

Nuclear Equations• Nucleons: particles in the nucleus:

– p+: proton

– n0: neutron.

• Mass number: the number of p+ + n0.• Atomic number: the number of p+.• Isotopes: have the same number of p+ and different

numbers of n0.• In nuclear equations, number of nucleons is conserved:

23892U 234

90Th + 42He

RadioactivityRadioactivity

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Prentice Hall © 2003 Chapter 21

Nuclear Equations• In the decay of 131I an electron is emitted. We balancing

purposes, we assign the electron an atomic number of -1.• The total number of protons and neutrons before a

nuclear reaction must be the same as the total number of nucleons after reaction.

RadioactivityRadioactivity

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Prentice Hall © 2003 Chapter 21

Types of Radioactive Decay• There are three types of radiation which we consider:

-Radiation is the loss of 42He from the nucleus,

-Radiation is the loss of an electron from the nucleus, -Radiation is the loss of high-energy photon from the nucleus.

• In nuclear chemistry to ensure conservation of nucleons we write all particles with their atomic and mass numbers: 4

2He and 42 represent -radiation.

RadioactivityRadioactivity

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Prentice Hall © 2003 Chapter 21

Types of Radioactive Decay

RadioactivityRadioactivity

Page 6: Chapter 21 Nuclear Chemistry

Prentice Hall © 2003 Chapter 21

Types of Radioactive Decay

RadioactivityRadioactivity

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Prentice Hall © 2003 Chapter 21

Types of Radioactive Decay• Nucleons can undergo decay:

10n 1

1p+ + 0-1e- (-emission)

0-1e- + 0

1e+ 200 (positron annihilation)

10p+ 1

0n + 01e+ (positron or +-emission)

11p+ + 0

-1e- 10n (electron capture)

• A positron is a particle with the same mass as an electron but a positive charge.

RadioactivityRadioactivity

Page 8: Chapter 21 Nuclear Chemistry
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Neutron-to-Proton Ratio• The proton has high mass and high charge.• Therefore the proton-proton repulsion is large.• In the nucleus the protons are very close to each other.• The cohesive forces in the nucleus are called strong

nuclear forces. Neutrons are involved with the strong nuclear force.

• As more protons are added (the nucleus gets heavier) the proton-proton repulsion gets larger.

Patterns of Nuclear Patterns of Nuclear StabilityStability

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Neutron-to-Proton Ratio• The heavier the nucleus,

the more neutrons are required for stability.

• The belt of stability deviates from a 1:1 neutron to proton ratio for high atomic mass.

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Prentice Hall © 2003 Chapter 21

Neutron-to-Proton Ratio• At Bi (83 protons) the belt of stability ends and all nuclei

are unstable.– Nuclei above the belt of stability undergo -emission. An

electron is lost and the number of neutrons decreases, the number of protons increases.

– Nuclei below the belt of stability undergo +-emission or electron capture. This results in the number of neutrons increasing and the number of protons decreasing.

– Nuclei with atomic numbers greater than 83 usually undergo -emission. The number of protons and neutrons decreases (in steps of 2).

Patterns of Nuclear Patterns of Nuclear StabilityStability

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Radioactive Series• A nucleus usually undergoes more than one transition on

its path to stability.• The series of nuclear reactions that accompany this path

is the radioactive series.• Nuclei resulting from radioactive decay are called

daughter nuclei.

Patterns of Nuclear Patterns of Nuclear StabilityStability

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Radioactive SeriesFor 238U, the first decay is to 234Th (-decay). The 234Th undergoes -emission to 234Pa and 234U. 234U undergoes -decay (several times) to 230Th, 226Ra, 222Rn, 218Po, and 214Pb. 214Pb undergoes -emission (twice) via 214Bi to 214Po which undergoes -decay to 210Pb. The 210Pb undergoes -emission to 210Bi and 210Po which decays () to the stable 206Pb.

Patterns of Patterns of Nuclear StabilityNuclear Stability

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Further Observations• Magic numbers are nuclei with 2, 8, 20, 28, 50, or 82

protons or 2, 8, 20, 28, 50, 82, or 126 neutrons.• Nuclei with even numbers of protons and neutrons are

more stable than nuclei with any odd nucleons.• The shell model of the nucleus rationalizes these

observations. (The shell model of the nucleus is similar to the shell model for the atom.)

• The magic numbers correspond to filled, closed-shell nucleon configurations.

Patterns of Nuclear Patterns of Nuclear StabilityStability

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Using Charged Particles• Nuclear transmutations are the collision between nuclei.• For example, nuclear transmutations can occur using high

velocity -particles:14N + 4 17O + 1p.

• The above reaction is written in short-hand notation: 14N(,p)17O.

• To overcome electrostatic forces, charged particles need to be accelerated before they react.

Nuclear TransmutationsNuclear Transmutations

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Using Charged Particles• A cyclotron consists of D-shaped electrodes (dees) with a

large, circular magnet above and below the chamber.• Particles enter the vacuum chamber and are accelerated

by making he dees alternatively positive and negative.• The magnets above and below the dees keep the particles

moving in a circular path.• When the particles are moving at sufficient velocity they

are allowed to escape the cyclotron and strike the target.

Nuclear TransmutationsNuclear Transmutations

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• 90Sr has a half-life of 28.8 yr. If 10 g of sample is present at t = 0, then 5.0 g is present after 28.8 years, 2.5 g after 57.6 years, etc. 90Sr decays as follows

9038Sr 90

39Y + 0-1e

• Each isotope has a characteristic half-life.• Half-lives are not affected by temperature, pressure or

chemical composition.• Natural radioisotopes tend to have longer half-lives than

synthetic radioisotopes.

Rates of Radioactive Rates of Radioactive DecayDecay

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Rates of Radioactive Rates of Radioactive DecayDecay

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• Half-lives can range from fractions of a second to millions of years.

• Naturally occurring radioisotopes can be used to determine how old a sample is.

• This process is radioactive dating.

Rates of Radioactive Rates of Radioactive DecayDecay

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Dating• Carbon-14 is used to determine the ages of organic

compounds because half-lives are constant.• We assume the ratio of 12C to 14C has been constant over

time.• For us to detect 14C the object must be less than 50,000

years old.• The half-life of 14C is 5,730 years.• It undergoes decay to 14N via -emission:

146C 14

7N + 0-1e

Rates of Radioactive Rates of Radioactive DecayDecay

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Calculations Based on Half Life• Radioactive decay is a first order process:

• In radioactive decay the constant, k, is the decay constant.• The rate of decay is called activity (disintegrations per

unit time).

• If N0 is the initial number of nuclei and Nt is the number of nuclei at time t, then

Rates of Radioactive Rates of Radioactive DecayDecay

kNRate

ktNNt

0ln

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Calculations Based on Half Life

• With the definition of half-life (the time taken for Nt = ½N0), we obtain

Rates of Radioactive Rates of Radioactive DecayDecay

21693.0t

k

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• Matter is ionized by radiation.• Geiger counter determines the amount of ionization by

detecting an electric current.• A thin window is penetrated by the radiation and causes

the ionization of Ar gas.• The ionized gas carried a charge and so current is

produced.• The current pulse generated when the radiation enters is

amplified and counted.

Detection of Detection of RadioactivityRadioactivity

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Detection of Detection of RadioactivityRadioactivity

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Radiotracers• Radiotracers are used to follow an element through a

chemical reaction.• Photosynthesis has been studied using 14C:

• The carbon dioxide is said to be 14C labeled.

Detection of Detection of RadioactivityRadioactivity

614CO2 + 6H2O 14C6H12O6 + 6O2sunlightchlorophyll

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• Einstein showed that mass and energy are proportional:

• If a system loses mass it loses energy (exothermic).• If a system gains mass it gains energy (endothermic).• Since c2 is a large number (8.99 1016 m2/s2) small

changes in mass cause large changes in energy.• Mass and energy changed in nuclear reactions are much

greater than chemical reactions.

Energy Changes in Energy Changes in Nuclear ReactionsNuclear Reactions

2mcE

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E 23892U 234

90Th + 42He

– for 1 mol of the masses are

238.0003 g 233.9942 g + 4.015 g.

– The change in mass during reaction is

233.9942 g + 4.015 g - 238.0003 g = -0.0046 g.

– The process is exothermic because the system has lost mass.

– To calculate the energy change per mole of 23892U:

Energy Changes in Energy Changes in Nuclear ReactionsNuclear Reactions

J 101.4

kg 100046.0m/s 109979.2

11

328

22

mcmcE

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Nuclear Binding Energies• The mass of a nucleus is less than the mass of their

nucleons.• Mass defect is the difference in mass between the nucleus

and the masses of nucleons.• Binding energy is the energy required to separate a

nucleus into its nucleons.• Since E = mc2 the binding energy is related to the mass

defect.

Energy Changes in Energy Changes in Nuclear ReactionsNuclear Reactions

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Nuclear Binding Energies• The larger the binding energy the more likely a nucleus

will decompose.• Average binding energy per nucleon increases to a

maximum at mass number 50 - 60, and decreases afterwards.

• Fusion (bringing together nuclei) is exothermic for low mass numbers and fission (splitting of nuclei) is exothermic for high mass numbers.

Energy Changes in Energy Changes in Nuclear ReactionsNuclear Reactions

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• Splitting of heavy nuclei is exothermic for large mass numbers.

• During fission, the incoming neutron must move slowly because it is absorbed by the nucleus,

• The heavy 235U nucleus can split into many different daughter nuclei, e.g.

10n + 238

92U 14256Ba + 91

36Kr + 310n

releases 3.5 10-11 J per 235U nucleus.

Nuclear FissionNuclear Fission

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• For every 235U fission 2.4 neutrons are produced.• Each neutron produced can cause the fission of another

235U nucleus.• The number of fissions and the energy increase rapidly.• Eventually, a chain reaction forms.• Without controls, an explosion results.• Consider the fission of a nucleus that results in daughter

neutrons.

Nuclear FissionNuclear Fission

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• Each neutron can cause another fission.• Eventually, a chain reaction forms.• A minimum mass of fissionable material is required for a

chain reaction (or neutrons escape before they cause another fission).

• When enough material is present for a chain reaction, we have critical mass.

• Below critical mass (subcritical mass) the neutrons escape and no chain reaction occurs.

Nuclear FissionNuclear Fission

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• At critical mass, the chain reaction accelerates.• Anything over critical mass is called supercritical mass.• Critical mass for 235U is about 1 kg.• We now look at the design of a nuclear bomb.• Two subcritical wedges of 235U are separated by a gun

barrel.• Conventional explosives are used to bring the two

subcritical masses together to form one supercritical mass, which leads to a nuclear explosion.

Nuclear FissionNuclear Fission

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Nuclear Reactors• Use fission as a power source.• Use a subcritical mass of 235U (enrich 238U with about 3%

235U).

• Enriched 235UO2 pellets are encased in Zr or stainless steel rods.

• Control rods are composed of Cd or B, which absorb neutrons.

Nuclear FissionNuclear Fission

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Nuclear Reactors• Moderators are inserted to slow

down the neutrons.• Heat produced in the reactor

core is removed by a cooling fluid to a steam generator and the steam drives an electric generator.

Nuclear FissionNuclear Fission

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• Light nuclei can fuse to form heavier nuclei.• Most reactions in the Sun are fusion.• Fusion products are not usually radioactive, so fusion is a

good energy source.• Also, the hydrogen required for reaction can easily be

supplied by seawater.• However, high energies are required to overcome

repulsion between nuclei before reaction can occur.

Nuclear FusionNuclear Fusion

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• High energies are achieved by high temperatures: the reactions are thermonuclear.

• Fusion of tritium and deuterium requires about 40,000,000K:

21H + 3

1H 42He + 1

0n

• These temperatures can be achieved in a nuclear bomb or a tokamak.

Nuclear FusionNuclear Fusion

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• A tokamak is a magnetic bottle: strong magnetic fields contained a high temperature plasma so the plasma does not come into contact with the walls. (No known material can survive the temperatures for fusion.)

• To date, about 3,000,000 K has been achieved in a tokamak.

Nuclear FusionNuclear Fusion

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• The penetrating power of radiation is a function of mass.• Therefore, -radiation (zero mass) penetrates much

further than -radiation, which penetrates much further than -radiation.

• Radiation absorbed by tissue causes excitation (nonionizing radiation) or ionization (ionizing radiation).

• Ionizing radiation is much more harmful than nonionizing radiation.

Biological Effects of Biological Effects of RadiationRadiation

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• Most ionizing radiation interacts with water in tissues to form H2O+.

• The H2O+ ions react with water to produce H3O+and OH.

• OH has one unpaired electron. It is called the hydroxy radical.

• Free radicals generally undergo chain reactions.

Biological Effects of Biological Effects of RadiationRadiation

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Radiation Doses• The SI unit for radiation is the becquerel (Bq).• 1 Bq is one disintegration per second.• The curie (Ci) is 3.7 1010 disintegrations per second.

(Rate of decay of 1 g of Ra.)• Absorbed radiation is measured in the gray (1 Gy is the

absorption of 1 J of energy per kg of tissue) or the radiation absorbed dose (1 rad is the absorption of 10-2 J of radiation per kg of tissue).

Biological Effects of Biological Effects of RadiationRadiation

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Radiation Doses• Since not all forms of radiation have the same effect, we

correct for the differences using RBE (relative biological effectiveness, about 1 for - and -radiation and 10 for radiation).

• rem (roentgen equivalent for man) = rads.RBE• SI unit for effective dosage is the Sievert (1Sv =

RBE.1Gy = 100 rem).

Biological Effects of Biological Effects of RadiationRadiation

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Radon

• The nucleus 22286Rn is a product of 238

92U.

• Radon exposure accounts for more than half the 360 mrem annual exposure to ionizing radiation.

• Rn is a noble gas so is extremely stable.• Therefore, it is inhaled and exhaled without any chemical

reactions occurring.• The half-life of is 3.82 days.

Biological Effects of Biological Effects of RadiationRadiation

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Radon• It decays as follows:

22286Rn 218

84Po + 42He

• The -particles produced have a high RBE.• Therefore, inhaled Rn is thought to cause lung cancer.• The picture is complicated by realizing that 218Po has a

short half-life (3.11 min) also:218

84Po 21482Pb + 4

2He

Biological Effects of Biological Effects of RadiationRadiation

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Radon• The 218Po gets trapped in the lungs where it continually

produces -particles.• The EPA recommends 222Rn levels in homes to be kept

below 4 pCi per liter of air.

Biological Effects of Biological Effects of RadiationRadiation

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End of Chapter 21End of Chapter 21Nuclear ChemistryNuclear Chemistry