Development of Atomic Model
Development of Atomic Model
460 BC: Democritus
Proposed the concept of atoms as tiny, indivisible spheres.
Introduced the idea that atoms could not be broken down further.
1804: John Dalton
Agreed with Democritus' idea of atoms as tiny, hard structures.
Proposed that each element is composed of different types of atoms, which are distinct and combine in fixed ratios to form compounds.
1897: J.J. Thomson
Discovered electrons, which led to revisions of Dalton's model.
Suggested a new model where atoms consist of a positively charged 'cloud' with negatively charged electrons ('Plum Pudding Model').
1909: Ernest Rutherford
Conducted the Rutherford Scattering Experiment, which involved shooting alpha particles at a thin gold foil.
Conclusions from the experiment:
Conclusion 1: Most alpha particles passed straight through, suggesting atoms are mainly empty space.
Conclusion 2: A small number of particles were deflected backwards , indicating the presence of a dense, positively charged nucleus.
Conclusion 3: Further movement of alpha particles at large angles hinted at a concentrated mass within the atom.
1913: Niels Bohr
Developed the Bohr Model that suggested electrons orbited the nucleus at specific energy levels (or shells) and could jump between levels.
Atoms remain stable because electrons in these shells do not spiral into
1933: Rutherford and James Chadwick
Chadwick proved the existence of neutrons, completing the understanding of protons, neutrons, and electrons in the atomic structure.
Illustrated that the atomic nucleus contains protons (positive charge) and neutrons (neutral) with electrons in shells around the nucleus.
Current Model of the Atom
Structure of the Atom
Nucleus: Contains protons and neutrons.
Positive charge due to protons.
Very dense.
Electrons: Carry a negative charge and occupy energy levels or shells around the nucleus.
Atoms have a significant amount of empty space between the nucleus and electrons.
Behaviour of Electrons
Electrons can gain energy by absorbing electromagnetic (EM) radiation, moving to higher energy levels further from the nucleus.
When releasing energy, they move to lower levels and emit EM radiation.
Isotopes
Isotopes are defined as two elements having the same number of protons and electrons but differing in the number of neutrons.
Isotopes of an element have unique mass numbers (total protons + neutrons).
Radioactive Decay
Types of Radioactive Decay
1. Alpha Decay
Alpha Particles: alpha particle emitted from nucleus
Composed of 2 protons and 2 neutrons.
Highly ionising but low penetration ability; can be stopped by paper.
Often used in smoke detectors due to their ability to ionize air and create a current.
2. Beta Decay
Beta Particles: High-speed electrons emitted from the nucleus.
Medium ionisation and penetration capabilities; can be stopped by thin sheets of aluminium.
In beta decay, a neutron is transformed into a proton, emitting a beta particle.
3. Gamma Decay
Gamma Rays: High-energy electromagnetic waves emitted from a nucleus.
Have no mass and can penetrate effectively; most penetrating type of radiation.
Stopped only by thick sheets of lead.
Summary of Radiation Characteristics
Alpha Radiation:
Symbol: \alpha
Composition: 2 protons, 2 neutrons
Low penetration, highly ionizing.
Beta Radiation:
Symbol: \beta
Composition: 0 protons, 0 neutrons
Moderate penetration, medium ionizing.
Gamma Radiation:
Symbol: \gamma
Composition: 0 protons, 0 neutrons
Highest penetration, least ionizing.
Nuclear Decay Equations
Alpha Decay Equation
A \rightarrow A-4 \text{ , } Z \rightarrow Z-2 + \text{He}^{2+} $$
Example:
^{226}{88} \text{Ra} \rightarrow ^{222}{86} \text{Rn} + \text{He}^{2+}
Beta Decay Equation
A \rightarrow A \text{ , } Z \rightarrow Z+1
Example:
^{14}{6} \text{C} \rightarrow ^{14}{7} \text{N} + \beta
Gamma Decay Equation
A \rightarrow A \text{ , } Z \rightarrow Z
Example:
^{234}{90} \text{Th} \rightarrow ^{234}{90} \text{Th} + \gamma $$
Radioactive Decay Characteristics
Decay Characteristics
Radioactive decay is spontaneous and cannot be controlled; it is impossible to predict which nucleus will decay next.
Half-life: The time taken for half of the radioactive nuclei in a sample to decay.
Activity is measured in Becquerels (Bq) where 1 Bq = 1 decay per second.
Short half-life isotopes present high initial activity, rapidly decaying and potentially leading to dangerous exposure to radiation.
Long half-life isotopes decay slowly, maintaining lower activity levels over extended periods, posing a risk due to prolonged exposure.
Background Radiation
Sources of Background Radiation
Naturally occurring radioactive substances (rocks, soil, food).
Cosmic rays originating from outer space.
Human activities (nuclear explosions, medical treatment).
Radiation Exposure and Protection
To mitigate the effects of radiation exposure, strategies include:
Keeping radioactive sources in lead-lined boxes.
Using physical barriers and maintaining distance from radioactive materials.
Wearing protective gear (gloves, gowns) when handling radioactive substances.
Contamination vs. Irradiation
Contamination occurs when radioactive materials make contact and attach to an object or person.
Dangerous because it can introduce radioactive particles internally.
Methods to reduce contamination risks:
Use of gloves and protective suits.
Irradiation refers to exposure to radiation without direct contact with radioactive substances, such as radiation from external sources.
Effects of Radiation
Biological Effects
High doses of radiation can kill cells, while lower doses may cause changes leading to uncontrolled cell growth or cancer.
Symptoms of radiation exposure can include vomiting and fatigue, commonly termed radiation sickness.
Applications of Radioactivity
Medical Uses
Radioactive isotopes can be ingested to track bodily functions (e.g., Iodine-123 for thyroid imaging).
Radiotherapy: High doses of radiation are used to target and destroy cancer cells while trying to minimize damage to surrounding healthy tissues.
Gamma rays are typically employed due to their penetration depth.
Nuclear Reactions
Nuclear Fission
Definition: The process of splitting a nucleus into smaller nuclei, releasing energy.
A neutron collides with a nucleus,make nuclei unstable, splits into two , neutrons are released & process restarts.
Chain Reaction: Some released neutrons can initiate further fission events, making it possible to sustain a reaction and release large amounts of energy.
Control of nuclear fission reactions can be achieved by using absorbent materials that capture neutrons.
Nuclear Fusion
Definition: The joining or combining of smaller nuclei to form a larger, heavier nucleus, such as fusing hydrogen nuclei to create helium.
Fusion releases significantly more energy than fission.
Challenges of achieving fusion include the need for high temperatures and pressures to overcome e the repulsion