Applications & Explore Online ആറ്റത്തിന്റെ ഘടന
The discharge tube of 1875 still lights up the neon signboards of a Kerala town at night. Cathode rays drew the pictures on the old TV at grandma's house. The isotopes ഐസോടോപ്പുകൾ of this chapter treat cancer at the Regional Cancer Centre in Thiruvananthapuram, tell archaeologists how old a piece of charcoal is, run nuclear power stations and find leaks in buried pipes. Every lab below uses only the ideas of this chapter. The page ends with radiation safety and a hub of links to explore online.
- A gas at low pressure conducts electricity at high voltage. Cathode rays (electrons) travel from the cathode, make a coating glow, and are deflected by electric and magnetic fields (page 4).
- Bohr: an electron that jumps to a higher orbit absorbs energy, and when it falls back it gives out energy (page 7).
- Isotopes have the same atomic number but different mass numbers. Some are radioactive റേഡിയോ ആക്ടീവത: they give out radiation by themselves (Table 1.6, page 10).
Parts marked go further are beyond the textbook. Enjoy them, but for the exam stick to the textbook ideas. All the animations are slowed down and simplified.
1. Glowing signboards, street lamps and tube lights
At night, the shops in a Kerala town light up with red-orange neon signs. A neon sign is a discharge tube ഡിസ്ചാർജ് ട്യൂബ്: a glass tube with an electrode at each end, filled with a little neon gas at low pressure, and run on a high voltage, just like Crookes’ tube. Electrons rush from the cathode and crash into the gas atoms. Each collision lifts an electron of the atom to a higher energy level (it absorbs energy). When the electron falls back, it gives out that energy as light. Every gas gives its own colour: neon is red-orange and sodium vapour is yellow-orange, like the old street lamps. In a tube light or CFL, mercury vapour gives out invisible ultraviolet light, which makes the white coating on the inside of the glass glow go further.
Colours are approximate. A real signboard tube is bent into letters, and the voltage is made by a transformer inside the sign.
2. The old CRT television at grandma's house
Before flat screens, every TV and computer monitor had a big glass cathode ray tube (CRT) at the back, which is why the old TV at grandma's house is so deep. At the narrow end, a hot cathode gives out electrons, and an anode at high voltage speeds them into a thin beam: these are cathode rays. Just as in Fig 1.4, electric plates (or magnetic coils) bend the beam up and down and from side to side, so that it sweeps the screen line by line. The inside of the screen is coated with a substance that glows where the electrons hit it, like the zinc sulphide in Crookes’ tube. The beam paints the whole picture many times every second, so your eyes see a steady picture.
Here the beam paints 16 lines very slowly. A real TV painted 625 lines, 25 times every second. Colour TVs used three beams and three kinds of glowing dot (red, green and blue) go further.
3. Radioactive isotopes in hospitals
Table 1.6 lists three medical uses. Iodine-131 is used to study and treat the thyroid gland. The thyroid in the neck collects iodine from the blood, so after a patient swallows a tiny dose, a detector outside the neck “sees” how much the gland has taken up. A larger dose destroys an overactive gland or thyroid cancer from the inside. Cobalt-60 gives out powerful gamma rays that are used to treat cancer. The machine turns around the patient, so the tumour receives the rays from every side while the healthy skin gets only a little from each direction. Cancer hospitals such as the Regional Cancer Centre (RCC), Thiruvananthapuram have used cobalt-60 machines for many years. Iron-59 helps to diagnose anaemia: doctors follow how fast the body takes iron into new red blood cells.
4. Carbon-14: how old is this fossil?
Plants take in carbon dioxide, and animals eat plants. So every living thing contains carbon, and a tiny, fixed share of it is radioactive carbon-14, 146C (8 neutrons). While the plant or animal is alive, the share stays the same, because it keeps taking in fresh carbon. After death no new carbon comes in, and the carbon-14 slowly breaks down. Every 5730 years about half of what is left is gone go further. By measuring how much carbon-14 is left in a bone, a piece of wood or charcoal, scientists find its age ഫോസിലുകളുടെ കാലപ്പഴക്കം. Archaeologists use this at excavation sites such as Pattanam in Ernakulam district, where charcoal and wood help to date the remains of an ancient port.
Carbon dating works for remains up to about 50 000 years old. Dinosaur fossils are millions of years old, so they are dated with other radioactive isotopes found in the rocks around them go further.
5. Uranium-235 and heavy water in nuclear power stations
Uranium-235, 23592U (92 protons, 143 neutrons), is the fuel in nuclear power stations (Table 1.6). When a slow neutron hits a uranium-235 nucleus, the nucleus splits into two smaller nuclei, gives out two or three new neutrons and releases a huge amount of heat. This is called nuclear fission go further. The heat boils water, and the steam turns a turbine that makes electricity. Heavy water ഘനജലം is D₂O, the oxide of deuterium (hydrogen with 1 proton and 1 neutron). It slows the neutrons down so that they can split the next uranium nuclei, and control rods soak up the extra neutrons to keep the reaction steady. Most of India’s nuclear power stations, for example at Tarapur, Rawatbhata and Kaiga, use heavy water in this way go further. Kudankulam in Tamil Nadu uses ordinary water. Kerala has no nuclear power station.
6. Sodium-24: finding a leak in a buried pipe
Factories and cities carry oil, water and chemicals in pipes buried under the ground. To find a leak without digging up the whole road, engineers add a very small amount of a liquid containing radioactive sodium-24 to the pipe. Where the pipe leaks, the liquid soaks into the soil and the sodium-24 collects there. A worker walks along the road with a radiation detector, and the reading jumps right above the leak. Sodium-24 loses half of its radioactivity in about 15 hours, so within a few days almost none is left go further.
7. Radiation safety – the ☢ symbol
The radiation from radioactive isotopes can damage the cells of living things, which is why the same gamma rays that kill a tumour must be kept away from healthy people. Radioactive isotopes are therefore handled only by trained people, in special laboratories, with shielding. The warning sign is a black trefoil on a yellow background. Wherever you see it, it means: radiation, keep away. Of the three radiations in the radioactivity box (α, β, γ), alpha is stopped by a sheet of paper, beta by a few millimetres of aluminium, and gamma only by thick lead or concrete go further.
Spend as little time as possible near a source.
Stay far away. The radiation gets much weaker with distance.
Lead, concrete and thick walls stop the radiation. Cobalt-60 machines sit in thick-walled rooms.
Never touch, open or carry home anything with this sign, or any strange metal object found in scrap.
✅ Check yourself
🌐 Explore online – resources hub
Everything in this guide works offline. The links below are extras: simulations and websites from trusted sources (PhET, the Nobel Prize, the Science History Institute, India’s Department of Atomic Energy and others), grouped by topic. They need internet and open in a new tab, so you will not lose your place here. Ask a parent or teacher before you go online. The PhET simulations Build an Atom, Rutherford Scattering and Isotopes and Atomic Mass run directly in the browser, with nothing to install.
Atom models: Thomson, Rutherford and Bohr
- 🧪 Rutherford Scattering (PhET simulation) PhET, University of Colorado Boulder
Fire alpha particles at a gold atom: compare a plum-pudding atom with a tiny nucleus and watch which particles bounce back. - 🧪 Models of the Hydrogen Atom (PhET simulation) PhET, University of Colorado Boulder
Try the plum pudding, Rutherford (classical solar system) and Bohr models one after another and see what each can and cannot explain. - 📄 Rutherford scattering experiments Wikipedia
The 1909–1913 experiments of Geiger and Marsden under Rutherford, with drawings of the apparatus and how the nucleus was discovered. - 📄 Niels Bohr – Biographical The Nobel Prize
The life of the Danish scientist who gave the atom fixed energy levels (Nobel Prize in Physics 1922).
Discharge tubes and cathode rays
- 📄 Crookes tube Wikipedia
Photos and diagrams of the discharge tube in your textbook, including the Maltese-cross shadow and the paddle-wheel tube. - 📄 Cathode ray Wikipedia
How cathode rays were studied by Plücker, Hittorf, Goldstein, Crookes and Thomson, and why they turned out to be electrons. - 📄 Anode ray (canal rays) Wikipedia
Goldstein's canal rays: positive particles that pass through holes in a perforated cathode.
Electrons, protons and neutrons
- 📄 Joseph John “J. J.” Thomson Science History Institute
A short, readable biography of the scientist who identified the electron and proposed the plum pudding model. - 📄 Oil drop experiment Wikipedia
How Robert Millikan measured the charge of the electron (about 1.6 × 10⁻¹⁹ C) using tiny charged oil drops. - 📄 James Chadwick – Biographical The Nobel Prize
The discoverer of the neutron (1932) and his Nobel Prize in Physics 1935.
Atomic number and mass number
- 🧪 Build an Atom (PhET simulation) PhET, University of Colorado Boulder
Drag protons, neutrons and electrons into an atom and watch the element, mass number and charge change. Try the game too. - 📄 Atomic number Wikipedia
Why the number of protons (Z) decides which element an atom is, and how Z and A are written beside the symbol.
Electron configuration and shells
- 📄 Electron shell Wikipedia
The K, L, M, N shells and the 2n² rule. The parts on subshells (s, p, d) are for higher classes. - 🧪 Ptable – interactive periodic table Ptable
Click any element to see its atomic number, its mass and how its electrons are arranged, then compare it with your shell diagrams.
Isotopes and isobars
- 🧪 Isotopes and Atomic Mass (PhET simulation) PhET, University of Colorado Boulder
Add neutrons to an atom to make its isotopes and see which ones are stable and how common each is in nature. - 📄 Isotopes of hydrogen Wikipedia
Protium, deuterium and tritium: the only isotopes with their own names. - 📄 Isobar (nuclide) Wikipedia
Atoms of different elements with the same mass number, such as argon-40, potassium-40 and calcium-40.
Uses of radioactive isotopes
- 📄 Radioisotopes in Medicine World Nuclear Association
How iodine-131, cobalt-60, technetium-99m and other isotopes are used to find and treat disease. - 📄 Board of Radiation & Isotope Technology (BRIT) BRIT, Department of Atomic Energy, India
The Indian government unit in Navi Mumbai that makes radioisotopes for hospitals, industry and agriculture. - 📄 Radiocarbon dating Wikipedia
How carbon-14 in old wood, bones and charcoal tells archaeologists their age. - 📄 Cobalt-60 Wikipedia
The isotope used in radiotherapy machines for cancer treatment and to sterilise medical equipment.
More to explore
- 📄 Ernest Rutherford Science History Institute
Rutherford's life and work: a good starting point for the imaginary-interview activity. - 📄 The ABC's of Nuclear Science Lawrence Berkeley National Laboratory
A friendly guide to the nucleus, isotopes, radioactivity and alpha, beta and gamma rays. - 📄 Radiation Basics U.S. Nuclear Regulatory Commission
What radiation is, where it comes from and why people who work with it use shielding, distance and short times.
Now pull the whole chapter together: Summary & Quick Quiz ▶