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Question

Q.(a) Name the parts of the electromagnetic spectrum which are:

(i) also known as heat waves, and
(ii) absorbed by the ozone layer in the atmosphere.
(b) Write briefly one method each for the production and detection of these radiations.
CBSECBSE Class XII Board 2024Subjective· 3mImportance★★★★★
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Infrared radiation is known as heat waves, while ultraviolet radiation is absorbed by the ozone layer. Both can be produced by hot sources and detected using specialized sensors or materials.

The electromagnetic (EM) spectrum encompasses a vast range of radiation, from long radio waves to short gamma rays, all travelling at the speed of light. These different types of radiation are distinguished by their wavelengths and frequencies, which in turn dictate their properties and interactions with matter. Understanding these interactions is key to answering this question.

(a) Naming Parts of the Electromagnetic Spectrum

  1. Understanding "Heat Waves":

    When we talk about "heat waves" in the context of electromagnetic radiation, we are referring to radiation that is readily absorbed by matter, causing its temperature to rise. All objects above absolute zero emit thermal radiation due to the vibration and rotation of their constituent atoms and molecules. The wavelength at which an object emits most of its thermal radiation depends on its temperature.

    • Identification: The part of the electromagnetic spectrum commonly known as heat waves is Infrared (IR) radiation.
    • Reasoning: At typical ambient temperatures (like human body temperature or a warm object), the peak emission of thermal radiation falls within the infrared region. When IR radiation is absorbed by a material, it increases the kinetic energy of its molecules, leading to a direct increase in temperature, which we perceive as heat. This is why infrared cameras can "see" heat.
  2. Understanding Absorption by the Ozone Layer:

    The Earth's atmosphere contains a layer of ozone (O3O_3) primarily in the stratosphere, about 10 to 50 kilometers above the surface. This ozone layer plays a crucial role in protecting life on Earth by absorbing certain types of high-energy radiation from the Sun.

    • Identification: The part of the electromagnetic spectrum absorbed by the ozone layer is Ultraviolet (UV) radiation.
    • Reasoning: Ultraviolet radiation carries enough energy to break chemical bonds. Specifically, UV-B and UV-C radiation from the Sun have sufficient energy to cause the photodissociation of ozone molecules (O3O_3). This process involves the absorption of a UV photon, leading to the breakdown of O3O_3 into O2O_2 and OO. This absorption prevents most of the harmful UV radiation from reaching the Earth's surface, where it could cause significant damage to living organisms.

(b) Production and Detection Methods

Now, let's look at how these radiations are produced and detected.

  1. Infrared (IR) Radiation:

    • Production:

      • Hot Bodies: Any object with a temperature above absolute zero (0 K0 \text{ K} or −273.15 °C-273.15 \text{ °C}) emits infrared radiation. The hotter the object, the more intense the IR emission and the shorter its peak wavelength. Examples include electric heaters, incandescent light bulbs, and even the human body.
      • Molecular Vibrations: Molecules can absorb and emit IR radiation when their vibrational and rotational energy states change. This principle is used in various IR sources and spectroscopy.
    • Detection:

      • Thermopiles: These devices consist of multiple thermocouples connected in series. When IR radiation falls on one set of junctions, it heats them up, creating a temperature difference between these junctions and reference junctions. This temperature difference generates a measurable voltage (Seebeck effect), which is proportional to the incident IR radiation.
      • Bolometers: A bolometer detects IR radiation by measuring the change in electrical resistance of a material (often a thin metal strip or semiconductor) as it heats up due to the absorption of IR radiation. The change in resistance is then converted into an electrical signal.
      • Infrared Cameras: These cameras use specialized sensors (e.g., microbolometers or cooled photon detectors) that are sensitive to IR wavelengths. They convert the detected IR radiation into an electrical signal, which is then processed to create a thermal image visible to the human eye. …

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