Exposure, air kerma and absorbed dose



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Exposure, air kerma and absorbed dose

These 3 quantities play a central role in clinical radiation dosimetry. A detailed discussion and history is given in the article in this issue by Cormack and Carrier[1] and various international reports discuss the definitions in great detail[2]. I wish to give a brief outline here for completeness.

The quantity exposure is defined as the total charge of one sign produced in dry air when all electrons liberated by photons in a unit mass of air are completely stopped in air. The energetic knock-on electrons produce about 30 electrons for every keV of energy they lose, thus a single 100 keV knock-on electron produces 3000 free electrons. The SI unit for exposure is C/kg as

 

suggested by the definition, but the old unit, the roentgen (1R=2.58 10 C/kg) is still often used. The definition refers to all electrons set in motion by photons in the volume of air with mass m, and the charge is collected from throughout the electron's path as it slows down (fig 1). This quantity has the advantage of being directly measurable, at least for low-energy photons (<300 keV or so) where the electrons don't move too far as they slow down. The primary measurement standard is a free air chamber which has two parallel plates with a potential across them for collecting the charge liberated by a well defined photon beam passing between them. This works very well for low-energy photons, and allows a direct measurement with an accuracy of about 0.5%. The measurement technique breaks down for photons with energies typical of beams (up to 1.33 MeV). In this case very different techniques using ion chambers and Bragg-Gray cavity theory are needed to measure exposure (discussed below). However, exposure suffers from two fundamental flaws. The first is that it is only defined for photons interacting in air; the second is that the quantity becomes ill-defined as photon energies become higher as in accelerator beams because the range of the electrons slowing down becomes so large.

These problems are both overcome by introducing the quantity kerma, which is the Kinetic Energy Released per unit MAss (unit J/kg or gray). For photon beams the kinetic energy released is the kinetic energy transferred to electrons in the material. The quantity must always be defined with respect to the specific material in which the interactions are taking place (e.g. air kerma, water kerma etc). This quantity is well defined at all energies and for all materials and in fig 1 it is just the sum of all the energy transfers to charged particles, E, in the volume divided by the mass m. For kerma, it does not matter whether the charged particles slow down inside the volume or not. As we shall see below, air kerma and exposure are closely related, and although the measurement standards are embodied in the same equipment, air kerma is not directly measurable in the same sense as exposure. Nonetheless kerma plays an important role in radiation dosimetry because it is the energy released per unit mass of material, and not surprisingly this is closely related to the energy absorbed per unit mass of material.

The absorbed dose to a material, is:

 

where is the energy absorbed (J) in a mass m (kg) of the materialgif. In fig 1 the absorbed dose sums the energy deposition on all the tracks from P to P. For volumes which are large compared to the tracklength, the kerma and absorbed dose are virtually identical, especially since absorbed dose also includes energy deposition within the volume by electrons set in motion outside the volume. This tends to balance the energy deposited outside the volume by those electrons starting inside the volume.

Absorbed dose is currently taken as the best physical indicator of biological response. Because of this, absorbed dose to water (which closely resembles human tissue but is well defined) is the quantity which is used to specify the amount of radiation to be used in clinical practice. Absorbed dose has the further advantage that it is directly measurable in a variety of ways. The most straightforward is by calorimetry which determines the energy deposited per unit mass of material by measuring the temperature rise. The temperature rise in water for a typical radiotherapy dose of 200 cGy (2 J/kg), delivered in 1 or 2 minutes, is 500 K (specific heat capacity of water is 4181 J/(kg K)).


next up previous contents
Next: Bragg-Gray cavity theory Up: Ionizing Radiation Dosimetry and Previous: Introduction



Dave Rogers' generic account
Sat Nov 25 10:18:46 EST 1995