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there are 4 - 6 layers of iridophores that collectively comprise an<br />

area of up to 60 urn in thickness. Their presence increases the reflectance<br />

by about 65%. In insects, color change generally involves<br />

phase changes of li pids or other materials within the cuticle.<br />

Often these alterations produce a change from nearly black to a<br />

shiny metallic blue or green, depending on the ambient temperature.<br />

168<br />

UV<br />

UV-CI UV-BIUV-A<br />

100 280 315<br />

400 nm<br />

Chapter 23. PHOTOBIOLOGY<br />

Photobiology is the branch of biophysics concerned with the<br />

effect of light on living organisms.<br />

23.1. ELECTROMAGNETIC SPECTRUM<br />

The entire frequency range of electromagnetic waves is called<br />

the electromagnetic spectrum. Part of the spectrum is shown in<br />

fig. 23.1. The upper part of the top bar shows two of the most<br />

important sources of radiation (solar and thermal) and the lower<br />

part names three important bands - ultraviolet (290 - 400 nm),<br />

visible (400 - 700 nm) and near-infrared (700 - 2500 nm). The<br />

second bar shows three bands of the ultraviolet (UV-C, UV-B<br />

and UV-A) and the wave bands of the visible colors.<br />

400<br />

Visible<br />

IR<br />

700 nm<br />

3<br />

6 10 um<br />

Fig. 23.1. Scale of electromagnetic waves in ultraviolet,<br />

visible and infrared parts of spectrum<br />

r<br />

23.2. EFFECT OF ULTRAVIOLET RADIATION<br />

ON LIVING ORGANISMS<br />

23.2.1. Human and Animal Health<br />

Ultraviolet radiation (UV) is generally divided into three<br />

groups, based upon the biological effectiveness of the photons in<br />

each. The UV-C range contains the shortest wavelengths « 280<br />

nm) and the highest energy photons, which are capable of causing<br />

ionizing reactions in the upper atmosphere. Due to absorption<br />

by ozone in the stratosphere, UV-C radiation does not reach<br />

the Earth's surface. UV-B radiation (280 - 320 nm), however,<br />

does reach the biosphere in small and variable quantities. The radiation<br />

is of sufficient energy to cause direct damage to chromophoric<br />

regions of absorbing macromolecules such as nucleic acids<br />

and proteins. UV-B radiation is responsible for damage to crop<br />

plants. At longer wavelengths, UV-A radiation (320 - 400 nm)<br />

absorption is usually less strong and is dominated by molecules<br />

with conjugated double bonds, and cyclic and polycyclic molecules<br />

(e.g., isoprenoids, flavonoids, quinines, alkaloids), metal<br />

enzymes, and others. The increase in UV-B radiation entering the<br />

biosphere is associated with stratospheric ozone depletion and is<br />

likely to have a significant detrimental impact on human health.<br />

Eye diseases. UV radiation can damage the cornea and lens of<br />

the eye. Chronic exposure to UV-B is one of several factors clearly<br />

associated with the risk of cataracts. Artificial sources of UV radiation<br />

also cause corneal damage. For example, the injury from a<br />

welder's arc is known as flash burn, welder's flash or arc eye.<br />

Other sources of UV radiation injury include sun tanning beds,<br />

carbon arcs, photographic flood lamps, lightning, electric sparks,<br />

and halogen desk lamps. Prolonged exposure to UV radiation can<br />

lead to several ocular surface disorders such as pinguecula, pterygium,<br />

climatic droplet keratopathy, and even squamous metaplasia<br />

and carcinoma.<br />

Immune suppression. Some components of the immune system<br />

are present in the skin. UV exposure decreases the immune response<br />

to skin cancer, infectious agents, and other antigens.<br />

Erythema. The normal acute effects of visible and ultraviolet<br />

radiation arise by photochemical change in the epidermis due to<br />

169

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