The Secchi disk, created in 1865 by Angelo Secchi, is a circular disk used to measure water transparency in oceans and lakes. The disc is mounted on a pole or line, and lowered slowly down in the water. The depth at which the pattern on the disk is no longer visible is taken as a measure of the transparency of the water. This measure is known as the Secchi depth and is related to water turbidity.
George C. Whipple modified the original all-white Secchi disk to “…a disc about 8 inches in diameter, divided into quadrants painted alternately black and white like the target of a level-rod…”  The black and white Secchi disk is the standard disk currently used in limnology investigations and marine water quality studies. 
The Secchi depth is reached when the reflectance equals the intensity of light backscattered from the water. This depth in metres divided into 1.7 yields an attenuation coefficient (also called an extinction coefficient), for the available light averaged over the Secchi disk depth. The light attenuation coefficient, k, can then be used in a form of the Beer–Lambert law,
to estimate Iz, the intensity of light at depth z from I0, the intensity of light at the ocean surface.
The Secchi disk readings do not provide an exact measure of transparency, as there can be errors because of the sun's glare on the water, or one person may see the disk at one depth, but another person with better eyesight may see it at a greater depth. However, it is an inexpensive and straightforward method of measuring water clarity. Because of the potential for variation between practitioners, methods should be standardized as much as possible.
A Secchi disk measurement should always be taken off the shady side of a boat or dock between 9 am and 3 pm The period for best results is between 10 am and 2 pm. The same observer should take Secchi depth measurements in the same manner every time. One can approach the measurement by lowering the disk beyond a point of disappearance, then raising it and lowering it slightly to set the Secchi depth. Another method is to record the depth at which the disk disappears, lower another few feet, then record the depth at which the disk reappears as it is slowly brought up. The Secchi depth is taken as the average of the two values.
Secchi disk measurements have been an integral component of Minnesota's lake water quality assessment programs for some time; lake residents make periodic measurements and submit their readings to state and local agencies. The aggregated longitudinal data are used to reveal general trends in water quality. Similarly, the Indiana Clean Lakes Program trains and relies on volunteers to monitor turbidity in over 80 Indiana lakes using secchi disks, and uses data submitted by volunteers to monitor lake quality in the state.
Secchi disk measurements do not indicate how attenuation changes with depth or particular wavelengths of light. Submarine photometers can operate at depths of 150 m and can record visible, ultraviolet and infrared parts of the spectrum. Turbidimeters have their own light source and can measure transparency with scientific accuracy.
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- Whipple, George C. (1899). The Microscopy of Drinking-Water. New York: John Wiley & Sons, 73–5.
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- Leszek Bledzki (Lead Author);Nidhi Nagabhatla (Topic Editor) "Secchi disk". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth October 15, 2009; Last revised Date October 5, 2010; Retrieved January 6, 2012 <http://www.eoearth.org/article/Secchi_disk>
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