Portions of the following has been excerpted from from copyrighted material.  Material in this section should not be reproduced without specific permission of the North American Lake Management Society ( www.NALMS.org).  The reader is encouraged to read the original material for more details on Secchi disk theory and methods.  These are:

Carlson, R.E. 1995.  The Secchi disk and the volunteer monitor.  LakeLine. 15(1):  28-29, 35-37.
Carlson, R.E. and J. Simpson.  1996.  A Coordinatorís Guide to Volunteer Lake Monitoring Methods. North American Lake Management Society.  96 pp.
Carlson, R.E.  1997.  The Secchi disk in black and white.  LakeLine.  17: 14-15, 58-59.  (7/20/97)

   LakeLine is available through the North American Lake Management Society

Why a Black and White Secchi Disk?

The original "Secchi's" disk was all-white.  Today most disks used in lakes have alternating black and white quadrants, while marine disks are usually all-white.  The reasons for the difference is not clear, and may be more historical than theoretical.  Early disks of the 19th century were all white, but George C. Whipple (1899) stated that a disk with alternating black and white quadrants was more easily seen (Fig. 1), and "Whipple's" disk became the standard in freshwater situations.

Figure 1.  The "Whipple Sector Disk," as illustrated in the 4th edition of The MIcroscopy of Drinking Water (Whipple, 1933)

 In the1899 edition he states:

"The authorís experiments have shown that the limit of visibility may be determined most accurately by using a disc about 8 inches in diameter, divided into quadrants painted alternately black and white like the target of a level-rod, and looking vertically down upon it through a water-telescope provided with a suitable sunshade."

In theory, the Secchi disk works as a contrast instrument.  It disappears when the human eye can no longer see it, meaning that there no longer remains any contrast between the disk and its background.  A white disk should remain visible longest if viewed against a completely black background.  In many lakes, the background is less than totally black because the light is reflected off the bottom or back-scattered from suspended particles.  In these situations, a white disk may disappear sooner than would be expected than if the background were black. The black quadrants may serve as a constant black background, thus standardizing the contrast.  It may be that the all-white disk used in the ocean is acceptable because the background color in the deep ocean is black, thus making the black quadrants unnecessary.  

The newest trend in disk color is the all-black disk (Davies-Colley 1988).  Developed and used extensively in New Zealand, the disk  has the advantage that it can be used in shallow rivers and streams.  Unlike the horizontally-held Secchi disk, the black disk is held vertically and is viewed over a horizontal distance using an inverted periscope.  Because the black disk does not require much water depth, it can be used in streams.  The ability to use black disk in rivers and streams could establish cooperation and compatible data with stream volunteer programs.  Lake monitors could use the black disk to discover which streams entering a lake are the most turbid.

Davies-Colley, R.J.  1988.  Measuring water clarity with a black disk.  Limnol. and Oceanogr.  33: 616-623.

Whipple, G.C.  1899, 1910, 1914, 1933.  The Microscopy of Drinking Water.  John Wiley and Sons.  New York and London.
Carlson, R.E.  1997.  The Secchi disk in black and white.  LakeLine.  17: 14-15, 58-59.  (7/20/97)