I have noticed over the years how many Apollo photographs appear to show the lunar surface as having varying levels of brightness within the same photograph. I guess this can be due to varying levels of surface material brightness and/or colour. However I would like to know how much retroreflectivity comes into play.
I am, of course, referring to the digital scans available within the online Project Apollo Image Gallery and not to some of the poor quality reproductions that have been published down the years.
I have noticed that the surface often appears to be significantly brighter in the 'down-sun' direction. With a horizontal Field of View of 53.5 degrees for the Hasselblad & Zeiss Biogon combination, many single shots can easily capture the surface in directions ranging from 'down-sun' to more than halfway to the 'cross-sun' direction, so this effect can be very noticeable. It can be even more noticeable in a stitched panorama - especially the 'Post Landing Panoramas' where the surface either side of the LM shadow and beyond to the west is very much brighter than the surface to left and right extremities. There is also a tendency for the surface near to the horizon to be less bright - I guess because retroreflected sunlight from the horizon would pass over the camera position.
Referring to the 'Photography' page at ww.clavius.org, I found the following statement interesting:
Shutter speeds were typically 1/125 or 1/250 second. F-stop settings varied from f/5.6 for up-sun photos to f/8 and f/11 for cross-sun and down-sun photos.
When I first read this I thought that it must contain a typo as it suggested that the aperture would be closed down for 'down-sun' shots and opened up for 'up-sun' shots. I felt certain it should be the other way around. However if it is correct it would appear that the surface retroreflectivity was anticipated before even the Apollo 11 landing (not that I would be suprised by that).
I have noted retroreflectivity cited as the reason for the extra brightness of the full moon vs the half-moon etc, and also the 'heiligenschein' effect in photographs where the photographer's shadow appears in the photograph. I guess I am saying here that I know the surface is retroreflective, but I would like some confirmation that this is a good explanation for the apparent variations in the surface's apparent brightness within the same photograph.
Thank you in advance to any who take the time to reply.