The geotechnical engineer is likley looking at the ground water observations during the time of the field study. If the field study is done in August, the water may be at one depth, if it's done in February it may be at another depth.
The geotechnical engineer may also be looking at the water table in a boring that extends 15 or 20 ft into the ground and into underlying water table conditions. A static water table may be present at 10 ft (or so) in some sand layer and a separate perched water condition may develop at some higher depth during the wet season.
An environmental consultant (or a soil scientist) will look at other factors. The presence of hydric soils (low chroma), the presence of oxidized rhysosphers (sp) or in some cases the population of hydrophytic vegetation. If you have a ground surface covered by facultative vegetation (or wetter), it's reasonable to assume that the high water table during the year is within 12 inches of the ground surface, irrespective of the well data (albiet it may be a perched condition).
The problem with dry pond design is that the typical design standard is to set the bottom grade 4 or 5 ft above the seasonal high water table. But, after you complete all your civil improvements you will ultimatly focus ALOT of infiltration in that very location. This in turn should (will) lead to a mound on the water table, which could ultimatly reduce the headroom between the design base grade and the pre-construction water table elevation. This is never addressed by design and where I believe is where the body is buried.
f-d
¡papá gordo ain’t no madre flaca!