By Paul Hoste
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By using the geologic map, it is possible to estimate the thickness of each unit and the anticipated well depth. If data exists for this aquifer in other areas, it may also be possible to predict the expected well yield and groundwater quality. In soils, the stratigraphic sequence is usually less extensive, more variable, and not as well known as rock. Alluvial deposits often consist of interbedded gravel, sand, silt, clay, mixtures of these materials, and, possibly, interbedded evaporite deposits.
Pivot irrigation patterns (Figure 2-34) are distinctive and are usually supplied by centrally located water-supply wells. Such features are good indications that quality groundwater is present at economic pumping depths. (11) Reservoirs and Lakes. Surface water bodies can be groundwater recharge, discharge, or both artificial surface-water reservoirs usually capture surface water and represent areas of 2-32 FM 5-484/NAVFAC P-1065/AFMAN 32-1072 recharge, as do natural reservoirs created by the damming of streams.
Down the slope of a fan, aquifers get progressively thinner (pinch out). In the lower part of a large fan, test drilling may be needed to locate a productive bed. (d) Basins. Alluvial basins are in regions where mountains alternate with structural troughs (Figure 2-21, page 2-20). Erosional products from the mountains partly fill the basins with alluvium laid down as a series of coalescing alluvial fans. The upper alluvial slopes form piedmont plains or alluvial aprons that gradually decrease in slope toward the interior of the basin until they merge with the interior flats.