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Depressions, or dolines, are fairly common, although cenotes open to the water table are exceedingly rare in most of the study area.
Likewise, failure and success may not always be predicted by distance from the coast or depth of the water table.
These changes he interpreted as a response to variations in water table levels.
The water table in the experimental site ranged from 1.2 to 1.4 m throughout the crop growth periods.
Because the water table was below 2.0 m depth, the soil was medium textured, and the area was flat, capillary rise was ignored.
Nodulation occurred on tabular buttresses in horizontal lines just above the water table level.
The nodules below the water table showed a similar distribution of colour.
These gradual rises in the number of plant species reflect improved peat-forming conditions resulting from local rises of the water table.
This is particularly suggested by the succession of evaporite couplets, which are attributed to pulsating episodes of water table change.
The water table had an average depth of 25 cm along the sampled radial segment and was visible in the depressions.
Both environmental changes could result in water table changes fatal for survival of some plant species.
It is produced in the dry season, in areas with a high water table or with irrigation, and in the rainy season.
In either case the toxic or radioactive waste is trapped in the solid, preventing it from leaching into the local water table.
According to the relative abundance of legume species, possibilities for comparisons between plots, and water table, representative species and individuals were chosen for nodulation studies.
Blocks with water extraction more than recharge indicate receding water table zones.
