The phrase "average water table" is correct and usable in written English.
It can be used in discussions related to hydrology, geology, or environmental science when referring to the mean level of groundwater in a specific area.
Example: "The average water table in this region has been steadily declining due to prolonged drought conditions."
Alternatives: "mean water table" or "typical water table".
The average water table level was significantly lower at Drained than Pristine sites especially near the ditches.
Monthly measurements of the piezometric heads in observation wells based on a Thiessen polygon approach were used to compute annual average water table heights over the whole aquifer.
In both seasons, the average water table depth during critical flowering stage was 100 cm. Figure 4 shows the crop at various stages in the RS trials after stress imposition.
Figure 3 d) shows the average water table height, h(t), from the ground surface level, zs; estimated from the water level variations of four shallow wells within 50 m of the gravity observatory.
The potential for increasing the average water table depth by up to 1.1 and 0.7 m in the two respective modeled regions, thereby reducing the threat of waterlogging and lowering non-beneficial consumptive use from adjacent fallow and naturally-vegetated lands, is demonstrated for the alternative management intervention scenarios considered.
In this study, a Soil Water Atmosphere Plant (SWAP) package was integrated into a groundwater flow model (MODFLOW) in such a way that the SWAP package calculates vertical flux for MODFLOW, while MODFLOW provides averaged water table depth to determine the bottom boundary condition for SWAP zones.
Aedes triseriatus occupancy was positively related to average water volume (Table 3), suggesting that occupancy is higher in larger treeholes with more stable hydroperiods, a finding inconsistent with Ellis et al. [ 3].
(5) The average ambient water table position follows the boundary between saprolite and fractured bedrock.
Open image in new window Fig. 7 Average annual water table in the Dehgolan aquifer.
As the NS model efficiency is biased to the higher values, the index of agreement (I A) is used and expressed as below (Legates and McCabe 1999): I_{A} = 1 - frac{{sumlimits_{i = 1}^{N} {(O_{i} - S_{i} )^{2} } }}{{sumlimits_{i = 1}^{N} {left( {left| {S_{i} - mu_{0} } right.| + left| {left. {O_{i} - mu_{0} } right|} right.} right)^{2} } }} (11 where μ 0 is the average observed water table depth.
aThe probability of SLEV transmission incidence is represented as a function of two time lags of weekly averaged modeled water table depth (WTD).
