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Figure 21 Table depth map and histogram.
This mismatch arises from differences in baseline water table depth prior to urbanization.
Data such as drain discharge, soil salinity, water table depth, and soil properties were collected.
Reciprocally, crops can influence ground water, altering water table depth and chemical composition.
Hence, seasonal water table depth parameters do not explain the wide variation in boundary depth.
CO2 and N2O emissions depended on soil temperature and water table depth.
The proposed model uses monthly water diversion, evaporation, precipitation, temperature, and time as input data to predict water table depth.
Water use was estimated for the spring-fall period using volumetric water content, water table depth and daily precipitation.
The results show that the impacts of water table depth and irrigation frequency vary according to the season.
The water table depth reached less than 100 cm before flowering during both seasons.
The water table depth is commonly 0.60 to 2.3 m below the ground.
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