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BoolQ / is the depth of the water table always the same

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is the depth of the water table always the same
passage · full text (603 characters)
The groundwater may be from precipitation or from groundwater flowing into the aquifer. In areas with sufficient precipitation, water infiltrates through pore spaces in the soil, passing through the unsaturated zone. At increasing depths, water fills in more of the pore spaces in the soils, until a zone of saturation is reached. Below the water table, in the phreatic zone (zone of saturation), layers of permeable rock that yield groundwater are called aquifers. In less permeable soils, such as tight bedrock formations and historic lakebed deposits, the water table may be more difficult to define.

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task_id
6eef4133-9d51-5520-ac42-f2bdf6d69ac9
task_key
default--validation--6eef4133-9d51-5520-ac42-f2bdf6d69ac9
task_revision_id
1
config / split
default / validation

Official source

initial import