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The 34 pages that link to Water table, each with the reason it gives.

• KarstRelated: Its position influences where dissolution, cave passages, and underground drainage develop.

• GroundwaterRelated: Its depth marks the upper boundary of groundwater in an unconfined aquifer.

• AquiferRelated: Its position marks the boundary between saturated and unsaturated ground.

• Groundwater depletionRelated: Pumping-related declines in this boundary are a common sign of depletion.

• OasisRelated: A shallow water table can allow plants to reach moisture in an arid setting.

• PeatlandRelated: Its height helps determine whether peatland soils remain saturated.

• HydrologyRelated: Marks the boundary between unsaturated ground and groundwater storage.

• Groundwater rechargeRelated: Recharge raises the water table when added water exceeds local losses.

• PeatRelated: A high water table keeps peat-forming plant matter saturated and oxygen-poor.

• QanatRelated: The mother well must reach groundwater below the local water table.

• SpeleogenesisRelated: Its position influences whether cave passages remain water-filled or drain into air.

• Groundwater flowRelated: Its shape indicates the upper boundary and gradient of unconfined groundwater.

• Ogallala AquiferRelated: Pumping lowers the water table where withdrawals exceed local recharge.

• PolderRelated: Polder water management controls groundwater levels as well as visible surface water.

• HydrogeologyRelated: Its depth marks the upper boundary of the saturated zone in many settings.

• Soil liquefactionRelated: Shallow groundwater leaves near-surface soils saturated and potentially susceptible.

• StalagmiteRelated: Changes in groundwater level can alter cave flooding, drip paths, and mineral growth.

• Supergene enrichmentRelated: Its position helps determine where descending metal-bearing water encounters reducing conditions.

• Vadose zoneRelated: It forms the lower boundary of the vadose zone.

• Artesian wellCompared with: Unlike the water table, the pressure level in a confined aquifer can lie above its rock layer.

• MarshRelated: Its position helps determine whether marsh soils remain saturated.

• Peatland drainageRelated: Drainage lowers this boundary, exposing deeper peat to air.

• Pit latrineRelated: Its depth affects the risk that a pit will reach groundwater or allow contaminants to leach into it.

• Confined aquiferCompared with: A confined aquifer's upper boundary is not its water table.

• Oxidation zoneRelated: Its position influences where oxygenated groundwater can oxidize sulfide ore.

• Water wellRelated: Its depth determines how far a shallow well must reach to encounter groundwater.

• BoreholeRelated: Its depth determines how far a water borehole must reach to encounter groundwater.

• Oasis agricultureRelated: Its depth and seasonal changes constrain wells, springs, and irrigated cultivation.

• Peat swamp forestRelated: A high water table limits oxygen and slows the decay of plant material.

• Soil vapor extractionRelated: Its depth defines the lower boundary of the zone treated by conventional soil vapor extraction.

• Vasyugan SwampRelated: A persistently high water table restricts oxygen and slows plant decomposition in peat.

• Fresh waterRelated: Its depth helps determine how much groundwater is accessible to wells.

• Solutional caveRelated: Its position helps determine where cave passages form and how they later drain.

• Underground lakeRelated: Its elevation often sets the level of water in connected cave passages.