Aquifer: Béda antarrépisi
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== Klasifikasi Aquifer ==
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Diagram ieu ngindikasikeun arah aliran tipikal dina [[potongan lintang (géométri)|potongan lintang]] tina sistim aquifer ''confined/unconfined'' basajan (dua aquifer kalayan hiji [[aquitard]] diantarana, dilingkung ku ''bedrock aquiclude'') numana huhubungan jeung [[aliran]] (tipical dina daerah [[lembaba]] ). ''[[Water table]]'' jeung [[zona vadose|zona henteu jenuh]] ogé diilustrasikeun.
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== Misconception about aquifers and groundwater ==
A common [[misconception]] is that [[groundwater]] exists in ''underground rivers'' (e.g. [[cave]]s where water flows freely underground). This is only sometimes true in [[erosion|eroded]] [[limestone]] areas known as [[karst topography]] which make up only a small percentage of Earth's area. More usual is that the [[porosity|pore spaces]] of rocks in the subsurface are simply saturated with water
The [[beach]] is an example of what most aquifers are like. If you dig a hole into the [[sand]] at the beach you will find very wet or saturated sand at a shallow depth. This hole is a crude [[water well|well]], the beach sand is an aquifer, and the level to which the water rises in this hole represents the [[water table]].
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{{Aquiferproperties}}
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[[ca:Aqüífer]]
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[[lt:Vandeningas sluoksnis]]
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[[pl:Warstwa wodonośna]]
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