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A perched water table is a localized zone of saturation above the main water table in an aquifer. It impacts groundwater flow and storage by creating a barrier that can restrict the movement of water between the perched and main water tables. This can affect the overall flow and storage capacity of the aquifer system, potentially leading to variations in water availability and quality in different parts of the aquifer.

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Is limestone a good aquifer?

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How is the type of bedrock affect groundwater?

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What has the author Janae Wallace written?

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