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When the elevation of the water table is below the stream, the stream is considered to be gaining water from the surrounding groundwater, a process known as gaining or effluent stream. In this situation, the stream acts as a discharge point for groundwater, contributing to its flow. Conversely, if the water table is above the stream, the stream may lose water to the groundwater, referred to as a losing or influent stream.
If the water table rises, the stream may become more full and flow faster due to increased groundwater discharge into the stream. This could potentially lead to flooding and erosion along the stream banks.
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If a well were drilled near the stream and lowered the water table, it could lead to reduced stream flow, potentially causing the stream to dry up or decrease in size. This change could negatively impact local wildlife that relies on the stream for habitat and drinking water. Additionally, residents might experience changes in groundwater availability for their own use, potentially leading to conflicts over water resources and affecting vegetation and landscaping in the area.
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The stream table system is a microscopic scale system, as it typically models processes that occur at the scale of sediment transport and river dynamics, which are observable and measurable. It involves the behavior of water and sediment at a scale larger than atoms or molecules, focusing on physical features like erosion and deposition in a controlled environment. In contrast, atomic scale systems deal with individual atoms and their interactions, which are not the focus of stream table experiments.