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Static level is the level of water in the well when no water is being removed from the well by pumping. [8] Water table is the upper level of the zone of saturation, an underground surface in which the soil or rock is permanently saturated with water. [9] Well yield is the volume of water per unit time that is produced by the well from pumping. [8]
An image of an aurora captured by officials at Butler University's Holcomb Observatory & Planetarium in Indiana. The northern lights were visible across large swaths of the United States thanks to ...
Created in 1837, the Indiana Geological and Water Survey (IGWS) is an official agency of the U.S. state of Indiana charged with geological research and the dissemination of information about the state's energy, mineral and water resources. [1] In 2017, the Indiana Geological Survey was renamed to the Indiana Geological and Water Survey. [2]
In hydrology, a well test is conducted to evaluate the amount of water that can be pumped from a particular water well.More specifically, a well test will allow prediction of the maximum rate at which water can be pumped from a well, and the distance that the water level in the well will fall for a given pumping rate and duration of pumping.
The aurora borealis put on a dazzling light show in skies over the United States this weekend.Thanks to geomagnetic storms that pushed the northern lights further south, many Hoosiers caught a ...
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The reservoir it creates, Mississinewa Lake, has a normal water surface of five square miles (13 km 2), has a maximum capacity of 368,400 acre-feet (454,400,000 m 3), and a normal capacity of 75,200 acre-feet (92,800,000 m 3). [6]
The lake is the largest entirely situated in Indiana with 10,750 acres (43.5 km 2) of water surface area spread over the counties of Monroe and Brown. Capacity varies from 292 gigalitres (237,000 acre⋅ft) to 428 gigalitres (347,000 acre⋅ft) [ 2 ] depending on water level.