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I 75 Drinking Fountain? EarthCache

Hidden : 5/11/2010
Difficulty:
2 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

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Flowing artesian wells are created when the pressure in a confined aquifer (water- bearing geologic formation) forces ground water above the ground surface so that the well will flow without a pump. This water is forced up through either man-made holes or natural fissures (cracks). An aquifer is a layer of permeable material in which water can easily move such as unconsolidated sand, gravel, clay or silt. It can also be composed of soft rock like fractured limestone or sandstone that absorbs water from an inlet path. Large solution openings that are produced when part of the rock is dissolved by ground water are common in carbonate rocks. Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone and dolomite. These openings store and transmit large quantities of water. Porous stone is crushed between impermeable rocks or clay. This keeps the pressure high, so when the water finds a hole, it overcomes gravity and is forced up and out. The principal water-yielding aquifers of North America can be grouped into five types: unconsolidated and semi-consolidated sand and gravel aquifers, sandstone aquifers, carbonate-rock aquifers, aquifers in interbedded sandstone and carbonate rocks, and aquifers in igneous and metamorphic rocks. This well and others in the area are produced from a Carbonate-Rock aquifer (sometimes referred to as a Silurian-Devonian aquifer). The average thickness of the carbonate rocks that compose most of the Silurian-Devonian aquifer is about 300 to 400 feet; the aquifer also contains some sandstone, shale, and evaporite beds (rock and mineral deposits left over from evaporation process when Michigan was covered by sea water). Water movement is primarily through secondary openings, such as joints, fractures, and bedding-plane openings, many of which have been enlarged by dissolution (dissolving of underground rocks). The pH of the groundwater is affected by the type of rock material it moves through and how long it remains in contact before it is released. The indicator for acidity or alkalinity, or basic, is known as the pH value. A pH value of 7 means a substance is neutral. The lower value indicates acidity, and a higher value is a sign of alkalinity. To display the range in pH, take a look at these examples: Lemon- 2.5 Coffee-5-6.5 Milk- 6.2 Soapy water-7-10 Beer- 4.5 So, what does pH mean for water? Basically, the pH value determines whether water is hard or soft. The pH of pure water is 7. In general, water with a pH lower than 7 is considered acidic, and with a pH greater than 7, basic. The normal range for pH in surface water systems is 6.5 to 8.5 and for groundwater systems 6 to 8.5. According to U.S. Environmental Protection Agency criteria, water for domestic use should have a pH between 5.5 and 9. Alkalinity is a measure of the capacity of the water to resist a change in pH that would tend to make the water more acidic. The measurement of alkalinity and pH is needed to determine the corrosiveness of the water. In general, water with a low pH ( 8.5 could indicate that the water is hard. Hard water does not pose a health risk, but can cause aesthetic problems. These problems include an alkali taste to the water (making that morning coffee taste bitter!), formation of a deposit on dishes, utensils, and laundry basins, difficulty in getting soaps and detergents to lather, and formation of insoluble precipitates on clothing. While the ideal pH level of drinking water should be between 6-8.5, the human body maintains pH equilibrium on a constant basis and will not be affected by water consumption. For example our stomachs have a naturally low pH level of 2 which is beneficial acid that helps us with food digestion. To claim a find, e-mail me through my profile after completing the following tasks. You will need a camera, tape measure, and pH testing strips. 1). What is the distance from the ground to the tip of the pipe where the water exits? 2). Take a picture of you/your team and/OR your GPSr at the location. 3). What is the pH level of the water?

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