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Water Smarts 2002
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3/27/2013 12:48:13 PM
Creation date
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Year
2002
Title
Water Smarts
Author
Upper Arkansas Area COG USGS Pueblo Office
Description
A well and septic system owner's guide to ground water in the upper arkansas area chaffee, custer, fremont, and lake counties, Colorado
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Definitions <br />The following definitions describe the meanings of terms, which are used in this booklet and with which the <br />reader may not be familiar. <br />Acid -mine drainage <br />Acidic water forms through the chemical reaction <br />of water with rock containing sulfide minerals (such <br />as pyrite) forming sulfuric acid. The acid leaches <br />heavy metals from the mineralized rock and keeps <br />the metals dissolved in water. This acid rock <br />drainage can adversely impact aquatic life and <br />human health if it mixes with water supplies. <br />Aquifer <br />A geologic formation, part of a formation, or group <br />of formations, that will yield usable quantities to a <br />well or a spring. <br />Confining unit (bed) <br />A geologic formation, part of a formation, or group <br />of formations, whose hydraulic conductivity may <br />range from nearly zero to some value distinctly <br />lower than that of the aquifer that it confines. <br />Corrosivity <br />Refers to the aggressiveness of water. This is in <br />part a function of how acidic the water is. The EPA <br />defines "corrosive" as, " A chemical agent that <br />reacts with the surface of a material causing it to <br />deteriorate or wear away." <br />Fault <br />A fracture or a zone of fractures along which there <br />has been displacement of the sides relative to one <br />another parallel to the fracture. <br />Fracture <br />A crack or break in a rock formation due to <br />structural stresses. Fractures are often the result of <br />the natural process at work when the mountains <br />were formed (i.e., folding and faulting). Fractures <br />may or may not hold ground water. <br />Ground water <br />The water found beneath the Earth's surface at <br />pressure equal to or greater than atmospheric <br />pressure. <br />Unconfined ground water has a water table. <br />Confined ground water is under pressure <br />23 <br />significantly greater than atmospheric, and its upper <br />limit is the bottom of a bed of distinctly lower <br />hydraulic conductivity than that of the material in <br />which confined water occurs. <br />Hydraulic conductivity <br />The property of a porous medium, which allows <br />water to flow through it. It is analogous to <br />electrical conductivity. <br />Igneous rocks <br />Said of a rock or mineral that solidified from <br />molten or partly molten material. These include <br />intrusive igneous rocks, such as granite, and <br />extrusive rocks, such as volcanic rocks. <br />Metamorphic rocks <br />Any rock derived from pre- existing rocks by <br />mineralogical, chemical, and /or structural changes, <br />in response to marked changes in temperature, <br />pressure, and chemical environment, generally at <br />depth in the Earth's crust. <br />Overburden <br />The loose soil, silt, sand, gravel, and other <br />unconsolidated material overlying bedrock, either <br />transported or formed in place (regolith). <br />Sedimentary rocks <br />A rock resulting from the consolidation of loose <br />sediment that has accumulated in layers, consisting <br />of mechanically formed fragments of pre- existing <br />rock transported from its source and deposited in <br />water or from air or ice, or formed by precipitation <br />from solution, or consisting of the remains or <br />secretions of plants and animals. <br />Unconsolidated material <br />A sediment that is loosely arranged or unstratified, <br />or whose particles are not cemented together. <br />Water table <br />That surface in an unconfined water body at which <br />the pressure is atmospheric. <br />
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