The following sections of this BookRags Literature Study Guide is offprint from Gale's For Students Series: Presenting Analysis, Context, and Criticism on Commonly Studied Works: Introduction, Author Biography, Plot Summary, Characters, Themes, Style, Historical Context, Critical Overview, Criticism and Critical Essays, Media Adaptations, Topics for Further Study, Compare & Contrast, What Do I Read Next?, For Further Study, and Sources.
(c)1998-2002; (c)2002 by Gale. Gale is an imprint of The Gale Group, Inc., a division of Thomson Learning, Inc. Gale and Design and Thomson Learning are trademarks used herein under license.
The following sections, if they exist, are offprint from Beacham's Encyclopedia of Popular Fiction: "Social Concerns", "Thematic Overview", "Techniques", "Literary Precedents", "Key Questions", "Related Titles", "Adaptations", "Related Web Sites". (c)1994-2005, by Walton Beacham.
The following sections, if they exist, are offprint from Beacham's Guide to Literature for Young Adults: "About the Author", "Overview", "Setting", "Literary Qualities", "Social Sensitivity", "Topics for Discussion", "Ideas for Reports and Papers". (c)1994-2005, by Walton Beacham.
All other sections in this Literature Study Guide are owned and copyrighted by BookRags, Inc.
In discussions of groundwater, a zone of saturation is an area where water exists and will flow freely to a well, as it does in an aquifer. The thickness of the zone varies from a few feet to several hundred feet, determined by local geology, availability of pores in the formation, and the movement of water from recharge to points of discharge.
Saturation can also be a transient condition in the soil profile or vadose zone during times of high precipitation or infiltration. Such saturation can vary in duration from a few days or weeks to several months. In soils, the saturated zone will continue to have unsaturated conditions both above and below it; when a device used to measure saturation, called a piezometer, is placed in this zone, water will enter and rise to the depth of saturation. During these periods, the soil pores are filled with water, creating reducing conditions due to lowered oxygen levels. This reduction, as well as the movement of iron and manganese, creates distinctive soil patterns that allow the identification of saturated conditions even when the soil is dry.