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Published in:
Effects of Climate Change and Sea Level Rise on Coastal Water Resources Read chapter Read first chapter

2016 | OriginalPaper | Chapter

3. Deficit Irrigation as a Strategy to Cope with Declining Groundwater Supplies: Experiences from Kansas

Authors : I. Kisekka, J. Aguilar

Published in: Emerging Issues in Groundwater Resources

Publisher: Springer International Publishing

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Abstract

The High Plains aquifer shown in Fig. 3.1 underlies 453,248 km2 in parts of eight states (Nebraska, Texas, Kansas, Colorado, New Mexico, Oklahoma, Wyoming, and South Dakota) making it the biggest aquifer in North America (Fig. 3.1). The predominant formation in the High Plains aquifer is the Ogallala Formation of the Miocene/Pliocene age (Sophocleous 2012), thus this aquifer is commonly referred to as the Ogallala aquifer. This predominantly unconfined aquifer comprises of silt, sand, gravel and clay, and varies in saturated thickness and permeability (Buchanan et al. 2009). For example, the predevelopment aquifer thickness and depth to water in Kansas varies from 15 m to over 90 m, and 8 m to over 105 respectively (High Plain Atlas). Most of the water from the aquifer is paleo or fossil water associated with the events of the last ice age when glaciers covered the Great Plains.

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previous chapter Assessing Groundwater Pollution Risk in Response to Climate Change and Variability
next chapter Hydraulic Fracturing and Its Potential Impact on Shallow Groundwater
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Metadata
Title
Deficit Irrigation as a Strategy to Cope with Declining Groundwater Supplies: Experiences from Kansas
Authors
I. Kisekka
J. Aguilar
Copyright Year
2016
Book
Emerging Issues in Groundwater Resources

Print ISBN: 978-3-319-32006-9

Electronic ISBN: 978-3-319-32008-3

Copyright Year: 2016

DOI
https://doi.org/10.1007/978-3-319-32008-3_3