Water in the unsaturated zone
Read Online
Share

Water in the unsaturated zone L"eau dans la zone non saturée; proceedings of the Wageningen Symposium by Symposium on Water in the Unsaturated Zone Wageningen 1966.

  • 908 Want to read
  • ·
  • 24 Currently reading

Published by IASH/AIHS in [Gentbrugge, Belgium] .
Written in English

Subjects:

  • Groundwater -- Congresses.,
  • Soil moisture -- Congresses.

Book details:

Edition Notes

Other titlesL"eau dans la zone non saturée.
Statementedited by P. E. Rijtema and H. Wassink.
SeriesStudies and reports in hydrology, 2
ContributionsRijtema, P. E., ed., Wassink, H., ed., Unesco.
Classifications
LC ClassificationsGB1005 .S93 1966
The Physical Object
Pagination2 v.
ID Numbers
Open LibraryOL5473823M
LC Control Number73177081

Download Water in the unsaturated zone

PDF EPUB FB2 MOBI RTF

The unsaturated zone, often called the vadose zone, is the portion of the subsurface above the water table. It contains, at least some of the time, air as well as water in the pores. Its thickness can range from zero, as when a lake or marsh is at the surface, to hundreds of meters, as is common in arid regions. These models helped improve our understanding of unsaturated-zone processes and develop sustainable land-management practices. Aimed at professional soil scientists, soil-water modelers, irrigation engineers etc., this book discusses our progress in soil-water modeling. Above the water table - the soil and rock in this zone contains air and water. Some places don't have unsaturated zones, like marshes, and other places have unsaturated zones . Documentation of the Unsaturated-Zone Flow (UZF1) Package for Modeling Unsaturated Flow Between the Land Surface and the Water Table with MODFLOW Techniques and Methods 6-A19 A Product of the Ground-Water Resources Program U.S. Department of the Interior U.S. Geological Survey Chapter 19 of Section A, Ground Water, of Book 6, Modeling.

unsaturated zone, immediately below the land surface, contains water and air in the open spaces, or pores. The saturated zone, a zone in which all the pores and rock fractures are filled with water, underlies the unsaturated zone. The top of the saturated zone is called the water table (Diagram 1). The water table may be just below or hundreds.