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A new method for predicting transient states of salinity intrusion into the Sacramento-San Joaquin Delta

dc.contributor.authorGlover, Robert E., author
dc.contributor.authorAmerican Geophysical Union, publisher
dc.date.accessioned2022-10-31T17:45:14Z
dc.date.available2022-10-31T17:45:14Z
dc.date.issued1955-08
dc.descriptionReprint from Transactions, American Geophysical Union, V. 36, Number 4, August 1955.
dc.descriptionIncludes bibliographical references.
dc.description.abstractThe mechanism by which the tidal changes propagate salinity into the Delta channels and the manner in which this propagation is opposed by the fresh water stream flows are expressed in mathematical form. Solutions of the basic differential equation are given which are suitable for computation of salinity changes and a method of computation is described. As an example of the use of these methods they are applied to the historical records to determine a depletion curve for the Delta by using the observed salinities as an indicator and finding the flows out of the Delta which were necessary to hold the salinities to the observed amounts. While the primary usefulness of this depletion curve is to form a basis for further estimates of ocean salinity encroachment, it is compared to use curves derived from independent sources.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/235819
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991011952699703361
dc.relationTA7.C6 CER 58-12
dc.relation.ispartofCivil Engineering Reports
dc.relation.ispartofCER, 58-12
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subject.lcshSaltwater encroachment -- Mathematical models
dc.subject.lcshSaltwater encroachment -- California -- Delta Region
dc.subject.lcshSaltwater encroachment
dc.subject.lcshSalinity
dc.titleA new method for predicting transient states of salinity intrusion into the Sacramento-San Joaquin Delta
dc.typeText
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