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Solute Transport in a Stream‐aquifer system: 2. Application of model identification to the River Murray
Author(s) -
Jakeman A. J.,
Dietrich C. R.,
Thomas G. A.
Publication year - 1989
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/wr025i010p02177
Subject(s) - aquifer , hydrology (agriculture) , calibration , identification (biology) , salinity , geology , environmental science , variable (mathematics) , soil science , geotechnical engineering , groundwater , mathematics , statistics , oceanography , ecology , mathematical analysis , biology
In paper 1 (Dietrich et al., this issue) a model was derived for the transport of a conservative solute along a stream connected to an aquifer. In this paper the model is applied to a 207‐km reach of the River Murray in Australia. The appropriate model structure and its parameter values are determined using principles of system identification. The major tools applied are instrumental variable estimation techniques. Accurate downstream salinity prediction is obtained on independent data sets not used for model calibration.

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