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- W82969948 abstract "This repo rt dese ribes the deve lopm!'!nt. cali bJ;'Bt ion and use of a quantitative. predictive management model for the groundwater in the Utah portion of the Cache Valley in northern Utah. The quasi-three-dimensional finite difference computer model was adapted from the u.s. Geological Survey's TJ:'escott and Larson mode 1 and simulates the groundwater levels and fl OWB in the gt'ollndW'at.~t basin. The variab Ie s'Pa~ing glid systew is 23 nodes x 38 x 2 and represents the complex natural system by a simpler approximation with one unconfined and one confined aquife r and the. appropriate bounds ry and iai t ial cond it ions. River nodes, spring nodes. and constant head nodes were developed to simulate the real interactions of the aquifers with streams, springs, and reservoirs. EvapotranspiJ:'ation from the land surface is also represented by t he program. The program. was calibrated by adjusting the model pal':'ameteJ:'s such e.s transmissivity) storativity) teakance. I:'iver nodes) spring nodes) etc. until the predicted values of head and flow wet'e nearly the same as the observed conditions. Calibration was done in two stages: first a steady-state comparison with 1969 conditions and tben a transient-state comparison with the water level change maps of 1969 to 1972. The calibrated model w~s then eKercised to predict the grouo.dwater 5YS tem response to various assumed scenarios of groundwate~ recharge and draft. Thus the model pt'ovides a cool to guide future groundwater developmenr:: and management towards the best alternatives." @default.
- W82969948 created "2016-06-24" @default.
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- W82969948 date "1984-01-01" @default.
- W82969948 modified "2023-09-27" @default.
- W82969948 title "A Groundwater Model of Cache Valley, Utah" @default.
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