scholarly journals Water quality in the Las Vegas Valley area and the Carson and Truckee River basins, Nevada and California, 1992-96

Circular ◽  
1998 ◽  
Author(s):  
Hugh E. Bevans ◽  
Michael S. Lico ◽  
Stephen J. Lawrence
Keyword(s):  
Water Quality ◽  
Las Vegas ◽  
River Basins ◽  
Truckee River ◽  
Las Vegas Valley ◽  
Valley Area

scholarly journals Inverse modeling using PS-InSAR for improved calibration of hydraulic parameters and prediction of future subsidence for Las Vegas Valley, USA

2015 ◽  
Vol 372 ◽  
pp. 411-416 ◽  
Author(s):  
T. J. Burbey ◽  
M. Zhang
Keyword(s):  
Model Calibration ◽  
Surface Deformation ◽  
Las Vegas ◽  
Water Levels ◽  
Mitigation Measures ◽  
Hydraulic Parameters ◽  
Las Vegas Valley ◽  
The North ◽  
History Of ◽  
Valley Area

Abstract. Las Vegas Valley has had a long history of surface deformation due to groundwater pumping that began in the early 20th century. After nearly 80 years of pumping, PS-InSAR interferograms have revealed detailed and complex spatial patterns of subsidence in the Las Vegas Valley area that do not coincide with major pumping regions. High spatial and temporal resolution subsidence observations from InSAR and hydraulic head data were used to inversely calibrate transmissivities (T), elastic and inelastic skeletal storage coefficients (Ske and Skv) of the developed-zone aquifer and conductance (CR) of the basin-fill faults for the entire Las Vegas basin. The results indicate that the subsidence observations from PS-InSAR are extremely beneficial for accurately quantifying hydraulic parameters, and the model calibration results are far more accurate than when using only water-levels as observations, and just a few random subsidence observations. Future predictions of land subsidence to year 2030 were made on the basis of existing pumping patterns and rates. Simulation results suggests that subsidence will continue in northwest subsidence bowl area, which is expected to undergo an additional 11.3 cm of subsidence. Even mitigation measures that include artificial recharge and reduced pumping do not significantly reduce the compaction in the northwest subsidence bowl. This is due to the slow draining of thick confining units in the region. However, a small amount of uplift of 0.4 cm is expected in the North and Central bowl areas over the next 20 years.

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