Skip to main navigation Skip to search Skip to main content

Using multivariate statistical analysis of groundwater major cation and trace element concentrations to evaluate groundwater flow in a regional aquifer

  • University of Nevada, Las Vegas
  • Old Dominion University

Research output: Contribution to journalArticlepeer-review

Abstract

Groundwater samples were collected from 11 springs in Ash Meadows National Wildlife Refuge in southern Nevada and seven springs from Death Valley National Park in eastern California. Concentrations of the major cations (Ca, Mg, Na and K) and 45 trace elements were determined in these groundwater samples. The resultant data were subjected to evaluation via the multivariate statistical technique principal components analysis (PCA), to investigate the chemical relationships between the Ash Meadows and Death Valley spring waters, to evaluate whether the results of the PCA support those of previous hydrogeological and isotopic studies and to determine if PCA can be used to help delineate potential groundwater flow patterns based on the chemical compositions of groundwaters. The results of the PCA indicated that groundwaters from the regional Paleozoic carbonate aquifers (all of the Ash Meadows springs and four springs from the Furnace Creek region of Death Valley) exhibited strong statistical associations, whereas other Dealth Valley groundwaters were chemically different. The results of the PCA support earlier studies, wherepotentiometric head levels, δ18O and δD, geological relationships and rare earth element data were used to evaluate groundwater flow, which suggest groundwater flows from Ash Meadows to the Furnace Creek springs in Death Valley. The PCA suggests that Furnace Creek groundwaters are moderately concentrated Ash Meadows groundwater, reflecting longer aquifer residence times for the Furnace Creek groundwaters. Moreover, PCA indicates that groundwater may flow from springs in the region surrounding Scotty's Castle in Death Valley National Park, to a spring discharging on the valley floor. The study indicates that PCA may provide rapid and relatively cost-effective methods to assess possible groundwater flow regimes in systems that have not been previously investigated.

Original languageEnglish
Pages (from-to)2655-2673
Number of pages19
JournalHydrological Processes
Volume13
Issue number17
DOIs
StatePublished - Dec 15 1999

ASJC Scopus Subject Areas

  • Water Science and Technology

Keywords

  • Ash Meadows
  • Death valley
  • Geochemistry
  • Groundwater
  • Principal components analysis
  • Rare earth elements
  • Trace elements
  • Yucca Mountain

Fingerprint

Dive into the research topics of 'Using multivariate statistical analysis of groundwater major cation and trace element concentrations to evaluate groundwater flow in a regional aquifer'. Together they form a unique fingerprint.

Cite this