Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Environmental and Engineering Geoscience   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Environmental and Engineering Geoscience; November 1998; v. 4; no. 4; p. 479-489
This Article
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Zhan, H.
Right arrow Articles by McKay, W. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

An assessment of nitrate occurrence and transport in Washoe Valley, Nevada

Hongbin Zhan, and W. Alan McKay

Texas A&M University, Department of Geology and Geophysics, College Station, TX, United States
University and Community College System of Nevada, United States

Using an unsewered subdivision in western Nevada as a field site, the occurrence and transport of nitrate from septic tanks was first studied using nitrogen and nitrate mass balance calculations, and was then simulated by using a solute transport model (MT3D) for two different input scenarios. The results from the transport simulations are compared with the results from the mass balance calculations, which predict that average nitrate concentrations are rarely above the federal drinking water standard of 10 mg/I NO 3 -N in the study area. The simulation using a uniform nitrogen-to-nitrate conversion ratio provides greater detail of nitrate behavior, but results are not compatible with observed values in portions of the study area. Hydrogeochemical data suggest that the study area is characterized by zones of contrasting redox conditions and associated contrasts in nitrogen speciation. These variable geochemical conditions provide the basis for regionalizing nitrogen-->nitrate conversion ratios in the simulations. Resulting simulations are improved, and agree better with observed field data. We also address the capabilities and limitations of transport simulations. The limitations of simulations originated from the incomplete input information related to field conditions even though the adopted models (MODFLOW and MT3D) are robust themselves.

This record provided courtesy of AGI/GeoRef.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Association of Engineering Geologists