Variations in flow and transport in thick desert vadose zones in response to paleoclimatic forcing (0–90 kyr): Field measurements, modeling, and uncertainties
- 10 July 2003
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 39 (7)
- https://doi.org/10.1029/2002wr001604
Abstract
No abstract availableThis publication has 39 references indexed in Scilit:
- Testing a full-range soil-water retention function in modeling water potential and temperatureWater Resources Research, 2000
- UNSAT-H Version 3.0:Unsaturated Soil Water and Heat Flow Model: Theory, User Manual, and ExamplesPublished by Office of Scientific and Technical Information (OSTI) ,2000
- Uses of Chloride/Bromide Ratios in Studies of Potable WaterGroundwater, 1998
- Soil‐water movement under natural‐site and waste‐site conditions: A multiple‐year field study in the Mojave Desert, NevadaWater Resources Research, 1997
- Properties and Variability of Soil and Trench Fill at an Arid Waste‐Burial SiteSoil Science Society of America Journal, 1996
- Diffusion And Flow In Gravel, Soil, And Whole RockHydrogeology Journal, 1992
- Sediment properties and water movement through shallow unsaturated alluvium at an arid site for disposal of low-level radioactive waste near Beatty, Nye County, NevadaPublished by US Geological Survey ,1992
- Chronology of expansion and contraction of four great Basin lake systems during the past 35,000 yearsPalaeogeography, Palaeoclimatology, Palaeoecology, 1990
- Soil heat and water flow with a partial surface mulchWater Resources Research, 1987
- Enhancement of Thermal Water Vapor Diffusion in SoilSoil Science Society of America Journal, 1984