John Nimmo
Menlo Park, CA
Activity
2024
-
NUMERICAL MODELING TO AQUIFER RECHARGE TO PREFERENTIAL FLOW--POWERFUL INSIGHTS OF RICK HEALY
76 D8. Groundwater Recharge and Unsaturated-zone Processes at Local and Regional Scales: A Reflection on Rick Healy's LegacyMonday, 23 September 20248:00 AM - 12:00 PM211A
2013
-
PREFERENTIAL FLOW CHARACTERIZATION IN A GEOLOGICALLY COMPLEX UNSATURATED ZONE, IDAHO NATIONAL LABORATORY
T201 Vadose Zone Flow and Transport in Natural or Engineered SystemsTuesday, 29 October 20138:00 AM - 12:00 PMRoom 301
-
HIGH INPUT-SENSITIVITY OF NONCAPILLARY FLOW IN THE UNSATURATED ZONE
T102 Advances in Unsaturated Zone Geophysics and Process UnderstandingMonday, 28 October 20138:00 AM - 12:00 PMRoom 207
-
ASSESSING EFFECTS OF NATIVE REFORESTATION ON SOIL MOISTURE DYNAMICS AND POTENTIAL AQUIFER RECHARGE, AUWAHI, MAUI
T168 Impacts of Land-Use Change and Disturbances on Unsaturated-Zone Ecohydrology and Process CharacterizationMonday, 28 October 20131:00 PM - 5:00 PMRoom 301
-
A COUPLED SOURCE-RESPONSE/RICHARDS-EQUATION MODEL FOR SIMULATING INFILTRATION IN THE PRESENCE OF PREFERENTIAL FLOW PATHS
T102 Advances in Unsaturated Zone Geophysics and Process UnderstandingMonday, 28 October 20138:00 AM - 12:00 PMRoom 207
2010
-
A SOURCE-RESPONSIVE MODELING APPROACH FOR EXAMINING ANTHROPOGENICALLY AUGMENTED RECHARGE AND ACCELERATED CONTAMINANT TRANSPORT AT THE IDAHO NATIONAL LABORATORY (INL)
T8 Impacts of Land Use and Climate Change on Water Resources Sustainability ISunday, 31 October 20108:00 AM - 12:00 PMMile High Ballroom 1AB
2009
-
EXPERIMENTAL AND SIMULATED SOLUTE TRANSPORT AND SHALLOW SUBSURFACE FLOW AT AN AGRICULTURAL SITE IN NORTHWESTERN MISSISSIPPI
3 Hydrogeology I: ChemicalSunday, 18 October 20098:00 AM - 12:00 PME141/142
2008
-
Techniques to Answer Hydrologic Questions of the Unsaturated Zone: Borrow, Adapt, Steal, and Dream
82 Soil Physics and Vadose Zone Hydrology: Our Future ContributionsThursday, 9 October 20088:00 AM - 12:00 PM
-
Subsurface Initiation of Film Flow In Rock Fractures and Soil Macropores
75 Variably Saturated Flow in Soil and Rock: What's the Same, What's Different?Wednesday, 8 October 20088:00 AM - 12:00 PM
-
Contaminant Travel Time Estimates through a Thick Unsaturated Zone at Rainier Mesa and Shoshone Mountain, Nevada
75 Variably Saturated Flow in Soil and Rock: What's the Same, What's Different?Wednesday, 8 October 20088:00 AM - 12:00 PM
-
Unsaturated Hydraulic Properties of Rocks: How to Measure Them In the Laboratory and In the Field?
75 Variably Saturated Flow in Soil and Rock: What's the Same, What's Different?Wednesday, 8 October 20088:00 AM - 12:00 PM
-
Modelling Unsaturated Flow and Transport of Pollutant in a Fractured Limestone Affected by Industrial Sludge Deposits at the Altamura Site (South Italy)
75 Variably Saturated Flow in Soil and Rock: What's the Same, What's Different?Wednesday, 8 October 20088:00 AM - 12:00 PM
2005
-
SPATIAL AND TEMPORAL VARIABILITY OF GROUND-WATER RECHARGE IN MINNESOTA USING MULTIPLE METHODS
15 Ground Water Sustainability IIThursday, 19 May 20051:20 PM - 5:20 PM
2004
-
UNSATURATED-ZONE CASE STUDY AT THE IDAHO NATIONAL ENGINEERING AND ENVIRONMENTAL LABORATORY: CAN DARCIAN HYDRAULIC PROPERTIES PREDICT CONTAMINANT MIGRATION?
T169 Innovative Tracer Applications in Hydrogeology: New Techniques, Design and Interpretation Methods, and Case Studies IITuesday, 9 November 20041:30 PM - 5:30 PM
2003
-
UNSATURATED HYDRAULIC CHARACTERIZATION OF CARBONATIC ROCK IN THE LABORATORY
T14 Karst Hydrology and Geomorphology in North America Over the Past Half Century I: In Honor of Derek Ford and William WhiteSunday, 2 November 20038:00 AM - 12:00 PM
Date Unknown
-
Field Evaluation of Preferential Flow In Agricultural Soils of the Mississippi Delta
67 Subsurface Fate and Transport of Agricultural Contaminants (Posters)