Prof. Garry Willgoose
| Work Phone | (02) 4921 6050 |
|---|---|
| Fax | (02) 4921 6991 |
| Garry.Willgoose@newcastle.edu.au | |
| Office | EA131, Engineering A |
Research Supervision
| Number of current supervisions | 7 |
|---|---|
| Total current UoN Masters EFTSL | 3.6 |
| Total current UoN PhD EFTSL | 0.4 |
For supervisions undertaken at an institution other that the University of Newcastle, details are shown in italics, and the institution name is listed below the program name.
Current Supervision
| Commenced | Proposed Completion |
Program | Supervisor Type | Research Title |
|---|---|---|---|---|
| 2013 | 2015 | M Philosophy (Enviro Eng) | Principal Supervisor | A Next Generation Spatially Distributed Model for Soil Profile Dynamics and Pedogenesis Incorporating Soil Geochemistry and Organic Matter |
| 2013 | 2015 | M Philosophy (Civil Eng) | Principal Supervisor | The Influence of East Coast Lows (ECLs) on the Water Security of Coastal New South Wales (NSW) |
| 2013 | 2015 | M Philosophy (Enviro Eng) | Principal Supervisor | Testing the Hydrologic Validity of Downscaled Climate Data for Water Security Assessment |
| 2013 | 2021 | PhD (Environmental Sc) | Co-Supervisor | mARM Pedogenesis Model: Application as a Tool in Precision Agriculture in Eastern New South Wales |
| 2012 | 2014 | M Philosophy (Enviro Eng) | Principal Supervisor | Coal Seam Gas (CSG) Production Challenges Related to Wastewater |
| 2011 | 2013 | M Philosophy (Civil Eng) | Principal Supervisor | A Screening Method for Rural Flash Flooding Risk Assessment |
| 2010 | 2013 | PhD (Environmental Eng) | Principal Supervisor | Carbon Isotopes and Chemistry in Soil Particle-Size fractions at Different Depths: Insight on C Dynamics in Two NSW Forest Soils |
Past Supervision
| Year | Program | Supervisor Type | Research Title |
|---|---|---|---|
| 2013 | PhD (Environmental Eng) | Principal Supervisor | On the Predictability of Hydrology Using Land Surface Models and Field Soil Moisture Data |
| 2010 | PhD (Environmental Sc) | Co-Supervisor | Spatial Description of Soil Properties Through Landscape-Pedogenesis Modelling |
| 2007 | PHD Hydrology University of Melbourne |
Co-Supervisor | Data assimilation of streamflow to estimate catchment soil moisture |
| 2007 | PhD (Civil Surv & Environ Eng) | Co-Supervisor | Aggregation and Disaggregation of Soil Moisture Measurements |
| 2005 | Masters Hydrology University of Leeds |
Principal Supervisor | Design standards for the construction of anthropogenic landforms using the landform evolution model SIBERIA |
| 2005 | Masters Hydrology University of Leeds |
Co-Supervisor | Design rules for use of armour to reduce erosion on mine batter slopes |
| 2005 | Masters Hydrology University of Leeds |
Co-Supervisor | Long term evolution of tailings dam batter slopes |
| 2004 | Masters Hydrology University of Leeds |
Co-Supervisor | Geomorphic analysis of South Yorkshire |
| 2003 | PHD Hydrology Charles Darwin University |
Consultant Supervisor | Erosion at the Jabiluka mine site |
| 2001 | PHD Hydrology University of Newcastle |
Sole Supervisor | Long term soil development on mine spoils |
| 2000 | Masters Hydrology University of Newcastle |
Co-Supervisor | Hydrology of mine spoils |
| 2000 | PHD Hydrology The University of Newcastle |
Co-Supervisor | Remote sensing of soil moisture |
| 1999 | PHD Environmental Engineering The University of Newcastle |
Principal Supervisor | Hydrology of a disturbed estuarine wetland, Hunter River, Australia: Field investigation, process modelling, and management implications |
| 1998 | PHD Civil Engineering The University of Newcastle |
Principal Supervisor | The hydro-geomorphic modelling of saturation excess runoff generation |
| 1997 | PHD Civil Engineering The University of Newcastle |
Principal Supervisor | Experimental testing of the SIBERIA catchment evolution model |
| 1997 | PHD Civil Engineering The University of Newcastle |
Principal Supervisor | Runoff and erosion characteristics of a post-mining rehabilitated landform at Ranger Uranium Mine, Northern Territory, Australia and the implications for its topographic evolution |