G R Hancock
Biographic Data
| ID | 3759359 |
|---|---|
| NAME | G R Hancock |
| GIVEN NAMES | G R |
| FAMILY NAME | Hancock |
| SIGNATURE | HANCOCK G R |
| AFFILIATIONS | University of Newcastle Australia |
| ORCID | 0000-0002-1619-1265 |
| VERIFIED | Yes |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Evaluating Erosional Stability of Reconstructed Mine Landscapes Using Landform Evolution Models
Ensuring the long‐term erosional stability of post‐mining landforms remains a major challenge in open‐pit mining. Reconstructed landscapes must support the agreed post‐mining land use, such as cattle grazing in the Hunter region of southeastern Australia, requiring stable pasture and minimal soil loss. Numerical modelling is widely used to evaluate landform stability, but continued development and validation of landform evolution models (LEMs) ac…
Quantifying the Role of Vegetation in Reducing Erosion on Post‐Mining Landforms
For post‐mining landscapes, erosion rates need to be demonstrably similar to that of the surrounding areas. Post‐mining landscapes are assessed (usually with a numerical model) to determine their erosion potential both in the pre‐ and post‐construction phases. Field plots, which rely on natural rainfall, provide the most reliable data; however, it can take many years for a reliable data set to become available. They are also costly to install and…
Temporal stability of soil organic carbon in grazing lands of Eastern Australia
Sequestering soil organic carbon (SOC) has been identified as a critical tool to mitigate anthropogenic climate change. Therefore, the response of SOC to climate variability needs to be quantified to achieve carbon sequestration over decadal to centennial scales. This study assesses the temporal variability of SOC for a grazed catchment in Australia that has been exposed to periods of drought and flood over the last 100 years. The analysis utilis…
Soil–landscape response to mid and late Quaternary climate fluctuations based on numerical simulations
We use a numerical dynamic soil–landscape model to study one aspect of the spatio-temporal soil–landscape evolution process, the effect of climatic fluctuations on soil grading distribution in space and time in response to the interplay between physical weathering and surface erosion (soil mineralogical fluxes). We simulate a synthetic soil–landscape system over the middle and late Quaternary (last 400 ka). The results show that (1) soil–landscap…
Implementing Instruction in the Alphabetic Principle Within a Sign Bilingual Setting
The purpose of the present study was to examine the results of implementing remedial instruction in the alphabetic principle with deaf and hard-of-hearing (DHH) students educated in a sign bilingual setting. Data were analyzed in 2 phases, with the first using paired-sample t tests and Pearson correlations and the second phase employing structural equation modeling. Results indicate that study participants (N = 127) from a range of grade placemen…
Estimation of Soil Erosion Using Field and Modelling Approaches in an Undisturbed Arnhem Land Catchment, Northern Territory, Australia
An assessment of slope erosion at Tin Camp Creek catchment, Arnhem Land, Northern Territory, Australia, was carried out using the fallout environmental radioisotope caesium-137 (137Cs) as an indicator of soil erosion status, two numerical models (SIBERIA and the Revised Universal Soil Loss Equation (RUSLE)) and erosion pins. This undisturbed drainage basin is situated in the seasonally wet-dry tropics, with high energy storms and a mean annual ra…
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Estimation of Soil Erosion Using Field and Modelling Approaches in an Undisturbed Arnhem Land Catchment, Northern Territory, Australia
An assessment of slope erosion at Tin Camp Creek catchment, Arnhem Land, Northern Territory, Australia, was carried out using the fallout environmental radioisotope caesium-137 (137Cs) as an indicator of soil erosion status, two numerical models (SIBERIA and the Revised Universal Soil Loss Equation (RUSLE)) and erosion pins. This undisturbed drainage basin is situated in the seasonally wet-dry tropics, with high energy storms and a mean annual ra…
Soil–landscape response to mid and late Quaternary climate fluctuations based on numerical simulations
We use a numerical dynamic soil–landscape model to study one aspect of the spatio-temporal soil–landscape evolution process, the effect of climatic fluctuations on soil grading distribution in space and time in response to the interplay between physical weathering and surface erosion (soil mineralogical fluxes). We simulate a synthetic soil–landscape system over the middle and late Quaternary (last 400 ka). The results show that (1) soil–landscap…
Implementing Instruction in the Alphabetic Principle Within a Sign Bilingual Setting
The purpose of the present study was to examine the results of implementing remedial instruction in the alphabetic principle with deaf and hard-of-hearing (DHH) students educated in a sign bilingual setting. Data were analyzed in 2 phases, with the first using paired-sample t tests and Pearson correlations and the second phase employing structural equation modeling. Results indicate that study participants (N = 127) from a range of grade placemen…
Temporal stability of soil organic carbon in grazing lands of Eastern Australia
Sequestering soil organic carbon (SOC) has been identified as a critical tool to mitigate anthropogenic climate change. Therefore, the response of SOC to climate variability needs to be quantified to achieve carbon sequestration over decadal to centennial scales. This study assesses the temporal variability of SOC for a grazed catchment in Australia that has been exposed to periods of drought and flood over the last 100 years. The analysis utilis…
Quantifying the Role of Vegetation in Reducing Erosion on Post‐Mining Landforms
For post‐mining landscapes, erosion rates need to be demonstrably similar to that of the surrounding areas. Post‐mining landscapes are assessed (usually with a numerical model) to determine their erosion potential both in the pre‐ and post‐construction phases. Field plots, which rely on natural rainfall, provide the most reliable data; however, it can take many years for a reliable data set to become available. They are also costly to install and…
Evaluating Erosional Stability of Reconstructed Mine Landscapes Using Landform Evolution Models
Ensuring the long‐term erosional stability of post‐mining landforms remains a major challenge in open‐pit mining. Reconstructed landscapes must support the agreed post‐mining land use, such as cattle grazing in the Hunter region of southeastern Australia, requiring stable pasture and minimal soil loss. Numerical modelling is widely used to evaluate landform stability, but continued development and validation of landform evolution models (LEMs) ac…
Environmental Science (4 works) · Soil erosion and sediment transport (4 works) · Erosion (3 works) · Geography (3 works) · Geology (3 works) · Geomorphology (3 works) · Soil Science (3 works) · Soil water (3 works) · Climate change (2 works) · Geology (2 works)