0000000000555494

AUTHOR

Daniel M. Hammes

showing 4 related works from this author

Reconstruction of 3D grain boundaries from rock thin sections, using an advanced polarised-light microscopy method

2017

Grain boundaries play a significant role in materials by initiating reactions and collecting impurities. Here we present FAGO (Fabric Analyser Grain boundary recOnstruction), a first step towards the automatic determination of three-dimensional (3D) grain boundary geometry using polarised light. The trace of the grain boundaries from 2D rock thin sections are determined primarily from data acquired using an automatic fabric analyser microscope and the FAME software (fabric analyser-based microstructure evaluation; Peternell and colleagues and Hammes and Peternell). Based on the Fabric Analyser G50's unique arrangement of nine differently oriented light sources the retardation can be determi…

HistologyMaterials scienceMicroscope010504 meteorology & atmospheric sciencesPixelOrientation (computer vision)AnalyserMineralogyField of viewGeometry010502 geochemistry & geophysicsMicrostructure01 natural sciencesPathology and Forensic Medicinelaw.inventionlawMicroscopyGrain boundary0105 earth and related environmental sciencesJournal of Microscopy
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Strain rate dependence for evolution of steady state grain sizes: Insights from high-strain experiments on ice

2019

Abstract Understanding of the microstructural evolution and equilibrium grain size development during steady state tertiary flow is essential in order to improve our knowledge of ice and rock deformation. This contribution presents results from in situ transmitted light deformation experiments of natural glacier ice, with the development of the microstructure in a tertiary flow regime. We conducted one relative slower ( 1 × 10 − 6 1/s) and two relative faster-strain rate ( 2 × 10 − 6 1/s) pure shear experiments at −10 °C, up to a shortening of ∼57%. Microstructure development was followed by time-lapse observations, and two new microstructure-based indicators, the ‘seeding rate’ and the ‘mi…

010504 meteorology & atmospheric sciencesMechanicsSlip (materials science)Pure shearStrain rate010502 geochemistry & geophysicsMicrostructure01 natural sciencesGrain sizeGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyParticle-size distributionEarth and Planetary Sciences (miscellaneous)SeedingGeology0105 earth and related environmental sciencesStress concentrationEarth and Planetary Science Letters
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FAME: Software for analysing rock microstructures

2016

Determination of rock microstructures leads to a better understanding of the formation and deformation of polycrystalline solids. Here, we present FAME (Fabric Analyser based Microstructure Evaluation), an easy-to-use MATLAB®-based software for processing datasets recorded by an automated fabric analyser microscope. FAME is provided as a MATLAB®-independent Windows® executable with an intuitive graphical user interface. Raw data from the fabric analyser microscope can be automatically loaded, filtered and cropped before analysis. Accurate and efficient rock microstructure analysis is based on an advanced user-controlled grain labelling algorithm. The preview and testing environments simplif…

010504 meteorology & atmospheric sciencesComputer sciencebusiness.industryOrientation (computer vision)AnalyserComputingMethodologies_IMAGEPROCESSINGANDCOMPUTERVISIONcomputer.file_format010502 geochemistry & geophysics01 natural sciencesVisualizationSoftwareComputer graphics (images)Batch processingExecutableComputers in Earth SciencesbusinesscomputerSimulation0105 earth and related environmental sciencesInformation SystemsRock microstructureGraphical user interfaceComputers & Geosciences
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Experimental deformation of deuterated ice in 3D and 2D: identification of grain-scale processes

2015

Major polar ice sheets and ice caps experience cycles of variable flow during different glacial periods and as a response to past warming. The rate and localisation of deformation inside an ice body controls the evolution of ice microstructure and crystallographic fabric. This is critical for interpreting proxy signals for climate change, with deformation overprinting and disrupting stratigraphy deep under ice caps due to the nature of the flow. The final crystallographic fabric in polar ice sheets provides a record of deformation history, which in turn controls the flow properties of ice during further deformation and affects geophysical sensing of ice sheets. For example, identification o…

geography.geographical_feature_categoryEcologyMeteorologyClimate changeGeologyGeophysicsGrain sizeProxy (climate)Physics::GeophysicsIce-sheet modelGeographyAstrophysics::Earth and Planetary AstrophysicsGlacial periodClimate stateLayeringIce sheetPhysics::Atmospheric and Oceanic PhysicsProceedings of the Royal Society of Victoria
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