Geological and Soil Evidence: Forensic ApplicationsThe forensic potential of geological and soil evidence has been recognized for more than a century, but recently these types of evidence are used much more widely as an investigative intelligence tool and as evidence in court. There is, however, still a poor understanding of the potential value and the limitations of geological and soil evidence am |
Contents
1 | |
Chapter 2 Types of Geological and Soil Materials That May be Useful as Trace Evidence | 11 |
Chapter 3 Bulk Properties of Geological and Soil Materials | 59 |
Chapter 4 Properties of Individual Particles | 119 |
Chapter 5 Sampling and Sample Handling | 183 |
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150 µm fraction analysis analyzed angular Arborfield Arborfield Bridge assemblage AVON beach carbonate cathodoluminescence chemical clay minerals color COMET compared comparison contain control samples crime scene Croft database degree density determined diagenesis diameter diatom dust electron environmental examination example Figure foraminifera forensic geology Forensic palynology Forensic Science forensic soil fragments geochemical geological and soil gravel particles groups heavy mineral ICP-AES ICP-MS identified Igneous Rocks laser mass spectrometry material measure metamorphic method microscope mineralogical murder nature obtained ooids optical parameters particle size distribution particle types Petrology Phytoliths pollen potential properties quartz questioned sample Raman spectroscopy range relatively rocks sand grains scale Sedimentary sediments sediments and soils shoe significant silt similar soil evidence soil samples taken Soil Science soils and sediments spectrometry sphericity statistical surface texture suspect Table techniques trace elements trace evidence values variability variation x-ray
Popular passages
Page 279 - Clark. JS (1988a). Particle motion and the theory of charcoal analysis: source area, transport, deposition, and sampling. Quaternary Research 30, 67-80. Clark, JS (19886).
Page 287 - Mazzullo, 1988. The original shapes of quartz silt grains: a test of the validity of the use of quartz grain shape analysis to determine the sources of terrigenous silt in marine sedimentary deposits.
Page 295 - Pb-206/U-238 age determination on zircons by laser ablation microprobe-inductively coupled plasma-mass spectrometry using continuous linear ablation.