Micromeritics SediGraph. Particle Size Data based on Consolidated Certainties
|
|
- Whitney Williamson
- 6 years ago
- Views:
Transcription
1 Micromeritics SediGraph Particle Size Data based on Consolidated Certainties Dr. Michael Frenz Pedology Workshop Napoli,
2 Outline Size This! Particle Size is a Relative Attribute! Comparison between Methods SediGraph Method Examples from the Atlantic Ocean Saturn DigiSizer II 525 Particle Insight Image Analyser Summary
3 Size this!
4 Size this!
5 Courtesy: C. Vogt, ZEKAM, University Bremen
6 Micromeritics Techniques SediGraph Saturn Elzone Particle Insight
7 Glass beads D1 D5 D9 Mode µm µm µm µm 41, 61,6 89,1 63,1 45, 66,9 85, 71,1 45,1 61,7 75,9 67,1 49,5 66,5 82,4 72,4
8 Garnet D1 D5 D9 Mode µm µm µm µm 16,4 25,4 4,8 25,1 2,1 32,4 53,4 31,8 21,9 29,8 42,8 28,5 19,7 25,6 33,8 24,9
9 Wollastonite D1 D5 D9 Mode µm µm µm µm 2,7 8,3 18,4 1, 2,9 12,7 53,5 13,4 11,7 23,6 41,3 25,7 5,5 11,1 18,9 12,5
10 Mica D1 D5 D9 Mode µm µm µm µm 1,5 1,9 27,4 16,8 1,4 14, 39,5 28, 8, 17, 35,2 18,2 1,8 14, 28,9 16,1
11 Kaolinite Courtesy: C. Vogt, ZEKAM, University Bremen D1 D5 D9 Mode µm µm µm µm -,35 1,5,38,12,65 3,82,42 Top-Cut ~3 µm: 99% <3 µm SediGraph 85% <3 µm Saturn
12 SediGraph Method X-ray Detector X-ray Source Attenuated X-ray beam Cell
13 X-ray Intensity (kc/s) SediGraph Method Highest Concentration Reference Cell Position (cm)
14 SediGraph III 512 Sedimentation Simple, well understood Theory: Lambert-Beer Law, Stokes Law Representative sample amount Range,1-3 µm Weight-% <d min High Resolution Easy Maintenance
15 SediGraph Data in Sedimentology Examples from Suolo di Mare
16 Water Wassertiefe Depth (m) (m) Alter Age (ka) Terr. Silt ( ) Estimating Current Velocities from Particle Size Terr. Silt ( ) VC Today 18 ka BP NADW AABW 45 5 Ledbetter & Johnson 1976 Vema Channel
17 Frequency Estimating Current Velocities from Particle Size Sortable Silt Current Velocity < 5 cm/s 1-15 cm/s > 15 cm/s Particle Size (µm) Robinson & McCave 1994, McCave et al Rockall Plateau
18 Unravel Sediment Input Smith & Sandwell (1997), Wessel & Smith (1998)
19 Water Depth (m) Latitude Unravel Sediment Input -2 Water Mass Distribution BC AABW NADW Antarctic Bottom Water North Atlantic Deep Water -3 MC Malvinas- (Falkland-) Current -4 MC B M C AABW Argentinien- Becken BC BMC MC Brazil Current Brasil-Malvinas-Confluence BMC NADW AABW BC Longitude Modified from Piola & Matano 21
20 Wassertiefe (m) Unravel Sediment Input -2 B B CaCO 3 (wt-%) C org (wt-%) A A A B A B Frenz et al. 24
21 Frequency Haufigkeit (wt-% (% /,1 /,1 ) ) 8 Unravel Sediment Input EM1: Bottom & Residual Sediment Korngröße (µm) Particle Size (µm) B % A A B Korngröße ( ) Particle Size ( ) Frenz et al. 24
22 Frequency Haufigkeit (wt-% (% /,1 /,1 ) ) Unravel Sediment Input EM2: Coarse Suspension Korngröße (µm) Particle Size (µm) B % A A B Korngröße ( ) Particle Size ( ) Frenz et al. 24
23 Frequency Haufigkeit (wt-% (% /,1 /,1 ) ) Differentiate Sediment Input EM3: Fine Suspension Korngröße (µm) Particle Size (µm) B % A A B Korngröße ( ) Particle Size ( ) Frenz et al. 24
24 Quantifying Carbonate Smith & Sandwell (1997), Wessel & Smith (1998) Frenz et al. 25
25 Häufigkeit Frequency (Gew.-% (wt-% / /,1 ) ) Differentiating Particle Size of Components Particle Size (µm) Korngröße (µm) Terrigenous Silt Bulk (TS) Silt Korngröße ( ) Particle Size ( ) Paull et al. 1988, Robinson & McCave 1994, Frenz et al. 25
26 Häufigkeit Frequency (Gew.-% (wt-% / /,1 ) ) Differentiating Particle Size of Components Particle Size (µm) Korngröße (µm) Carbonate Silt 1 TS relative (21%) Korngröße ( ) Particle Size ( ) Paull et al. 1988, Robinson & McCave 1994, Frenz et al. 25
27 Häufigkeit Frequency (Gew.-% (wt-% /,1 ) Quantifying Carbonate Equatorial MAR Central MAR Southern MAR Particle Size (µm) Korngröße (µm) Korngröße ( ) Particle Size ( ) Frenz et al. 25
28 Quantifying Carbonate Silt 5 µm 1 µm Clay 5 µm 5 µm Frenz et al. 24
29 Quantifying Carbonate Silt 5 µm 1 µm Silt 5 µm 1 µm Frenz et al. 24
30 Breite Quantifying Carbonate Foraminifer Carbonate Coccolith Carbonate Länge wt-% Länge Frenz et al. 25
31 Wassertiefe Water Depth (m) (m) Häufigkeit Frequency (Gew.-% (wt-% /,1 ) Quantifying Carbonate Modalkorngröße (µm) Modal Particle Size (µm) CaCO 3 Dissolution Modal Particle Size ( ) Modalkorngröße ( ) Particle Size (µm) Korngröße (µm) Korngröße ( ) Particle Size ( ) Frenz et al. 25, Frenz & Henrich 27
32 Quantifying Carbonate E. huxleyi Nominal Size 1 µm Frenz et al. 25
33 Häufigkeit (Gew.-% /,1 ) Häufigkeit Quantifying Carbonate Korngröße (µm) F. profunda E. huxleyi U. sibogae H. carteri R. clavigera C. leptoporus (A+C) Electron Microscope C. leptoporus (B) 6 4 SediGraph Deconvolution Korngröße ( ) Frenz et al. 25
34 Breite Häufigkeit (Gew.-%) 1 Quantifying Carbonate Korngröße (µm) Länge Korngröße ( ) Frenz et al. 25
35 Laser Light Scattering Mie-Theory Reflection Diffraction Refraction Scattering pattern Intensity vs Angle
36 Saturn DigiSizer II 525 Highlights: Detector: CCD 3,4 Megapixel 14 angle positions (-65 ), multiple exposure High resolution from low to high angles 591 real data points (intensity vs angle) Range:,4 µm 25 µm Optional AquaPrep degasser
37 Saturn DigiSizer II 525 Highlights: Detector: CCD 3,4 Megapixel 14 angle positions (-65 ), multiple exposure High resolution from low to high angles 591 real data points (intensity vs angle) Range:,4 µm 25 µm Optional AquaPrep degasser
38 Relative Intensity Saturn DigiSizer II 525 Measured Intensity Model Intensity Calcium Carbonate Goodness of Fit Reference Material Weighted Residual =.19%
39 Incremental Volume Percent Saturn DigiSizer II 525 Test 3 Test 1 Test 2 Calcium Carbonate Reference Material Incremental Volume Percent vs. Particle Diameter Gra
40 Relative Intensity Saturn DigiSizer II 525 Goodness of Fit 5, Measured Intensity Model Intensity Weighted Residual =.76% Glass Beads & µm 1, 5, 1,
41 Incremental Volume Percent Saturn DigiSizer II Test 4 Test 1 Test 2 Test 3 Glass Beads & µm Incremental Volume Percent vs. Particle Diameter Graph
42 Relative Intensity 1 Saturn DigiSizer II 525 Measured Intensity Model Intensity Goodness of Fit 16 µm Latex Weighted Residual = 8.38% 1, 1, 1 1
43 Incremental Volume Percent Saturn DigiSizer II 525 Test 8 Test 1 Test 2 Test 3 Test 4 Test 5 Test 6 Test 7 16 µm Latex Incremental Volume Percent vs. Particle Diameter Gra
44 Particle Insight Particle Size & Particle Shape Dynamic digital image analysis Up to 3 frames per second 28 particle size and shape models in real time Sample re-circulation Telecentric Lense Working range 3-3 (8-8) µm Comprehensive post-run data reduction
45 Post-run Processing: Thumbnails Parameter distributions Correlation plots Particle Insight
46 Summary Size matters! Method matters! Hydrodynamic Size in Geosciences Resolution matters! Applications: Unraveling Sediment Input and Distribution Differentiating and Quantifying Components Deconvoluting Microfossil Species Tracking Carbonate Dissolution Micromeritics: Four high-resolution Methods Sedimentation: SediGraph III 512 Laser Light Scattering: Saturn DigiSizer II 525 Image Analysis: Particle Insight Electric Sensing: ElZone 539
47 Grazie!
PARTICLE SIZE ANALYTICAL RANGES AND APPLICABILITY. m mm (10-6 m) nm (10-9 m)
P A R T I C L E S I Z E A N A L Y S I S PARTICLE SIZE Accurately determining particle size has become essential in many industries, as it is a fundamental physical characteristic that must be selected,
More informationRatio of coccolith CaCO 3 to foraminifera CaCO 3 in late Holocene deep sea sediments
PALEOCEANOGRAPHY, VOL. 24,, doi:10.1029/2009pa001731, 2009 Ratio of coccolith CaCO 3 to foraminifera CaCO 3 in late Holocene deep sea sediments Wallace Broecker 1 and Elizabeth Clark 1 Received 30 December
More informationGeoffrey (Jake) Gebbie Research Associate, Harvard University Visiting Scientist, MIT
Our basic understanding of past ocean circulation Geoffrey (Jake) Gebbie Research Associate, Harvard University Visiting Scientist, MIT ACDC Summer School, 5 June 2009 The view down a borehole (Helen Freeman,
More informationHolographic Characterization of Agglomerates in CMP Slurries
Holographic Characterization of Agglomerates in CMP Slurries Total Holographic Characterization (THC) Comparison of THC to other technologies Dynamic Light Scattering (DLS) Scanning Electron Microscopy
More informationI. CALCIUM-CARBONATE AND SAND-FRACTION ANALYSIS OF CENOZOIC AND MESOZOIC SEDIMENTS FROM THE MOROCCAN BASIN
I. CALCIUM-CARBONATE AND SAND-FRACTION ANALYSIS OF CENOZOIC AND MESOZOIC SEDIMENTS FROM THE MOROCCAN BASIN Marthe Melguen, Centre Océanologique de Bretagne, BP, 9 Brest Cedex, France INODUCTION As the
More informationAn Investigation of Antarctic Circumpolar Current Strength in Response to Changes in Climate. Presented by Matt Laffin
An Investigation of Antarctic Circumpolar Current Strength in Response to Changes in Climate Presented by Matt Laffin Presentation Outline Introduction to Marine Sediment as a Proxy Introduction to McCave
More informationRefractive index determination of single sub micrometer vesicles in suspension using dark field microscopy
Refractive index determination of single sub micrometer vesicles in suspension using dark field microscopy Edwin van der Pol 1,2 Frank Coumans 1,2, Anita Böing 2, Auguste Sturk 2, Rienk Nieuwland 2, and
More informationQbD QUANTITATIVE MEASUREMENTS OF CQAS IN SOLID DOSAGE FORM UNIT OPERATIONS
QbD QUANTITATIVE MEASUREMENTS OF CQAS IN SOLID DOSAGE FORM UNIT OPERATIONS Particle Size Material Segregation-Flow USP USP USP Ph. Eur. 2.9.31 Ph. Eur. 2.9.36 JP 1 JP 18 Light Diffraction
More informationThis is start of the single grain view
SOIL TEXTURE, PARTICLE SIZE DISTRIBUTION, SPECIFIC SURFACE AND CLAY MINERALS We will assess the physical realm of soil science in a piecewise fashion starting with the physical phases of soil, -- a single
More informationGSA DATA REPOSITORY
GSA DATA REPOSITORY 2011084 Anderson Data Repository Table DR1: Bison Lake Geochronological Data Core Depth (cm) Material Lab number Measured age ( 14 C yr B.P.) Calibrated 1-sigma age ranges & (relative
More informationMinimal change in Antarctic Circumpolar Current flow speed between the last glacial and Holocene
Minimal change in Antarctic Circumpolar Current flow speed between the last glacial and I.N. McCave, S.J. Crowhurst, G. Kuhn, C-D. Hillenbrand and M.P. Meredith Methods Cores Twelve cores forming the transect
More informationProcesses affecting continental shelves
Marine Sediments Continental Shelves Processes affecting continental shelves 1. Glaciation 2. Sea-level change (±130 m during continental glaciation) 3. Waves and currents 4. Sedimentation 5. Carbonate
More information*To whom correspondence should be addressed: FAX: (886) ;
DATA REPORT: CARBONATE AND ORGANIC CARBON CONTENTS OF SEDIMENTS FROM SITES 1143 AND 1146 IN THE SOUTH CHINA SEA Li-Wen Wang* and Hui-Ling Lin Institute of Marine Geology and Chemistry National Sun Yat-Sen
More informationAnnouncements. First problem set due next Tuesday. Review for first exam next Thursday. Quiz on Booth (1994) after break today.
Announcements First problem set due next Tuesday. Review for first exam next Thursday. Quiz on Booth (1994) after break today. Intertidal, Lowes Cove, ME Marine Sediments: Clues to the ocean s past There
More informationA bit of background on carbonates. CaCO 3 (solid)
A bit of background on carbonates CaCO 3 (solid) Organisms need both carbon dioxide and carbonate Kleypas et al 2005 The two pumps put CO 2 into the deep ocean The long term record of climate change Or:
More information1 Millimeter. 1 Micron. 1 Nanometer. 1 Angstrom ELECTRON SEPARATION PROCESS COMMON MATERIALS PARTICLE SIZE LOG SCALE MAGNETIC RANGE SPECTRUM
HANDOUT 3. Millimeter Micron Nanometer Angstrom 00 APPROX. MOLEC. WT. 0 000 00 0 000 00 0 8 7 6 5 4 3 2 0 Radio waves Infrared Ultraviolet Visible X-rays MACRO MICRO MOLECULAR IONIC MOLECULE MACRO 200k
More informationA Broecker Brief Origin of the Atlantic s glacial age lower deep water
A Broecker Brief Origin of the Atlantic s glacial age lower deep water Today s deep Atlantic shows no hint of nutrient stratification (see Figure 1). By contrast, during the last glacial maximum (LGM),
More informationJim Hagerman 4/12/99
This is an electro-optical analysis of the UCMS (underwater camera mapping system) designed for TerraSystems. Jim Hagerman 4/1/99 For simplicity the SNR of only one 5nm wide channel near 5nm is determined.
More informationSalinity distribution in the Oceans
Salinity distribution in the Oceans Average practical salinity of open ocean waters 34.72 http://eps.mcgill.ca/~courses/c542/ 1/58 Salinity distribution in the Oceans Factors that control seawater salinity:
More informationSite Location (Latitude/ Longitude)
Core Identification: Expedition Site & Hole Core & Type* Pacific Cores TABLE 2.. Seafloor cores Physiographic Site Location Site Location (Latitude/ Longitude) Water Depth (m) 2-687A-2H Peru continental
More informationAnalysis of Clays and Soils by XRD
Analysis of Clays and Soils by XRD I. Introduction Proper sample preparation is one of the most important requirements in the analysis of powder samples by X-ray diffraction (XRD). This statement is especially
More informationFloc Strength Scale-Up: A Practical Approach
Floc Strength Scale-Up: A Practical Approach Dr Mick Dawson Mr Brian Perkins Process Director mdawson@bhrgroup.co.uk 25 th October 2011 BHR Group 2011 BHR Group is a trading name of VirtualPiE Limited
More informationThe Physical Properties of Sea Water OCEA 101
The Physical Properties of Sea Water OCEA 101 Why should you care? - water provides the primary environment for marine organisms - properties of water significantly influence the evolution of marine organisms
More informationSTABILITY OF PIGMENT INKJET INKS
Application paper (2009) 1-5 Ink STABILITY OF PIGMENT INKJET INKS Abstract Stability is a key issue for the formulator developing new inkjet ink formulations using pigments. can take place in such systems
More informationSeeing the Nano-scale: Nanoparticle Tracking Analysis HVM MNT Expo 2006 Oxford. Jeremy Warren CEO, NanoSight Ltd
Seeing the Nano-scale: Nanoparticle Tracking Analysis HVM MNT Expo Oxford Jeremy Warren CEO, NanoSight Ltd 1 NanoSight Particle Characterisation at Nano-scale: Electron Microscopy PCS (Photon Correlation
More informationBACKSCATTERING BY NON-SPHERICAL NATURAL PARTICLES: INSTRUMENT DEVELOPMENT, IOP S, AND IMPLICATIONS FOR RADIATIVE TRANSFER
BACKSCATTERING BY NON-SPHERICAL NATURAL PARTICLES: INSTRUMENT DEVELOPMENT, IOP S, AND IMPLICATIONS FOR RADIATIVE TRANSFER Emmanuel Boss School of Marine Sciences 5741 Libby Hall University Of Maine Orono,
More informationInform is a series of white papers designed to provide advice on material characterization issues. Mie theory The rst 100 years
Inform is a series of white papers designed to provide advice on material characterization issues Mie theory The rst 100 years Mie theory the rst 100 years One hundred years ago Gustav Mie developed an
More informationIntroduction to Dynamic Light Scattering for Particle Size Determination
www.horiba.com/us/particle Jeffrey Bodycomb, Ph.D. Introduction to Dynamic Light Scattering for Particle Size Determination 2016 HORIBA, Ltd. All rights reserved. 1 Sizing Techniques 0.001 0.01 0.1 1 10
More informationChapter 4 Implications of paleoceanography and paleoclimate
Age ka / Chapter 4 Implications of paleoceanography and paleoclimate 4.1 Paleoclimate expression 4.2 Implications of paleocirculation and tectonics 4.3 Paleoenvironmental reconstruction MD05-2901 (Liu
More informationApplication of Micro-Flow Imaging (MFI TM ) to The Analysis of Particles in Parenteral Fluids. October 2006 Ottawa, Canada
Application of Micro-Flow Imaging (MFI TM ) to The Analysis of Particles in Parenteral Fluids October 26 Ottawa, Canada Summary The introduction of a growing number of targeted protein-based drug formulations
More informationSUPPLEMENTARY INFORMATION
SUPPLEMENTARY INFORMATION DOI: 1.138/NGEO168 "Strength and geometry of the glacial Atlantic Meridional Overturning Circulation" S2 Map of core locations Core locations of the Holocene and LGM 231 / 23
More informationCurrents & Gyres Notes
Currents & Gyres Notes Current A river of water flowing in the ocean. 2 Types of Currents Surface Currents wind-driven currents that occur in the top 100m or less Deep Currents density-driven currents
More informationFinal exam questions ED
Final exam questions ED 2015-2016 1. Radiation a) Properties and types of radiation b) Physical parameters of radiation 2. Law of attenuation of radiation a) Experimental interpretation of the law b) Forms
More informationFINE-GRAINED INORGANIC SEDIMENT CHARACTERISTICS AND SIZE. Paul Robert Auerbach
FINE-GRAINED INORGANIC SEDIMENT CHARACTERISTICS AND SIZE Paul Robert Auerbach SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF COMBINED HONOURS BACHELOR OF SCIENCE IN EARTH SCIENCES
More information429 LIGHT DIFFRACTION MEASUREMENT OF PARTICLE SIZE
Search USP29 429 LIGHT DIFFRACTION MEASUREMENT OF PARTICLE SIZE Light diffraction is one of the most widely used techniques for measuring the size of a wide range of particles from very fine to very coarse.
More informationActivity of the Month
Activity of the Month September, 2008 It s Sedimentary, My Dear Watson Summary National Math Standards In this introductory activity, students will analyze core sample data to identify sediment composition
More informationIntroduction to Nanoparticle Tracking Analysis (NTA) Measurement Principle of ZetaView
Technical Note Nanoparticle Tracking Key words: Introduction to Nanoparticle Tracking Analysis (NTA) Measurement Principle of ZetaView Particle characterization, Nanoparticle Tracking Analysis (NTA), Brownian
More informationGoing down in the Weddell Sea why deep water formation is of vital importance
Dr. Barbara Donner Research Center Ocean Margins (RCOM), Bremen Going down in the Weddell Sea why deep water formation is of vital importance Outline 1. Modern ocean circulation 2. Motors of ocean circulation
More informationUniverse. Chapter 6. Optics and Telescopes 8/12/2015. By reading this chapter, you will learn. Tenth Edition
Roger Freedman Robert Geller William Kaufmann III Universe Tenth Edition Chapter 6 Optics and Telescopes By reading this chapter, you will learn 6 1 How a refracting telescope uses a lens to form an image
More informationBackscattering and Polarization Properties of Marine Particles -- Instrument Development and Field Work
Backscattering and Polarization Properties of Marine Particles -- Instrument Development and Field Work Yogesh Agrawal Sequoia Scientific, Inc. 27 Richards Road Bellevue, WA 985 phone: (425) 867-2464 fax:
More informationMarine Sediments EPSS15 Spring 2017 Lab 4
Marine Sediments EPSS15 Spring 2017 Lab 4 Why Sediments? Record of Earth s history - Tectonic plate movement - Past changes in climate - Ancient ocean circulation currents - Cataclysmic events 1 Classification
More informationDetermination of an Appropriate Method for Dispersion of Soil Samples in Laser Diffraction Particle Size Analyses
International Journal of Computational and Experimental Science and Engineering (IJCESEN) Vol. 1-No.1 (2015) pp. 19-25 Copyright 2015- IJCESEN www.ijcesen.com Special Issue for International Conference
More informationMeasurements, applications, and impact of the refractive index of extracellular vesicles
Measurements, applications, and impact of the refractive index of extracellular vesicles Edwin van der Pol June 26th, 2014 Laboratory Experimental Clinical Chemistry; Biomedical Engineering and Physics,
More informationNew Trends in Shallow Geophysical/Seismic Surveying and Borehole Logging
New Trends in Shallow Geophysical/Seismic Surveying and Borehole Logging Dr. Michael Haschke Principal Geologist UIT GmbH Zum Windkanal 21 01109 Dresden-Germany email: m.haschke@uit-gmbh.de www.uit-gmbh.de
More informationMethod Development. Creating the Perfect Standard Operating Procedure (SOP) 2007 HORIBA, Ltd. All rights reserved.
Method Development Creating the Perfect Standard Operating Procedure (SOP) Method Development Goal: Reproducible method that tracks product performance Choose measurement approach (dry vs. suspension)
More informationUniverse. Chapter 6. Optics and Telescopes 11/16/2014. By reading this chapter, you will learn. Tenth Edition
Roger Freedman Robert Geller William Kaufmann III Universe Tenth Edition Chapter 6 Optics and Telescopes By reading this chapter, you will learn 6 1 How a refracting telescope uses a lens to form an image
More informationMAR 110 LECTURE #10 The Oceanic Conveyor Belt Oceanic Thermohaline Circulation
1 MAR 110 LECTURE #10 The Oceanic Conveyor Belt Oceanic Thermohaline Circulation Ocean Climate Temperature Zones The pattern of approximately parallel oceanic surface isotherms (lines of constant temperature)
More informationParticle sizing by multi-wavelength photo-sedimentation
Particle sizing by multi-wavelength photo-sedimentation Dietmar Lerche, Prof. Dr. Dr. LUM Berlin, Germany 1. Introduction 2. Application broadening by multi-wavelength STEP-Technology 3. PSD with no information
More informationA measurement of the diffuse reflectivity of 1056 Tyvek in air and water
Nuclear Instruments and Methods in Physics Research A 553 (2005) 312 316 www.elsevier.com/locate/nima A measurement of the diffuse reflectivity of 1056 Tyvek in air and water J.C. Arteaga-Vela zquez,c.va
More informationPhysics 30: Chapter 5 Exam Wave Nature of Light
Physics 30: Chapter 5 Exam Wave Nature of Light Name: Date: Mark: /33 Numeric Response. Place your answers to the numeric response questions, with units, in the blanks at the side of the page. (1 mark
More informationTelescopes: Portals of Discovery
Telescopes: Portals of Discovery How do light and matter interact? Emission Absorption Transmission Transparent objects transmit light Opaque objects block (absorb) light Reflection or Scattering Reflection
More informationLecture Outlines. Chapter 5. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc.
Lecture Outlines Chapter 5 Astronomy Today 8th Edition Chaisson/McMillan Chapter 5 Telescopes Units of Chapter 5 5.1 Optical Telescopes 5.2 Telescope Size 5.3 Images and Detectors 5.4 High-Resolution Astronomy
More informationPTM: A Lagrangian Particle Tracking Model. Joseph Gailani
PTM: A Lagrangian Particle Tracking Model Joseph Gailani Joe.Z.Gailani@usace.army.mil OUTLINE Motivation for sediment/constituent modeling system Objectives of modeling system Description of PTM PTM Example
More informationDEEP CIRCULATION CHANGES IN THE SOUTH ATLANTIC OCEAN: RESPONSE TO INITIATION OF NORTHERN HEMISPHERIC GLACIATION. A Thesis.
DEEP CIRCULATION CHANGES IN THE SOUTH ATLANTIC OCEAN: RESPONSE TO INITIATION OF NORTHERN HEMISPHERIC GLACIATION A Thesis Presented to The Faculty of the Department of Geology San Jose State University
More informationThree-dimensional Visualization and Quantification of Gold Nanomaterial Deposition and Aggregation in Porous Media via Raman Spectroscopy
Raman Spectroscopy Nanomaterials Exposure? Three-dimensional Visualization and Quantification of Gold Nanomaterial Deposition and Aggregation in Porous Media via Raman Spectroscopy Matthew Y. Chan, Weinan
More informationItem #9: Amphipod Tox Proposal Modification Page 1 of 9
Item #9: Amphipod Tox Proposal Modification Page 1 of 9 The effects of particle size and shape and animal health on toxicity test results using the amphipod Eohaustorius estuarius. Estimated Cost: $30,000
More informationInstrumental Polarization of Telescopes on Alt-Azimuth and Equatorial Mounts
Project Documentation Report #0009 Revision #A Instrumental Polarization of Telescopes on Alt-Azimuth and Equatorial Mounts Christoph U. Keller 4 December 2002 Advanced Technology Solar Telescope 950 N.
More informationEPSS 15 Fall 2017 Introduction to Oceanography. Marine Sediments
EPSS 15 Fall 2017 Introduction to Oceanography Marine Sediments INTRODUCTION There are two basic methods used for classification of marine sediments: genetic and descriptive. Genetic classifications distinguish
More informationCHEM*3440. Photon Energy Units. Spectrum of Electromagnetic Radiation. Chemical Instrumentation. Spectroscopic Experimental Concept.
Spectrum of Electromagnetic Radiation Electromagnetic radiation is light. Different energy light interacts with different motions in molecules. CHEM*344 Chemical Instrumentation Topic 7 Spectrometry Radiofrequency
More informationAbyssal eddy in the southwest Atlantic
Deep-Sea Research, Vol. 33, No. 6, pp. 839-847, 1986. 0198-(1149/86 $3.01) + 0.00 Printed in Great Britain. Pergamon Journals Ltd. NOTE Abyssal eddy in the southwest Atlantic ARNOLD L. GOaDON* and CHERYL
More informationLight scattering Small and large particles
Scattering by macromolecules E B Incident light Scattered Light particle Oscillating E field from light makes electronic cloud oscillate surrounding the particle Intensity: I E Accelerating charges means
More information1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite.
1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite. An arrangement of atoms such as the one shown in the diagram determines
More informationImpact of the 2002 stratospheric warming in the southern hemisphere on the tropical cirrus clouds and convective activity
The Third International SOWER meeting,, Lake Shikotsu,, July 18-20, 2006 1 Impact of the 2002 stratospheric warming in the southern hemisphere on the tropical cirrus clouds and convective activity Eguchi,
More information1 Carbon - Motivation
1 Carbon - Motivation Figure 1: Atmospheric pco 2 over the past 400 thousand years as recorded in the ice core from Vostok, Antarctica (Petit et al., 1999). Figure 2: Air-sea flux of CO 2 (mol m 2 yr 1
More informationWhy is the sky blue?
Why is the sky blue? Volcanic: June 12, 1991: Mt Pinatubo ejected 20 million tons of sulfur dioxide. Aerosols spread globally Haze lowered a drop of global temperature by 1F Size parameter: Rayleigh
More informationCliffsNotes.com. Stream Erosion. 18 Oct 2012 < ,articleId 9511.html>.
I. Introduction What is your science question? Is there a relationship between local base plateau elevation and depth, width, and length of channels within them? Why is this question important and interesting?
More informationLECTURE 11 ELECTROMAGNETIC WAVES & POLARIZATION. Instructor: Kazumi Tolich
LECTURE 11 ELECTROMAGNETIC WAVES & POLARIZATION Instructor: Kazumi Tolich Lecture 11 2 25.5 Electromagnetic waves Induced fields Properties of electromagnetic waves Polarization Energy of electromagnetic
More informationDecomposing white light into its components:
Decomposing white light into its components: a. Look through a spectroscope at a white light from within the lab (if possible a fluorescent bulb output as well as a regular incandescent bulb) and the natural
More informationLecture 0 A very brief introduction
Lecture 0 A very brief introduction Eli Tziperman Climate variability results from a very diverse set of physical phenomena and occurs on a very wide range of time scales. It is difficult to envision a
More informationParticle size analysis -Chapter 3
Particle size analysis -Chapter 3 Importance of PSA Size and hence surface area of particles affect: The rate of drug dissolution and release from dosage forms Flow properties of granules and powders.
More information13. CHERTS FROM RIO GRANDE RISE SEDIMENTS, DEEP SEA DRILLING PROJECT LEG 72, HOLE 516F 1
13. CHERTS FROM RIO GRANDE RISE SEDIMENTS, DEEP SEA DRILLING PROJECT LEG 72, HOLE 516F 1 M. A. Levitan, V. P. Strizhov, and A. Ya. Schevtchenko, Institute of Oceanology, The Academy of Sciences of the
More informationMidterm 2: Nov. 20 (Monday)
Introduction to Oceanography Lecture 18, Current 2 Surface Ocean Currents. Video by Chris Henze, NASA Ames, Public Domain Midterm 2: Nov. 20 (Monday) Review Session & Video Screenings TBA Image from Sverdrup,
More information16. DATA REPORT: CARBONATE
Prell, W.L., Wang, P., Blum, P., Rea, D.K., and Clemens, S.C. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 184 16. DATA REPORT: CARBONATE AND ORGANIC CARBON CONTENTS OF SEDIMENTS
More informationFundamentals of Particle Counting
Fundamentals of Particle Counting 1 Particle Counting: Remains the most significant technique for determining the cleanliness level of a fluid Useful as a tool for qualification and monitoring cleanroom
More informationThe role of ice cores in understanding the dust cycle
The role of ice cores in understanding the dust cycle Ash layer Sepp Kipfstuhl, AWI Anna Wegner 24.5.2010 Dustspec Workshop Lamont Overview Short introduction What have we learned in the past decade? (1)
More informationPetroleum Thermodynamic Research Group
Petroleum Thermodynamic Research Group Labs 6-128 & 6-133 Chemical and Materials Engineering (CME) Bldg. The Petroleum Thermodynamic Research Group investigates the properties of hydrocarbon resources
More informationParticles, drops, and bubbles. Lecture 3
Particles, drops, and bubbles Lecture 3 Brownian Motion is diffusion The Einstein relation between particle size and its diffusion coefficient is: D = kt 6πηa However gravitational sedimentation tends
More informationLAB 3: Confocal Microscope Imaging of single-emitter fluorescence. LAB 4: Hanbury Brown and Twiss setup. Photon antibunching. Roshita Ramkhalawon
LAB 3: Confocal Microscope Imaging of single-emitter fluorescence LAB 4: Hanbury Brown and Twiss setup. Photon antibunching Roshita Ramkhalawon PHY 434 Department of Physics & Astronomy University of Rochester
More informationA New Atmospheric Motion Vector Intercomparison Study
A New Atmospheric Motion Vector Intercomparison Study David Santek 1, Javier García-Pereda 2, Chris Velden 1, Iliana Genkova 3, Dave Stettner 1, Steve Wanzong 1, Sharon Nebuda 1, Régis Borde 4, Manuel
More informationλmax = k d Supplementary Figures
Supplementary Figures a b HQ CCD Transmission Grating Beam splitting lens Color CCD Objective Sample Dark-field Condenser Raw data Gaussian fit c λmax = k d k = 1.733 nm/pixel 53 nm 307 pixels d Supplementary
More informationBOTTOM CURRENTS DEPOSITS ALONG THE URUGUAYAN MARGIN: CONCEPTUAL AND ECONOMIC IMPLICATIONS
Canning House London, 20 th October 2017 BOTTOM CURRENTS DEPOSITS ALONG THE URUGUAYAN MARGIN: CONCEPTUAL AND ECONOMIC IMPLICATIONS F. J. Hernández- Molina Dept. Earth Sciences Royal Holloway Univ. London
More informationSUBJECT INDEX. ~ ~5 physico-chemical properties 254,255 Redox potential 254,255
Aggregates: beds formed by deposition 81,82 breakup by fluid shear, introduction 85,86 deposition from flowing water 80 implications in cohesive sediment transport 102-105 needs for further research 83
More informationInterpreting Your PSA Results
Interpreting Your PSA Results Decoding the Acronyms and Finding Insights Ian Treviranus ian.treviranus@horiba.com www.horiba.com/us/particle Outline The Basics Define Parameters Choose Parameters Interpret
More informationSupporting Information
Supporting Information Title Boron Doping and Defect-Engineering of Graphene Aerogels for Ultrasensitive NO 2 Detection Sally Turner 1,5,6, Wenjun Yan 2,3, Hu Long 5,6, Art J. Nelson 4, Alex Baker 4, Jonathan
More informationLaboratory#6 Sediment Particle Size Distribution and Turbidity Flows
Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows Although this laboratory will pertain to oceanic sediments similar processes can also be observed on land and other aquatic systems
More informationBIO & PHARMA ANALYTICAL TECHNIQUES. Chapter 5 Particle Size Analysis
BIO & PHARMA ANALYTICAL TECHNIQUES Chapter 5 by Dr Siti Umairah Mokhtar Faculty of Engineering Technology umairah@ump.edu.my Chapter Description Aims Discuss theory, principles and application of analytical
More informationWhat are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to
What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to 10µm Concentrations decrease exponentially with height N(z) = N(0)exp(-z/H) Long-lived
More information17. DATA REPORT: CARBONATE, ORGANIC CARBON, AND OPAL CONCENTRATIONS SOUTHWEST AFRICA MARGIN 1
Wefer, G., Berger, W.H., and Richter, C. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 175 17. DATA REPORT: CARBONATE, ORGANIC CARBON, AND OPAL CONCENTRATIONS AND ORGANIC
More informationHydrothermal Chemistry/ Reverse Weathering. Marine Chemistry Seminar
Hydrothermal Chemistry/ Reverse Weathering Marine Chemistry Seminar 1974 Drever, The Sea Chapter 10:The Magnesium Problem 1979 Edmonds et al., Ridge Crest Hydrothermal Activity and the Balances of Major
More informationInvited paper on the South Atlantic J. Lutjeharms
AGU Chapman Conference on the Agulhas System Stellenbosch South Africa October 8 12, 2012 With regard to the thermohaline circulation, we identify some key locations where very important processes occur,
More informationMarine Sediments. Introductory Oceanography. Ray Rector: Instructor
Marine Sediments Introductory Oceanography Ray Rector: Instructor Ocean Basins are Vast Sinks for Huge Amounts of Sediment from Numerous Different Sources Four Major Types of Seafloor Sediments 1. Lithogenous
More informationA laboratory investigation of the mechanical behaviour of a volcanic ash
2th IMEKO TC4 International Symposium and 8th International Workshop on ADC Modelling and Testing Research on Electric and Electronic Measurement for the Economic Upturn Benevento, Italy, September 5-7,
More informationDoes the Mg/Ca in Foraminifera Tests Provide a Reliable Temperature Proxy?
Grand Valley State University ScholarWorks@GVSU Student Summer Scholars Undergraduate Research and Creative Practice 2009 Does the Mg/Ca in Foraminifera Tests Provide a Reliable Temperature Proxy? Sarah
More informationHow DLS Works: Interference of Light
Static light scattering vs. Dynamic light scattering Static light scattering measures time-average intensities (mean square fluctuations) molecular weight radius of gyration second virial coefficient Dynamic
More informationOcean Sediments. Key Concepts
Ocean Sediments Key Concepts 1. What are the processes that control what types of sediments are deposited in which places? 2. Conversely, how can we use the sedimentary record to figure out tectonic and
More informationCHAPTER 3 Ocean Basins
Review: What Drives Plate Motions: (1) Density vs. Gravity: causes oceanic crust to sink in subduction zones, causes crust to extend at spreading ridges (called ridge push, but the ridge is not pushing,
More informationSalinity variability associated with changes in the hydrological cycle variables
Salinity variability associated with changes in the hydrological cycle variables Olga Sato Paulo Polito olga.sato@usp.br Oceanographic Institute of the University of SÃčo Paulo Olga Sato (IOUSP) Salinity
More informationArnold L. Gordon Retroflections and Bifurcations Johann Lutjeharms Memorial Lecture
The Agulhas System and its Role in Changing Ocean Circulation, Climate & Marine Ecosystems Spier Hotel, Stellenbosch, Western Cape, South Africa 8 12 October 2012 Brazil/Malvinas Agulhas Retroflection
More informationFACTORS AFFECTING IN-LINE PHASE CONTRAST IMAGING WITH A LABORATORY MICROFOCUS X-RAY SOURCE
Copyright JCPDS-International Centre for Diffraction Data 26 ISSN 197-2 FACTORS AFFECTING IN-LINE PHASE CONTRAST IMAGING WITH A LABORATORY MICROFOCUS X-RAY SOURCE 31 K. L. Kelly and B. K. Tanner Department
More information