Micromeritics SediGraph. Particle Size Data based on Consolidated Certainties

Size: px
Start display at page:

Download "Micromeritics SediGraph. Particle Size Data based on Consolidated Certainties"

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)

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 information

Ratio of coccolith CaCO 3 to foraminifera CaCO 3 in late Holocene deep sea sediments

Ratio 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 information

Geoffrey (Jake) Gebbie Research Associate, Harvard University Visiting Scientist, MIT

Geoffrey (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 information

Holographic Characterization of Agglomerates in CMP Slurries

Holographic 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 information

I. 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 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 information

An 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 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 information

Refractive 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 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 information

QbD QUANTITATIVE MEASUREMENTS OF CQAS IN SOLID DOSAGE FORM UNIT OPERATIONS

QbD 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 information

This is start of the single grain view

This 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 information

GSA DATA REPOSITORY

GSA 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 information

Minimal 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 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 information

Processes affecting continental shelves

Processes 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) ;

*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 information

Announcements. 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. 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 information

A bit of background on carbonates. CaCO 3 (solid)

A 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 information

1 Millimeter. 1 Micron. 1 Nanometer. 1 Angstrom ELECTRON SEPARATION PROCESS COMMON MATERIALS PARTICLE SIZE LOG SCALE MAGNETIC RANGE SPECTRUM

1 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 information

A 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 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 information

Jim Hagerman 4/12/99

Jim 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 information

Salinity distribution in the Oceans

Salinity 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 information

Site Location (Latitude/ Longitude)

Site 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 information

Analysis of Clays and Soils by XRD

Analysis 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 information

Floc Strength Scale-Up: A Practical Approach

Floc 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 information

The Physical Properties of Sea Water OCEA 101

The 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 information

STABILITY OF PIGMENT INKJET INKS

STABILITY 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 information

Seeing 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 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 information

BACKSCATTERING 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 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 information

Inform 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 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 information

Introduction to Dynamic Light Scattering for Particle Size Determination

Introduction 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 information

Chapter 4 Implications of paleoceanography and paleoclimate

Chapter 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 information

Application 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 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 information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY 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 information

Currents & Gyres Notes

Currents & 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 information

Final exam questions ED

Final 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 information

FINE-GRAINED INORGANIC SEDIMENT CHARACTERISTICS AND SIZE. Paul Robert Auerbach

FINE-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 information

429 LIGHT DIFFRACTION MEASUREMENT OF PARTICLE SIZE

429 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 information

Activity of the Month

Activity 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 information

Introduction to Nanoparticle Tracking Analysis (NTA) Measurement Principle of ZetaView

Introduction 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 information

Going down in the Weddell Sea why deep water formation is of vital importance

Going 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 information

Universe. Chapter 6. Optics and Telescopes 8/12/2015. By reading this chapter, you will learn. Tenth Edition

Universe. 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 information

Backscattering and Polarization Properties of Marine Particles -- Instrument Development and Field Work

Backscattering 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 information

Marine Sediments EPSS15 Spring 2017 Lab 4

Marine 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 information

Determination of an Appropriate Method for Dispersion of Soil Samples in Laser Diffraction Particle Size Analyses

Determination 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 information

Measurements, applications, and impact of the refractive index of extracellular vesicles

Measurements, 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 information

New Trends in Shallow Geophysical/Seismic Surveying and Borehole Logging

New 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 information

Method Development. Creating the Perfect Standard Operating Procedure (SOP) 2007 HORIBA, Ltd. All rights reserved.

Method 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 information

Universe. Chapter 6. Optics and Telescopes 11/16/2014. By reading this chapter, you will learn. Tenth Edition

Universe. 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 information

MAR 110 LECTURE #10 The Oceanic Conveyor Belt Oceanic Thermohaline Circulation

MAR 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 information

Particle sizing by multi-wavelength photo-sedimentation

Particle 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 information

A measurement of the diffuse reflectivity of 1056 Tyvek in air and water

A 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 information

Physics 30: Chapter 5 Exam Wave Nature of Light

Physics 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 information

Telescopes: Portals of Discovery

Telescopes: 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 information

Lecture Outlines. Chapter 5. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc.

Lecture 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 information

PTM: A Lagrangian Particle Tracking Model. Joseph Gailani

PTM: 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 information

DEEP 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. 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 information

Three-dimensional Visualization and Quantification of Gold Nanomaterial Deposition and Aggregation in Porous Media via Raman Spectroscopy

Three-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 information

Item #9: Amphipod Tox Proposal Modification Page 1 of 9

Item #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 information

Instrumental Polarization of Telescopes on Alt-Azimuth and Equatorial Mounts

Instrumental 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 information

EPSS 15 Fall 2017 Introduction to Oceanography. Marine Sediments

EPSS 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 information

CHEM*3440. Photon Energy Units. Spectrum of Electromagnetic Radiation. Chemical Instrumentation. Spectroscopic Experimental Concept.

CHEM*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 information

Abyssal eddy in the southwest Atlantic

Abyssal 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 information

Light scattering Small and large particles

Light 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 information

1. 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. 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 information

Impact of the 2002 stratospheric warming in the southern hemisphere on the tropical cirrus clouds and convective activity

Impact 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 information

1 Carbon - Motivation

1 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 information

Why is the sky blue?

Why 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 information

CliffsNotes.com. Stream Erosion. 18 Oct 2012 < ,articleId 9511.html>.

CliffsNotes.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 information

LECTURE 11 ELECTROMAGNETIC WAVES & POLARIZATION. Instructor: Kazumi Tolich

LECTURE 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 information

Decomposing white light into its components:

Decomposing 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 information

Lecture 0 A very brief introduction

Lecture 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 information

Particle size analysis -Chapter 3

Particle 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 information

13. 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 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 information

Midterm 2: Nov. 20 (Monday)

Midterm 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 information

16. DATA REPORT: CARBONATE

16. 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 information

Fundamentals of Particle Counting

Fundamentals 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 information

The role of ice cores in understanding the dust cycle

The 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 information

Petroleum Thermodynamic Research Group

Petroleum 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 information

Particles, drops, and bubbles. Lecture 3

Particles, 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 information

LAB 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 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 information

A New Atmospheric Motion Vector Intercomparison Study

A 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 information

λmax = k d Supplementary Figures

λmax = 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 information

BOTTOM CURRENTS DEPOSITS ALONG THE URUGUAYAN MARGIN: CONCEPTUAL AND ECONOMIC IMPLICATIONS

BOTTOM 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 information

SUBJECT INDEX. ~ ~5 physico-chemical properties 254,255 Redox potential 254,255

SUBJECT 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 information

Interpreting Your PSA Results

Interpreting 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 information

Supporting Information

Supporting 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 information

Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows

Laboratory#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 information

BIO & PHARMA ANALYTICAL TECHNIQUES. Chapter 5 Particle Size Analysis

BIO & 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 information

What 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 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 information

17. DATA REPORT: CARBONATE, ORGANIC CARBON, AND OPAL CONCENTRATIONS SOUTHWEST AFRICA MARGIN 1

17. 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 information

Hydrothermal Chemistry/ Reverse Weathering. Marine Chemistry Seminar

Hydrothermal 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 information

Invited paper on the South Atlantic J. Lutjeharms

Invited 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 information

Marine Sediments. Introductory Oceanography. Ray Rector: Instructor

Marine 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 information

A laboratory investigation of the mechanical behaviour of a volcanic ash

A 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 information

Does the Mg/Ca in Foraminifera Tests Provide a Reliable Temperature Proxy?

Does 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 information

How DLS Works: Interference of Light

How 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 information

Ocean Sediments. Key Concepts

Ocean 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 information

CHAPTER 3 Ocean Basins

CHAPTER 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 information

Salinity variability associated with changes in the hydrological cycle variables

Salinity 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 information

Arnold L. Gordon Retroflections and Bifurcations Johann Lutjeharms Memorial Lecture

Arnold 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 information

FACTORS AFFECTING IN-LINE PHASE CONTRAST IMAGING WITH A LABORATORY MICROFOCUS X-RAY SOURCE

FACTORS 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