J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.

Slides:



Advertisements
Similar presentations
Hydrodynamics and Sediment Transport Modelling Ramiro Neves
Advertisements

JSSBIO1Huttula Lecture Set Sediment transport models.
The percentage of particles in various size ranges is determined and data can be displayed as a particle size distribution, or cumulative size distribution.
Ecotoxicology Transport of contaminants. The transport of contaminants in the atmosphere takes place: Globally Large-scale:> 1000 km Meso-scale:
6.i. Modelling environmental processes: kinetic and equilibrium (quasi-thermodynamic) modelling 6(i)
Sorption of Anions Important because: Several nutrients and agricultural chemicals are negatively charged. –Nitrate, phosphate, sulfate, selenate,… Tropical,
Prairie View A&M University HBCU/MI Environmental Technology Consortium Hylton G. McWhinney, Ph.D. Principal Investigator John R. Williams, Ph.D. Steering.
Suspended particle property variation in Gaoping Submarine Canyon Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry, National Sun Yat-sen.
Particle Settling Velocity Put particle in a still fluid… what happens? Speed at which particle settles depends on: particle properties: D, ρ s, shape.
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS
Ch. 4 continued Soil Properties.
Introduction to GW contamination and
Particulate scavenging and lateral transport processes in the Kaoping River-Sea System based on 210 Po and 210 Pb distributions and disequilibrium Hung.
Information from stream sediments Measurement of concentration of metals present (as solids) in sediment Gives information on: 1.Background levels of contamination.
Suspended particle property variations in Gaoping Submarine Canyon Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry, National Sun.
Lecture 3 Trace Metals in Seawater What are trace elements? Why are they important? Principal of Oceanographic Consistency. Profiles shapes as clues for.
Cycling of Ocean Micronutrients: What do we Know and What do we Need to Know? Ed Boyle Earth, Atmospheric and Planetary Sciences Massachusetts Institute.
Water Quality.
Solute (and Suspension) Transport in Porous Media
Environmental Processes Partitioning of pollutants 3.i Sorption involving organic matter (between air/soil and water/soil)
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
Field Methods of Monitoring Atmospheric Systems Chemical Analysis of Particulate Matter Copyright © 2006 by DBS.
Environmental Engineering Lecture 6. Sources of Drinking Water  Rivers: upland and lowland  Lakes and reservoirs  Groundwater aquifers  Sea water.
Earth Science 4-5 ES2 Formation of Earth Materials.
210 Po, 210 Pb, and POC in the mesopelagic: multi-technique water column sampling in MEDFLUX G. Stewart P. Masque, J.K. Cochran, J.C. Miquel, B. Gasser,
Satellite Data Assimilation into a Suspended Particulate Matter Transport Model.
A Study of the Spatial Distribution of Suspended Sediments and their Settling Behaviour in the Dartmouth Lake System By: Lori Wrye Supervisor: Dr. Paul.
1 The Turtle by Ogden Nash Ogden Nash The turtle lives 'twixt plated decks Which practically conceal its sex. I think it clever of the turtle In such a.
Amos Russak1,2, Orit Sivan1, Yoseph Yechieli2 and Boaz Lazar3
 Colloids and contaminants in a porous fractured rock  Processes Considered  Important sites and interested parties Introduction Colloid/Contaminant.
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
Third annual CarboOcean meeting, 4.-7.December 2007, Bremen, Segschneider et al. Uncertainties of model simulations of anthropogenic carbon uptake J. Segschneider,
16. Sediment Transport Across the Continental Shelf and Lead-210 Sediment Accumulation Rates William Wilcock OCEAN/ESS 410.
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
Case study: 137 Cs as tracer for sedimentation processes in an Italian coastal area Roberta Delfanti, ENEA - La Spezia, Italy IAEA Regional Training Course.
Tracking the fate of carbon in the ocean using thorium-234 Ken Buesseler Dept. of Marine Chemistry and Geochemistry Woods Hole Oceanographic Institution.
CALCULATIONS IN NANOTECHNOLOGY
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
Geodynamics-based Core the University of Minnesota (UMN) - Twin Cities Martin O. Saar Donna L. Whitney 2)Overview.
Catherine Jeandel, Marseille 2004: Geochemistry in KEOPS Chlorophyll (mg m -3 ) Among the objectives of KEOPS - Identification of the mechanisms of natural.
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS 410.
Controls on Suspended Particle Properties and Water Clarity along a Partially-Mixed Estuary, York River Estuary, Virginia Kelsey A. Fall 1, Carl T. Friedrichs.
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
210 Po Enrichment Relative to 210 Pb in the Planktons Collected from the Northern South China Sea and the Luzon Strait P. Wang and Y. Chung Institute of.
Abstract Man-made dams influence more than just the flow of water in a river. The build up of sediments and organic matter, increased residence times,
Sedimentology Lecture #6 Class Exercise The Fenton River Exercise.
 The health of a water system is determined by the balance between physical, chemical, and biological variables.
An introduction to cohesive sediment transport processes
Chapter 23 Electric Fields.
THE SPATIAL VARIABILITY OF BERYLLIUM-7 DEPTH DISTRIBUTION STUDY Jalal a *, Zainudin Othman b, Dainee Nor Fardzila Ahmad Tugi a, Noor Fadzilah.
Course TEN-702 Industrial waste management unit-2
Biogenic opal diagenesis in sediments. Biogenic opal What is it? Amorphous silica: (~ 10% water)
Near-surface Geologic Environments
FISHERIES POSTER SESSION
Redahegn Sileshi1, Robert Pitt2 , and Shirley Clark3
Drinking-water Treatment
Rejection and Mass Transport in Membranes
Theme 2: Abiotic Cycling and Scavenging
Elizabeth River PCB TMDL Study: Numerical Modeling Approach
ECOLOGY OF THE SEASHORE
James River PCB TMDL Study: Numerical Modeling Approach
OCEAN/ESS Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons)
Aerosol Drug Therapy Copyright © 2013, 2009, 2003, 1999, 1995, 1990, 1982, 1977, 1973, 1969 by Mosby, an imprint of Elsevier Inc.
Water Pollution.
Major Water Pollutants
SETTLING AND SEDIMENTATION.
Radionuclide transport modelling
Can the Hurst Exponent be used to detect Levy Flights?
Presentation transcript:

J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008 Project Lecture 1: Radionuclides of the environment and general aspects Concentration and distribution factors. k d variability Granulometric speciation k d in saturated porous media : “intrinsic” values Experiments on depth penetration patterns J.M. Abril, University of Seville

Some radionuclides and other hazardous materials, such as heavy metals, are highly particle-reactive. Their uptake by suspended particulate matter (SPM) and bottom sediments plays an important role in the fate of these pollutants. Remember: Depending on the pollutant, 1 gram of SPM can uptake more activity (or units of pollutants) than 1 m 3 of water. J.M. Abril, University of Seville

The uptake is a surface-mediated phenomenon. SPM has very high specific surface area (SSA) Naturally occurring particulate matter in aquatic systems usually exhibits areas with uncompensated negative charges. J.M. Abril, University of Seville

K d provides a convenient means to describe the relationship between radionuclide concentrations in SPM or bottom sediments and water Notes: Field observation Laboratory experiments Dynamic equilibrium Notes: Field observation Laboratory experiments Dynamic equilibrium J.M. Abril, University of Seville 4

5

Concentration facfors J.M. Abril, University of Seville 6

7

Concentration facfors J.M. Abril, University of Seville 8

K d variability For many radionuclides, field k d values from different environments, can vary within a range of more than two orders of magnitude ( IAEA, 1985) J.M. Abril, University of Seville 9

K d vs. particle-size Basic model handling spherical particles Pores and free edges 10 J.M. Abril, University of Seville

Definitions: a s, a c, ξ J.M. Abril, University of Seville 11

Man-made radionuclides interacting with “natural” particles J.M. Abril, University of Seville 12

Naturally occurring radionuclides a c > 0 The full equation has to be used Two extreme behaviors depending on radionuclide solubility Depleted outer layer for relatively soluble radionuclides Enriched outer layer for highly particle-reactive radionuclides J.M. Abril, University of Seville 13

J.M. Abril, University of Seville 14

Caesium J.M. Abril, University of Seville 15

J.M. Abril, University of Seville 16

SPM in natural waters is mainly present in the form of flocs (or aggregates) mixed with single mineral particles. “Many particles” effects in k d variability J.M. Abril, University of Seville 17

J.M. Abril, University of Seville 18

Global effects of particle size spectra and mineralogical composition J.M. Abril, University of Seville 19

J.M. Abril, University of Seville 20

Bathymetric map for lake HÁRSVATTEN (Sweden). Understanding spatial speciation… J.M. Abril, University of Seville 21

Hydrodynamic transport Z Path length Settling velocity Stokes’ Law J.M. Abril, University of Seville 22

J.M. Abril, University of Seville 23

J.M. Abril, University of Seville 24

210 Pb J.M. Abril, University of Seville 25

Competition with cations related to SALINITY [ S ] J.M. Abril, University of Seville 26

More details in: Parts I and II J.M. Abril, University of Seville 27

J.M. Abril, University of Seville 28

A phosphate fertilizer factory pumped into the Odiel river (SW Spain) a suspension of PG particles (NORM material). We wanted to know how these radionuclide-enriched material was spread onto bottom sediments Direct gamma measurements of radionuclide concentrations would provide concentrations under MDL J.M. Abril, University of Seville 29

kdkd r r kdkd C(r) r r PG susp Natural p. F1F1 F2F2 J.M. Abril, University of Seville 30

kdkd r J.M. Abril, University of Seville 31

Materials and methods 3-5 kilograms of sediments were collected at each sampling point The samples were dried (24 h at 110°C), mechanically disaggregated and sieved in a sieving-pile. J.M. Abril, University of Seville 32

234 Th J.M. Abril, University of Seville 33

226 Ra J.M. Abril, University of Seville 34

Bickford Reservoir (USA) Benoit and Hemond, Geochimica et Cosmochimica Acta 55, Evidence for diffusive redistribution of 210 Pb in lake sediments % in solids J.M. Abril, University of Seville 35

Bickford Reservoir (USA) J.M. Abril, University of Seville 36

Bickford Reservoir (USA) J.M. Abril, University of Seville 37

Radionuclide uptake by sediment columns H. Barros and J.M. Abril Radionuclide uptake by sediment columns H. Barros and J.M. Abril J.M. Abril, University of Seville 38

J.M. Abril, University of Seville 39

J.M. Abril, University of Seville 40