MnO 2 Resin and Automated Measurements of Ra Isotopes Bill Burnett Dept. Oceanography Florida State University.

Slides:



Advertisements
Similar presentations
Ra in Water using MnO2 Resin: New Developments
Advertisements

Analysis of Actinide Elements from Large Environmental Samples
Removal of Cu(II) ions from aqueous solution effluent using Melamine-Formaldehyde-DTPA resin in a fixed-bed up-flow column By Ahmad Baraka Supervisors.
Nutrient Removal Project: Chemical Phosphorus Removal Jill Crispell, Stephanie Wedekind, Sarah Rosenbaum.
Measurements of Ra Isotopes via MnO2 Resin
Analysis of Actinide Elements from Large Samples Henrieta Dulaiova Guebuem Kim Bill Burnett Florida State University and E. Philip Horwitz PG Research.
Fundamental Techniques and Measurements  Mass Measurements  Volume Measurements  Preparation of a solution of known concentration  UV-Visible Spectrophotometer.
Nuclear Physics & Society (2009) 1 Radioactivity Three main types, all release energy through the relation Q=  E=  mc 2 –A–Alpha (  ) decay Emission.
Why do some reactions happen and others don’t? Are the products more stable than the reactants? Thermodynamics Does the reaction go at a reasonable rate?
B IOCHEMICAL INSTRUMENTAL ANALYSIS -11 Dr. Maha Al-Sedik.
Fundamentals of Radium and Uranium Removal from Drinking Water Supplies Dennis Clifford University of Houston.
MnO 2 Resin: Concentration of Radium Isotopes Deok-Soo Moon Bill Burnett Department of Oceanography Florida State University Tallahassee, Florida.
AM 1 and AM 2 Review.
Why do YOU need to know about Nuclear Physics?
The Determination of 226 Ra in Water Samples Anil H. Thakkar Eichrom Technologies, Inc. eichrom TECHNOLOGIES INC.
112.3 PHOSPHATE ADSORPTION RESULTS Measuring Phosphorus Retention Capacity in the Marsh Substrate of an Ecologically Engineered Wastewater Treatment Facility.
Detailed Design Review: Pre-Filter P13418
Lee, Myeong Jae DMRC, Seoul national university
New methodologies and techniques for 234 Th analysis Future Applications of 234 Th in Aquatic Ecosystems Woods Hole, August 2004.
The Determination of 224 Ra, 226 Ra, & 228 Ra in Water Samples Michael Fern Eichrom Technologies, Inc.
Applications of Extraction Chromatography in Marine Geochemistry
The Nucleus and Radioactivity
Radioactive Isotope Isotope which is unstable. It emits radiation & changes into another kind of atom.
Chapter 18.  Mass # Symbol  Element Name or symbol – Mass #  Parts of a Reaction Reactants  Products.
Analysis of Actinide Elements from Large Samples Henrieta Dulaiova Guebuem Kim Bill Burnett Florida State University and E. Philip Horwitz PG Research.
Actinide Analysis from Large- Volume Seawater Samples Bill Burnett & Guebuem Kim Department of Oceanography Florida State University and Phil Horwitz PG.
Polymer Nanofibers from Recycling of Waste Expanded Polystyrene Research at The University Of Akron C. Shin and G. G. Chase Polymer Nanofibers from Recycling.
MnO 2 Resin: Concentration of Radium Isotopes Deok-Soo Moon Bill Burnett Department of Oceanography Florida State University Tallahassee, Florida.
Chemistry Final Review. Subatomic Particles ParticleLocationChargeMass Proton Neutron Electron.
Radioisotopes, and their use in “dating” rocks. Radioactive Decay Certain isotopes of some elements are not stable. They naturally change (decay) over.
Radioactive Decay. I can solve half-life problems. Radioisotopes decay in a predictable way – The time is takes for half of a sample to decay is called.
Radioactivity. Contents Atomic Structure Atomic Structure Isotopes Isotopes Background Radiation Background Radiation Alpha, Beta, Gamma Alpha, Beta,
Imran Syakir Mohamad Chemistry DMCU Chemical Reaction Chapter 3 C2H6OC2H6O.
General Engineering Laboratories Use of Eichrom Resins for Bioassay Pa-231 Bob Timm - GEL Tim Chandler - GEL Bill Burnett - FSU Mike Schultz - PerkinElmer.
Developments in Environmental Radiochemistry* Environmental Radioactivity Measurement Facility Department of Oceanography Florida State University Tallahassee,
The Determination of 226Ra in Water Samples
Chapter 18.  Mass # Symbol  Element Name or symbol – Mass #  Parts of a Reaction Reactants  Products.
Radioactivity.  Total mass of nucleus is always less than the sum of its protons and neutrons  Compare the mass of He-4 to that of its nucleus - mass.
Updates from Eichrom’s Tech Support Lab Anil Thakkar May 4 th 2004 Charleston, SC.
Spontaneous emission of radiation when the nucleus of an atom breaks down to form a different element.
Half-Life & Carbon Dating pg
Americium and Samarium Determination in Aqueous Solutions after Separation by Cation-Exchange Tasoula Kiliari and Ioannis Pashalidis Radioanalytical Chemistry.
Nuclear Chemistry Chapter 18.
Nguyen Thi Kim Phuong Institute of Chemical Technology
Nuclear Equations Nucleons: particles in the nucleus: –p + : proton –n 0 : neutron. Mass number: the number of p + + n 0. Atomic number: the number of.
Optimizing Radiochemical Methods at SRS (Ni-63, I-129, Actinides) Sherrod L. Maxwell, III Westinghouse Savannah River Company.
UNIT 7 NUCLEAR REACTIONS 7.3 Calculating Half Life? May 17, 2011 DO NOW: = /4.5 = If we start with 4.5 grams of Radon-222 and over a period.
Evaluation of a New Arsenic Adsorbing Resin (WASP) Dr. Robert Stanforth, Ng Aik Teng and Woo Su-Fang National University of Singapore July 2002.
CALCULATING HALF-LIFE Aim: How can we measure how much of a radioactive element decayed? DO NOW: If we start with 4.5 grams of Radon- 222 and over a period.
Get a Charge Out of Matter Jeopardy Sub-Atomic Awesomeness What the heck? Q & A Reaction Jackson
Radioactive Decay Problems #1. 1. What is the mass number of Radium-226?
NEM433 Radiation Detection and Measurement Laboratory Fall 2013 Osman Şahin ÇELİKTEN.
An Improved Method for Determination of Ra-228 * Jamie Christoff & Bill Burnett Department of Oceanography Florida State University “The Double-Pass Approach”
Emanation of Radon from Radium Removal Point of Use Units
Anil H.Thakkar Eichrom Industries, Inc.. Darien, IL
Alpha, Gamma and Neutron Radiation
The Atomic Nucleus & Radioactive Decay
The Determination of 226Ra in Water Samples
Characterization of n_TOF fission samples
Polymer Nanofibers from Recycling of Waste Expanded Polystyrene
Ra in Water using MnO2 Resin: Update
Rapid Emergency Methods for Actinides and Sr-89/90
Particulate and Dissolved 210Po and 210Pb in Water Columns from the
I. Nuclear Equations Mass numbers and atomic numbers are conserved in nuclear equations.
Section 10.1 Separable Equations II
Half-Life.
Solubility & Ksp & Nuclear.
National Air and Radiation Environmental Lab
Problem Session.
Presentation transcript:

MnO 2 Resin and Automated Measurements of Ra Isotopes Bill Burnett Dept. Oceanography Florida State University

MnO 2 Resin Developed by PGRF mesh High adsorption of Ra, trivalent and tetravalent actinides (Ac, Am, Pu, Th) Preconcentration approach in batch, column, or pump (filtration) modes

IsotopeDirectParentHalf-life Decay Mode EnergyMeV 223 Ra 227 Th 11.4 d  Ra 228 Th 3.66 d  Ra 230 Th 1600 y  Ra 232 Th 5.75 y 0.046 Natural Radium Isotopes

Tracers for Characterization Ba-133 (commercial, nominal activity) Ra-228, Ra-224 (separated from 40-year old Th(SO 4 ) 2, calibrated by gamma spect Ra-226 NIST solution standard

Distribution Coefficient C 1 = amount adsorbed per gram dry resin; and C 2 = amount that remains in solution after equilbrium has been reached. Units = mL/g

K D Determinations w Tracers A o = initial activity solution, cpm A f = final activity solution, cpm V = volume solution, mL W = weight of resin, g

Percent Recovery K D = 2.8 x 10 4

Kinetics, pH = 7 pH = 7 Resin = 25 mg Solution = 10 mL Floridan Aquifer groundwater ~ mg/L ( o / oo )

pH Variation pH = variable Resin = 25 mg Solution = 10 mL Reaction time = 90 min Surface charge Ra 2+ speciation The optimum pH for adsorption of Ra 2+ is from 5 to 8 – nearly all natural waters fall into this range.

Pump Tests Peristaltic pump; cartridge loaded with 1 g MnO 2 Resin; single pass

Pump Video Fresh waters can be processed at high flow rates (  300 mL/min) without any loss. Highly salted waters require longer equilibration times

Ra Isotopes via RAD-7 MnO 2 -Resin ( 226,228,224,223 Ra) Alpha Detector Rn 220 Rn 219 Rn 222 Rn, 220 Rn, 219 Rn 215 Po 216 Po 214 Po 218 Po Drierite Air Pump RAD7

Optimum Moisture Content Water/Fiber Ratio = (x i -x o )/x o ; where x i = mass at each stage; and x o = mass when completely dry

Recoil Effect on Rn Emanation Recoil range in air = 0.07 cm Recoil Range in water = 9.1 x cm

“DRYSTIK” Approach Drierite

Moisture Control During Counting

Effect on Countrate

Results: Ra-224 Counting Water sample passed through MnO 2 Resin and 220 Rn counted periodically over many days produced the correct half-life for 224 Ra.

Results: Ra-226 ( 222 Rn Ingrowth) T 1/2 = 3.84 days Several standards prepared with NIST 226 Ra solution. Theoretical line drawn with decay constant for 222 Rn.

Summary MnO 2 Resin is an excellent adsorber of Ra from natural waters May be used for preconcentration to combine with traditional techniques (e.g.,  -spect,  -spect) Interfacing with a RAD-7 Radon analyzer allows determination of 224 Ra and 226 Ra without chemical separations