OBJECTIVES

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Occurrence of Radium-224, Radium-226, and Radium-228 in Aquifers Used Primarily for Drinking Water in the United States: Retrospective Survey of Results from 1987 to 2004 Zoltan Szabo, Eric Jacobsen, Jeffrey M Fischer, Thomas F Kraemer, and Vincent T dePaul U.S. Geological Survey

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Occurrence of Radium-224, Radium-226, and Radium-228 in Aquifers Used Primarily for Drinking Water in the United States: Retrospective Survey of Results from 1987 to 2004. Zoltan Szabo, Eric Jacobsen, Jeffrey M Fischer, Thomas F Kraemer, and Vincent T dePaul U.S. Geological Survey. OBJECTIVES. - PowerPoint PPT Presentation

Transcript of OBJECTIVES

Page 1: OBJECTIVES

Occurrence of Radium-224, Radium-226, and Radium-228 in

Aquifers Used Primarily for Drinking Water in the United

States: Retrospective Survey of Results from 1987 to 2004

Zoltan Szabo, Eric Jacobsen, Jeffrey M Fischer, Thomas F Kraemer,

and Vincent T dePaul

U.S. Geological Survey

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OBJECTIVES

• Where does Ra occur? • Are there geochemical or

geological features on National and local scales that help evaluate occurrence of Ra?

• Is measurement of gross alpha helpful?

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Radionuclide Health Effects

U ran iumBone cancer (50% )

K id ney toxicity (50% )

R ad iu mBone C ancer (228>226>224)

S inus C ancer (226)Bone fracturing (224, 226)

R ad onL ung cancer (>80% )

S tom ach cancer (<20% )

M C L s: A b out 1 in 20,000 riskC arcinogens (M C L G = 0)

C lass "A " = H um ansL inear d ose, N o thresho ld

Ionizing Radiation Damage = Long-term cancer riskTissue Retention Controls Dose (Time = Dose, Linear)

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Gross alpha = many individual isotope contributions!

Radium Decay Series Uranium 238 Thorium 232

Radium-226

Radium-224

Radon-222

Radium-228Radon-220

alph

a de

cay

beta

deca

y

Gross beta = many individual isotope contributions!

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Drinking Water MCLs

• Ra-226 + Ra-228 5 pCi/L

• Gross alpha 15 pCi/L

• Gross beta 4 millirems/yr

• Uranium 30 ug/L

EPA recommends samples be

collected and analyzed within 48 hours

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Where does Ra occur?

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Gundersen and Szabo,1995

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0

10

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60

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Num

ber o

f Sam

ples

Exc

eedi

ng th

e M

DC

Ra-226

Ra-224Ra-228

Percent Detection

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Distribution of NAWQA Radium Sampling

114 sites sampled in 2004

>200 sites sampled in 1998-9

Other sites sampled in 1996 -2001

Over 800 total sites, about 450 domestic wells

Picocuries/liter

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Western U.S., draft NAWQA data

Pacific Northwest Cal-Nev Rockies Southwest

National 90th percentile for sum of Ra-226 & 228

National – 90th percentile Ra-226

90th percentile for sum of Ra-226 & 228 90th percentile Ra-226

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Central U.S., draft NAWQA data

High Texas Upper Midwest Gulf Plains Coast

90th percentile for sum of Ra-226 & 228 90th percentile Ra-226

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Eastern U.S., draft NAWQA data

New North South SoutheastEngland Mid-Atlantic Mid-Atlantic

90th percentile for sum of Ra-226 & 228 90th percentile Ra-226

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Radium 228 & 226 co-occurrence

Draft NAWQA data

MCL, Ra-228 + Ra 226 = 5 pci/L

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72 Hour Gross Alpha

15 p

Ci/

L M

CL

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30 Day Gross alpha from Uranium Decay

15 p

Ci/

L M

CL

5 pci/L MCL

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Are there geochemical or geological features on National (NAWQA) and local scales that help evaluate occurrence of Ra?

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Distribution of NAWQA Ra-228 Data

198 sites, mostly Coastal Plain

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Draft NAWQA data

North Carolina NJ-Penn New England Tenn-Ala

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Hypothetical Chemical Reactions by which Hydrogen Ions in Water Increase

Radium Mobility

Ion-exchange, desorption reactions:

2H+ + Rax Ra+2 + 2Hx

•Ra is preferentially removed from solid.

•Hydrogen ion is a master variable that exerts significant control over these

reactions.

•Hydrogen ions with high concentrations of other cations preferentially

remove Ra from solid.

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Draft NAWQA data

Desorption in the presence of Nitrate

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Hypothetical Chemical Reaction That Produces Hydrogen Ions in Water and

Increases Radium Mobility

Redox reactions:

Nitrification:

NH3 + 2O2 NO3- + H2O + H+

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Ra leaching + recoil

recoil

?

Draft NAWQA data

Chemical and Physical Processes in Different Regions

Atlantic Coastal PlainHigh Plains

New EnglandTexas

Yellowstone

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CONCLUSIONS 1. Higher concentrations of Ra occur

primarily in unconsolidated aquifers - usually in acidic regions of the Eastern US

2. Ra-224 likely source of gross alpha in Eastern US

2. Ra-224 is likely to occur where other radium isotopes are present & correlates with Ra-228.

3. Ra-224 may be a substantial source of alpha activity in western US, but mobilization mechanism not understood (recoil?).

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CONCLUSIONS4. Further characterization of geochemical implications for monitoring programs and treatment applications is warranted!

More data collection and analysis is

planned

Contacts: Zoltan Szabo [email protected] 609-771-3929Jeff Fischer [email protected] 609-771-3953