Published January 1990 | Version v1
Report Restricted

Natural radionuclides in groundwaters

Description

The U-234 and Th-230 radionuclides are highly retarded by factors of 104 to 105 in basalt groundwater (Hanford) and briny groundwaters from Texas and geothermal brine from the Salton Sea Geothermal Field (SSGF). In basalt groundwaters (low ionic strength), Ra is highly sorbed, while in brines (high ionic strength), Ra is soluble. This is probably because the sorption sites are saturated with Na+ and Cl- ions and RaCl2 is soluble in brines. Pb-210 is soluble in SSGF brine, probably as a chloride complex. The U-234/Th-230 ratios in basalt groundwaters and brines from Texas and SSGF are nearly unity, indicating that U is in the +4 state, suggesting a reducing environment for these aquifers. 19 refs., 3 figs

Availability note (English)

MF available from INIS under the Report Number; NTIS, PC A03/MF A01 as DE90015286; OSTI; INIS; US Govt. Printing Office Dep.

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Additional details

Publishing Information

Imprint Pagination
14 p.
Report number
PNL-SA--17438

Conference

Title
3. international conference on low-level measurements of actinides and long-lived radionuclides in biological and environmental samples.
Dates
29 Jan - 2 Feb 1990.
Place
Bombay (India).

Optional Information

Contract/Grant/Project number
Contract AC06-76RL01830
Secondary number(s)
CONF-900125--1.