Paper No. 13
Presentation Time: 11:35 AM
SR ISOTOPE COMPOSITIONS OF GROUNDWATER IN THE HANFORD SITE UNCONFINED AQUIFER AS A RECORD OF FLOW, RECHARGE, AND VADOSE ZONE INFILTRATION
SINGLETON, Michael J.1, MAHER, Katharine
2, DEPAOLO, Donald J.
2, CONRAD, Mark E.
1 and DRESEL, P. Evan
3, (1)Center for Isotope Geochemistry, Earth Sciences Division, Lawrence Berkeley National Lab, 1 Cyclotron RD, MS 70A-4418, Berkeley, CA 94720, (2)Center for Isotope Geochemistry, UC Berkeley, Berkeley, CA 94720-4746, (3)Field Hydrology & Chemistry Group, Battelle Northwest, MS K6-96, 3110 Port of Benton BLVD, Richland, WA 99352-2230, mjsingleton@lbl.gov
Sr isotope compositions from more than 260 wells in the unconfined
aquifer below the contaminated Hanford Site, WA provide a means to
image groundwater recharge, infiltration, and perturbations from site
activity. Natural recharge to the unconfined aquifer primarily
comes from the exposed basalt of the Yakima Ridge and Rattlesnake Hills
at the western margin of the site, and thus groundwater in this area
has lower
87Sr/
86Sr (~0.707) than either Columbia River water
(0.714±0.0004) or water that has equilibrated with the granitic
sediments (~0.712). Anthropogenic recharge of the unconfined
aquifer from disposed Columbia River water has resulted in plumes of
high
87Sr/
86Sr groundwater down gradient from infiltration ponds.
Transient, high concentration Sr flushed out of the vadose zone by
infiltrating disposal water at the 200 areas dominates the shift of Sr
isotopes caused by weathering of aquifer sediments. Low
87Sr/
86Sr
water south of Gable Mountain is evidence of upwelling from the upper
confined aquifer, which may affect the shape of contamination plumes in
this area.
Groundwater 87Sr/86Sr increases systematically from 0.707 to 0.712
along aquifer flow paths, generally running west to east across the
Hanford Site. This observed variation in groundwater Sr isotope
composition is modeled as a process whereby lower 87Sr/86Sr recharge
waters are shifted toward a ratio of 0.712, due to the addition of Sr
from weathering of the aquifer sediments and infiltration through the
vadose zone. The degree to which groundwater 87Sr/86Sr approaches
the dissolving or infiltrating Sr is governed by the groundwater
velocity, infiltration flux, aquifer thickness, and by weathering rates
in the aquifer sediments. Infiltrating vadose zone pore waters
are approximately an order of magnitude higher in Sr concentration than
the groundwater, and therefore have a strong effect on the Sr isotope
composition of groundwaters. Combining measurements of hydraulic
head and aquifer thickness with measurements of groundwater 87Sr/86Sr
and Sr concentration allows for estimates of vadose zone infiltration
flux. The 87Sr/86Sr increase along a "background" profile across
the Hanford site is consistent with an average vadose zone flux of 5-8
mm/yr, based on a steady-state model of Sr reactive transport and
infiltration.