Eg. Drozhko et al., JOINT RUSSIAN-AMERICAN HYDROGEOLOGICAL-GEOCHEMICAL STUDIES OF THE KARACHAI-MISHELYAK SYSTEM, SOUTH URALS, RUSSIA, Environmental geology, 29(3-4), 1997, pp. 216-227
Citations number
NO
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
In September 1994, a Russian-American team conducted hydrogeological,
geochemical, geophysical, and radiometric measurements in the territor
y of the Mayak Production Association, Russia. The primary purpose of
these operations was to examine the frontal area of a radioelement- an
d nitrate-laden groundwater plume moving from the disposal site, Lake
Karachai, toward the Mishelyak River. Activities encompassed (1) isola
tion of hydrologic intervals in two wells and production of water from
these intervals, to compare isolated versus open-well sampling method
s and to determine hydraulic transmissivities of the aquifer(s); (2) s
urface and soil-water sampling, accompanying radiometric measurements
and subsequent chemical analyses; and (3) electrical resistivity profi
ling in areas of expected contrasting resistivity. Preliminary results
indicate that (1) Co-60, Cs-137, and Sr-90 are present in small conce
ntrations (similar to 0.1% of permissible levels) in water of the Mish
elyak River; (2) analyses of water samples collected by a downhole sam
pler and of water produced from packed-off intervals agree within limi
ts of laboratory accuracy, attesting to the efficacy of the sampling m
ethods presently used by the Russian workers; (3) considerable differe
nces in contaminant concentrations exist between nearby wells, support
ing the concept that the plume from Lake Karachai toward the Mishelyak
River is controlled by steeply dipping fractures and shear zones; and
(4) strong contrasts occur between the electrical resistivities of so
il and bedrock. Further collaborative work is strongly recommended and
should include more detailed isolation of intervals in wells by multi
-packer installations, to better determine the geochemical and hydrolo
gical characteristics of the Karachai-Mishelyak system; deployment of
a broader soil water and soil sampling array; a more detailed examinat
ion of the distribution and concentration of radionuclides by high-res
olution field gamma spectrometry; and a detailing of the area's electr
ical resistivity setting, using a mobile electromagnetic measurement s
ystem.