U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
Spatial Variability of Unsaturated-Zone Properties in Relation
to Topography in a Sand-Plain Setting near Princeton, Minnesota
by
G.N. Delin (U.S. Geological Survey, Mounds View, Minn.), M.K.
Landon (U.S. Geological Survey, Mounds View, Minn.), R.W. Healy (U.S. Geological
Survey, Lakewood, Colo.), and H.W. Olsen (U.S. Geological Survey, Golden,
Colo.)
Abstract
The spatial distribution of preferential flow paths and unsaturated-zone
properties in two topographic settings were determined from a dye-tracing
and trenching study done at the Management Systems Evaluation Area (MSEA)
near Princeton, Minnesota. The topographic settings are upland and lowland
sites about 78 m (meters) apart that differ in elevation by 1.4 m. A 3 percent
solution of rhodamine-WT dye was applied uniformly as a tracer to a 3.5-
by 6-m area at both sites at 10-day intervals from July 5 through September
13, 1991. After application of the dye, a 3- by 2-m trench was dug to a
depth of 2 m in the middle of each dye-application area to locate the dye
and to collect soil samples.
Water samples were collected periodically from a multiport well, located
2.5 m horizontally downgradient of each dye-application area, to estimate
the time-of-travel of recharge water through the unsaturated zone. The dye
was first detected in ground water about 100 days after application. On
the basis of average ground-water velocity at the Princeton MSEA of 10 cm/d
(centimeters per day), the transport velocity of dye through the unsaturated
zone was calculated to be 3.7 cm/d at the lowland site and 5.3 cm/d at the
upland site. The dye moved 2 m vertically through the saturated zone over
a horizontal distance of about 9 m, whereas a steady-state ground-water-flow
model predicted less than 0.2 m of vertical movement.
A total of about 450 soil samples were collected from the sides and bottom
of the trenches for analyses of bulk density, dye fluorescence, grain-size
distribution, hydraulic conductivity, moisture-retention characteristics,
organic-carbon content, and volumetric moisture content. The distribution
of dye through the unsaturated zone was highly variable at the upland and
lowland sites. Dye movement was greatest beneath the furrows and least beneath
the corn rows. Preliminary results indicate the dye moved preferentially
in response to tillage patterns (corn rows and furrows), microtopography,
presence of plant roots, differences in total organic carbon, and coarser-grained
heterogeneities in the unsaturated zone. Visible dye distribution did not
correlate strongly with bulk density, saturated hydraulic conductivity,
moisture-retention characteristics, and volumetric moisture content.
|
|