USGS/Cascades Volcano Observatory, Vancouver, Washington
DESCRIPTION:
Experimental Debris-Flow Flume
- Debris-Flow Flume
- To Create a Debris Flow
-
[Image,38K,JPG]
Debris-Flow Flume, Annotated
From:
Iverson, Costa, and LaHusen, 1992,
Debris-Flow Flume at H.J. Andrews Experimental Forest, Oregon:
USGS Open-File Report 92-483
-
Scientific understanding of debris flows has been
hampered by their unpredictable timing, location and
magnitude, which make systematic observation and
measurement of natural events both difficult and dangerous.
Consequently, in 1991 the U.S. Geological Survey (USGS),
in cooperation with the U.S. Forest Service, constructed a
flume to conduct controlled experiments on debris flows.
Located about 45 miles east of Eugene, Oregon, in the Cascades
Range foothills near the headquarters of the H.J. Andrews
Experimental Forest, Blue River Ranger District, Willamette
National Forest, this unique facility provides research
opportunities available nowhere else.
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The flume is a reinforced concrete channel 95 meters (310
feet) long, 2 meters (6.6 feet) wide, and 1.2 meters (4 feet)
deep that slopes 31 degrees (60 percent), an angle typical of
terrain where natural debris flows originate.
Twelve large bolts grouted into deep boreholes and tensioned to
concrete pads adjoining the flume help anchor the structure
to the underlying soil and rock. Removable glass windows
built into the side of the flume allow flows to be observed and
photographed as they sweep past. Eighteen data-collection
ports in the floor of the flume permit measurements of
forces due to particles sliding and colliding at the
base of flows.
From:
Iverson, Costa, and LaHusen, 1992,
Debris-Flow Flume at H.J. Andrews Experimental Forest, Oregon:
USGS Open-File Report 92-483
-
To create a debris flow, up to 20 cubic meters (about 40
tons) of sediment are placed behind a steel gate at the head
of the flume, saturated with water from subsurface channels
and surface sprinklers, and then released. Alternatively, a
sloping mass of sediment can be placed behind a retaining
wall at the flume head and watered until slope failure occurs.
The ensuing debris flow descends the flume and forms a
deposit on a nearly flat runout surface at the flume base.
The flume design thus accommodates research on all
stages of the debris-flow process, from initiation through
deposition. Experiments can be conducted using a variety of
materials, from mixtures of well-sorted gravel and water to
heterogeneous natural slope debris. Experimental materials
are recycled by excavating deposits with a front-end loader,
placing them in a dump truck, and hauling them back to the
staging area at the head of the flume.
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03/21/02, Lyn Topinka