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Scott Ducar Thesis Defense
October 23 @ 3:00 pm - 5:00 pm MDT
DECIPHERING THE SIGNAL OF MODERN TO HOLOCENE DRIVERS OF COMPLEX CHANNEL RESPONSE OF A SMALL ALLUVIAL STREAM
Small alluvial stream (~100km2 drainage area) are important for water resources and aquatic habitat. Small streams throughout the Western United States are impacted by anthropogenic land-use including urban development, mining, logging, beaver trapping, grazing, and farming. Often land-use causes a complex series of channel response which varies spatially and temporally in the watershed. However, streams are also undergoing response from other external variables, (tectonics, base-level, and climate) which makes disentangling the drivers of channel response complicated. Therefore, it is important to place modern channel changes into a longer geomorphic context to fully understand the complex response initiated by land-use. In this study we use a representative small alluvial stream, Lower Dry Creek (LDC), a tributary to the Boise River in Idaho, to understand how changes in land-use may drive channel response which vary spatially in the watershed.
LDC marks the transition from the rugged and largely un-developed upland Dry Creek Experimental Watershed to the lower gradient, agricultural, and residential section of the watershed. LDC has a complex history of placer mining, beaver trapping, grazing, and farming since the 1850’s. Recent (post-1997) growth in the region converted LDC’s expansive floodplain from agricultural land to housing developments. Most of the recent development and historic and current farmland are on the broad, low gradient Hidden Springs Terrace. We use remote sensing, hydraulic modeling, grain size analysis, and field observations to quantify how the distinct reaches of LDC are changing over human time scales; we use Quaternary dating methods and geomorphic mapping to examine how LDC has changed over centennial to millennial time scales.
Optically Stimulated Luminescence (OSL) dates of fluvial sediments in an upper reach indicate incision in LDC after 4.79 ± 1.05 ka. Around 0.79 to 0.67 ka, a large packet of sheetfloods and cross-bedded sands is deposited, which correlates to a period of more fire activity and alluvial fan deposition in the region. After approximately 0.67 ka the reach incised 2.4 m. Late 1800’s placer mining activity shifted the channel behavior from incision to lateral adjustment. We measured an average of 0.6 m/yr of meander migration from 1938 to 2019 in an upper reach. Migration rate increased threefold after 1992, which corresponds temporally with a large rain-on-snow flood event in 1997 but slowed after 2011.
Comparison of the modern longitudinal profile of LDC with the longitudinal profile of the Hidden Springs Terrace, combined with grain size analysis and historic dating reveals how prior land use change is impacting the present channel. LDC’s current profile is convex in middle reaches, and grain size analysis shows a fining in the middle reaches and then coarsening downstream. The convexity and grain size change is consistent with increased aggradation from a slug of sediment from upstream placer mining progressing downstream. Downstream where the valley is unconfined, LDC aggraded 0.75 cm/yr from 1642 to 1950 AD to form the broad Hidden Springs Terrace. However, a downstream reach is incised 4.7 m below the Hidden Springs Terrace. A modern radiocarbon date provides evidence the incision occurred post-1950 AD, potentially from channelization of Currant Creek (a tributary of LDC) as farmland is converted to housing. Hydraulic modeling shows the incised reach has a lower width/depth ratio and increased shear stress. It also illustrates LDC’s median grain size is mobile at estimated bankfull flows for all reaches, which allows the stream to rapidly adjust both vertically and laterally.
We find LDC channel response in the upper and lower reaches indicates anthropogenic land-use resulted in vertical and lateral channel change: upstream aggradation and meander migration following placer mining, and downstream incision following farmland conversion. This represents a shift from the observed channel adjustments and large-scale formation of the Hidden Springs Terrace observed over Holocene timescales. LDC illustrates textbook complex response as the stream both incises and aggrades in different locations due to differing drivers.
This study shows small alluvial streams can be very sensitive to changes in land-use. Stream incision, aggradation, and channel shifts impact aquatic and riparian species and developments adjacent to the channel. This study illustrates that determining the drivers of modern channel change need to be placed within a longer more complete context. Results of this study can support stakeholders as they strive to understand the characteristics and response of small alluvial streams to anthropogenic land-use, and best options for restoration of degraded systems.
Advisor: Jen Pierce
Co-Advisors: James McNamara, Caroline Nash, Spencer Wood, and Elowyn Yager
When: October 23, 2020
Time: 3:00 PM
Where: Zoom Meeting ID: 984 7407 4645