Jill A. Marshall is co-author of “The problem of predicting the size distribution of sediment supplied by hillslopes to rivers.” The first author, Leonard Sklar received his PhD in Earth and Planetary Science at Berkeley. The article came out in Volume 277, 15 January 2017 of the journal Geomorphology.
Sediments link hillslopes to river channels. The size of sediments entering channels is a key control on river morphodynamics across a range of scales, from channel response to human land use to landscape response to changes in tectonic and climatic forcing. However, very little is known about what controls the size distribution of particles eroded from bedrock on hillslopes, and how particle sizes evolve before sediments are delivered to channels. Here Marshall and her co-authors take the first steps toward building a geomorphic transport law to predict the size distribution of particles produced on hillslopes and supplied to channels. They begin by identifying independent variables that can be used to quantify the influence of five key boundary conditions: lithology, climate, life, erosion rate, and topography, which together determine the suite of geomorphic processes that produce and transport sediments on hillslopes. The researchers then consider the physical and chemical mechanisms that determine the initial size distribution of rock fragments supplied to the hillslope weathering system, and the duration and intensity of weathering experienced by particles on their journey from bedrock to the channel. They propose a simple modeling framework with two components. First, the initial rock fragment sizes are set by the distribution of spacing between fractures in unweathered rock, which is influenced by stresses encountered by rock during exhumation and by rock resistance to fracture propagation. That initial size distribution is then transformed by a weathering function that captures the influence of climate and mineralogy on chemical weathering potential, and the influence of erosion rate and soil depth on residence time and the extent of particle size reduction. Model applications illustrate how spatial variation in weathering regime can lead to bimodal size distributions and downstream fining of channel sediment by down-valley fining of hillslope sediment supply, two examples of hillslope control on river sediment size. Overall, this work highlights the rich opportunities for future research into the controls on the size of sediments produced on hillslopes and delivered to channels.
Jill Marshall, Ph.D. is a postdoctoral researcher in the Berkeley Earth and Planetary Science Department. Dr. Marshall received her doctoral degree in Geosciences from the Univ. of Oregon. She is an NSF Postdoctoral Fellow working in Professor William Dietrich's Lab.
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