scholarly journals Median bed-material sediment particle size across rivers in the contiguous U.S.

2021 ◽  
Author(s):  
Guta Wakbulcho Abeshu ◽  
Hong-Yi Li ◽  
Zhenduo Zhu ◽  
Zeli Tan ◽  
L. Ruby Leung

Abstract. Bed-material sediment particle size data, particularly for the median sediment particle size (D50), are critical for understanding and modeling riverine sediment transport. However, sediment particle size observations are primarily available at individual sites. Large-scale modeling and assessment of riverine sediment transport are limited by the lack of continuous regional maps of bed-material sediment particle size. We hence present a map of D50 over the contiguous U.S. in a vector format that corresponds to millions of river segments (i.e., flowlines) in the National Hydrography Dataset Plus (NHDplus) dataset. We develop the map in four steps: 1) collect and process the observed D50 data from 2577 U.S. Geological Survey stations or U.S. Army Corps of Engineers sampling locations; 2) collocate these data with the NHDplus flowlines based on their geographic locations, resulting in 1691 flowlines with collocated D50 values; 3) develop a predictive model using the eXtreme Gradient Boosting (XGBoost) machine learning method based on the observed D50 data and the corresponding climate, hydrology, geology and other attributes retrieved from the NHDplus dataset; 4) estimate the D50 values for flowlines without observations using the XGBoost predictive model. We expect this map to be useful for various purposes such as research in large-scale river sediment transport using model- and data-driven approaches, teaching of environmental and earth system sciences, planning and managing floodplain zones, etc. The map is available at http://doi.org/10.5281/zenodo.4921987 (Li et al., 2021).

2018 ◽  
Vol 40 ◽  
pp. 05025 ◽  
Author(s):  
Jeremy Lepesqueur ◽  
Renaud Hostache ◽  
Núria Martinez-Carreras ◽  
Luc Manceau ◽  
Claire Delus ◽  
...  

Many studies focusing on suspended sediment transport modelling in river systems only consider one class of sediment grain size. Rather recently, the SISYPHE sediment transport model has integrated sand-mud mixture transport processes using two classes of sediment. However, this new modelling framework still suffers from limitations, and increasing the number of sediment classes would arguably improve sediment transport and therefore riverbed evolution simulations. Moreover, current sediment transport models do not simulate sediment particle aggregation and disaggregation processes while these can play an important role in sediment transport. Integrating these new concepts would then contribute to significant improvements to river bed morphodynamics and sediment transport modelling. In this study, we further develop the SISYPHE model by extending the sediment particle size distribution to ten classes and integrating flocculation processes (coupling with the flocculation FLOCMOD model). The preliminary results we present in this paper are based on a large-scale flood event, which occurred in river Orne, north-eastern France. We clearly show that the proposed developments of SYSIPHE improves qualitatively and quantitatively the predictions of sediment transport and riverbed morphodynamics.


2016 ◽  
Vol 572 ◽  
pp. 207-215 ◽  
Author(s):  
Yun Zhang ◽  
Jodi L. Sangster ◽  
Lukasz Gauza ◽  
Shannon L. Bartelt-Hunt

2021 ◽  
pp. 104548
Author(s):  
Jon Barry ◽  
Claire Mason ◽  
Lydia McIntyre-Brown ◽  
Keith M. Cooper

2020 ◽  
Vol 710 ◽  
pp. 136348
Author(s):  
Tatenda Dalu ◽  
Ross N. Cuthbert ◽  
Tiyisani L. Chavalala ◽  
P. William Froneman ◽  
Ryan J. Wasserman

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