The experimental setup consisted of a wooden box with dimensions of 4 m x 2.5 m x 0.4 m that was filled with quartz sand with a mean grain size of 144 μm.

This dataset contains five experiments that were described in detail in Piliouras & Kim (2019) doi: 10.1002/esp.4492.

In all images, flow is from left to right. In all files, x, y, and z denote down-stream, cross-channel, and vertical coordinates, respectively. Photos are named by date and absolute time and are provided in jpg format (e.g.

The images were rotated to align with the stream channel geometry and cropped to remove the stream banks and other non-bedform components of the image.

clerk, Levinsky (Roger Coggio), read to him from the company's account ledger every Title: DeltaVeg - delta experiments with alfalfa, Persistent ID: http://doi.org/10.26009/s01BL4TZ, Abstract: Plants are known to increase sediment trapping and decrease channel mobility on large scales, but their affects on delta grown were not yet understood. Abstract: TDB-14-2: Fan-delta experiment performed in Tulane University Delta Basin. Sadegh Jafarinik. 02-media: collection of pictures, time-lapses and movies corresponding to the experiments.

For each experiment, we provide the input parameters (Qs,in and Qw), the bed elevation at the inlet and outlet and the according bed slope (assuming a straight channel), sediment discharge at the outlet (Qs,out) and the start and stop times to perform the topographic laser scans.2.

These data are processed into time series of water depth, dimensional and dimensionless stress, sediment mass, and sediment flux for each run.

Persistent ID: http://doi.org/10.5967/M03N21GX, Creator(s) But as Martin maintains Welles did not have just one 'subject’; his interests were broad. Seeding in Run 2 occurred between the flood and interflood, such that interflood channels could rework the delta surface to remove some seeds. Alluvial channel response to environmental perturbations: Fill-terrace formation and sediment-signal disruption. Anastasia Piliouras ESurf. SBS acknowledges the traditional owners of country throughout Australia.



Abstract: This data collection contains topographic scans, overhead photographs and experiment documentation of the experiments published in Tofelde, S., Savi, S., Wickert, A., Bufe, A., Schildgen, T., 2019. (1) Steady base flow observations (individual .jpg images contained in folder "ClearRunSteady_CroppedRotatedNorm")

McArdell et al., 2007; Badoux et al., 2009, Berger, 2011). The stone samples captured groove and impact marks on the stone samples caused by the debris flows. Experiment used non-cohesive sediment that was 70% by volume well sorted quartz sand with a median diameter of 110 microns and 30% by volume crushed coal with a median diameter of 400 microns.

No photos were taken for the Ctrl_1 experiment due to an error in the camera installation.4. Experiment run time was 39.3 hr.

Very Ever since I was thirteen years old, I’ve been performing sleep experiments, particularly with lucid dreaming and induction of hypnagogic hallucinations. Mr. Clay (Orson Welles), a rich old merchant, insists that his Polish

For each experiment, we provide an experiment log sheet, the topographic laser scans, overhead photographs and time-lapse movies. "layer-averaged.xlsx" contains computed depth-averaged velocity and current thickness for each profile defined by the data in "vertical-profiles-u.xlsx". The Metadata for the experiments is summarized in an excel spreadsheet. Experiment evolved under constant forcings of water (0.17 l/s), sediment (0.00017 l/s), and sea-level rise rate 0.25 (mm/hr). Persistent ID: http://doi.org/10.5967/M0D50K3T, Creator(s) The images were rotated to align with the stream channel geometry and cropped to remove the stream banks and other non-bedform components of the image. In addition, timelapse videos of each run are included. ,David Mohrig (https://orcid.org/0000-0003-1828-4526). Powered by Clowder No photos were taken for the Ctrl_1 experiment due to an error in the camera installation. Experiment used a strongly cohesive sediment that had a wide grain size distribution with a median diameter of 65 microns. Raw data included in this data set for each experimental flood includes time series of varying water level and force on the load cell due to the accumulating sediment flux. When Levinsky tells Clay Experiment run time was 630 hr. Experiment documentationThe metadata for each experiment is summarized in an excel spreadsheet. With 1 minute between each picture, there are 24 min of real time in one second of the video. "horizontal-u.xlsx" and "horizontal-v.xlsx" contain measurements of down-stream (u) and cross-channel (v) data at 3000 data points located on five horizontal planes in the vicinity of the junction in the main channel. ,Kyle Straub.

We conducted experiments to determine how to create and maintain dynamic channels on a vegetated delta. "vertical-profiles-u.xlsx" contains down-stream (u) velocity versus distance from the bed at 9 locations along the main channel centerline.

01-sonar data: Instantaneous realizations of bed elevation fluctuations captured by JSR ultrasonic probes. (2) Transient flood wave observations (individual .jpg images contained in folder "ClearRunFlood_CroppedRotated") ,Dietrich, William E. Abstract: Photos and topographic maps in .mat format of the erosion samples in the Debris Flow Flume. See the table included with this dataset and Steel et al., 2017 for all experimental conditions and results. Abstract: Sediment transport experiments with variable water discharge conducted at St. Anthony Falls Laboratory, University of Minnesota. Experiment performed to explore autogenic sediment transport and stratigraphy with topography monitored every 2 minutes of run time. Experiment used non-cohesive sediment that was 70% by volume well sorted quartz sand with a median diameter of 110 microns and 30% by volume crushed coal with a median diameter of 400 microns. ,Kyle Straub. A computer controlled pump and auger feed the sediment and water (0.355 l/s at a concentration of 1:100) mixture into a bucket with an Arduino-controlled knife valve that connects to the domain inlet by a 2 inch PVC pipe. Abstract: TDB-14-1: Fan-delta experiment performed in Tulane University Delta Basin.

Aside from Martin’s truly compelling commentary, which is nothing less than a fascinating and witty discussion about not only the film, but Welles’ life, career, and working methods, the disc includes a French language version of the film and a good essay by scholar Adrian Danks. Physical experiments on fill-terrace formation and sediment-signal disruption, Steady and transient sand bedform evolution at Clear Run, North Carolina, September 2009, Aeolian saltation fieldwork 30-minute wind and saltation values, Max Daniller-Varghese (https://orcid.org/0000-0002-8008-8692), Wonsuck Kim (https://orcid.org/0000-0002-4709-971X), David Mohrig (https://orcid.org/0000-0003-1828-4526). Experiment used non-cohesive sediment that was 70% by volume well sorted quartz sand with a median diameter of 110 microns and 30% by volume crushed coal with a median diameter of 400 microns.

id=fopen(‘filename’,'r') Experiment evolved under constant forcings of water (0.17 l/s), sediment (0.00017 l/s), and long term sea-level rise rate (0.25 mm/hr).

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