experimentalist in bed
An additional metadata file ("ClearRun_metadata.xlsx") provides timing information for each of the photos in the steady and transient flow collections. Movies were generated from the unprocessed photos and are thus for display only, not for analyses. Creator(s) These observations were made as part of a larger study of "hyporheic" (i.e., surface-subsurface) solute and fine particle exchange through the injection and tracking of tracer solutes and particles in the stream channel. clerk, Levinsky (Roger Coggio), read to him from the company's account ledger every Photos are named by date and absolute time and are provided in jpg format (e.g. Abstract: Description of the photogrammetry technique for measuring topography in the Small and Big Basins of the Richmond Field Station, University of California, Berkeley. You must be a logged-in member of the Project Space to access all the datasets and collections. ,Dietrich, William E. Topography data were collected by a laser altimeter with 5-mm resolution in x and y, and sub-millimeter vertical resolution.
The experiments had to be interrupted to acquire the scans (absolute times given in the excel spreadsheet). In particular, two scenarios were considered for observing hyporheic exchange and associated bedform evolution: (1) steady background "base" flow conditions, and (2) time-varying "flood wave" conditions associated with the opening of an artificial dam upstream of the observation section on the stream. Specific details for each set of images are provided here:(1) Steady base flow observations (individual .jpg images contained in folder "ClearRunSteady_CroppedRotatedNorm")Images numbered 12 to 588 (577 total images, numbers increasing through time) were captured at 30-second intervals during steady base flow conditions on 18 September 2009, starting at 11:00:32 AM local time (Eastern Daylight Time). The images provided here were captured with a Nikon D5000 camera looking downward from approximately 2.5m above the stream bed. Leslie Hsu The scans were acquired in five parallel, overlapping swaths that were merged afterwards (merged scans provided here). Experiments were conducted to examine the role of basin depth on autogenic reworking timescales and delta morphology for fan deltas. All experiments are conducted with 170um silica sand, alfalfa for vegetation, and 0.02m basin depth. Experiment run time was 1000 hr.
Assume no refrigerator or heat pump is used in the process.
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). ,Huppert, Kimberly L.
The data are separated as follows: Experimental deltas are highly depositional by nature, so plants effectively erased channels. Time-lapse images were captured every 30 seconds.
Abstract: TDB-13-1: Fan-delta experiment performed in Tulane University Delta Basin. K) in order to reduce the heat loss by 90 percent, Assuming the outer surface temperature of the metal section still remains at about 110°C, determine the thickness of the insulation that needs to be used. This dataset includes several image image types for each experiment: (1) raw unprocessed time lapse photos for all floods and interfloods; (2) binary masks of delta topsets; (3) binary masks of wetted area; and (4) binary masks of vegetation cover, only for experiments that had vegetation. Creator(s) At the inlet, water discharge (Qw) and sediment supply (Qs,in) could be regulated separately. Yinan Wang
Each folder contains two additional text files containing the image names and the according experimental runtime in seconds. In all images, flow is from left to right. equilibrium or aggradational runs. 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. Title: Delta size and plant density experiments, Persistent ID: http://doi.org/10.26009/s0QMHSQP. It was founded in 2014 with as its main mission to make a simple, accessible test to help beginning kinksters determine which labels are or aren't suitable for them; and to be a fun experience for everyone taking it, beginners and experts alike.
Paper run names and dataset run numbers:
"layer-averaged.xlsx" contains computed depth-averaged velocity and current thickness for each profile defined by the data in "vertical-profiles-u.xlsx". ,Sweeney, Kristin
U and H are depth-averaged velocity and current thickness, respectively. 01-sonar data: Instantaneous realizations of bed elevation fluctuations captured by JSR ultrasonic probes. Images numbered 12 to 588 (577 total images, numbers increasing through time) were captured at 30-second intervals during steady base flow conditions on 18 September 2009, starting at 11:00:32 AM local time (Eastern Daylight Time). Abstract: This experiment is part of a larger ensemble exploring flood intermittency and delta island growth. ,Wonsuck Kim. And naturally that brought trouble with filmmaking’s power brokers – studios, distributors, financiers. In particular, two scenarios were considered for observing hyporheic exchange and associated bedform evolution: (1) steady background "base" flow conditions, and (2) time-varying "flood wave" conditions associated with the opening of an artificial dam upstream of the observation section on the stream. ,Sklar, Leonard S. We performed experiments to determine what controlled dune subsidence rates and the amount of subsidence, such that we might produce variable subsided dune topographies. Experiment run time was 630 hr. Overhead photographs The video files are named by [Run ##]_[MMSS_start]-[MMSS_end]_[velocity m/s]. Title: Steady and transient sand bedform evolution at Clear Run, North Carolina, September 2009, Persistent ID: http://doi.org/10.5967/M0GM85FG, Creator(s) If not explicitly set, the owner of the original collection has been assumed as the creator for migration purposes. ,Eckart Meiburg, Abstract: Videos from experiments performed in 2015 at the University of Texas at Austin. But as Martin maintains Welles did not have just one 'subject’; his interests were broad.
You are not authorized to access this Project Space. Very Ever since I was thirteen years old, I’ve been performing sleep experiments, particularly with lucid dreaming and induction of hypnagogic hallucinations. Roering, Joshua The second stage had sea-level cycles with periods of 24.5 hrs and amplitudes of 3.06 mm. (1.10.1#68
We conducted experiments to determine how to create and maintain dynamic channels on a vegetated delta. There is one unvegetated experiment (Run 1) and one vegetated experiment (Run 2).
1. The first stage had sea-level cycles with periods of 24.5 hrs and amplitudes of 6.125 mm. The overall study is described in Harvey et al. 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. ,Wonsuck Kim. (1) Steady base flow observations (individual .jpg images contained in folder "ClearRunSteady_CroppedRotatedNorm") Experiment performed to explore autogenic sediment transport and stratigraphy with topography monitored every 2 minutes of run time. ,Paola, Chris.
Photos taken without running water, or when the dye was not working, were removed. Abstract: This collection contains the photographs and the topographic scans of the experiments published in Bufe A., Paola C., Burbank D.W., 2016. Experiment performed to explore autogenic sediment transport and stratigraphy with topography monitored every 2 minutes of run time. In all images, flow is from left to right.
These experiments were subjected to constant water discharge (65 cm^3/s), constant sediment discharge (1 cm^3/s) and constant base level (1 cm , 5 cm, 10 cm). Badoux, Alexandre Full details of the experimental parameters and methods can be found in Table 1 and the methods section in the paper referenced above.
copy.jpg). This dataset contains seven experiments. The images provided here were captured with a Nikon D5000 camera looking downward from approximately 2.5m above the stream bed. In each experiment, we varied either upstream water discharge (Qw), upstream sediment supply (Qs,in) or downstream base level.
Scans are numbered with the numbers given in the excel spreadsheet. This work was supported by the STC program of the National Science Foundation via the National Center for Earth-surface dynamics under the agreement EAR-0120914. 02-media: collection of pictures, time-lapses and movies corresponding to the experiments. 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. ,Dietrich, William E. Abstract: Photos and topographic maps in .mat format of the erosion samples in the Debris Flow Flume. Abstract: Files in this dataset are from a set of two experiments designed to investigate the co-evolution of vegetation and a delta channel network. Experiment evolved under constant forcings of water (0.902 l/s), sediment (0.022 l/s), and sea-level rise rate 10 mm/hr). 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.
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