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Stanford Gibson
เข้าร่วมเมื่อ 23 ต.ค. 2008
Bed Sampling Considerations in an Incised Clay Channel (ft. Dr. David Biedenharn)
Sometimes the sediment on the channel bed at low flow does not characterize the bed material or the channel geometry during an event. Dr. David Biedenharn from the US Army Corps of Engineers describes his method for exploring the thickness of cohesionless bed sediment in clay streams and implications of these thicknesses for geomorphic assessments and modeling.
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Hans Albert Einstein Award Address (2024 - Stanford Gibson)
มุมมอง 666หลายเดือนก่อน
I won the Hans Albert Einstein award this year, which is the American Society of Civil Engineers' award for contributions to Sediment and Erosion. This is the "Einstein Lecture" from the EWRI congress (in Milwaukee May 2024) that I presented when I accepted the award. The list of previous Einstein award winners is here: www.asce.org/career-growth/awards-and-honors/hans-albert-einstein-award/han...
HEC RAS Debris Flow Speed Run
มุมมอง 775หลายเดือนก่อน
How long does it take to build an HEC-RAS debris flow model. How about under 12 minutes. In this video I leverage a theme from the video game youtubes and ask the question "how quickly can I stand up a simplified mud and debris, post wildfire model to get a hazard map in HEC-RAS starting with only the USGS hazard map web site (and an estimate of peak flow)?" Because I work through this pretty q...
Vertical Sorting Processes ft. Dr. Alain Recking
มุมมอง 3242 หลายเดือนก่อน
This is an excerpt from the RSM River Mechanics Podcast. The full interview is available here: podcasts.apple.com/us/podcast/rsm-river-mechanics-podcast/id1650989239 and other videos and interviews are available on the podcast website: www.hec.usace.army.mil/confluence/rasdocs/rastraining/latest/the-rsm-river-mechanics-podcast Bacchi, V. Recking, R., Eckert, N., Pilton, G. & Naaim, (2014) "The ...
The Exner Equation (ft Tony Thomas) Computing Sediment Continuity
มุมมอง 5753 หลายเดือนก่อน
HEC-RAS uses the version of the Exner (sediment continuity) equation in 1D that Tony Thomas developed for HEC 6 and 6T. In this found footage from his first ever HEC6 class (1976), Tony explains this fundamental equation behind the fundamental approach we use to simulate sediment transport. For a contemporary conversation with Tony about the early days of sediment transport modeling and the thi...
Compound Sediment Boundary Conditions in HEC-RAS (New in Version 6.5)
มุมมอง 4614 หลายเดือนก่อน
Rating curves can be excellent boundary conditions for suspended and wash load but modelers rarely have data for bed load rating curves. Alternately, equilibrium load can estimate bed load and even some bed material load in the absence of data, but performs very poorly with finer grain classes and wash load. So modelers would often like to use a rating curve for some grain classes and equilibri...
Iruya Debris Flows (ft. Dr. Marcelo Garcia)
มุมมอง 4605 หลายเดือนก่อน
We talked to Dr. Marcelo Garcia in episodes 3.2 and 3.3 of the podcast. podcasts.apple.com/us/podcast/rsm-river-mechanics-podcast/id1650989239 In episode 3.3. he talked about his work on "Sedimentation Hazards" including descriptions of a periodic debris flow in Iruya. podcasts.apple.com/us/podcast/marcello-garcia-part-2-on-sedimentation-hazards-the/id1650989239?i=1000643029954 He also provided...
Reservoir Sediment Managment Options ft. Dr. George Annandale
มุมมอง 4876 หลายเดือนก่อน
Dr. George Annandale provides a brief overview of some of the options available to manage reservoir sediment. This is an excerpt from Episode 2:1 of the RSM River Mechanics Podcast. You can find the full interview with Dr. George Annandale here: podcasts.apple.com/us/podcast/george-annandale-on-the-reservoir-sedimentation/id1650989239?i=1000622609844 More conversations and videos on reservoir s...
HEC-RAS "Capacity Only" 2D Sediment Modeling Demo
มุมมอง 1.6K7 หลายเดือนก่อน
HEC-RAS "Capacity Only" 2D Sediment Modeling Demo
Adding an Internal Structure to a 2D Mesh in HEC-RAS
มุมมอง 6K8 หลายเดือนก่อน
Adding an Internal Structure to a 2D Mesh in HEC-RAS
Simplified 2D Sediment Modeling with HEC-RAS ("Capacity Only" and "Concentration Only" Modes)
มุมมอง 3.6K9 หลายเดือนก่อน
HEC has added some simplified, "fixed bed," sediment transport options to the 2D Sediment model. Stanford Gibson gave this presentation to the Corps' River Engineering Working Group about how the tools developed, what they do, and how they have been applied. 2D Sediment Background and Motivation 0:05 Conceptual Model of Morphological Analysis: 3:22 Story of Tool Development (Iao Project): 5:47 ...
Spencer Drawdown Reservoir Sediment Flush (Abbreviated Version)
มุมมอง 10K10 หลายเดือนก่อน
Spencer Dam filled with sand within a couple decades of construction int he 1920s. After that, it flushed sediment twice a year to make room for hydropower operations. Dr. Paul Boyd recorded a time lapse video of the first day of the flush in 2014. We talk about this operation on season 2 of the RSM River Mechanics Podcast, which is dedicated to Reservoir Sediment Management: www.hec.usace.army...
Reservoir Sediment Modeling with HEC-RAS: (Part 3) Reservoir Modeling Demo
มุมมอง 1.5K10 หลายเดือนก่อน
Part 1: th-cam.com/video/WtM4vGMnqSU/w-d-xo.html Part 2: th-cam.com/video/XMCNJc_t7tk/w-d-xo.html Intro: 0:00 Quasi Unsteady Flow Data: 2:03 Sediment Initial Condition: 10:14 Sediment Boundary Conditions (Including developing a rating curve): 13:20 Reservoir Modeling Options: 28:33 Sediment Plan File and Simulation: 38:33 Evaluating Results: 41:00
River Mechanics Podcast Season 2 Trailer (Audio Only)
มุมมอง 12710 หลายเดือนก่อน
River Mechanics Podcast Season 2 Trailer (Audio Only)
Ecuador Travel Video: Galapagos and Ecuadorian Amazon
มุมมอง 23011 หลายเดือนก่อน
Ecuador Travel Video: Galapagos and Ecuadorian Amazon
Calibrating a 2D HEC-RAS Model with ADCP Transects
มุมมอง 2.3K11 หลายเดือนก่อน
Calibrating a 2D HEC-RAS Model with ADCP Transects
How to Copy Mods Between HEC-RAS Terrains (unexpected steps and big file hacks)
มุมมอง 1.1K11 หลายเดือนก่อน
How to Copy Mods Between HEC-RAS Terrains (unexpected steps and big file hacks)
Computing Annual Sediment Load and LOESS with HEC-RAS (Coming in v6.4)
มุมมอง 765ปีที่แล้ว
Computing Annual Sediment Load and LOESS with HEC-RAS (Coming in v6.4)
Importing USGS Terrain Directly into HEC-RAS Mapper
มุมมอง 7Kปีที่แล้ว
Importing USGS Terrain Directly into HEC-RAS Mapper
The Rio Coca Regressive Erosion (ft. Pablo Espinoza Giron and Pedro David Barrera Crespo)
มุมมอง 1.6Kปีที่แล้ว
The Rio Coca Regressive Erosion (ft. Pablo Espinoza Giron and Pedro David Barrera Crespo)
Insights from the USGS Debris Flow Flume (ft. Dr. Richard Iverson)
มุมมอง 1.4Kปีที่แล้ว
Insights from the USGS Debris Flow Flume (ft. Dr. Richard Iverson)
The Mount Saint Helens Sediment Retention Structure (ft Chris Nygaard)
มุมมอง 838ปีที่แล้ว
The Mount Saint Helens Sediment Retention Structure (ft Chris Nygaard)
Missouri River Management and Sediment (ft. John Remus)
มุมมอง 542ปีที่แล้ว
Missouri River Management and Sediment (ft. John Remus)
Step-Pool Spacing, Formation, and Experiments (ft. Dr Joanna Curran)
มุมมอง 1.1Kปีที่แล้ว
Step-Pool Spacing, Formation, and Experiments (ft. Dr Joanna Curran)
The Copeland Analytical Channel Design Approach (ft. Dr. Ron Copeland) (07Dec2022 repost)
มุมมอง 434ปีที่แล้ว
The Copeland Analytical Channel Design Approach (ft. Dr. Ron Copeland) (07Dec2022 repost)
Using HEC-RAS Mapper Mods to REMOVE an Irregular Feature
มุมมอง 2.1Kปีที่แล้ว
Using HEC-RAS Mapper Mods to REMOVE an Irregular Feature
Sediment Measurement Variability - ft. Molly Wood (Podcast Excerpt)
มุมมอง 568ปีที่แล้ว
Sediment Measurement Variability - ft. Molly Wood (Podcast Excerpt)
Plotting 2D HEC-RAS Results Along a Breakline
มุมมอง 1.8Kปีที่แล้ว
Plotting 2D HEC-RAS Results Along a Breakline
Very cool! This reminds me of how different periods of freezing/thawing (as well as many other processes) create distinct layers of snow and ice crystals over a snow slope - which can be responsible for avalanches.
These Podcasts are really cool, the excerpts with additional complemenary data/videos/graphics makes it super interesting. One thing I would like to see added, is the option of having video format for the whole podcast like Joe Rogan does IT just gives a nice feel to it, Morevoer, these images can be shown in real time, during the podcast with some help ofcourse, Furthermore, these edits can still be continued after the podcasts.
For sure...that would be great...but the editing time would preclude any new sediment features in RAS for the foreseeable future. :)
Congratulations Stan! Great acceptance speech!
I love you!! Thank you much.....
Well deserved
Bro, you just found fresh Troll dung!! 😅
Hahaha...for sure. I update my hypothesis.
It's so much fun to see a former student! I always wonder what the "kids" are doing with their lives. Congratulations, Stan. Well deserved recognition.
BRAVO!!!
Too good to give thanks......but still thank you so much sir❤
Model of How the Grand Canyon was made.
Congrats!!! And thank you for the general tip about using "Rules" for gate controls. I just used it in a Debris Model by assuming the bridge will clog when approximately half amount of material passes through the bridge opening.
Excellent! Very creative. I have done something very similar. We often make blanket assumptions about bridge clogging (e.g. all bridges will clog 50 or 80% except freeways) in debris flow. But clogging them from the start can mess with arrival times (flooding arrives too early). So using a gate to "clog" a "bridge" is a great way to get the best of both worlds.
Thank you very much for this very useful video, from Cote d'Ivoire (Ivory Coast)
Congratulations!🎉🎉🎉🎉
Very useful, thanks for the lesson! I'm working with this Bingham model in my master thesis. I have a question about the non newtonian Cv parameter: If I set the Cv = 60% and select the "Do Not Bulk" option, then the simulation doesn't take into account the volume concentration? Or is it actually taken into account but its assumed that it is included in the flow hydrograph? (and if so, how does the bulking factor work in this case?) I have been running the model all this time with "do not bulk" option, does this mean I am modeling clear water?
The bulking option assumes your boundary condition is a clear water hydrograph and RAS is adding your solids to it. "Do not bulk" assumes that your boundary hydrograph is a time series of the whole mixture volume.
But, if you use the O'Brian or exponential rheology equations, those use Cv, so you can choose "do not bulk" and still have effects from Cv. If you choose user specified parameters and "do not bulk" the model will be insensitive to your Cv...assuming that you already included it in your boundary hydrograph. HMS includes both options, a bulk mixture hydrograph, or a clear water hydrograph and a Cv time series.
Thanks sir. thats helpful for ma paper. How to solve the error, Minimum error exceds allowable tolerance at ??? I am from Afrika Ethiopian 🇪🇹
Congratulations🎉
How to export the clone terrain to a raster for use in arcgis or other programs. Tried to use the export raster option, but it just export the image raster.
🎉🎉🎉
I'am very grateful for people like you.
Interesting! A quick question: how does RAS account for the fluid density of the debris flow mixture, and how to specify the material’s specific grain density? Density is often twice as large as clear water and can have significant impact on flow dynamics. Thanks in advance!
We compute fluid density based on the concentration by volume (CV) in the non-Newtonian fixed bed model, which means that for now we assume the solid phase has a specific gravity of 2.65. I suppose you could estimate higher density material with some sort of "apparent Cv" that converts mass in to volume...but I'd need to think/read more about that. Overall, though, most of the density effects are in the empirical parameters, not the physics, anyway, so I don't think it matters too much. In the mobile-bed sediment transport model you can edit the specific gravity of each grain class and simulate multiple grain density transport....but that is a much bigger effort.
I am going to post a video on Binham parameters in a couple months...if you would like to preview a rough draft, reach out ot me on linkedin and I can give you a link
Hello, i have written to you before. I'm working on my bachelors thesis on HEC-RAS sediment moddeling and have run into an issue while hydraulicaly calibraing my model. I have 6 gates in a SA/2D connections opening based on the rules i've set but based on my previous runs it seems like they dont follow the rules at all in fact most of the gates dont open at all. This has left me and all my professors confused since we do not see any problem with my model. Would you please help me because i have been trying to resolve this issue for over a month now and I'm at my wits end. Thank you very much.
I don't think I've tested connections with rules in a 2D sediment model. There is a chance that that particular confluence of features has a bug. If you believe there is a bug, please send the files to the RAS inbox www.hec.usace.army.mil/contact/
@@stanfordgibson I have not tried adding any sediment data yet because I can't calibrate the model hydraulicaly. I semt an email to the email you have send. I've run more tests and the gates just do not work...
Good job Stanford
thank you so much! very helpful!
Wow, even the huge natural arch is gone now.
Thank you for your instructions!
Thank you for this video, greetings from Prague
Hi Dr. Gibson, I want to know the difference between the 2D Initial Condition/WarmUp (Ramp Up hours) and the 2D Sediment WarmUp Periods (concentration, gradation & bathymetry). Do I need both warmup parameters for a 2D Sediment analysis or when I'd need to introduce those 3 sediment warmup periods? Thank you so much for your videos!! (I'm from Peru btw)
Hello! Is there a way to print this results directly from RASMapper Plot? I don't see an option other than a screenshot or snip. Thanks!
Dr. Gibson, please help me. I cant visualize “bed change” in RAS Mapper
When I try and run a model with a dataset and following the instructions in the videos I get the following error: An error occurred while reading sediment data at (blank) review your data at this location for completeness and consistency I checked and there is bed gradation data and all my cross sections and I am testing out my downstream boundary condition as equilibrium load to rule out any errors. What is the overall meaning of this error and how do I fix it?
Usually some of your initial conditions data is not complete...you are missing gradations or control volume values at one or more cross sections
Is it possible to set up model where there is essentially a dam break of large cobbles and boulders? I was thinking that I could do this by modeling a short burst hydrograph (only a minute long), but am weary that there will be numerical oscillations in the process.
A question: can we run the turbulence model without a sediment transport simulation.I mean just for a 2D inondation mapping ? or not possible because we need to have solutes to solve the equations for the advection.
Yes, you can run turbulence for a simple hydraulic model. It will affect the velocity distribution across the channel. So if you are interested in detailed velocities it can help. But it is essential in sediment because we are so dependent on detailed veleocities.
Hello! Wondering if you have a video on bridge scour calculations? I have not been able to find one but perhaps missed one?
Hello Gibson, I have been following your videos on RAS analysis, and I find them incredibly helpful. I have a question regarding the datum. You mentioned the High-Water Mark (HWM) elevation as 6.4 feet, and you also mentioned some calculations with terrain. Could you please explain a bit more about your datum and how you arrived at the value of 693.4 feet after performing those calculations? I often get confused between HWM elevation and model projections. For example, I have an HEC-RAS model projected in NAD_1983_UTM_Zone_16N. Additionally, I’ve collected HWM data from USGS, "Black Sharpie mark on red fire hydrant 2.25' above ground in the liberty ball field, hydrant is 9.3 meters from edge of parking lot" measure at 278.9 feet above NAVD88. How can I adjust the HWM height and compare it with the RAS-simulated stage?
This content is pure gold! Thanks for sharing! Greetings from Brazil
Thank you / gracias to everyone involved in the making of this video. This geologic event has been fascinating to watch from afar and it has been very interesting to me!
there's equations for sedimentations ?? wow
Hello, Thanks for the video. I'd like to know the HEC-RAS limitations. When we simulate sediment transport, usually we have rivers with steep slopes ( greather than 4%). Which is the max bed slope of the channel that HEC-RAS could handle? could you help me with this question please?
I have a 10' x 10' culvert with water coming out at 17 fps and going into a natural channel. Our 2 ton riprap got washed away with the recent rains here in CA. So now I'm trying to size the riprap so it doesn't get washed away. so I'm making my upstream reference section to be the culvert which has the most velocity. The design section is about 15 ' downstream and I'm using that. So now the question: What section is used for the input data? It's all straight so there is no radius. But the side slope of the reference section is 90 and the side slope of the design section is 35 in the natural channel. So what numbers do I use?
You can find the podcast episode here: podcasts.apple.com/us/podcast/tony-thomas-on-the-origin-of-sediment-modeling/id1650989239?i=1000648600876
Thank for a great video, but how can one go for calibration if one does not has ADCP data
You can only calibrate to data you have...so you could still do a quasi-1D calibration to high water marks (preferably for multiple flows). It won't resolve your lateral velocity distribution (which is important for sediment) but is MUCH better than not calibrating.
@@stanfordgibson Can you explain it in more detail.
Many thanks Dr. Stanford.
The Tony Thomas episode was extremely informative. Thank you for putting these together.
can I use any similar technique to estimate the sediment rating curve/total sediment load for an un-gaged river?
Hello Stanford, I hope this message finds you well. I wanted to commend you on the superb content and engaging work you've been producing. I have a question regarding the "Concentration Only" Mode. Currently, I am in the process of calibrating experiments conducted by GUTA at LEGI LAB Grenoble, France, using HEC-RAS 2D. The setup involves different settings of incoming loads (below capacity) categorized as LOW, MED, and HIGH, with a flume width of 0.35m. I've encountered a few challenges: 1. Firstly, I am working with a particle density of 1192 kg/m³. Utilizing "User Defined Grain Classes," I inputted SG = 1.192 and BD = 655.6 kg/m³ with a porosity of 45%. I also adjusted the classes' diameters as required. My question is, does this approach work effectively? 2. Secondly, when inputting the upstream inflow boundary condition, whether using the Rating Curve or Time Series, I entered a value of 2 tonnes/day, which translates to 0.078 kg/m/s. However, the Results Map for "Total Load Transport Capacity" is indicating a significantly lower value of about 0.003 kg/m/s. Which Results Map should I refer to for the sediment rate or flux? I find it peculiar that the induced value is not reflected accurately in the model. Any insights on this discrepancy would be greatly appreciated. 3. Thirdly , is there a way to separate the sediment boundary condition from the flow boundary location? In the lab flume, the inflow is controlled by a hopper/funnel, positioned precisely. Is there a workaround for this? Your expertise and guidance on these matters would be invaluable. Thank you for your time and assistance. 4. Lastly, I'm interested in understanding how to utilize the Non-Erodible Method in Adaptation Parameters. Could you please provide guidance on its implementation?
If you reach out to me on LinkedIn or ResearchGate I can look at your model and see if there is a bug in the boundary
Thank you for this. That last bit about the checking the cell elevation that the structure is connected to helped me solve the error on my model.
Great. Yeah, that is a common issue.
Hello, thanks for the tutorial. How do you "define your own grain classes" ? This log2 scale is really not convenient and I was not able to find where to customize it. Thanks in advance !
Go to Options-->User Defined Grain Classes (top option) in the sediment editor. There you can change the grain sizes (note-the program only actually uses the mean size) and names. If your material is sand, start with grain class 6 and higher. RAS automatically assumes those first 5 grain glasses are silt and clay regardless of their size. www.hec.usace.army.mil/confluence/rasdocs/rassed1d/1d-sediment-transport-user-s-manual/entering-and-editing-sediment-data/sediment-properties-options/define-grain-classes-and-sediment-properties
@@stanfordgibson Thanks a lot for your answer
Where is Eddie's PFD?
very cool, will look for this..
Great video, Stanford! Thanks for sharing. Bridges still seem like a bit of an afterthought at USACE. Getting detailed info through bridges is primary importance for DOT's and other owners. This is a good procedure toward that end. Our group will work with this methodology for skewed bridges, column bents, etc. where we need to have good understanding of what's happening under and around our bridges. Hope you'll provide other similar videos in the near future! Also hoping USACE will finally address their outdated scour procedures. Maybe version 7.0?