Posts Tagged ‘fluvial processes’

Sampling variability

Friday, May 4th, 2012

June 2012 article (Early View):Spatial Variability of Pool-Tail Fines in Mountain Gravel-Bed Stream Affects Grid-Count Results,” by Kristin Bunte, John P. Potyondy, Kurt W. Swingle, and Steven R. Abt.

The study demonstrated how bankward fining and longitudinal differences of pool-tail fines can affect amounts, variability, and accuracy of grid-count results obtained by different sampling schemes.

Fine sediment (<2 and <6 mm) particles underlying a 49-intersection grid placed on a streambed at 25, 50, and 75% of the wetted pool-tail width are commonly counted to assess the status and trend of aquatic ecosystems or to monitor changes in the supply of fines in mountain gravel-bed streams. However, results vary even when crews perform nearly identical procedures. This study hypothesized that spatial variability of pool-tail fines affects grid-count results and that a sampling scheme can be optimized for precision and accuracy. Grid counts taken at seven evenly spaced locations across the wetted width of 10 pool tails in a pool-riffle study stream indicated a bankward fining trend with secondary peaks of fines within the stream center. Sampling locations close to the waterlines harbored more than twice as many fines as central locations. Most of the five grid-count schemes derived from the seven sampled locations produced significantly different results. Compared with sampling at all seven locations, schemes that focus near waterlines overpredicted fines, while those that focus on the center underpredicted them. Variability of fines among pool tails was the highest within a broad band along the waterlines; hence, focusing sampling there yielded the most variable results. The scheme sampling at 25, 50, and 75% of the wetted width had the lowest precision and moderate accuracy. Accuracy and precision of grid-count results can be greatly improved by sampling at seven even-spaced locations across the pool tail.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own.]

Sediment Transport

Wednesday, May 11th, 2011

August 2011 article (Early View): “Impacts of Land-Cover Change on Suspended Sediment Transport in Two Agricultural Watersheds,” by Keith E. Schilling, Thomas M. Isenhart, Jason A. Palmer, Calvin F. Wolter, and Jean Spooner

Paired watershed studies are considered the gold standard for research. Daily discharge and suspended sediment export from two 5,000-ha watersheds in central Iowa were monitored over a 10-year period. In Walnut Creek watershed, a large portion of land was converted from row crop to native prairie, whereas in Squaw Creek land use remained predominantly row crop agriculture. Although modeling suggested differently, suspended sediment loads were similar in both watersheds. Stream mapping indicated that Walnut Creek had three times more eroding streambank lengths than did Squaw Creek suggesting that streambank erosion dominated sediment sources in Walnut Creek and sheet and rill sources dominated sediment sources in Squaw Creek. The results demonstrate that an accounting of all sources of sediment erosion and delivery is needed to characterize sediment reductions in watershed projects combined with long-term, intensive monitoring and modeling to account for possible lag times in the manifestation of the benefits of conservation practices on water quality

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]

Sediment budget

Thursday, November 18th, 2010

December 2010 article:Sediment Source Assessment in a Lowland Watershed Using Nitrogen Stable Isotopes,” by James F. Fox, Charles M. Davis, and Darren K. Martin.

This study provides the first attempt to assess the sediment budget in a lowland watershed using Nitrogen-15  tracer analysis. Sediment sources and transported sediments were sampled in a lowland watershed with pronounced fine sediment storage in the streambed. Sediments were analyzed for carbon and nitrogen content and stable nitrogen isotopic composition. Analysis of the data shows that temporarily stored streambed sediments dominate the sediment load during moderate- and low-flow hydrologic events.

Graph from paper

During very high-flow hydrologic events, however, deposition is pronounced in the streambed and sediment is replenished to the bed. Nitrogen model results show that elemental and isotopic nitrogen of streambed sediments vary substantially over the simulation period. In this manner, the streambed in a lowland watershed functions as a temporary storage zone that, in turn, can impact the nitrogen elemental and isotopic signature of sediments. The variation could significantly impact estimates of sediment provenance using nitrogen tracer-based methods.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]

Testing Stream Restoration

Friday, August 20th, 2010

October 2010 Article: Design of Experimental Streams for Simulating Headwater Stream Restoration, by Jung-Chen Huang, William J. Mitsch, Andrew D. Ward.

Map of research facility

Stream restoration is a billion dollar industry in the U.S. — and a very controversial topic. JAWRA has published a number of articles on this topic in the past several years, and almost all have generated spirited discussions and replies. One problem is the uniqueness of each restoration project: a park agency restoring a stream, for example, is not inclined to build several different versions just to test the theories. At the Olentangy River Wetland Research Park, Columbus, Ohio, however, researchers are doing exactly that.

This study designs three experimental channels – two-stage, self-design, and straightened channels – on a human-created swale for long-term evaluation of headwater stream evolution after restoration. The swale receives a continuous flow of pumped river water from upstream wetlands. These stream channels, after construction, will be monitored to evaluate physical, chemical, and biological responses to different channels over a decade-long experiment.

This article is the first of what likely will be a series of journal articles over the years describing the progress of the restoration project. It looks at the characteristics of the facility and how the experimental channels are hypothesized to evolve.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]

Sometimes you find … nothing

Friday, June 11th, 2010

June 2010 Article: Hydrologic and Morphologic Variability of Streams With Different Cranberry Agriculture Histories, Southern New Jersey, United States, by Nicholas A. Procopio.

To facilitate the cultivation and harvest of cranberries, large reservoirs are created upstream of bogs by impounding stream segments. The reservoirs accommodate the large amount of water needed for seasonal harvests, either in late summer or autumn, for winter and spring flooding to prevent against frost, and for irrigation and pest control. Ahah! Sounds like those goofy guys in the TV cranberry advertisements must be doing some big-time environmental damage.

Nicholas A. Procopio looked at this situation in New Jersey by comparing the flow regimes of basins with upstream active-cranberry bogs, upstream abandoned-cranberry bogs, and basins with no apparent agricultural history. His surprising conclusion: It appears that neither historic nor current cranberry agricultural practices considerably influence flow regimes or the channel morphology of streams in the New Jersey Pinelands. It is possible that the magnitude and timing of current diversions and water releases may not be great enough or frequent enough to cause significant alterations of the flow regimes or channel dimensions from condi- tions associated with forested streams.

This article is one of those unusual cases of an interesting negative result. It’s also a reminder that, while intuition has its proper role, we must always keep an open mind and let the facts guide our reasoning.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]

Ecologically Functional Floodplains

Tuesday, April 13th, 2010

April 2010 Article: “Ecologically Functional Floodplains: Connectivity, Flow Regime, and Scale,” by Jeffrey J. Opperman, Ryan Luster, Bruce A. McKenney, Michael Roberts, and Amanda Wrona Meadows.

Recent stream restoration efforts seem to place a lot of emphasis on designing to a single characteristic such as bankfull flow. The ideas in this article offer a more complex, nuanced view which looks at the flood regime in its totality.

The authors propose a conceptual model encompassing three basic elements: (1) hydrologic connectivity between the river and the floodplain, (2) a variable hydrograph that reflects seasonal precipitation patterns and retains a range of both high and low flow events, and (3) sufficient spatial scale to encompass dynamic processes and for floodplain benefits to accrue to a meaningful level.

For streamflow, the authors consider three kinds of representative floods. The “floodplain activation flood” is a small-magnitude flood that occurs relatively frequently and supports many of the processes ascribed to overbank flow pulses. The “floodplain maintenance flood” is a higher magnitude flood capable of performing geomorphic work including bank erosion and deposition on the floodplain that creates and maintains floodplain surfaces and contributes to heterogeneous floodplain topography. The third kind, “floodplain activation floods,” are rare, high-magnitude events that result in extensive geomorphic changes.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]

Protecting River Corridors

Monday, March 22nd, 2010

In their April 2010 JAWRA article, “Protecting River Corridors in Vermont,” Michael Kline and Barry Cahoon describe river corridor planning in Vermont, whereby corridors are sized based on the meander belt width and assigned a sensitivity rating based on the likelihood of channel adjustment due to stressors. The approach is fundamentally based on restoring fluvial processes associated with dynamic equilibrium, and associated habitat features.

The authors freely concede Vermont has large geomorphic datasets based on rigorous assessment protocols — Vermont is, after all, a small state — but the techniques seem to have great value nationwide.  The article gives examples of how “active” restoration projects to confine a river to a fixed channel have consumed program budgets and required continued investments to correct failures. So Vermont switched to a restoration program that embraces the concepts and practices associated with dynamic and deformable rivers. Thus river corridors are delineated based upon existing and estimated meander belt width. The purpose of a river corridor easement is to give the river the space to re-establish a natural slope, meander pattern, and floodplain connection.

The authors note a passive approach may often be a desirable alternative due to its lower upfront costs and maintenance, but like active restoration, it is highly dependent upon reducing watershed stressors, and landowner willingness to accept changes in land use.

[Please note: I have quoted and paraphrased freely from the article, but the interpretation is my own!]