scholarly journals Dynamic Hyporheic Zones: Exploring the Role of Peak Flow Events on Bedform‐Induced Hyporheic Exchange

2019 ◽  
Vol 55 (1) ◽  
pp. 218-235 ◽  
Author(s):  
Tanu Singh ◽  
Liwen Wu ◽  
Jesus D. Gomez‐Velez ◽  
Jörg Lewandowski ◽  
David M. Hannah ◽  
...  
Keyword(s):  
Peak Flow ◽  
Hyporheic Exchange ◽  
Hyporheic Zones

scholarly journals Hillslope Contribution to the Clark Instantaneous Unit Hydrograph: Application to the Seolmacheon Basin, Korea

Water ◽  
2021 ◽  
Vol 13 (12) ◽  
pp. 1707
Author(s):  
Chulsang Yoo ◽  
Huy Phuong Doan ◽  
Changhyun Jun ◽  
Wooyoung Na
Keyword(s):  
Peak Flow ◽  
Peak Time ◽  
Rainfall Runoff ◽  
Maximum Rainfall ◽  
Rainfall Events ◽  
Storage Coefficient ◽  
Channel Velocity ◽  
Linear Reservoir ◽  
Mountainous Basin

In this study, the time–area curve of an ellipse is analytically derived by considering flow velocities within both channel and hillslope. The Clark IUH is also derived analytically by solving the continuity equation with the input of the derived time–area curve to the linear reservoir. The derived Clark IUH is then evaluated by application to the Seolmacheon basin, a small mountainous basin in Korea. The findings in this study are summarized as follows. (1) The time–area curve of a basin can more realistically be derived by considering both the channel and hillslope velocities. The role of the hillslope velocity can also be easily confirmed by analyzing the derived time–area curve. (2) The analytically derived Clark IUH shows the relative roles of the hillslope velocity and the storage coefficient. Under the condition that the channel velocity remains unchanged, the hillslope velocity controls the runoff peak flow and the concentration time. On the other hand, the effect of the storage coefficient can be found in the runoff peak flow and peak time, as well as in the falling limb of the runoff hydrograph. These findings are also confirmed in the analysis of rainfall–runoff events of the Seolmacheon basin. (3) The effect of the hillslope velocity varies considerably depending on the rainfall events, which is also found to be mostly dependent upon the maximum rainfall intensity.

Effects of riffle–step restoration on hyporheic zone chemistry in N-rich lowland streams

2006 ◽  
Vol 63 (1) ◽  
pp. 120-133 ◽  
Author(s):  
Tamao Kasahara ◽  
Alan R Hill
Keyword(s):  
Urban Areas ◽  
Hyporheic Zone ◽  
Stream Water ◽  
Ion Concentration ◽  
Hyporheic Exchange ◽  
Ecosystem Functions ◽  
Exchange Flow ◽  
Nutrient Inputs ◽  
Lowland Streams ◽  
Hyporheic Zones

Stream restoration projects that aim to rehabilitate ecosystem health have not considered surface–subsurface linkages, although stream water and groundwater interaction has an important role in sustaining stream ecosystem functions. The present study examined the effect of constructed riffles and a step on hyporheic exchange flow and chemistry in restored reaches of several N-rich agricultural and urban streams in southern Ontario. Hydrometric data collected from a network of piezometers and conservative tracer releases indicated that the constructed riffles and steps were effective in inducing hyporheic exchange. However, despite the use of cobbles and boulders in the riffle construction, high stream dissolved oxygen (DO) concentrations were depleted rapidly with depth into the hyporheic zones. Differences between observed and predicted nitrate concentrations based on conservative ion concentration patterns indicated that these hyporheic zones were also nitrate sinks. Zones of low hydraulic conductivity and the occurrence of interstitial fines in the restored cobble-boulder layers suggest that siltation and clogging of the streambed may reduce the downwelling of oxygen- and nitrate-rich stream water. Increases in streambed DO levels and enhancement of habitat for hyporheic fauna that result from riffle–step construction projects may only be temporary in streams that receive increased sediment and nutrient inputs from urban areas and croplands.

scholarly journals Effects of Successive Peak Flow Events on Hyporheic Exchange and Residence Times

2020 ◽  
Vol 56 (8) ◽  
Author(s):  
Tanu Singh ◽  
Jesus D. Gomez‐Velez ◽  
Liwen Wu ◽  
Anders Wörman ◽  
David M. Hannah ◽  
...  
Keyword(s):  
Peak Flow ◽  
Hyporheic Exchange ◽  
Residence Times

The role of unilateral nasal inspiratory peak flow in nasal obstruction—A study of 70 patients undergoing septorhinoplasty surgery

2019 ◽  
Vol 44 (3) ◽  
pp. 427-430
Author(s):  
Anika Kaura ◽  
Jagdeep S. Virk ◽  
Jonathan Joseph ◽  
Catherine Rennie ◽  
Prem Singh Randhawa ◽  
...  
Keyword(s):  
Nasal Obstruction ◽  
Peak Flow ◽  
Nasal Inspiratory Peak Flow

scholarly journals Role of Asthma Education in the Management of Adult Asthma

1995 ◽  
Vol 2 (suppl a) ◽  
pp. 38A-42A
Author(s):  
Johanne Côté
Keyword(s):  
Environmental Factors ◽  
Airway Inflammation ◽  
Symptom Severity ◽  
Peak Flow ◽  
Action Plan ◽  
Asthma Treatment ◽  
Newly Diagnosed ◽  
Inhalation Device ◽  
Asthma Attack

When a patient is newly diagnosed as having asthma, he or she is often prescribed new medication without getting much information on the disease and its treatment. This article emphasizes the need to educate asthmatics. Asthma treatment should begin with a proper adjustment of the medication, allowing asthmatics to lead a normal life. All asthmatics should be shown how to use their inhalation device properly. They should he knowledgeable about the basic aspects of asthma, airway inflammation and bronchoconstriction, use or medication and early symptoms heralding an asthma attack. Environmental factors that may trigger an asthma attack should be explained. Patients should be able to self-monitor asthma using either symptom severity or a peak flow meter. Because asthma is an unpredictable disease, patients should have a self-action plan to implement when their asthma deteriorates.

The role of thermal contraction crack polygons in cold-desert fluvial systems

2008 ◽  
Vol 20 (6) ◽  
pp. 565-579 ◽  
Author(s):  
Joseph S. Levy ◽  
James W. Head ◽  
David R. Marchant
Keyword(s):  
Thermal Contraction ◽  
Patterned Ground ◽  
Sediment Grain Size ◽  
Cold Desert ◽  
Fluvial Systems ◽  
Hyporheic Zones ◽  
Continuous Presence ◽  
And Storage ◽  
Composite Wedge

AbstractThermal contraction crack polygons modify the generation, transport, and storage of water in Wright Valley gullies. Water generation is contributed to by trapping of windblown snow in polygon troughs. Water transport is modified by changes to the ice-cement table and active layer topography caused by polygon trough formation. Water storage is modified by sediment grain-size distribution within polygons in gully distal hyporheic zones. Patterned ground morphological variation can serve as an indicator of fluvial modification, ranging from nearly unmodified composite-wedge polygons to polygons forming in association with gully channels. Thermal contraction crack polygons may also constrain the gully formation sequence, suggesting the continuous presence of permafrost beneath the Wright Valley gullies during the entire period of gully emplacement. This analysis provides a framework for understanding the relationships between polygons and gullies observed on Mars. If comparable stratigraphic relationships can be documented, the presence of an analogous impermeable ice-cemented layer beneath the gullies can be inferred, suggesting an atmospheric source for Martian gully-carving fluids.

scholarly journals Hyporheic hydraulic geometry: Conceptualizing relationships among hyporheic exchange, storage, and water age

PLoS ONE ◽  
2022 ◽  
Vol 17 (1) ◽  
pp. e0262080
Author(s):  
Geoffrey C. Poole ◽  
S. Kathleen Fogg ◽  
Scott J. O’Daniel ◽  
Byron E. Amerson ◽  
Ann Marie Reinhold ◽  
...  
Keyword(s):  
Hyporheic Zone ◽  
Quantitative Description ◽  
Hyporheic Exchange ◽  
Water Volume ◽  
Mathematical Framework ◽  
Hydraulic Geometry ◽  
Water Age ◽  
Mathematical Basis ◽  
Hyporheic Zones ◽  
Improved Accuracy

Hyporheic exchange is now widely acknowledged as a key driver of ecosystem processes in many streams. Yet stream ecologists have been slow to adopt nuanced hydrologic frameworks developed and applied by engineers and hydrologists to describe the relationship between water storage, water age, and water balance in finite hydrosystems such as hyporheic zones. Here, in the context of hyporheic hydrology, we summarize a well-established mathematical framework useful for describing hyporheic hydrology, while also applying the framework heuristically to visualize the relationships between water age, rates of hyporheic exchange, and water volume within hyporheic zones. Building on this heuristic application, we discuss how improved accuracy in the conceptualization of hyporheic exchange can yield a deeper understanding of the role of the hyporheic zone in stream ecosystems. Although the equations presented here have been well-described for decades, our aim is to make the mathematical basis as accessible as possible and to encourage broader understanding among aquatic ecologists of the implications of tailed age distributions commonly observed in water discharged from and stored within hyporheic zones. Our quantitative description of “hyporheic hydraulic geometry,” associated visualizations, and discussion offer a nuanced and realistic understanding of hyporheic hydrology to aid in considering hyporheic exchange in the context of river and stream ecosystem science and management.

Effect of sediment-organism interactions on hyporheic exchange in streams: role of sediment reworking time

2021 ◽  
Author(s):  
Shivansh Shrivastava ◽  
Michael Stewardson ◽  
Meenakshi Arora
Keyword(s):  
Flow Regime ◽  
Experimental Work ◽  
Laboratory Experiments ◽  
Hyporheic Exchange ◽  
Residence Times ◽  
Sediment Reworking ◽  
Hyporheic Flow ◽  
Mean Residence Times ◽  
Organism Interactions

<p>In-stream faunal organisms constantly interact with their habitat to modify its physical and hydraulic properties. However, little is known about how sediment-organism interactions could modify the hyporheic exchange. Previous experimental work investigating the effects of the activities of faunal organisms on exchange across the sediment-water interface has been largely conducted in small mesocosms or infiltration columns that do not represent the lotic environment adequately. Therefore, the experimental findings from these studies may not be transferable to flowing water environments (e.g., streams). Our previous experimental work demonstrated that sediment reworking by macroinvertebrates could significantly alter the hyporheic flux, mean residence times, and depth of exchange in streambeds. In this work, we explore how sediment-organism contact time influence the effect of the activities of model organisms, Lumbriculus variegatus, on the hyporheic flow regime. We conduct laboratory experiments in re-circulating flumes subject to different sediment reworking times (5 and 10 days). The hyporheic flow characteristics in these flumes were studied by conducting dye tracer tests after the bed sediments were reworked. Deposition of fecal pellets and holes/burrows dug by sample organisms were visible at the bed surface in both the experimental flumes. The flume reworked for a longer time exhibited higher hyporheic flux, longer median/mean residence times, and deeper depth of solute penetration compared to the flume reworked for a shorter period. The modification of hyporheic flow regime to different degrees depending on the sediment reworking times has direct relevance to the biogeochemistry in hyporheic zones, and thus on the overall quality of surface and sub-surface waters. We advocate that more intensive laboratory experiments and field investigations must be conducted to support the findings from our study and advance our understanding of the role of the activities of faunal organisms on fluvial ecosystem functioning.</p>

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