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Journal articles on the topic 'Eco-hydraulics'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Wang, Zhaoyin, Joseph H. W. Lee, and Mengzhen Xu. "Eco-hydraulics and eco-sedimentation studies in China." Journal of Hydraulic Research 51, no. 1 (2013): 19–32. http://dx.doi.org/10.1080/00221686.2012.753554.

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2

Nikora, V. I., D. G. Goring, and B. J. F. Biggs. "Silverstream eco‐hydraulics flume: Hydraulic design and tests." New Zealand Journal of Marine and Freshwater Research 32, no. 4 (1998): 607–20. http://dx.doi.org/10.1080/00288330.1998.9516848.

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3

Termini, Donatella. "Fluvial eco-hydraulics and morphodynamics: New insights and challenges." Advances in Water Resources 81 (July 2015): 1–3. http://dx.doi.org/10.1016/j.advwatres.2015.04.003.

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4

Ramos, Helena M., Armando Carravetta, Aonghus Mc Nabola, and Kemi Adeyeye. "Environmental Hydraulics Research." Water 12, no. 10 (2020): 2749. http://dx.doi.org/10.3390/w12102749.

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Environmental hydraulics research includes the different domains of hydrodynamics, such as the investigation and implementation of the physical and experimental applications, and research into the quantity, quality, modelling and simulation of the attributes associated with flowing water. This topic is studied both from a technical and environmental point of view, with the objective of protecting and enhancing the quality of the environment. It is a cross-disciplinary field of study which comprises open channel/river flows and pressurised systems, combining, among others, new technological, so

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5

Noss, Christian, Pascal Bodmer, Kaan Koca, and Andreas Lorke. "Flow and Turbulence driven Water Surface Roughness and Gas Exchange Velocity in Streams." E3S Web of Conferences 40 (2018): 05018. http://dx.doi.org/10.1051/e3sconf/20184005018.

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Gas exchange velocity in streams and rivers controls fluxes of atmospheric gases across the air-water interface and is commonly related to the turbulence at the water side. Similarly, river flow hydraulics influences the water surface roughness, which is frequently used (in terms of surface flow types) for eco- and morphological mapping of spatial variations of hydraulic conditions. We investigated the relationships between gas exchange velocity, water surface roughness and flow hydraulics for different surface flow types in a low-mountain stream. We used the flux chamber-method to estimate ex

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6

Yin, Hai-long, Zu-xin Xu, Yi-jun Yao, and Shen-fa Huang. "Eco-Hydraulics Techniques for Controlling Eutrophication of Small Scenery Lakes—A Case Study of Ludao Lake in Shanghai." Journal of Hydrodynamics 19, no. 6 (2007): 776–83. http://dx.doi.org/10.1016/s1001-6058(08)60017-7.

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7

Clifford, Nicholas J., Oliver P. Harmar, Gemma Harvey, and Geoffrey E. Petts. "Physical habitat, eco-hydraulics and river design: a review and re-evaluation of some popular concepts and methods." Aquatic Conservation: Marine and Freshwater Ecosystems 16, no. 4 (2006): 389–408. http://dx.doi.org/10.1002/aqc.736.

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8

Kalmbach, Lothar, and Ykä Helariutta. "Sieve Plate Pores in the Phloem and the Unknowns of Their Formation." Plants 8, no. 2 (2019): 25. http://dx.doi.org/10.3390/plants8020025.

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Sieve pores of the sieve plates connect neighboring sieve elements to form the conducting sieve tubes of the phloem. Sieve pores are critical for phloem function. From the 1950s onwards, when electron microscopes became increasingly available, the study of their formation had been a pillar of phloem research. More recent work on sieve elements instead has largely focused on sieve tube hydraulics, phylogeny, and eco-physiology. Additionally, advanced molecular and genetic tools available for the model species Arabidopsis thaliana helped decipher several key regulatory mechanisms of early phloem

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9

St-Hilaire, André. "Book Review by André St-Hilaire,Environmental Hydrology and Hydraulics: Eco-technological Practices for Sustainable Development.Science Publishers. Enfield, NH." Canadian Water Resources Journal 33, no. 1 (2008): 95–96. http://dx.doi.org/10.4296/cwrj3301095.

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10

Guse, Björn, Jochem Kail, Johannes Radinger, et al. "Eco-hydrologic model cascades: Simulating land use and climate change impacts on hydrology, hydraulics and habitats for fish and macroinvertebrates." Science of The Total Environment 533 (November 2015): 542–56. http://dx.doi.org/10.1016/j.scitotenv.2015.05.078.

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11

Wang, Wei-Jie, Wen-Qi Peng, Wen-Xin Huai, et al. "Derivation of Canopy Resistance in Turbulent Flow from First-Order Closure Models." Water 10, no. 12 (2018): 1782. http://dx.doi.org/10.3390/w10121782.

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Quantification of roughness effects on free surface flows is unquestionably necessary when describing water and material transport within ecosystems. The conventional hydrodynamic resistance formula empirically shows that the Darcy–Weisbach friction factor f~(r/hw)1/3 describes the energy loss of flowing water caused by small-scale roughness elements characterized by size r (<<hw), where hw is the water depth. When the roughness obstacle size becomes large (but <hw) as may be encountered in flow within canopies covering wetlands or river ecosystem, the f becomes far more complicated.

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12

Novak, Gorazd, José M. Domínguez, Angelo Tafuni, et al. "3-D Numerical Study of a Bottom Ramp Fish Passage Using Smoothed Particle Hydrodynamics." Water 13, no. 11 (2021): 1595. http://dx.doi.org/10.3390/w13111595.

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Worldwide, the overwhelming number of man-made barriers in fluvial systems has been identified as one of the major causes of the reported staggering average declines of migratory fish. Fish passages have been shown to help mitigate such problems. Close-to-nature types of fish passages, such as bottom ramps, bypass channels, and fish ramps can be used to minimize the impact of artificial steep drops (e.g., weirs) on the migration of aquatic fauna, especially in cases of low-head barriers. This study focuses on the characterization of the flow pattern in a bottom ramp. A 3-D numerical model base

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13

Santini, Nadia S., James Cleverly, Rolf Faux, Katie McBean, Rachael Nolan, and Derek Eamus. "Root xylem characteristics and hydraulic strategies of species co-occurring in semi-arid Australia." IAWA Journal 39, no. 1 (2018): 43–62. http://dx.doi.org/10.1163/22941932-20170188.

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Xylem traits such as xylem vessel size can influence the efficiency and safety of water transport and thus plant growth and survival. Root xylem traits are much less frequently examined than those of branches despite such studies being critical to our understanding of plant hydraulics. In this study, we investigated primary lateral and sinker roots of six co-occurring species of semi-arid Australia. Two species are restricted to a floodplain, two were sampled only from the adjacent sand plain, and two species co-occur in both habitats. We assessed root wood density, xylem traits (i.e., vessel

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14

Blanckaert, Koen, Xavier-François Garcia, Johannes Steiger, and Wim Uijttewaal. "Ecohydraulics: linkages between hydraulics, morphodynamics and ecological processes in rivers." Ecohydrology 6, no. 4 (2013): 507–10. http://dx.doi.org/10.1002/eco.1414.

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15

Mallen-Cooper, Martin, and Brenton P. Zampatti. "History, hydrology and hydraulics: Rethinking the ecological management of large rivers." Ecohydrology 11, no. 5 (2018): e1965. http://dx.doi.org/10.1002/eco.1965.

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16

Stout, T. L., M. Majerova, and B. T. Neilson. "Impacts of beaver dams on channel hydraulics and substrate characteristics in a mountain stream." Ecohydrology 10, no. 1 (2016): e1767. http://dx.doi.org/10.1002/eco.1767.

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17

Karamma, Riswal, Rita Tahir Lopa, and Mukhsan Putra Hatta. "The Revitalization of Makassar Urban Drainage System Based on Eco Drainage Retention Pond." INTEK: Jurnal Penelitian 8, no. 1 (2021): 47. http://dx.doi.org/10.31963/intek.v8i1.2811.

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One of the causes of flooding in Makassar City is the management of the water system that is not optimal. It is necessary to arrange a drainage system to overcome flooding in Makassar City. In this study the topography on Catchment area analysis, analysis of hydrology and hydraulics analysis. Modeling the distribution of flood performed using HEC-RAS applications. This research was conducted in the Tallo watershed which consists of the Upper Tallo sub-watershed and the Mangalarang sub-watershed. The results of the analysis of flood discharge in the Tallo Hilir sub-watershed are 523.76 m3/s and

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18

"Environmental hydrology and hydraulics: eco-technological practices for sustainable development." Choice Reviews Online 44, no. 03 (2006): 44–1541. http://dx.doi.org/10.5860/choice.44-1541.

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