Relevant bibliographies by topics / Estuarine mixing

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Estuarine mixing'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Estuarine mixing"

1

Burchard, Hans. "A Universal Law of Estuarine Mixing." Journal of Physical Oceanography 50, no. 1 (2020): 81–93. http://dx.doi.org/10.1175/jpo-d-19-0014.1.

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AbstractA universal law of estuarine mixing is derived here, combining the approaches of salinity coordinates, Knudsen relations, total exchange flow, mixing definition as salinity variance loss, and the mixing–exchange flow relation. As a result, the long-term average mixing within an estuarine volume bounded by the isohaline of salinity S amounts to M(S) = S2Qr, where Qr is the average river runoff into the estuary. Consequently, the mixing per salinity class is m(S) = ∂SM(S) = 2SQr, which can also be expressed as the product of the isohaline volume and the mixing averaged over the isohaline
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Hetland, Robert D., and W. Rockwell Geyer. "An Idealized Study of the Structure of Long, Partially Mixed Estuaries*." Journal of Physical Oceanography 34, no. 12 (2004): 2677–91. http://dx.doi.org/10.1175/jpo2646.1.

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Abstract Classic models of estuarine circulation are reexamined using a three-dimensional, primitive equation numerical ocean model. The model is configured using an idealized estuary/shelf domain with rectangular cross section, constant vertical mixing, and steady riverine discharge. Tidal dispersion is neglected, so the analysis does apply to well-mixed estuaries and lagoons. Estuarine scales for the length of steady-state salt intrusion, vertical stratification, and estuarine exchange flow estimated from steady-state model results are found to have the same functional relationships to verti
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Shin, Hyun-Jung, Guan-hong Lee, KiRyong Kang, and Kyeong Park. "Shift of estuarine type in altered estuaries." Anthropocene Coasts 2, no. 1 (2019): 145–70. http://dx.doi.org/10.1139/anc-2018-0013.

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To better understand the alteration of the estuarine circulation caused by estuarine dams, four major Korean estuaries were classified by using the Hansen and Rattray stratification–circulation classification scheme. The stratification and circulation parameters were calculated for both discharge and no-discharge periods from the tidally averaged salinity and velocity data obtained from these four Korean estuaries. The estuarine types of the altered Korean estuaries were compared with the previous results for natural estuaries in other countries of similar magnitude in tidal range, water depth
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Antoranz, Ana M., J. L. Pelegrí, and P. Masciangioli. "Tidal currents and mixing in the Lake Maracaibo estuarine system." Scientia Marina 65, S1 (2001): 155–66. http://dx.doi.org/10.3989/scimar.2001.65s1155.

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Burchard, Hans, Xaver Lange, Knut Klingbeil, and Parker MacCready. "Mixing Estimates for Estuaries." Journal of Physical Oceanography 49, no. 2 (2019): 631–48. http://dx.doi.org/10.1175/jpo-d-18-0147.1.

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AbstractThe well-known Knudsen relations and the total exchange flow (TEF) analysis framework provide quantifications of exchange flow across an open boundary to the adjacent ocean in terms of bulk values (Knudsen theory: inflow and outflow volume or salinity) or with resolution in salinity space (TEF: profiles of volume and salt flux in salinity coordinates). In the present study, these theories are extended toward mixing of salinity, defined as the decay of salinity variance due to turbulent mixing. In addition to the advective fluxes, diffusive fluxes across the boundary are also considered
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MacCready, Parker. "Estuarine Adjustment." Journal of Physical Oceanography 37, no. 8 (2007): 2133–45. http://dx.doi.org/10.1175/jpo3082.1.

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Abstract Subtidal adjustment of estuarine salinity and circulation to changing river flow or tidal mixing is explored using a simplified numerical model. The model employs tidally averaged, width-averaged physics, following Hansen and Rattray, extended to include 1) time dependence, 2) tidally averaged mixing parameterizations, and 3) arbitrary variation of channel depth and width. By linearizing the volume-integrated salt budget, the time-dependent system may be distilled to a first-order, forced, damped, ordinary differential equation. From this equation, analytical expressions for the adjus
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Osadchiev, Alexander, Igor Medvedev, Sergey Shchuka, et al. "Influence of estuarine tidal mixing on structure and spatial scales of large river plumes." Ocean Science 16, no. 4 (2020): 781–98. http://dx.doi.org/10.5194/os-16-781-2020.

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Abstract. The Yenisei and Khatanga rivers are among the largest estuarine rivers that inflow to the Arctic Ocean. Discharge of the Yenisei River is 1 order of magnitude larger than that of the Khatanga River. However, spatial scales of buoyant plumes formed by freshwater runoff from the Yenisei and Khatanga gulfs are similar. This feature is caused by different tidal forcing in these estuaries, which have similar sizes, climate conditions, and geomorphology. The Khatanga discharge experiences strong tidal forcing that causes formation of a diluted bottom-advected plume in the Khatanga Gulf. Th
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Lorenz, Marvin, Knut Klingbeil, and Hans Burchard. "Impact of Evaporation and Precipitation on Estuarine Mixing." Journal of Physical Oceanography 51, no. 4 (2021): 1319–33. http://dx.doi.org/10.1175/jpo-d-20-0158.1.

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AbstractRecent studies could link the quantities of estuarine exchange flows to the volume-integrated mixing inside an estuary, where mixing is defined as the destruction of salinity variance. The existing mixing relations quantify mixing inside an estuary by the net boundary fluxes of volume, salinity, and salinity variance, which are quantified as Knudsen or total exchange flow bulk values. So far, river runoff is the only freshwater flux included, and the freshwater exchange due to precipitation and evaporation is neglected. Yet, the latter is the driving force of inverse estuaries, which c
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Hetland, Robert D. "Estuarine Overmixing." Journal of Physical Oceanography 40, no. 1 (2010): 199–211. http://dx.doi.org/10.1175/2009jpo4247.1.

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Abstract H. Stommel and H. G. Farmer derived a theory for the maximal exchange between an estuary and the adjacent shelf sea based on a combination of mass and salt conservation (also known as Knudsen’s relation) and hydraulic control theory at the estuary mouth. This upper limit of exchange flow is termed overmixing, because there is more than enough mixing in the estuary to maintain the density difference and exchange flow at the mouth. This seminal work inspired a number of papers on hydraulic control of baroclinic flow through constrictions. However, none of these papers returned to the id
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Lange, Xaver, and Hans Burchard. "The Relative Importance of Wind Straining and Gravitational Forcing in Driving Exchange Flows in Tidally Energetic Estuaries." Journal of Physical Oceanography 49, no. 3 (2019): 723–36. http://dx.doi.org/10.1175/jpo-d-18-0014.1.

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AbstractIn straight tidal estuaries, residual overturning circulation results mainly from a competition between gravitational forcing, wind forcing, and friction. To systematically investigate this for tidally energetic estuaries, the dynamics of estuarine cross sections is analyzed in terms of the relation between gravitational forcing, wind stress, and the strength of estuarine circulation. A system-dependent basic Wedderburn number is defined as the ratio between wind forcing and opposing gravitational forcing at which the estuarine circulation changes sign. An analytical steady-state solut
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Dissertations / Theses on the topic "Estuarine mixing"

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Sheridan, Megan. "Mixing and dispersion of a small estuarine plume." Thesis, University of Plymouth, 2018. http://hdl.handle.net/10026.1/12817.

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Entrainment velocity, salt flux and the turbulent diffusivity of salt are estimated in the outflow of a small, radially spreading buoyant outflow, just outside of the Teign Estuary mouth, as a means to compare mixing dynamics between very small and larger-scale estuarine and river plumes, and build on a scant knowledge base regarding the former. The analysis was made using a control volume approach, based on the conservation of momentum, volume and salt, from a Lagrangian perspective. Drifting buoys were used to accomplish this. The analysis was based on that employed by McCabe et al. (2008),
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Fang, Tien-Hsi. "Studies of the behaviour of trace metals during mixing in some estuaries of the Solent region." Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262240.

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Williams, Mark Steven. "Radionuclides as tracers of sediment mixing in natural and enclosed estuaries." Thesis, University of Plymouth, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.247510.

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Cudaback, Cynthia Nova. "The effect of vertical mixing on along channel transport in a layered flow /." Thesis, Connect to this title online; UW restricted, 1998. http://hdl.handle.net/1773/6821.

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Hudson, Andrew Neil. "The kinetics and mechanisms of destabilisation and aggregation of microcolloidal iron and associated phosphate during simulated estuarine mixing." Thesis, University of Southampton, 1999. https://eprints.soton.ac.uk/42096/.

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The removal of iron from the <0.45m fraction of Tamar River water on addition of both calcium chloride solution and sea water was studied using a continuous autoanalytical system. The addition of increasing concentrations of either calcium ions or sea water caused increased iron removal, but at all of the concentrations studied a fraction of iron was found to remain within the <0.45jim fraction (termed the residual or unreactive fraction). Storage time was shown to have a marked effect on the residual concentration. Kinetic analysis of the experimental results showed that when a residual fract
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Elston, Susan Anne. "Secondary Circulation in a Sinuous Coastal Plain Estuary." Diss., Available online, Georgia Institute of Technology, 2005, 2005. http://etd.gatech.edu/theses/available/etd-05042005-143327/.

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Thesis (Ph. D.)--Earth and Atmospheric Sciences, Georgia Institute of Technology, 2005.<br>Dr. Curry, Judith, Committee Co-Chair ; Dr. Blanton, Jackson - Committee Chair, Committee Chair ; Dr. Cunnold, Derek, Committee Member ; Dr. Seim, Harvey, Committee Member ; Dr. Webster, Donald, Committee Member ; Dr. Webster, Peter, Committee Member ; Dr. Wong, Kuo, Committee Member.
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Ahad, Jason Michael Elias. "Evaluating the origins and transformations of organic matter and dissolved inorganic nitrogen in two contrasting North Sea estuaries." Thesis, University of Edinburgh, 2005. http://hdl.handle.net/1842/866.

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In order to delineate the potential sources and to understand the main controls on the biogeochemical cycling of dissolved and particulate organic matter (DOM, POM) and dissolved inorganic nitrogen (DIN) during estuarine mixing, comprehensive seasonal geochemical and isotopic and surveys across the freshwater-tidal interface were carried out in the Tyne and Tweed Estuaries, NE UK. This study provided a contrast between a relatively pristine system (Tweed) with one that is heavily influenced by anthropogenic activity (Tyne). Geochemical and isotopic (13C, 14C and 15N) analyses demonstrated the
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Whyte, Kenneth K. "Entrainment and mixing in rivers, estuaries and reservoirs." Thesis, University of Liverpool, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.400129.

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Ott, Michael William. "Mixing and secondary circulation in Juan de Fuca Strait." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ52768.pdf.

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Bárcena, Gómez Javier Francisco. "Desarrollo de una metodología para delimitar zonas de mezcla de vertidos industriales en estuarios. Development of a methodology to allocate mixing zones of industrial discharges in estuaries." Doctoral thesis, Universidad de Cantabria, 2015. http://hdl.handle.net/10803/329011.

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El objetivo del presente trabajo es proporcionar una metodología escalonada con un grupo de herramientas numéricas seleccionadas y/o desarrolladas con el fin de establecer dónde se requiere una zona de mezcla y determinar su tamaño y aceptabilidad con un nivel de detalle apropiado de acuerdo a su relevancia para cada vertido industrial descargado por boca única situado en un estuario. Esta propuesta puede ser aplicada tanto por los Estados miembros como las industrias a la hora de delimitar zonas de mezcla según lo establecido en la Directiva 2008/105/EC y la Directiva 2013/39/EU. La estructu
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Books on the topic "Estuarine mixing"

1

Prandle, David. Estuaries: Dynamics, mixing, sedimentation, and morphology. Cambridge University Press, 2009.

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Dispersion in estuaries and coastal waters. Wiley, 1997.

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Pattiaratchi, C., ed. Mixing in Estuaries and Coastal Seas. American Geophysical Union, 1996. http://dx.doi.org/10.1029/ce050.

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Langerak, A. Predictive ability of two-dimensional models for mixing in estuaries. Rand, 1987.

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Estuaries: Dynamics, Mixing, Sedimentation and Morphology. University of Cambridge ESOL Examinations, 2009.

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1957-, Pattiaratchi Charitha, and International Conference on Physics of Estuaries and Coastal Seas (6th : 1992 : Margaret River, Augusta-Margaret River Shire, W.A.), eds. Mixing in estuaries and coastal seas. American Geophysical Union, 1996.

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J, Van de Kreeke, Rosenstiel School of Marine and Atmospheric Science., Coastal Engineering Research Council, and Symposium Physics of Shallow Estuaries and Bays (1984 : Miami, Fla.), eds. Physics of shallow estuaries and bays. Springer-Verlag, 1986.

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Estuaries : dynamics, mixing, sedimentation and morphology - 1. edición. Cambridge University Press, 2011.

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Salt Intrusion Tides And Mixing In In Multichannel Estuaries. Taylor & Francis Group, 2008.

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Nguyen, Anh Duc. Salt Intrusion, Tides and Mixing in Multi-Channel Estuaries : PhD: UNESCO-IHE Institute, Delft. Taylor & Francis Group, 2008.

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Book chapters on the topic "Estuarine mixing"

1

Lung, Wu-Seng. "Estuarine Mixing Zone Analysis." In Water Quality Modeling. CRC Press, 2021. http://dx.doi.org/10.1201/9781003208969-8.

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Boudreau, Bernard P. "Modelling mixing and diagenesis." In Coastal and Estuarine Studies. American Geophysical Union, 2005. http://dx.doi.org/10.1029/ce060p0323.

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Bruner de Miranda, Luiz, Fernando Pinheiro Andutta, Björn Kjerfve, and Belmiro Mendes de Castro Filho. "Circulation and Mixing in Estuaries." In Fundamentals of Estuarine Physical Oceanography. Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-3041-3_2.

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Simpson, J. H., and P. B. Tett. "An Induced Mixing Experiment?" In Lecture Notes on Coastal and Estuarine Studies. Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4966-5_20.

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Simpson, J. H., and P. B. Tett. "An Induced Mixing Experiment?" In Lecture Notes on Coastal and Estuarine Studies. Springer-Verlag, 2013. http://dx.doi.org/10.1029/ln017p0483.

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Bruner de Miranda, Luiz, Fernando Pinheiro Andutta, Björn Kjerfve, and Belmiro Mendes de Castro Filho. "Mixing Processes in Estuaries: Simplifyed Methods." In Fundamentals of Estuarine Physical Oceanography. Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-3041-3_6.

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Wolanski, Erik, and Peter Ridd. "Mixing and trapping in Australian tropical coastal waters." In Coastal and Estuarine Studies. American Geophysical Union, 1990. http://dx.doi.org/10.1029/ce038p0165.

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Okamoto, I., S. Endoh, and M. Kumagai. "Distribution and mixing of the River Seri water." In Coastal and Estuarine Studies. American Geophysical Union, 1995. http://dx.doi.org/10.1029/ce048p0101.

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Sheng, Y. Peter. "Modeling Wind-Induced Mixing and Transport in Estuaries and Lakes." In Estuarine Water Quality Management. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75413-5_5.

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Demers, S., L. Legendre, and J. C. Therriault. "Phytoplankton Responses to Vertical Tidal Mixing." In Lecture Notes on Coastal and Estuarine Studies. Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4966-5_1.

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Conference papers on the topic "Estuarine mixing"

1

Arega, Feleke, and Brett F. Sanders. "Modeling Circulation and Mixing in Tidal Wetlands of the Santa Ana River." In Eighth International Conference on Estuarine and Coastal Modeling. American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40734(145)46.

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Blain, Cheryl Ann, and Jayaram Veeramony. "The Role of River Discharge and Vertical Mixing Formulation on Barotropic Circulation in Bay St. Louis, MS." In Seventh International Conference on Estuarine and Coastal Modeling. American Society of Civil Engineers, 2002. http://dx.doi.org/10.1061/40628(268)48.

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Gross, Edward S., Nicholas J. Nidzieko, Michael L. MacWilliams, and Mark T. Stacey. "Parameterization of Estuarine Mixing Processes in the San Francisco Estuary Based on Analysis of Three-Dimensional Hydrodynamic Simulations." In 10th International Conference on Estuarine and Coastal Modeling. American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40990(324)20.

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Maher, Ali, Vernon Schaefer, and David Yang. "In-Situ Deep Soil Mixing for Solidification of Soft Estuarine Sediments Shear Strength." In GeoCongress 2008. American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40970(309)84.

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Lips, Urmas, Inga Lips, Taavi Liblik, and Juri Elken. "Estuarine transport versus vertical movement and mixing of water masses in the Gulf of Finland (Baltic Sea)." In 2008 IEEE/OES US/EU-Baltic International Symposium (BALTIC). IEEE, 2008. http://dx.doi.org/10.1109/baltic.2008.4625535.

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Khoroshevskaya, Victoria. "CHANGES IN THE VANADIUM MIGRATION FORMS ON GEOCHEMICAL BARRIERS IN THE RIVER-SEA MIXING ZONES." In GEOLINKS Conference Proceedings. Saima Consult Ltd, 2021. http://dx.doi.org/10.32008/geolinks2021/b1/v3/47.

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The article is devoted to the study of vanadium, a metal capable of stimulating the growth of phytoplankton in situ and has the greatest biological activity in dissolved form. The pattern of an increase in the concentration of vanadium dissolved forms in the mixing zones during the transition from river waters to seawaters is known. In this article, we examine the behavior, ratio and change in the concentrations of vanadium dissolved and suspended forms during the passage of geochemical barriers. The estuarine zone of the Razdolnaya River–Amur Bay (Sea of Japan) is considered as "river-sea" mi
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Savenko, Alla, Alla Savenko, Oleg Pokrovsky, Oleg Pokrovsky, Irina Streletskaya, and Irina Streletskaya. "DISTRIBUTION OF DISSOLVED CHEMICAL ELEMENTS IN THE YENISEI RIVER ESTUARY AND ADJACENT WATER AREA OF THE KARA SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43172445b0.

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The distribution of dissolved chemical elements (major ions, nutrients, and trace elements) in the Yenisei River estuary and adjacent water area in 2009 and 2010 are presented. These results were compared to the data obtained during previous hydrochemical studies of this region. The transport of major cations (Na, K, Mg, Ca) and some trace elements (Rb, Cs, Sr, B, F, As, Mo, U) in the estuary follows conservative mixing. Alkalinity also belongs to conservative components, however this parameter exhibits substantial spatial heterogeneity caused by complex hydrological structure of the Yenisei B
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Savenko, Alla, Alla Savenko, Oleg Pokrovsky, Oleg Pokrovsky, Irina Streletskaya, and Irina Streletskaya. "DISTRIBUTION OF DISSOLVED CHEMICAL ELEMENTS IN THE YENISEI RIVER ESTUARY AND ADJACENT WATER AREA OF THE KARA SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b947e8aa678.89317861.

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The distribution of dissolved chemical elements (major ions, nutrients, and trace elements) in the Yenisei River estuary and adjacent water area in 2009 and 2010 are presented. These results were compared to the data obtained during previous hydrochemical studies of this region. The transport of major cations (Na, K, Mg, Ca) and some trace elements (Rb, Cs, Sr, B, F, As, Mo, U) in the estuary follows conservative mixing. Alkalinity also belongs to conservative components, however this parameter exhibits substantial spatial heterogeneity caused by complex hydrological structure of the Yenisei B
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Yang, Mingyuan, and Wei Zhang. "Study on Salinity Stratification and Distribution in Lingding Yang Estuary." In ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57123.

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Ling Ding Yang (LDY) estuary is one of the main parts of the whole Zhujiang estuary, which lies in the south sea, China. It is about 60km wide from Hong Kong in the east to Macao in the west and the water areas are approximately 2110 km2. The mixing process of salt water and fresh water in the estuary is influenced by many factors, such as the estuarine geometry, tidal range and ravine flows, etc. In this paper, based on the data from the tidal gauge stations and synchronously surveyed data during July 2003, a study on the temporal and spatial distribution characteristics of salinity was made.
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Hao, Jialing, Jinhai Zheng, and Wei Zhang. "Observations of the Boundary Layer Characteristics at the Yangtze Estuary." In ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79897.

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Measurements of the flow velocity profiles through one tidal cycle were taken in the Yangtze Estuary. The flow velocity profile during the experiment was characteristic of a tidal boundary layer growing through the tide, and with increasing velocity, especially on the accelerating flood tide. Due to the bed friction, the near bottom flow, which forms the bottom boundary layer, is different from that of the water body far from the bed in estuarine and coastal waters. In near bottom layer, due to the frequent flux and momentum exchanges between the flow and the bed, the study of near bottom play
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