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Journal articles on the topic 'Water mass'

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Author: Grafiati

Published: 4 June 2021

Last updated: 25 May 2024

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1

Thuy, Pham Thi, Pham Thanh Tuan, and Nguyen Manh Khai. "Industrial Water Mass Balance Analysis." International Journal of Environmental Science and Development 7, no. 3 (2016): 216–20. http://dx.doi.org/10.7763/ijesd.2016.v7.771.

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2

Kenway, Steven, Alan Gregory, and Joseph McMahon. "Urban Water Mass Balance Analysis." Journal of Industrial Ecology 15, no. 5 (August 18, 2011): 693–706. http://dx.doi.org/10.1111/j.1530-9290.2011.00357.x.

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3

Ono, Kazuya, Kay I. Ohshima, Tokihiro Kono, Motoyo Itoh, Katsuro Katsumata, Yuri N. Volkov, and Masaaki Wakatsuchi. "Water mass exchange and diapycnal mixing at Bussol’ Strait revealed by water mass properties." Journal of Oceanography 63, no. 2 (April 2007): 281–91. http://dx.doi.org/10.1007/s10872-007-0028-3.

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4

Yang, Dongfang, Dong Lin, Longlei Zhang, Qi Wang, and Haixia Li. "Isothermal Water Mass in the Bottom Water at the Bay Mouth of Jiaozhou Bay Isothermal Water Mass Existence." IOP Conference Series: Earth and Environmental Science 512 (June 18, 2020): 012041. http://dx.doi.org/10.1088/1755-1315/512/1/012041.

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5

Jiang, Pei-Xue, V. S. Protopopov, Ze-Pei Ren, and Bu-Xuan Wang. "Turbulent convection mass transfer of water with internal mass sources." Heat Transfer?Asian Research 29, no. 3 (May 2000): 166–80. http://dx.doi.org/10.1002/(sici)1523-1496(200005)29:3<166::aid-htj2>3.0.co;2-m.

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6

Yang, Dongfang, Jing Fang, Chunhua Su, Ming Wang, and Sixi Zhu. "Isothermal Water Mass in the Bottom Water at the Bay Mouth of Jiaozhou Bay?. Isothermal Water Mass scale and location." IOP Conference Series: Earth and Environmental Science 512 (June 18, 2020): 012038. http://dx.doi.org/10.1088/1755-1315/512/1/012038.

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7

Maamaatuaiahutapu, Keitapu, Véronique C. Garçon, Christine Provost, Mostefa Boulahdid, and Ana Paula Osiroff. "Brazil-Malvinas Confluence: Water mass composition." Journal of Geophysical Research 97, no. C6 (1992): 9493. http://dx.doi.org/10.1029/92jc00484.

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8

Saputra, Frilla Renty Tama, and Yohanis Dominggus Lekalette. "WATER MASS DYNAMICS IN AMBON BAY." Widyariset 2, no. 2 (November 30, 2016): 143. http://dx.doi.org/10.14203/widyariset.2.2.2016.143-152.

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9

McDougall, Trevor J. "Thermobaricity, cabbeling, and water-mass conversion." Journal of Geophysical Research 92, no. C5 (1987): 5448. http://dx.doi.org/10.1029/jc092ic05p05448.

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10

Stuhlmeier, Raphael. "Gerstner’s Water Wave and Mass Transport." Journal of Mathematical Fluid Mechanics 17, no. 4 (July 23, 2015): 761–67. http://dx.doi.org/10.1007/s00021-015-0219-4.

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11

Lynch, Daniel R. "Mass balance in shallow water simulation." Communications in Applied Numerical Methods 1, no. 4 (July 1985): 153–59. http://dx.doi.org/10.1002/cnm.1630010404.

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12

Meyer, Elisabeth. "The relationship between body length parameters and dry mass in running water invertebrates." Archiv für Hydrobiologie 117, no. 2 (December 20, 1989): 191–203. http://dx.doi.org/10.1127/archiv-hydrobiol/117/1989/191.

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13

Yang, Hei-Cheon. "Mass Transfer Characteristics with Mass Ratio of Air-Water Mixed Jet." Transactions of the Korean Society of Mechanical Engineers - B 46, no. 5 (May 31, 2022): 267–74. http://dx.doi.org/10.3795/ksme-b.2022.46.5.267.

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14

Marov, Mikhail Ya, and Sergei I. Ipatov. "Water inventory from beyond the Jupiter’s orbit to the terrestrial planets and the Moon." Proceedings of the International Astronomical Union 14, S345 (August 2018): 164–67. http://dx.doi.org/10.1017/s1743921319001479.

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AbstractComputer simulations of migration of planetesimals from beyond the Jupiter’s orbit to the terrestrial planets have been made. Based on obtained arrays of orbital elements of planetesimals and planets during the dynamical lifetimes of planetesimals, we calculated the probabilities of collisions of planetesimals with planets, the Moon, and their embryos. The results of calculations showed that for the total mass of planetesimals of about 200 Earth masses, the mass of water delivered to the Earth from beyond the orbit of Jupiter could be about the mass of the terrestrial oceans. For the growth of the mass of the Earth embryo up to a half of the present mass of the Earth, the mass of water delivered to the embryo could be up to 30% of all water delivered to the Earth from the zone of Jupiter and Saturn. The water of the terrestrial oceans and its D/H ratio could be the result of mixing of water from several exogenic and endogenic sources with large and low D/H ratios. The ratio of the mass of water delivered from beyond the orbit of Jupiter to a planet to the mass of the planet for Venus, Mars, and Mercury was not smaller than that for the Earth. The mass of water in planetesimals that collided the Moon and migrated from beyond the Jupiter’s orbit could be not more than 20 times smaller than that for the Earth.

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15

Lapeira, E., M. M. Bou-Ali, J. A. Madariaga, and C. Santamaría. "Thermodiffusion Coefficients of Water/Ethanol Mixtures for Low Water Mass Fractions." Microgravity Science and Technology 28, no. 5 (July 4, 2016): 553–57. http://dx.doi.org/10.1007/s12217-016-9508-7.

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16

Zhang, Xinxing. "Mass spectrometry at the air-water interface." International Journal of Mass Spectrometry 462 (April 2021): 116527. http://dx.doi.org/10.1016/j.ijms.2021.116527.

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17

Davis, Michael J., Robert Janke, and Thomas N. Taxon. "Mass imbalances in EPANET water-quality simulations." Drinking Water Engineering and Science 11, no. 1 (April 6, 2018): 25–47. http://dx.doi.org/10.5194/dwes-11-25-2018.

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Abstract. EPANET is widely employed to simulate water quality in water distribution systems. However, in general, the time-driven simulation approach used to determine concentrations of water-quality constituents provides accurate results only for short water-quality time steps. Overly long time steps can yield errors in concentration estimates and can result in situations in which constituent mass is not conserved. The use of a time step that is sufficiently short to avoid these problems may not always be feasible. The absence of EPANET errors or warnings does not ensure conservation of mass. This paper provides examples illustrating mass imbalances and explains how such imbalances can occur because of fundamental limitations in the water-quality routing algorithm used in EPANET. In general, these limitations cannot be overcome by the use of improved water-quality modeling practices. This paper also presents a preliminary event-driven approach that conserves mass with a water-quality time step that is as long as the hydraulic time step. Results obtained using the current approach converge, or tend to converge, toward those obtained using the preliminary event-driven approach as the water-quality time step decreases. Improving the water-quality routing algorithm used in EPANET could eliminate mass imbalances and related errors in estimated concentrations. The results presented in this paper should be of value to those who perform water-quality simulations using EPANET or use the results of such simulations, including utility managers and engineers.

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18

Arnone, Robert, Michelle Wood, and Richard Gould. "The Evolution of Optical Water Mass Classification." Oceanography 17, no. 2 (June 1, 2004): 14–15. http://dx.doi.org/10.5670/oceanog.2004.42.

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19

Braida, Washington J., and Say Kee Ong. "Air sparging: Air-water mass transfer coefficients." Water Resources Research 34, no. 12 (December 1998): 3245–53. http://dx.doi.org/10.1029/98wr02533.

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20

Pearlstein, Sol. "Critical Mass Variation of239Pu with Water Dilution." Nuclear Technology 113, no. 1 (January 1996): 110–11. http://dx.doi.org/10.13182/nt96-a35203.

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21

INAGAKI, Taiichi, Takanobu ODA, and Takashi Kawakami. "Additional water mass in pump impeller vibration." Transactions of the Japan Society of Mechanical Engineers Series C 55, no. 511 (1989): 651–55. http://dx.doi.org/10.1299/kikaic.55.651.

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22

McDougall, Trevor J. "Water mass analysis with three conservative variables." Journal of Geophysical Research 96, no. C5 (1991): 8687. http://dx.doi.org/10.1029/90jc02739.

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23

Speer, Kevin G., H.-J. Isemer, and A. Biastoch. "Water Mass Formation from Revised COADS Data." Journal of Physical Oceanography 25, no. 10 (October 1995): 2444–57. http://dx.doi.org/10.1175/1520-0485(1995)025<2444:wmffrc>2.0.co;2.

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24

Badin, Gualtiero, Richard G. Williams, and Jonathan Sharples. "Water-mass transformation in the shelf seas." Journal of Marine Research 68, no. 2 (March 1, 2010): 189–214. http://dx.doi.org/10.1357/002224010793721442.

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25

Lee, Chung-te, and Wen-chuan Hsu. "A method of measuring aerosol water mass." Journal of Aerosol Science 28 (September 1997): S19—S20. http://dx.doi.org/10.1016/s0021-8502(97)85011-2.

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26

Nguyen, Thien Khoi V., Qi Zhang, Jose L. Jimenez, Maxwell Pike, and Annmarie G. Carlton. "Liquid Water: Ubiquitous Contributor to Aerosol Mass." Environmental Science & Technology Letters 3, no. 7 (June 10, 2016): 257–63. http://dx.doi.org/10.1021/acs.estlett.6b00167.

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27

Iskandarani, Mohamed, and Philip L. F. Liu. "Mass transport in two-dimensional water waves." Journal of Fluid Mechanics 231 (October 1991): 395–415. http://dx.doi.org/10.1017/s0022112091003440.

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Mass transport in various kind of two-dimensional water waves is studied. The characteristics of the governing equations for the mass transport depend on the ratio of viscous lengthscale to the amplitude of the free-surface displacement. When this ratio is small, the nonlinearity is important and the mass transport flow acquires a boundary-layer character. Numerical schemes are developed to investigate mass transport in a partially reflected wave and above a hump in the seabed. When the mass transport is periodic in the horizontal direction, a spectral scheme based on a Fourier–Chebyshev expansion, is presented for the solution of the equations. For the ease of a hump on the seabed, the flow domain is divided into three regions. Using the spectral scheme, the mass transport in the uniform-depth regions is calculated first. and the results are used to compute the steady flow in the inhomogeneous flow region which encloses the hump on the seabed.

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28

Iskandarani, Mohamed, and Philip L. F. Liu. "Mass transport in three-dimensional water waves." Journal of Fluid Mechanics 231 (October 1991): 417–37. http://dx.doi.org/10.1017/s0022112091003452.

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A spectral scheme is developed to study the mass transport in three-dimensional water waves where the steady flow is assumed to be periodic in two horizontal directions. The velocity–vorticity formulation is adopted for the numerical solution, and boundary conditions for the vorticity are derived to enforce the no-slip conditions. The numerical scheme is used to calculate the mass transport under two intersecting wave trains; the resulting flow is reminiscent of the Langmuir circulation patterns. The scheme is then applied to study the steady flow in a three-dimensional standing wave.

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29

Oguz, Hasan N., Andrea Prosperetti, and Ali R. Kolaini. "Air entrapment by a falling water mass." Journal of Fluid Mechanics 294 (July 10, 1995): 181–207. http://dx.doi.org/10.1017/s0022112095002850.

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The impact of a nearly cylindrical water mass on a water surface is studied both experimentally and theoretically. The experiments consist of the rapid release of water from the bottom of a cylindrical container suspended above a large water tank and of the recording of the free-surface shape of the resulting crater with a high-speed camera. A bubble with a diameter of about twice that of the initial cylinder remains entrapped at the bottom of the crater when the aspect ratio and the energy of the falling water mass are sufficiently large. Many of the salient features of the phenomenon are explained on the basis of simple physical arguments. Boundary-integral potential-flow simulations of the process are also described. These numerical results are in fair to good agreement with the observations.

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30

Hulthe, Gustaf, Gunnar Stenhagen, Olof Wennerström, and Carl-Henrik Ottosson. "Water clusters studied by electrospray mass spectrometry." Journal of Chromatography A 777, no. 1 (August 1997): 155–65. http://dx.doi.org/10.1016/s0021-9673(97)00486-x.

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31

Nagl, Roland, Patrick Zimmermann, and Tim Zeiner. "Interfacial Mass Transfer in Water–Toluene Systems." Journal of Chemical & Engineering Data 65, no. 2 (September 13, 2019): 328–36. http://dx.doi.org/10.1021/acs.jced.9b00672.

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32

Ochi, Tadashi, and Hidetaka Takeoka. "The anoxic water mass in Hiuchi-Nada." Journal of the Oceanographical Society of Japan 42, no. 1 (February 1986): 1–11. http://dx.doi.org/10.1007/bf02109187.

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33

Takeoka, Hidetaka, Tadashi Ochi, and Kazuhiko Takatani. "The anoxic water mass in Hiuchi-Nada." Journal of the Oceanographical Society of Japan 42, no. 1 (February 1986): 12–21. http://dx.doi.org/10.1007/bf02109188.

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34

Våge, Kjetil, G. W. K. Moore, Steingrímur Jónsson, and Héðinn Valdimarsson. "Water mass transformation in the Iceland Sea." Deep Sea Research Part I: Oceanographic Research Papers 101 (July 2015): 98–109. http://dx.doi.org/10.1016/j.dsr.2015.04.001.

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35

Pace, D. R., Yocie Yoneshigue, and Salvador A. Jacob. "Phytoplankton mass culture in discontinuously upwelling water." Aquaculture 58, no. 1-2 (November 1986): 123–32. http://dx.doi.org/10.1016/0044-8486(86)90161-4.

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36

Mills, R. H. "Mass transfer of water vapour through concrete." Cement and Concrete Research 15, no. 1 (January 1985): 74–82. http://dx.doi.org/10.1016/0008-8846(85)90010-9.

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37

Oguz, H. "Air entrapment by a falling water mass." International Journal of Multiphase Flow 22 (December 1996): 129. http://dx.doi.org/10.1016/s0301-9322(97)88422-4.

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38

Oguz, H. "Air entrapment by a falling water mass." International Journal of Multiphase Flow 22 (December 1996): 130. http://dx.doi.org/10.1016/s0301-9322(97)88435-2.

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39

Rowiński, Paweł M., and Subhasish Dey. "Water-Worked Bedload: Hydrodynamics and Mass Transport." Water 11, no. 7 (July 7, 2019): 1396. http://dx.doi.org/10.3390/w11071396.

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40

Hieronymus, Magnus, Johan Nilsson, and Jonas Nycander. "Water Mass Transformation in Salinity–Temperature Space." Journal of Physical Oceanography 44, no. 9 (September 1, 2014): 2547–68. http://dx.doi.org/10.1175/jpo-d-13-0257.1.

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Abstract This article presents a new framework for studying water mass transformations in salinity–temperature space that can, with equal ease, be applied to study water mass transformation in spaces defined by any two conservative tracers. It is shown how the flow across isothermal and isohaline surfaces in the ocean can be quantified from knowledge of the nonadvective fluxes of heat and salt. It is also shown how these cross-isothermal and cross-isohaline flows can be used to form a continuity equation in salinity–temperature space. These flows are then quantified in a state-of-the-art ocean model. Two major transformation cells are found: a tropical cell driven primarily by surface fluxes and dianeutral diffusion and a conveyor belt cell where isoneutral diffusion is also important. Both cells are similar to cells found in earlier work on the thermohaline streamfunction. A key benefit with this framework over a streamfunction approach is that transformation due to different diabatic processes can be studied individually. The distributions of volume and surface area in S–T space are found to be useful for determining how transformations due to these different processes affect the water masses in the model. The surface area distribution shows that the water mass transformations due to surface fluxes tend to be directed away from S–T regions that occupy large areas at the sea surface.

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41

Steinberger, Nancy, and Midhat Hondzo. "Diffusional Mass Transfer at Sediment-Water Interface." Journal of Environmental Engineering 125, no. 2 (February 1999): 192–200. http://dx.doi.org/10.1061/(asce)0733-9372(1999)125:2(192).

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42

SAWAMURA, Toshihiro, and Shingo TSUBOTA. "1917 Mass Distributions in Abrasive Water Jet." Proceedings of the JSME annual meeting 2008.2 (2008): 233–34. http://dx.doi.org/10.1299/jsmemecjo.2008.2.0_233.

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43

Rosen, Ran. "Mass spectrometry for monitoring micropollutants in water." Current Opinion in Biotechnology 18, no. 3 (June 2007): 246–51. http://dx.doi.org/10.1016/j.copbio.2007.03.005.

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44

Schöck, W., and V. Vrangos. "Calorimetric measurement of water fog mass concentration." Journal of Aerosol Science 17, no. 3 (January 1986): 525–29. http://dx.doi.org/10.1016/0021-8502(86)90149-7.

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45

Groeskamp, Sjoerd, Ryan P. Abernathey, and Andreas Klocker. "Water mass transformation by cabbeling and thermobaricity." Geophysical Research Letters 43, no. 20 (October 18, 2016): 10,835–10,845. http://dx.doi.org/10.1002/2016gl070860.

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46

Canepari, S., G. Simonetti, and C. Perrino. "Mass size distribution of particle-bound water." Atmospheric Environment 165 (September 2017): 46–56. http://dx.doi.org/10.1016/j.atmosenv.2017.06.034.

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47

Koroleva, Marina Yu, and Evgeny V. Yurtov. "Water mass transfer in W/O emulsions." Journal of Colloid and Interface Science 297, no. 2 (May 2006): 778–84. http://dx.doi.org/10.1016/j.jcis.2005.10.046.

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48

J. Mahmood, Omar, Riyadh S.Al-mukhtar, and Asawer A. Alwasit. "Mass transfer of ozone in purified water." Engineering and Technology Journal 27, no. 4 (March 1, 2009): 776–86. http://dx.doi.org/10.30684/etj.27.4.13.

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49

Feijó Delgado, Francisco, Nathan Cermak, Vivian C. Hecht, Sungmin Son, Yingzhong Li, Scott M. Knudsen, Selim Olcum, et al. "Intracellular Water Exchange for Measuring the Dry Mass, Water Mass and Changes in Chemical Composition of Living Cells." PLoS ONE 8, no. 7 (July 2, 2013): e67590. http://dx.doi.org/10.1371/journal.pone.0067590.

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50

Rajappa, Sacchi, John P. Kurian, Abhishek Tyagi, and Nuncio Murukesh. "Interaction between seabed morphology and water mass in the South Eastern Arabian Sea: deductions of water mass flow." Geo-Marine Letters 40, no. 5 (July 24, 2020): 725–40. http://dx.doi.org/10.1007/s00367-020-00663-7.

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