Relevant bibliographies by topics / Water mass

Academic literature on the topic 'Water mass'

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Published: 4 June 2021
Last updated: 25 May 2024

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Journal articles on the topic "Water mass"

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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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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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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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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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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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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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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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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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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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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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Dissertations / Theses on the topic "Water mass"

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LI, ZHIWEI. "NETWORK WATER QUALITY MODELING WITH STOCHASTIC WATER DEMANDS AND MASS DISPERSION." University of Cincinnati / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1147989825.

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Jullion, Loĭc. "Water mass modification in the southwestern Atlantic." Thesis, University of East Anglia, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.446168.

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LEE, YEONGHO. "MASS DISPERSION IN INTERMITTENT LAMINAR FLOW." University of Cincinnati / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1085750678.

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Lindblom, Jenny. "Condensation irrigation : simulations of heat and mass transfer." Licentiate thesis, Luleå : Luleå University of technology, 2006. http://epubl.luth.se/1402-1757/2006/08.

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Brunet, Robert A. H. "Silent discharge water treatment, mass transfer and reaction rates." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ39805.pdf.

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Brandon, Mark Alan. "Winter surface water mass modification in the Greenland Sea." Thesis, University of Cambridge, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.388764.

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Zhang, Huai-Min Ph D. Massachusetts Institute of Technology. "Circulations and water mass balances in the Brazil Basin." Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/57934.

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Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences and Woods Hole Oceanographic Institution, 1991.
Bibliography: p.151-155.
by Huai-Min Zhang.
M.S.
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PIVETTA, TOMMASO FERRUCCIO MARIA. "Gravimetry for monitoring water mass movements in karstic areas." Doctoral thesis, Università degli Studi di Trieste, 2021. http://hdl.handle.net/11368/2988158.

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Karst aquifers represent a significant source of water for about 1/4 of the world’s population. The water circulation in karst occurs mostly underground and it is mainly controlled by alternation of small conduits and large voids present in the rock massif. Such intricate void distribution combined with an irregular recharge provided by the rain results in fast and complex water flows with temporary accumulation of huge water volumes in the voids. The knowledge of the dynamics of such system is usually limited to the areas where a direct access to the vadose zone through speleological exploration is possible. Given the importance of such aquifers and their vulnerability it is important to have a detailed picture of the water dynamics and of the underground water paths. Gravimetry offers a valid complement to classical hydrologic measurements in order to monitor the recharge process. In this thesis, I show an innovative integration of gravimetric and hydrologic observations to constrain a hydrodynamic model of the Škocjan cave system (Slovenia). The Škocjan caves hydrology is mostly governed by the allogenic contribution of the Reka River, which during flood event causes the accumulation of several millions of m3 of water in the cave system for few hours. In 2018 I installed a continuous recording gravimeter nearby Škocjan which allowed the detection of several gravity transients related to the local hydrologic contribution. Gravity observations are sensitive to several other contributions apart the hydrology, such as Earth and marine tides, atmospheric mass redistribution, water mass variations in oceans. All these phenomena superpose their effects and should be carefully evaluated and removed before unveiling the local hydrology contribution. Before discussing the hydrologic gravity signals, the thesis illustrates the efforts in modelling and removing all the non-hydrologic related gravity contributions. The study area is close to the Adriatic Sea, hence global models of tidal and non-tidal ocean (NTO) gravity effects could be inadequate for the correction. I prove that while tidal models are sufficiently accurate to remove the marine tidal influence a dedicated correction of the NTO is required. This was fulfilled by modelling the gravity variations due to a 4D mass model of the NTO constrained by tide gauge observations. The gravity residuals, obtained after reducing the observations for all the non-hydrologic effects, revealed anomalies correlated to the Reka flooding; the transients lasted for 12-24 hours with amplitudes in the range 10-450 nm/s2. I focused my analysis on a large flood event in February 2019 that caused water level variations >90 m inside the caves and gravity variations >400 nm/s2. The gravity and the hydrologic data were used to constrain a hydraulic model of the cave system which approximated the cavity through a series of interconnected conduits with rectangular cross-section. I fitted hydrologic and gravity observations obtaining a 4D model of the water mass variations in the cave system; the model revealed that >3 106 m3 of water were temporary accumulated during the peak’s flood. The inclusion of gravity observations improves water mass budget of the caves, which previously were based relying only on hydrological observations. Finally, the gravity data allowed to draw some general conclusions on the detectability of water storage variations in karst through gravimetry. I assessed the noise level of the Škocjan gravimeter which is about 10 nm/s2 in the diurnal spectral band and which can be taken as representative of the noise level of a typical spring based gravimeter. Relying on realistic water level variations I estimated the expected gravity signals on surface due to temporary water accumulation in other caves of the Classical Karst. For all the considered caves the gravity signal is above the noise threshold, suggesting that a remote monitoring of the storage variations is feasible.
Karst aquifers represent a significant source of water for about 1/4 of the world’s population. The water circulation in karst occurs mostly underground and it is mainly controlled by alternation of small conduits and large voids present in the rock massif. Such intricate void distribution combined with an irregular recharge provided by the rain results in fast and complex water flows with temporary accumulation of huge water volumes in the voids. The knowledge of the dynamics of such system is usually limited to the areas where a direct access to the vadose zone through speleological exploration is possible. Given the importance of such aquifers and their vulnerability it is important to have a detailed picture of the water dynamics and of the underground water paths. Gravimetry offers a valid complement to classical hydrologic measurements in order to monitor the recharge process. In this thesis, I show an innovative integration of gravimetric and hydrologic observations to constrain a hydrodynamic model of the Škocjan cave system (Slovenia). The Škocjan caves hydrology is mostly governed by the allogenic contribution of the Reka River, which during flood event causes the accumulation of several millions of m3 of water in the cave system for few hours. In 2018 I installed a continuous recording gravimeter nearby Škocjan which allowed the detection of several gravity transients related to the local hydrologic contribution. Gravity observations are sensitive to several other contributions apart the hydrology, such as Earth and marine tides, atmospheric mass redistribution, water mass variations in oceans. All these phenomena superpose their effects and should be carefully evaluated and removed before unveiling the local hydrology contribution. Before discussing the hydrologic gravity signals, the thesis illustrates the efforts in modelling and removing all the non-hydrologic related gravity contributions. The study area is close to the Adriatic Sea, hence global models of tidal and non-tidal ocean (NTO) gravity effects could be inadequate for the correction. I prove that while tidal models are sufficiently accurate to remove the marine tidal influence a dedicated correction of the NTO is required. This was fulfilled by modelling the gravity variations due to a 4D mass model of the NTO constrained by tide gauge observations. The gravity residuals, obtained after reducing the observations for all the non-hydrologic effects, revealed anomalies correlated to the Reka flooding; the transients lasted for 12-24 hours with amplitudes in the range 10-450 nm/s2. I focused my analysis on a large flood event in February 2019 that caused water level variations >90 m inside the caves and gravity variations >400 nm/s2. The gravity and the hydrologic data were used to constrain a hydraulic model of the cave system which approximated the cavity through a series of interconnected conduits with rectangular cross-section. I fitted hydrologic and gravity observations obtaining a 4D model of the water mass variations in the cave system; the model revealed that >3 106 m3 of water were temporary accumulated during the peak’s flood. The inclusion of gravity observations improves water mass budget of the caves, which previously were based relying only on hydrological observations. Finally, the gravity data allowed to draw some general conclusions on the detectability of water storage variations in karst through gravimetry. I assessed the noise level of the Škocjan gravimeter which is about 10 nm/s2 in the diurnal spectral band and which can be taken as representative of the noise level of a typical spring based gravimeter. Relying on realistic water level variations I estimated the expected gravity signals on surface due to temporary water accumulation in other caves of the Classical Karst. For all the considered caves the gravity signal is above the noise threshold, suggesting that a remote monitoring of the storage variations is feasible.
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Glogowski, Silke [Verfasser]. "Water mass dynamics around cold-water coral reefs in the North Atlantic / Silke Glogowski." Kiel : Universitätsbibliothek Kiel, 2017. http://d-nb.info/1141678004/34.

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Padowski, Julie C. "Direct measurement of water and solute mass fluxes using a passive surface water flux meter." [Gainesville, Fla.] : University of Florida, 2005. http://purl.fcla.edu/fcla/etd/UFE0013283.

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Books on the topic "Water mass"

1

E, Peters Norman, Bricker Owen P. 1936-, and Kennedy M. M, eds. Water quality trends and geochemical mass balance. Chichester: Wiley, 1997.

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Kang, Ersi. Energy, water, mass balance, and hydrological discharge. Zürich: Geologisches Institut ETH, 1994.

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Mahapatra, Richard. Weapon of mass appeal: Drinking water security in drought prone areas. New Delhi: WaterAid India, 2010.

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Vedanayagam, Samuel. Mass balance analysis of suspended solids in the Tualatin River. [Corvallis]: Oregon Water Resources Research Institute, 1995.

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Molot, Lewis A. Nitrogen mass balances and denitrification rates in Central Ontario lakes. [Toronto]: Queen's Printer for Ontario, 1993.

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Dugan, Jack T. Mass water-level measurements of fall 1984 in the central Platte River Basin, Nebraska. Lincoln, Neb: U.S. Dept. of the Interior, Geological Survey, 1985.

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T, Dugan Jack. Mass water-level measurements of fall 1984 in the central Platte River Basin, Nebraska. Lincoln, Neb: U.S. Dept. of the Interior, Geological Survey, 1985.

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United States. Bureau of Reclamation and Geological Survey (U.S.), eds. Mass water-level measurements of fall 1984 in the central Platte River Basin, Nebraska. Lincoln, Neb: U.S. Dept. of the Interior, Geological Survey, 1985.

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United States. Bureau of Reclamation and Geological Survey (U.S.), eds. Mass water-level measurements of fall 1984 in the central Platte River Basin, Nebraska. Lincoln, Neb: U.S. Dept. of the Interior, Geological Survey, 1985.

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T, Dugan Jack. Mass water-level measurements of fall 1984 in the central Platte River Basin, Nebraska. Lincoln, Neb: U.S. Dept. of the Interior, Geological Survey, 1985.

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Book chapters on the topic "Water mass"

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Lung, Wu-Seng. "Quantifying Estuarine Mass Transport." In Water Quality Modeling, 9–42. New York: CRC Press, 2021. http://dx.doi.org/10.1201/9781003208969-3.

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Reynolds, John S. "Shade, mass and water." In Activism in Architecture, 83–92. New York : Routledge, 2019. | Series: Routledge research in architecture: Routledge, 2018. http://dx.doi.org/10.4324/9781315182858-9.

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Goudie, Andrew. "Water Erosion and Mass Movements." In Landscapes of the Anthropocene with Google Earth, 191–219. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-45385-4_9.

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Callender, Edward, and Liba Granina. "Biogeochemical silica mass balance in Lake Baikal, Russia." In Water-Rock Interaction, 341–44. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-85.

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Poli, Diana. "Determination of Chlorinated Compounds in Dialysis Water and in Biological Fluids/Matrices." In Mass Spectrometry Handbook, 631–44. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2012. http://dx.doi.org/10.1002/9781118180730.ch29.

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Waller, Peter, and Muluneh Yitayew. "Water and Solute Mass Balance Models." In Irrigation and Drainage Engineering, 455–74. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-05699-9_26.

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Na, Chongzheng, and Terese M. Olson. "Disinfectant and By-Product Analysis in Water Treatment by Membrane Introduction Mass Spectrometry." In Mass Spectrometry Handbook, 593–603. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2012. http://dx.doi.org/10.1002/9781118180730.ch27.

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Pelto, Mauri. "Glacier Mass Balance." In Climate Driven Retreat of Mount Baker Glaciers and Changing Water Resources, 25–47. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-22605-7_3.

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Pellizzari, E. D., and J. T. Bursey. "Gas Chromatography/Mass Spectrometry in Water Pollution Studies." In Mass Spectrometry in Environmental Sciences, 139–58. Boston, MA: Springer US, 1985. http://dx.doi.org/10.1007/978-1-4613-2361-7_8.

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Weaver, P. P. E., D. G. Masson, D. E. Gunn, R. B. Kidd, R. G. Rothwell, and D. A. Maddison. "Sediment mass wasting in the Canary Basin." In Atlas of Deep Water Environments, 287–96. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_43.

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Conference papers on the topic "Water mass"

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Elmore, Andrew Curtis. "A Mass Balance-Based 1D Mass Transport Model." In World Environmental and Water Resources Congress 2008. Reston, VA: American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40976(316)74.

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Lenhart, James H., and Paula P. Calvert. "Mass Loading and Mass Load Design of Stormwater Filtration Systems." In World Environmental and Water Resources Congress 2007. Reston, VA: American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40927(243)13.

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Lee, Johnny. "Mass Transfer Coefficient and Gas Solubility." In World Environmental and Water Resources Congress 2017. Reston, VA: American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480632.004.

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Boni, M. R., S. Sbaffoni, P. Tedesco, and M. Vaccari. "Mass balance of emerging organic micropollutants in a small wastewater treatment plant." In WATER POLLUTION 2012. Southampton, UK: WIT Press, 2012. http://dx.doi.org/10.2495/wp120301.

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Sabia, Roberto, Diego Fernández-Prieto, Marlene Klockmann, Luigi Castaldo, and Aqeel Piracha. "Satellite based estimation of water-mass formation areas and extents." In Remote Sensing of the Ocean, Sea Ice, Coastal Waters, and Large Water Regions 2018, edited by Charles R. Bostater, Stelios P. Mertikas, and Xavier Neyt. SPIE, 2018. http://dx.doi.org/10.1117/12.2325699.

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Brunsch, A. F. "Mass flow analysis for anthropogenic micropollutants as performed in the Swist river catchment." In WATER POLLUTION 2014. Southampton, UK: WIT Press, 2014. http://dx.doi.org/10.2495/wp140081.

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Shikazono, N. "Water-Rock Interaction And Mass Transfer In Hydrothermal System: Kinetics, FLUID Flow And Mixing Model." In WATER DYANMICS: 3rd International Workshop on Water Dynamics. AIP, 2006. http://dx.doi.org/10.1063/1.2207089.

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Ceci, S., L. De Biase, and G. Fossati. "Heat transfer in 3D water and ice basins." In HEAT AND MASS TRANSFER 2006. Southampton, UK: WIT Press, 2006. http://dx.doi.org/10.2495/ht060141.

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Pisano, William C., Steve L. White, and Owen O'Riordian. "Implementation of Automated Sewer and Drainage Flushing Systems in Cambridge, Mass." In Joint Conference on Water Resource Engineering and Water Resources Planning and Management 2000. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40517(2000)152.

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Novozhilov, Vasily, Behdad Moghtaderi, J. H. Kent, and David F. Fletcher. "Extinguishment of Burning Solid Materials by a Water Spray." In Heat and Mass Transfer Australasia. Connecticut: Begellhouse, 2023. http://dx.doi.org/10.1615/978-1-56700-099-3.300.

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Reports on the topic "Water mass"

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Pickart, Robert S. Winter Water Mass Transformation in the Labrador Sea. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada628692.

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Kunze, Eric. Finescale Water-Mass Variability from ARGO Profiling Floats. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada590612.

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Kunze, Eric. Lateral Mixing DRI Analysis: Submesoscale Water-Mass Spectra. Fort Belvoir, VA: Defense Technical Information Center, September 2013. http://dx.doi.org/10.21236/ada601168.

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Kunze, Eric. Finescale Water-Mass Variability from ARGO Profiling Floats. Fort Belvoir, VA: Defense Technical Information Center, September 2014. http://dx.doi.org/10.21236/ada624695.

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Lieb, B. W., A. P. Jacala, and R. P. Glasser. Added mass for plates partially submerged in water. Office of Scientific and Technical Information (OSTI), September 1988. http://dx.doi.org/10.2172/10173548.

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Fitzgerald, Robert, and Vicki L. Van Blaricum. Water Hammer and Mass Oscillation (WHAMO) 3.0 User's Manual. Fort Belvoir, VA: Defense Technical Information Center, September 1998. http://dx.doi.org/10.21236/ada360720.

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Clewell, Rebecca A., Wayne T. Brashear, David T. Tsui, Sanwat Chaudhuri, and Rachel S. Cassady. Analysis of Trace Level Perchlorate in Drinking Water and Ground Water by Electrospray Mass Spectrometry. Fort Belvoir, VA: Defense Technical Information Center, October 1998. http://dx.doi.org/10.21236/ada428122.

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Yang, Jiann C., Charles I. Boyer, and William L. Grosshandler. Minimum mass flux requirements to suppress burning surfaces with water sprays. Gaithersburg, MD: National Institute of Standards and Technology, 1996. http://dx.doi.org/10.6028/nist.ir.5795.

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Webb, Stephen W., James M. Phelan, Teklu Hadgu, Joshua S. Stein, and Cedric M. Sallaberry. Measurement and Modeling of Energetic-Material Mass Transfer to Soil-Pore Water. Fort Belvoir, VA: Defense Technical Information Center, May 2006. http://dx.doi.org/10.21236/ada631327.

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Desiderati, Christopher. Carli Creek Regional Water Quality Project: Assessing Water Quality Improvement at an Urban Stormwater Constructed Wetland. Portland State University, 2022. http://dx.doi.org/10.15760/mem.78.

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Abstract:
Stormwater management is an ongoing challenge in the United States and the world at-large. As state and municipal agencies grapple with conflicting interests like encouraging land development, complying with permits to control stormwater discharges, “urban stream syndrome” effects, and charges to steward natural resources for the long-term, some agencies may turn to constructed wetlands (CWs) as aesthetically pleasing and functional natural analogs for attenuating pollution delivered by stormwater runoff to rivers and streams. Constructed wetlands retain pollutants via common physical, physicochemical, and biological principles such as settling, adsorption, or plant and algae uptake. The efficacy of constructed wetlands for pollutant attenuation varies depending on many factors such as flow rate, pollutant loading, maintenance practices, and design features. In 2018, the culmination of efforts by Clackamas Water Environment Services and others led to the opening of the Carli Creek Water Quality Project, a 15-acre constructed wetland adjacent to Carli Creek, a small, 3500-ft tributary of the Clackamas River in Clackamas County, OR. The combined creek and constructed wetland drain an industrialized, 438-acre, impervious catchment. The wetland consists of a linear series of a detention pond and three bioretention treatment cells, contributing a combined 1.8 acres of treatment area (a 1:243 ratio with the catchment) and 3.3 acre-feet of total runoff storage. In this study, raw pollutant concentrations in runoff were evaluated against International Stormwater BMP database benchmarks and Oregon Water Quality Criteria. Concentration and mass-based reductions were calculated for 10 specific pollutants and compared to daily precipitation totals from a nearby precipitation station. Mass-based reductions were generally higher for all pollutants, largely due to runoff volume reduction on the treatment terrace. Concentration-based reductions were highly variable, and suggested export of certain pollutants (e.g., ammonia), even when reporting on a mass-basis. Mass load reductions on the terrace for total dissolved solids, nitrate+nitrite, dissolved lead, and dissolved copper were 43.3 ± 10%, 41.9 ± 10%, 36.6 ± 13%, and 43.2 ± 16%, respectively. E. coli saw log-reductions ranging from -1.3 — 3.0 on the terrace, and -1.0 — 1.8 in the creek. Oregon Water Quality Criteria were consistently met at the two in-stream sites on Carli Creek for E. coli with one exception, and for dissolved cadmium, lead, zinc, and copper (with one exception for copper). However, dissolved total solids at the downstream Carli Creek site was above the Willamette River guidance value 100 mg/L roughly 71% of the time. The precipitation record during the study was useful for explaining certain pollutant reductions, as several mechanisms are driven by physical processes, however it was not definitive. The historic rain/snow/ice event in mid-February 2021 appeared to impact mass-based reductions for all metals. Qualitatively, precipitation seemed to have the largest effect on nutrient dynamics, specifically ammonia-nitrogen. Determining exact mechanisms of pollutant removals was outside the scope of this study. An improved flow record, more targeted storm sampling, or more comprehensive nutrient profiles could aid in answering important questions on dominant mechanisms of this new constructed wetland. This study is useful in establishing a framework and baseline for understanding this one-of-a-kind regional stormwater treatment project and pursuing further questions in the future.
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