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Artykuły w czasopismach na temat "Water temperature"
Martin, Lorenz, Marc Schneebeli i Christian Mätzler. "Tropospheric water and temperature retrieval for ASMUWARA". Meteorologische Zeitschrift 15, nr 1 (27.02.2006): 37–44. http://dx.doi.org/10.1127/0941-2948/2006/0093.
Pełny tekst źródłaL., Jaya Sekhar. "Automatic Temperature Monitoring and Controlling Water Supply System". International Journal of Psychosocial Rehabilitation 24, nr 5 (20.04.2020): 2781–87. http://dx.doi.org/10.37200/ijpr/v24i5/pr201981.
Pełny tekst źródłaZhu, Bei, Shiyan Wang, Chang Liu, Wei Su, Jiapeng Wu, Cunwu Li i Jingshi Shang. "Impacts of Discharged Low-Temperature Water on Water Table and Temperature in the Riparian Zone". Nature Environment and Pollution Technology 21, nr 1 (6.03.2022): 141–48. http://dx.doi.org/10.46488/nept.2022.v21i01.015.
Pełny tekst źródłaNarins, Rhoda S. "Water Temperature Changes". Dermatologic Surgery 25, nr 5 (maj 1999): 422. http://dx.doi.org/10.1046/j.1524-4725.1999.09995-2.x.
Pełny tekst źródłaQUAN, LINDA, i KIM R. WENTZ. "Water Temperature and Drowning". Pediatrics 87, nr 5 (1.05.1991): 747–48. http://dx.doi.org/10.1542/peds.87.5.747a.
Pełny tekst źródłaCrisp, D. T. "Water temperature of Plynlimon streams". Hydrology and Earth System Sciences 1, nr 3 (30.09.1997): 535–40. http://dx.doi.org/10.5194/hess-1-535-1997.
Pełny tekst źródłaTenuzzo, Lorenzo, Gaia Camisasca i Paola Gallo. "Protein-Water and Water-Water Long-Time Relaxations in Protein Hydration Water upon Cooling—A Close Look through Density Correlation Functions". Molecules 25, nr 19 (7.10.2020): 4570. http://dx.doi.org/10.3390/molecules25194570.
Pełny tekst źródłaLiu, Wendi, Yan Yang, Qunke Xia, Yu Ye, Zhongping Wang, Peipei Zhang i Guowu Li. "Water decreases displacive phase transition temperature in alkali feldspar". European Journal of Mineralogy 30, nr 6 (20.12.2018): 1071–81. http://dx.doi.org/10.1127/ejm/2018/0030-2775.
Pełny tekst źródłaPavlovic, Marko, Alexander Plucinski, Lukas Zeininger i Bernhard V. K. J. Schmidt. "Temperature sensitive water-in-water emulsions". Chemical Communications 56, nr 50 (2020): 6814–17. http://dx.doi.org/10.1039/d0cc02171g.
Pełny tekst źródłaVerma, Priyanka, i Khushboo Thapliyal. "Diatom Analysis in Thermophilic water bodies: A Study on Hot Water Springs of Madhya Pradesh". Indian Journal of Forensic Medicine and Pathology 16, nr 2 (15.06.2023): 133–43. http://dx.doi.org/10.21088/ijfmp.0974.3383.16223.6.
Pełny tekst źródłaRozprawy doktorskie na temat "Water temperature"
Dudd, Lucinda M. "Organic chemistry in high-temperature water". Thesis, Nottingham Trent University, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.403413.
Pełny tekst źródłaMcNeill, Laurie S. "Water Quality Factors Influencing Iron and Lead Corrosion in Drinking Water". Diss., Virginia Tech, 2000. http://hdl.handle.net/10919/28242.
Pełny tekst źródłaPh. D.
Chinnaswamy, Arulmani. "Water vapour and sea surface temperature retrievals". Thesis, University of Reading, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270328.
Pełny tekst źródłaWhelton, Andrew James. "Temperature Effects on Drinking Water Odor Perception". Thesis, Virginia Tech, 2001. http://hdl.handle.net/10919/36221.
Pełny tekst źródłaThirteen volunteer panelists were trained according to Standard Method 2170, flavor profile analysis (FPA). Following training these panelists underwent triangle test screening to determine whether or not they could detect the odorants used in this study. Following triangle testing, panelists underwent directional difference testing to determine if temperature affected odor perception when presented with two water samples. Following directional difference testing, panelists used FPA and evaluated water samples that contained odorants at either 25°C or 45°C. Samples containing geosmin cooled to 5°C were also evaluated.
Sensory analyses experiments indicate that odor intensity is a function of both aqueous concentration and water temperature for geosmin, MIB, nonadienal, n-hexanal, free chlorine, and 1-butanol. The higher water temperature resulted in an increase in odor intensity for some, but not all, concentrations of geosmin, 2-methylisoborneol, trans-2, cis-6-nonadienal, n-hexanal, free chlorine, and 1-butanol. Additionally, above 400 ng/L of geosmin, 400 ng/L of MIB, and 100 ng/L the odor intensity was equal to or less than the odor intensity at 600, 600, and 200 ng/L, respectively. Henry's Law should predict that an increase in concentration would increase the amount of odorant the panelist comes into contact with; however, results demonstrated that at specific aqueous odorant concentrations odor perception did not follow Henry's Law. Odor response to drinking water containing isobutanal was affected by concentration but not water temperature.
Master of Science
Rosén, Elin, Andreas Abdelki, Beyar Abdulla, Alan Bugurcu i Nabelsi Mahmoud El. "Oxygenation conducted in low temperature clean water". Thesis, Uppsala universitet, Institutionen för teknikvetenskaper, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-384153.
Pełny tekst źródłaSardo, Rachel. "Anomalous effects while cooling liquid water". Diss., Online access via UMI:, 2007.
Znajdź pełny tekst źródłaTaylor, Diana Jacqueline Falcon. "Temperature insensitive microemulsions". Thesis, University of Hull, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.310404.
Pełny tekst źródłaGryga, Michele E. "Water Temperature Controls in the Sheepscot River, Maine". Thesis, Boston College, 2006. http://hdl.handle.net/2345/414.
Pełny tekst źródłaThe Sheepscot River watershed is 590 km2 located in mid-coast Maine. Two branches comprise the river: the main stem and the West Branch, which merge in North Whitefield before flowing into the Gulf of Maine. The Sheepscot River has an imposed form that is strongly influenced by the Norumberga Fault Zone and it flows through glacial deposits. The watershed has a temperate climate because of its location in mid-latitudes in the northern hemisphere. Water temperatures vary in the Sheepscot River over time and along the length of the river. The temporal and spatial variability of the river is due to air temperature, precipitation, discharge from the Palermo Fish Rearing Station, Long Pond, tree shade, confluence, and drainage area. Analysis of these hypothesized controls revolves around field water temperature measurements made between August 2005 and January 2006 and data collected from the North Whitefield gauging station. Supplementary digital spatial data from the Maine Geographic Information Systems data set were also used. Field measurements were taken at seven sites directly upstream and downstream of assumed controls. Climactic features of the watershed exert the main control over the entire river. Air temperature is the first order controls on water temperatures. Precipitation has some effect on water temperature but of less significance than air temperature. The river system has three areas that are affected by different combinations of the other controls: the upper main stem, the West Branch, and the lower main stem. Discharge from the Palermo Fish Rearing Station is the second major controlling factor of water temperature in the upper main stem. Its buffering effect is diluted downstream. Long Pond also affects the upper main stem by warming the water in the summer and cooling it in the winter. Drainage area explains variability in the West Branch and lower main stem. As drainage area increases downstream, water temperatures are controlled by more integrated factors. As a result of this the West Branch fluctuates more than the main stem because it has a smaller drainage area. Temperatures in the downstream reaches are less sensitive to any single control. Confluence and tree cover exert less influence over the system than other controls
Thesis (BS) — Boston College, 2006
Submitted to: Boston College. College of Arts and Sciences
Discipline: Geology and Geophysics
Discipline: College Honors Program
Parks, Olivia Waverly. "Effect of water temperature on cohesive soil erosion". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/49663.
Pełny tekst źródłaeffect of water temperature on cohesive soil erosion should be explored. The objectives of this study are to: determine the effect of water temperature on the erosion rates of clay; determine how erosion rates vary with clay mineralogy; and, explore the relationship between zeta potential and erosion rate. Samples of kaolinite- and montmorillonite-sand mixtures, and vermiculite-dominated soil were placed in the wall of a recirculating flume channel using a vertical sample orientation. Erosion rate was measured under a range of shear stresses (0.1-20 Pa) for a period of five minutes per shear stress at water temperatures of 12, 20, and 27�"C. The zeta potential was determined for each clay type at the three testing temperatures and compared to mean erosion rates. The kaolinite erosion rate doubled when the temperature increased from 12 to 20�"C, and erosion of vermiculite samples tripled when the temperature increased from 20 to 27�"C. The montmorillonite samples generally eroded through mechanical failure rather than fluvial erosion, and the limited fluvial erosion of the montmorillonite-sand mixture was not correlated with water temperature. The data suggest correlation between zeta potential and erosion rate; however, due to the small sample size (n=3), statistically significant correlation was not indicated. Research should continue to explore the influence of water temperature on cohesive soil erosion to better understand the influence of clay mineralogy. Due to the high degree of variability in cohesive soil erosion, multiple replications should be used in future work. The vertical sample orientation enabled discrimination between fluvial erosion and mass wasting and is recommended for future studies.
Master of Science
Sousa, Magda Catarina Ferreira de. "Water temperature variability analysis along the Espinheiro Channel". Master's thesis, Universidade de Aveiro, 2008. http://hdl.handle.net/10773/2594.
Pełny tekst źródłaO canal do Espinheiro é um dos quatro principais canais da Ria de Aveiro, fazendo a ligação entre o Rio Vouga e o Oceano Atlântico. Nesta zona é onde se dá a mistura entre a água salgada proveniente do oceano e a água doce de origem fluvial. Para fazer a monitorização da temperatura da água no Canal do Espinheiro foi utilizada uma nova tecnologia que consiste num cabo de fibra óptica longitudinal de 10 km de extensão, com 18 sensores de temperatura espaçados de 500 m, desde a embocadura até à foz do Rio Vouga. Resultados de um ano de monitorização da temperatura da água permitiram estudar a sua variabilidade espacial e temporal em função de dois forçamentos principais: maré e condições meteorológicas. A evolução temporal longitudinal da temperatura da água foi estudada, tendo sido aplicadas técnicas matemáticas, tais como: análise espectral, análise espectral cruzada e funções empíricas ortogonais (EOFs). A análise espectral mostra picos de maior energia que surgem nas frequências semi-diurnas e diurnas. Estas frequências podem estar relacionadas com a variação diurna da temperatura do ar e da maré, mostrando a importância das variáveis meteorológicas na modulação da temperatura da água em regiões pouco profundas. A análise espectral cruzada permitiu avaliar o desfasamento temporal entre a temperatura da água e do ar, que varia conforme a profundidade do local. Também permitiu observar que a maré tem uma grande influência na distribuição da temperatura da água, nomeadamente perto da embocadura da laguna. As EOFs mostram que a variabilidade da temperatura da água pode ser explicada maioritariamente pela primeira componente, que está relacionada com a variação anual da temperatura do ar. Os resultados mostram que os dois forçamentos principais (maré e condições meteorológicas) determinam a temperatura da água no interior do canal do Espinheiro. Verifica-se ainda que a distribuição da temperatura da água é influenciada também pela variação sazonal das condições meteorológicas e pelas variações de profundidade do canal, que apresenta zonas de reduzida profundidade. ABSTRACT: The Espinheiro channel is one of the four main branches of Ria de Aveiro, establishing the connection between the Vouga River and the Atlantic Ocean. This zone is where occurs the mixing between the salt water from the ocean and the freshwater from fluvial origin. In order to monitoring the water temperature in the Espinheiro channel a new technology was used, consisting on an optical-fibre longitudinal cable 10 km long with 18 temperature sensors separated by 500 m, from the mouth of the lagoon to the mouth of Vouga River. Results of a one year monitoring of water temperature permitted to study its spatial and temporal variability in terms of two major forcing: tides and meteorological conditions. The temporal evolution of the longitudinal water temperature was studied, and mathematical techniques, such as spectral analysis, cross-spectral analysis and Empirical Orthogonal Functions (EOFs) were applied to the data. The spectral analysis shows high energy peaks in both semidiurnal and diurnal frequencies. These frequencies may be related to the daily variation and tidal forcing, demonstrating the importance of the meteorological variables in the modulation of the water temperature in shallow areas. The cross-spectral analysis permitted to evaluate the time lag between the water and air temperature, which varies depending on the local depth. It also permitted to observe that the tide has a great influence on the water temperature distribution, particularly near the mouth of the lagoon. EOFs show that the variability of the water temperature can be explained by the first component, which is closely related to the annual variation of the air temperature. The results show the importance of the two major forcings (tides and meteorological conditions) that determine the water temperature within the Espinheiro channel. It can also be observed that the water temperature distribution is also influenced by the seasonal variation of meteorological conditions and by the channel’s depth variation, which presents very shallow areas.
Książki na temat "Water temperature"
Theurer, Fred D. Instream water temperature model. Washington, DC: Western Energy and Land Use Team, Division of Biological Services, Research and Development, Fish and Wildlife Service, U.S. Dept. of the Interior, 1985.
Znajdź pełny tekst źródłaCarpenter, Michael C. Water-level fluctuations, water temperatures, and tilts in sandbars-6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93. Tucson, Ariz: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Znajdź pełny tekst źródłaCarpenter, Michael C. Water-level fluctuations, water temperatures, and tilts in sandbars-6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93. Tucson, Ariz: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Znajdź pełny tekst źródłaCarpenter, Michael C. Water-level fluctuations, water temperatures, and tilts in sandbars-6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93. Tucson, Ariz: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Znajdź pełny tekst źródłaCarpenter, Michael C. Water-level fluctuations, water temperatures, and tilts in sandbars-6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93. Tucson, Ariz: U.S. Geological Survey, 1995.
Znajdź pełny tekst źródłaCarpenter, Michael C. Water-level fluctuations, water temperatures, and tilts in sandbars-6.5R, 43.1L, and 172.3L, Grand Canyon, Arizona, 1990-93. Tucson, Ariz: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Znajdź pełny tekst źródłaService, Canada Atmospheric Environment. Great Lakes surface water temperature climatology. Ottawa: Environment Canada., 1992.
Znajdź pełny tekst źródłaWashington (State). Dept. of Ecology., red. New temperature criteria for fresh water. [Olympia, Wash.]: Dept. of Ecology., 2002.
Znajdź pełny tekst źródłaWashington (State). Dept. of Ecology., red. Revised temperature criteria for fresh water. [Olympia, Wash.]: Washington State Dept. of Ecology, 2002.
Znajdź pełny tekst źródłaDyar, T. R. Stream-temperature characteristics in Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.
Znajdź pełny tekst źródłaCzęści książek na temat "Water temperature"
Gooch, Jan W. "Cangle Water Temperature". W Encyclopedic Dictionary of Polymers, 113. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_1886.
Pełny tekst źródłaBoyd, Claude E. "Solar Radiation and Water Temperature". W Water Quality, 21–39. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-23335-8_2.
Pełny tekst źródłaCastro, Lina, i Jorge Gironás. "Precipitation, Temperature and Evaporation". W World Water Resources, 31–60. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-56901-3_3.
Pełny tekst źródłaWang, Chi-Yuen, i Michael Manga. "Temperature and Composition Changes". W Earthquakes and Water, 97–115. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-00810-8_6.
Pełny tekst źródłaBonacci, Ognjen. "Water Temperature in Karst". W Karst Hydrology, 141–49. Berlin, Heidelberg: Springer Berlin Heidelberg, 1987. http://dx.doi.org/10.1007/978-3-642-83165-2_8.
Pełny tekst źródłaRaney, F. C., i Yoshiaki Mihara. "Water and Soil Temperature". W Irrigation of Agricultural Lands, 1024–36. Madison, WI, USA: American Society of Agronomy, 2015. http://dx.doi.org/10.2134/agronmonogr11.c58.
Pełny tekst źródłaBenedini, Marcello, i George Tsakiris. "Temperature Dependence". W Water Quality Modelling for Rivers and Streams, 87–89. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5509-3_8.
Pełny tekst źródłaChristy, John R. "Measuring Global Temperature". W Handbook of Weather, Climate, and Water, 869–83. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2004. http://dx.doi.org/10.1002/0471721603.ch46.
Pełny tekst źródłaOverdieck, Dieter. "Water Use Efficiency and Stomatal Conductance". W CO2, Temperature, and Trees, 57–64. Singapore: Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-1860-2_5.
Pełny tekst źródłaZachariassen, Karl Erik. "The Water Relations of Overwintering Insects". W Insects at Low Temperature, 47–63. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4757-0190-6_3.
Pełny tekst źródłaStreszczenia konferencji na temat "Water temperature"
Weckström, Thua. "Comparison of Water Triple Point Cells in Finland". W TEMPERATURE: Its Measurement and Control in Science and Industry; Volume VII; Eighth Temperature Symposium. AIP, 2003. http://dx.doi.org/10.1063/1.1627130.
Pełny tekst źródłaChen, Huey-Long, A. Ramachandra Rao i Miki Hondzo. "Segmentation on Temperature Gradient Microstructure Data". W 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)230.
Pełny tekst źródłaTsai, Shu-Fei. "Studies on the Behavior of Water Triple-Point Cells". W TEMPERATURE: Its Measurement and Control in Science and Industry; Volume VII; Eighth Temperature Symposium. AIP, 2003. http://dx.doi.org/10.1063/1.1627129.
Pełny tekst źródłaSano, Asami. "Determination of Stability Filed of Delta-AlOOH Under High Pressure and Temperature". W WATER DYANMICS: 3rd International Workshop on Water Dynamics. AIP, 2006. http://dx.doi.org/10.1063/1.2207098.
Pełny tekst źródłaBezerra, Karolina, Lidia Gonzalez, Jose Machado, Vitor Carvalho, Filomena Soares i Demetrio Matos. "Smartbath: Water temperature control system". W 2017 International Conference on Engineering, Technology and Innovation (ICE/ITMC). IEEE, 2017. http://dx.doi.org/10.1109/ice.2017.8279991.
Pełny tekst źródłaMahbob, Ahmad Johan, Mahanijah Md Kamal i Faieza Hanum Yahaya. "Water temperature using fuzzy logic". W Its Applications (CSPA). IEEE, 2009. http://dx.doi.org/10.1109/cspa.2009.5069253.
Pełny tekst źródłaWu, Rong. "Water temperature distribution of bathtub". W 2016 2nd Workshop on Advanced Research and Technology in Industry Applications (WARTIA-16). Paris, France: Atlantis Press, 2016. http://dx.doi.org/10.2991/wartia-16.2016.124.
Pełny tekst źródłaGong, Mengyuan, i Zhou Ye. "Reservoir water temperature numerical simulation". W International Conference on Statistics, Applied Mathematics, and Computing Science (CSAMCS 2021), redaktorzy Ke Chen, Nan Lin, Romeo Meštrović, Teresa A. Oliveira, Fengjie Cen i Hong-Ming Yin. SPIE, 2022. http://dx.doi.org/10.1117/12.2628410.
Pełny tekst źródłaST-HILAIRE, ANDRÉ, CLAUDINE BOYER, NORMAND BERGERON i ANIK DAIGLE. "WATER TEMPERATURE MONITORING IN EASTERN CANADA: A CASE STUDY FOR NETWORK OPTIMIZATION". W WATER POLLUTION 2018. Southampton UK: WIT Press, 2018. http://dx.doi.org/10.2495/wp180251.
Pełny tekst źródłaJensen, Mark R., i Cynthia L. Lowney. "Temperature Modeling with HEC - RAS". W World Water and Environmental Resources Congress 2004. Reston, VA: American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40737(2004)404.
Pełny tekst źródłaRaporty organizacyjne na temat "Water temperature"
Xu, Hui, Judith Lattimer, Yamini Mohan i Steve McCatty. High-Temperature Alkaline Water Electrolysis. Office of Scientific and Technical Information (OSTI), wrzesień 2020. http://dx.doi.org/10.2172/1826376.
Pełny tekst źródłaSamson P. i C. Karns. Water Temperature vs. BtA Stability Explored. Office of Scientific and Technical Information (OSTI), wrzesień 2000. http://dx.doi.org/10.2172/1061620.
Pełny tekst źródłaMartin, Sandra K., i Stacy E. Howington. Wynoochee Dam Water Temperature Control Study. Fort Belvoir, VA: Defense Technical Information Center, sierpień 1990. http://dx.doi.org/10.21236/ada226764.
Pełny tekst źródłaVAN KATWIJK, C. Ashcroft temperature switch and thermowell - tempered water cask inlet high temperature. Office of Scientific and Technical Information (OSTI), maj 1999. http://dx.doi.org/10.2172/782341.
Pełny tekst źródłaWeissinger, Rebecca, i Carolyn Hackbarth. Water quality in the Northern Colorado Plateau Network: Water years 2019?2022. National Park Service, 2024. http://dx.doi.org/10.36967/2304433.
Pełny tekst źródłaMark D. McKay. Water Power Calculator Temperature and Analog Input/Output Module Ambient Temperature Testing. Office of Scientific and Technical Information (OSTI), luty 2011. http://dx.doi.org/10.2172/1023475.
Pełny tekst źródłaBrill, Thomas B. Energetics Solids Degradation in High Temperature Water. Fort Belvoir, VA: Defense Technical Information Center, lipiec 1992. http://dx.doi.org/10.21236/ada255679.
Pełny tekst źródłaHunter, J. A., P. J. Kurfurst i S. M. Birk. Water - Column Temperature, Salinity and Conductivity Measurements. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132224.
Pełny tekst źródłaRana B. Gupta. Water Recycling removal using temperature-sensitive hydronen. Office of Scientific and Technical Information (OSTI), październik 2002. http://dx.doi.org/10.2172/816026.
Pełny tekst źródłaDavila, Alejandro, Carmen Cejudo Marmolejo i Katherine LM Stoughton. Domestic Hot Water Temperature Maintenance Technology Review. Office of Scientific and Technical Information (OSTI), sierpień 2021. http://dx.doi.org/10.2172/1813897.
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