Gotowe bibliografie tematyczne / Water temperature

Gotowa bibliografia na temat „Water temperature”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 30 lipca 2024

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Artykuły w czasopismach na temat "Water temperature"

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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.

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L., 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.

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Zhu, 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.

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We observed the water level and temperature in the lower stretch of the Hsin-an river in China for different times to show the characteristics of the water table and temperature in the riparian zone under the influence of discharged low-temperature water. The water table in the riparian zone showed a typical daily cycle change with a fluctuation range of 239.42-275.99 cm, according to the findings. With increasing distance from the river, the amplitudes of the water table fluctuation were reduced, and the phases were lagged. In the high-temperature period, riparian temperatures range from 20.4°C to 26.0°C, whereas in the low-temperature phase, temperatures range from 12.9°C to 19.2°C. The temperature distribution in the riparian zone was described in the vertical direction as “warmer on the surface and cooler at the bottom” during high-temperature periods and “cooler on the surface and warmer at the bottom” during low-temperature periods, with the temperature gradient gradually decreasing with depth. There was clear temperature zonation in the horizontal direction during the high-temperature phase but none during the low-temperature period. The study will serve as a benchmark for future hyporheic zone ecological impact assessments.
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Narins, 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.

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QUAN, 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.

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In Reply.— Dr Nichter et al propose that the normal or mildly impaired survival of five asystolic children in our series was due to the rapid induction of hypothermia by the cold waters of the Puget Sound area. However, we reported that hypothermia (rectal temperature <34°C) was not associated with increased survival. In addition, the data in the Table show that none of these five children experienced cold-water submersions. The ambient temperatures and thus possibly swimming pool temperatures in this temperate area's summers are certainly less warm than Florida's.
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Crisp, 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.

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Abstract. Water temperature data were collected from five stations in the upper Severn system. Temperatures were compared between a stream with a 335 ha catchment after it had flowed for c. 1.5 km through clear felled land and a stream with a 347 ha catchment after it had flowed for c. 2.5 km through coniferous forest. The results suggest that the effect of forest cover was to lower the annual mean water temperature by c. 0.4°C, mainly in summer and through depression of both daily maxima and daily minima, though mainly the former. There was no clear evidence of temperature elevation in the afforested stream in winter. It is important to note that these conclusions depend on several assumptions that cannot be substantiated objectively. There is some evidence that water temperatures in some parts of the upper Severn system may be influenced by groundwater inputs.
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Tenuzzo, 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.

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We report results on the translational dynamics of the hydration water of the lysozyme protein upon cooling obtained by means of molecular dynamics simulations. The self van Hove functions and the mean square displacements of hydration water show two different temperature activated relaxation mechanisms, determining two dynamic regimes where transient trapping of the molecules is followed by hopping phenomena to allow to the structural relaxations. The two caging and hopping regimes are different in their nature. The low-temperature hopping regime has a time scale of tenths of nanoseconds and a length scale on the order of 2–3 water shells. This is connected to the nearest-neighbours cage effect and restricted to the supercooling, it is absent at high temperature and it is the mechanism to escape from the cage also present in bulk water. The second hopping regime is active at high temperatures, on the nanoseconds time scale and over distances of nanometers. This regime is connected to water displacements driven by the protein motion and it is observed very clearly at high temperatures and for temperatures higher than the protein dynamical transition. Below this temperature, the suppression of protein fluctuations largely increases the time-scale of the protein-related hopping phenomena at least over 100 ns. These protein-related hopping phenomena permit the detection of translational motions of hydration water molecules longly persistent in the hydration shell of the protein.
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Liu, 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.

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Pavlovic, 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.

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Temperature sensitive water-in-water (W/W) emulsions are described utilizing the thermal induced conformation change of tailored thermoresponsive block copolymers to reversibly stabilize and destabilize water–water interfaces.
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Verma, 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.

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INTORDUCTION: This study was done with the objective to study the presence of various species of diatoms present in the thermophilic water bodies of Madhya Pradesh (Anhoni and ChavalPani). And to determine the correlation of physiological variables such as temperature and pH to the diatom density. METHODOLOGY: For the detection of diatom species in the water samples acid digestion method was used.50 ml of sample was taken and 10 ml of concentrated nitric acid (HNO3) was added. The sample is then kept undisturbed for 24 hours. The sample was then centrifuged for 10 minutes at 3000rpm 3 times. The palettes formed were suspended in distilled water and centrifuged at 3000 rpm to remove acid content. The palettes are then transferred onto a clean and dry slide and are dried by keeping them on a hot plate at 30-40 C for 4-5 minutes. This slide is then observed under a phase contrast microscope and pictures are taken of varied diatom species using the attached camera. OBSERVATIONS AND RESULTS: The analysis in our research concluded that there are various diatoms present in these thermal water springs belonging to the class Bacillariophyceae, Mediophyceae and Fragiariophyceae. The diatoms that were viewed and captured under Phase contrast microscope were, Nitzschiapalea, Nitzschialinearis, Discostellastelligera, Achnanthidium Sp., Tabularia Sp., Anomoeoneissphaerophora, Amphipleura Sp., Tryblionella Sp., Fragilariacrotonensis., and Nitzschiafi liformis The research lead us to the results that hot water springs that had lower temperatures had more percentage of diatom density as compared to the hot water springs with higher temperatures. According to our research 60% of the diatomsfound were from the geothermal spring of Anhoni, Madhya Pardesh which had a lower temperature while the geothermal spring at Chawalpani, Madhya Pradesh was found to have lower diatom density due to its high temperatures and low nutrient index. When the pH of these water samples was studied against the diatom density, no signifi cant diff erence was found due to the nominal range diff erence in pH. Yet geothermal springs had a 10% more diatom density at a low pH level which is 5 in this case study. This research leads to certain crucial conclusions that gave us strong evidence for co-relation amidst temperature, pH and diatoms. Conclusion: Geothermal springs are a habitat to many diatom species. These diatom species are specifi c to a particular site and are used in cases of drowning death for leads. On extraction and analysis of these diatoms we can detect and compare them to the standard diatoms present in the water sources of that area. This helps Forensic Scientist fi nds leads in any case of death due todrowning. the analysis in our research concludes the presence of diatom species in the geothermal springs of Madhya Pradesh, namely Anhoni and Chawalpani. These diatoms include species belonging to class of Bacillariophyceae, Mediophyceae and Fragilariophyceae. it also establishes the correlation between the temperature, pH and diatom density of these geothermal springs. It can be concluded that the geothermal springs that have lower temperature and pH are prove tohave higher diatom density and diversity as compared to the ones with higher temperature.
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Rozprawy doktorskie na temat "Water temperature"

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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.

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McNeill, Laurie S. "Water Quality Factors Influencing Iron and Lead Corrosion in Drinking Water". Diss., Virginia Tech, 2000. http://hdl.handle.net/10919/28242.

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Corrosion is one of the most complicated and costly problems facing drinking water utilities. Corrosion of iron pipes can lead to economic losses and customer complaints, while lead corrosion poses a serious health risk. This work first synthesizes nearly 100 years of iron corrosion research to provide the water industry with an updated understanding of factors that influence iron pipe corrosion including water quality and composition, flow conditions, biological activity, and corrosion inhibitors. Potential impacts of upcoming regulations on iron corrosion are also considered. Next, a four-year study is presented that evaluated the effect of water quality and phosphate inhibitors on the corrosion of iron pipes under extended stagnant water conditions. Surprisingly, many of the water quality parameters traditionally thought to influence iron corrosion were not controlling under these "worst case" stagnant conditions. Moreover, addition of phosphate inhibitors often had either no statistically significant effect or actually increased iron concentration, scale build-up and overall weight loss. Temperature is often overlooked when corrosion of distribution systems pipes is considered. Temperature impacts many parameters that are critical to pipe corrosion including physical properties of the solution, thermodynamic and physical properties of corrosion scale, chemical rates, and biological activity. Moreover, variations in temperature and temperature gradients may give rise to new corrosion phenomena worthy of consideration by water treatment personnel. In laboratory experiments, cast iron samples at 5° C had 23% more weight loss, ten times higher iron release to water, and twice as much tuberculation compared to samples at 25°C. For lead corrosion, hexametaphosphate inhibitors were proven to increase release of both particulate and soluble lead to drinking water by 200 - 3500% over a wide range of water qualities when compared to orthophosphate, effectively ending a long term debate as to their impacts. Utilities should consider these adverse effects whenever polyphosphate is used to prevent scaling or iron precipitation.
Ph. D.
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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.

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Whelton, Andrew James. "Temperature Effects on Drinking Water Odor Perception". Thesis, Virginia Tech, 2001. http://hdl.handle.net/10919/36221.

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Thirteen 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.


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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.

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Aeration tests were conducted under non-standard conditions with clean tap water in various temperatures below 20 °C, with the aim of studying changes that may occur. An initial deoxygenation of 0.8 litre water was performed with sodium sulfite and a cobalt catalyst pre-dissolved in water, in order to bind already present dissolved oxygen. The resulting dissolved oxygen concentration after 20 minutes did not decrease below 2 mg/L, despite increasing the sodium sulfite concentrations. Thereafter, a reoxygenation with the same time interval was conducted by using an aeration system, which resulted in an increase of saturated oxygen concentration with lower temperatures. pH-measurements were carried out during the whole experiment in order to follow the conversion of sulfite to sulfate. The pH-data obtained confirmed that sulfite had been converted to sulfate, although, a few deviations could be observed for most of the experiments. The conductivity was also measured to ensure that the sulfite had been properly dissolved when added to the water tank. In general, the conductivity never deviated and held a constant trend throughout the tests. The collected data could not be made of use in order to properly determine how the aeration, for temperatures below 20 °C, could be evaluated. Further tests have to be performed in order for a definite conclusion to be drawn.
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Sardo, Rachel. "Anomalous effects while cooling liquid water". Diss., Online access via UMI:, 2007.

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Taylor, Diana Jacqueline Falcon. "Temperature insensitive microemulsions". Thesis, University of Hull, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.310404.

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Gryga, Michele E. "Water Temperature Controls in the Sheepscot River, Maine". Thesis, Boston College, 2006. http://hdl.handle.net/2345/414.

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Thesis advisor: Noah P. Snyder
The 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
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Parks, Olivia Waverly. "Effect of water temperature on cohesive soil erosion". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/49663.

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In light of increased stream temperatures due to urbanization and climate change, the
effect 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.
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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.

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Mestrado em Meteorologia e Oceanografia Física
O 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.
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Książki na temat "Water temperature"

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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.

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Carpenter, 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.

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Carpenter, 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.

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Carpenter, 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.

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Carpenter, 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.

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Carpenter, 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.

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Service, Canada Atmospheric Environment. Great Lakes surface water temperature climatology. Ottawa: Environment Canada., 1992.

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Washington (State). Dept. of Ecology., red. New temperature criteria for fresh water. [Olympia, Wash.]: Dept. of Ecology., 2002.

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Washington (State). Dept. of Ecology., red. Revised temperature criteria for fresh water. [Olympia, Wash.]: Washington State Dept. of Ecology, 2002.

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Dyar, T. R. Stream-temperature characteristics in Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

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Części książek na temat "Water temperature"

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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.

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Boyd, 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.

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Castro, 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.

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Wang, 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.

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Bonacci, 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.

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Raney, 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.

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Benedini, 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.

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Christy, 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.

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Overdieck, 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.

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Zachariassen, 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.

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Streszczenia konferencji na temat "Water temperature"

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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.

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Chen, 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.

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Tsai, 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.

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Sano, 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.

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Bezerra, 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.

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Mahbob, 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.

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Wu, 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.

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Gong, 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.

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ST-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.

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Jensen, 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.

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Raporty organizacyjne na temat "Water temperature"

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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.

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Samson 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.

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Martin, 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.

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VAN 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.

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Weissinger, 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.

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Water quality monitoring in National Park Service units of the Northern Colorado Plateau Network (NCPN) is made possible through partnerships between the National Park Service Inventory & Monitoring Division, individual park units, the U.S. Geological Survey, and the Utah Department of Environmental Quality. This report evaluates water quality data from site visits at 42 different locations within and around eight park units in Utah and Colorado from October 1, 2018 through September 30, 2022. Data are compared to state water quality standards for the purpose of providing information to park managers about potential water quality problems. Parks included for evaluation are Arches National Park (NP), Bryce Canyon NP, Canyonlands NP, Capitol Reef NP, Dinosaur National Monument (NM), Hovenweep NM, Timpanogos Cave NM, and Zion NP. Evaluation of water quality parameters relative to state water quality standards indicated that 21,644 (96.8%) of the 22,356 total designated beneficial-use evaluations completed for the period covered in this report met state water quality standards. The most common parameters that did not meet a standard include fecal indicator bacteria (Escherichia coli), water temperature, and total dissolved solids (TDS). While TDS can be an indicator of pollution, in NCPN parks, it mostly occurs downstream of rock outcrops that naturally increase TDS in streams. Phosphorus concentrations were often greater than acceptable thresholds but were rarely associated with indicators of impairment such as algal blooms, fish kills, or low dissolved oxygen. Sites monitored in Arches NP, Bryce Canyon NP, Capitol Reef NP, Dinosaur NM, Hovenweep NM, and Zion NP all had occurrences when fecal indicator bacteria concentrations were greater than associated state standards. State-coordinated plans to reduce waste contamination are in place for the North Fork Virgin River (Zion NP) and the Fremont River (Capitol Reef NP). The plans have resulted in a decrease in the number of chronic and acute standard violations at Zion. Elevated water temperatures occurred at sites in Canyonlands NP, Capitol Reef NP, and Zion NP. Water temperature is strongly correlated with air temperature in surface waters across the Colorado Plateau. Additional issues of management concern include low dissolved oxygen in Salt Wash at Wolfe Ranch (Arches NP) and Square Tower Spring (Hovenweep NM), as well as selenium in the Colorado River (Arches NP and Canyonlands NP). State-coordinated plans to reduce selenium concentrations in the Upper Colorado River basin are in place.
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Mark 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.

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Brill, 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.

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Hunter, 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.

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Rana 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.

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Davila, 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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