Relevant bibliographies by topics / Rewetting

Academic literature on the topic 'Rewetting'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 April 2022

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Journal articles on the topic "Rewetting"

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Chan, S. H., J. D. Blake, T. R. Shen, and Y. G. Zhao. "Effects of Gravity on Rewetting of Capillary Groove Surface at Elevated Temperatures—Experimental and Theoretical Studies." Journal of Heat Transfer 117, no. 4 (November 1, 1995): 1042–47. http://dx.doi.org/10.1115/1.2836279.

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Theoretical and experimental investigations of the rewetting characteristics of thin liquid films over heated and unheated capillary grooved plates were performed. To investigate the effect of gravity on rewetting, the grooved surface was placed in upward and downward-facing positions. Profound gravitational effects were observed as the rewetting velocity was found to be higher in the upward than in the downward-facing orientation. The difference was even greater with higher initial plate temperatures. With either orientation, it was found that the rewetting velocity increased with the initial plate temperature. But when the temperature was raised above a rewetting temperature, the rewetting velocity decreased with the initial plate temperature. Hydrodynamically controlled and heat conduction controlled rewetting models were then presented to explain and to predict the rewetting characteristics in these two distinct regions. The predicted rewetting velocities were found to be in good agreement with experimental data with elevated plate temperatures.
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Zheng, Ying Ying, Xin Shan Song, and Xiao Xiang Zhao. "The Effect of Drying-Rewetting on Soil Nitrogen Nitrification." Advanced Materials Research 610-613 (December 2012): 385–89. http://dx.doi.org/10.4028/www.scientific.net/amr.610-613.385.

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More frequently drying-rewetting is likely to be expected for soils this century, with strong effect on nitrogen transformation. Experiments were conducted in semi-disturbed soils which were incubated under 4 different moisture regimes (dry wet\constant wet\constant dry\constant flooded) for 71 d. The results show that the dry soil has a rapid NO3--N increase after rewetting. Drying-rewetting increases soil nitrification which shows a "pulse" increasing. The drying and rewetting soil has the highest nitrification intensity when the soil moisture content (g/g) ranging at 15.82% ~ 17.06%. Drying-rewetting contributes to the accumulation of NO3--N.
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Peterson, G. P., and X. F. Peng. "Experimental Investigation of Capillary-Induced Rewetting in a Flat Porous Wicking Structure." Journal of Energy Resources Technology 115, no. 1 (March 1, 1993): 62–69. http://dx.doi.org/10.1115/1.2905971.

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An experimental program was conducted to investigate the rewetting characteristics of liquid flowing through multiple layers of screen mesh covering a heated vertical plate. Data obtained for acetone and R-11 were analyzed and compared with previously developed theoretical expressions for the rewetting velocity, the maximum liquid rise height, and the maximum heat flux for which rewetting could occur. The experimental results indicate that the thickness of the screen mesh layer and the liquid thermophysical properties are the most important factors affecting the rewetting behavior. As predicted by the theoretical model, small increases in the thickness of the screen layer initially caused the maximum permissible rewetting heat flux to increase. Once the layer thickness had reached a critical value, continued increases resulted in a decrease in the maximum permissible rewetting heat flux.
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Lestari, Iska, Daniel Murdiyarso, and Muh Taufik. "Rewetting Tropical Peatlands Reduced Net Greenhouse Gas Emissions in Riau Province, Indonesia." Forests 13, no. 4 (March 24, 2022): 505. http://dx.doi.org/10.3390/f13040505.

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Draining deforested tropical peat swamp forests (PSFs) converts greenhouse gas (GHG) sinks to sources and increases the likelihood of fire hazards. Rewetting deforested and drained PSFs before revegetation is expected to reverse this outcome. This study aims to quantify the GHG emissions of deforested PSFs that have been (a) reforested, (b) converted into oil palm, or (c) replanted with rubber. Before rewetting, heterotrophic soil respiration in reforested, oil palm, and rubber plantation areas were 48.91 ± 4.75 Mg CO2 ha−1 yr−1, 54.98 ± 1.53 Mg CO2 ha−1 yr−1, and 67.67 ± 2.13 Mg CO2 ha−1 yr−1, respectively. After rewetting, this decreased substantially by 21%, 36%, and 39%. Conversely, rewetting drained landscapes that used to be methane (CH4) sinks converted them into CH4 sources; almost twice as much methane was emitted after rewetting. Nitrous oxide (N2O) emissions tended to decrease; in nitrogen-rich rubber plantations, N2O emissions halved; in nitrogen-poor reforested areas, emissions reduced by up to a quarter after rewetting. Overall, rewetting reduced the net emissions up to 15.41 Mg CO2-eq ha−1 yr−1 (25%) in reforested, 18.36 Mg CO2-eq ha−1 yr−1 (18%) in oil palm, and 28.87 Mg CO2-eq ha−1 yr−1 (17%) in rubber plantation areas.
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Chan, S. H., and W. Zhang. "Rewetting Theory and the Dryout Heat Flux of Smooth and Grooved Plates With a Uniform Heating." Journal of Heat Transfer 116, no. 1 (February 1, 1994): 173–79. http://dx.doi.org/10.1115/1.2910852.

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The evaporation and condensation of thin liquid films are of significant importance in a wide variety of problems ranging from specific applications in the heat pipe field to more general ones in the chemical, nuclear, and petrochemical industries. Although several investigations have been conducted to determine the rewetting characteristics of liquid films on heated rods, tubes, and flat plates, no solutions are yet available to describe the rewetting process of a hot plate subjected to a uniform heating. A model is presented to analyze the rewetting process of such plates with and without grooves. Approximate analytical solutions are presented for the prediction of the rewetting velocity and the transient temperature profiles of the plates. It is shown that the present rewetting velocity solution reduces correctly to the existing solution for the rewetting of an initially hot isothermal plate without heating from beneath the plate. Numerical solutions have also been obtained to validate the analytical solutions. Finally, a simple method is presented to predict the dryout heat flux of a liquid film flowing over a heated smooth or grooved plate. The results of the prediction are found to be in reasonable agreement with the existing experimental data.
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Weislogel, M. M., and S. H. Collicott. "Capillary Rewetting of Vaned Containers: Spacecraft Tank Rewetting Following Thrust Resettling." AIAA Journal 42, no. 12 (December 2004): 2551–61. http://dx.doi.org/10.2514/1.3394.

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Leizeaga, Ainara, Annelein Meisner, Johannes Rousk, and Erland Bååth. "Repeated drying and rewetting cycles accelerate bacterial growth recovery after rewetting." Biology and Fertility of Soils 58, no. 4 (February 7, 2022): 365–74. http://dx.doi.org/10.1007/s00374-022-01623-2.

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AbstractTwo patterns of bacterial growth response upon drying and rewetting (DRW) of soils have previously been identified. Bacterial growth can either start increasing immediately after rewetting in a linear fashion (“type 1” response) or start increasing exponentially after a lag period (“type 2” response). The effect of repeated DRW cycles was studied in three soils with different response patterns after a single DRW cycle (“type 1”, “type 2” with a short lag period and “type 2” with a long lag period). The soils were exposed to seven DRW cycles, and respiration and bacterial growth were monitored after 1, 2, 3, 5, and 7 cycles. Exposure to repeated DRW shifted the bacterial growth response from a “type 2” to a “type 1” pattern, resulting in an accelerated growth recovery to a pre-disturbance growth rate. Bacterial growth in soils that initially had a “type 1” response also tended to recover faster after each subsequent DRW cycle. The respiration patterns after DRW also indicated the same transition from a “type 2” to a “type 1” pattern. Our results show that exposure to repeated DRW cycles will shape the bacterial response to future DRW cycles, which might be mediated by a shift in species composition, a physiological adjustment, evolutionary changes, or a combination of the three.
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Zhang, Yushuai, Baokun Xu, Jiangpei Han, and Liangsheng Shi. "Effects of Drying-Rewetting Cycles on Ferrous Iron-Involved Denitrification in Paddy Soils." Water 13, no. 22 (November 12, 2021): 3212. http://dx.doi.org/10.3390/w13223212.

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Soil moisture status has an important effect on the process of denitrification in paddy soils. However, it is unclear how it affects the ferrous iron-involved denitrification. Here, the influence of drying-rewetting cycles on ferrous iron-involved denitrification in paddy soil were studied with batch experiments. The dynamics of nitrate, ammonia, Fe2+, Fe3+ and total organic carbon (TOC), as well as nitrous oxide (N2O) were investigated using the iron-rich paddy soil in Jiangxi province, South China. Results demonstrated that the denitrification rate dropped while ammonia nitrogen content (NH4+-N) showed a rapid accumulation in the drying period. In the rewetting period, organic carbon played two-side roles. Organic carbon and ferrous iron together provided electron donors to denitrification, and organic carbon simultaneously reduced ferric iron under anaerobic environment. There were complex interactions among organic carbon, nitrate and Fe2+/Fe3+ under drying-rewetting cycles. Soil rewetting led to denitrification flush, especially after a moderately long drying period, while excessively frequent drying-rewetting alternation was not favorable to nitrate denitrification.
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Kumar, M., and D. Mukhopadhyay. "Heat transfer characterization under radial jet and falling film induced rewetting." Kerntechnik 86, no. 5 (October 1, 2021): 325–37. http://dx.doi.org/10.1515/kern-2021-0013.

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Abstract Empirical correlations are developed for rewetting velocity and maximum heat transfer coefficient during rewetting phase of single hot vertical Fuel Pin Simulator (FPS) by using radial jet impingement and falling film. Emergency Core Cooling System (ECCS) has been designed for Advance Heavy water Reactor (AHWR) to rewet the hot fuel pin under the loss of coolant accident. Coolant injection takes place from a water rod which is located at the center of the fuel bundle in form of jets to rewet hot surface of fuel pin under loss of coolant accident. This kind of design to reflood the fuel bundle is different than bottom and top spray reflooding practiced in PWR and BWR type of nuclear reactors. There are two different kinds of rewetting found during radial jet induced cooling. The first one is due to radial jet impingement and the second one is due to falling film which is below the jet impingement point. Rewetting velocity has been predicted along the length of fuel pin due to radial jet impingement cooling. Temperature of FPS has been varied from 400°C to 700°C with help of different powers supply, simulating decay heat of reactor. A variation of coolant radial jet mass flow rate is from 0.5 lpm to 1.8 lpm. It is considered during ECCS injection. It has been observed from the experiments that rewetting velocity decreases with increasing the clad surface temperature and increases with increasing the coolant mass flow rate. The rewetting velocity in falling film is found to be nearly 1.8 times higher than rewetting velocity predicted in circumferential direction. Further, it is found that maximum heat transfer coefficient increases with increasing the radial jet coolant mass flow rate. The maximum heat transfer coefficient in case of radial jet impingement is found to be nearly 1.5 times the falling film rewetting. Developed correlation predicts the maximum heat transfer coefficient with experimental data well within the error band of ±10%.
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Ouenzerfi, Safouene, Souad Harmand, and Jesse Schiffler. "Leidenfrost Self-Rewetting Drops." Journal of Physical Chemistry B 122, no. 18 (April 19, 2018): 4922–30. http://dx.doi.org/10.1021/acs.jpcb.7b11944.

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Dissertations / Theses on the topic "Rewetting"

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Ilyas, Muhammad. "Rewetting processes during PWR reflood." Thesis, Imperial College London, 2011. http://hdl.handle.net/10044/1/6378.

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Rewetting of heated surfaces is important in many physical processes and has important technological applications. Understanding of this phenomenon is required in many engineering and scientific fields. It is one of the most crucial phenomena to be considered for the safety analysis of the design basis Loss‐of‐Coolant Accident (LOCA) in light water reactors (Pressurized Water and Boiling Water Reactors). To mitigate the consequences of LOCA, water is fed into the reactor core via an emergency core cooling system; in the PWR, this water is fed to the core via the lower plenum (“bottom reflooding”) and in the BWR, this water is sprayed onto the top of the core (“top reflooding”). In both the cases, a quench front is formed which moves rather slowly. Ahead of quench front, complex and chaotic processes are occurring over a very small axial region where high temperature gradient exists. The heat transfer mechanism is not well known in this region. In this work, the detailed physics of the rewetting processes has been investigated both theoretically and experimentally. The thermal hydraulic behaviour of hot vertical channels during emergency core cooling conditions would be expected to be flow direction‐dependent, it was important to consider the two cases (top reflooding and bottom reflooding) separately. It was possible for the first time, to the author’s knowledge, to apply the fast response infra‐red thermal imaging system to study the rewetting process during top and bottom reflooding of heated vertical surfaces. The important contribution of this work was the use of this new technology to sense the variation of temperature with time at multiple nearby locations at the quench front. In the top reflood experiments, a heated stainless steel pate was quenched by a falling film flow. Through an infrared‐transparent substrate embedded in the plate and coated with platinum, temperature measurements at a location near the rewetting front were achieved using infrared thermal imaging system. The temperature/time traces showed fluctuations in temperature indicating occurrence of intermittent contacts at the quench front. A high speed video camera was also employed to capture rewetting processes by the visual observation of the rewetting front from the top surface. In the visual observations, the liquid film has been seen making intermittent contacts with the hot surface. In these experiments, the effect of the flow rate and the degree of sub‐cooling of the feed liquid has been studied. The rewetting temperature and the characteristic length of the intermittent contact region have been deduced from the experimental results. Experiments were also done to measure temperature changes at the rewetting front for the case of bottom reflooding of a heated tube using a similar technique to that employed for the studies of top reflooding. The results suggested that the rewetting behaviour was different depending on whether the reflood rate was high or low. For high reflood rate, the observations are consistent with the regime above the rewetting front being of the inverted annular type and, for lower reflooding rates, the results are consistent with the rewetting front corresponding to a film dryout in annular flow. An important finding from these experiments is the identification of transient temperature fluctuations in the transition region for the high flooding rate case. These are similar to those observed in the top reflood case and it seems very likely that these fluctuations are associated with intermittent wetting of the surface in this region. An attempt has been made to model rewetting phenomena in which the mechanism of heat transfer at the quench has been proposed. The postulated mechanism is transient near‐surface cooling resulting from intermittent solid‐liquid contacts, followed by recovery of the surface temperature of the metal substrate, with explosive vaporization occurring when the homogeneous nucleation temperature is restored at the metal‐water interface. A one‐dimensional rewetting model was constructed to explain the cyclical process; this model predicted the cyclical behaviour, with the expected qualitative dependence on system parameters. Its predictions are quantitatively consistent with experimental observation, in that the unsteady model analysis brackets the experimentally observed periodicity of the quasi‐steady actual process. The one‐dimensional model of the process has been complemented by twodimensional simulations using a commercial finite element code (ANSYS). In these simulations, an intermittent contact region has been modelled by imposing a heat transfer coefficient over a certain length between dry and wet regions. A parametric study was performed to see the effect of the rewetting velocity, the wet side heat transfer coefficient, intermittent contact heat transfer coefficient, and the length of intermittent contact region.
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Mao, Chris Qun. "Local rewetting and distortion of paper." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp05/MQ62919.pdf.

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Pereira, Paulo Manuel Sendim Aires. "Heat transfer in rewetting of hot surfaces." Thesis, Imperial College London, 1998. http://hdl.handle.net/10044/1/7284.

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Engelhardt, Ilonka. "Impact of changing precipitation patterns on the plant-microbial response to rewetting." Thesis, Bourgogne Franche-Comté, 2018. http://www.theses.fr/2018UBFCK017/document.

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La disponibilité en eau exerce un contrôle majeur sur les cycles des nutriments terrestres, à travers ses impacts sur le fonctionnement des plantes et des microorganismes du sol. Les changements de magnitude et de fréquence des épisodes de pluie (c’est-à-dire les régimes de précipitations) prédits par les modèles et associés au changement climatique vont ainsi avoir des conséquences importantes sur le fonctionnement des écosystèmes. Les écosystèmes arides et semi-arides sont particulièrement vulnérables à des changements de régime de précipitations, car ils sont déjà contraints par la disponibilité en eau. Cependant, des systèmes plus tempérés peuvent aussi être soumis à des périodes sèches qui peuvent affecter le fonctionnement plante-sol. Dans la présente thèse, les effets d’un historique de régimes de précipitations contrastés ont été étudiés dans des systèmes sol seul et plante-sol, afin de déterminer dans quelle mesure plusieurs semaines de régime hydrique peuvent moduler la réponse des écosystèmes à une réhumectation lors d’un événement pluvieux important. Premièrement, nous avons évalué les effets de régimes de précipitations contrastés dans des mésocosmes de sol seul, sur les communautés bactériennes et fongiques actives et inactives dans le sol, 2 et 5 jours après réhumectation. Nous avons employé une approche de 18O-SIP (stable isotope probing), en réhumectant le sol avec H218O puis en utilisant la métagénomique ciblée sur les bactéries et champignons du sol. Deuxièmement, nous avons mis en place deux expériences séparées en mésocosmes plante-sol avec couvert de blé. La première expérience sol-plante s’est intéressée à la profondeur de sol. Nous avons évalué les effets de régimes de précipitations contrastés sur le flux de C depuis les plantes vers les microorganismes du sol ainsi que la la réponse des microorganismes à différentes profondeurs de sol (de 0 à 35 cm) en utilisant des approches de traceur isotopiques stables (13C-CO2) et 18O-SIP, respectivement. La deuxième expérience plante-sol a évalué les effets de régimes de précipitations contrastés sur la dynamique temporelle (durant 29h) de la réponse du système plante-sol à la réhumectation. En outre, deux niveaux de fertilisation azotée ont permis de déterminer l’éventuelle modulation de la réponse par la disponibilité en N dans le sol. La réponse des communautés bactériennes et fongiques potentiellement actives dans le sol a été évaluée par métagénomique ciblée. La réponse de cycles biogéochimiques a été évaluée à l’aide de traceurs isotopiques stables (13C-CO2 et 15N- NO3-) pour quantifier le flux de C des plantes vers les microorganismes du sol et déterminer la compétition plantes-microorganismes du sol au cours du temps après réhumectation.Nos résultats ont montré un contrôle du régime de précipitation sur la morphologie et physiologie des plantes, les communautés microbiennes du sol ainsi que sur le cycle de l’azote du sol dans nos systèmes. En particulier, des régimes de précipitations peu fréquentes (cycles de périodes sèches longues suivies de périodes de pluie plus importantes) se sont traduits par une augmentation des potentiels de transformation de l’azote dans le sol et une réduction des stocks d’azote minéral dans le sol. Ceci a façonné l’environnement de la réponse de nos systèmes à la réhumectation, que nous avons évaluée en déterminant les dynamiques du C (couplage plantes-microbes et émissions de CO2 du sol), de l’azote du sol (compétition plantes-microorganismes du sol pour le N et émissions de N2O) et de la composition des communautés microbiennes du sol (bactéries et champignons actifs et potentiellement actifs) après réhumectation (...)
Water availability governs terrestrial nutrient cycles by impacting the functioning of both plants and of soil microorganisms. The predicted changes in precipitation patterns (i.e. the magnitude and frequency of precipitation events) associated with climate change, will thus likely have important consequences on ecosystem functioning. Dry and seasonally dry ecosystems are particularly vulnerable to changes in precipitation patterns, as they are already constrained to a large extent by water availability. However, more mesic systems may also experience dry periods that may impact plant-soil functions. In this thesis, experiments in soil-only systems and plant-soil systems were used to gain insight into how the legacy effects of several weeks of exposure to contrasted precipitation patterns set the scene for the rewetting response of the system. First, in an experiment using soil-only mesocosms, we evaluated the effects of contrasting precipitation regimes on the actively growing as well as the inactive bacterial and fungal communities 2 and 5 days after rewetting, using an 18O-SIP (stable isotope probing) approach by applying H218O followed by metagenomics targeting soil bacteria and fungi. Second, we performed two separate and complementary experiments using plant-soil mesocosms with wheat plant cover. The first plant-soil experiment focused on soil depth. It determined the effects of contrasting precipitation patterns on the flux of C from plants to microbes and the microbial response to rewetting at different soil depths, using a heavy isotope tracer approach (13C-CO2) and 18O-SIP with metagenomics respectively. The second plant-soil experiment evaluated the effects of a history of contrasting precipitation patterns on the dynamics of the rewetting response of the plant-soil system over time (over 29 hours post-rewetting). In addition, two levels of N inputs allowed to determine how N availability modulated plant-soil responses. The response of the potentially active soil bacterial and fungal communities to rewetting was assessed using targeted metagenomics. The responses of biogeochemical cycles were evaluated using heavy isotope tracers (13C-CO2 and 15N-NO3-) to quantify C flux from plants to soil microorganisms and plant-microbial competition for N over time post-rewetting.We found that precipitation patterns shaped plant morphology and physiology, microbial community composition as well as soil N cycling in our systems, which set contrasting scenes for the rewetting responses in our systems. In particular, infrequent precipitation patterns (cycles of longer dry periods followed by larger magnitude rain events) resulted in increased microbial N transformation potentials and smaller inorganic N pools. The rewetting responses were determined by evaluating C dynamics (plant-microbial coupling and soil CO2 efflux rate), N dynamics (plant-microbial competition for N and soil N2O efflux rate) and microbial dynamics (composition of active and potentially active bacterial and fungal communities after rewetting). First, we found that plant-microbial coupling (i.e the microbial assimilation of C from fresh photosynthate) may be reduced under more infrequent precipitation patterns, especially near the soil surface, and under conditions of low N availability. Our findings also suggest that whilst in soil-only systems, dead microbial cells appear to be a major source fuelling soil CO2 efflux pulse upon rewetting, in plant-soil systems root respiration plays an important role in the magnitude of the CO2 efflux upon rewetting. Second, concerning soil N dynamics, we found, in concurrence with previous studies, that soil microorganisms were the stronger competitor for N over short time scales, likely due to their overall fast response rates and high affinity for substrate, whilst plants outcompeted soil microbes for soil N assimilation, over longer time scales likely taking advantage of the fast microbial turnover (...)
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Lee, Sung-Ching. "Annual greenhouse gas budget for a bog ecosystem undergoing restoration by rewetting." Thesis, University of British Columbia, 2016. http://hdl.handle.net/2429/58985.

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Many peatlands have been drained and harvested for peat mining, which turned those landscapes into carbon (C) emitters. Rewetting of disturbed peatlands facilitates their ecological recovery, and may help them revert to carbon dioxide (CO₂) sinks. However, it may also cause substantial emissions of the powerful greenhouse gas (GHG) methane (CH₄). Our knowledge on year-round measurements of CO₂ and CH₄ fluxes in restored peatlands is currently very limited. This study quantifies C exchanges in a disturbed and rewetted area located in the Burns Bog Ecological Conservancy Area (BBECA) in Delta, BC, Canada. The BBECA is recognized as the largest raised bog ecosystem on North America’s West Coast. It was substantially reduced in size and degraded by peat mining and agriculture. Since 2005, the bog has been declared a conservancy area, and restoration efforts focus on rewetting disturbed ecosystems to recover Sphagnum and suppress fires. Year-round (16th June 2015 to 15th June 2016) turbulent fluxes of CO₂ and CH₄ were measured from a tower platform in an area rewetted in 2007 using the eddy-covariance (EC) technique. The annual CO₂ budget was -179 g CO₂-C m-² year-¹ and the annual CH₄ budget was 16 g CH₄-C m-² year-¹. Gross ecosystem productivity (GEP) exceeded ecosystem respiration (Re) during summer months (June-August), causing a net CO₂ uptake. In summer, high CH₄ emissions were measured. In winter (December-February), substantially lower CH₄ emissions and roughly equal magnitudes of GEP and Re made the bog C neutral. Oxygen limitation due to the high water table caused by ditch blocking suppressed Re. With low temperatures in winter, CH₄ emission was more suppressed than Re. The key environmental factors controlling the seasonality of these exchanges in the study area were downwelling photosynthetically active radiation and 5-cm soil temperature. Annual net GHG flux from CO₂ and CH₄ during the study period totaled to -23.48 g CO₂e m-² year-¹ and 1242.04 g CO₂e m-² year-¹ by using 100-year and 20-year global warming potential (GWP) values, respectively. Consequently, the ecosystem was almost CO₂e neutral annually on a 100-year time horizon but was a significant CO₂e source on a 20-year time horizon.
Arts, Faculty of
Geography, Department of
Graduate
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Silva, Ana Beatriz de Albuquerque Morais. "Phosphorous cycling in dry and rewet incubated soils subjected to different fertilization histories." Master's thesis, ISA/UTL, 2011. http://hdl.handle.net/10400.5/3919.

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Mestrado em Engenharia do Ambiente - Instituto Superior de Agronomia
Phosphorus continuous application in fertilizers, in quantities superior to those required by plants causes a P buildup in soils, potentially increasing nutrient losses and compromising water quality by eutrophication process. This work was aimed at assessing the effect of DRW cycles, in two soils with different fertilization histories subjected to organic and mineral fertilization, over P availability. Soils were collected from a long-term fertilizer management platform (NW Italy) divided in two plots experiencing since 1996 different fertilization management (one plot fertilized with low N and K levels and no P and another with fertilization high on N and P levels), and each was divided in 3 subplots treated with mineral, compost and without fertilization, since 2010. The soils were subjected, under laboratory conditions, to four DRW cycles and compared with another set at constant moisture. Weekly the soils were sampled and analyzed for some of their P forms. Soluble P increased in compost fertilized soil, especially after the third dry and rewet cycle, following microbial decay. Yet, this was more pronounced in the overfertilized soils. From these findings it is possible to conclude that the availability of P may be further enhanced by water content variations as by compost addition.
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Henstra, Steven W. "Vegetation responses to ecological restoration (rewetting) of abandoned block-cut peatlands in eastern Québec." Thesis, University of British Columbia, 2012. http://hdl.handle.net/2429/40829.

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Abandoned block-cut peatlands are typified by an alternating topography of mined trenches and raised baulks. Although these sites re-vegetate densely with native bog species, Sphagnum species characteristic of undisturbed bogs are conspicuously absent and peat accumulation has not recommenced. Ecological restoration of abandoned block-cut peatlands involves blocking remnant drainage ditches, “rewetting” the residual peat body to: 1) re-establish vegetation assemblages dominated by Sphagnum, and 2) re-establish the upper, hydrologically active layer (acrotelm) that characterizes intact peatlands. This study evaluates the progress towards achieving these goals in three rewetted block-cut sites in eastern Québec. Plant species composition, above-ground biomass, and accumulated organic matter data were collected from mined trenches within rewetted and non-rewetted sectors of the study sites and used for comparison with nearby undisturbed reference bogs. Comparisons of current patterns of community vegetation structure in rewetted and non-rewetted sectors of the study sites indicated that vegetation assemblages are strongly influenced by water table position. In areas where rewetting resulted in a water table position at or just above the peat surface, rapid community scale vegetation change occurred, with widespread mortality of vascular vegetation followed by recolonization by hydrophytic ericaceous and herbaceous species, and hollow/lawn Sphagnum species (<4 years following rewetting). Despite this positive change, vegetation assemblages within rewetted sectors still differ significantly from those found in natural reference sites up to 17 years following rewetting. Changes in above-ground biomass indicated a significant reduction in tree biomass, a significant portion of which is present as dead-standing tree biomass 4 years following rewetting. Shrub biomass initially decreased, but then increased 10 years following rewetting as species compositions shifted. Accumulated organic matter shifted from a predominance of ericaceous litter to fibric peat in rewetted sectors, the depth of which is increasing as a function of time. These findings provide initial evidence of re-establishment of the acrotelm; however, additional research is required to determine whether the newly accumulated peat will provide the hydrological functions perceived of the acrotelm in undisturbed bogs. Continued detailed observation of the biotic recovery of these ecosystems will provide valuable information for future restoration endeavors.
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Sjöstrand, Björn. "Dewatering aspects at the forming section of the paper machine : Rewetting and forming fabric structure." Licentiate thesis, Karlstads universitet, Institutionen för ingenjörs- och kemivetenskaper (from 2013), 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:kau:diva-47640.

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The underlying motives of the research undertaken here are twofold: to obtain a deeper understanding of the dewatering mechanisms at the forming section of a papermaking machine and to develop numerical models that describe the flow through forming fabrics. More comprehensive knowledge of dewatering in the forming section allows suggestions to be made for improvements that reduce the amount of energy used in the process without affecting the quality of the end product.   The objective of this thesis is to answer the following questions: How and why does rewetting occur at the high vacuum suction boxes? How does the structure of the forming fabric affect dewatering at the forming section? Is it possible to create accurate numerical models for forming fabrics, and can these be used to predict the dewatering behaviour of new types of fabrics?   Laboratory and pilot studies simulating high vacuum suction boxes were performed together with numerical modelling of the flow of air and water through both the forming fabric and the paper sheet.   The conclusion drawn from the pilot study is that rewetting significantly lowers the dryness of the paper sheet exiting the suction boxes. The phenomenon is extremely rapid and is most likely driven by capillary forces. The high speed at which this rewetting occurs makes it difficult to impede by placing the suction boxes closer to the couch pick-up: the solution is more likely to be the use of new and improved designs of the forming fabric. The structure of the forming fabric has been shown to affect the dewatering rate at certain conditions of vacuum dewatering, and can possibly be connected partly to the fact that fibres penetrate the surface of the fabric to varying degrees and partly to the flow resistance of the different fabric structures. Numerical models of high accuracy can be constructed and used to predetermine how new fabric designs would affect dewatering at the forming section.   This thesis quantifies aspects of dewatering such as rewetting and the influence of the forming fabric. Understanding these dewatering aspects further provides for the potential enhancement of energy efficiency in the forming section, and thereby the entire papermaking process. The forming fabric can play an important role in improving energy efficiency: rewetting after the high vacuum suction boxes occurs more rapidly than was previously known, so its design might be the only possible way of impeding it. The forming fabric can also improve the rate of dewatering: it is therefore likely that its design will be important in the next stage of developing energy efficiency and thereby play a part in achieving a more sustainable future.
This thesis quantifies aspects of dewatering such as rewetting and the influence of the forming fabric. Understanding these dewatering aspects further provides for the potential enhancement of energy efficiency in the forming section, and thereby the entire papermaking process. The forming fabric can play an important role in improving energy efficiency: rewetting after the high vacuum suction boxes occurs more rapidly than was previously known, so its design might be the only possible way of impeding it. The forming fabric can also improve the rate of dewatering: it is therefore likely that its design will be important in the next stage of developing energy efficiency and thereby play a part in achieving a more sustainable future.
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Dinh, Mai-Van [Verfasser], and Egbert [Akademischer Betreuer] Matzner. "Soluble phosphorus in forest soil : Effects of drying and rewetting / Mai-Van Dinh ; Betreuer: Egbert Matzner." Bayreuth : Universität Bayreuth, 2017. http://d-nb.info/1143009843/34.

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Gordon, Helen. "Drying and rewetting effects on microbial community composition and nutrient leaching form soils of contrasting management." Thesis, Lancaster University, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.533122.

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Books on the topic "Rewetting"

1

Holden, Nicholas Mark. The mechanism of milled peat rewetting: Development of a stockpile rewetting model. Dublin: University College Dublin, 1998.

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Mao, Chris Qun. Local rewetting and distortion of paper. Ottawa: National Library of Canada, 2001.

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Weislogel, Mark M. Analysis of tank PMD rewetting following thrust resettling. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 2002.

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Blackburn, D. Analysis of Zircaloy rewetting experiments and their implication for reactor fuel. Luxembourg: Commission of the European Communities, 1985.

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Carbon credits from peatland rewetting: Climate, biodiversity, land use : science, policy, implementation, and recommendations of a pilot project in Belarus. Stuttgart: Schweizerbart Science Publishers, 2011.

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Ryan, Miriam G. The influence of draught and rewetting on the dynamics of nitrogen, potassium and disolved organic carbon in a coniferous forest ecosystem. Dublin: University College Dublin, 1997.

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Kaiser, N. E. Study of rewetting and quench phenomena by single pin out-of-pile experiments: With especial emphasis on the effect of pin composition. Luxembourg: Commission of the European Communities, 1985.

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A, Sala M., Collicott S. H, and NASA Glenn Research Center, eds. Analysis of tank PMD rewetting following thrust resettling. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 2002.

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Xie, Stella Xiao Min. Roughening due to inkjet rewetting: Effect of paper treatment and composition. 2006.

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10

United States. National Aeronautics and Space Administration., ed. An analytical investigation of transient effects on rewetting of heated thin flat plates. [Washington, DC: National Aeronautics and Space Administration, 1993.

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Book chapters on the topic "Rewetting"

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Jian, Fuji, and Digvir S. Jayas. "Fundamental Principles of Aeration, Drying, and Rewetting." In Grains, 217–86. Boca Raton: CRC Press, 2021. http://dx.doi.org/10.1201/9781003186199-4.

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Denham, M. K., and D. Blackburn. "Rewetting Propagation Over Zircaloy Under Bottom Flooding Conditions." In Safety of Thermal Water Reactors, 153–63. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4972-0_16.

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Yuwati, Tri Wira, Dony Rachmanadi, M. Abdul Qirom, Purwanto B. Santosa, Kitso Kusin, and Hesti Lestari Tata. "Peatland Restoration in Central Kalimantan by Rewetting and Rehabilitation with Shorea balangeran." In Tropical Peatland Eco-management, 595–611. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4654-3_21.

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Silviana, Sinta H., Bambang H. Saharjo, Sigit Sutikno, Erianto I. Putra, and Imam Basuki. "The Effect of Fire and Rewetting on the Groundwater Level in Tropical Peatlands." In Tropical Peatland Eco-management, 613–24. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4654-3_22.

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Alves-Filho, Odílio, and Thomas R. Rumsey. "Thin-Layer Drying and Rewetting Models to Predict Moisture Diffusion in Spherical Agricultural Products." In Drying ’85, 434–37. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-662-21830-3_59.

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van Duinen, G. A., Y. Zhuge, W. C. E. P. Verberk, A. M. T. Brock, H. H. van Kleef, R. S. E. W. Leuven, G. van der Velde, and H. Esselink. "Effects of rewetting measures in Dutch raised bog remnants on assemblages of aquatic Rotifera and microcrustaceans." In Living Rivers: Trends and Challenges in Science and Management, 187–200. Dordrecht: Springer Netherlands, 2006. http://dx.doi.org/10.1007/1-4020-5367-3_12.

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Kaiser, N. E., and O. Rathmann. "Study of Rewetting and Quench Phenomena by Single Pin Out-of- Pile Experiments, with Special Emphasis on the Effect of Pin Composition." In Safety of Thermal Water Reactors, 125–34. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4972-0_14.

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Marando, Graciela, Patricia Jiménez, Ramón Josa, Maria Julià, Marta Ginovart, and Manuel Bonmatí. "Effects of Air-Drying and Rewetting on Extractable Organic Carbon, Microbial Biomass, Soil Respiration and β-Glucosidase and β-Galactosidase Activities of Minimally Disturbed Soils Under Mediterranean Conditions." In Environmental Science and Engineering, 103–18. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-21162-1_8.

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"rewetting agent." In The Fairchild Books Dictionary of Textiles. Fairchild Books, 2021. http://dx.doi.org/10.5040/9781501365072.13498.

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Tessier, D., A. Beaumont, and G. Pedro. "Influence of Clay Mineralogy and Rewetting Rate on Clay Microstructure." In Soil Micro-Morphology: A Basic and Applied Science, Proceedings of the VIIIth International Working Meeting of Soil Micromorphology, 115–21. Elsevier, 1990. http://dx.doi.org/10.1016/s0166-2481(08)70322-2.

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Conference papers on the topic "Rewetting"

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Ilyas, Muhammad, Masroor Ahmad, Colin P. Hale, Simon P. Walker, and Geoff F. Hewitt. "Rewetting Processes During Top/Bottom Re-Flooding of Heated Vertical Surfaces." In ASME/JSME 2011 8th Thermal Engineering Joint Conference. ASMEDC, 2011. http://dx.doi.org/10.1115/ajtec2011-44187.

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Rewetting of the heated fuel rods is one of the most important phenomena to be considered in analysis of the design basis loss of coolant accident (LOCA) in light water reactors. The rewetting phenomenon is a complex and violent one with the rewetting front moving rather slowly over the heated surface. For water temperature close to saturation, the rate of progression of rewetting front is independent of flow rate of the water approaching the rewetting front; this is an indication of the fact that the rewetting process is governed by events local to the rewetting front [1]. This paper describes an experimental study on the rewetting of heated vertical surfaces during top/bottom reflooding. Through an infrared transparent substrate fixed in the surface, processes occurring locally at the quench front have been studied by using a fast response thermal imaging system (Cedip Titanium 560M). The existence of a cyclic bursting phenomenon at the quench front has been observed. Multiple events of this type gradually remove heat from the metal, allowing the rewetting front to progress slowly over the surface. These intermittent contacts occur over a short axial length. Temperature measurements indicate that the metal surface temperature at the rewetting front is close to the homogeneous nucleation temperature.
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Wada, Yuki, Dan Le, Akira Satou, Yasuteru Sibamoto, and Taisuke Yonomoto. "On the Liquid Film Flow Characteristics During the Rewetting in the Single Rod Air-Water System." In 2018 26th International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/icone26-82491.

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Dry-out and rewetting phenomenon may occur on a fuel rod surface during anticipated operational occurrences (AOOs) for a boiling water reactor (BWR). The conventional rewetting model included in the current system code tends to underestimate the rewetting propagation velocity due to the absence of an appropriate precursory cooling model. The present research aims at the development of a mechanistic model for the precursory cooling in the annular mist flow regime typical of AOO and anticipated transition without scrum (ATWS). Rewetting experiments were carried out using a single heater rod in the circular glass pipe with air-water flow at atmospheric pressure to visualize the rewetting behavior and obtain mechanistic understanding on the phenomena. This paper summarizes the experimental results and discusses the liquid film flow characteristics including roll wave formation and spattering at the rewetting front.
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AMBROSE, J., L. CHOW, and J. BEAM. "Transient heat pipe response and rewetting behavior." In 4th Thermophysics and Heat Transfer Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1986. http://dx.doi.org/10.2514/6.1986-1359.

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Abe, Yoshiyuki, Kotaro Tanaka, Takuya Yokoyama, and Akira Iwasaki. "Heat Transfer Devices With Self-Rewetting Fluids." In ASME 2004 International Mechanical Engineering Congress and Exposition. ASMEDC, 2004. http://dx.doi.org/10.1115/imece2004-61328.

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The authors have been proposing the utilization of “self-rewetting fluids” as a new phase change heat transfer media, especially in space applications. Self-rewetting fluids show a quite unique thermophysical behavior—an increase in the surface tension with increasing temperature. Since self-rewetting fluids are non-azeotropic compositions of dilute aqueous solutions of alcohols, the Marangoni effects due to both temperature gradient and concentration gradient work in the same direction in the course of liquid/vapor phase change, and induce a strong liquid flow to hotter interface. A series of terrestrial experiments for conventional heat pipes with self-rewetting fluids have been conducted, and compared with those with water as a reference. Appreciable heat transfer performance improvement from water heat pipes was recognized. Furthermore, a series of low gravity experiments for wickless heat pipes with a self-rewetting fluid have also been conducted by using parabolic flights of aircraft. The heat transfer performance of wickless heat pipes in low gravity was evaluated, and superior characteristics was confirmed.
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Nagashima, Nozomi, Hiroyasu Ohtake, and Yasuo Koizumi. "Measurements of Rewetting Temperatures of Hot Dry Surface in Saturated and Subcooled Film Boiling." In ASME/JSME 2011 8th Thermal Engineering Joint Conference. ASMEDC, 2011. http://dx.doi.org/10.1115/ajtec2011-44533.

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The behavior of rewetting on a high superheated and dry surface, focusing on rewetting temperature just as collapse of saturated and subcooled film boiling was investigated experimentally by using a commercial separated-type infrared thermometer. Saturated and subcooled impingement jet experiments were conducted by using a silicon wafer with 20 mm length, 20 mm width and 0.5 mm thickness and pure water at atmospheric condition. Temperature of the test heater was measured by using a commercial separated-type infrared thermometer from a back side of it. The present experimental results showed that as the liquid subcooling was high, Minimum Heat Flux temperature (i.e., Minimum Film Boiling, rewetting temperature or quenching temperature) was higher. Furthermore, the effect of the rewetting temperature on liquid subcooling was similar to that of Dhir-Purohit’s correlation quantitatively.
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Ohtake, Hiroyasu, Hiroyuki Satoh, and Yasuo Koizumi. "Study on the Behavior of a Wetted Area Right After Liquid-Wall Contact in Pool Film Boiling." In ASME 2000 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2000. http://dx.doi.org/10.1115/imece2000-1507.

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Abstract The behaviors of the rewetting on pool film boiling, focusing on observations of a collapse of a vapor film, a wetted area and a contact angle on a superheated surface were investigated experimentally. Using a U-shaped platinum wire with 2 mm diameter and 140 mm long, pool film-boiling experiments were performed for saturated water at atmospheric pressure. After a stable film-boiling state at a prescribed initial wall temperature was established, saturated water from a nozzle, set above the test wire, was injected on the superheated surface in the stable film-boiling, then artificial rewetting was forced on the superheated surface. During forming the artificial rewetting, the temperature fluctuation right under the liquid injection and the behavior of the rewetting were obtained for the initial wall temperatures of 600, 420, 400 and 300 degree-C, respectively. The present experimental results showed that the propagative collapse of the vapor film occurred when the initial wall superheat was below 300 K. On the other hand, above the initial wall superheat of 320 K, the rewetting declined after liquid injection was finished then film boiling recovered. The temperature was related to the thermodynamic limit of superheat, according to the measured temperature fluctuation during supplying the liquid. The wetted area right after liquid-wall contact and the advancing velocity of the rewetting front increased as the initial wall superheat decreased. The measured angles between the liquid-vapor interfacial line and the heated wall corresponded to dynamic contact angles were close to the dynamic advancing contact-angles in room temperature.
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Sibamoto, Yasuteru, Yu Maruyama, and Hideo Nakamura. "Measurement and Analysis for Rewetting Velocity Under Post-BT Conditions During Anticipated Operational Occurrence of BWR." In 17th International Conference on Nuclear Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/icone17-75287.

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A series of experiments was performed for rewetting phenomena on dryed-out fuel rod surfaces under post-BT (Boiling Transition) conditions with high-pressure and high-water flow rate simulating anticipated operational occurrences of a BWR. An analytical model for rewetting velocity, defined by a propagation velocity of a quench front, has been developed on the basis of the experimental results. The rewetting for the post-BT condition is characterized by the faster propagation of the quench front than that for reflood phase conditions during a postulated large-break loss-of-coolant accident. In order to provide an explanation of this characteristic, the present analytical model took an effect of a precursory cooling into account by modifying the existing correlation by Sun-Dix-Tien [1] which is based on a one-dimensional analysis in a flow direction during the reflood phase. The present model demonstrates that the precursory cooling can significantly increase the rewetting velocity by more than an order of magnitude. Applying the experimental correlation developed in the separately conducted experiment into the heat transfer coefficient in the present model at a wet and a dry region with precursory cooling, our data of the rewetting velocity as well as the wall temperature profiles for the variable flow rates are successfully predicted.
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Ohtake, Hiroyasu, Yasuo Koizumi, Shingo Kobayashi, and Takeshi Watanabe. "Study on Behavior of Rewetting on Hot Wall." In ASME/JSME 2007 Thermal Engineering Heat Transfer Summer Conference collocated with the ASME 2007 InterPACK Conference. ASMEDC, 2007. http://dx.doi.org/10.1115/ht2007-32860.

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The behavior of rewetting on high superheated surface, focusing on rewetting temperature during collapse of saturated and subcooled film boiling was investigated experimentally and analytically. Saturated and subcooled film-boiling experiments were conducted by using a Silicon wafer with 20 mm length, 20 mm width and 0.5 mm thickness and pure water at atmospheric condition. Both pool boiling and impingement jet experiments were preformed in the present study. Then, the present experimental results were examined by using hydrodynamics instability on liquid-vapor interface (Rayleigth-Tayor instability) and a heat conduction model (rewetting model under a falling-flow of a liquid layer).
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Weislogel, M., and S. Collicott. "Analysis of tank PMD rewetting following thrust resettling." In 40th AIAA Aerospace Sciences Meeting & Exhibit. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2002. http://dx.doi.org/10.2514/6.2002-757.

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Yan, Y. H., Jay M. Ochterbeck, and Xiao-Feng Peng. "NUMERICAL STUDY OF CAPILLARY REWETTING IN POROUS MEDIA." In International Heat Transfer Conference 11. Connecticut: Begellhouse, 1998. http://dx.doi.org/10.1615/ihtc11.4190.

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Reports on the topic "Rewetting"

1

Lin, W. ,. LLNL. Report on laboratory tests of drying and rewetting of intact rocks from the drift-scale and single-heater tests. Office of Scientific and Technical Information (OSTI), April 1998. http://dx.doi.org/10.2172/675024.

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