Virtaavan veden hyödyntäminen keskitetyssä lämmöntuotannossa

Tässä työssä tutkittiin uudenlaista kaukolämmön tuotantotapaa, joka perustuu lämmöntal-teenottoon jokivedestä lämpöpumpuilla. Tutkimuksessa luotiin kokonaiskuva uudenlaisen lämmöntuotannon toiminnasta, sekä selvitettiin tuotannon soveltumista Suomeen. Tuotan-non kattavuus selvitettiin laskennan avulla käymällä läpi kaikki kaukolämpöä myyvien yri-tysten kaukolämpöverkot. Verkoston kulutustietoihin yhdisteltiin jokien virtaamatietoja. Laskenta tehtiin taulukkolaskentaohjelmalla ja kohteita oli yhteensä 184. Työssä tutkittiin myös laitoksen ympäristövaikutuksia lämpövaraston, jokiekosysteemin ja hiilidioksidipäästöjen osalta. Merkittävimmät vaikutukset tulisivat Suomen ilmastossa suu-riksi muodostuvien lämpövarastojen rakentamisesta. Jokiekosysteemin kannalta laitoksen toiminnan vaikutukset osoittautuivat pääasiassa positiivisiksi. Hiilidioksidipäästöjen lasken-nassa laitos oletettiin täysin päästöttömäksi, koska sähköverkkoa tarkasteltiin vuoden 2050 näkökulmasta, jolloin sähköntuotannon oletettiin olevan päästötöntä. Laskennasta selvisi, että laitoksilla pystyttäisiin kattamaan 22,7 % kaukolämmityksen tar-peesta. Tämä tarkoittaisi noin 1,6 milj. tonnin hiilidioksidipäästöjen välttämistä vuositasolla. Laitostyypin todettiin soveltuvan paremmin vain kesänaikaisen lämmöntarpeen kattami-seen. Talviaikainen lämmöntarve olisi parempi kattaa jollakin muulla ratkaisulla.

Estudo do Sujamento da Superfície de Transferência de Calor do Evaporador de uma Bomba de Calor aquecido pelo efluente de uma fábrica de pasta para papel

O presente trabalho tem como principal objectivo a avaliação do sujamento da superfície de transferência de calor do evaporador de uma bomba de calor, quando se utiliza o efluente da fábrica de pasta e papel da Portucel Soporcel em Cacia como fluido de aquecimento. Para a realização deste estudo montou-se uma instalação, composta por uma bomba de calor, um circuito de água de arrefecimento do condensador da bomba de calor e um circuito de água residual quente para o aquecimento do evaporador da bomba de calor. O ensaio decorreu durante um período de 84 dias, durante o qual foram registadas as temperaturas em vários pontos dos circuitos e os caudais de circulação. A evolução temporal da quantidade de calor transferida no evaporador, assim como, a comparação do coeficiente global de transferência de calor em condições ideias e experimentais, permitiu verificar que a razão U/U0 para o evaporador da bomba de calor não teve um comportamento decrescente ao longo do período de ensaio, permitindo concluir que, nas condições operatórias da experiência, não ocorreu sujamento na superfície do evaporador. No estudo de corrosão do cobre quando exposto à água residual em questão, obteve-se, para a velocidade de corrosão, o valor de 1,56 mg/(dm2 .dia), indicando assim que a corrosão do cobre naquele meio é praticamente inexistente.

WRITING A COMMUNITY GUIDEBOOK FOR EVALUATING LOW-GRADE GEOTHERMAL ENERGY FROM FLOODED UNDERGROUND MINES FOR HEATING AND COOLING BUILDINGS

When underground mines close they often fill with water from ground and surface sources; each mine can contain millions to billions of gallons of water. This water, heated by the Earth’s geothermal energy, reaches temperatures ideal for heat pumps. The sheer scale of these flooded underground mines presents a unique opportunity for large scale geothermal heat pump setups which would not be as economically, socially, and environmentally feasible anywhere else. A literature search revealed approximately 30 instances of flooded underground mines being used to heat and cool buildings worldwide. With thousands of closed/abandoned underground mines in the U.S. and a million estimated globally, why hasn’t this opportunity been more widely adopted? This project has found perception and lack of knowledge about the feasibility to be key barriers. To address these issues, this project drafted a guidebook for former mining communities titled A Community Guide to Mine Water Geothermal Heating and Cooling.

Naturmuseet Vänern : Energieffektivisering med fokus på kyltekniska lösningar

År 2006 införde Boverket, som lyder under regeringen krav för specifik energianvändning (kWh/m2år) för byggnader i syfte att minska energianvändningen för bostäder och lokaler. För att följa Boverkets krav för specifik energianvändning är det därför relevant att bygga mer energieffektiva byggnader. Naturmuseet Vänern är en byggnad i Karlstad som befinner sig vid Vänern. Byggnaden är omgiven av en naturskön miljö och dess verksamhet är huvudsakligen ett museum. Som helhet är Naturmuseet Vänern högt i tak och har stora fönsterytor vilket leder till att byggnaden behöver kylas på grund av den stora mängden solinstrålning. För att hålla sig till en låg specifik energianvändning är det därför relevant att hitta ett hållbart kylsystem. För att en byggnad ska bli energieffektiv i ett klimat såsom det i Sverige krävs ett byggnadsmaterial med lågt U-värde samt väl anpassade systemlösningar för värme, ventilation och kyla. Utifrån datorprogrammet VIP-Energy har en energianalys gjorts för Naturmuseet Vänern, vilket legat som grund för byggnadens utformning samt valet av byggnadsmaterial och kylsystem. Resultatet har utöver hur byggandes klimatskal ska se ut även landat i systemhandlingar i form av ritningar, driftstrategi och materialspecifikation för kylsystemet. Den lägsta specifika energianvändningen för Naturmuseet Vänern är 37 kWh/m2år, vilket fås då bergkyla väljs som kylsystem.

Sviluppo di un modello Simulink per la gestione termica di un veicolo elettrico a batteria

Obiettivo di questo progetto di tesi è la realizzazione di un modello per la gestione termica di un veicolo elettrico a batteria: l’elettrificazione in ambito automotive richiede un approfondito studio delle problematiche termiche allo scopo di incrementare l’efficienza del veicolo, le performance e la vita della batteria. In particolare, l’oggetto di ricerca consiste nella modellazione di una pompa di calore. Partendo dalla definizione dei requisiti e degli obiettivi del sistema di gestione termica, ogni componente della pompa di calore viene analizzato modellato e connesso all’intero sistema. La modellazione è stata affrontata mediante l’utilizzo dell’ambiente MATLAB/Simulink. Il primo passo è stato avanzato nell’analisi del ciclo termodinamico ideale, analizzando il comportamento di vari fluidi frigorigeni, la funzionalità dei singoli componenti e l’interazione di quest’ultimi al variare delle condizioni di funzionamento, principalmente potenze scambiate, pressioni, temperature e portata massica di refrigerante. Il principale lavoro di simulazione è legato alla realizzazione di un modello configurabile dell’intero apparato di gestione termica della batteria per un veicolo elettrico. Per mezzo dello studio delle relazioni termodinamiche dei componenti principali del ciclo frigorifero sono state valutate tutte le grandezze che variano durante le trasformazioni che compie il fluido refrigerante all’interno del ciclo frigorifero. L’attività di validazione del modello implementato è stata svolta mediante il confronto tra le condizioni del fluido refrigerante determinate mediante le relazioni termodinamiche e quelle ottenute valutando le trasformazioni sui diagrammi di stato dei fluidi frigorigeni trattati. Il modello implementato è da ritenersi primordiale nel contesto legato alla modellazione e controllo dei sistemi di gestione termica per i sistemi propulsivi dei veicoli elettrici a batteria.

Numerical and ExperimentalModelling of Gas Flow and Heat Transfer in the Air Gap of An Electric Machine

This work deals with the cooling of high-speed electric machines, such as motors and generators, through an air gap. It consists of numerical and experimental modelling of gas flow and heat transfer in an annular channel. Velocity and temperature profiles are modelled in the air gap of a high-speed testmachine. Local and mean heat transfer coefficients and total friction coefficients are attained for a smooth rotor-stator combination at a large velocity range. The aim is to solve the heat transfer numerically and experimentally. The FINFLO software, developed at Helsinki University of Technology, has been used in the flow solution, and the commercial IGG and Field view programs for the grid generation and post processing. The annular channel is discretized as a sector mesh. Calculation is performed with constant mass flow rate on six rotational speeds. The effect of turbulence is calculated using three turbulence models. The friction coefficient and velocity factor are attained via total friction power. The first part of experimental section consists of finding the proper sensors and calibrating them in a straight pipe. After preliminary tests, a RdF-sensor is glued on the walls of stator and rotor surfaces. Telemetry is needed to be able to measure the heat transfer coefficients at the rotor. The mean heat transfer coefficients are measured in a test machine on four cooling air mass flow rates at a wide Couette Reynolds number range. The calculated values concerning the friction and heat transfer coefficients are compared with measured and semi-empirical data. Heat is transferred from the hotter stator and rotor surfaces to the coolerair flow in the air gap, not from the rotor to the stator via the air gap, althought the stator temperature is lower than the rotor temperature. The calculatedfriction coefficients fits well with the semi-empirical equations and precedingmeasurements. On constant mass flow rate the rotor heat transfer coefficient attains a saturation point at a higher rotational speed, while the heat transfer coefficient of the stator grows uniformly. The magnitudes of the heat transfer coefficients are almost constant with different turbulence models. The calibrationof sensors in a straight pipe is only an advisory step in the selection process. Telemetry is tested in the pipe conditions and compared to the same measurements with a plain sensor. The magnitudes of the measured data and the data from the semi-empirical equation are higher for the heat transfer coefficients than thenumerical data considered on the velocity range. Friction and heat transfer coefficients are presented in a large velocity range in the report. The goals are reached acceptably using numerical and experimental research. The next challenge is to achieve results for grooved stator-rotor combinations. The work contains also results for an air gap with a grooved stator with 36 slots. The velocity field by the numerical method does not match in every respect the estimated flow mode. The absence of secondary Taylor vortices is evident when using time averagednumerical simulation.

Contribution of land use changes to near-surface air temperatures during recent summer extreme heat events in the Phoenix Metropolitan Area

The impact of 1973–2005 land use–land cover (LULC) changes on near-surface air temperatures during four recent summer extreme heat events (EHEs) are investigated for the arid Phoenix, Arizona, metropolitan area using the Weather Research and Forecasting Model (WRF) in conjunction with the Noah Urban Canopy Model. WRF simulations were carried out for each EHE using LULC for the years 1973, 1985, 1998, and 2005. Comparison of measured near-surface air temperatures and wind speeds for 18 surface stations in the region show a good agreement between observed and simulated data for all simulation periods. The results indicate consistent significant contributions of urban development and accompanying LULC changes to extreme temperatures for the four EHEs. Simulations suggest new urban developments caused an intensification and expansion of the area experiencing extreme temperatures but mainly influenced nighttime temperatures with an increase of up to 10 K. Nighttime temperatures in the existing urban core showed changes of up to 2 K with the ongoing LULC changes. Daytime temperatures were not significantly affected where urban development replaced desert land (increase by 1 K); however, maximum temperatures increased by 2–4 K when irrigated agricultural land was converted to suburban development. According to the model simulations, urban landscaping irrigation contributed to cooling by 0.5–1 K in maximum daytime as well as minimum nighttime 2-m air temperatures in most parts of the urban region. Furthermore, urban development led to a reduction of the already relatively weak nighttime winds and therefore a reduction in advection of cooler air into the city.

Separating the influence of projected changes in air temperature and wind on patterns of sea level change and ocean heat content

We present ocean model sensitivity experiments aimed at separating the influence of the projected changes in the “thermal” (near-surface air temperature) and “wind” (near-surface winds) forcing on the patterns of sea level and ocean heat content. In the North Atlantic, the distribution of sea level change is more due to the “thermal” forcing, whereas it is more due to the “wind” forcing in the North Pacific; in the Southern Ocean, the “thermal” and “wind” forcing have a comparable influence. In the ocean adjacent to Antarctica the “thermal” forcing leads to an inflow of warmer waters on the continental shelves, which is somewhat attenuated by the “wind” forcing. The structure of the vertically integrated heat uptake is set by different processes at low and high latitudes: at low latitudes it is dominated by the heat transport convergence, whereas at high latitudes it represents a small residual of changes in the surface flux and advection of heat. The structure of the horizontally integrated heat content tendency is set by the increase of downward heat flux by the mean circulation and comparable decrease of upward heat flux by the subgrid-scale processes; the upward eddy heat flux decreases and increases by almost the same magnitude in response to, respectively, the “thermal” and “wind” forcing. Regionally, the surface heat loss and deep convection weaken in the Labrador Sea, but intensify in the Greenland Sea in the region of sea ice retreat. The enhanced heat flux anomaly in the subpolar Atlantic is mainly caused by the “thermal” forcing.

An assessment of air-sea heat fluxes from ocean and coupled reanalyses

Sixteen monthly air–sea heat flux products from global ocean/coupled reanalyses are compared over 1993–2009 as part of the Ocean Reanalysis Intercomparison Project (ORA-IP). Objectives include assessing the global heat closure, the consistency of temporal variability, comparison with other flux products, and documenting errors against in situ flux measurements at a number of OceanSITES moorings. The ensemble of 16 ORA-IP flux estimates has a global positive bias over 1993–2009 of 4.2 ± 1.1 W m−2. Residual heat gain (i.e., surface flux + assimilation increments) is reduced to a small positive imbalance (typically, +1–2 W m−2). This compensation between surface fluxes and assimilation increments is concentrated in the upper 100 m. Implied steady meridional heat transports also improve by including assimilation sources, except near the equator. The ensemble spread in surface heat fluxes is dominated by turbulent fluxes (>40 W m−2 over the western boundary currents). The mean seasonal cycle is highly consistent, with variability between products mostly <10 W m−2. The interannual variability has consistent signal-to-noise ratio (~2) throughout the equatorial Pacific, reflecting ENSO variability. Comparisons at tropical buoy sites (10°S–15°N) over 2007–2009 showed too little ocean heat gain (i.e., flux into the ocean) in ORA-IP (up to 1/3 smaller than buoy measurements) primarily due to latent heat flux errors in ORA-IP. Comparisons with the Stratus buoy (20°S, 85°W) over a longer period, 2001–2009, also show the ORA-IP ensemble has 16 W m−2 smaller net heat gain, nearly all of which is due to too much latent cooling caused by differences in surface winds imposed in ORA-IP.

Experimental analysis of heat transfer in packed beds with air flow

Heat-transfer studies were carried out in a packed bed of glass beads, cooled by the wall, through which air percolated. Tube-to-particle diameter ratios (D/dp) ranged from 1.8 to 55, while the air mass flux ranged from 0.204 to 2.422 kg/m2·s. The outlet bed temperature (TL) was measured by a brass ring-shaped sensor and by aligned thermocouples. The resulting radial temperature profiles differed statistically. Angular temperature fluctuations were observed through measurements made at 72 angular positions. These fluctuations do not follow a normal distribution around the mean for low ratios D/dp. The presence of a restraining screen, as well as the increasing distance between the temperature measuring device and the bed surface, distorts TL. The radial temperature profile at the bed entrance (T0) was measured by a ring-shaped sensor, and T 0 showed to be a function of the radial position, the particle diameter, and the fluid flow rate.

Resistive polymer versus forced-air warming: comparable heat transfer and core rewarming rates in volunteers

BACKGROUND: Mild perioperative hypothermia increases the risk of several severe complications. Perioperative patient warming to preserve normothermia has thus become routine, with forced-air warming being used most often. In previous studies, various resistive warming systems have shown mixed results in comparison with forced-air. Recently, a polymer-based resistive patient warming system has been developed. We compared the efficacy of a standard forced-air warming system with the resistive polymer system in volunteers. METHODS: Eight healthy volunteers participated, each on two separate study days. Unanesthetized volunteers were cooled to a core temperature (tympanic membrane) of 34 degrees C by application of forced-air at 10 degrees C and a circulating-water mattress at 4 degrees C. Meperidine and buspirone were administered to prevent shivering. In a randomly designated order, volunteers were then rewarmed (until their core temperatures reached 36 degrees C) with one of the following active warming systems: (1) forced-air warming (Bair Hugger warming cover #300, blower #750, Arizant, Eden Prairie, MN); or (2) polymer fiber resistive warming (HotDog whole body blanket, HotDog standard controller, Augustine Biomedical, Eden Prairie, MN). The alternate system was used on the second study day. Metabolic heat production, cutaneous heat loss, and core temperature were measured. RESULTS: Metabolic heat production and cutaneous heat loss were similar with each system. After a 30-min delay, core temperature increased nearly linearly by 0.98 (95% confidence interval 0.91-1.04) degrees C/h with forced-air and by 0.92 (0.85-1.00) degrees C/h with resistive heating (P = 0.4). CONCLUSIONS: Heating efficacy and core rewarming rates were similar with full-body forced-air and full-body resistive polymer heating in healthy volunteers.

An experimental study of heat transfer at high temperature differences in turbulent air flow between a rotating cylinder and a stationary concentric auter cylinder,

Final report no. AFOSR 3207.

Observation blanks in physics; air -- liquids -- heat.

Mode of access: Internet.