The He^3/He^4 Dilution Refrigerator
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Dry Dilution Refrigerator for Experiments on Quantum Effects in the Microwave Regime
1 453 Dry Dilution Refrigerator for Experiments on Quantum Effects in the Microwave Regime A. Marx, J. Hoess, and K. Uhlig Walther-Meißner-Institut Garching, Germany 85748 ABSTRACT At the Walther-Meißner-Institut (WMI), a new cryogen-free 3He/4He dilution refrigerator (DR) has been completed; the cryostat will be employed to cool experiments on superconducting quantum circuits for quantum information technology and quantum simulations. All major components have been made at the WMI. The DR offers a great amount of space at the various stages of the apparatus for microwave components and cables, e. g., the usable space at the mixing chamber has a height of more than 60 cm and a diameter of 30 cm (mixing chamber mounting plate). To cool the cables and the cold amplifiers, the DR is equipped with a separate 4He-1K-loop which offers a cooling power of up to 100 mW near 1K. The refrigeration power of the still is 18 mW at 0.9 K; and the diameter of its mounting plate is 35 cm. The cryostat rests in an aluminum trestle on air springs to attenuate building vibrations. It is pre cooled by a Cryomech PT410-RM pulse tube cryocooler (PTC) which is mechanically decoupled from the vacuum can of the cryostat by a bellows assembly. The two stages of the PTC are thermally connected to the DR via copper ropes. There are no nitrogen cooled traps with this DR to purify the gas streams of the 3He and 4He loops; instead, charcoal traps are mounted inside the DR at the first stage of the PTC. -
Chapter 8 and 9 – Energy Balances
CBE2124, Levicky Chapter 8 and 9 – Energy Balances Reference States . Recall that enthalpy and internal energy are always defined relative to a reference state (Chapter 7). When solving energy balance problems, it is therefore necessary to define a reference state for each chemical species in the energy balance (the reference state may be predefined if a tabulated set of data is used such as the steam tables). Example . Suppose water vapor at 300 oC and 5 bar is chosen as a reference state at which Hˆ is defined to be zero. Relative to this state, what is the specific enthalpy of liquid water at 75 oC and 1 bar? What is the specific internal energy of liquid water at 75 oC and 1 bar? (Use Table B. 7). Calculating changes in enthalpy and internal energy. Hˆ and Uˆ are state functions , meaning that their values only depend on the state of the system, and not on the path taken to arrive at that state. IMPORTANT : Given a state A (as characterized by a set of variables such as pressure, temperature, composition) and a state B, the change in enthalpy of the system as it passes from A to B can be calculated along any path that leads from A to B, whether or not the path is the one actually followed. Example . 18 g of liquid water freezes to 18 g of ice while the temperature is held constant at 0 oC and the pressure is held constant at 1 atm. The enthalpy change for the process is measured to be ∆ Hˆ = - 6.01 kJ. -
A Comprehensive Review of Thermal Energy Storage
sustainability Review A Comprehensive Review of Thermal Energy Storage Ioan Sarbu * ID and Calin Sebarchievici Department of Building Services Engineering, Polytechnic University of Timisoara, Piata Victoriei, No. 2A, 300006 Timisoara, Romania; [email protected] * Correspondence: [email protected]; Tel.: +40-256-403-991; Fax: +40-256-403-987 Received: 7 December 2017; Accepted: 10 January 2018; Published: 14 January 2018 Abstract: Thermal energy storage (TES) is a technology that stocks thermal energy by heating or cooling a storage medium so that the stored energy can be used at a later time for heating and cooling applications and power generation. TES systems are used particularly in buildings and in industrial processes. This paper is focused on TES technologies that provide a way of valorizing solar heat and reducing the energy demand of buildings. The principles of several energy storage methods and calculation of storage capacities are described. Sensible heat storage technologies, including water tank, underground, and packed-bed storage methods, are briefly reviewed. Additionally, latent-heat storage systems associated with phase-change materials for use in solar heating/cooling of buildings, solar water heating, heat-pump systems, and concentrating solar power plants as well as thermo-chemical storage are discussed. Finally, cool thermal energy storage is also briefly reviewed and outstanding information on the performance and costs of TES systems are included. Keywords: storage system; phase-change materials; chemical storage; cold storage; performance 1. Introduction Recent projections predict that the primary energy consumption will rise by 48% in 2040 [1]. On the other hand, the depletion of fossil resources in addition to their negative impact on the environment has accelerated the shift toward sustainable energy sources. -
Cryogenicscryogenics Forfor Particleparticle Acceleratorsaccelerators Ph
CryogenicsCryogenics forfor particleparticle acceleratorsaccelerators Ph. Lebrun CAS Course in General Accelerator Physics Divonne-les-Bains, 23-27 February 2009 Contents • Low temperatures and liquefied gases • Cryogenics in accelerators • Properties of fluids • Heat transfer & thermal insulation • Cryogenic distribution & cooling schemes • Refrigeration & liquefaction Contents • Low temperatures and liquefied gases ••• CryogenicsCryogenicsCryogenics ininin acceleratorsacceleratorsaccelerators ••• PropertiesPropertiesProperties ofofof fluidsfluidsfluids ••• HeatHeatHeat transfertransfertransfer &&& thermalthermalthermal insulationinsulationinsulation ••• CryogenicCryogenicCryogenic distributiondistributiondistribution &&& coolingcoolingcooling schemesschemesschemes ••• RefrigerationRefrigerationRefrigeration &&& liquefactionliquefactionliquefaction • cryogenics, that branch of physics which deals with the production of very low temperatures and their effects on matter Oxford English Dictionary 2nd edition, Oxford University Press (1989) • cryogenics, the science and technology of temperatures below 120 K New International Dictionary of Refrigeration 3rd edition, IIF-IIR Paris (1975) Characteristic temperatures of cryogens Triple point Normal boiling Critical Cryogen [K] point [K] point [K] Methane 90.7 111.6 190.5 Oxygen 54.4 90.2 154.6 Argon 83.8 87.3 150.9 Nitrogen 63.1 77.3 126.2 Neon 24.6 27.1 44.4 Hydrogen 13.8 20.4 33.2 Helium 2.2 (*) 4.2 5.2 (*): λ Point Densification, liquefaction & separation of gases LNG Rocket fuels LIN & LOX 130 000 m3 LNG carrier with double hull Ariane 5 25 t LHY, 130 t LOX Air separation by cryogenic distillation Up to 4500 t/day LOX What is a low temperature? • The entropy of a thermodynamical system in a macrostate corresponding to a multiplicity W of microstates is S = kB ln W • Adding reversibly heat dQ to the system results in a change of its entropy dS with a proportionality factor T T = dQ/dS ⇒ high temperature: heating produces small entropy change ⇒ low temperature: heating produces large entropy change L. -
A Critical Review on Thermal Energy Storage Materials and Systems for Solar Applications
AIMS Energy, 7(4): 507–526. DOI: 10.3934/energy.2019.4.507 Received: 05 July 2019 Accepted: 14 August 2019 Published: 23 August 2019 http://www.aimspress.com/journal/energy Review A critical review on thermal energy storage materials and systems for solar applications D.M. Reddy Prasad1,*, R. Senthilkumar2, Govindarajan Lakshmanarao2, Saravanakumar Krishnan2 and B.S. Naveen Prasad3 1 Petroleum and Chemical Engineering Programme area, Faculty of Engineering, Universiti Teknologi Brunei, Gadong, Brunei Darussalam 2 Department of Engineering, College of Applied Sciences, Sohar, Sultanate of Oman 3 Sathyabama Institute of Science and Technology, Chennai, India * Correspondence: Email: [email protected]; [email protected]. Abstract: Due to advances in its effectiveness and efficiency, solar thermal energy is becoming increasingly attractive as a renewal energy source. Efficient energy storage, however, is a key limiting factor on its further development and adoption. Storage is essential to smooth out energy fluctuations throughout the day and has a major influence on the cost-effectiveness of solar energy systems. This review paper will present the most recent advances in these storage systems. The manuscript aims to review and discuss the various types of storage that have been developed, specifically thermochemical storage (TCS), latent heat storage (LHS), and sensible heat storage (SHS). Among these storage types, SHS is the most developed and commercialized, whereas TCS is still in development stages. The merits and demerits of each storage types are discussed in this review. Some of the important organic and inorganic phase change materials focused in recent years have been summarized. The key contributions of this review article include summarizing the inherent benefits and weaknesses, properties, and design criteria of materials used for storing solar thermal energy, as well as discussion of recent investigations into the dynamic performance of solar energy storage systems. -
Principles of Dilution Refrigeration
Principles of dilution refrigeration A brief technology guide 3He 4He About the authors Dr Graham Batey Dr Gustav Teleberg Chief Technical Engineer ULT Product Manager United Kingdom Sweden Graham completed his PhD Gustav Teleberg gained in Low Temperature Physics his PhD in cryogenics at Nottingham University for astronomy at Cardiff in 1985 and joined Oxford University where he Instruments designing top developed miniature loading plastic dilution refrigerators to run in pulsed dilution refrigerators and heat switches for telescope magnets, a rotating dilution refrigerator, and dark applications. He joined Oxford Instruments in 2007 as matter systems installed deep underground. He was a Cryogenic Engineer where he worked on developing involved in designing Oxford Instruments’ KelvinoxTM the Cryofree® dilution refrigerator that today is known range of dilution refrigerators and the world’s leading as TritonTM. He also worked on several patented cryogen free range of dilution refrigerators – TritonTM, technologies for rapid sample exchange and heat which in 2010 received the Queen’s award for pipes for accelerated cooling. innovation. In 2011, Graham received ‘The Business & Innovation’ award from the Institute of Physics and was elected Fellow of the IOP. Dilution refrigerators Principles of dilution refrigeration By Graham Batey and Gustav Teleberg Published by: Oxford Instruments NanoScience Tubney Woods, Abingdon, Oxon, OX13 5QX, United Kingdom, Telephone: +44 (0) 1865 393200 Email: [email protected] www.oxford-instruments.com/nanoscience © Oxford Instruments Nanotechnology Tools Limited, 2015. All rights reserved. Dilution refrigerators History The dilution refrigerator was first proposed by Heinz London in the early 1950s, and was realised experimentally in 1964 at Leiden University. -
Approach to Absolute Zero 3
SERIES I ARTICLE Approach to Absolute Zero 3. 0.3 K to a Few Milli-Kelvin R Srinivasan In part 2 of this series we dealt with the 3He cryostat. By R Srinivasan is a Visiting Professor at the Raman pumping on liquid 3He bath a temperature down to 0.3 K Research Institute after can be attained. To reach still lower temperatures in the retiring as Director of the milli-Kelvin region one uses a dilution refrigerator. In this Inter-University part the principles of operation of a dilution refrigerator Consortium for DAE Facilities at Indore. will be described. Earlier, he was at the Physics Department of Introduction liT, Chennai for many years. He has worked in The 3He cryostat was described in part 2 of this series of articles. low temperature physics By reducing the pressure on the 3He bath one can reach a and superconductivity. temperature down to about 0.3K. To reach still lower temperatures Debye and Giauque suggested the adiabatic The previous articles of this series were: demagnetization of a paramagnetic salt. This one-shot technique 1. liquefaction of gases, was used till the development of the dilution refrigerator in the December1996. late sixties and early seventies. The dilution refrigerator has the 2. Approach to absolute zero, advantage that it provides continuous refrigeration down to February 1997. about 10 lnilli-Kelvin. The development of the dilution refrigerator had to await the availability of the rare isotope, 3He, of helium in sufficiently large quantities. This became possible around the early sixties. As mentioned in part 2, 3He is a Fermion while the more abundant isotope 4He is a Boson. -
Lecture 11. Surface Evaporation and Soil Moisture (Garratt 5.3) in This
Atm S 547 Boundary Layer Meteorology Bretherton Lecture 11. Surface evaporation and soil moisture (Garratt 5.3) In this lecture… • Partitioning between sensible and latent heat fluxes over moist and vegetated surfaces • Vertical movement of soil moisture • Land surface models Evaporation from moist surfaces The partitioning of the surface turbulent energy flux into sensible vs. latent heat flux is very important to the boundary layer development. Over ocean, SST varies relatively slowly and bulk formulas are useful, but over land, the surface temperature and humidity depend on interactions of the BL and the surface. How, then, can the partitioning be predicted? For saturated ideal surfaces (such as saturated soil or wet vegetation), this is relatively straight- forward. Suppose that the surface temperature is T0. Then the surface mixing ratio is its saturation value q*(T0). Let z1 denote a measurement height within the surface layer (e. g. 2 m or 10 m), at which the temperature and humidity are T1 and q1. The stability is characterized by an Obhukov length L. The roughness length and thermal roughness lengths are z0 and zT. Then Monin-Obuhkov theory implies that the sensible and latent heat fluxes are HS = ρLvCHV1 (T0 - T1), HL = ρLvCHV1 (q0 - q1), where CH = fn(V1, z1, z0, zT, L)" We can eliminate T0 using a linearized version of the Clausius-Clapeyron equations: q0 - q*(T1) = (dq*/dT)R(T0 - T1), (R indicates a reference temp. near (T0 + T1)/2) HL = s*HS +!LCHV1(q*(T1) - q1), (11.1) s* = (L/cp)(dq*/dT)R (= 0.7 at 273 K, 3.3 at 300 K) This equation expresses latent heat flux in terms of sensible heat flux and the saturation deficit at the measurement level. -
Heat and Thermodynamics Course
Heat and Thermodynamics Introduction Definitions ! Internal energy ! Kinetic and potential energy ! Joules ! Enthalpy and specific enthalpy ! H= U + p x V ! Reference to the triple point ! Engineering unit ! ∆H is the work done in a process ! J, J/kg More Definitions ! Work ! Standard definition W = f x d ! In a gas W = p x ∆V ! Heat ! At one time considered a unique form of energy ! Changes in heat are the same as changes in enthalpy Yet more definitions ! Temperature ! Measure of the heat in a body ! Heat flows from high to low temperature ! SI unit Kelvin ! Entropy and Specific Entropy ! Perhaps the strangest physics concept ! Notes define it as energy loss ! Symbol S ! Units kJ/K, kJ/(kg•k) ! Entropy increases mean less work can be done by the system Sensible and Latent Heat ! Heat transfers change kinetic or potential energy or both ! Temperature is a measure of kinetic energy ! Sensible heat changes kinetic (and maybe potential energy) ! Latent heat changes only the potential energy. Sensible Heat Q = m⋅c ⋅(t f − ti ) ! Q is positive for transfers in ! c is the specific heat capacity ! c has units kJ/(kg•C) Latent Heat Q = m⋅lv Q = m⋅lm ! Heat to cause a change of state (melting or vaporization) ! Temperature is constant Enthalpy Changes Q = m⋅∆h ! Enthalpy changes take into account both latent and sensible heat changes Thermodynamic Properties of H2O Temperature °C Sensible heat Latent heat Saturation temp 100°C Saturated Saturated liquid steam Superheated Steam Wet steam Subcooled liquid Specific enthalpy Pressure Effects Laws of Thermodynamics ! First Law ! Energy is conserved ! Second Law ! It is impossible to convert all of the heat supplied to a heat engine into work ! Heat will not naturally flow from cold to hot ! Disorder increases Heat Transfer Radiation Conduction • • A 4 Q = k ⋅ ⋅∆T QαA⋅T l A T2 T1 l More Heat Transfer Convection Condensation Latent heat transfer Mass Flow • from vapor Q = h⋅ A⋅∆T Dalton’s Law If we have more than one gas in a container the pressure is the sum of the pressures associated with an individual gas. -
Module P7.4 Specific Heat, Latent Heat and Entropy
FLEXIBLE LEARNING APPROACH TO PHYSICS Module P7.4 Specific heat, latent heat and entropy 1 Opening items 4 PVT-surfaces and changes of phase 1.1 Module introduction 4.1 The critical point 1.2 Fast track questions 4.2 The triple point 1.3 Ready to study? 4.3 The Clausius–Clapeyron equation 2 Heating solids and liquids 5 Entropy and the second law of thermodynamics 2.1 Heat, work and internal energy 5.1 The second law of thermodynamics 2.2 Changes of temperature: specific heat 5.2 Entropy: a function of state 2.3 Changes of phase: latent heat 5.3 The principle of entropy increase 2.4 Measuring specific heats and latent heats 5.4 The irreversibility of nature 3 Heating gases 6 Closing items 3.1 Ideal gases 6.1 Module summary 3.2 Principal specific heats: monatomic ideal gases 6.2 Achievements 3.3 Principal specific heats: other gases 6.3 Exit test 3.4 Isothermal and adiabatic processes Exit module FLAP P7.4 Specific heat, latent heat and entropy COPYRIGHT © 1998 THE OPEN UNIVERSITY S570 V1.1 1 Opening items 1.1 Module introduction What happens when a substance is heated? Its temperature may rise; it may melt or evaporate; it may expand and do work1—1the net effect of the heating depends on the conditions under which the heating takes place. In this module we discuss the heating of solids, liquids and gases under a variety of conditions. We also look more generally at the problem of converting heat into useful work, and the related issue of the irreversibility of many natural processes. -
Appendix B: Petroski
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Recap: First Law of Thermodynamics Joule: 4.19 J of Work Raised 1 Gram Water by 1 ºC
Recap: First Law of Thermodynamics Joule: 4.19 J of work raised 1 gram water by 1 ºC. This implies 4.19 J of work is equivalent to 1 calorie of heat. • If energy is added to a system either as work or as heat, the internal energy is equal to the net amount of heat and work transferred. • This could be manifest as an increase in temperature or as a “change of state” of the body. • First Law definition: The increase in internal energy of a system is equal to the amount of heat added minus the work done by the system. ΔU = increase in internal energy ΔU = Q - W Q = heat W = work done by system Note: Work done on a system increases ΔU. Work done by system decreases ΔU. Change of State & Energy Transfer First law of thermodynamics shows how the internal energy of a system can be raised by adding heat or by doing work on the system. U -W ΔU = Q – W Q Internal Energy (U) is sum of kinetic and potential energies of atoms /molecules comprising system and a change in U can result in a: - change on temperature - change in state (or phase). • A change in state results in a physical change in structure. Melting or Freezing: • Melting occurs when a solid is transformed into a liquid by the addition of thermal energy. • Common wisdom in 1700’s was that addition of heat would cause temperature rise accompanied by melting. • Joseph Black (18th century) established experimentally that: “When a solid is warmed to its melting point, the addition of heat results in the gradual and complete liquefaction at that fixed temperature.” • i.e.