Solar, Vacuum and Radio- Frequency Drying of Wood Forestry 486 Lecture 3-6.

Slides:



Advertisements
Similar presentations
Heat and Air Temperature
Advertisements

Chapter 16: Weather Factors
Solar Radiation and Insolation
Seasons.
Earth’s Global Energy Balance Overview
Chapter 2 Solar Heating. (Variations in) Solar Heating Power Weather Important Global and Seasonal Variations: Low latitudes receive more solar heating.
Chapter 22 Section 2 Review Page 560
Energy Ability to do work Many different forms Conservation of energy (Law) Transformed: example: – Radiant to Thermal – Kinetic to Thermal (friction)
Chapter 17 Study Guide Answers
Chapter 22 Section 2 Review Page 560 #’s 1-9
Chapter 6 part 2 Passive Solar Space Heating
Handout (yellow) Solar Energy and the Atmosphere Standard 3 Objective 1 Indicators a, b, and c Standard 3 Objectives 1, 2, and 3 Workbook Pages 3,
Lecture 3.1 Solar energy. This week we’ll contemplate little things like… Why there’s life on Earth Why you don’t want to live at the South Pole Why you.
Solar Energy & the Atmosphere
Solar Energy and the Atmosphere
1 Met 10 Weather Processes Jeff Gawrych Temperature, Heat Transfer and Earth’s Energy Balance.
EARTH’S CLIMATE. Latitude – distance north or south of equator Elevation – height above sea level Topography – features on land Water Bodies – lakes and.
WEATHERCLIMATE  The state of the atmosphere at a given time and place  Combination of Earth’s motion and sun’s energy  Influences everyday activities.
Objectives Explain how radiant energy reaches Earth.
Solar Radiation and Insolation Incoming solar radiation:
Earth Science Golodolinski/Black 2009
Mini Lesson 1: Energy transfer - Radiation
Unit 6.  Climate – the average weather conditions of an area over a long period of time  Weather is the day to day conditions *Climate you expect and.
Climate Chapter 25. Climate – the average weather conditions of an area over a long period of time –But weather is the day to day conditions Climate you.
Ch Solar Energy and the Atmosphere
Solar energy The photons take a long time to reach the surface of the sun, about 1 million years. Why? Deep in the sun, the density is very high. The photons.
Solar Energy and the Atmosphere
The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.
Basic Geoscience Unit 5 Lecture.
Weather Review. Air Masses Air Mass – A large body of air through which temperature and moisture are the same. Types 1. Continental – formed over land.
Understanding the Greenhouse Effect:  Learning Objectives : 1) Relate strength of the greenhouse effect to common experience (i.e. its generally warmer.
Topic 6. Without energy from the sun, conditions on Earth would be different. What is the energy that is radiated from the Sun? The energy that is radiated.

Solar Energy Heat and Light. Energy Can take many different forms –____________ –Heat –____________.
HEATING EARTH’S SURFACE AND ATMOSPHERE. INTERESTING The sun radiates to the Earth phenomenal amounts of energy, too much, in fact… We term this quantity.
Satellite Image Basics  Visible: Senses reflected solar (lunar) radiation Visible –Cloud thickness, texture; not useful at night  Infrared (IR): Senses.
17.1 Atmosphere Characteristics
Earth’s climate and how it changes
Solar Lumber Kilns Jake Altemus. The Sun  Provides huge amounts of “low intensity energy” (Wengert and Oliveria)  Really Dispersed.
Heat in the Atmosphere The sun’s energy is transferred to earth and the atmosphere three ways Radiation, Convection and Conduction.
The Atmosphere: Structure and Temperature
17 Chapter 17 The Atmosphere: Structure and Temperature.
Heat Transfer, Albedo, and the Natural Greenhouse Effect.
Journal #22 What is the purpose of a barometer? What is the most commonly used barometer?
How much makes it through the atmosphere. Why a seasonal variation? First, why do we have seasons? Earth’s axis is tilted 23.5° to the plane of its orbit.
Insolation INcoming SOLar radiATION Strength is dependent on 1.Angle of insolation 2.Duration of insolation 3.Type of surface receiving the insolation.
INSOLATION Incoming Solar Radiation Portion of sun’s output of electromagnetic radiation that is received by earth.
Topic 6: Insolation and the Earth ’ s Surface. Insolation- The portion of the Sun ’ s radiation that reaches the Earth INcoming SOLar RadiATION Angle.
23.2 Solar Radiation & the Atmosphere Electromagnetic Radiation The EM spectrum Radiation is energy that does no require matter to travel. It travels as.
Journal #27 What were your results from yesterday? Why did you get the results you did?
Chapter 17 Study Guide Answers
Unit 9 Section 2: Solar Energy and the Atmosphere
Disciplines of Science, ch. 16
TOPIC 6 INSOLATION.
Planetary Energy Budget
Today's Outline Topic: Energy Transfer Class Outline: - Weather Tracking - Energy Transfer note - Worksheet - Start a documentary Today’s Assigned.
Heat in the Atmosphere.
Solar Power Power derived directly from sunlight
Radiation.
Influences on temperature Random Air pressure
Seasons of Change 22 September 2014.
Solar Energy and the Atmosphere
DO NOW Turn in Review #13. Pick up notes and Review #14.
Section 2: Solar Energy and the Atmosphere
“Energy in Earth Processes”
The Greenhouse Effect Electromagnetic (EM) radiation, radiation processes “Clear Sky” Exercise Earth-Sun System Greenhouse Gases “Cloudy Sky” Exercise.
Atmosphere & Solar Energy
Heat in the Atmosphere.
Energy Transfer & Heat Transference cont.
Unit 5: Energy The Transfer of Energy between the Sun, Earth’s Surface and our Atmosphere.
Presentation transcript:

Solar, Vacuum and Radio- Frequency Drying of Wood Forestry 486 Lecture 3-6

Solar Drying Basics Characteristics of solar energy: – Low intensity solar “insolation” (amount of available energy): approx. 428 BTU/hr/ft 2 in the upper atmosphere vs BTU/hr/ft 2 at surface due to interception by clouds etc. – Intermittent (day vs. night; seasonal variation) – Subject to interruption (cloud cover, smoke, etc.)

Solar Drying Basics Classes of solar radiation: – Ultraviolet (UV): < 0.38 μm wavelength, approximately 7% of solar radiation – Visible: μm, 47% – Infrared (IR): > 0.78 μm, 46%. (lower wavelength, e.g., UV=higher energy light)

Solar drying basics… Available energy influenced by angle of incidence; determined by position of sun in the sky and the collector tilt angle A “rule of thumb” for north temperate region is to set collector tilt angle as follows: – Summer, latitude – 10 o – Winter, latitude +15 o

Types of Solar Collectors used for wood drying “Hothouse” – not unlike a plant greenhouse External collectors – Heat transfer medium Air; low “energy volume” Liquid; efficient but more complicated – Flat plate collectors – Concentrating collectors, e.g., parabolic mirror with sun tracking capability

Solar Drying A home-built solar drier can provide quality lumber drying at an accelerated rate 4/4 hardwood may be dried in 6 weeks of good weather 8/4 hardwood may be dried in 15 weeks

Greenhouse-design solar dry kiln

Semi-greenhouse design

Solar dry kiln with external collector

Solar drying attributes Can dry wood 2-3x faster than air drying Can dry to 7-12% final MC Can reduce casehardening by shutting off fans and/or vents at night (increase EMC during evening hours) Largest design I’ve seen was for 50Mbf Most are used by hobbyists or in developing countries (not a bad idea for tropical regions with greater amount of sunlight)

Solar Drying References “Improvements in Solar Dry Kiln Design”, available at “Constructing and Operating a Small Solar-Heated Lumber Dryer” Chen, P.Y.S Design and tests of a 500 bf solar dry kiln. Forest Products Journal 31(3): Tschernitz, J.L., and W.T. Simpson Design for lumber dry kiln using solar/wood energy in tropical latitudes. Drying Technology 4(4): Lumley, T.G., and E.T. Choong Technical and economic characteristics of two solar kiln designs. Forest Products Journal 29(7):49-56.

Solar/Dehumidification Drying References Chen, P.Y.S., W.A. Helmer, and H.N. Rosen Energy efficient lumber dry kiln using solar collectors and refrigeration systems. United States Patent No. 4,432,147. Helmer, W.A., and P.Y.S. Chen Computer simulation of a new method to dry lumber using solar energy and absorption refrigeration. Wood and Fiber Science 17(4):

Additional References on Drying Small Quantities of Lumber Miceli, C.M., H.N. Rosen, and H.A. Spalt Drying small quantities of green hardwoods. U.S. Department of Agriculture, Forest Service, North Central Forest Experiment Station Research Paper NC-228. Bois, P.J., E.M. Wengert, and R.S. Boone A checklist for drying small amounts of lumber. U.S. Department of Agriculture, Forest Service, Forest Products Laboratory. Forest Products UtilizationTechnical Report No. 6.

Vacuum Drying of Lumber Use of vacuum permits a low EMC condition at lower temperature than conventional Advantageous for refractory species, thick stock, color maintenance Time and energy savings possible Russian vacuum lumber driers

Vacuum may be used to dry wood at lower temperatures - Example An oven set at 102 o C, operating in a room at 20 o C and 50% RH will have a relative humidity in the oven of 1.1% and corresponding EMC of 0.2% A vacuum oven with an absolute pressure of 0.13 kpa at 50 o C, in the same 20 o C/50%RH room will also have a 1.1% RH and 0.2% EMC. See Siau 1995, p. 13

Vacuum drying… Various means are used for heat transfer, including: – Convective heat transfer…inefficient and ineffective in a partial vacuum. May use alternating vacuum and atmospheric pressure – Steam-heated platens or electrically-heated conductive blankets in contact with lumber (see fig of DKOM) – Radio-frequency energy (see papers by Avramidis et al. for principles of operation)

See pix from Zwick and Lamb pdfs to illustrate vacuum & vacuum/rf kilns…

RFV References Avramidis, S., R.L. Zwick, and J.B. Neilson Commercial scale RF/V drying of softwood lumber. Part I. Basic kiln design considerations. For. Prod. J. 45(5): Avramidis, S. and R.L. Zwick Commercial scale RF/V drying of softwood lumber. Part II. Drying characteristics and lumber quality. For. Prod. J. 46(6): Avramidis, S. and R.L. Zwick Commercial scale RF/V drying of softwood lumber. Part III. Energy consumption and economics. For. Prod. J. 47(1):48-56.