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    ECO MALAYSIA

    stop killing the planetSurah al-a raf ayat 56 bermaksud .dan janganlah kamu berbuat KEROSAKAN

    dibumi setelah diciptanya debgan baik. Berdoalah kepada tuhan dengan rasa takut dan

    penuh harap, sesungguhnya rahmat Allah sangat dekat kepada orang yang berbuat

    demikian

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    HEAT ISLAND (GLOBAL WARMING ) "Urban Heat Island" (UHI) refers to the tendency for a city to remain warmer than its

    surroundings. This effect is caused mostly by the lack of vegetation and soil moisture,

    which would normally use much of the absorbed sunlight to evaporate water as partof photosynthesis (a process called "evapotranspiration"). Instead, the sunlight is

    absorbed by manmade structures: roads, parking lots, and buildings. With little or no

    water to evaporate, the sunlight's energy goes into raising the temperature of those

    surfaces. After the sun sets, the city is so warm that it never cools down as much as

    the countryside around it, and so retains the heat island effect all night long. There is

    some evidence that the Urban Heat Island effect modifies the rainfall patternsaround cities, at least in the summertime.

    The first

    documentation on

    heat island occurs in

    1818 by Luke

    Howards

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    CAUSESCommon construction materials absorb and retain more of the suns heat. Most materials are

    impermeable and watertightDark materials can reach up to 80 c

    Less vegetation surface

    Human produced heat

    Slower wind

    Air pollution

    CAN CONTRIBUTE TO:Human discomfort

    Health problems

    Higher energy bills

    Increased pollutionGlobal warming

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    Five main causes of heat island.

    1. Reduced evaporator

    2. Increased heat storage

    3. Increased net radiation

    4. Reduced convection

    5. Increased anthropogenic heat

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    Characteristic contributing to heat

    urban heat island.Causes EffectsLack of vegetation Reduces evaporation

    Widespread used of impermeable

    surfaces

    Reduces evaporation

    Increased thermal diffusivity of urban

    material

    Increases heat storage

    Low solar reflectance of urban material Increases net radiation

    Urban geometric that slow wind speeds Reduces convection

    Increased levels of air pollution Increases net radiation

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    Man-made Causes

    Pollution:Burning fossil fuels is one thing that causes pollution. When fossil fuels are burned

    they give off a green house gas called CO2. Also, mining coal and oil allows methane to

    escape. How does it escape? Methane is naturally in the ground. When coal or oil is

    mined you have to dig up the earth a little bit. When you dig up the fossil fuels you dig

    up the methane as well letting it escape into the atmosphere.

    Population:More people means more food, and more methods of transportation. That means

    more methane because there will be more burning of fossil fuels, and more

    agriculture. If you've been in a barn filled with animals and you smelled something

    terrible, you were smelling methane. Another problem with the increasing population

    is transportation. More people means more cars, and more cars means more

    pollution. Since CO2 contributes to global warming, the increase in population makes

    the problem worse because we breathe out CO2. Also, the trees that convert our CO2

    to oxygen are being cut down. (trees are a very important part of our eco-system)

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    MITIGATION

    Trees and Vegetation Shade trees and smaller plants such as shrubs,

    vines, grasses, and ground cover, help cool the

    urban environment.

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    How It Works Trees and vegetation help cool urban climates through shading and

    evapotranspiration. Shading Leaves and branches reduce the amount of solar radiation that

    reaches the area below the canopy of a tree or plant.

    generally 10 to 30 percent of the suns energy reaches the area below a

    tree, with the remainder being absorbed by leaves and used for

    photosynthesis, and some being reflected back into the atmosphere. For example, a multi-month study measured maximum surface

    temperature reductions ranging from 20 to 45F (11-25C) for walls and

    roofs at two buildings. Another study examined the effects of vines on

    wall temperatures and found reductions of up to 36F (20C). A third

    study found that tree shading reduces the temperatures inside parked cars

    by about 45F (25C).

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    Tree canopies, such as the deciduous trees around this home in

    Virginia, can block much of the sunlight from reaching the ground or

    the building

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    evapotranspiration.

    Trees and vegetation absorb water through their roots and emit it through

    their leavesthis movement of water is called transpiration.

    Evaporation, the conversion of water from a liquid to a gas, also occurs

    from the soil around vegetation and from trees and vegetation as they

    intercept rainfall on leaves and other surfaces.

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    Benefits

    lower energy use,

    reduced air pollution and greenhouse gas emissions

    protection from harmful exposure to ultraviolet (UV) rays,

    decreased storm water runoff, potential reduced pavement maintenanced

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    Cool Roofs

    Cool roofing refers to the use of highly reflective and emissive materials. Cool roofing can help address the problem of heat islands, which results in

    part from the combined heat of numerous individual hot roofs in a city or

    suburb. Cool roofing products are made of highly reflective and emissive

    materials that can remain approximately 50 to 60F (28-33C) cooler than

    traditional materials during peak

    Traditional roof can create problems such as:

    1. Hotter indoor

    2. Reduced indoor comfort

    3. More energy used for cooling

    4. More money

    5. More wear on cooling system

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    Solar Energy

    Solar energy is composed of ultraviolet (UV) rays, visible light, and infraredenergy, each reaching the Earth in different percentages: 5 percent of solar

    energy is in the UV spectrum, including the type of rays responsible for

    sunburn; 43 percent of solar energy is visible light, in colors ranging from

    violet to red; and the remaining 52 percent of solar energy is infrared, felt as

    heat.

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    Solar Reflectance

    Solar reflectance, or albedo, is the percentage of solar energy reflected by

    a surface. Researchers have developed methods to determine solar

    reflectance by measuring how well a material reflects energy at each solar

    energy wavelength. Traditional roofing materials have low solar

    reflectance of 5 to 15 percent, which means they absorb 85 to 95 percent

    of the energy reaching them instead of reflecting the energy back out to

    the atmosphere. The coolest roof materials have a high solar reflectance

    of more than 65 percent, absorbing and transferring to the building 35

    percent or less of the energy that reaches them

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    Thermal Emittance

    A materials thermal emittance determines how much heat it will radiate

    per unit area at a given temperature, that is, how readily a surface givesup heat. When exposed to sunlight, a surface with high emittance will

    reach thermal equilibrium at a lower temperature than a surface with low

    emittance, because the high-emittance surface gives off its heat more

    readily.

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    Cool Roof Types

    Cool RoofCoatings.

    Coatings are surface treatments that are best applied to low-sloped roofsin good condition. They have the consistency of thick paint and contain

    additives that improve their adhesion, durability, suppression of algae and

    fungal growth, and ability to self-wash, or shed dirt under normal rainfall.

    EPDM (ethylene propylene diene monomer), a synthetic rubber material,

    with seams that must be glued or taped together. CSPE (chlorosulfonated polyethylene), a polymer material, with seams

    that can be heat-welded together.

    PVC (polyvinyl chloride) and TPO (thermoplastic olefins),

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    Cool pavingCover large percentage of urban and suburban areas.

    There is 2 way to make pavement cooler:

    1. By increasing their solar reflectance

    2. By increasing their ability to store and evaporate water.

    Conventional pavements in the United States are impervious concrete*

    and asphalt, which can reach peak summertime surface temperatures of

    120150F (4867C).2

    These surfaces can transfer heat downward to be stored in the pavement

    subsurface, where it is re-released as heat at night. The warmer daytime

    surface temperatures also can heat storm water as it runs off the

    pavement into local waterways.

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    TYPES OF COOL PAVING

    1 asphalt cement concrete (ACC)

    2 Portland cement concrete (PCC)

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    Current

    Future = global Warming