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This Programme:

''Reports 1 - 6'

Reports:

Bricking It - Zimbabwe

Cementing Alternatives - Zimbabwe

Fishing For Change

Holding Up The Himalayas - Nepa

Safa Tempos Nepal

Stop The Leak

Other Episodes:

Blood, Sweat and Business

From the Grass Roots

Vogue to Vehicle

What a Difference a Loan Makes

What a Lot of Rubbish

Who's Got the Power

Reports 25 - 31

Reports 19 - 24

Reports 13 - 18

Reports 7 - 12

Reports 1 - 6

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Series 1: Programme 1 of 11 'Reports 1 - 6'


Report 6 (of 6): Stop the leak!

Introduction

Life on earth has been safeguarded for thousands of years because of a life-protecting layer in the atmosphere. This layer, composed of ozone, acts as a shield to protect the earth against the harmful ultraviolet radiation from the sun. If it were to disappear, the sun's ultraviolet radiation would sterilise the surface of the globe, annihilating most terrestrial life.

The Ozone Layer

Ozone is a gas composed of three oxygen atoms, instead of the normal two. It is formed when powerful ultraviolet rays from the sun cause oxygen molecules to break apart into atoms which then react with other oxygen molecules to form ozone. Thus, ozone is naturally converted to oxygen (and vice-versa) by the sun's ultraviolet rays. Ozone is a trace gas found at altitudes between 15 and 60 kilometres which forms the ozone layer (figure 1).

The Effects of Ozone Depletion

The ozone layer is a vital part of the earth's atmosphere because it efficiently screens out almost all the harmful ultraviolet rays of the sun, by absorbing the most dangerous radiations, and therefore, preventing them from reaching the earth's surface. Any damage that is done to the ozone layer will lead to increased amounts of the dangerous ulraviolet radiations perforating the filter and reaching the earth's surface. Although a certain amount of ultraviolet rays are needed to support life, too many can create adverse effects on animal and plant life.

An increase in the risk of developing skin cancer and an increase in the incidents of eye damage, for example, cataracts and deformation of the eye lenses, are serious effects resulting from ozone depletion.

Increased ultraviolet radiation would cause changes in the chemical composition of several species of plants, resulting in decreased crop yields and damage to forests. The quality of certain types of crops, for example, tomatoes, potatos and soya bean, would also be reduced and the growth of others would be affected, for example, rye and maize.

Ultraviolet radiation affects ocean life and causes damage to aquatic organisms, for example, plankton, shrimp and aquatic plants, to a depth of 20 metres in clear waters. These organisms form part of the marine food web and a decrease in their numbers may lead to a decrease in fish higher up the food chain. Countries that rely heavily on fish as a fundamental food source could be seriously affected.

Materials used in buildings, paints, packaging and other substances could be degraded by ultraviolet radiation. Plastics that are used outdoors are most likely to be affected, and damage could be more severe in tropical regions where temperatures and levels of sunshine are high. The cost of such damage would be immense.

In order to contribute to ozone depletion, a substance must contain chlorine, hydrogen, nitrogen or another similar atom to participate in the ozone to oxygen chemical reaction. It must also be sufficiently stable in the lower atmosphere (troposphere) to allow it time to reach the ozone layer.

Chlorofluorocarbons (CFCs)

Chlorofluorocarbon (CFC) is a chemical compound consisting of one or more carbon atoms surrounded by chlorine and fluorine atoms. It is a "greenhouse gas" and, as such, contributes to the reduction of the earth's ozone layer. CFCs are manufactured for use in aerosol propellants, blowing agents for plastic foams, solvents and refrigerants.

A refrigerant is a fluid (liquid or gas) which transfers heat away from one point to another. It is used as a refrigeration device for chillers to cool water or air. In a typical vapour system the refrigerant changes from a liquid to a gas when it absorbs heat and changes back to a liquid when it gives up heat.

Most refrigerants used today for vapour compression air conditioning are called halocarbons. A halocarbon is a hydrocarbon molecule containing one or more halogens. The halogen elements most commonly used in refrigerants are chlorine and fluorine, and where this is the case, the refrigerants are CFCs.

Some CFCs have atmospheric lives of over 100 years and therefore, once these chemicals are emitted, they will influence the process of ozone depletion for a long time. Refrigerants are so stable that they do not breakdown in the troposphere. Instead, by forces of air circulation, they spread around the globe until they eventually reach the stratosphere (the upper part of the atmosphere) where they are exposed to powerful ultraviolet radiation which break apart the refrigerant chemical, releasing the chlorine. As the chlorine reacts with ozone, oxygen is created which, in turn, allows more ultraviolet light to pass toward the earth. The chlorine atom acts as a catalyst which means that it is not used up in the reaction but can continue to convert ozone to oxygen through thousands of similar reactions.

The concentration of CFCs in the atmosphere is increasing, mainly as a result of industrial activity, and as more gases are emitted, the atmospheric ozone gradually breaks down.

The Greenhouse Effect and Global Warming

The earth's temperature is maintained by a balance between heating from solar radiation flowing in from space, and cooling from infrared radiation emitted by the earth's warm surface and atmosphere escaping back to space. The sun is the earth's only external source of heat.

When solar radiation, in the form of visible light, reaches the earth's surface, it is partially absorbed by the atmosphere, and partially reflected from clouds and land, especially deserts and snow. The remainder is absorbed by the surface which is heated and in turn warms the atmosphere. The warm surface and atmosphere of the earth emit invisible infrared radiation.

Greenhouse gases act like a blanket and prevent much of the infrared radiation from escaping directly to space (figure 2). By slowing the release of the cooling radiation, these gases warm the earth's surface. This process is known as the greenhouse effect' because it works in a similar way to a greenhouse. Glass allows sunlight in but prevents some infrared radiation from escaping, warming the air (and plant life) inside it.

Although the greenhouse effect is essential for life and keeps the planet over 30 degrees centigrade warmer than it would otherwise be, enhanced global warming may have severe consequences. The presence of greenhouse gases is growing larger, due to mankind's activities, and produce an increasing concentration of heat trapping gases which causes the temperature of the earth's atmosphere to gradually rise.

Once a greenhouse gas is released to the atmosphere, it can contribute to global warming. The amount by which it does so depends on the capacity of the gas to absorb infrared energy and the amount of time that elapses before it is removed from the earth's atmosphere. The most obvious result of such warming would be a rise in sea level due to the thermal expansion of the oceans and melting of some ice land, for example, glaciers and snowfields.

Apart from CFCs, the greenhouse gases can all occur naturally, for example, water vapour and carbon dioxide, and therefore, the contribution CFCs make to global warming can be reduced by controlling and limiting the use of them.

The information provided below is a summary explanation of options available to protect the environment against CFC emissions in refrigeration systems. The decision to implement one of the alternatives documented requires careful consideration of a wide range of situation-specific parameters, many of which are not addressed here.

Preventing Unneccessary Release of Refrigerants

In the short term, preventing unneccessary release of refrigerants can only be achieved by reducing refrigerant losses from existing systems. The three main sources of refrigerant losses are intrinsic leaks within the system; accidental leaks, for example, over pressuring and release through a relief valve; and emission due to transfer or maintenance - emptying or filling systems - because of bad practices.

Leak tests should be performed at regular intervals and if a leak is found, the refrigerant should be recovered from the system, the leak should be repaired and the system should be rechecked to ensure that the repairs are effective. The whole system should be tested and any leaks found marked so they can be easily repaired.

New service procedures should be introduced to avoid the venting of any refrigerant. For example, refrigerants should be recovered from the system prior to repair; after the liquid refrigerant has been removed from the system, the remaining vapour charge must be properly recovered for reuse in the system; refrigerant-contaminated components must be disposed of in an environmentally acceptable manner so they do not vent the atmosphere; and there are new service tools available to minimise emissions when opening refrigerant drums.

Equipment Retrofit/Replacement Strategy

The equipment retrofit/replacement strategy aims to eliminate CFCs through either retrofitting CFC chillers, that is, replacing an old refrigerant with a new one in an existing system, or replacing CFC chillers with newer systems that use environmentally acceptable alternative refrigerants. Chiller retrofits and replacements involve considerable cost which will depend on the compatibility of materials, the efficiency and capacity of the system, the leakage rate and type of drive.

Refrigerant Recycling

Refrigerant recycling is an attempt to remove some contaminants and return the refrigerants to the chiller cleaner than it was when recovered by oil separation, non-condensable removal and core filter-driers which reduce moisture, acidity and particulate matter.

There are two types of recycling equipment : single pass or multipass, which refer to whether the refrigerant passes through the equipment once or many times. Equipment is available to recycle in the vapour phase or in the liquid phase.

For vapour phase recycling, the refrigerant vapour is drawn into the recycling device, the oil is separated out, filtered and reintroduced into the chiller. Alternatively, the recycled refrigerant is recycled into the original pressure vessel, recirculating through the recycling device several times.

For liquid phase recycling, the refrigerant is drawn off through the liquid valve of the recovery vessel and introduced into the recycling device where the refrigerant is evaporated and the oil is separated. It is then cleaned and condensed through filters and introduced into a clean storage vessel. In multipass systems, the refrigerant is recycled back into the recovery storage.

Recovery Equipment

Refrigerant recovery is the removal of refrigerant from a piece of equipment, such as a chiller, to a suitable external storage container (figure 3). Three types of recovery apparatus are available: a self-contained recovery unit has its own compressor to pump the refrigerant out of the chiller; a system- dependent recovery unit relies upon the pressure of the refrigerant in the appliance to assist in the recovery; passive recovery refers to a deflated bag on an activated charcoal canister which is used to store small amounts of refrigerant near or above atmospheric pressure.

The method of refrigerant recovery depends upon the type of refrigerant being recovered - high pressure where the boiling point of the refrigerant is between -50 and 10 degrees centigrade at atmospheric pressure; and low pressure where the boiling point is above 10 degrees centigrade at atmospheric pressure and the liquid refrigerant is recovered first.

Reclaiming Refrigerants

Reclaiming is a process which removes contaminants and purifies refrigerants to the same standard as new refrigerants and is generally done at specially designated factories.

For governments and companies with a special interest in recycling, recovery and reclaiming refrigerants, please contact the United Nations Environment Programme at the address given below for more information on the appropriate equipment required and the training materials available.

The Montreal Protocol

The Montreal Protocol, in 1987, identified the main ozone depleting substances and set specific limits on their production levels in the future. Amendments made to the Protocol in 1992 established phase out schedules for all CFCs. A ten year grace period for developing countries was granted to allow them to expand their economies without hinderance by CFC phase out but by 2006 all CFCs must be eliminated.

For further information please contact:

United Nations Environment Programme Industry and Environment 39-43 Quai Andre Citroen 75739 Paris Cedex 15 France

Multilateral Fund for the Implementation of the Montreal Protocol 1800 McGill College Avenue, 27th Floor Montreal, Quebec H3A 3JC Canada

A 25 minute UNEP video produced by TVE for the refrigeration trade is available at the cost of copying and posting the video cassette.

Please contact: Dina Junkermann, TVE Distribution Manager at tve-dist@tve.org.uk
Or write to: TVE International
Prince Albert Road
London NW1 4RZ
United Kingdom


TVE/ Practical Action gratefully acknowledge support for the HANDS ON programmes from the UK's Department for International Development (DFID), the European Commission (EC), the UN Foundation and UNDP/The Equator Initiative in collaboration with the Government of Canada, IDRC, IUCN, BrasilConnects and the Nature Conservancy.

 

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