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Manual for Refrigeration Servicing Technicians - UNEP - Division of ...

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Glossary<br />

hole in late 1985, governments recognized the need <strong>for</strong> firm measures to<br />

reduce the production and consumption <strong>of</strong> a number <strong>of</strong> CFCs (CFC-11,<br />

-12, -113, -114, and -115) and several Halons (1211, 1301, 2402). The<br />

Protocol was designed so that the phase-out schedules could be revised<br />

on the basis <strong>of</strong> periodic scientific and technological assessments. Following<br />

such assessments, the Protocol was adjusted to accelerate the phaseout<br />

schedules in 1990 (London), 1992 (Copenhagen), 1995 (Vienna), 1997<br />

(Montreal), 1999 (Beijing) and again in 2007 in Montreal.<br />

Multilateral Fund<br />

Part <strong>of</strong> the financial mechanism under the Montreal Protocol. The Multilateral<br />

Fund was established by a decision <strong>of</strong> the Second Meeting <strong>of</strong> the Parties to<br />

the Montreal Protocol (London, June 1990) and began its operation in 1991.<br />

The main objective <strong>of</strong> the Multilateral Fund is to assist Article 5 parties to the<br />

Montreal Protocol whose annual per capita consumption and production <strong>of</strong><br />

ODS is less than 0.3 kg to comply with the control measures <strong>of</strong> the Protocol.<br />

Non-condensable gases<br />

Gases with very low temperature boiling points, which are not easily<br />

condensed. Nitrogen and oxygen are the most common ones.<br />

Normal boiling point (NBP)<br />

The boiling point <strong>of</strong> a compound at atmospheric pressure (1.013 bar).<br />

Occupied space<br />

A completely enclosed space which is occupied <strong>for</strong> a significant period by<br />

people. The occupied space may be accessible to the public (<strong>for</strong> example<br />

supermarket) or only to trained persons (<strong>for</strong> example cutting up <strong>of</strong> meat).<br />

In an occupied space, both parts <strong>of</strong> a refrigerating system or the complete<br />

refrigerating system may be located/installed.<br />

Open compressor<br />

A compressor having a drive shaft penetrating the refrigerant-tight housing.<br />

Ozone depletion<br />

Accelerated chemical destruction <strong>of</strong> the stratospheric ozone layer by the<br />

presence <strong>of</strong> substances produced by human activities.<br />

Ozone depleting potential (ODP)<br />

A relative index indicating the extent to which a chemical product may cause<br />

ozone depletion compared with the depletion caused by R11. Specifically, the<br />

ODP <strong>of</strong> an ozone depleting substance is defined as the integrated change in<br />

total ozone per unit mass emission <strong>of</strong> that substance relative to the integrated<br />

change in total ozone per unit mass emission <strong>of</strong> R11.<br />

Ozone layer<br />

The layer in the stratosphere where the concentration <strong>of</strong> ozone is greatest.<br />

The layer extends from about 12 to 40 km. This layer is being depleted by<br />

anthropogenic emissions <strong>of</strong> chlorine and bromine compounds. Every year,<br />

during the Southern Hemisphere spring, a very strong depletion <strong>of</strong> the<br />

ozone layer takes place over the Antarctic region. This depletion is caused<br />

by anthropogenic chlorine and bromine compounds in combination with the<br />

specific meteorological conditions <strong>of</strong> that region. This phenomenon is called<br />

the Antarctic ozone hole.<br />

Ozone<br />

The triatomic <strong>for</strong>m <strong>of</strong> oxygen (O3), which is a gaseous atmospheric<br />

constituent. In the troposphere it is created by photochemical reactions<br />

involving gases occurring naturally and resulting from anthropogenic activities<br />

(‘smog’). Tropospheric ozone acts as a greenhouse gas. In the stratosphere<br />

ozone is created by the interaction between solar ultraviolet radiation<br />

and molecular oxygen (O2). Stratospheric ozone plays a major role in the<br />

stratospheric radiative balance. Its concentration is highest in the ozone<br />

layer.<br />

Ozone depleting substances (ODS)<br />

Substances known to deplete the stratospheric ozone layer. ODS controlled<br />

under the Montreal Protocol and its Amendments are chlor<strong>of</strong>luorocarbons,<br />

hydrochlor<strong>of</strong>luorocarbons, halons, methyl bromide, carbon tetrachloride,<br />

methyl chloro<strong>for</strong>m, hydrobrom<strong>of</strong>luorocarbons and bromochloromethane.<br />

Perfluorocarbons (PFCs)<br />

Synthetically produced halocarbons containing only carbon and fluorine<br />

atoms. They are characterized by extreme stability, non-flammability, low<br />

toxicity, zero ozone depleting potential and high global warming potential.<br />

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