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L1644_C03.fm  Page 80  Tuesday, October 21, 2003  3:11 PM










                              TABLE 3.2
                              GWP for Some Substances Depending on the Time Horizon
                                                                                GWP
                                                                         (kg CO 2  eq./kg substance)
                                 Substance     Formula    Lifetime years
                                                                      20 years  100 years  500 years
                              Carbon dioxide     CO 2        150         1       1        1
                              Methane            CH 4        14.5       62      24.5      7.5
                              Nitrous oxide      N 2 O       120        290      320      180
                              Source: Data taken from Houghton et al., 1995.


                                CO  was chosen as a reference substance by the IPCC because it makes the
                                   2
                             most significant contribution to the manmade greenhouse effect. The expected con-
                             tribution in terms of warming from a greenhouse gas is calculated based on knowl-
                             edge of its specific IR absorption capacity and its expected lifetime in the atmo-
                             sphere. The GWP is internationally accepted and well documented, and provides
                             characterization factors for the substances encountered in an LCA. Table 3.2 presents
                             examples of GWP  values for direct contribution of three substances mentioned
                             previously: CO , CH  and N O.
                                                    2
                                             4
                                         2
                             3.3.3  STRATOSPHERIC OZONE DEPLETION
                             Human activities have caused an increase of substances as different chloride and
                             bromide-containing halocarbons, especially CFCs, tetrachloromethane, 1,1,1-
                             trichloroethane, HCFCs, halons and methyl bromide, involved in the breakdown of
                             ozone in the stratosphere. A common characteristic of these compounds is that they
                             are chemically stable because they can survive long enough to reach the stratosphere,
                             where they can release their content of chlorine and bromide under the influence of
                             UV radiation (Solomon and Albritton, 1992).
                                The Earth’s atmosphere receives ultraviolet radiation from the sun but not at full
                             intensity. Ozone molecules in the atmosphere absorb large quantities of UV radiation.
                             The reduction of the ozone layer supposes that more UV radiation reaches the surface
                             of the earth and causes damage, especially to plants, animals and humans.
                                Table 3.3 presents a list of factors to calculate the stratospheric ozone depletion
                             potential of different chemical substances expressed in kilograms of CFC-11 (Freon
                             11) equivalent as a reference.

                             3.3.4  HUMAN TOXICITY
                             Chemical emissions such as heavy metals, persistent organic substances (POPs),
                             volatile organic compounds (VOCs) and others may lead to direct human exposure
                             (inhalation or drinking  water) or to indirect  exposure (food consumption). Apart
                             from their toxicity, these substances are all persistent as common characteristics
                             (low degradability in the environment and ability to bioaccumulate). In contrast to
                             other impact categories, e.g., global  warning and ozone depletion, no common


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