Page 378 - Çevre Şehir İklim İngilizce - Sayı 4
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Settlement Model From Lowlands to Mountains
                                 May Prevent Carbon Dioxide Toxicity
               The Positive Effects of Carbon Dioxide on Plants

               As it is known, CO  is the basic input for plants to perform photosynthesis.
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            Idso and his team (1998), in their study on urban CO  dome of the Phoenix
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            city, found that CO  values in the afternoon are lower than pre-dawn values
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            since  urban vegetation probably consumes CO by photosyntesis, and stated
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            that  high  CO    concentrations  in  cities  could  show  positive  effects  on  the
                         2
            vegetation growing in the city. In a study conducted in Kuwait, it was found
            that following the seasons when plants bloom, CO values decrease and the
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            following the seasons when plants dry out, CO values increase (Nasrallah et al.,
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            2003). Lichtfouse and his team (2003) also conducted a study in Paris in which
            they revealed the contribution of CO  emitted from fossil fuels to plant tissues
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            with an isotope-based study. High CO  not only supports photosynthesis as a
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            raw material, but also supports the formation of urban heat islands in a small
            amount and promote plant growth in temperate regions (Rogers et al., 1999;
            Menzel and Fabian, 1999; Balling Jr. et al. 2001).
               It is necessary to apply spraying (fertilizing) CO  in under cover production
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            systems such as greenhouses, and when CO  values fall below 1200 ppm, the
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            efficiency decreases in parallel (Tezcan et al., 2011). When the carbon dioxide
            concentration in greenhouse air is increased, plants grow more; their growth
            rate can be increased by 100-200% and average yield by 50-55% (De Pascale
            and Maggio, 2008; Tezcan et al., 2011).

               Using the Lowlands For Agriculture, Slopes For Settlement
               Lowlands are available areas for agriculture; however, earthquakes have a
            destructive effect due to the growth of the amplitude of earthquake waves
            in lowlands (loose soils), liquefaction and ground displacement movements
            (Yilmazer, 2002:12; Yilmazer and Yilmazer, 2002). A striking example of this can
            be seen in the Düzce Plain. Faults heat the Düzce Plain from below, ventilate it
            and feed it with minerals; thus, they turn it into a productive agricultural land
            (Yılmazer et al., 2022). Düzce which was settled by the end of 19th century in
            the middle of a plain, has experienced many earthquake and flood disasters
            to  date;  on  the  other  hand,  the  thousands  of  years  of  historical  Konuralp
            adjacent to the fault/plain has not been damaged by earthquakes and floods
            (Yılmazer et al., 1999; Yilmazer et al., 2004, Yilmazer et al., 2020, Yilmazer et al.,
            2021) (Figure 3).











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