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Bilgi Sarihan - Ramazan Acar Çakır
                                            Aydın Uzun

                With the model approach, it is aimed to present the wind erosion situation at
              the national scale and, when necessary, at different watershed sizes, as part of the
              outcomes of the study. At the end of 2018, after updating all the parameters of
              the model, the map showing the amount of sediment transported due to wind
              erosion and the areas with wind erosion potential at the national scale revealed
              that, in the initial findings, severe and very severe wind erosion sensitivity was
              calculated for an area of 1.2 million hectares.  Spatially, the Kızılırmak, Konya,
              and Dicle-Fırat basins stand out as the basins with the highest sensitivity. At the
              local scale, Konya-Karapınar, Iğdır-Aralık, and some coastal dunes exhibit high
              sensitivity.  The model study has revealed that wind erosion sensitivity is very severe
              in arid and semi-arid areas with vast plains, lacking vegetation cover, exposed to
              strong winds, with a long and significant soil moisture deficit, and areas that have
              undergone land degradation and are on the verge of desertification, as well as
              in dunes. At the same time, the model plays an important role in identifying the
              areas that serve as the material source for sand-dust storms.

                2.3. Marginal Areas

                Another  significant  issue  in  arid  and  semi-arid  areas  is  the  threat  of
              salinization-alkalization (barrenness), which is also referred to as marginal land.
              According to the World Soil Map data, it is reported that 954 million hectares
              of  land  worldwide  have  experienced  a  significant  decrease  in  agricultural
              productivity  due  to  salinity  issues.  Salinity  occurs,  especially  in  agricultural
              areas, in dry and semi-arid regions where improper irrigation methods and
              weak drainage are present (Ekmekçi, 2005).
                According to the salinity-alkalinity criteria of the Turkey’s Developed Soil Map
              Studies (1966-1971), there is salinity (salinization-alkalization) in 1,518,722 hectares
              of land in the country. According to the Provincial Land Resources Reports of
              the General Directorate of Village Services, the total area in the country affected
              by drainage and salinity problems is 2,569,297 hectares (Sönmez, 2003). The salt
              that accumulates in the soil alter its physical and chemical structure, hindering
              the development of plants in the region (Güngör, 1993).


              Table 1: Classification of Arid Soils (U.S. SalinityLab. Staff, 1954)

                                           Exchangeable
                Total Salt (%)  EC dS/m                      pH         Soil Type
                                            Sodium (%)
                   0.15<          4<           15>          8.5>        Saline Soil
                   0.15<          4<           15<          8.5<       Saline-Alkali
                   0.15>          4>           15<          8.5-10       Alkali



              184 Journal of Environment, Urban and Climate
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