Page 198 - Çevre Şehir ve İklim Dergisi İngilizce - Özel Sayı
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Use of Climate-Resilient Plants in Arid and Semi-Arid Lands


               According to the classification of barren soils, a total of 74% of the barren
            land  consists  of  saline  soils,  25.5%  consists  of  saline-alkali  soils,  and  0.5%
            consists of alkali soils.
               The formation of barren areas, their distinct characteristics, and their effects
            on plants are detailed in Table 2.


            Table 2: Formation, Characteristics, and Effects of Barrenness
            (Sözmez, 2003)
              BARRENNESS    NATURAL      PHYSICAL     CHEMICAL      IMPACT ON
              SITUATION    FORMATION     QUALITIES    QUALITIES       PLANTS



                                                     Sodium, calci-
                                                     um, and mag-  Salts increase the
                                         Salts help   nesium chloride   osmotic pressure
                                        clay particles   and sulfate   of the soil solution,
                          They are seen   aggregate and   neutral soluble   reducing water
                            in arid and   maintain the   salts dominate.   availability and
                            semi-arid
                           regions. They   soil in a stable   Its pH is less   causing physiolog-
              SALINE SOILS  generally form   structure. Their   than 8.2, elec-  ical drought.
                                        air and water
                                                      trical conduc-
                            under the
                                        permeability,
                                                      tivity (EC) is
                           influence of   along with other   higher than 4
                          seawater and in   properties, are   dS m-1, and the    Toxicity from
                            lake areas.
                                       similar to those   exchangeable   specific ions such
                                       of normal soils.  sodium percent-  as Na, Cl, B, etc.,
                                                     age (ESP) is less   may occur.
                                                        than 15.
                                       The structure is
                                       disrupted due to   Salts like
                                       the dispersion of   Na₂CO₃, which   The poor soil
                                           clays.     lead to alkali   structure and high
                          It occurs in arid   They have   hydrolysis, are   soil pH cause
                           and semi-arid   inadequate
                                                                    irregularities in
                          regions due to   drainage.   quite dense.  plant nutrition, and
                                                      A pH higher
                          the increase of   They generally
              ALKALI SOILS                            than 8.2 is a   the toxic effects of
                           sodium in the   become muddy   strong indicator   specific ions such
                           soil solution   and are slow to
                          caused by evap-  dry. When wet,   of alkalinity.  as Na, CO3-2, Mo,
                             oration.  they are greasy,   The exchangea-  and B negative-
                                                                    ly impact plant
                                                     ble sodium per-
                                         plastic, and
                                       sticky; when dry,   centage (ESP) is   growth.
                                                        typically
                                       they harden and
                                         form cracks.



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