© Benaki Phytopathological Institute
        
        
          Effect of superphosphate on glyphosate adsorption in soil
        
        
          31
        
        
          ing contrasting Danish surface soils, have re-
        
        
          vealed that adsorption of glyphosate and
        
        
          phosphate can be both competitive and
        
        
          additive, with the competition not always
        
        
          been as pronounced. Adsorption of the two
        
        
          anions seems actually to be only partially
        
        
          competitive.
        
        
          Increased glyphosate and AMPA adsorp-
        
        
          tion following the addition of superphos-
        
        
          phate fertilizer was observed with the two
        
        
          most acidic soils (KA1 and H1) and the fact
        
        
          that this superphosphate amendment de-
        
        
          creased the pH of these two soils to even
        
        
          lower values in the acidic range seems to
        
        
          contribute to that. It is well established that
        
        
          glyphosate and phosphate adsorption is
        
        
          mostly contributed to aluminium and iron
        
        
          in acid soils and to calcium in alkaline soils.
        
        
          Changing the pH of the soil from the alka-
        
        
          line to the acidic range would increase ad-
        
        
          sorption since higher charged cations (Al
        
        
          3+
        
        
          ,
        
        
          Fe
        
        
          3+
        
        
          ) are capable of complexing more gly-
        
        
          phosate than lower charged cations (Ca
        
        
          2+
        
        
          ).
        
        
          Furthermore, with decreasing pH both the
        
        
          clay and glyphosate become less negative-
        
        
          ly charged and thus more interactive (more
        
        
          adsorption). The pH and glyphosate adsorp-
        
        
          tion patterns of KA1 limed soil samples (Fig-
        
        
          ure 5) and of the H3 acidified soil samples
        
        
          (Figure 6) in this study further document the
        
        
          validity of theses statements.
        
        
          The strong acidifying action of the su-
        
        
          perphosphate fertilizers in the soil is already
        
        
          known (1). When granules of the fertilizer
        
        
          are incorporated into the soil, the sparing-
        
        
          ly soluble calcium dihydrogen phosphate
        
        
          [Ca(H
        
        
          2
        
        
          PO
        
        
          4
        
        
          )
        
        
          2
        
        
          ], which they contain, absorbs
        
        
          water and is hydrolyzed to calcium hydro-
        
        
          gen phosphate [CaHPO
        
        
          4
        
        
          ] and ortho-phos-
        
        
          phoric acid (H
        
        
          3
        
        
          PO
        
        
          4
        
        
          ). The three phosphate
        
        
          compounds coexist in an equilibrium, form-
        
        
          ing the so called “triple point solution”, with
        
        
          a pH of 1.0-1.5, which diffuses around the
        
        
          granules in the soil. It seems, therefore, that
        
        
          in acidic and neutral soils the ortho-phos-
        
        
          phoric acid, during diffusion of the triple
        
        
          point solution, lowers the soil pH and sol-
        
        
          ubilizes aluminium and iron oxides thus in-
        
        
          creasing the adsorption capacity of the soil.
        
        
          In alkaline calcareous soils, however, the or-
        
        
          tho-phosphoric acid is more quickly neutral-
        
        
          ized by calcium carbonate and precipitates
        
        
          as insoluble tricalcium phosphate, thus be-
        
        
          ing unable to affect glyphosate adsorption.
        
        
          Many other fertilizers are known to alter
        
        
          soil pH and it would be of interest to exam-
        
        
          ine how they affect glyphosate and AMPA
        
        
          adsorption.
        
        
          
            Literature Cited
          
        
        
          Analogidis, D. 1995. The agricultural fertilizers.
        
        
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          Borggaard, O.K. and Gimsing A.L. 2008. Fate of
        
        
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