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               Hexaaquairon(III) ions are cationic Brønstedt acids:
                                                          2+
                                3+
                      [Fe(H 2O) 6]  + H 2O ' [Fe(H 2O) 5OH]  + H 3O +                        pK S1 = 2.2
                                                                  +
                                     2+
                      [Fe(H 2O) 5(OH)]  + H 2O ' [Fe(H 2O) 4(OH) 2]  + H 3O +                pK S2 = 3.5
                                      +
                      [Fe(H 2O) 4(OH) 2]  + H 2O ' [Fe(H 2O) 3(OH) 3] (= Fe(OH) 3·aq) + H 3O +  pK S3 = 6.0

               The formation of ferric hydroxide Fe(OH) 3·aq hence already starts in weakly acidic media. The
               protolytic reactions are accompanied by condensation reactions, leading to hydroxido- and
               oxido-bridged aggregates and finally to colloids and hardly soluble ferric oxide hydrates. The
                                                                      5
               colloids can be spheroids of molecular mass M ca. 1.5⋅10  Da and ca. 70 Å diameter, or
                                       6
               needles/rods (M = 1.9·10 , length up to 500 Å). The composition of these ironoxide hydrates
               correspond to that of the minerals  FeO(OH) (goethite) and 5Fe 2O 3·9H 2O (ferrihydrite).


                                                 OH 2  H   OH 2     4+                OH 2     OH 2     2+
                               -H 2O, -2H +  H 2O     O        OH 2     -2H +   H 2O       O       OH 2
                2[Fe(H 2O) 6] 3+                 Fe        Fe                         Fe       Fe
                                           H 2O       O        OH 2             H 2O       O
                                                      H                                            OH 2
                                                 OH 2      OH 2                       OH 2     OH 2


                                                                            Fe
                                                                    H   O
                                                                    O
                                                                Fe      Fe
                                                                     O
                                                    Kolloide
                                                  Colloids     H O
                                                                   Fe
                                 3+
               Mobilisation of Fe  by siderophores

                                                                                 -39
               The extremely low solubility of Fe(OH) 3 [solubility product L = 2·10 , solubility (pH 7) l =
                         -1
                 -18
               10  mol·l ], and thus the unavailability of iron in aqueous media under oxic conditions, has
               forced many groups of organisms to develop suitable systems for the mobilisation of iron.
               These systems, so-called siderophores (Greek for iron transporter), excreted by the organisms,
                                                                                            3+
               are multidentate anionic ligands which form extremely stable complexes with Fe  (complex
                                              -1
                                          50
               formation constants up to 10  M ). The functional groups of these ligands are, in many cases,
               catecholates (o-
               hydroxyquinolates), as in
               the case of enterobactin, or            O  -     O             O  -                   3-
               hydroxamates                 Catecholate  -O  HN      O   NH O  -
               (ferrioxamines and                                  O       O              O  O  O
               ferriochromes). The                   O -     O   O   O                    O  Fe  O
               complexes are more or less   R        O -               O                     O
               globular, with the outer                        O   NH
               sphere furnished with                   Enterobaktin  O  - -   Fe 3+ -Enterobaktin-Komplex
               hydrophilic groups (amide                            O
               and ester groups), allowing                                O  NH  O  NH  O
               for the water solubility and        Hydroxamate       NH     NH    NH    NH
               easy transport in the aquatic           O               O      O      O
               medium. Internalisation of         R-C   N  O  -           (C H 2)3 O  -  (C H 2)3  -  (C H 2)3 O  -
                                                                          N
                                                                                 N
                                                                                        N
                                                                                   O
               the iron-loaded siderophore             R'                 C  O   C  O   C  O
               by the organism typically                          Ferrichrom  CH 3  CH 3  CH 3
                                                                                                       3+
               takes place by endocytosis; the cytosolic remobilisation of the iron either by reduction of Fe
                   2+
               to Fe  and recycling of the siderophore, or by oxidative destruction of the siderophore.
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