Die organischen Verbindungen und Komplexe von Germanium,Zinn und Blei

This field is of special interest within the organometallic chemistry, which was and still is one of the most developing areas of chemistry for twenty years. The electronic structure around the atoms of germanium, tin, and lead favors both polar and radical reactions, and a plentiful coordination chemistry, too. Modern quantum chemistry arrived at these heavy atoms and allows better understanding also of low valent species, R₂M. Chiral compounds with asymmetric Sn atoms, an object aimed at since 1905, have been prepared now, and dynamic stereochemistry has been studied. Industrial use of organotins has grown quickly and includes stabilization of plastics and plant and material protection as well. Biomethylation and environmental problems open this field both to biochemists and ecologists.     

Reduktion der Erdalkalimetagermanate und Darstellung einiger Orthothiogermanate

The Science of Nature -     

Neue Hexafluorochromate(IV)

The Science of Nature -     

The effect of light on the Mn(II) or Fet(lll)-catalyzed oxidation of aqueous S(IV)

ＴｈｅｅｆｆｅｃｔｏｆｌｉｇｈｔｏｎｔｈｅＭｎ（ＩＩ）ｏｒＦｅｔｌｌｌ）ｘａｔａｌｙｚｅｄｏｘｉｄａｔｉｏｎｏｆａｑｕｅｏｕｓＳ（ＩＶ）ＸｕＹｏｎｇｆｕ（ＩｎｓｔｉｔｕｔｅｏｆＡｔｍｏｓｐｈｅｒｉｃＰｈｙｓｉｃｓ，ＣｈｉｎｅｓｅＡｃａｄｅｍｙｏｆＳｃ...     

Migration and transformation of Sb are affected by Mn(III/IV) associated with lepidocrocite originating from Fe(II) oxidation

Antimony (Sb) is a recognized priority pollutant with toxicity that is influenced by its migration and transformation processes. Oxidation of Fe(II) to Fe(III) oxides, which is a common phenomenon in the environment, is often accompanied by the formation of Mn(III/IV) and might affect the fate of Sb. In this study, incorporated Mn(III) and sorbed/precipitated Mn(III/IV) associated with lepidocrocite were prepared by adding Mn(II) during and after Fe(II) oxidation, respectively, and the effects of these Mn species on Sb fate were investigated. Our results indicated that the association of these Mn species with lepidocrocite obviously enhanced Sb(III) oxidation to Sb(V), while concomitantly inhibiting Sb sorption due to the lower sorption capacity of lepidocrocite for Sb(V) than Sb(III). Additionally, Mn oxide equivalents increased in the presence of Sb, indicating that Sb oxidation by Mn(III/IV) associated with lepidocrocite was a continuous recycling process in which Mn(II) released from Mn(III/IV) reduction by Sb(III) could be oxidized to Mn(III/IV) again. This recycling process was favorable for effective Sb(III) oxidation. Moreover, Sb(V) generated from Sb(III) oxidation by Mn(III/IV) enhanced Mn(II) sorption at the beginning of the process, and thus favored Mn(III/IV) formation, which could further promote Sb(III) oxidation to Sb(V). Overall, this study elucidated the effects of Mn(III/IV) associated with lepidocrocite arisen from Fe(II) oxidation on Sb migration and transformation and revealed the underlying reaction mechanisms, contributing to a better understanding of the geochemical dynamics of Sb.