Nickel

About: Nickel is a research topic. Over the lifetime, 79308 publications have been published within this topic receiving 1210058 citations. The topic is also known as: Ni & element 28.

Nickel requirement for active hydrogenase formation in Alcaligenes eutrophus.

Abstract: The nickel-dependent chemolithoautotrophic growth of Alcaligenes eutrophus is apparently due to a requirement of nickel for active hydrogenase formation. Cells grown heterotrophically with fructose and glycerol revealed a specific activity of soluble and membrane-bound hydrogenase which was severalfold higher than the normal autotrophic level. The omission of nickel from the medium did not affect heterotrophic growth, but the soluble hydrogenase activity was reduced significantly. In the presence of ethylenediaminetetraacetic acid (EDTA), almost no hydrogenase activity was detected. The addition of nickel allowed active hydrogenase formation even when EDTA was present. When chloramphenicol was added simultaneously with nickel to an EDTA-containing medium, almost no hydrogenase activity was found. This indicates that nickel ions are involved in a process which requires protein synthesis and not the direct reactivation of a preformed inactive protein. The formation of the membrane-bound hydrogenase also appeared to be nickel dependent. Autotrophic CO2 assimilation did not specifically require nickel ions, since formate was utilized in the presence of EDTA and the activity of ribulosebisphosphate carboxylase was not affected under these conditions.

The ubiquity of iron.

Abstract: The importance of iron in living systems can be traced to the many complexes within which it is found, to its chemical mobility in undergoing oxidation–reduction reactions, and to the abundance of iron in Earth’s crust. Iron is the most abundant element, by mass, in the Earth, constituting about 80% of the inner and outer cores of Earth. The molten outer core is about 8000 km in diameter, and the solid inner core is about 2400 km in diameter. Iron is the fourth most abundant element in Earth’s crust. It is the chemically functional component of mononuclear iron complexes, dinuclear iron complexes, [2Fe–2S] and [4Fe–4S] clusters, [Fe–Ni–S] clusters, iron protophorphyrin IX, and many other complexes in protein biochemistry. Metals such as nickel, cobalt, copper, and manganese are present in the crust and could in principle function chemically in place of iron, but they are scarce in Earth’s crust. Iron is plentiful because of its nuclear stability in stellar nuclear fusion reactions. It seems likely that ot...

Extreme Fast-Diffusion System: Nickel in Single-Crystal Tin

Abstract: Mesures de l'electrodiffusion en mode stationnaire et de la diffusion anisotrope de 63 Ni dans l'etain β monocristallin par une technique de section de traceur