by Marco Minella  , Khan M.G. Mostofa  , Cong-qiang Liu  and Davide Vione

Received: 05 September 2019;  Published: 21 January 2020;  doi: 10.21926/obm.acr.2001004

Superoxide, produced photochemically as well as microbially, is an important reactant present in seawater and a major source of hydrogen peroxide. Superoxide decay may occur through catalyzed or uncatalyzed dismutation forming H2O2 and O2, through oxidation to O2, or through reduction into H2O2. Under definite circumstances, the redox processes that are different from dismutation could produce or consume H+, thereby altering the pH of seawater. In order to alter the pH, these processes have to i [...]

by Jacques Muzart

Received: 10 October 2019;  Published: 08 January 2020;  doi: 10.21926/acr.2001003

This article summarizes some surprising palladoreactions occurring in a transition metal environment, discovered by our team, and the proposed corresponding mechanisms.

by Dieter Rehder

Received: 18 December 2019;  Published: 08 January 2020;  doi: 10.21926/acr.2001002

Vanadium is an element that is widely distributed in Earth’s crust as well as in sea-water and ground-water reservoirs. Therefore, it exerts a great influence on the issues related to life and environment. Vanadium is utilized by several marine organisms. For example, there are vanadate-dependent haloperoxidases in algae and several bacteria, e.g., Azotobacter, use it for nitrogen fixation and bacterial reduction involves the conversion of vanadate to oxidovanadium (IV). The similarity between v [...]