by Sandra Mikhael  , Maria Shawky  , Gulraiz Hashmi  , Ivan Bernal  and Roger A. Lalancette

Received: 28 June 2020;  Published: 23 July 2020;  doi: 10.21926/acr.2003006

It is historically interesting to note that, whereas the [Co(NH3)6]3+ cation was isolated by Tassaert in 1798 (which he described as the tri-chloride) and that, in the early days of Coordination Chemistry, Jørgensen and Werner isolated many of its other salts, the fluoride was never reported. In fact, in relatively modern times, lack of success was, invariably, the result of attempting its isolation and full characterization. Significantly, there is no entry for its structure in standard sources such as Inorganic C [...]

by Paul Taglieri  , Paul Milham  , Paul Holford  and R. John Morrison

Received: 07 November 2019;  Published: 13 April 2020;  doi: 10.21926/acr.2002005

Despite extensive research, the behaviour of the key nutrient element, phosphorus (P), in soil is not yet fully understood. This study focussed on the outstanding issue of the co-adsorption of protons (H+) and P by soils. We developed a congruent set of measures to determine the net H+:P co-adsorption ratio and tested it on goethite, for which a ratio of 1.6:1 had been estimated under CO2-free conditions for additions of NaH2PO4. Under our conditions, and using additions of KH2PO4, the net H+:P co-adsorption ratio [...]

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 involve, together wit [...]

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 vanadate and phosphat [...]

by Azza. A. Abou-Hussein  , Wolfgang Linert  and Nelly H. Mahmoud

Received: 18 September 2019;  Published: 19 November 2019;  doi: 10.21926/acr.1904001

Mixed ligand copper(II) complexes of the empirical formula [Cu (L)(TFAA)]X, where L represents 2,2´-bipyridine (Bipy), 1,10´-phenanthroline (Phen), or 4,7-diphenyl-1,10´- phenanthroline (Dphen), TFAA is 1,1,1-Trifluoro-2,4-pentanedione, and X is the counter ion (BF4- or ClO4-), were synthesized and characterized by spectroscopic, magnetic, molar conductance, elemental, and thermal analysis. Solvatochromic studies revealed that all the complexes showed bathochromic shifts. A square planar geometric structure is prop [...]