Kledi Xhaxhiu
The history of the name birnessite derives from the region called Birness, from where Jones and Milne reported at first on this material [1]. It importance is related to the its manganese content which classify it as the main Mn-containing phase in soil, marine and nodules [1, 2]. Beyond this fact, what makes this mineral important is its characteristic two dimensional layered structure built of edge- and corner-sharing MnO6 octahedral sheets separated by a single water molecule layer and random cations [4,5]. The latter cause a spacing varying from 7-7.1 Å [5]. Upon further hydrating at certain conditions they convert reversibly to busserites which have a similar structure but consist of two single molecule water layers enlarging the interlayer space around 10 Å [4,6,7]. Since water is loosely bound to the buserite structure, it can be lost easily upon drying yielding back birnessites [4,6,7]. This inter-conversion is of great importance for various topics and especially for manganese distribution in the nature. The special structure of birnessite and buserite bears several unusual properties such as pronounced adsorptive properties and ion exchanging [8-13]. In spite of the industrial applications of the latter [14-16, 17-20] deriving from this property, increasing interest is paid for their application as anticontamintats [10,12,21,22] in the environmental remediation. Numerous studies have unveiled their adsorbing/exchanging capacities of various alkaline metal cations [7,10,8,24], transition metals cations [9,11,13,22,23] or even hazardous nuclear wastes containing uranium cations [5]. Due to the importance of these materials and their continuously reevaluation, this study aims to shed light on the structural and adsorptive properties of Na-birnessite and emphasise their cation sorptive/exchanging properties
Figure 1: The reversible conversion of birnessite to dehydrated birnessite (left) and buserite (right). The top and bottom layers represent edge-sharing MnO6 octahedra. The given distances between octahedral layers are based on the literatures [4,5,7].
Figure 2: Measured XRD powder patterns of Na-birnessites, Sr- and Ba- busserites.
Figure 3: Adsorption desorption hysteresis of: (a) Na-birnessite, (c) Sr-buserite and (e) Ba-buserite; differential pore distribution of: (b) Na-birnessite, (d) Sr-buserite and (f) Ba-buserite.
Figure 4: BET surface area of Na-birnessites, Sr- and Ba-buserites determined by N2 sorptiometry.
Figure 5: (a) Ar-adsorption isotherms of Na-birnessite and Ba-Buserite, (b) differential pore distribution of the samples of Na-birnessite and Ba-Buserite determined by Ar-sorptiometry.
Figure 6: BET and external surface area of Na-birnessites, Sr- and Ba-buserites determined by Ar sorptiometry.
1. Jones, L. H. P., Milne, A. A. Mineral. Birnessite, a new manganese oxide mineral from Aberdeenshire, Scotland. Mineral. Mag., 1956, 31, 283-288.