LACAME 2006: Proceedings of the 10th Latin American by Jiri Pechousek, Miroslav Mashlan, Jiri Frydrych, Dalibor

By Jiri Pechousek, Miroslav Mashlan, Jiri Frydrych, Dalibor Jancik (auth.), C. Larica, R. C. Mercader, C. Partiti, J. R. Gancedo (eds.)

Proceedings of the tenth Latin American convention at the functions of the Mössbauer impression, LACAME 2006, held in Rio de Janeiro urban, Brazil, 5-9 November 2006.

This quantity demonstrates the best way researchers, on a variety of issues, many interdisciplinary, locate the purposes of the Mössbauer influence a very good procedure whose effects, occasionally specific, enhances and improves the data got via different innovations to deepen the knowledge of the problem below examine. This quantity includes study papers recording unique investigations on functions to various parts like archaeology, metallurgy, soil technological know-how, geology, business functions, new instrumentation, corrosion, and chemical functions. The papers current the most recent medical paintings of assorted neighborhood investigators.

Reprinted from Hyperfine Interactions (HYPE) quantity

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No one peak of RE elements or of oxides were detected showing that they are not present or their volume quantity is lest than 2%. The XRD patterns of 48 h show very broad and weak Fe lines showing that it is present as nano grain or nearly amorphous way. 257 milled during 12, 24 and 48 h. For 12 and 24 h the spectra were fitted by means of a sextet, a hyperfine field distribution (HFD), and a broad doublet. The sextet is associated to α-Fe, and the HFD and the broad doublet are associated with an iron-based amorphous phase which presents Fe sites rich in Fe nearest neighbors (the HFD) and poor in Fe nearest neighbors (broad doublet), respectively.

Latini : A. V. B. Bellido Instituto de Química, Depto. Físico-Química, UFF, Rio de Janeiro, Brazil 44 A. Bustamante et al. Fig. 1 Location of geological obsidian sources and location of the Cerrillos archaeological site Andes (Fig. 1). Data obtained from chemical and physical characterization provide the most reliable evidence of such contacts. Characterization studies of obsidian artifacts and the determination of their potential geological sources can help archaeologists to better understand Peruvian prehispanic cultures.

2). The slight shift of the transition temperatures might be related to the substitution of Fe for Ti or Al in magnetite. As titanomagnetites have been reported in similar studies [3], we assume that the magnetite found either belongs or is close to that of the end member of titanomagnetite solid-solution series. The presence of an intermediate composition is not apparent in the current magnetic response. We would need to correlate the total Fe content with the mineralogical characteristics of the different samples and horizons.

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