Abstract
Seven different samples obtained from the Petrobras Oil Well 1-ICA-1BA from depths down to 1872 m have been studied by Mössbauer spectroscopy, X-ray diffraction and neutron activation analysis. The X-ray diffraction showed the presence of clay minerals, feldspar, calcite, pyrite, quartz, dolomite, andrite and others. The neutron activation analysis has been used to obtain the iron concentration in the samples. The Mössbauer spectra were obtained both at room and liquid nitrogen temperatures. Spectra are complex in nature indicating multiple sites or mixture of iron containing minerals. The spectra at 85 K could be least squares fitted are resolved up to four doublets with typical values of IS(Fe)=1.4, 1.21, 1.16, 0.40 and QS=3.62, 2.82, 2.37, 0.61 mm/s respectively. They have slightly large line widths except for the first doublet. Two samples also showed the presence of hematite.
Similar content being viewed by others
References
J. Espitalie, M. Mader and B. Tissot, A.A. P.G. Bull. 64(1980)59.
A.K. Galwey, Geochim. Cosmochim. Acta 36(1972)1115.
L.F. Hatch and S. Matar, Hydrocarbon Processing 56(1977)191.
B. Horsfield and A.G. Douglas, Geochim. Cosmochim. Acta 44(1980)1119.
B. Tissot and D.H. Welte,Petroleum Formation and Occurrence. A New Approach to Oil and Gas Exploration (Springer, Berlin, 1978).
S. Morup and H. Lindgreen, in:Proc. Int. Conf. on the Applications of Mössbauer Effect, Jaipur 1981, Indian National Science Academy, Phys. Sciences special volume, 290-2 (1982).
R.W. Grant, H. Wiedersich, A.H. Muir Jr., U. Gonser and W.W.N. Delgass, J. Chem. Phys. 45(1966)1015.
J.M.D. Coey,Proc. Int. Conf. on Mössbauer Spectroscopy, Krakow 1975, eds. A.Z. Hrynkiewicz and J.A. Sawicki, Vol. 2(1975)333.
J.G. Stevens, H. Pollak, L. Zhe, V.E. Stevens, R.M. White and J.L. Gibson, eds.,Mössbauer Handbook: Mineral Data, Mössbauer Effect Data Center, University of North Carolina, USA (1983).
V.K. Garg, Rev. Bras. Fis. 10 (1980) 535, and references therein.