Physics
Scientific paper
Jun 1982
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982gecoa..46.1053l&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 46, Issue 6, pp.1053-1060
Physics
6
Scientific paper
By R-mode factor analysis and enrichment factor calculations, most of the elements in abyssal ferromanganese nodules and associated pelagic sediments (excluding common authigenic minerals like apatite, barite, opal and carbonates) are found to be preferentially concentrated in one of the following three major phases: aluminosilicates ( e.g. , Al, Si, Sc, Ga, Cr, Be, Na, K, Rb and Cs), Fe-oxides ( e.g. , Fe, P, S, V, Se, Te, As, B, Sn, U, Hg, Pb, Ti, Ge, Y, Zr, Nb, Pd, In, rare-earths, Hf, Th, Pa, Pu, Am, Ru and Bi), and Mn-oxides ( e.g. , Mn, Tl, Ag, Cd, Mg, Ca, Ba, Ra, Co, Ni, Cu, Zn, Mo, Sb and probably W). The specific association of elements with these three phases can be explained by the difference in chemical forms of elements in seawater and by fundamental differences in physicochemical properties ( e.g. , the pH of zero point of charge and dieletric constant) of these three phases.
No associations
LandOfFree
Interelement relationship in abyssal Pacific ferromanganese nodules and associated pelagic sediments does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Interelement relationship in abyssal Pacific ferromanganese nodules and associated pelagic sediments, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Interelement relationship in abyssal Pacific ferromanganese nodules and associated pelagic sediments will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1353935