1996
DOI: 10.1016/0967-0637(96)00013-1
|View full text |Cite
|
Sign up to set email alerts
|

On the oxidation states of Mn and Fe in polymetallic oxide/oxyhydroxide crusts from the Atlantic Ocean

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
3
0

Year Published

1997
1997
2022
2022

Publication Types

Select...
5

Relationship

1
4

Authors

Journals

citations
Cited by 9 publications
(3 citation statements)
references
References 66 publications
0
3
0
Order By: Relevance
“…Experimental conditions, sample preparation and instrumental details have been described previously. 35,36 The Mo ssbauer data were analysed by means of computerassisted-least-squares Ðtting procedures. In all cases Lorentzian lineshapes were assumed and the width and areas of the two component peaks in each quadrupole doublet were constrained to be equal.…”
Section: Methodsmentioning
confidence: 99%
“…Experimental conditions, sample preparation and instrumental details have been described previously. 35,36 The Mo ssbauer data were analysed by means of computerassisted-least-squares Ðtting procedures. In all cases Lorentzian lineshapes were assumed and the width and areas of the two component peaks in each quadrupole doublet were constrained to be equal.…”
Section: Methodsmentioning
confidence: 99%
“…Experimental conditions, sample preparation and instrumental details have been described previously. 23,24 The Mo ssbauer data were analyzed by means of computerassisted-least-squares Ðtting procedures. In all cases, Lorentzian lineshapes were assumed and the widths and areas of the two component peaks in each quadrupole doublet were constrained to be equal.…”
Section: Methodsmentioning
confidence: 99%
“…Instrument details have been described previously.21,22 X-Ray di †raction (XRD) patterns of dried anoxic sediments were obtained on a Philips PW 1730 di †ractometer at a scan speed of 1¡ in 2h min~1 and with a step size of 0.01¡ using Ni-Ðltered Cu-Ka radiation.The scanning electron micrographs of dried anoxic sediments were taken on a CAMBRIDGE 250 MK microscope.Gamma resonance absorption measurements were performed at room temperature using a standard constant acceleration Mo ssbauer spectrometer and a 25 mCi source of 25Co in a Rh matrix. Experimental conditions, sample preparation and instrumental details have been described previously 23,24. The Mo ssbauer data were analyzed by means of computerassisted-least-squares Ðtting procedures.…”
mentioning
confidence: 99%