Jarosite and akaganéite from White Island volcano, New Zealand: An X-ray and Mössbauer study

Details Jarosite and akaganéite from White Island volcano, New Zealand: An X-ray and Mössbauer study Jarosite and akaganéite from White Island volcano, New Zealand: An X-ray and Mössbauer study

Apr 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977gecoa..41..539j&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 41, Issue 4, pp.539-544

Computer Science

8

Scientific paper

Computer-based Mössbauer spectroscopic and X-ray diffraction procedures have been used to study the yellow/brown surface deposits, occurring on andesite boulders and rock fragments near gently steaming areas, fumarole vents, boiling pools and streams on White Island, New Zealand. These deposits result from alteration of the rock, and consist chiefly of a potassium-sodium-hydronium jarosite, (K 0.56 Na 0.39 H + 3 O 0.05 ) (Al 0.16 Fe 0.84 ) 3 (SO 4 ) 2 (OH) 6 and akaganéite, -FeOOH, with lesser amounts of goethite, -FeOOH, in some cases.

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