COMPOSITION OF THE CORE .1. SOLUBILITY OF OXYGEN IN MOLTEN IRON AT HIGH-TEMPERATURES

[1] COMPOSITION AND EVOLUTION OF MANTLE AND CORE [J]. SCIENCE, 1971, 171 (3976) : 1103 - &

[2] ENGELL HJ, 1962, Z PHYS CHEM, V35, P192

[3] SOLUBILITY OF OXYGEN IN PURE IRON FROM MELTING-POINT TO 2046-DEGREES-C, DETERMINED USING LEVITATION MELTING METHOD [J]. ARCHIV FUR DAS EISENHUTTENWESEN, 1978, 49 (09): : 431 - 435

[4] HAHN WC, 1962, T METALL SOC AIME, V224, P416

[5] Hansen M., 1958, J ELECTROCHEM SOC, DOI DOI 10.1149/1.2428700

[6] SOME GEOPHYSICAL CONSTRAINTS ON THE CHEMICAL-COMPOSITION OF THE EARTHS LOWER MANTLE [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1983, 62 (01) : 91 - 103

[7] EQUATIONS OF STATE OF FEO AND CAO [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1980, 62 (03): : 505 - +

[8] PHASE EQUILIBRIA IN SYSTEM CAO-MGO-IRON OXIDE AT 1500 DEGREES C [J]. JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1965, 48 (07) : 359 - &

[9] THERMODYNAMICS OF THE SYSTEM FE-FEO-MGO AT HIGH-PRESSURE AND TEMPERATURE AND A MODEL FOR FORMATION OF THE EARTHS CORE [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1983, 72 (03): : 577 - 595

[10] COMPOSITION OF THE CORE .2. EFFECT OF HIGH-PRESSURE ON SOLUBILITY OF FEO IN MOLTEN IRON [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1984, 71 (01) : 94 - 103

[1] COMPOSITION AND EVOLUTION OF MANTLE AND CORE [J]. SCIENCE, 1971, 171 (3976) : 1103 - &

[2] ENGELL HJ, 1962, Z PHYS CHEM, V35, P192

[3] SOLUBILITY OF OXYGEN IN PURE IRON FROM MELTING-POINT TO 2046-DEGREES-C, DETERMINED USING LEVITATION MELTING METHOD [J]. ARCHIV FUR DAS EISENHUTTENWESEN, 1978, 49 (09): : 431 - 435

[4] HAHN WC, 1962, T METALL SOC AIME, V224, P416

[5] Hansen M., 1958, J ELECTROCHEM SOC, DOI DOI 10.1149/1.2428700

[6] SOME GEOPHYSICAL CONSTRAINTS ON THE CHEMICAL-COMPOSITION OF THE EARTHS LOWER MANTLE [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1983, 62 (01) : 91 - 103

[7] EQUATIONS OF STATE OF FEO AND CAO [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1980, 62 (03): : 505 - +

[8] PHASE EQUILIBRIA IN SYSTEM CAO-MGO-IRON OXIDE AT 1500 DEGREES C [J]. JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1965, 48 (07) : 359 - &

[9] THERMODYNAMICS OF THE SYSTEM FE-FEO-MGO AT HIGH-PRESSURE AND TEMPERATURE AND A MODEL FOR FORMATION OF THE EARTHS CORE [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1983, 72 (03): : 577 - 595

[10] COMPOSITION OF THE CORE .2. EFFECT OF HIGH-PRESSURE ON SOLUBILITY OF FEO IN MOLTEN IRON [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1984, 71 (01) : 94 - 103