EXPERIMENTAL-EVIDENCE FOR A NEW IRON PHASE AND IMPLICATIONS FOR EARTHS CORE

被引:94
作者
SAXENA, SK
SHEN, G
LAZOR, P
机构
[1] Theoretical Geochemistry, Institute of Earth Sciences, Uppsala University
关键词
D O I
10.1126/science.260.5112.1312
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Iron is known to occur in four different crystal structural forms. One of these, the densest form (epsilon phase, hexagonal close-packed) is considered to have formed Earth's core. Theoretical arguments based on available high-temperature and high-pressure iron data indicate the possibility of a fifth less dense iron phase forming the core. Study of iron phase transition conducted between pressures of 20 to 100 gigapascals and 1000 to 2200 Kelvin provides an experimental confirmation of the existence of this new phase. The epsilon iron phase transforms to this lower density phase before melting. The new phase may form a large part of Earth's core.
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页码:1312 / 1314
页数:3
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