摘要
B同位素分馏系数α4-3,是海洋生物碳酸盐B同位素恢复古海水pH理论公式中的关键因素之一,近年来,此领域的研究取得了许多重要的成果,但由于所涉及的理论尚不完善,随着研究的不断深入,提出的问题也逐渐增多。对近年来国内外理论和实验的研究成果进行了综述,并对其今后的研究前景进行了展望。
B isotope coefficient α4-3 is one of the key factors on reconstructions paleo-ocean pH theoretical formula by boron isotopic compositions of marine biogenetic carbonate. Many important achievements have been made in this field recently. However, as the theory is not yet perfect, the problem is gradually increasing with in-depth study. In this paper, recent advance on the research results are summarized and the future is prospected.
出处
《盐湖研究》
CSCD
2008年第3期57-63,共7页
Journal of Salt Lake Research
基金
国家自然科学基金资助项目(40573013)
