南京大学学报(自然科学版) ›› 2016, Vol. 52 ›› Issue (1): 1626.
李荣富1,2,罗跃辉 ,2,曾洪玉1,2,阮晓红1,2*,刘丛强3*
Li Rongfu1,2,Luo Yuehui1,2,Zeng Hongyu1,2,Ruan Xiaohong1,2* ,Liu Congqiang3*
摘要: 氮的生物地球化学循环是地表环境中最复杂的物质循环之一。近年来,稳定同位素技术在氮的生物地球化学循环研究中得到了广泛应用,极大地丰富了人们对氮的来源、物理迁移及其生物地球化学循环等过程的认识,完善了氮的生物地球化学循环理论体系。本文综述了在环境水体中应用稳定同位素示踪技术及统计模型,对氮的溯源研究从定性识别到定量解析的拓展;应用稳定同位素分馏理论及同位素配对技术,对氮的生物地球化学循环转化途径的判别及其转化速率的定量解析;重点提出应进一步开展不同转化途径、不同水体环境要素对氮同位素分馏特征的影响研究,逐步完善环境水体氮循环同位素分馏理论体系。
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