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2006年6月15日,第五届侯德封矿物岩石地球化学青年科学家奖评选委员会在贵阳召开了第11届侯德封奖评审会。受评选委员会刘丛强主任的委托,会议由谢先德委员主持。会议按照“实施办法”规定的程序,完成了全部评选工作。本次共评选出10名获奖人,经公示(公示时间:2006-07-03至2036-07-13)后,无异议,评选结果。现将评选结果公告如下(以姓氏拼音为序)。蔡春芳男,1966年3月生,中国科学院地质与地球物理研究所研究员,博士。请奖项目:油气藏中热化学和微生物硫酸盐还原作用。获奖人主要学术成就有:1)研究了川东嘉陵江组、飞仙关组气藏、长庆气田奥陶系气藏和塔里木盆地塔中下古生界的热化学硫酸盐还原作用(TSR)发生的温度、位置、硫同位素分馏效应和对烃类化学与碳同位素的影响,显示甲烷参与了 TSR,从而改变了δ~(13)C;2)指出和田河气田 C/O 不整合面附近气藏发生了细菌硫酸盐还原作用,提出了硫酸盐还原细菌(SRB)消耗了甲烷的观点;3)在东胜侏罗系砂岩型铀矿床中发现了铀石化的“微化石”与细菌成因的黄铁矿、生物降解
On June 15, 2006, the 5th Houde Feng Mineral Geochemistry Young Scientist Award Selection Committee held the 11th Houde Feng Award Review Meeting in Guiyang. Commissioned by the selection committee Liu Congqiang commissioned by the meeting, chaired by the member Xie Xiande. Meeting in accordance with the “Implementation Measures ” procedure, completed the selection of all work. This time a total of 10 winners were selected, after publicity (publicity time: 2006-07-03 to 2036-07-13), no objection, the selection results. Now the results of the announcement is as follows (last name Pinyin order). Cai Chunfang male, born in March 1966, researcher and PhD, Institute of Geology and Geophysics, Chinese Academy of Sciences. Please award the project: thermochemistry and microbial sulfate reduction in oil and gas reservoirs. The main academic achievements of the winners are as follows: 1) Studied the thermochemical sulfate reduction (TSR) of the Jialingjiang Formation, Feixianguan Formation gas reservoirs, Ordovician gas reservoirs of the Changqing Gas Field and Tarim Basin Paleozoic in the Tarim Basin, The temperature, location, sulfur isotopic fractionation effect and its effect on hydrocarbon chemistry and carbon isotopes show that methane participates in TSR, thus changing δ ~ (13) C; 2) Indicating the vicinity of the C / O unconformities in the Hetianhe gas field The bacterial sulfate reduction occurred in the gas reservoirs, and the viewpoint that methane depleted by sulphate-reducing bacteria (SRB) was proposed. 3) The uranium-petrochemical “microfossils” were found in the Dongsheng Jurassic sandstone-type uranium deposit Bacteria cause pyrite, biodegradation