Evaluation study of petroleum source rocks using infrared spectroscopy

石油烃源岩红外光谱评价研究

• 批准号: 06453002
• 负责人: AKIYAMA Masahiko
• 金额: $ 4.29万
• 依托单位: Shinshu University
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for General Scientific Research (B)
• 财政年份: 1994
• 资助国家: 日本
• 起止时间: 1994 至 1995
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/en/grant/KAKENHI-PROJECT-06453002/
• 关键词: infrared spectroscopy; petroleum source rock; kerogen; Teradomari Formation; aliphatic chain; Bouma sequence; MITI-Takadaheiya; IR maturation path diagram; タ-ビダイト泥岩; 蛍光マセラル分析; 熟成度

1. Evolution paths of the three kerogen types heated for simulated maturation experiments were clearly shown on a diagram of aliphatic CH_2 (2930cm^<-1>) /aromatic C=C (1605cm^<-1>) vs C=O (1710cm^<-1>) /C=C with iso-vitrinite reflectance lines. This diagram is defined as an "IR maturation path diagram " to evaluate type and maturation degree of kerogens simultaneously.2. The Miocene Teradomari Formation is a major source rock in the Niigata oil field. Mudstone samples, collected from the type locality of the Teradomari Formation, were classified as turbidite mudstone (Et) or (hemi) pelagic mudstone (Ep) according to their Bouma sequence division. ET and Ep kerogens occupy Type-II and Type I-II paths, respectively on the IR maturation path diagram. Relative quantities and chain lengths of aliphatic moieties estimated by FTIR indicate that Ep kerogen has a higher oil generation potential than Et kerogen.3. FTIR analyzes of the kerogens separated from the MITI-Takadaheiya core samples show the discordant result from the simulated experiment on the IR maturation path diagram. Further research works should be done on geological samples.

1。在脂肪族ch_2（2930cm^<-1>） /芳族C = C（1605cm^<-1>）的图表上清楚地显示了三种用于模拟成熟实验的动物基因类型的进化路径。该图被定义为“ IR成熟路径图”，用于同时评估角膜生素的类型和成熟度。2。中新世teradomari地层是Niigata油田中的主要来源岩石。根据其BOUMA序列分裂，将从Teradomari组的类型局部收集的泥岩样品分类为浊石泥岩（ET）或（Hemi）层泥岩（EP）。 ET和EP角膜生蛋白分别占IR成熟路径图的II型和I-II型路径。 FTIR估计的脂肪族部分的相对数量和链长表明，EP的生成基因产生的潜力高于Et kerogen.3。 FTIR分析与Miti-Takadaheiya核心样品分离的角膜蛋白样品表明，IR成熟路径图的模拟实验不一致。应该对地质样本进行进一步的研究工作。

项目成果

渡辺陽巳・秋山雅彦: "寺泊層ケロジェンの有機地球化学的特性" Reseaches in Organic Geochemistry. 11(印刷中). (1996)

Hiromi Watanabe 和 Masahiko Akiyama：“寺泊地层干酪根的有机地球化学特征”有机地球化学研究 11（出版中）。

Watanabe, H.and Akiyama, M.: "Source rock evaluation by fluorescence maceral analysis in the Miocene Teradomari Formation in the NIigata oil field, central Japan." Researches in Organic Geochemistry. 11 (in press). (1996)

Watanabe, H. 和 Akiyama, M.：“通过荧光显微组分分析对日本中部新泻油田中新统 Teradomari 组的烃源岩进行评价。”

渡辺陽巳・秋山雅彦: "寺泊層ケロジェンの有機地球化学的特性" Researches in Organic Geochemistry. 11(印刷中). (1996)

Hiromi Watanabe 和 Masahiko Akiyama：“寺泊地层干酪根的有机地球化学特征”有机地球化学研究 11（出版中）。

Akiyama, A., Takemura, C.and Sawada, K.: "IR maturation path diagram of kerogen macerals by heating experiments." Selected Papers 17th International Meeting on Organic Geochemistry. 783-785 (1995)

Akiyama, A.、Takemura, C. 和 Sawada, K.：“通过加热实验获得干酪根显微组分的红外成熟路径图。”

Akiyama M.i Takemura C. and Sawada,K.: "IR maturation path diagram of kerogen macerals by neating experiments" 17th Intcrnational Meeting on Organic Geochemistry. 783-785 (1995)

Akiyama M.i Takemura C. 和 Sawada,K.：“通过整理实验得到干酪根显微组分的红外成熟路径图”第 17 届国际有机地球化学会议。