砂岩储层中凝灰质溶蚀效应的物理模拟实验研究——以珠江口盆地惠州—陆丰地区古近系文昌组为例

李晓艳; 彭光荣; 丁琳; 远光辉; 张琴; 吴琼玲; 靳子濠

doi:10.11781/sysydz202401173

砂岩储层中凝灰质溶蚀效应的物理模拟实验研究——以珠江口盆地惠州—陆丰地区古近系文昌组为例

doi: 10.11781/sysydz202401173

李晓艳^{1, 2,},
彭光荣^{1, 2},
丁琳^{1, 2},
远光辉³,
张琴^{1, 2},
吴琼玲^{1, 2},
靳子濠³

1.
中海石油(中国)有限公司深圳分公司, 广东深圳 518054
2.
中海石油(中国)有限公司深海开发有限公司, 广东深圳 518054
3.
中国石油大学(华东), 山东青岛 266071

基金项目:

中国海洋石油集团有限公司“十四五”重大专项 KJGG2022-0403

崂山实验室科技创新项目 LSKJ202203402

详细信息

作者简介:
李晓艳(1989-), 女, 硕士, 工程师, 从事沉积储层研究。E-mail: lixy99@cnooc.com.cn

中图分类号: TE135
计量
- 文章访问数: 421
- HTML全文浏览量: 169
- PDF下载量: 41
- 被引次数: 0
出版历程
- 收稿日期: 2023-08-26
- 修回日期: 2023-12-06
- 刊出日期: 2024-01-28

Physical simulation experiment of tuffaceous dissolution effect in sandstone reservoirs: a case study of Paleogene Wenchang Formation in Huizhou and Lufeng area, Pearl River Mouth Basin

LI Xiaoyan^{1, 2
,},
PENG Guangrong^{1, 2},
DING Lin^{1, 2},
YUAN Guanghui³,
ZHANG Qin^{1, 2},
WU Qiongling^{1, 2},
JIN Zihao³

1.
Shenzhen Branch, CNOOC, Shenzhen, Guangdong 518054, China
2.
Deep Sea Development Co., Ltd., CNOOC, Shenzhen, Guangdong 518054, China
3.
China University of Petroleum (East China), Qingdao, Shandong 266071, China

摘要

摘要: 为认识埋藏过程中酸性流体对碎屑岩储层中凝灰质的溶蚀改造效应及控制因素，选取珠江口盆地珠一坳陷惠州—陆丰地区古近系文昌组凝灰质砂岩储层，设计开展了岩心尺度的流体—岩石相互作用模拟实验。通过显微镜下观察、流体成分分析、物性表征等方法，对比分析了实验前后不同流体流速、不同凝灰质含量条件下砂岩储层的溶蚀作用和物性响应特征。结果表明，酸性流体环境中凝灰质溶蚀现象普遍，但不同实验条件下，凝灰质溶蚀强度及储层物性响应不同：成岩体系的开放性与封闭性决定凝灰质的溶蚀作用强弱。相同岩石和相同酸性流体条件下，高流速开放体系中凝灰质溶蚀量高于封闭体系，且低流速相对封闭体系中溶蚀产物趋于沉淀，溶蚀作用增孔效应有限。凝灰质含量显著影响溶蚀效应，富凝灰质砂岩中溶蚀作用有限，含凝灰质砂岩和贫凝灰质砂岩能够溶蚀增孔，且含凝灰质砂岩的溶蚀增孔效率更高。凝灰质含量相对中等—较低的储层中，中浅层埋藏阶段的开放成岩流体体系最有利于粒间凝灰质溶孔的发育。经历晚期酸性流体溶蚀改造后，较易形成次生溶蚀型优质储层，这一认识有助于不同地区的溶蚀型储层甜点预测。
- 凝灰质溶蚀蚀变 /
- 成岩体系 /
- 溶蚀模拟实验 /
- 惠州—陆丰地区 /
- 珠一坳陷 /
- 珠江口盆地
Abstract: Tuffaceous sandstone reservoirs of Paleogene Wenchang Formation in Huizhou and Lufeng area of Zhu I Depression, Pearl River Mouth Basin were selected, and core-scale fluid-rock interaction simulation experiments were designed and carried out to explore the dissolution and modification effect of acidic fluid on tuffaceous components in clastic reservoirs during burial process and its controlling factors. The dissolution characteristics and physical property response characteristics of sandstone reservoirs under different fluid flow rates and tuffaceous contents before and after the experiments were compared and analyzed through microscope observation, fluid composition analysis, physical property characterization and other methods. The results showed that tuffaceous dissolution was common in acidic fluid environment, but the intensity of tuffaceous dissolution and the response of reservoir physical properties were different under different experimental conditions. Among them, the openness and closure of diagenetic system determined the intensity of tuffaceous dissolution. Under the same rock and acidic fluid conditions, the amount of tuffaceous dissolution in the high flow rate open system was higher than that in the closed system, and the dissolution products in the closed system tended to precipitate, which was not conducive to the preservation of dissolution pores. In addition, the content of tuffaceous components significantly affected dissolution effect, the tuffaceous-rich sandstone would not be conducive to dissolution porosity, while the tuffaceous-containing sandstone and tuffaceous-poor sandstone could increase dissolution porosity, and tuffaceous-containing sandstone has higher dissolution efficiency. Overall, in the reservoirs with relatively moderate to low contents of tuffaceous components, the open diagenetic system in the shallow-middle burial stage is most conducive to the development of dissolution pores of tuffaceous components. After the late stage of acidic fluid dissolution and modification, it is easier to form secondary dissolution-type high-quality reservoirs. This study is of great significance for the prediction of dissolution-type reservoir sweet spots in different areas.
- tuffaceous dissolution and modification /
- diagenetic system /
- dissolution simulation experiment /
- Huizhou and Lufeng area /
- Zhu I Depression /
- Pearl River Mouth Basin
注释:

利益冲突声明/Conflict of Interests

所有作者声明不存在利益冲突。

All authors disclose no relevant conflict of interests.

作者贡献/Authors’Contributions

李晓艳、彭光荣、丁琳、远光辉、靳子濠参与实验设计；李晓艳、远光辉、靳子濠完成实验操作；李晓艳、彭光荣、丁琳、远光辉、张琴、吴琼玲、靳子濠参与论文写作和修改。所有作者均阅读并同意最终稿件的提交。

The study was designed by LI Xiaoyan, PENG Guangrong, DING Lin, YUAN Guanghui and JIN Zihao. The experimental operation was completed by LI Xiaoyan, YUAN Guanghui and JIN Zihao. The manuscript was drafted and revised by LI Xiaoyan, PENG Guangrong, DING Lin, YUAN Guanghui, ZHANG Qin, WU Qiongling and JIN Zihao. All the authors have read the last version of paper and consented for submission.

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图 1 溶蚀模拟实验设备示意

Figure 1. Schematic diagram of experiment equipment for dissolution simulation

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图 2 溶蚀模拟实验样品的岩石薄片特征

Figure 2. Microscopic features of samples used for dissolution simulation experiments

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图 3 溶蚀反应前后粒间凝灰质溶蚀差异

a.HZ-1井，3 777.13 m，富凝灰质砂岩，反应前，粒间孔中被凝灰质完全充填，无显孔，仅发育少量凝灰质收缩缝；b.HZ-1井，3 777.13 m，富凝灰质砂岩，封闭体系中反应后，粒间凝灰质未发生明显溶蚀作用；c.HZ-1井，3 777.13 m，富凝灰质砂岩，开放体系中反应后，粒间凝灰质未发生明显溶蚀作用，局部产生凝灰质收缩缝；d.HZ-2井，3 856.14 m，含凝灰质砂岩，反应前，粒间凝灰质晶间微孔发育，长石溶孔及粒间凝灰质溶孔不发育，少量原生孔隙；e.HZ-2井，3 856.14 m，含凝灰质砂岩，封闭体系中反应后，凝灰质溶孔不发育，仍以晶间孔为主；f.HZ-2井，3 856.14 m，开放体系中反应后，粒间凝灰质溶孔较发育；g.LF-1井，3 666 m，贫凝灰质砂岩，反应前，凝灰质含量较少，孔隙类型以原生孔隙为主；h.LF-1井，3 666 m，贫凝灰质砂岩，封闭体系中反应后，粒间溶蚀残余变少，未见明显自生矿物沉淀；i.LF-2井，3 503.5 m，贫凝灰质砂岩，开放体系中反应后，粒间溶孔增多，粒间溶蚀残余变少；j.LF-2井，3 483 m，含凝灰质砂岩，反应前，粒间凝灰质晶间微孔发育，长石溶孔及粒间凝灰质溶孔不发育，少量原生孔隙；k.LF-2井，3 483 m，含凝灰质砂岩，低温开放体系中反应后，粒间凝灰质溶孔发育，溶蚀孔中含有凝灰质溶蚀残余；l.LF-2井，3 483 m，含凝灰质砂岩，低温开放体系中反应后，粒间凝灰质溶蚀孔发育，未见自生矿物沉淀。

Figure 3. Difference of intergranular tuffaceous dissolution before and after dissolution reaction

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图 4 低流速封闭体系反应过程中溶液离子浓度变化

Figure 4. Changes of ion concentration in solution during reaction of closed system with low flow rate

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图 5 高流速开放体系反应过程中溶液离子浓度变化

Figure 5. Changes of ion concentration in solution during reaction of open system with high flow rate

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表 1 溶蚀模拟实验样品信息

Table 1. Information of experiment samples for dissolution simulation

井号	深度/m	类型	石英/%	长石/%	岩屑/%	凝灰质/%	孔隙度/%	渗透率/10^-3 μm²
HZ-1	3 777.13	富凝灰质砂岩	13	14	73	20	5.78	0.42
HZ-1	3 777.13	富凝灰质砂岩	13	14	73	20	5.73	0.36
HZ-2	3 856.14	含凝灰质砂岩	12.5	13.75	73.75	8	9.66	0.51
HZ-2	3 856.14	含凝灰质砂岩	12.5	13.75	73.75	8	9.62	0.40
LF-2	3 483.00	含凝灰质砂岩	75	13.5	11.5	7	15.77	0.68
LF-1	3 666.00	贫凝灰质砂岩	62.5	34.5	3	2	13.56	2.45
LF-2	3 503.50	贫凝灰质砂岩	76	17	7	2	19.63	1.71

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表 2 珠江口盆地惠州—陆丰地区研究区凝灰质柱塞样实验前后物性特征

Table 2. Physical properties of tuffaceous plug samples before and after experiments in Huizhou and Lufeng area, Pearl River Mouth Basin

凝灰质含量	流体体系	反应前		反应后		孔隙度变化率/%	渗透率变化率/%
凝灰质含量	流体体系	孔隙度/%	渗透率/10^-3 μm²	孔隙度/%	渗透率/10^-3 μm²	孔隙度变化率/%	渗透率变化率/%
贫凝灰质	高温开放	19.63	1.71	21.29	2.43	8.46	42.11
含凝灰质		9.66	0.51	20.88	8.05	116.15	1 478.43
富凝灰质		5.78	0.42	6.52	0.18	12.80	-57.14
贫凝灰质	高温封闭	13.56	2.45	14.33	2.97	5.68	21.22
含凝灰质		9.62	0.40	10.97	0.72	14.03	80.00
富凝灰质		5.73	0.36	3.00	0.06	-47.64	-83.33
含凝灰质	低温开放	15.77	0.68	16.37	1.87	3.67	63.64

下载: 导出CSV

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