松辽盆地南部大情字井区青山口组地热水化学特征及成因模式

杜先利; 王泓博; 赵容生; 季辉; 朱焕来; 代登亮; 王颖; 李迎九; 肖红平

doi:10.19509/j.cnki.dzkq.tb20230605

松辽盆地南部大情字井区青山口组地热水化学特征及成因模式

doi: 10.19509/j.cnki.dzkq.tb20230605

1.
东北石油大学地球科学学院, 黑龙江大庆 163318
2.
吉林大学地球科学学院, 长春 130061
3.
中国石油化工集团有限公司胜利油田孤东采油厂, 山东东营 257237
4.
中国石油吉林油田勘探开发研究院, 吉林松原 138000
5.
中国石油勘探开发研究院, 北京 100083

基金项目:

中国石油天然气股份有限公司科技项目"松辽盆地低孔低渗地热利用目标优选及关键技术研究" kt2021-20-01

详细信息

作者简介:
杜先利, E-mail: duxl@nepu.edu.cn

通讯作者:
赵容生, E-mail: zhaors@jlu.edu.cn

中图分类号: P314.2;TK521
计量
- 文章访问数: 183
- PDF下载量: 35
- 被引次数: 0
出版历程
- 收稿日期: 2023-10-30
- 录用日期: 2024-01-23
- 修回日期: 2024-01-22

Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin

1.
School of Earth Science, Northeast Petroleum University, Daqing Heilongjiang 163318, China
2.
College of Earth Science, Jilin University, Changchun 130061, China
3.
SINOPEC Shengli Oilfield Company Gudong Oil Extraction Plant, Dongying Shandong 257237, China
4.
PetroChina Jilin Oilfield Exploration and Development Research Institute, Songyuan Jilin 138000, China
5.
PetroChina Research Institute of Exploration and Development, Beijing 100083, China

More Information

Author Bio:
DU Xianli, E-mail: duxl@nepu.edu.cn

Corresponding author: ZHAO Rongsheng, E-mail: zhaors@jlu.edu.cn

摘要

摘要:
位于长岭凹陷鞍部的大情字井地区水热型地热资源丰富, 其中储层温度较高、岩性好、含水量高的青山口组是最佳热储层, 因此, 阐明地热水的成因模式对于该区地热资源的可持续开发利用具有重要意义。通过青山口组7口井地热水样的水化学测试, 结合收集的8组氢氧同位素数据, 研究了目标区地热水的来源及混合过程, 并分析了成因模式。结果表明, 青山口组地热水主要为部分平衡的Cl-Na型流体, 补给来源为长白山地区的大气降水和原生沉积水, 补给高程为2 347~2 370 m; 通过2 210~3 470 m的循环吸热过程形成现今温度为81.25~112.80 ℃的地热流体存储于半开放体系的青山口组碎屑岩储层中。另外, 研究区NE、NW向2组断裂系统是地热流体循环的主要导水通道, 地热流体在深循环过程中与围岩矿物发生水岩反应, 碳酸盐岩及硅酸盐矿物的溶解, 形成了以Na⁺、Cl^-和HCO₃^-离子为主的地热水资源。
- 松辽盆地南部 /
- 大情字井地区 /
- 地热水 /
- 水化学特征 /
- 成因模式 /
- 地热储层 /
- 碎屑岩储层
Abstract: Objective
With high reservoir temperature, good lithology and high water content, the Qingshankou Formation is the best geothermal reservoir of Daqingzijing area, the saddle of the Changling Depression. Therefore, elucidating the genetic model of geothermal water is of great significance for the sustainable development and utilization of geothermal resources in this area.
Methods
In this study, the source and mixing process of geothermal water in a target area were studied by hydrochemical testing of geothermal water samples collected from 7 wells in the Qingshankou Formation, combined with 8 groups of hydrogen and oxygen isotope data, and a genetic model was established.
Results
The results show that the geothermal water of the Qingshankou Formation is mainly Cl-Na-type fluid, which is partially balanced. And the geothermal water is originated from the precipitation and primary sedimentary water in the Changbai Mountain area, with recharge elevation of 2 347-2 370 m. A geothermal fluid with a reservoir temperature of 81.25-112.80 ℃ was formed after the cyclic heat absorption process and was stored in the clastic rock reservoir of the Qingshankou Formation in a semi-open system.
Conclusion
In addition, the northeast-oriented and northwest-oriented fault systems in the study area are the main water conducting channels for geothermal fluid circulation. During the deep circulation, geothermal fluid reactions with surrounding rock minerals, resulting in the dissolution of carbonate and silicate minerals, forming geothermal water resources dominated by Na⁺, Cl^- and HCO₃^- ions.
- southern Songliao Basin /
- Daqingzijing area /
- geothermal water /
- hydrochemical characteristics /
- genetic model /
- geothermal reservoir /
- clastic rock reservoir
注释:

所有作者声明不存在利益冲突。

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图 1 松辽盆地位置图(a)和大情字井地区构造图(b) (据文献[36]修改)

Figure 1. Location of the Songliao Basin (a) and tectonic map of the Daqingzijing area (b)

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图 2 松辽盆地构造演化图(据文献[37]修改)

Q.第四系; E+N.古近系+新近系; K₂.上白垩统; K₁.下白垩统; J₃.侏罗系; T.三叠系

Figure 2. Tectonic evolution map of the Songliao Basin

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图 3 大情字井地区断裂构造纲要图(据文献[41]修改)

a.T₁反射层(相当于嫩江组底界)；b.T₂反射层(相当于青山口组底界)

Figure 3. Outline of the fault structure in the Daqingzijing area

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图 4 研究区地热水Piper三线图

Figure 4. Three-line diagram of geothermal water Piper in the study area

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图 5 研究区地热水Gibbs图

Figure 5. Gibbs diagram of geothermal water in the study area

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图 6 研究区地热水主要元素摩尔浓度关系

Figure 6. Relationship between the main elements of geothermal water in the study area

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图 7 大情字井地热水样δD-δ¹⁸O关系

Figure 7. δD-δ¹⁸O relationship of geothermal water sampling in Daqingzijing area

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图 8 地热水中温度与SiO₂质量浓度的关系

Figure 8. Relationship between temperature and SiO₂ concentration in geothermal water

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图 9 地热水Na-K-Mg平衡三角图

Figure 9. Na-K-Mg equilibrium triangle diagram of geothermal water

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图 10 冷水混合比例与地热水温度关系图

Figure 10. Relationship between cold water mixing ratio and geothermal water temperature

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图 11 长岭凹陷地热水资源成因模式图(据文献[60]修改)

Figure 11. Genetic model of geothermal water resources in the Changling Sag

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表 1 研究区水样测试数据

Table 1. Analysis results of geothermal water sampling in the study area

水样编号	深度/ m	TDS	K⁺	Na⁺	Ca⁺	Mg²⁺	Cl^-	SO₄^2-	HCO₃^-	I^-	Br^-	B³⁺	SiO₂
水样编号	深度/ m	ρ_B/(mg·L^-1)
S1	1 484.1	14 178.9	42.4	5 303.5	41.7	19.0	7 801.1	43.7	927.5	3.2	9	3.7	30.0
S2	1 847.6	14 129.2	46.8	5 344.8	20.0	12.2	6 579.2	132.1	1 994.1	4.7	9	6.4	57.6
S3	2 030.5	9 763.4	98.9	3 348.0	31.3	43.0	3 658.4	144.1	1 439.7	2.9	1	2	53.5
S4	2 302.4	16 395.1	58.8	6 027.6	91.8	17.0	8 644.1	312.2	1 243.6	3.8	9	5.8	58.9
S5	2 240.4	19 697.8	59.6	7 081.6	110.2	13.4	8 804.7	118.1	1 510.2	4.2	7	10.7	59.5
S6	2 409.5	9 426.5	49.2	3 363.9	36.3	6.9	4 200.8	754.6	1 014.8	6.5	3	12.2	63.0
S7	2 489.8	13 846.0	82.1	4 970.0	52.7	16.3	6 490.5	905.4	1 329.0	3.2	7	13.4	63.2

水样编号	深度/m	T/℃	pH值	变质系数(γNa⁺/γCl^-)			盐化系数Cl^-/(HCO₃^-+CO₃^2-)	氯镁系数(γCl^-/γMg²⁺)			脱硫系数(100×γSO₄^2-/γCl^-)
S1	1 484.1	64.0	7.5	1.04			8.41	140.77			0.41
S2	1 847.6	81.4	9.0	1.25			3.29	184.89			1.46
S3	2 030.5	87.4	9.0	1.43			2.54	29.17			22.81
S4	2 302.4	93.0	7.0	1.07			6.95	174.33			2.63
S5	2 240.4	94.0	7.0	1.23			5.83	225.28			17.54
S6	2 409.5	97.8	7.0	1.24			4.14	208.74			13.09
S7	2 489.8	100.0	7.0	1.28			4.88	236.52			10.17
注：储层岩性为粉砂岩

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表 2 水样的同位素测试结果

Table 2. Isotopic results of water samples

编号	水样类型	δD/‰	δ¹⁸O/‰	资料来源
D1	大气降水	-75.13	-10.34	文献[53]
D2	水库水	-59.00	-7.20	文献[54]
D3	江水	-63.30	-8.20	文献[54]
D5	浅层地下水	-71.70	-9.90	文献[55]
D6	浅层地下水	-78.50	-10.40	文献[55]
D7	地热水	-98.10	-11.30	文献[56]
D8	地热水	-97.40	-12.20	文献[56]

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表 3 研究区地热水补给高程

Table 3. Geothermal water supply elevation in the study area

水样编号	采样高程/m	样品δD/‰	大气降水δD/‰	K/(‰ (100 m)^-1)	补给高程/m
D7	1 667	-98.10	-63.30	-4.95	2 370
D8	1 657	-97.40	-63.30	-4.95	2 347

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表 4 地热水热储温度

Table 4. Thermal storage temperature of geothermal water

水样编号	ρ(SiO₂)/ (mg·L^-1)	热储温度/℃
水样编号	ρ(SiO₂)/ (mg·L^-1)	石英(无蒸汽损失)地温计	石英(有蒸汽损失)地温计	SiO₂计算/℃	K-Mg温标/℃
S1	30.00	79.40	83.10	81.25	94.80
S2	57.57	108.60	108.40	108.50	103.56
S3	53.50	105.00	105.40	105.20	106.90
S4	58.93	109.70	109.40	109.55	105.31
S5	59.53	110.20	109.80	110.00	109.09
S6	63.00	112.90	112.20	112.55	113.18
S7	63.23	113.20	112.40	112.80	115.61

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表 5 地热水循环深度调查

Table 5. Investigated geothermal water circulation depth

水样编号	地热增温级/ (m·℃^-1)	SiO₂热储温度/℃	年平均气温/℃	恒温带深度^[38]/m	循环深度/m
S1	29.41	81.25	4.5	25	2 282
S2	21.14	108.50	4.5	25	2 222
S3	25.71	105.20	4.5	25	2 612
S4	23.81	111.50	4.5	25	2 572
S5	24.10	110.00	4.5	25	2 572
S6	31.95	112.55	4.5	25	3 482
S7	27.47	112.80	4.5	25	3 002

下载: 导出CSV

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