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Study on Phase Transition and Gas Deviation Coefficient of Natural Gas with High Carbon Dioxide Content 高二氧化碳天然气相变及气相偏差系数研究
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.314014
Tao Zhou
It is the basic research subject that analyzes and calculate the law and numerical value of phase change and gas deviation coefficient of natural gas with high-CO 2 content in the process of safe and effective development of gas reservoirs, which is obtained by high-pressure physical properties PVT (Pres-sure-Volume-Temperature) experiments and different calculation methods calculations. Aiming at natural gas with high-CO 2 content in the Dongfang gas field, the phase change characteristics and physical parameters of different PVT samples are simulated and tested by Chandler 3000-GL analyzer and PVT SIM software. The experimental data shows that the phase state of natural gas with different content of CO 2 has not changed in the study range. At the same time, the deviation coefficient calculated by different calculation methods (DPR, DAK, BB, HY, Gopal) are compared with the experimental data, and the applicable scope of different calculation methods are obtained. The results show that the improved Gopal has high accuracy and is suitable for the calculation of the deviation coefficient of natural gas with high-CO 2 content under high temperature and high pressure in the Dongfang gas field.
通过高压物性PVT (pressure - volume - temperature,压力-体积-温度)实验和不同计算方法计算得到的高co2含量天然气在气藏安全有效开发过程中的相变和气偏差系数规律及数值,是基础研究课题。针对东方气田高co 2含量天然气,利用Chandler 3000-GL分析仪和PVT SIM软件对不同PVT样品的相变特征和物性参数进行了模拟测试。实验数据表明,在研究范围内,不同CO 2含量天然气的相态没有发生变化。同时,将不同计算方法(DPR、DAK、BB、HY、Gopal)计算出的偏差系数与实验数据进行对比,得出不同计算方法的适用范围。结果表明,改进后的Gopal具有较高的精度,适用于计算东方气田高温高压下高co 2含量天然气的偏差系数。
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引用次数: 1
Structural Characteristics and Evolution Process of the Metamorphic Buried Hill: A Case of BZ Oilfield in Bohai Bay, China 变质岩潜山构造特征及演化过程——以渤海湾BZ油田为例
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.131001
Huaichang Zheng, Xuwei Bie, Xin-Qiang Song, Yong Jiang, Wencai Liu
Bozhong oilfield which is abbreviated as BZ oilfield is the first oilfield with deep metamorphic buried hill that is discovered reserves of billion-ton in Bohai Bay. Affected by multi-stage tectonic movements, the distribution of fractures is very complex in this area, therefore it is significant to study the evolution of structures for understanding the distribution of fractures. In view of the complexity on the tectonic evolution of the buried hill region in the study area, the influence of tectonic movements on the formation of fractured reservoir is analyzed, and the research results lay the foundation for the efficient development in this type of the oilfield. The results show that main faults, which is formed during early Indosinian and Yanshanian period, are mainly developed in the BZ oilfield area, and the fracture strike has mainly east-west and north-east-east trend. Based on the analysis of the relationship among tectonic evolution, regional stress field and fracture development, it is considered that Indosinian extrusion is the main reason for the formation of main direction faults in the study area. Yanshanian strike-slip transformation and Himalayan reactivation further controlled the development of the fractured reservoirs in the later stage, and formed the present fracture network system. Well block 5 is located in passive plate system during Indosinian period, it is affected by Himalayan stretching and long-term activation of large faults in the later stage, so that the effective fractures are relatively developed. The result plays an important role in guiding the overall plan deployment of the BZ oilfield.
渤中油田,简称BZ油田,是渤海湾地区第一个探明储量达十亿吨的深变质潜山油田。受多期构造运动的影响,本区裂缝分布十分复杂,因此研究构造演化对认识裂缝分布具有重要意义。针对研究区潜山地区构造演化的复杂性,分析了构造运动对裂缝性储层形成的影响,为该类型油田的高效开发奠定了基础。结果表明:BZ油区主要发育早印支期和燕山期形成的主断裂,裂缝走向以东-西、北-东走向为主;在分析构造演化、区域应力场与断裂发育关系的基础上,认为印支挤压作用是研究区主向断裂形成的主要原因。燕山期走滑改造和喜马拉雅期再活化进一步控制了裂缝性储层的后期发育,形成了现今的裂缝网络体系。5井区块在印支期处于被动板块体系,后期受喜马拉雅拉张和大断裂长期活化的影响,有效裂缝相对发育。研究结果对指导BZ油田总体规划部署具有重要意义。
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引用次数: 1
TEC Variability during Fluctuating Events at Koudougou Station during Solar Cycle 24 第24太阳活动周期间口斗沟站波动事件中的TEC变率
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.1310047
Tinlé Pahima, D. A. Gnabahou, Sibri Alphonse Sandwidi, F. Ouattara
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引用次数: 1
Evaluation of the Influence of Shale on the Petrophysical Properties of Hydrocarbon-Bearing Reservoir Sand in “CAC” Field in the Niger Delta, Nigeria 尼日利亚尼日尔三角洲“CAC”油田页岩对含油气储层砂岩物性影响评价
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.131005
C. C. Ugbor, Chinwe Adaobi Obumselu, Jethro O. Ogboke
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引用次数: 0
Study of the Geothermal Potential of the Locality of Kaladi and Its Surroundings (Adamawa-Cameroon) from the Frequency Processing of Magnetic Data 从磁资料的频率处理研究Kaladi及其周边地区(adamawa -喀麦隆)的地热潜力
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.1311052
Ndam Njikam Mohamed Moustapha, Meying Arsène, Z. Alain, Abdou Raouf, Nkemndem Agendia Demianus
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引用次数: 0
The Importance of Integrating Geological Mapping Information with Validated Assay Data for Generating Accurate Geological Wireframes in Orebody Modelling of Mineral Deposit in Mineral Resource Estimation: A Case Study in AngloGold Ashanti, Obuasi Mine 结合地质填图信息和验证分析数据生成准确地质线框在矿产资源估算中矿床矿体建模中的重要性——以盎格鲁阿散蒂奥布西矿为例
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.136023
Joshua Wereko Opong, Chiri G. Amedjoe, A. Asante, M. C. Wilson
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引用次数: 0
Groundwater Exploration Using Multi Criteria Decision Analysis and Analytic Hierarchy Process in Federal Capital Territory, Abuja, Central Nigeria 利用多准则决策分析和层次分析法在尼日利亚中部阿布贾联邦首都地区进行地下水勘探
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.131003
J. S. Ejepu, Muftau Owolabi Jimoh, S. Abdullahi, Marrietta Adaobi Mba
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引用次数: 6
Electrical Resistivity Sounding for Groundwater Investigation around Enugu Metropolis and the Environs, Southeast Nigeria 尼日利亚东南部埃努古大都市及其周边地区地下水电阻率测深研究
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.131004
Claris C. Nwachukwu, C. C. Ugbor, Osim Jethro Ogboke
This report evaluates the use of electrical method and borehole data to investigate the subsurface to delineate the groundwater potential in Enugu metropolis and the environs, south-eastern Nigeria other than rely only on resistivity method which could lead to interpretation error. Integrating these 2 data sets is key in this study. The study area is located in the Anambra Basin and is underlain by Nkporo/Enugu Shale which is overlain by the Mamu Formation. It is bounded by Latitudes 6 ̊2 0'00"N to 6 ̊30'00"N and Longitudes 7 ̊25'00"E to 7 ̊35'00"E and covers surface area of about 342 m2. Thirty-one vertical electrical soundings (VES) were carried out across the area using the Schlumberger electrode array with current electrode separation from 2 to 500 m to identify the depths and resistivity values of the identified geo-electric layers. Through data analysis using WinResist software, the apparent resistivity, thicknesses and depths and the thicknesses of the aquifers were generated. The resistivity and depths were modelled to generate resistivity map and depth map. The resistivity of the aquiferous zone within the study area varied from 20.55 427.8 ohm-m at depths of between 10.7 40.05 m. Depth to the water table appears to be shallow at the south western part of the map. The interpreted geo-electric layers show a sequence of lateritic top soil, shale, sand and shale. The frequency distribution of the VES curves generated shows the presence of 3 to 5 layers with HK type as the highest. Also, a 2D model was generated using the correlation of VES to VES data and borehole data to VES data to show the underlying stratigraphy beneath the study area as well as the direction of ground water flow. Result of the VES curve analysis reveals that the sub-surface is underlain by three lithological layers namely: lateritic top soil, shale, sand and shales with NW direction of groundwater flow from the 2D model. Groundwater prospective zones can be seen along NW, SW and How to cite this paper: Nwachukwu, C.C., Ugbor, C.C. and Ogboke, O.J. (2022) Electrical Resistivity Sounding for Groundwater Investigation around Enugu Metropolis and the Environs, Southeast Nigeria. International Journal of Geosciences, 13, 54-70. https://doi.org/10.4236/ijg.2022.131004 Received: September 26, 2021 Accepted: January 26, 2022 Published: January 29, 2022 Copyright © 2022 by author(s) and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Open Access C. C. Nwachukwu et al. DOI: 10.4236/ijg.2022.131004 55 International Journal of Geosciences central parts of the study area which have low resistivity values.
本报告评估了在尼日利亚东南部埃努古市及其周边地区,利用电法和钻孔数据调查地下以划定地下水潜力,而不是仅仅依靠可能导致解释误差的电阻率法。整合这两个数据集是本研究的关键。研究区位于Anambra盆地,下覆Nkporo/Enugu页岩,上覆Mamu组。它以北纬6纬20′00”~ 6纬30′00”,东经7纬25′00”~ 7纬35′00”为界,面积约342平方米。使用斯伦贝谢电极阵列,在整个区域内进行了31次垂直电测深(VES),电流电极间距为2至500 m,以确定已识别的地电层的深度和电阻率值。利用WinResist软件对数据进行分析,得到视电阻率、厚度、深度及含水层厚度。对电阻率和深度进行建模,生成电阻率图和深度图。研究区内含水层电阻率变化范围为20.55 ~ 27.8 ω -m,深度为10.7 ~ 0.05 m。在地图的西南部分,地下水位的深度似乎很浅。解释的地电层为红土表土-页岩-砂-页岩序列。生成的电磁测深曲线的频率分布显示存在3 ~ 5层,以HK型最高。利用VES数据与VES数据、钻孔数据与VES数据的相关性,生成二维模型,显示研究区下伏地层及地下水流动方向。VES曲线分析结果表明,地下发育红土、页岩、砂、页岩3个岩性层,2D模型地下水流向为NW方向。Nwachukwu, C.C., Ugbor, C.C.和Ogboke, O.J.(2022)尼日利亚东南部埃努古大都市及其周边地区地下水电阻率测深调查。地球科学进展,26(3):544 - 544。https://doi.org/10.4236/ijg.2022.131004收稿日期:2021年9月26日收稿日期:2022年1月26日出版日期:2022年1月29日版权所有©2022 by作者和Scientific Research Publishing Inc。本作品采用知识共享署名国际许可协议(CC BY 4.0)。http://creativecommons.org/licenses/by/4.0/ Open Access C. C. Nwachukwu等。研究区中部低电阻率值区域。
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引用次数: 1
Geological Specimens, Minerals, and Actions Affecting Polar Shift and Earth’s Magnetic Field 影响极移和地球磁场的地质标本、矿物和活动
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.1310043
Shreyas Banaji
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引用次数: 0
My Research Connections with Russian Scientists over the Past Half Century 我在过去半个世纪里与俄罗斯科学家的研究联系
Pub Date : 2022-01-01 DOI: 10.4236/ijg.2022.133009
R. Liebermann
Over the past half century, I have maintained research connections with Russian scientists during investigations in seismology and mineral physics. These studies have focused on detection and discrimination of underground nuclear explosions and measurements of the physical properties of minerals at high pressures and temperatures. During this period, I have also visited many research laboratories in Russia, including Moscow, Chernogolovka, Novosibirsk and St. Petersburg. The objective of this paper is to relate this history.
在过去的半个世纪里,我在地震学和矿物物理学的研究中与俄罗斯科学家保持着研究联系。这些研究的重点是探测和辨别地下核爆炸以及在高压和高温下测量矿物的物理性质。在此期间,我还参观了俄罗斯的许多研究实验室,包括莫斯科、切尔诺戈洛夫卡、新西伯利亚和圣彼得堡。本文的目的是将这段历史联系起来。
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引用次数: 0
期刊
地球科学国际期刊(英文)
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