Dolostones in the Cambrian Longwangmiao Formation have become one of the most significant gas exploration domains in China. Over a trillion cubic meters of gas reservoirs have been discovered in the Gaoshiti-Moxi area...Dolostones in the Cambrian Longwangmiao Formation have become one of the most significant gas exploration domains in China. Over a trillion cubic meters of gas reservoirs have been discovered in the Gaoshiti-Moxi area; however, the origins and distribution of the dolostone reservoirs are not well understood. This work discussed the geology and geochemistry of the dolostone reservoirs in the Longwangmiao Formation to determine their origin and distribution. Two understandings are acquired： firstly, a carbonate ramp provided excellent conditions for grain beach deposition, while the presence of a hypersaline lake was favorable for the contemporaneous dolomitization of grain beach deposits. Petrographic and geochemical evidence further confirm that the Longwangmiao dolostone was formed during the contemporaneous stage. Secondly, the reservoir characteristics indicate that the grain beach sediments provide material basis for the development of the Longwangmiao dolostone reservoirs. Reservoir dissolution simulation experiments show that the porosity of the reservoirs was formed by dissolution during contemporaneous and burial stages. The dissolution pores formed during the contemporaneous stage were controlled by sequence interfaces. The large scale dissolution vugs formed during the burial stage subsequently spread along the pre-existing porosity and fracture zones. This study therefore identified that the development of grain dolostone reservoirs in a shallow water ramp under arid climatic conditions generally met the following conditions：（1） reefal beach deposits lay a foundation for reservoir development;（2） superficial conditions are an important determining factor for reservoir porosity; and（3） burial conditions provide environment for porosity preservation and modification.展开更多
A new method for reconstructing the geological history of hydrocarbon accumulation is developed, which are constrained by U-Pb isotope age and clumped isotope((35)47) temperature of host minerals of hydrocarbon-bearin...A new method for reconstructing the geological history of hydrocarbon accumulation is developed, which are constrained by U-Pb isotope age and clumped isotope((35)47) temperature of host minerals of hydrocarbon-bearing inclusions. For constraining the time and depth of hydrocarbon accumulation by the laser in-situ U-Pb isotope age and clumped isotope temperature, there are two key steps:(1) Investigating feature, abundance and distribution patterns of liquid and gaseous hydrocarbon inclusions with optical microscopes.(2) Dating laser in-situ U-Pb isotope age and measuring clumped isotope temperature of the host minerals of hydrocarbon inclusions. These technologies have been applied for studying the stages of hydrocarbon accumulation in the Sinian Dengying gas reservoir in the paleo-uplift of the central Sichuan Basin. By dating the U-Pb isotope age and measuring the temperature of clumped isotope((35)47) of the host minerals of hydrocarbon inclusions in dolomite, three stages of hydrocarbon accumulation were identified:(1) Late Silurian: the first stage of oil accumulation at(416±23) Ma.(2) Late Permian to Early Triassic: the second stage of oil accumulation between(248±27) Ma and(246.3±1.5) Ma.(3) Yanshan to Himalayan period: gas accumulation between(115±69) Ma and(41±10) Ma. The reconstructed hydrocarbon accumulation history of the Dengying gas reservoir in the paleo-uplift of the central Sichuan Basin is highly consistent with the tectonic-burial history, basin thermal history and hydrocarbon generation history, indicating that the new method is a reliable way for reconstructing the hydrocarbon accumulation history.展开更多
Objective The recent discovery of commercial natural gas accumulations in the Middle Permian coarse-crystalline dolomites in the northwest Sichuan Basin has attracted attention to the formation mechanism of these deep...Objective The recent discovery of commercial natural gas accumulations in the Middle Permian coarse-crystalline dolomites in the northwest Sichuan Basin has attracted attention to the formation mechanism of these deep-burial carbonate reservoirs.Due to their temporal relationship to the flooded basalts that represent the end-Middle-Permian Emeishan Large Igneous Province(ELIP),the Middle Permian dolomites were prev iously thought to be products of hydrothermal dolomitization related to the ELIP magmatism.Field and core observations,however,show that the occurrence and distribution of these dolomites are not controlled by faults,the supposed conduits for hydrothermal fluids.Conversely,they are somewhat strata-bound.Hence,the objective of this study,by employing LA-ICP-MS U-Pb dating,clumped isotope thermometry(047)and routine stable isotope geochemistry(C carbon,O oxygen and Sr strontium isotopes),is to re-evaluate the genesis of these dolomite reservoirs,with special attention focusing on the diagenetic environment and timing of dolomitization,and the attributes of dolomitizing fluids.展开更多
文章立足于电池储能应急支撑与规模化应用背景,指出电池储能电站(Battery Energy Storage Power Station,BESPS)即插即用(Plug and Play,PNP)的现实需求。通过分析2018年7月投运的江苏镇江MW级BESPS典型架构,首次提出实现BESPS PNP运行...文章立足于电池储能应急支撑与规模化应用背景,指出电池储能电站(Battery Energy Storage Power Station,BESPS)即插即用(Plug and Play,PNP)的现实需求。通过分析2018年7月投运的江苏镇江MW级BESPS典型架构,首次提出实现BESPS PNP运行的关键技术应从信息流和能量流两个维度进行考虑。针对信息流层面分层通信要求,提出了BESPS并网自描述模型建立方法与信息交互机制,并阐述了分层通信的具体实现方法。针对能量流层面的物理接口集成驱动技术要求,研究并综述BESPS多状态平滑切换、主动电压与频率支撑、削峰填谷以及黑启动等高级应用。最后,采用多状态平滑切换的控制算法,通过仿真对BESPS能量流层面的柔性接入与退出响应过程进行验证。文章的研究工作对开发具有增强的可扩展性PNP功能BESPS设备,解决BESPS规模化灵活并网等实现问题有十分积极的指导意义与参考价值。展开更多
基金granted by the National Major Science and Technology Projects (grant No.2016ZX05004002)PetroChina Major Science and Technology Projects (grant No.2014E-32)PetroChina Science and Technology Projects (grant No.2016B-0402-01)
文摘Dolostones in the Cambrian Longwangmiao Formation have become one of the most significant gas exploration domains in China. Over a trillion cubic meters of gas reservoirs have been discovered in the Gaoshiti-Moxi area; however, the origins and distribution of the dolostone reservoirs are not well understood. This work discussed the geology and geochemistry of the dolostone reservoirs in the Longwangmiao Formation to determine their origin and distribution. Two understandings are acquired： firstly, a carbonate ramp provided excellent conditions for grain beach deposition, while the presence of a hypersaline lake was favorable for the contemporaneous dolomitization of grain beach deposits. Petrographic and geochemical evidence further confirm that the Longwangmiao dolostone was formed during the contemporaneous stage. Secondly, the reservoir characteristics indicate that the grain beach sediments provide material basis for the development of the Longwangmiao dolostone reservoirs. Reservoir dissolution simulation experiments show that the porosity of the reservoirs was formed by dissolution during contemporaneous and burial stages. The dissolution pores formed during the contemporaneous stage were controlled by sequence interfaces. The large scale dissolution vugs formed during the burial stage subsequently spread along the pre-existing porosity and fracture zones. This study therefore identified that the development of grain dolostone reservoirs in a shallow water ramp under arid climatic conditions generally met the following conditions：（1） reefal beach deposits lay a foundation for reservoir development;（2） superficial conditions are an important determining factor for reservoir porosity; and（3） burial conditions provide environment for porosity preservation and modification.
基金Supported by the China National Science and Technology Major Project(2016ZX05004-002)Basic Research and Strategic Reserve Technology Research Fund of Institutes Directly Under CNPC(2018D-5008-03)PetroChina Science and Technology Project(2019D-5009-16)。
文摘A new method for reconstructing the geological history of hydrocarbon accumulation is developed, which are constrained by U-Pb isotope age and clumped isotope((35)47) temperature of host minerals of hydrocarbon-bearing inclusions. For constraining the time and depth of hydrocarbon accumulation by the laser in-situ U-Pb isotope age and clumped isotope temperature, there are two key steps:(1) Investigating feature, abundance and distribution patterns of liquid and gaseous hydrocarbon inclusions with optical microscopes.(2) Dating laser in-situ U-Pb isotope age and measuring clumped isotope temperature of the host minerals of hydrocarbon inclusions. These technologies have been applied for studying the stages of hydrocarbon accumulation in the Sinian Dengying gas reservoir in the paleo-uplift of the central Sichuan Basin. By dating the U-Pb isotope age and measuring the temperature of clumped isotope((35)47) of the host minerals of hydrocarbon inclusions in dolomite, three stages of hydrocarbon accumulation were identified:(1) Late Silurian: the first stage of oil accumulation at(416±23) Ma.(2) Late Permian to Early Triassic: the second stage of oil accumulation between(248±27) Ma and(246.3±1.5) Ma.(3) Yanshan to Himalayan period: gas accumulation between(115±69) Ma and(41±10) Ma. The reconstructed hydrocarbon accumulation history of the Dengying gas reservoir in the paleo-uplift of the central Sichuan Basin is highly consistent with the tectonic-burial history, basin thermal history and hydrocarbon generation history, indicating that the new method is a reliable way for reconstructing the hydrocarbon accumulation history.
基金jointly funded by the China National Science and Technology Major Project(granted No.2016ZX05004-002 and 2018A-0103)PetroChina Science and Technology Project(granted No.2018D-5006-35)。
文摘Objective The recent discovery of commercial natural gas accumulations in the Middle Permian coarse-crystalline dolomites in the northwest Sichuan Basin has attracted attention to the formation mechanism of these deep-burial carbonate reservoirs.Due to their temporal relationship to the flooded basalts that represent the end-Middle-Permian Emeishan Large Igneous Province(ELIP),the Middle Permian dolomites were prev iously thought to be products of hydrothermal dolomitization related to the ELIP magmatism.Field and core observations,however,show that the occurrence and distribution of these dolomites are not controlled by faults,the supposed conduits for hydrothermal fluids.Conversely,they are somewhat strata-bound.Hence,the objective of this study,by employing LA-ICP-MS U-Pb dating,clumped isotope thermometry(047)and routine stable isotope geochemistry(C carbon,O oxygen and Sr strontium isotopes),is to re-evaluate the genesis of these dolomite reservoirs,with special attention focusing on the diagenetic environment and timing of dolomitization,and the attributes of dolomitizing fluids.
文摘文章立足于电池储能应急支撑与规模化应用背景,指出电池储能电站(Battery Energy Storage Power Station,BESPS)即插即用(Plug and Play,PNP)的现实需求。通过分析2018年7月投运的江苏镇江MW级BESPS典型架构,首次提出实现BESPS PNP运行的关键技术应从信息流和能量流两个维度进行考虑。针对信息流层面分层通信要求,提出了BESPS并网自描述模型建立方法与信息交互机制,并阐述了分层通信的具体实现方法。针对能量流层面的物理接口集成驱动技术要求,研究并综述BESPS多状态平滑切换、主动电压与频率支撑、削峰填谷以及黑启动等高级应用。最后,采用多状态平滑切换的控制算法,通过仿真对BESPS能量流层面的柔性接入与退出响应过程进行验证。文章的研究工作对开发具有增强的可扩展性PNP功能BESPS设备,解决BESPS规模化灵活并网等实现问题有十分积极的指导意义与参考价值。
