烃源岩生排烃理论研究与泥页岩油气

泥页岩油气的研究与勘探,必然涉及到烃源岩生排烃理论.但目前的干酪根热降解晚期生烃学说,是在油页岩热解生成页岩油概念基础上的提升,其理论明显脱离石油地质演化过程的实际,以该学说为指导研制的盆地模拟方法计算的油气资源量,表示的是烃源岩总有机碳全部热解生成石油的总量,即所谓的生油(烃)潜量,不是实际的生油量.通常含油气盆地都经历了持续沉降、整体上升、全面萎缩三个明显不同的发育阶段,盆地每个发展阶段都与成烃成藏过程有密切的关联,因此成盆成烃成藏是一个相辅相成、统一的石油地质演化过程.在持续沉降阶段,主要烃源岩基本上实现了成烃过程；整体上升阶段是盆地油气成藏的重要时期,并导致油气运移；全面萎缩阶段继续成烃完善成藏,不仅使整体上升阶段形成的油气藏继续充注油气,而且形成新的油气藏.干酪根热降解生成的石油受烃源岩(泥质岩)的孔隙空间限制,即烃源岩生油是在有限空间中进行的.通过确定烃源岩孔隙体积及其含油度等可定量计算烃源岩的生油量；通过盆地整体上升前后的烃源岩孔隙体积的变小量等可定量计算烃源岩的排油量.利用自行研制的DK-Ⅱ型地层孔隙热压生排烃模拟实验仪,开展了盆地持续沉降阶段烃源岩有限空间生烃模拟实验研究.要了解泥页岩油气的特征,必须从盆地的演化阶段及其与成烃成藏的密切关联入手.     

利用测井资料确定页岩储层有机碳含量的方法优选——以焦石坝页岩气田为例

国内外利用测井资料计算页岩储层有机碳含量的方法众多,但各种计算方法都有其相应的适用性及计算精度的优劣。因此,探讨各种计算方法的适用性并最终确定页岩储层有机碳含量的区域性经验计算模型就显得尤为重要。为此,以四川盆地焦石坝地区上奥陶统五峰组—下志留统龙马溪组页岩储层为例,在继承和发展前人研究成果的基础上,结合区域地质特征,利用改进的ΔlgR技术、体积密度法、自然伽马能谱法、多元拟合法、体积模型法等分别建立了有机碳含量的计算模型,并利用岩心分析资料对模型进行对比优选,最终确立了体积密度法为区域性经验计算模型。实践证明:改进的ΔlgR技术和自然伽马能谱法计算精度相对较差;多元拟合法和体积密度法的计算成果均能满足精度要求,但体积密度法方法更为简单且适用范围更广。为进一步验证经验模型的普适性,应用该方法对焦石坝页岩气田重点井的总有机碳含量开展测井精细解释评价,并利用岩心实测资料进行精度分析,其有机碳含量测井解释符合率介于90.5%~91.0%。     

涪陵页岩气田开发建设水污染防控探索与实践

页岩气作为新兴、绿色、清洁能源,近年来在全球范围内得到越来越多的关注。从目前国内外页岩气开发情况来看,除开发工艺技术难度大以外,其开发过程中的水污染防控和工业废水的处理也是影响页岩气产业发展的当务之急。如何实现经济高效处理页岩气污水和实现水循环利用,对页岩气的长远发展和当地环境保护有着举足轻重的意义。结合中国石化涪陵页岩气田环境保护,特别是水污染防控工作实践,从页岩气开采工艺过程出发,对水污染防控措施、污水处理工艺和污水的减量循环利用进行了探讨和研究。     

Hydrodynamic behaviour of a new permeable pavement material under high rainfall conditions

Permeable pavements are among the most effective alternative solutions for sustainable stormwater management. They decrease impervious surfaces in urban areas, reduce the risk of flooding under high rainfall conditions and protect the natural environment against stormwater pollution. In a view to ensuring sustainable stormwater management, a new eco-material has been designed for producing permeable pavements. This material is a mixture of construction wastes (crushed concrete) and organic matter (compost). The crushed concrete is the structural support and the compost is used for retention and the biological treatment of stormwater pollution. The purpose of the research work presented in this paper was to evaluate the hydrodynamic behaviour of a new permeable pavement material under high rainfall conditions. The experimental approach adopted for this research study is a temporal moment analysis. Therefore, for the experimental study, we simulated high rainfall with a return period of 10 years (Torreilles in 2001, France). The rainfall data were provided by Meteo France. The rainfall was maintained at an intensity of 126 mm/h, corresponding to a flow rate of 16 l/h at laboratory apparatus scale. Then, the flow rate was increased three times, to 25 l/h, 50 l/h and finally 100 l/h to subject the material to extreme conditions.     

歧口凹陷歧北次凹沙河街组三段页岩油地质特征与勘探突破

歧口凹陷歧北次凹沙河街组三段（沙三段）湖泛期细粒沉积发育、烃源岩品质好、页岩油资源丰富，但其研究尚处于起步阶段，在沧东凹陷孔店组二段湖相页岩油工业化开发的带动下，落实其勘探前景势成必然。为探究歧北次凹沙三段页岩油的地质特征及勘探潜力，依据F39X1井、QY10-1-1井等多口井的岩心、分析化验、测井资料和录井资料，对沙三段页岩层系的地质特征、页岩油类型与富集模式、甜点的空间分布规律等开展了综合研究。歧北次凹沙三段的矿物组成和岩石类型多样，主要包括灰质白云质页岩、长英质页岩、混合质页岩及微晶白云岩、亮晶生屑白云岩、粉砂岩等；烃源岩的总有机碳（TOC）含量主要分布在1%~3%，以Ⅱ型干酪根为主且指示热演化成熟度的镜质体反射率（R_o）普遍高于0.7%；储集空间主要包括粒间孔、晶间孔、生物体腔孔、有机孔及层理缝、构造（微）缝等；页岩油的超越效应明显（油饱和度指数平均为116.3 mg/g）、荧光显示良好。在歧北次凹沙三段中识别出单一型和夹层型2类页岩油，构建了高TOC滞留型页岩油和低TOC运移型页岩油2种富集模式，并建立了基于油饱和度指数、TOC和脆性指数等多参数的甜点定量评价方法及标准。针对甜点区部署了QY10-1-1水平井，其初期的折算产油量达103.5 t/d，预计可形成亿吨级增储新领域。勘探发现证实歧口凹陷的沙三段细粒岩段具备良好的页岩油勘探潜力。     

Analysis of the corrosion failure causes of shale gas surface pipelines

A shale gas gathering and transportation pipeline in a good block in Sichuan Province started leaking after less than a year of operation. To investigate the causes of corrosion of the sulfate-reducing bacteria (SRB), optical microscopy, scanning electron microscopy, and X-ray diffraction were used to analyze the corrosion and perforation of the shale gas surface pipeline in conjunction with bacterial corrosion simulation experiments. The results showed that the pipeline material (L360N) conformed to the requirements of the American Petroleum Institute 5 L standard and that extracellular polymeric substances were present in the corrosion pits. The corrosion products mainly included FeCO₃, FeS, CaCO₃, MgCO₃, and Fe mineralization. At 40°C, the uniform corrosion rate of L360N in the simulation experiment was 0.234 mm/a, and the local corrosion rate was 0.458 mm/a. SRB, saprophytes, and iron bacteria were detected in the on-site water medium and corrosion products, indicating that the main causes of shale gas pipeline corrosion are bacterial and CO₂ corrosion.