1. 长安大学地球科学与资源学院,陕西,西安,710064
2. 延安大学石油工程与环境工程学院,陕西,延安,716000
3. 延长油田股份有限公司杏子川采油厂,陕西,延安,717400
4. 陕西延长石油(集团)有限责任公司研究院,陕西,西安,710000
[ "王霞(1982—),女,讲师,在读博士研究生,石油地质学研究。" ]
纸质出版:2018
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王霞, 付国民, 郭爱华, 等. 低孔低渗储层有效厚度确定方法研究——以安塞油田长2储层为例[J]. 油气藏评价与开发, 2018,8(6):1-6.
Wang Xia, Fu Guomin, Guo Aihua, et al. Research on determination of effective thickness for oil reservoirs with low permeability: A case of Chang-2 reservoir of Ansai oilfield[J]. Petroleum Reservoir Evaluation and Development, 2018, 8(6): 1-6.
王霞, 付国民, 郭爱华, 等. 低孔低渗储层有效厚度确定方法研究——以安塞油田长2储层为例[J]. 油气藏评价与开发, 2018,8(6):1-6. DOI: 10.13809/j.cnki.cn32-1825/te.2018.06.001.
Wang Xia, Fu Guomin, Guo Aihua, et al. Research on determination of effective thickness for oil reservoirs with low permeability: A case of Chang-2 reservoir of Ansai oilfield[J]. Petroleum Reservoir Evaluation and Development, 2018, 8(6): 1-6. DOI: 10.13809/j.cnki.cn32-1825/te.2018.06.001.
针对安塞油田长2储层低孔、低渗、物性变化快、纵横向非均质性强的地质特点
综合应用目的层段的岩心分析、试油、生产动态及测井等资料
在储层四性关系研究基础上
采用直方图法和交会图法确立了有效厚度下限标准
采用多种测井曲线半定量、半定性分析结合的方式
建立了不同类型夹层测井定量识别图及夹层扣除标准。研究区长2储层有效厚度含油性下限为油迹级
岩性下限为细砂岩
物性下限为孔隙度11.5 %、渗透率0.63×10
-3
μm
2
电性下限为
RILD
≥13 Ω·m、Δ
t
≥230 μs/m;夹层类型主要为泥质夹层和钙质夹层
利用自然伽马、声波时差、井径和微梯度等曲线的定量和自然电位、深感应电阻率、中感应电阻率、微球电阻率及微电位等曲线的定性可以识别和扣除夹层。
The Chang-2 reservoir of Ansai oilfield has the geological characteristics of low porosity
low permeability
fast change of physical properties and strong vertical and horizontal heterogeneity. Based on the
''
four properties
''
relation of reservoir
we established the minimum standards of effective thickness by using the core analysis
oil test
production dynamics and logging by the way of histogram method and cross plot method. Then we proposed the different types of interlayer logging quantitative identification chart and the elimination criterion of various interlayer on the basis of the semi-quantification and semi-qualitative analysis by m
any kinds of logging curves. The minimum values were as follows: the oil-bearing property was to see the grease spots; the lithological property was to see the fine-grained sandstone; the physical property were the porosity was more than or equaled to 11.5 % and the permeability was more than or equaled to 0.63×10
-3
μm
2
; the electrical property were the resistivity was more than or equaled to 13 Ω·m and the acoustic was more than or equaled to 230 μs/m. The main types of interlayer were calcareous interlayer and muddy interlayer. We could identify and eliminate the interlayer by the quantification of curves of natural gamma
acoustic and microelectrode
and the qualitative analysis of the curves of spontaneous potential
RILD
RILM
microsphere resistivity and micronormal.
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