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次生
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  secondary
    Study of Petrological Characteristics and Thermodynamic Mechanism of Secondary Pores in Deep Reservoirs, Songliao Basin
    松辽盆地深层储层岩石学特征及次生孔隙形成热力学机制
短句来源
    DISCUSSION ON THE MECHANISM OF FORMING JURASSIC SECONDARY GAS RESERVOIR IN THE SOUTH PART OF WEST SICHUAN
    川西地区南部侏罗系次生气藏形成机制探讨
短句来源
    A Study of Deep Buried Secondary Pores in Carbonate Rock of Lower Ordovician System in Eerduosi Basin
    鄂尔多斯盆地下奥陶统碳酸盐岩储层深埋次生孔隙研究
短句来源
    Abnormal high pressure plays an important role in some aspects,such as pressure compartments,secondary pore development and preservation,fluid migration leak point and its prevention from bottom water,destruction of gas reservoir by oxygen and germ in the process of Kela 2 gasfield.
    异常高压在压力封存箱、次生孔隙的发育与保存、流体运移泄漏点以及阻止地下水活动、氧和细菌对油气藏的破坏等方面,对克拉2气田的形成过程起到非常重要的作用。
短句来源
    Development Mechanism of the Secondary Pores in the Oil gas Reservoirs of Northeastern Basins of China
    东北含油气盆地储层次生孔隙形成机制
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  “次生”译为未确定词的双语例句
    Experimental Study on the Spectral Analysis of Induced Gamma-Ray
    次生伽马能谱分析方法的实验研究
短句来源
    On the basis of thin-section analysis,the area percent of pore of reservoir sandstone ranges from 9.13% to 12.66%,with moderate maturity of composition and texture.
    通过薄片分析确定,储集层砂岩有效面孔率为9.13%~12.66%,结构成熟度和成分成熟度中等,储层次生孔隙和裂缝发育。
短句来源
    The Second Hydrocarbon-generation Evolution of Palaeozoic Source Rocks in Qigu-1 Well in the Huanghua Depression
    黄骅坳陷歧古1井古生界烃源岩的二次生烃演化
短句来源
    An experiment study on influence of subfault to petroleum migration and accumulation of Guantao Formation of Feiyantan area
    次生断层对飞雁滩地区馆陶组石油运移和聚集影响的模拟实验研究
短句来源
    2. Reservoir have more induced and less primary pore;
    2.储层孔隙以次生孔隙为主,原生孔隙较少;
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  secondary
The 3D QSAR studies using Apex 3D expert system led to the identification of the pharmacophore in terms of common biophoric sites and secondary sites for interacting with PPARγ receptors.
      
1) for R isomers with correlation coefficient r =0.9, chance= 0.05 and match= 0.47 has four biophoric sites and three secondary sites while the best model for S isomers (model no.
      
2) with correlation coefficient r =0.86, chance =0.01 and match = 0.45 has three biophoric sites and two secondary sites.
      
Biological Evaluation of a Secondary Metabolite, 9-O-methylfusarubin, from Fusarium oxysporum
      
In this paper a new mathematical model of secondary frost heave is presented.
      
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  secondary pool
The increase in relative content of polysaccharides during needle senescence reflects the involvement of photosynthetic products into the secondary pool of carbon metabolites.
      
Resolution Testing For a positive Secondary Pool, test each of the individual specimens in that Secondary Pool.
      


Based on the quantitative mineralogical studies, the sandstonecomposition of the first zone of the Third Member of Shahejie Formationin Shulu Depression is thought to coincide with the interpretation oftectonic setting--the inner plate active rifting zone. It also shows theinfluence of transitions between tectonic regimes. Under certain conditionssedimentary environments have some determinative effects on the sandstonecomposition. Compaction and quartz overgrowth dominated during earlydiagenesis of the sandstones...

Based on the quantitative mineralogical studies, the sandstonecomposition of the first zone of the Third Member of Shahejie Formationin Shulu Depression is thought to coincide with the interpretation oftectonic setting--the inner plate active rifting zone. It also shows theinfluence of transitions between tectonic regimes. Under certain conditionssedimentary environments have some determinative effects on the sandstonecomposition. Compaction and quartz overgrowth dominated during earlydiagenesis of the sandstones and carbonate cementation characterizeits late diagenetic period. Authogenic kaolinite suggests that the rockshave re--entered into fresh water circulation zone.

根据定量矿物研究,束鹿凹陷沙三段一带(Es_3~1)砂岩成分,符合于板块内部活动裂谷带成因,也显示出板块相互作用转变的影响。在一定条件下,沉积环境对砂岩成分亦有决定性影响。Es_3~1砂岩在其成岩早期以压实作用和石英次生加大为主,碳酸盐胶结作用则是晚期成岩变化的特征。自生高岭石意味着成岩后再次进入雨水循环之中。

Xihepu formation (miocene) of Kokeya condensate field can be divided into two members, upper member and lower one. The former, indicated as X_4~2—X_5~2, sequenel, is a secondary oil-gas condensate reservoir with edge water and oil-ring gas cap. During the production, it is recognized that there were three periods of the reservoir pressure, i. e, stable, fall-off and build-up periods. The change in pressure gradient was evidently controlled by its edge water horizontally or vertically.Belonging to fluvial sedimentary...

Xihepu formation (miocene) of Kokeya condensate field can be divided into two members, upper member and lower one. The former, indicated as X_4~2—X_5~2, sequenel, is a secondary oil-gas condensate reservoir with edge water and oil-ring gas cap. During the production, it is recognized that there were three periods of the reservoir pressure, i. e, stable, fall-off and build-up periods. The change in pressure gradient was evidently controlled by its edge water horizontally or vertically.Belonging to fluvial sedimentary facies, this reservoir is characterized by serious heterogeneities with permeability changing from higher for the lower to lower for the upper, and the horizontal higher than the vertical. However, no cross flow occurred between zones. The effect of the edge water and gas cap on the properties of its oil-gas condensate has been variable during the period of production and, with increase of oil-gas ratio, the content of condensate was reduced generally.

柯克亚凝析油气田上第三系中新统西河甫组分上、下两套油组。上油组X_4~2—X_5~2开发层系为具边水、气顶带油环的次生凝析油气藏,地层压力在开发过程中分稳定期、衰减期和回升期三个阶段,平面或垂向的压力梯度变化明显受边水驱控制。 X_4~2—X_5~2储层属河流相沉积,非均质性严重,渗透性能具有下大上小、水平渗透率高于垂直渗透率的特点,但层间不存在窜流现象。开采过程中,油气性质受边水和气顶影响,变化不一;生产油气比不断上升,凝析油含量普遍下降。

The theoretical values of dimensioness buildup pressure P_(SD) and dimensionlesssandfacc flow rate Q_(FD) are calculated by using a program of single-well reservoirsimulation. It is found by mathematical, analysis that there is a linear relationship between P_(SD) and Q_(FD) of pressure buildup curve(including the pure wellbore storage stageand most of the transition stage)at the early-time stage. Moreover, the slop m~* of thelinear section is dependent On the dimensionless production time (t_p)_D and dimensionnesscoefficient...

The theoretical values of dimensioness buildup pressure P_(SD) and dimensionlesssandfacc flow rate Q_(FD) are calculated by using a program of single-well reservoirsimulation. It is found by mathematical, analysis that there is a linear relationship between P_(SD) and Q_(FD) of pressure buildup curve(including the pure wellbore storage stageand most of the transition stage)at the early-time stage. Moreover, the slop m~* of thelinear section is dependent On the dimensionless production time (t_p)_D and dimensionnesscoefficient C_D of wellbore storage. A new method for interpreting early-time pressurebuildup curves drawn via the data from well testing is developed. The resuits of applicationof this method in the field show that it is reliable and efficient.

本文利用单井油层的模拟程序,计算出无因次压力恢复值P_(SD)和无因次井壁产量Q_(FD)的理论数值。通过数学方法分析发现,在压力恢复曲线的早期段(包括纯井筒储集阶段和大部分过渡段)中,P_(SD)和Q_(FD)之间存在线性关系,且直线段斜率m~*和无因次生产时问(t_P)_D、无因次井筒储集系数C_D无关。因此,经过数学处理获得了压力恢复曲线早期段的新的解释方法,实例分析表明,这一解释方法是可靠而有效的。

 
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