1) SP correction
自然电位校正
2) SP(spontaneous potential)
自然电位
1.
It can provide perfect formation water resisitivity in argillaceous sand- stone by using SP(spontaneous potential)data.
地层水电阻率是测井解释中一个极其重要的参数,以纯地层条件推导的用于确定地层水电阻率的自然电位理论模型不适合泥质砂岩地层。
2.
On the basis of the theory of sequence stratigraphy,identifying sequence stratigraphy boundaries using well logging of SP(spontaneous potential),AC(acoustic time),RA(apparent resistivity),electric conductivity were comprehensively analyzed.
以层序地层学理论为基础,应用自然电位、电阻率、声波时差和感应电导率等测井资料,采用自然电位和自然电位镜像法、自然电位与视电阻率曲线组合法、声波时差法、声波时差与电阻率曲线交汇法和感应电导率法等5种方法进行层序界面识别。
3) spontaneous potential
自然电位
1.
Two-dimensional forward of spontaneous potential in interlayer oxidation zone sandstone type uranium deposits
层间氧化带型砂岩铀矿自然电位二维正演计算
2.
Strata physical nature is good for geophysical prospecting in lqe coalfield,there are less interference in the area, while the spontaneous potential curve anomalies are clearly reflected.
鱼卡煤田地层物性条件较好,区内干扰较小,自然电位曲线异常反映比较明显。
3.
The traditional model used to describe the distribution of natural electric field in open hole is interfacial potential that shows spontaneous potential distributes on the interface between formation and mud.
传统的界面电位模型认为裸眼井中自然电位分布在地层与泥浆的接触面上,这种模型不完善。
4) natural potential
自然电位
1.
The text building up the return equation with natural potential data of well tests and analyses coal sulphur content in labo- ratories,expanses the application that the natural potential data of the well tests in actual work.
文中将自然电位测井数据和实验室分析原煤全硫含量进行回归,建立回归方程,进而推广自然电位测井资料在实际工作中的应用。
2.
According to the relation of natural potential logging data and reservoir water salinity,based on the layer thickness emendation,slime emendation,temperature emendation and oil & gas effect emendation of natural potential,formation water electrical resistivity can be confirmed accurately.
根据自然电位测井数据与地层水矿化度之间的关系,在自然电位层厚校正、泥质校正、温度校正及油气影响校正基础上,可较为精确地确定地层水电阻率。
3.
Variation of natural potentials, cathodic polarization curves and variation of stable current density with time for carbon steels in flowing fresh water with different velocities and in three different surface states are tested.
在淡水中 ,对处于不同流速、3种表面状态的普通碳素钢进行了自然电位变化、阴极极化曲线和稳定电流密度随时间变化等试验 。
5) SP
自然电位
1.
Reason Analysis for SP Curve Abnormality;
自然电位曲线异常原因分析
2.
Simulated Experiment and Study SP Logging;
自然电位测井模拟实验及其研究
3.
EFFECT AND INFLUENTIAL FACTORS SP FOR OIL;
自然电位法寻找油气藏效果及影响因素
6) self-potential
自然电位
1.
Theory-based of electric double layer and electrokinetic,this paper states the main factors causing electrokinetic phenomenon are abnormal pressure and salinity decrease and multiphase flow in oil field development,and investigates the positive and negative changes of self-potential which is the expression of the streaming potential,and hig.
本文依据多孔介质中的双电层模型及动电理论,对油气田开发过程中的动电现象进行研究,提出陆相非均质复杂构造油气藏开发过程中压力异常、地层水淡化及多相流动是动电现象产生的主要原因,流动电流的形成不仅使老区新钻井的自然电位曲线发生畸变,表现为平直及正异常现象,还导致水淹层的电阻率升高,严重干扰已动用层的评价工作。
2.
Combiningthis method with phase state hydrocarbon method and self-potential method, the authorsobtained satisfactory results over some known oil and gas fields.
并将它和相态烃法、自然电位法相配合，在已知油气田开展了试验，取得令人十分满意的效果。
补充资料：表面电位与电动电位
表面电位与电动电位
surface potentials and electro- kinetic potentials
匕一oom一an dianwe一丫u dlandong dl占nwei表面电位与电动电位(surfaee potentials andeleetrokinetie Potentials)矿物界面双电层的两个重要的电性参数，表示矿物一水界面荷电的程度。浮选时矿物粒子在水溶液中要和各种离子发生作用，作用的结果经常使矿物表面的电性发生变化。故研究矿物表面的电性，即测定表面电位或电动电位的变化，可以找出矿物与浮选药剂作用的一些规律，进而分析矿物与药剂作用的机理。 表面电位是指固体表面与溶液内部的电位差，以申。表示。它主要取决于溶液中定位离子的浓度。表面电位与定位离子的活度之间的关系服从于能斯特方程，故表面电位的表达式为 RT，a+RT，a生 口n一.一二二In甲丁-一二丁In— n厂a千n厂a一式中R为气体常数;T为绝对温度;n为离子价数;F为法拉第常数;a+、a一为正、负定位离子的活度，在稀溶液中就等于它们的浓度;“年、a巴为表面电位为。时的正、负离子的活度。对于一些氧化矿物，H+和OH-离子是定位离子。当n一1，25C时上述表达式可以简化为必。=0.0591(pH。一pH)。式中pH。为表面电位为。时溶液的pH值，即为矿物的零电点。(见零电点与等电.点)可见，当溶液pH值大于矿物的零电点时矿物表面荷负电，反之荷正电。电动电位是指当溶液处在电场作用下，矿物粒子与溶液之间产生相对运动时，滑动界面上显示的电位，以夸表示。这一电位可用电泳法、电渗法、流动电位法或沉降电位法测出。使用得较多的方法是显微电泳法口对于一些氧化矿物，由于它不导电，理论研究上经常测定它的电动电位。 (龚焕高)
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条