typical curve meaning in Chinese
标准曲线
典型曲线
Examples
- As a result , the typical curves recorded in on - line tests are given in the summery
在课题小结部分，介绍了软件的功能，并给出了现场运行的实测曲线。 - The studies of in - layer heterogeneity are as follows : the text depicts the characteristics of heterogeneity by calculating the coefficient of variability , kmax / k and k . max / k . min of sand layers of different sedimentous microfacies ; divides interlayer into two types , and counts their numbers , thickness , frequency and density of a single sand layer according to the characteristics of lithology and logging , finally summarizes the characteristics of interlayer distributing ; sets up five in - layer heterogeneity models and points out that the primary models are model a and c . the studies of between - layer heterogeneity are as follows : the text depicts sand layers " growth and distributing conditions by calculating the lamination factor , sandstone density and overlap coefficient ; makes certain the lithology and thickness of interlayer by the method of contrasting the typical curves
层内非均质性研究，通过计算不同沉积微相砂体渗透率的变异系数、突进系数以及级差来说明主要储集微相的非均质特征；据岩性及电性特征，将层内夹层分为两类，统计单砂层段内夹层的个数、累积夹层厚度、夹层频率及夹层密度，并且根据夹层频率及密度平面分布图统计出每层的频率相对高值区和低值区，总结夹层分布特征；根据物性参数随深度的变化趋势建立了五种储层层内物性非均质模式，指出研究区内以a型和c型模式为主。 - This paper describes the conjunction relationship of the basic point of the flat surface outline on the parts and reveals the internal law of the intersections connecting with the typical curve ; the principle of the calculation and the characteristics on straight line to parabola basic points are illustrated
摘要介绍了平面轮廓零件各组成元素之间的连接关系，并揭示了典型曲线交接的内在规律，阐述了直线与抛物线交接点的计算原理和特点，总结归纳直线与抛物线连接的处理方法，以及自动淘汰无效基点的基本准则。 - This paper has described the principle of the contact polarization curve method and the technique for measuring basic parameters , analyzed the influence of such factors as oxidation conditions of the ore deposits , arrangement of electrodes and structures of orebodies on the basis of studying some typical polarization curves , inferred several parameters such as independency of orebodies , reacted minerals , effective areas of reacted minerals , reserves of elements and grades of elements for some measured typical curves , and compared the inferences with the exploration results
摘要介绍了接触极化曲线法的原理及基本参数的测取方法；通过一些典型极化曲线，对矿床氧化状态、电极排布、矿体结构等因素的影响作了分析；对所测得的部分典型曲线进行了矿体独立性、反应矿物、反应矿物有效面积、元素储量、元素品位等参数的推断，并将推断与勘探结果进行了对比分析。