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A new method for calculating the primary porosity of unconsolidated sands based on packing texture: Application to modern beach sand

机译:基于包装纹理计算未挥霍砂初级孔隙的一种新方法:现代海滩沙滩

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摘要

The primary porosity is one of the fundamental parameters for quantitatively predicting reservoir quality and studying diagenetic evolution. Primary porosity is usually estimated by empirical approaches or empirical formula, through using a single parameter, such as sorting or grain size. However, these methods have some disadvantages which lead to obvious errors. Primary porosity can be affected by multiple factors, such as particle size, sorting, grain shape and packing texture, therefor, one empirical formula is not practical for different type of sands. A new mathematical model is proposed in this paper for calculating the primary porosity of unconsolidated sands based on the concept of packing texture. The grain size, grain size distribution curve and packing texture are considered in this mathematical model. This paper tests the practicability of the mathematical model through using 40 modern beach sands sample collected from eastern China and 37 samples from literature. These modern beach sands in the study area can be divided into three types based on the particle size distribution curve. Each type sample is further divided into several units according to the particle size ratio. The mathematical model firstly calculates the primary porosity of two adjacent units by using the binary packing model, and then the primary porosity of the entire sand sample. The error of model-predicted primary porosity ranges between -2% and 2%, and the correlation coefficients are all above 0.9. As a comparison, the errors of empirical formula-predicted results range between -6% and 6%, and the correlation coefficient is 0.63. The newly-proposed mathematical model for the primary porosity based on grain size distribution and packing texture is more reliable compared to the traditional empirical formula.
机译:主要孔隙度是用于定量预测储层质量和研究成岩型进化的基本参数之一。通过使用单个参数,例如分类或晶粒尺寸,通常通过经验方法或经验公式估计主要孔隙率。然而,这些方法具有一些缺点,这导致了明显的误差。初级孔隙率可以受到多种因素的影响,例如粒度,分选,晶粒形状和填充纹理,因此,对于不同类型的砂脂,一个经验公式是不实际的。本文提出了一种新的数学模型,用于计算基于包装纹理概念的未叠加砂的主要孔隙率。在该数学模型中考虑了晶粒尺寸,粒度分布曲线和包装纹理。本文通过从中国东部和37个样品中收集的40个现代海滩沙子样本来测试数学模型的实用性。这些现代海滩砂在研究区域可根据粒度分布曲线分为三种类型。根据粒度比进一步分成几个单元。数学模型首先通过使用二元填充模型来计算两个相邻单元的主要孔隙率,然后通过整个砂样的主要孔隙率来计算。模型预测的主孔隙度误差范围为-2%和2%,并且相关系数全部高于0.9。作为比较,经验公式预测结果的误差在-6%和6%之间,相关系数为0.63。与传统经验公式相比,基于晶粒尺寸分布和包装纹理的初级孔隙率的新提出的数学模型更可靠。

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