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A novel laboratory method for reliable water content determination of shale reservoir rocks

机译:一种新型实验室方法,可靠含水量测定页岩储层岩石

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摘要

The paper presents a novel laboratory evaporation method (EM) of the water saturation measurement of the shale reservoir rock samples with initial water content down to below 1 wt%. The EM offers fast, efficient, and accurate measurements of the total water content, free and loosely clay-bound water. The method is characterized in terms of its operating domain and relative measurement error. The research results show that a good quality data set requires the use of fresh samples with a maximum preserved initial water saturation, fragmented into pieces with specific dimensions of a few centimetres. A comprehensive comparison between the EM and the Dean-Stark method conducted on low-permeable shale rocks of the Bazhenov formation clearly shows EM's advantages regarding accuracy and turn-around time.
机译:本文提出了一种新的实验室蒸发方法(EM)的水饱和度测量,初始水含量下降至低于1wt%。 EM提供快速,高效,准确地测量总水含量,自由且松散地粘土水。 该方法的特征在于其操作域和相对测量误差。 研究结果表明,良好的质量数据集需要使用最大保存的初始水饱和度的新鲜样品,分离成具有几厘米的特定尺寸的块。 EM与Bazhenov Mailation的低可渗透页岩岩石中进行的全面比较明确显示了EM的准确性和周转时间的优势。

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