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February 5, 2026Minerals2 citationsOpen Access

Pore Structure and Fractal Dimension Analysis of Nephrite Deposits in Luanchuan, Western Henan, Central China

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XWXiaodi WangWLWeiqing LiuLZLixin Zhang

Key Points

  • This research aims to analyze the pore structure and fractal dimensions of nephrite deposits to evaluate their quality.
  • Utilized scanning electron microscopy (SEM) for detailed imaging.
  • Applied X-ray diffraction (XRD) to identify mineral composition.
  • Employed low-temperature nitrogen adsorption (LT-N2GA) for pore analysis.
  • Calculated fractal dimensions using the FHH model.
  • Identified three varieties of micropores in the nephrite deposit.
  • Found nitrogen adsorption curves resembling type IV with hysteresis loops categorized as H2 and H3.
  • Measured average fractal dimensions of 2.474 and 2.572, indicating irregular pore surfaces.
  • Established correlations between specific surface area and mineral content.

Abstract

Pore structure and fractal dimension analysis of nephrite deposits are essential for assessing potential quality, conducting investigations, and exploiting jade resources. This research explored nephrite (tremolite) jade from Tonggou in the Luanchuan Group, utilizing techniques such as scanning electron microscopy (SEM), X-ray diffraction (XRD), and low-temperature nitrogen adsorption (LT-N2GA) to illustrate the pore structure of the jade deposit and to examine its developmental features, complexity, and implications for jade quality assessment. The findings revealed that the Tonggou nephrite jade deposit comprises three varieties of micropores. The nitrogen adsorption curve was similar to type IV, featuring hysteresis loops that were mainly classified as H2 and H3, suggesting a predominantly mesoporous nature. The fractal dimensions (DF1 and DF2), determined using the FHH model, averaged 2.474 and 2.572, respectively. This implies that the pore surface of the Tonggou jade deposit is irregular, the pore structure is intricate, and displays a pronounced heterogeneity. In the Tonggou deposit, the specific surface area (SSA) and pore volume (PV) show moderate positive and negative correlations with antigorite and calcite, respectively. Tremolite exhibits a strong negative correlation with SSA. The fractal dimension reveals weak, moderate, and strong negative correlations with SSA, PV, and average pore size (APS), respectively. As the content of siliceous minerals increases, the fractal dimension gradually increases. Conversely, a rise in carbonate mineral content results in a gradual decrease in the fractal dimension.

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Cite This Study

Wang et al. (2026) studied this question.

synapsesocial.com/papers/698435b9f1d9ada3c1fb4ce4https://doi.org/10.3390/min16020170
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