- Article
Assessment of the Swelling Potential of the Brebi, Mera, and Moigrad Formations from the Transylvanian Basin Through the Integration of Direct and Indirect Geotechnical and Mineralogical Analysis Methods
- Ioan Gheorghe Crișan,
- Octavian Bujor and
- Eduárd András
- + 2 authors
This study evaluates the swelling potential in clayey soils of the Paleogene Brebi, Mera, and Moigrad formations in the Transylvanian Basin (Romania) by integrating direct free-swelling tests (FS; STAS 1913/12-88) with indirect index-property diagrams and semi-quantitative X-ray diffraction (XRD; RIR method). The indirect analysis combines three swelling-susceptibility classification charts—Seed et al. (AI–clay), Van der Merwe (PI–clay), and Dakshanamurthy and Raman (LL–PI)—with mineralogical trends from the Casagrande plasticity chart, complemented by Holtz and Kovacs’s clay-mineral reference fields and Skempton’s activity concept (AI = PI/% < 2 µm). The geotechnical dataset comprises 88 Brebi, 46 Mera, and 263 Moigrad specimens (with parameter counts varying by test), an XRD was performed on a representative subset. The free swell (FS) results indicate that Brebi soils range from low to active behavior (50–135%) without reaching the very active class; most Brebi specimens fall in the medium-activity range. Moigrad spans the full FS spectrum (20–190%) but is predominantly in the medium-to-active range. In contrast, Mera soils exhibit predominantly active behavior, covering the full range of activity classes (30–170%). The empirical classification charts diverge systematically: clay-sensitive schemes tend to assign higher swell susceptibility than the LL–PI approach, especially in carbonate-influenced soils. XRD results corroborate these patterns: Brebi is calcite-rich (mean ≈ 53.5 wt% CaCO3) with minor expandable minerals (mean ≈ 3.1 wt%); Mera is feldspathic (orthoclase mean ≈ 55.3 wt%) with variable expandable phases; and Moigrad has a higher clay-mineral content (mean ≈ 38.8 wt%). Overall, swelling is controlled by the combined effects of clay-fraction reactivity, clay volume continuity, and carbonate-related microstructural constraints.
3 February 2026


![Geological overview. (A)—Geological map of the north-western Transylvanian Basin and its surroundings (modified by [18], based on [19]); (B)—Simplified geological map of the Sânpaul commune area of interest (based on [20]); (C)—Simplified geological map of the Cluj area of interest [21].](https://mdpi-res.com/cdn-cgi/image/w=470,h=317/https://mdpi-res.com/geotechnics/geotechnics-06-00016/article_deploy/html/images/geotechnics-06-00016-g001-550.jpg)
![Violin plots for input parameters from the study by Chen et al. [8].](https://mdpi-res.com/cdn-cgi/image/w=281,h=192/https://mdpi-res.com/geotechnics/geotechnics-06-00015/article_deploy/html/images/geotechnics-06-00015-g001-550.jpg)

