Research Article

A Case Study of Thaumasite Sulfate Attack in Tunnel Engineering

Table 2

Identification results of surrounding rock samples in section YK34 + 500.

No.Test itemsTest results/descriptions

1Name of rock sampleGypsum rock
2Naked-eye observation on colorGrey-white
3Sample preparationThin slice
4StructureGranular structure
5TectonicsLump
6Identification basisGB/T17412.1
7Essential mineral97%-98% gypsum
8Secondary minerals2-3% dolomite
9Accessory mineralApatite
10Microscopic observationThe rock has lump tectonics and a granular structure.
Gypsum is tabular and colorless with a particle size distribution of 0.01–2.0 mm and has a negative protrusion. The highest interference color is first-order yellow and white, and cleavage in one direction is observed.
Dolomite has a semi-automorphic rhombohedral shape with a particle size distribution of 0.01–0.03 mm and is unevenly distributed. It has a prominent flash protrusion and high-order white interference color.