Causes of seepage water in drainage and grouting galleries of the Pandoh Dam, Central Himalaya

At the Pandoh Dam in the Central Himalaya, a reddish brown material was observed seeping through drainage holes in three of the galleries. Initially considered to be phyllitic oxide, this was chemically analysed and found to be sulphate radicals. A sulphate concentration of 861.50 ppm was recorded in the seepage water. Petrography of the bedrocks and X-ray analysis of the suspended reddish brown powder as well as chemical analysis of the seepage water revealed the presence of chalcopyrite, pyrrhotite and the conversion of monosulphate phases into ettringite phases as the major cause of expansion and seepage. This process is accompanied by a significant volume increase which it was concluded was responsible for the internal stresses causing the cracking through which the seepage water entered the drainage and grouting galleries.