Volume 51, Number 5, 775-779, DOI: 10.1007/s00254-006-0394-y

Leakage below dam sites in limestone terrains by enhanced karstification: a modeling approach

Douchko Romanov, Franci Gabrovsek and Wolfgang Dreybrodt

From the issue entitled "Special Issue: Cvijic Karst 2005: “Water Resources and Environmental Problems in Karst” (pp 673-796)"

View Related Documents

Abstract

Unnaturally high hydraulic gradients below dam sites enhance dissolutional widening of fractures in limestone. A model is presented which suggests that under unfavorable conditions, leakage rates could become unbearably high during the lifetime of the dam. At the beginning when water is impounded, leakage rates are low and increase slowly. A positive feedback loop, however, causes a sudden dramatic increase of leakage within a few years. Deep grouting becomes necessary to prevent such failures. Inefficiencies in grouting may leave some open fractures in the grouting curtain. These fractures widen faster than pathways below the grouting curtain, and reduce the effect of the grouted region located below. Therefore, open fractures act in a similar way as reduction of the grouting depth.

Keywords  Dissolution of limestone - Karstification - Dam site

Fulltext Preview

Image of the first page of the fulltext document