Abstract
Geological mapping has confirmed the presence of swelling clays in the area of the proposed water transport canal between Köklüce and Erbaa, Turkey. A swelling pressure distribution map was prepared for this part of the route, based mainly on the analyses of soils in the Erbaa and Niksar basins. It is concluded that the potential swelling pressures will exceed the overburden weight of the reinforced concrete canal, not only when empty but also when full. In addition, variations in the characteristics of the soil mean differential movement is likely along the alignment, particularly important as the canal is planned to be a rigid structure. Recommendations are made to minimise the effect.
Résumé
La cartographie géologique a confirmé la présence d’argiles gonflantes dans la région du canal de transfert d’eau entre Köklüce et Erbaa en Turquie. Une carte représentant les pressions de gonflement a été préparée pour cette section du canal, principalement basée sur des analyses de sols des bassins d’Erbaa et Niksar. Il est apparu que les pressions de gonflement potentielles dépasseront le poids des terrains au niveau des revêtements en béton armé, non seulement pour le canal vide mais aussi pour le canal plein. De plus, la variabilité des propriétés des sols le long du tracé se traduira par des mouvements différentiels, avec des conséquences importantes sur le comportement de la structure conçue pour être rigide. Des recommandations sont faites pour minimiser ces effets.
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Yilmaz, I. The effect of swelling clays on a water transport canal between Köklüce HPP and Erbaa HPP (Turkey). Bull Eng Geol Environ 66, 467–472 (2007). https://doi.org/10.1007/s10064-007-0086-1
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DOI: https://doi.org/10.1007/s10064-007-0086-1