Summary
Karst processes taking place on the shores of reservoirs and associated phenomena are of great interest when studying the engineering geological situation of the region chosen for dam construction. The processes are important from the viewpoint of filtration leakage control and the forecast of the shore-retrogressing process and land stability by construction of industrial and civil projects.
The problem under consideration is the dynamics of karst massif formation under reservoir conditions. Three stages are singled out. Interaction between the processes of solution and suffosional removal of the filling material of karst cavities is shown. The authors describe the characteristic features of the processes taking place in sulphate and carbonate rocks. To evaluate the time of collapse and volume of shore retreat special formulae are used.
Résumé
Les processus karstiques qui se passent sur les rivages des réservoirs d'eau et les phénomènes qu'ils provoquent out un grand intérêt quand on étudie la construction géologique du territoire où l'on construit un barrage, quand on révèle la fuite d'eau de filtration. Ces processus doivent être pris en considération pour le pronostic de la destruction du rivage et de la stabilité du sol en cas de constructions industrielles et civiles.
Il s'agit dans le rapport du dynamisme de la modification du massif riverain karstifié. On distingue trois stades. On examine la corrélation des processus de solution et de suffosion des cavités karstiques. On caractérise des processus qui ont lieu dans les roches sulphatées et carbonatées. On cite des formules pour calculer le temps de la formation de l'éboulement et le volume de la destruction du rivage.
Similar content being viewed by others
References
BÖGLI A. (1960): Kalklösung und Karrenbildung. Geomorph., Suppl. 2.
FERSMAN A. E. (1973): Geohimija t. III, M., 640.
GAMES I. (1965): Types of accelerated karst corrosion. Prob. Speleol. Res. Proc., Ist Speleol. Conf., Brno.
LAPTEV F. F. (1936): Agressivnoye deystvie vodi na karbonatnye porodi, gypsi, betoni. M-L., 135.
LE GRAND H. E.—STRINGFIELD V. T. (1973): Differential erosion of carbonate rock terrains. South-eastern geology. Durnam, vol. 13, No. 1, 1–17.
OGILVI N. A. (1956): Odna iz vozmoznih prichin svyazi karstovih yavlenyi s tektonicheskimi zonami. Tez. dokl. na soveschanii po izucheniu karsta. B. 7, M., 11–13.
PECHERKIN A. I. (1978): Dinamika i prognoz pereformirovania poberezyi vodohranilisch, slozennih karstujuschimisja porodami. Klimaticheskji faktor reljefoobrazovanja. Tez. dokl. Vsesojuznogo soveschanja. Kazan, 144–145.
PECHERKIN A. I.—PECHERKIN I. A. (1978): Gidrodinamicheskaja zonalnost karstovih vod v uslovijah podpora ruslovimi vodohranilischami. Int. Symp. on Karst Hydrology, Budapest, 70–79.
PECHERKIN I. A. (1969): Geodinamika poberezji kamskih vodohranilisch. Perm, 307.
SMITH J. F.—ALBRITTON C. C. (1941): Solution effects on limestone as function of slope. Bull. Geol. Soc. of America, 63–77.
SOKOLOV D. S. (1955): O vozmoznih prichinah pervichnogo dolomitoobrazovanja. BMOIP, t. XXX (5), Otd. geol.
SWEETING M. M. (1973): Karst Landforms. Columbia University Press, New York.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Pecherkin, I.A., Pecherkin, A.I. Theoretical aspects and engineering geological forecast on the shores of karst reservoirs. Bulletin of the International Association of Engineering Geology 20, 187–189 (1979). https://doi.org/10.1007/BF02591279
Published:
Issue Date:
DOI: https://doi.org/10.1007/BF02591279