Hidrogeological features of carbonate karst

Authors

  • Валерій Васильович Сухов V. N. Karazin Kharkiv National University Svobody Sq. 4, Kharkiv, Ukraine, 61022, Ukraine
  • Василий Григорьевич Суярко V. N. Karazin Kharkiv National University Svobody Sq. 4, Kharkiv, Ukraine, 61022,, Ukraine https://orcid.org/0000-0003-2841-0071
  • Ольга Олексіївна Сердюкова Poltava national technical Yurі Kondratiyk university Pershotravnevyi avenue, 24, Poltava, Ukraine, 36011, Ukraine

DOI:

https://doi.org/10.15587/2313-8416.2015.46954

Keywords:

ground water, carbonate rocks, karstification, leaching, dissolution, carbon dioxide, epikarst, hypokarst, chemical denudation, occlusion.

Abstract

On the example of loamy-chalky Upper Cretaceous strata (K2cm) of Sviatogirsk brachyanticline it has been found out that carbonate karst forms with the participation of different on dynamics and chemical composition kinds of groundwater.

Basic chemical reactions that lead to leaching and dissolution of carbonate rocks during their interaction with groundwater have been characterized. Geological, hydrogeological and geochemical conditions of formation of various morphogenetic types of karst - surface (epikarst) and deep (hypokarst) have been well-grounded.

Author Biographies

Валерій Васильович Сухов, V. N. Karazin Kharkiv National University Svobody Sq. 4, Kharkiv, Ukraine, 61022

Department of hydrogeology,

Senior Lector

Василий Григорьевич Суярко, V. N. Karazin Kharkiv National University Svobody Sq. 4, Kharkiv, Ukraine, 61022,

Department of hydrogeology,

Senior Lector

Ольга Олексіївна Сердюкова, Poltava national technical Yurі Kondratiyk university Pershotravnevyi avenue, 24, Poltava, Ukraine, 36011

Department of oil and gas exploitation and geotechnics,

Нead of laboratory

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Published

2015-07-27

Issue

Section

Geological and geographical sciences