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Environmental Pollution | 2003

Environmentally acceptable effect of hydrogen peroxide on cave "lamp-flora", calcite speleothems and limestones.

Jiří Faimon; Jindřich Štelcl; Svatava Kubešová; Jiří Zimák

Mosses, algae, and cyanobacteria (lamp-flora) colonize illuminated areas in show caves. This biota is commonly removed by a sodium hypochlorite solution. Because chlorine and other deleterious compounds are released into a cave environment during lamp-flora cleansing, hydrogen peroxide was tested as an alternative agent. In a multidisciplinary study conducted in the Kateinská Cave (Moravian Karst, Czech Republic), 12 algae- and cyanobacteria taxons and 19 moss taxons were detected. The threshold hydrogen peroxide concentration for the destruction of this lamp-flora was found to be 15 vol.%. Based on laboratory experiments in stirred batch reactors, the dissolution rates of limestones and calcite speleothems in water were determined as 3.77 x 10-3 and 1.81 x 10-3 mol m-2 h-1, respectively. In the 15% peroxide solution, the limestone and speleothem dissolution rates were one order of magnitude higher, 2.00 x 10-2 and 2.21 x 10-2 mol m-2 h-1, respectively. So, the peroxide solution was recognised to attack carbonates somewhat more aggressively than karst water. In order to prevent the potential corrosion of limestone and speleothems, the reaching of preliminary peroxide saturation with respect to calcite is recommended, for example, by adding of few limestone fragments into the solution at least 10 h prior to its application.


Science of The Total Environment | 2006

Anthropogenic CO2-flux into cave atmosphere and its environmental impact: A case study in the Císařská Cave (Moravian Karst, Czech Republic)

Jiří Faimon; Jindřich Štelcl; Daniel Sas


Geologické výzkumy na Moravě a ve Slezsku | 2016

Sedimentárně petrografická charakteristika půdních profilů na vybraných lokalitách Moravského krasu

Monika Schwarzová; Ivana Zatloukalová; Jindřich Štelcl; Jiří Faimon


Archive | 2008

Průvodce po geologických zajímavostech kraje Vysočina

Václav Vávra; Jindřich Štelcl; Karel Malý


Acta Musei Moraviae, Sci. geol. | 1998

The correlation between radioactivity and mineral assemblages:an example from alkali feldspar syenites; Gfohl unit,Moldanubian zone

Jaromír Leichmann; Jindřich Štelcl; Kateřina Zachovalová


Journal of the Czech. Geol. Soc. | 1997

A Highly Radioactive Syenite from the Moldanubian Zone (WesternMoravia).

Jaromír Leichmann; Jindřich Štelcl; Kateřina Zachovalová


Catena | 2018

Reflectance colourimetry as a method for estimating the approximate quantity of non-carbonate components in limestones: A case study in the Mokrá Quarry (Czech Republic)

Jiří Zimák; Jindřich Štelcl; Dalibor Všianský


Zprávy o geologických výzkumech | 2016

Využitelnost terénních rentgenfluorescenčních analyzátorů kestanovení chemismu cementářských surovin na příkladu velkolomuMokrá

Jiří Zimák; Kristýna Dalajková; Roman Donocik; Petr Krist; Daniel Reif; Jindřich Štelcl; Lenka Kopecká


Archive | 2016

Ověření využitelnosti kolorimetrie pro orientační stanoveníchemismu cementářských surovin ve velkolomu Mokrá

Jindřich Štelcl; Jiří Zimák


Archive | 2016

Den biologie 2016

Martina Jančová; Libuše Vodová; Blažena Brabcová; Václav Vávra; Jindřich Štelcl; Iva Frýzová; Kateřina Ševčíková

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