J 2016

Transfer of climatic variables by dripwater: a case study from Kateřinská Cave (Moravian Karst)

FAIMON, Jiří, Radoslava BODLÁKOVÁ, Pavel PRACNÝ and Jiří HEBELKA

Basic information

Original name

Transfer of climatic variables by dripwater: a case study from Kateřinská Cave (Moravian Karst)

Authors

FAIMON, Jiří (203 Czech Republic, belonging to the institution), Radoslava BODLÁKOVÁ (203 Czech Republic), Pavel PRACNÝ (203 Czech Republic, guarantor, belonging to the institution) and Jiří HEBELKA (203 Czech Republic)

Edition

Environmental Geology (Environmental Earth Sciences), Springer, 2016, 1866-6280

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10505 Geology

Country of publisher

United States of America

Confidentiality degree

není předmětem státního či obchodního tajemství

Impact factor

Impact factor: 1.569

RIV identification code

RIV/00216224:14310/16:00090876

Organization unit

Faculty of Science

UT WoS

000381986800001

Keywords in English

Cave dripwater discharge; Rainfall; Specific electrical conductivity; pH; Paleoclimate proxy; Water supersaturation

Tags

International impact, Reviewed
Změněno: 13/3/2018 14:53, Mgr. Pavel Pracný, Ph.D.

Abstract

V originále

Hydrogeochemical properties of drips in Kateřinská Cave (Moravian Karst) were studied with focus on their relation to climatic variables, especially rainfall and temperature. The discharges of two drips (marked as meteorologically sensitive drips) showed statistically significant positive correlations with rainfalls with lag of -5 and -2 days. In addition, the discharges showed statistically significant positive correlations with specific electrical conductivity, pH, and supersaturation with respect to calcite. Other drips in the same cave (marked as meteorologically insensitive drips) did not show this correlation. Because the climatic conditions are identical, the drip types must differ in their reaction/flow paths. It indicates that the paths may control some proxies possibly preserved in speleothems, which should be taken into consideration for paleoenvironmental reconstructions. In case of the speleothems formed by the meteorologically sensitive drips, we believe that it would be possible to distinguish even intra-annual climatic events via individual laminas and their composition.