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Projects / Programmes source: ARIS

Prenos snovi v kraških tleh in v kraško-razpoklinskih kamninah (Slovene)

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Research activity

Code Science Field Subfield
1.06.04  Natural sciences and mathematics  Geology  Geochemistry 

Code Science Field
P470  Natural sciences and mathematics  Hydrogeology, geographical and geological engineering 
P305  Natural sciences and mathematics  Environmental chemistry 
Keywords
karst, pollutant transport, vadose zone, natural isotopes, soil water balance, agricultural pollution
Evaluation (rules)
source: COBISS
Evaluation of bibliographic research performance indicators according to ARIS methodology
Citations Citations for bibliographic records in COBIB.SI that are linked to records in citation databases
source: WoS source: Scopus source: COBISS
Researchers (6)
no. Code Name and surname Research area Role Period No. of publications
1.  03611  Miran Bizjak  Geology  Researcher  2000 - 2001  58 
2.  15249  PhD Barbara Čenčur Curk  Geology  Researcher  1998 - 2001  512 
3.  13034  PhD Branka Trček  Control and care of the environment  Researcher  1998 - 2001  225 
4.  05511  PhD Marija Ulrich-Supovec  Geology  Researcher  2000 - 2001  114 
5.  02214  PhD Miran Veselič  Geology  Head  1999 - 2001  440 
6.  15886  PhD Goran Vižintin  Mining and geotechnology  Researcher  1998 - 2001  487 
Organisations (2)
no. Code Research organisation City Registration number No. of publications
1.  0210  Institute for Mining, Geotechnology and the Environment  Ljubljana  5051576000  4,554 
2.  0215  Geological Survey of Slovenia  Ljubljana  5051410000  11,243 
Abstract
The influence of karstic ground and the cracking of the rock on mass transport in their partial saturation with water will be studied by experiments. Additional tracing experiments will be performed in the ground and in the unsaturated zone of karstic aquifers on less crushed part of our experimental fiel site which was studied geologically in detail. The experimental field site will be equipped with an agrometeorological station. Natural and artificial tracers will be used (carbon, oxygen and hydrogen isotopes). Water flow will be traced from precipitation to a ground spring, and in the unsaturated and saturated zone of the aquifer.
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