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Projects / Programmes
Prenos snovi v kraških tleh in v kraško-razpoklinskih kamninah (Slovene)
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
(metodology)
Citations
Citations for bibliographic records in COBIB.SI that are linked to records in citation databases
Organisations (2) , Researchers (6)
0210 Institute for Mining, Geotechnology and the Environment
| no. | Code | Name and surname | Research area | Role | Period | No. of publicationsNo. of publications |
|---|---|---|---|---|---|---|
| 1. | 15249 | Geology | Researcher | 1998 - 2001 | 519 | |
| 2. | 05511 | Geology | Researcher | 2000 - 2001 | 114 | |
| 3. | 02214 | Geology | Head | 1999 - 2001 | 441 | |
| 4. | 15886 | Mining and geotechnology | Researcher | 1998 - 2001 | 492 |
0215 Geological Survey of Slovenia
| no. | Code | Name and surname | Research area | Role | Period | No. of publicationsNo. of publications |
|---|---|---|---|---|---|---|
| 1. | 03611 | Geology | Researcher | 2000 - 2001 | 58 | |
| 2. | 13034 | Control and care of the environment | Researcher | 1998 - 2001 | 231 |
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.