In the presented research I tried to find answers to the following questions: what the characteristics of the relation between recharge and discharge of the karst aquifer in the background of the ...Vipava springs are and which conclusions about the functioning of the karst system can be made based on stated relations between its input and output signal. Several different models of the system recharge-discharge were set. For each the conversion of the input signal to the system response was defined by transfer functions, which express conditions and processes in the karst system in mathematical form. Based on the comparison of the suitability of these different models an important influence of vegetation and processes in atmosphere and soil on the quantity of water that actually enters the karst aquifer and is expressed as recharge function was proved. An increase in the accuracy of the simulation was obtained also by the temporal distribution of recharge in fast and slow component, which is in agreement with the double mechanism of the functioning of the system: fast flow through the karst drainage net and longer retardation in the system with storage of water in less permeable zones.
Fotografija ja bila posneta v zimskem času. Prikazuje izvir Vipave “Pod skalo”, most, na hribu stavbi malega semenišča, v ozadju pa razvaline starega gradu. Razglednica je bila poslana v Trst leta ...1912.
Litografija je sestavljena iz treh manjših sličic: na levi strani mesto Vipava risano s severovzhodne strani, na desni strani Podskala, levo spodaj pa grad in hotel Adria. Razglednica je bila poslana ...2. maja 1899.
Litografija na razglednici je sestavljena iz treh manjših sličic: na levi strani zgoraj je mesto Vipava risano s severovzhodne strani, na desni strani je gostilna pri “Hribu”, levo spodaj pa najbrž ...gostilniška terasa. Poslana je bila leta 1913.
