The fact that flash floods initiated in arable catchments are often accompanied by massive sediment and nutrient loads often leads to the assumption that surface runoff is the principle pathway by which runoff reaches watercourses. On the basis of an evaluation of several rainfall-runoff events in a representative agricultural catchment, we show that runoff from cultivated land may be generated in a way similar to that seen on forested slopes, where shallow subsurface runoff is the predominant pathway by which runoff makes its way to watercourses in most runoff events. To identify the predominant runoff pathway, we employed a combination of turbidity measurements and stream discharge data. Suspended sediment flux, a newly introduced index representing the ratio between precipitation duration and total sediment yield, and direction of the discharge-turbidity hysteresis loops were proposed as reflective indicators of the frequency of runoff via different pathways. In our study, most of the events initiated by rainstorms of various intensities and durations resulted in rapid increases in stream discharge. Although we observed temporal variability of topsoil properties attributable to seasonal weather changes and agricultural activities, e.g. bulk density and porosity, runoff generation was mainly driven by precipitation characteristics and the initial catchment saturation.
In recent years the issue of the natural hydrological and meteorological time series fluctuation has been discussed more and more intensively. As the series of measured hydrological and climatological data become longer and easier worldwide accessible it is possible to deal with a large amount of historical data in their complexity. Handling these data we cannot go without new methods of mathematical statistics and mathematical analysis. In the study some methods of the long-term trends identification in the hydrological time series are presented. Apart from the classical methods, like that of moving averages, the paper focuses in detail on the Hodrick-Prescott (HP) filter. The HP filter is applicable to the trend analysis of the long-term hydrological time series. Next, a new method of the period length identification, the combined periodogramm method, is theoretically developed. Using this method the long cycles length identification becomes more precise. Here, the cycle is considered to be long when it takes the length of about 1/6 to 1/3 of the measured time series. Identification of such long cycles is important with respect to the future hydrospherical processes forecast. Results of application of these methods to the Slovak hydrological time series are presented in the second part of the study. and V posledných rokoch sa začína čoraz viac diskutovať na tému prirodzených fluktuácií hydrologických a meteorologických radov. So stále sa predlžujúcimi radmi meraných hydrologických a klimatických údajov a zlepšujúcim sa prístupom k meraným údajom na celom svete možno komplexnejšie spracovať veľký počet historicky nameraných časových radov. Pri spracovávaní týchto údajov sa nezaobídeme bez rozvoja nových metód štatistiky a matematickej analýzy. V predloženej štúdii boli opísané metódy identifikácie dlhodobého trendu hydrologických radov. Popri už klasických metódach (metóde kĺzavých priemerov) bol v tejto práci rozpracovaný Hodrickov-Prescottov (HP) filter. HP filter možno aplikovať na analýzu trendu dlhodobých ročných hydrologických časových radov. Ďalej bola v štúdii teoreticky rozpracovaná nová metóda identifikácie dĺžky periód časových radov - metóda kombinovaného periodogramu. Uvedená metóda spresňuje identifikáciu dĺžky dlhých cyklov, teda cyklov s dĺžkou okolo 1/6 až 1/3 meraného časového radu. Práve identifikácia týchto dlhých cyklov je veľmi dôležitá pri odhade budúceho vývoja hydrosféry. Praktické použitie uvedených metód na slovenských hydrologických radoch je prezentované v druhej časti štúdie.
In the second part of the paper long-term trends and cyclicity in hydrological time series are identified using both the Hodrick-Presoctt (HP) filter and the combined periodogram. The HP filter seems to be a good tool for analyzing annual time series. It clearly identifies the decrease in the Slovak rainfall time series 1900-1990 and the increase in those of 1990-2000. Using the combined periodogram method oscillation cycles in the discharge time series of main Slovak rivers were identified. These cycles are likely to be characteristic for all Slovak rivers in general. This means the discharge time series are not stationary, they involve a cyclical component. To calculate hydrological characteristics it is necessary to have such a sufficiently long time series that involves both complete wet and dry periods. Because of existence of an about 29 year cycle, a period consisting of 30 years is very suitable. From the long-term point of view, both Danube and Morava Rivers possess steady trends while in the Bodrog and Vah rivers a decrease in discharge occurred during the XX Century. This decrease was mainly due to lower annual rainfalls in Slovakia. When determine long-term discharges, an oscillation of wet and dry periods should be taken into account. The trends should be determined for closed cycles, i.e., either from minimum to minimum or from maximum to maximum. From the long-term trends analysis it follows that the linear trend is not adequate to extrapolate the hydrological time series to the future. and V druhej časti štúdie je identifikovaný dlhodobý trend a cyklickosť slovenských hydrologických časových radov použitím Hodrickovho-Prescottovho (HP) filtra a metódou kombinovaného periodogramu. HP filter sa ukázal byť dobrým nástrojom na analýzu časových radov ročných údajov. Zreteľne identifikuje pokles zrážkových úhrnov na územie SR v období 1900-1990 a nárast úhrnov v rokoch 1990-2000. Metódou kombinovaného periodogramu boli identifikované cykly kolísania prietokových radov najvýznamnejších slovenských tokov. Je pravdepodobné, že tieto cykly sú charakteristické pre všetky slovenské toky. Prietokové rady zahŕňajú v sebe cyklickú zložku. Pri výpočtoch hydrologických charakteristík je potrebné hydrologické charakteristiky počítať z dostatočne dlhých radov zachytávajúcich celý cyklus - mokré i suché obdobie. Tridsaťročné obdobie na výpočet hydrologických charakteristík tokov je vzhľadom na existenciu ca 29-ročného cyklu veľmi vhodné. Z dlhodobého hľadiska Dunaj a Morava majú vyrovnaný trend vodnosti, v Bodrogu a vo Váhu došlo v 20. storočí k poklesu odtoku. Na tomto poklese majú najväčší podiel nižšie ročné zrážkové úhrny na územie SR. Pri určovaní dlhodobých trendov prietokov je potrebné brať do úvahy cykly striedania sa suchých a mokrých období. Vývojové trendy je potrebné určovať za obdobia uzavretých cyklov - od minima po minimum, alebo od maxima po maximum. Z analýzy dlhodobých trendov vyplýva, že použitie lineárneho trendu nie je vhodné na extrapoláciu hydrologických radov do budúcnosti.
The paper presents relationship between the Standardised Precipitation Index (SPI) and physiological responses of individual trees in a beech stand using an example of an experimental plot in Bienska valley (Zvolen, Slovakia). SPI is a widely used tool for monitoring both short-term and long-term droughts, and for the assessments of drought impacts on agriculture. Due to the complex ecosystem bonds, monitoring of drought in forests often requires a sophisticated technological approach. The aim of the paper was to correlate the SPI on the physiological responses of trees that were recorded during the performed physiological research (sap flow, and stem circumference increment) at the site in the growing seasons (May to September) of the years 2012-2014. The results revealed a relationship between the index and the physiological responses, although the problem with the impact of other environmental factors has also come up. The secondary correlation, in which soil water potential that significantly affects physiological responses of forest tree species was used as a dependent variable, showed a tighter relationship with the SPI. We found the highest correlation between the soil water potential and the values of SPI aggregated for five weeks. This indicates that the beech forest has a five week resistance to drought stress. The results also enable simple monitoring of the initiation of the drought stress by applying SPI for five weeks.
In the realm of the philosophy of sounds and auditory experience there is an ongoing discussion concerned with the nature of sounds. One of the contestant views within this ontology of sound is that of the Property View, which holds that sounds are properties of the sounding objects. A way of developing this view is through the idea of dispositionalism, namely, by sustaining the theory according to which sounds are dispositional properties (Pasnau 1999; Kulvicki 2008; Roberts 2017). That portrayal, however, is not sufficient, as it has not inquired the metaphysical debates about dispositions beyond the conditional analysis. In this paper, I try to advance this view by including recent developments (for instance Bird 2007; Vetter 2015) in the field of dispositionalism and I analyse whether this new version can sort out known and new objections to Property View.
Konference se konala 10. června 2015 v budově Právnické fakulty Masarykovy univerzity v Brně and Na obálce nad názvem: Masarykova univerzita, Právnická fakulta, Právní dějiny a římské právo, katedra dějin státu a práva