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352. Eco-hydrological impacts of Eucalyptus in the semi humid Ethiopian Highlands: the Lake Tana Plain
- Creator:
- Chanie, Tilashwork, Collick, Amy S., Adgo, Enyew, Johannes Lehmann, C., and Steenhuis, Tammo S.
- Format:
- bez média and svazek
- Type:
- model:article and TEXT
- Subject:
- Eucalyptus, soil water repellency, Croton machrostachyus, and Koga watershed
- Language:
- Slovak
- Description:
- Eucalyptus is the tree of choice for wood production by farmers in Ethiopia. Although there are many claims about its harmful effect on ecology and water availability, little actual research exists. The main objective of this study was, therefore, to study the extent of harm of Eucalyptus on the ecosystem. This study was conducted at the Koga Watershed near Lake Tana in Ethiopia. Twenty-five farmers were interviewed and a field experiment with three replications was carried out to quantify the effect of Eucalyptus on various soil physical and chemical properties and maize crop measurements and to compare bulk density, soil moisture contents, maize crop counts and shading effects in fields bordered by Eucalyptus and Croton macrostachyus. Our results show that Eucalyptus decreased both soil nutrients and maize yields within 20 m of the trees. Although moisture content was not affected during the monsoon, it decreased faster within 30 m of the Eucalyptus trees than elsewhere. Soils become water repellent, too. Local farmers’ perception agreed with our experimental findings and indicated that Eucalyptus trees are exhausting the once productive land. They also reported that Eucalyptus dries up springs. Despite this, the growers insist on planting Eucalyptus because of its cash income.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
353. Editorial and preface to thematic issue on biohydrology
- Creator:
- Lichner, Ľubomír
- Format:
- bez média and svazek
- Type:
- model:article and TEXT
- Language:
- Slovak
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
354. Efektívnosť ílových minerálov pri znižovaní vooodpudivosti počas dlhého suchého a teplého obdobia
- Creator:
- Lichner, Ľubomír and Dlapa, Pavel
- Format:
- bez média and svazek
- Type:
- model:article and TEXT
- Subject:
- water repellency, sand, stearic acid, clay minerals, vodoodpudivosť, piesok, kyselina stearová, and ílové minerály
- Language:
- Slovak
- Description:
- The aim of this study was to evaluate an efficiency of clay minerals (kaolinite, illite, Na- and Ca-montmorillonite) in alleviating the water repellency of stearic acid sand during the course of long-term hot and dry spell. This spell was simulated by prolonged drying (incubation) of the samples in oven at 50°C. It was found that the kaolinite addition resulted in a drop in the persistence of water repellency of the stearic acid sand. On the contrary, the Ca-montmorillonite addition increased markedly the persistence of water repellency of the stearic acid sand. In most cases, the illite addition resulted in an increase in the persistence of water repellency, even though not so markedly as it was in the case of Ca-montmorillonite addition. In the case of Na-montmorillonite addition, the striking drop in the persistence of water repellency of the stearic acid sand was registered only after lowering the moisture below 5 %. An increase in the persistence of water repellency of the sand-clay mixture with an increase in the clay amount is another interesting finding, observed in case of kaolinite and Ca-montmorillonite. and Cieľom tejto štúdie bolo zhodnotenie efektívnosti ílových minerálov (kaolinitu, illitu, Na- a Camontmorillonitu) pri znižovaní stálosti vodoodpudivosti piesku pokrytého kyselinou stearovou počas dlhého suchého a teplého obdobia, simulovaného inkubáciou vzoriek pri teplote 50 °C. Zistili sme, že pridanie kaolinitu výrazne znížilo stálosť vodoodpudivosti piesku pokrytého kyselinou stearovou prakticky počas celého cyklu sušenia. Pridanie Ca-montmorillonitu naopak stálosť vodoodpudivosti piesku pokrytého kyselinou stearovou výrazne zvýšilo. Pridanie illitu vo väčšine prípadov zvýšilo stálosť vodoodpudivosti piesku pokrytého kyselinou stearovou, aj keď nie tak výrazne ako pridanie Ca-montmorillonitu. V prípade pridania Na-montmorillonitu sme výrazné zníženie vodoodpudivosti piesku pokrytého kyselinou stearovou zaznamenali až po poklese vlhkosti vzorky pod 5 %. Ďalším zaujímavým poznatkom je vzrast vodoodpudivosti so zvyšujúcim se obsahom ílu, ktorý sme zaregistrovali v prípade kaolinitu a Ca-montmorillonitu.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
355. Effect of drying on the sorption and desorption of copper in bottom sediments from water reservoirs and geochemical partitioning of heavy metals and arsenic
- Creator:
- Hiller, Edgar and Šutriepka, Michal
- Format:
- bez média and svazek
- Type:
- model:article and TEXT
- Subject:
- heavy metals, sorption, desorption, mobility, sequential extraction, dredged sediments, ťažké kovy, sorpcia, desorpcia, mobilita, sekvenčná extrakcia, and vyťažené sedimenty
- Language:
- Slovak
- Description:
- Bottom sediments can be significant sinks for a variety of heavy metals and metalloids coming from various anthropogenic sources. When these sediments are dredged and disposed of to land, drying and oxidation can lead to several changes in their physico-chemical properties, such as redox potential and pH, and hence to changes in metal mobility. Therefore, this work was conducted to study the adsorptiondesorption behaviour of one selected heavy metal - copper - in three bottom sediment samples before and after drying. Moreover, possible geochemical associations of As, Cd, Co, Cu, Hg, Ni, Pb and Zn in the airdried sediments were studied using a modified BCR sequential extraction protocol. Generally, redox state of the sediments changed from the highly anoxic to oxic and adsorption of Cu2+ decreased when the originally anoxic sediments were dried. On the other hand, the enhanced release of Cu2+ was observed from the air-dried sediments. The adsorption-desorption data showed that the changes in metal leachability occurred between originally anoxic and air dried sediments. In terms of water and soil pollution by Cu and likely other heavy metals, it appears that the dredged, air-dried sediments could represent somewhat greater contamination risks when compared with the originally anoxic sediments. Using the sequential extraction data, leaching potential of heavy metals and arsenic in the air-dried sediments was possible to evaluate with Cd, Co, Zn as the most mobile heavy metals, followed by Cu, Ni, As, Pb and Hg, respectively. and Dnové sedimenty sú významnými adsorbentmi celej rady ťažkých kovov a polokovov, ktoré pochádzajú z rôznych antropogénnych zdrojov. Po vyťažení týchto sedimentov z vodných nádrží na zemský povrch prechádzajú procesmi sušenia a oxidácie, ktoré menia niektoré ich vlastnosti, ako oxidačno-redukčný potenciál a pH, a teda môžu ovplyvňovať pohyblivosť potenciálne toxických kovov prítomných v sedimentoch. Z tohto dôvodu cieľom práce bolo štúdium adsorpcie a desorpcie jedného vybraného ťažkého kovu - medi - v troch vzorkách dnových sedimentov pred vysušením a po ňom. Okrem toho sme pomocou modifikovanej BCR metódy sekvenčnej extrakcie študovali možné geochemické interakcie ťažkých kovov (Cd, Co, Cu, Hg, Ni, Pb, Zn) a arzénu s jednotlivými zložkami dnových sedimentov. Ako ukázali experimentálne výsledky, počas sušenia sa zmenili redukčné podmienky v sedimentoch na oxidačné a adsorpčná kapacita vysušených sedimentov vzhľadom k Cu2+ bola výrazne nižšia ako u pôvodných sedimentov. Na druhej strane, množstvo uvoľneného Cu2+ z vysušených sedimentov bolo vyššie ako z pôvodných sedimentov. Uvedené zistenia teda poukazujú na zmenu v správaní a pohyblivosti potenciálne toxických prvkov medzi pôvodnými, redukčnými sedimentmi a tými, ktoré prešli procesom sušenia a oxidácie. Z hľadiska znečistenia prírodných vôd a pôd meďou a pravdepodobne aj ďalšími ťažkými kovmi sa zdá, že v porovnaní s pôvodnými kontaminovanými sedimentmi vyťažené a na vzduchu vysušené sedimenty môžu predstavovať vyššie riziko pre životné prostredie. Podľa výsledkov sekvenčnej extrakcie sa ukázalo, že Cd, Co a Zn sú po vysušení v skúmaných sedimentoch veľmi mobilnými prvkami, pričom pohyblivosť ostatných prvkov klesá v poradí Cu > Ni > As > Pb >> Hg.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
356. Effect of gravel content on soil water retention characteristics and thermal capacity of sandy and silty soils
- Creator:
- Beck-Broichsitter, Steffen, Haider Rizvi, Zarghaam, Horn, Rainer, and Wuttke, Frank
- Format:
- počítač and online zdroj
- Type:
- model:article and TEXT
- Subject:
- pore size distribution, soil water retention curve, thermal capacity, and PDI model
- Language:
- Slovak
- Description:
- The presence of gravel in soils modifies the porosity, pore connectivity and pore size distribution in the soil matrix as well as the soil matrix-gravel interfaces. The aim of the present study is to investigate the effect of relative volume of gravel in samples with gravel mass fractions of 5,10, 20 wt% and varying bulk densities (1.3, 1.45, 1.55, 1.60, 1.65 g cm–3) on (i) total porosity, field capacity, plant available water holding capacity, (ii) pore size distribution and (iii) thermal capacity of repacked sandy and silty soils. The focus of the study was to determine if laboratory measured soil water retention curves considering (i), (ii), and (iii) can be predicted by a gravel-based weighting factor, Rv, considering comprehensive significance tests. The sand-gravel mixtures show a decrease in the volume fractions of macropores and wide cores pores with an increase in the gravel contents, while the silt-gravel mixtures show an opposite trend. The root mean square errors (RMSE) between measured and fitted volumetric water contents, θ, between 0.006 and 0.0352 and between 0.002 and 0.004 for Rv-weighted volumetric water contents indicate that the van Genuchten-based Peters-Durner- Iden (PDI) model is appropriate for fitting. The soil water retention curves with mass gravel contents of up to 10 wt% for silt and 20 wt% for sand can be well predicted by weighting factors (relative volume of rock fragments) in the range between 0.045 and 0.058 for silt, and between 0.112 and 0.119 for sand. The results also indicate a decrease in the Rv-weighted saturated, cvsat, and dry, cvdry, thermal capacity with an increase in the gravel contents for both soils. Further investigations are needed to examine if and whether measured sand- and silt-gravel mixtures with mass gravel contents below 10 % or rather 20 % can be predicted with a weighting factor.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
357. Effect of mature spruce forest on canopy interception in subalpine conditions during three growing seasons
- Creator:
- Jančo, Martin, Mezei, Pavel, Kvas, Andrej, Danko, Michal, Sleziak, Patrik, Minďáš, Jozef, and Škvarenina, Jaroslav
- Format:
- počítač and online zdroj
- Type:
- model:article and TEXT
- Subject:
- precipitation, interception, synoptic types, Norway spruce (Picea abies L. Karst.), and growing season
- Language:
- Slovak
- Description:
- The interception process in subalpine Norway spruce stands plays an important role in the distribution of throughfall. The natural mountain spruce forest where our measurements of throughfall and gross precipitation were carried out, is located on the tree line at an elevation of 1,420 m a.s.l. in the Western Tatra Mountains (Slovakia, Central Europe). This paper presents an evaluation of the interception process in a natural mature spruce stand during the growing season from May to October in 2018–2020. We also analyzed the daily precipitation events within each growing season and assigned to them individual synoptic types. The amount and distribution of precipitation during the growing season plays an important role in the precipitation-interception process, which confirming the evaluation of individual synoptic situations. During the monitored growing seasons, precipitation was normal (2018), sub-normal (2019) and above-normal (2020) in comparison with long-term precipitation (1988–2017). We recorded the highest precipitation in the normal and above-normal precipitation years during the north-eastern cyclonic synoptic situation (NEc). During these two periods, interception showed the lowest values in the dripping zone at the crown periphery, while in the precipitation sub-normal period (2019), the lowest interception was reached by the canopy gap. In the central crown zone near the stem, interception reached the highest value in each growing season. In the evaluated vegetation periods, interception reached values in the range of 19.6–24.1% of gross precipitation total in the canopy gap, 8.3–22.2% in the dripping zone at the crown periphery and 45.7–51.6% in the central crown zone near the stem. These regimes are expected to change in the Western Tatra Mts., as they have been affected by windstorms and insect outbreaks in recent decades. Under disturbance regimes, changes in interception as well as vegetation, at least for some period of time, are unavoidable.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
358. Effect of microplastics on silty loam soil properties and radish growth
- Creator:
- Botyanszká, Lenka, Šurda, Peter, Vitková, Justína, Lichner, Ľubomír, and Igaz, Dušan
- Format:
- počítač and online zdroj
- Type:
- model:article and TEXT
- Subject:
- microplastics, silty loam soil, radish, and soil properties
- Language:
- Slovak
- Description:
- Microplastics (particles of plastics <5 mm) affect the physical, biological and hydrological properties of agricultural soil, as well as crop growth. We investigated the effect of the addition of three microplastics (high-density polyethylene (HDPE), polyvinyl chloride (PVC), and polystyrene (PS)) at a concentration of 5% (w/w) to a silty loam soil on selected soil properties and growth of radish (Raphanus sativus L. var. sativus). Changes in the soil properties and radish growth in three microplastic treatments were compared with the control. Soil properties (bulk density, hydraulic conductivity, sorptivity, water repellency) were estimated for each treatment at the beginning and at the end of the radish growing period (GP). The bulk density was significantly lower in the HDPE and PVC treatments compared to the control within the measurement at the beginning of the GP and in all microplastic treatments compared to the control at the end of the GP. The values of hydraulic conductivity and water sorptivity did not show significant differences between any treatments within the measurement at the beginning of GP, but they were significantly higher in the HDPE treatment compared to the control at the end of the GP. The growth of radish was characterized by the plant biomass and effective quantum yield of Photosystem II (Y (II)). We did not find a statistically significant difference in the total biomass of radish between any of the experimental treatments, maybe due to used concentration of microplastics. The mean value of Y (II) was significantly higher in all microplastic treatments compared to control only within the last measurement at the end of the GP. A statistically significant change of Y(II) in all microplastic treatments may indicate functional shift in soil properties; however, the measured values of the soil characteristics have not shown the significant changes (except for the bulk density values in all microplastic treatments and hydraulic conductivity together with sorptivity in HDPE treatment within the measurement at the end of GP).
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
359. Effect of river training on flood retention of the Bavarian Danube
- Creator:
- Skublics, Daniel, Blöschl, Günter, and Rutschmann, Peter
- Format:
- bez média and svazek
- Type:
- model:article and TEXT
- Subject:
- flood retention, flood plain, inundation areas, flood management, and hydrodynamic modelling
- Language:
- Slovak
- Description:
- The Bavarian Danube River has experienced numerous large flood events in recent years which make flood management an urgent matter. The propagation of flood waves along the river is heavily influenced by controlled and natural flood retention. Over the past centuries, natural flood retention areas were lost due to river training, and the hydraulic characteristics of the channel-flood plain system were modified. The purpose of this paper is to understand the effect of river training on the flood retention characteristics along the Bavarian Danube. Systematic two-dimensional hydrodynamic modelling shows that extreme floods are attenuated more strongly in the present state of the channel-flood plain system than they were historically. This is because the retention areas are filled later during the event, so the attenuation effect is much larger for the same magnitude of the retention volume. Natural flood retention is therefore not an effective management option for reducing extreme floods on the Bavarian Danube. Controlled flood retention measures provide a higher efficiency regarding peak attenuation to retention volume ratio. On the other hand, the delay of flood peaks due to natural retention may be beneficial for the superposition of the flood waves with contributions from downstream tributaries.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public
360. Effect of slope position on soil properties and soil moisture regime of Stagnosol in the vineyard
- Creator:
- Magdić, Ivan, Safner, Toni, Rubinić, Vedran, Rutić, Filip, Husnjak, Stjepan, and Filipović, Vilim
- Format:
- počítač and online zdroj
- Type:
- model:article and TEXT
- Subject:
- hillslope, agriculture, Stagnosol, soil properties, soil water content, and Bg horizon
- Language:
- Slovak
- Description:
- Hillslope hydrology in agricultural landscapes is complex due to a variety of hydropedological processes and field management possibilities. The aim was to test if there are any differences in soil properties and water regime along the hillslope and to compare vineyard rows (vine) with inter-rows (grass) area for those properties. The study determined that there are significant differences in the contents of soil particle fractions, pH, and humus content along the slope (P < 0.0001), with lower confidence level in bulk density (P < 0.05). Differences between row and inter-row space were significant for the pH, humus, and silt content, but for sand and clay content, and bulk density differences were not determined. The study determined differences in soil water content among five slope positions (P < 0.0001), and between row and inter-row vineyard space (all with P < 0.05). Where in the upper slope positions (e. g., P1) soil water content was higher than on lower slope positions. Higher soil water content was observed at higher slope positions, associated with clay content. However, it can be concluded that the retention of moisture on the slope is more influenced by local-scale soil properties (primarily soil texture) and variability of the crop (row/inter-row) than the position on the slope.
- Rights:
- http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public