@article{MTMT:33634768, title = {Copulas modelling of maize yield losses – drought compound events using the multiple remote sensing indices over the Danube River Basin}, url = {https://m2.mtmt.hu/api/publication/33634768}, author = {Potopová, V. and Trifan, T. and Trnka, M. and De Michele, C. and Semerádová, D. and Fischer, M. and Meitner, J. and Musiolková, M. and Muntean, N. and Clothier, B.}, doi = {10.1016/j.agwat.2023.108217}, journal-iso = {AGR WATER MANAGE}, journal = {AGRICULTURAL WATER MANAGEMENT}, volume = {280}, unique-id = {33634768}, issn = {0378-3774}, year = {2023}, eissn = {1873-2283} } @article{MTMT:34103558, title = {The importance of relief for explaining the diversity of the floodplain and terrace soil cover in the Dnipro River valley: The case of the protected area within the Dnipro-Orylskiy Nature Reserve}, url = {https://m2.mtmt.hu/api/publication/34103558}, author = {Tutova, G. F. and Kunakh, O. M. and Yakovenko, V. M. and Zhukov, O. V.}, doi = {10.15421/012319}, journal-iso = {BIOSYST DIV}, journal = {BIOSYSTEMS DIVERSITY}, volume = {31}, unique-id = {34103558}, issn = {2519-8513}, abstract = {Floodplains are centers of species diversity, so floodplain habitats often contain protected areas. However, conservation strategies pay little attention to soils, on which the functional stability of both individual ecosystems and landscape chains as a whole depends. Soil morphology provides structural and functional information about floodplain ecosystems. The spatial and temporal heterogeneity of soil morphology is a cost-effective ecological indicator that can be easily integrated into rapid assessment protocols for floodplain and riverine ecosystem restoration projects. Therefore, the aim of our work was to consider the morphological features of soils of the Dnipro-Orylskiy Nature Reserve and assess the role of soil diversity as a factor of structural and functional sustainability of ecosystems of the protected area, as well as to identify the significance of geomorphological predictors for differentiation of soil types to create a soil map of the territory. The World Reference Base for Soil Resources reference soil groups were classified using geomorphological predictors. Soil types were able to explain 90% of the variation in elevation occupied by soils. Arenosols occupied a statistically significantly higher position in topography than other soil types. In turn, Eutric Arenosols occupied a higher position (68.91 ± 0.48 m) than Eutric Lamellic Arenosols (63.32 ± 0.54 m). Other soils occupied positions in the topography that were not statistically significantly different in height. Soil types were able to explain 38% of the variation in elevation that the soils occupied. The highest Topography Wetness Index values were found for Fluvisols (12.73 ± 0.23) and Solonetz (13.06 ± 0.28 m). Differences between these soils were not statistically significant. Topography Wetness Index was slightly lower for Cambisols (11.80 ± 0.21) and Eutric Lamellic Arenosols (12.21 ± 0.28), which also did not differ on this measure. The lowest Topography Wetness Index value was found for Gleysols (11.15 ± 0.17) and Eutric Arenosols (10.95 ± 0.24), which did not differ from each other on this index. Eutric Arenosols and Eutric Lamellic Arenosols are formed at great depths of the water table (7.89 ± 0.50 and 2.62 ± 0.46 m, respectively). Gleysol and Solonetz form at close groundwater level to the surface (0.28 ± 0.27 and 0.21 ± 0.46 m, respectively) compared to Fluvisol and Cambisol (0.46 ± 0.38 and 0.41 ± 0.35 m, respectively). Elevation was the most informatively valuable predictor, but Topography Wetness Index and Vertical Distance to Channel Network significantly improved discrimination. Arenosols were very different from other soils which occupy an automorphic position. Cambisols occupied a transitional position. Other soils occupied hydromorphic positions. Fluvisols and Solonetz occupied wetter positions, while Gleysol occupied less wet positions. Fluvisols and Solonetz differed in the groundwater table. Solonetz predominantly occurred at close groundwater levels. The classification matrix confirmed the possibility of using geomorphological predictors to build a model of spatial variation of soils in the study area. The spatial model demonstrates the organization of the soil cover of the reserve. Calculations showed that Cambiosols occupy 20.7% of the area, Eutric Arenosols occupy 16.0%, Eutric Lamellic Arenosols occupy 17.9%, Fluvisols occupy 15.2%, Gleysols occupy 28.7%, and Solonetz occupy 1.5%.}, year = {2023}, eissn = {2520-2529}, pages = {177-190} } @article{MTMT:34183456, title = {Morphology and selected properties of alluvial soils in the Odra River valley, SW Poland}, url = {https://m2.mtmt.hu/api/publication/34183456}, author = {Kawałko, D. and Kaszubkiewicz, J. and Jezierski, P.}, doi = {10.37501/SOILSA/156062}, journal-iso = {SOIL SCI ANN}, journal = {SOIL SCIENCE ANNUAL}, volume = {73}, unique-id = {34183456}, issn = {2300-4967}, abstract = {The aim of the research carried out in the middle Odra valley, SW Poland, was to demonstrate the diversification of the morphology and selected properties of alluvial soils used for agricultural purposes and to assess their changes in the conditions of river regulation. The research was carried out in the low valley of the Odra River in its middle course downstream from Wrocław. Four soil profiles were exposed on the right bank of the Odra River on the Holocene floodplain terrace. Two profiles were located in the embanked zone used as grassland, and next two profiles were located outside the embankments in the areas used as arable lands. Soils were described, sampled and analyzed using the standard procedures in soil science. The studied soils differed in the morphological features of individual genetic horizons, the location of the groundwater table, the extent and intensity of redoximorphic features, as well as the depth and stratification of the alluvial parent material. This was reflected in the classification: Eutric Fluvic Gleysol (Pantoloamic), Eutric Gleyic Fluvic Cambisol (Ochric), Eutric Fluvic Stagnic Cambisol (Ochric), Eutric Stagnic Fluvisol (Katoarenic, Ochric, Brunic). In the area of this research, the effects of terrain micro-relief former meandering of the river are clearly visible, which is manifested by the heavier texture of the soils situated presently close to the river and lighter texture of soils located further away. The deep occurrence of the groundwater table in soils located in the slightly higher situated sites results in a lowering of vertical range of gleyic properties and their replacement with stagnic properties in the middle part of the soil profile. The change of the water regime contributed to the increase of biological activity, and thus the development of the cambic horizon. The transformation of alluvial soils used as permanent grassland into arable soils causes not only a decrease in the soil organic carbon content in the soil, but also a decrease in the unit sorption capacity of humus compounds. © 2022 by the authors. Licensee Soil Science Society of Poland.}, keywords = {soil properties; groundwater level; alluvial sediments; Floodplain terrace; Odra valley}, year = {2022}, eissn = {2300-4975} } @article{MTMT:34183454, title = {Origin, properties and agricultural value of alluvial soils in the Vistula and Pasłęka deltas, north Poland}, url = {https://m2.mtmt.hu/api/publication/34183454}, author = {Orzechowski, M. and Smólczyński, S. and Kalisz, B. and Sowiński, P.}, doi = {10.37501/SOILSA/157350}, journal-iso = {SOIL SCI ANN}, journal = {SOIL SCIENCE ANNUAL}, volume = {73}, unique-id = {34183454}, issn = {2300-4967}, abstract = {The aim of this study was to investigate the sorptive and air-water properties of alluvial soils of the Vistula and Pasłęka deltas, typologically differentiated in terms of habitat conditions, and to determine their agricultural values. Typical ordinary alluvial soils, humic ordinary alluvial soils, and typical brown alluvial soils were developed from loam, sandy loam and silty clay loam and were located in the oldest part of Żuławy, i.e. 'high' Żuławy (from + 2.5 to + 10.0 m a.s.l.). Typical chernozemic alluvial soils and gleyic chernozemic alluvial soils were formed mainly from silt clay, silt loam and clay loam. They were located mainly in the area of 'transitional' Żuławy (from 0.0 to + 2.5 m a.s.l.), 'low' Żuławy (less than 0.0 m a.s.l.) and in the Pasłęka delta. Chernozemic alluvial soils had greater cation exchange capacity, including base cations, than brown and ordinary alluvial soils. The least favorable air-water relationships were found in ordinary alluvial soils. The volume of macropores in arable horizons of these soils ranged from 3.1% to 4.5%. The ratio of macro- to meso- and micropores was wide: 1: 4.0-5.5: 3.6-5.4, while in chernozemic alluvial soils it was 1: 1.8-2.9: 2.5-3.8. The most favorable air-water relationships were found in arable horizons of typical brown alluvial soils, in which the macro- to meso- and micropores ratio was 1.0: 1.9: 0.7. Ordinary and brown alluvial soils were of 'high' Żuławy were properly or periodically excessively moist, and they are mainly classified as good and medium good arable soils, class RIIIa and RIIIb, of the good wheat soil-agricultural complex. The chernozemic alluvial soils of 'depressive' Żuławy were periodically excessively moist, periodically wet, or permanently wet in the depressive parts of the land. These soils are mainly classified as arable soils medium good, class RIIIb and medium value arable soils, classes RIVa and RIVb, of good wheat soil-agricultural complex and strong forage soil-agricultural complex. The alluvial soils particularly rich in fine silt and clay fractions (over 60%) in depressive areas should be used as permanent grasslands. The conducted research has shown that the soil conditions in the delta areas of the Vistula and Pasłęka river mouths are closely related to the origin and land hypsometry, which differentiates the water conditions, the grain size of soil formations, their type and thickness. © 2022 by the authors. Licensee Soil Science Society of Poland.}, keywords = {Alluvial soils; soil origin; Agricultural value; Air-water properties; Vistula and Pasłęka deltas}, year = {2022}, eissn = {2300-4975} } @article{MTMT:31918067, title = {Morphology and Physicochemical Properties of Alluvial Soils in Riparian Forests after River Regulation}, url = {https://m2.mtmt.hu/api/publication/31918067}, author = {Kawalko, Dorota and Jezierski, Paweł and Kabala, Cezary}, doi = {10.3390/f12030329}, journal-iso = {FORESTS}, journal = {FORESTS}, volume = {12}, unique-id = {31918067}, issn = {1999-4907}, year = {2021}, eissn = {1999-4907}, orcid-numbers = {Jezierski, Paweł/0000-0002-7765-741X; Kabala, Cezary/0000-0001-9796-3716} } @article{MTMT:31145686, title = {The Impact of Land-Use on the Hierarchical Pore Size Distribution and Water Retention Properties in Loamy Soils}, url = {https://m2.mtmt.hu/api/publication/31145686}, author = {Dlapa, Pavel and Hriník, David and Hrabovský, Andrej and Šimkovic, Ivan and Žarnovičan, Hubert and Sekucia, Frederik and Kollár, Jozef}, doi = {10.3390/w12020339}, journal-iso = {WATER-SUI}, journal = {WATER}, volume = {12}, unique-id = {31145686}, year = {2020}, eissn = {2073-4441} } @article{MTMT:31617595, title = {Perspectives of land evaluation of floodplains under conditions of aridification based on the assessment of ecosystem services}, url = {https://m2.mtmt.hu/api/publication/31617595}, author = {Lóczy, Dénes and Tóth, Gergely and Hermann, Tamás and Puhl-Rezsek, Marietta and Nagy, Gábor and Dezső, József and Salem, Ali and Gyenizse, Péter and Gobin, Anne and Vacca, Andrea}, doi = {10.15201/hungeobull.69.3.1}, journal-iso = {HUNG GEOGR BULL (2009-)}, journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)}, volume = {69}, unique-id = {31617595}, issn = {2064-5031}, year = {2020}, eissn = {2064-5147}, pages = {227-243}, orcid-numbers = {Lóczy, Dénes/0000-0002-2542-6775; Tóth, Gergely/0000-0002-4201-1678; Hermann, Tamás/0000-0002-6169-7214; Nagy, Gábor/0000-0003-1755-9719; Salem, Ali/0000-0001-6176-8345; Gyenizse, Péter/0000-0002-8175-9734; Gobin, Anne/0000-0002-3742-7062; Vacca, Andrea/0000-0002-5290-1498} } @article{MTMT:31270050, title = {Parameterizing the modified water cloud model to improve soil moisture data retrieval using vegetation models}, url = {https://m2.mtmt.hu/api/publication/31270050}, author = {Rawat, K S and Singh, S K and Ray, R and Szabó, Szilárd and Kumar, S}, doi = {10.15201/hungeobull.69.1.2}, journal-iso = {HUNG GEOGR BULL (2009-)}, journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)}, volume = {69}, unique-id = {31270050}, issn = {2064-5031}, year = {2020}, eissn = {2064-5147}, pages = {17-26}, orcid-numbers = {Szabó, Szilárd/0000-0002-2670-7384} } @article{MTMT:31187340, title = {Naturalness level of land use in a hilly region in north-eastern Slovenia = Stopnja naravnosti gričevnatega sveta severovzhodne Slovenije z vidika rabe tal}, url = {https://m2.mtmt.hu/api/publication/31187340}, author = {Ciglič, Rok and Nagy, Gábor}, doi = {10.3986/GV91101}, journal-iso = {GEOGRAFSKI VESTNIK}, journal = {GEOGRAFSKI VESTNIK}, volume = {91}, unique-id = {31187340}, issn = {0350-3895}, abstract = {Researchers analyse land use status and its rates of change and try to define the most appropriate structure that suits the environmental characteristics. The article focuses on an analysis of the naturalness level of land use in three hilly regions in north-eastern Slovenia (Slovenske Gorice, Haloze, and Goričko) with the help of geoinformation tools. Land use structure is one of the best indicators of human presence in the landscape. The aim was to expose those parts of catchments that can be regarded as less natural or more natural. We divided the catchments into hydrogeographical areas and analysed them by calculating the urbanity index. The least natural areas in 2018 were located in Slovenske Gorice Hills and the most natural were those in Haloze. The urbanity index diminished between 2002 and 2018 for all the areas except two. The main reason for a higher average of naturalness level is overgrowth – changing agricultural areas into areas with bushes and trees. Natural disasters, e.g. floods and intensive erosion can be mitigated with suitable land use. //}, year = {2019}, pages = {9-31} }