TY - JOUR AU - Potopová, V. AU - Trifan, T. AU - Trnka, M. AU - De Michele, C. AU - Semerádová, D. AU - Fischer, M. AU - Meitner, J. AU - Musiolková, M. AU - Muntean, N. AU - Clothier, B. TI - Copulas modelling of maize yield losses – drought compound events using the multiple remote sensing indices over the Danube River Basin JF - AGRICULTURAL WATER MANAGEMENT J2 - AGR WATER MANAGE VL - 280 PY - 2023 PG - 21 SN - 0378-3774 DO - 10.1016/j.agwat.2023.108217 UR - https://m2.mtmt.hu/api/publication/33634768 ID - 33634768 N1 - Department of Agroecology and Crop Production, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Czech Republic Global Change Research Institute of the Czech Academy of Sciences, Brno, Czech Republic Politecnico di Milano, Dept. of Civil and Env. Engineering, Italy Plant and Food Research Palmerston North, Manawatu Mail Centre, Palmerston North, New Zealand Export Date: 15 February 2023 CODEN: AWMAD Correspondence Address: Potopová, V.; Department of Agroecology and Crop Production, Czech Republic; email: potop@af.czu.cz LA - English DB - MTMT ER - TY - JOUR AU - Tutova, G. F. AU - Kunakh, O. M. AU - Yakovenko, V. M. AU - Zhukov, O. V. TI - 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 JF - BIOSYSTEMS DIVERSITY J2 - BIOSYST DIV VL - 31 PY - 2023 IS - 2 SP - 177 EP - 190 PG - 14 SN - 2519-8513 DO - 10.15421/012319 UR - https://m2.mtmt.hu/api/publication/34103558 ID - 34103558 N1 - Bogdan Khmelnitsky Melitopol State Pedagogical University, Hetmanskast., 20, Melitopol, 72318, Ukraine Oles Honchar Dnipro National University, Gagarinav., 72, Dnipro, 49000, Ukraine Dnipro State Agrarian and Economic University, Serhii Efremovst., 25, Dnipro, 49600, Ukraine Export Date: 9 October 2023 AB - 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%. LA - English DB - MTMT ER - TY - JOUR AU - Kawałko, D. AU - Kaszubkiewicz, J. AU - Jezierski, P. TI - Morphology and selected properties of alluvial soils in the Odra River valley, SW Poland JF - SOIL SCIENCE ANNUAL J2 - SOIL SCI ANN VL - 73 PY - 2022 IS - 3 PG - 11 SN - 2300-4967 DO - 10.37501/SOILSA/156062 UR - https://m2.mtmt.hu/api/publication/34183456 ID - 34183456 N1 - Cited By :1 Export Date: 9 October 2023 Correspondence Address: Kawałko, D.; Wrocław University of Environmental and Life Science, Grunwaldzka 53, Poland; email: dorota.kawalko@upwr.edu.pl Funding details: Uniwersytet Przyrodniczy we Wrocławiu, UPWr Funding text 1: The article was created as a result of the research project No. N090 / 0014/22 financed by the Wrocław University of Environmental and Life Sciences as part of the “MISTRZ” program. AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Orzechowski, M. AU - Smólczyński, S. AU - Kalisz, B. AU - Sowiński, P. TI - Origin, properties and agricultural value of alluvial soils in the Vistula and Pasłęka deltas, north Poland JF - SOIL SCIENCE ANNUAL J2 - SOIL SCI ANN VL - 73 PY - 2022 IS - 3 PG - 8 SN - 2300-4967 DO - 10.37501/SOILSA/157350 UR - https://m2.mtmt.hu/api/publication/34183454 ID - 34183454 N1 - Export Date: 9 October 2023 Correspondence Address: Orzechowski, M.; University of Warmia and Mazury in Olsztyn, Plac Łódzki 3, Poland; email: miroslaw.orzechowski@uwm.edu.pl Funding details: 30.610.005-110 Funding text 1: The results presented in this paper were obtained as part of a comprehensive study financed by University of Warmia and Mazury in Olsztyn, Faculty of Agriculture and Forestry, Department of Soil Science and Microbiology (No 30.610.005-110). AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Kawalko, Dorota AU - Jezierski, Paweł AU - Kabala, Cezary TI - Morphology and Physicochemical Properties of Alluvial Soils in Riparian Forests after River Regulation JF - FORESTS J2 - FORESTS VL - 12 PY - 2021 IS - 3 SN - 1999-4907 DO - 10.3390/f12030329 UR - https://m2.mtmt.hu/api/publication/31918067 ID - 31918067 N1 - Cited By :17 Export Date: 9 October 2023 Correspondence Address: Kawalko, D.; Wroclaw University of Environmental and Life Sciences, ul. Grunwaldzka 53, Poland; email: dorota.kawalko@upwr.edu.pl Funding details: Ministerstwo Edukacji i Nauki, MNiSW, MNiSW N N305 154537/2009 Funding text 1: Funding: This work was co-financed by the Ministry of Higher Education and Science of Poland, project MNiSW N N305 154537/2009 and a statute project of Wrocław University of Environmental and Life Sciences, Institute of Soil Science and Environmental Protection from a subsidy of the Ministry of Education and Science of Poland. LA - English DB - MTMT ER - TY - JOUR AU - Dlapa, Pavel AU - Hriník, David AU - Hrabovský, Andrej AU - Šimkovic, Ivan AU - Žarnovičan, Hubert AU - Sekucia, Frederik AU - Kollár, Jozef TI - The Impact of Land-Use on the Hierarchical Pore Size Distribution and Water Retention Properties in Loamy Soils JF - WATER J2 - WATER-SUI VL - 12 PY - 2020 IS - 2 SN - 2073-4441 DO - 10.3390/w12020339 UR - https://m2.mtmt.hu/api/publication/31145686 ID - 31145686 N1 - Department of Soil Science, Comenius University, Mlynská dolina, Ilkovicova 6, Bratislava, 84215, Slovakia Department of Landscape Ecology, Comenius University, Mlynská dolina, Ilkovicova 6, Bratislava, 84215, Slovakia Institute of Landscape Ecology SAS, Štefánikova 3, Bratislava, 81499, Slovakia Cited By :2 Export Date: 25 October 2020 Correspondence Address: Dlapa, P.; Department of Soil Science, Comenius University, Mlynská dolina, Ilkovicova 6, Slovakia; email: pavel.dlapa@uniba.sk LA - English DB - MTMT ER - TY - JOUR AU - Lóczy, Dénes AU - Tóth, Gergely AU - Hermann, Tamás AU - Puhl-Rezsek, Marietta AU - Nagy, Gábor AU - Dezső, József AU - Salem, Ali AU - Gyenizse, Péter AU - Gobin, Anne AU - Vacca, Andrea TI - Perspectives of land evaluation of floodplains under conditions of aridification based on the assessment of ecosystem services JF - HUNGARIAN GEOGRAPHICAL BULLETIN (2009-) J2 - HUNG GEOGR BULL (2009-) VL - 69 PY - 2020 IS - 3 SP - 227 EP - 243 PG - 17 SN - 2064-5031 DO - 10.15201/hungeobull.69.3.1 UR - https://m2.mtmt.hu/api/publication/31617595 ID - 31617595 N1 - Institute of Geography and Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, Keszthely, H-8360, Hungary Doctoral School of Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Civil Engineering Department, Faculty of Engineering, Minia University, Minia, 61111, Egypt Flemish Institute for Technological Research (VITO), Boeretang 200, Mol, B-2400, Belgium Department of Earth and Environmental Sciences, Faculty of BioScience Engineering, University of Leuven, Celestijnenlaan 200E, Heverlee, 3001, Belgium Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria (Axis D), Monserrato, I-09042, Italy Export Date: 25 October 2020 Institute of Geography and Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, Keszthely, H-8360, Hungary Doctoral School of Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Civil Engineering Department, Faculty of Engineering, Minia University, Minia, 61111, Egypt Flemish Institute for Technological Research (VITO), Boeretang 200, Mol, B-2400, Belgium Department of Earth and Environmental Sciences, Faculty of BioScience Engineering, University of Leuven, Celestijnenlaan 200E, Heverlee, 3001, Belgium Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria (Axis D), Monserrato, I-09042, Italy Export Date: 12 March 2021 Institute of Geography and Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, Keszthely, H-8360, Hungary Doctoral School of Earth Sciences, University of Pécs, Ifjúság útja 6., Pécs, H-7624, Hungary Civil Engineering Department, Faculty of Engineering, Minia University, Minia, 61111, Egypt Flemish Institute for Technological Research (VITO), Boeretang 200, Mol, B-2400, Belgium Department of Earth and Environmental Sciences, Faculty of BioScience Engineering, University of Leuven, Celestijnenlaan 200E, Heverlee, 3001, Belgium Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria (Axis D), Monserrato, I-09042, Italy Export Date: 11 August 2021 LA - English DB - MTMT ER - TY - JOUR AU - Rawat, K S AU - Singh, S K AU - Ray, R AU - Szabó, Szilárd AU - Kumar, S TI - Parameterizing the modified water cloud model to improve soil moisture data retrieval using vegetation models JF - HUNGARIAN GEOGRAPHICAL BULLETIN (2009-) J2 - HUNG GEOGR BULL (2009-) VL - 69 PY - 2020 IS - 1 SP - 17 EP - 26 PG - 10 SN - 2064-5031 DO - 10.15201/hungeobull.69.1.2 UR - https://m2.mtmt.hu/api/publication/31270050 ID - 31270050 LA - English DB - MTMT ER - TY - JOUR AU - Ciglič, Rok AU - Nagy, Gábor TI - Naturalness level of land use in a hilly region in north-eastern Slovenia = Stopnja naravnosti gričevnatega sveta severovzhodne Slovenije z vidika rabe tal JF - GEOGRAFSKI VESTNIK J2 - GEOGRAFSKI VESTNIK VL - 91 PY - 2019 IS - 1 SP - 9 EP - 31 PG - 23 SN - 0350-3895 DO - 10.3986/GV91101 UR - https://m2.mtmt.hu/api/publication/31187340 ID - 31187340 N1 - Cited By :3 Export Date: 9 October 2023 Funding details: Javna Agencija za Raziskovalno Dejavnost RS, ARRS, N6-0070 Funding details: Nemzeti Kutatási Fejlesztési és Innovációs Hivatal, NKFIH, SNN 125727 Funding text 1: Acknowledgements: The authors acknowledge the study was performed in the frame of a project Possible ecological control of flood hazard in the hilly regions of Hungary and Slovenia. The project was financially supported by the Slovenian Research Agency (ARRS, N6-0070) and the Hungarian Na tional Research, Development and Innovation Office (NKFIH, SNN 125727). We would like to thank prof. Dénes Loczy for his help. AB - 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. // LA - Slovenian DB - MTMT ER -