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Ákos Malatinszky Szilvia Ádám Eszter Falusi Dénes Saláta Károly Penksza 《Climatic change》2013,118(3-4):671-682
Land managers of wetlands face various challenges emerging from climate change. Exploration of these problems is a prerequisite to developing adaptive management of vulnerable areas. Central and Eastern European countries are highly vulnerable to climate change. The Balaton Uplands National Park, an attractive tourist destination with natural values of high national and community importance, has suffered the greatest extremities in precipitation in Hungary during 2010 and 2011. After identification of stakeholder groups, private landowners and land managers as being most likely affected by climate change were interviewed in the national park. A compilation of the most important land use problems that already have influence on the management of protected wetlands was listed. Land managers connect several problems to weather extremities and long-term changes, but take practically no actions in favor of mitigation or adaptation, or strengthening resilience. As there is strong evidence that wet habitats are becoming more sensitive and vulnerable, land managers have to adapt their objectives, strategies and measures to changing climate and be involved in the process of adapting the management measures of protected areas, especially wetlands, to probable effects of climate change. 相似文献
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Tamás Bozóki Eszter Ágnes Krasznai-Kun András Csercsa Gábor Várbíró Pál Boda 《Environmental Earth Sciences》2018,77(15):559
Urbanization is a current and increasing threat to biodiversity. The effects of urbanization on the functional and taxonomic composition of macroinvertebrate assemblages were investigated in two seasons along a small urban stream. Species composition was determined by the rate of urbanization; however, response of species richness could not be evidenced. Relative abundance of the sensitive macroinvertebrate groups (EPT%) was negatively related to urbanization. Almost all feeding groups showed a sharp decline in the number of specimens along the increase of urbanization. The study supports the view that urbanization has a negative effect on the biological quality of a stream, yet, this obvious impact can be overridden by different measures such as modification in streambed morphology. The altered conditions and new circumstances in urban environments lead to the creation of novel ecosystems, inhabited by macroinvertebrate communities with species richness approaching that of low impacted sites. However, species composition of these communities could be basically different from that of the natural ones. 相似文献
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Kálmán Török Bianka Németh Friedrich Koller Júlia Dégi Eszter Badenszki Csaba Szabó Aberra Mogessie 《Mineralogy and Petrology》2014,108(1):33-47
Felsic to mafic granulite xenoliths from late Neogene basalt pyroclastics in four localities of the western Pannonian Basin (Beistein, Kapfenstein, Szigliget and Káptalantóti (Sabar-hegy) were studied to find out their metamorphic and fluid history. The characteristic mineral assemblage of the granulites consists of Pl + Opx + Qtz ± Cpx ± Bt ± Grt ± Kfs. Based on abundant magmatic relic microstructural domains occurring in these rocks, the potential precursors might have been predominantly felsic igneous or high to ultrahigh temperature rocks. Ternary feldspar thermometry provides a rough estimate of temperatures of about 920–1070 °C. The first fluid invasion event, which is linked with this early high to ultrahigh temperature stage is characterised by primary pure CO2 inclusions in apatite and zircon. The densest primary CO2 inclusions indicate 0.52–0.64 GPa pressure at the estimated temperature range of crystallization. According to mineral equilibria and geothermobarometry, the high to ultrahigh temperature rock cooled and crystallized to granulite of predominantly felsic composition at about 750–870 °C and 0.50–0.75 GPa in the middle crust, between 20 and 29 km depths. The second fluid invasion event is recorded by primary CO2-rich fluid inclusions hosted in the granulitic mineral assemblage (plagioclase, quartz and orthopyroxene). In addition to CO2, Raman spectroscopy revealed the presence of minor N2, H2S, CO and H2O in these inclusions. Partial melting of biotite-bearing assemblages could be connected to the next fluid invasion shown by secondary CO2-rich fluids recorded along with healed fractures in plagioclase, clinopyroxene and orthopyroxene. This event could have happened at depths similar to the previous ones. The final step in the granulite evolution was the sampling in the middle crust and transportation to the surface in form of xenoliths by mafic melt. This event generated temperature increase and pressure decrease and thus, limited melting of the xenoliths. The youngest fluid inclusion generation, observed mostly in healed fractures of felsic minerals, could be associated with this event. 相似文献
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Indoor radon mapping and its relation to geology in Hungary 总被引：2，自引：0，他引：2
Mihály Minda György Tóth István Horváth Ivan Barnet Krisztián Hámori Eszter Tóth 《Environmental Geology》2009,57(3):601-609
Indoor radon mapping may show stronger dependence on geological formations if the measured homes are one-storied houses with
no basement. In Hungary, 17,244 homes were investigated on the yearly average of indoor radon concentrations; among these
homes, there were 6,154, one-storied, no-basement houses. In Hungary, 21 geological units were created relevant for indoor
radon index characterized by lithology, the position of the ground water table, and the gas permeability. Maps were drawn
of different topography (counties, grid, geological units) and different values (maximum, mean, indoor radon indexes). A kind
of standardization of houses was that only the one-storied, no-basement ones were chosen, but from geological point of view some more information was gained when the wall materials (bricks or adobe) were also taken
into account. (“Adobe” is made of clay and straw in Hungary, and not burned as brick, just dried on sunshine). Enhanced indoor
radon values can be observed on the bedrock of Cenozoic volcanic rocks and their eroded materials deposited on the local alluvial
valleys. Another group with relatively increased indoor radon values can be connected to granite bodies. The grid method is
useful for covering large state or even continental areas. For practical public use and detailed radon risk mapping geological
or administrative unit-systems could yield more reasonable and useful results. 相似文献
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