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Anna Dobos

Eszterházy Károly University, Department of Environmental Science, Faculty Member

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My name is Dobos Anna PhD., I am an associate pofessor. My research work is about Geomorphology, Soil Science, Geography, Landscape Ecology and Environmental Science. I work at Eszterházy Károly Catholic University in Hungary. I am a member of Community of Hungarian Academy of Sciences.

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Papers by Anna Dobos

Using geological, geomorphological and soil science description data in archaeological research. Andornaktálya, Gyilkos Hill as a case study

Dobos Anna (2018) A természeti és kultúrtörténeti egyedi tájértékek szerepének vizsgálata

A természeti és kultúrtörténeti egyedi tájértékek szerepének vizsgálata a fejlesztési tervekben, egy bükkaljai település példája alapján, 2018

Dobos Anna (2019) A talajadottságok és a tájhasználati rendszer változásainak vizsgálata Egerszalókon

A talajadottságok és a tájhasználati rendszer változásainak vizsgálata Egerszalókon, 2019

Kiss emoke balla daniel tajokologia kotet formazott

Három bükki völgyi település (Cserépfalu - Egerszólát - Kerecsend) tájhasználat változásai és az antropogén hatások mértékének vizsgálata 1763 és 2012 között, 2022

Felszínfejlődési rekonstrukciós vizsgálatok Eger környéki régészeti feltárások esetében, 2018

INVESTIGATION OF THE RELATIONSHIP BETWEEN SOIL EROSION, LAND COVER AND HEMEROBY LEVEL IN CSERÉPFALU BY ANALYSING SOIL PROFILES

INVESTIGATION OF THE RELATIONSHIP BETWEEN SOIL EROSION, LAND COVER AND HEMEROBY LEVEL IN CSERÉPFALU BY ANALYSING SOIL PROFILES Anna Dobos1*, Tamás Péter Hegyi2, Zoltán Zelei2, Balázs Hegyi3, 2023

We can measure the effects of anthropogenic processes to the nature in case of hilly agricultural... more We can measure the effects of anthropogenic processes to the nature in case of hilly agricultural areas with the rate of soil (water) erosion. There is actual question what kind of connection could be shown between the rate of soil erosion, land cover categories and hemeroby levels? How can the intensity of antropogenic effects influence the rate of soil erosion? We did some research work in the North Hungarian Region, in Cserépfalu in 2014. In Cserépfalu, the northern areas are under nature conservation and belong to the Southern Bükk Mountains while the southern dissected pediment is the extensive agricultural territory. We described the soil types in the southern areas using the soil description method of FAO. We collected data about the rate of soil erosion, the land cover types, slope angle, slope forms, slope aspect and data for the relief conditions too. We could point out the sheet erosion around the 15 investigated soil profiles and we could found 3 strongly eroded, 8 medium eroded and 4 accumulated soil profiles. The land cover categories were given based on FAO category system and topographic map from 1990. Our results showed that land cover categories were changed in time and it caused the change of hemeroby levels as well. The intensity of land cultivation in investigated areas was changed. We could point out in some cases that the stronger soil erosion rate was caused by former land cover system. In summary, some former agricultural areas were changed and became as an abandoned area so that the antropogenic effects were decreased in extensive agricultural areas in Cserépfalu. Our results can be compared with another pediment dissected by valleys where extensive agricultural areas are characteristic in Hungary.

Helyi védelem alatt álló természetvédelmi területek fejlesztési koncepciókba való beillesztése, konfliktuskezelési lehetőségek

Kérdőíves vizsgálat a földrajzi ismeretek mindennapi használatáról országos szinten és az egri környezettan hallgatók körében

The travertine mound as a special hydrogeological value and its surroundings at Egerszalók before the building investment

Felszíni formakincs és recens törmelékképződés rolittufa felszínen

A görögországi meteorák természeti és kultúrtörténeti tájértékei

Sajólád természeti értékei

Sajólád is sittuated in the Borsod-Abaúj-Zemplén county, in the microregion of the areas of Sajó-... more Sajólád is sittuated in the Borsod-Abaúj-Zemplén county, in the microregion of the areas of Sajó-Hernád plains. The fluvial cone of the Sajó-Hernád plain is sittuated in 90–161 meters height above the sea level. We have done the research work about the territorial appearance of geological, geomorphological, botanical and zoological values since 2003. This region mostly consists of Holocene and Pleistocene sediments (like as loess and clay, washed loess, and infused loess). As geomorphological values should be mentioned: Holocene alluvium divided by backwaters and bedremains and Holocene fluvial terraces. We have categorized the spatial distribution of botanical and zoological values in the settlement and we could pointed out that the Sajólád Wood is the most interesting and valuable area here

Tájtényezők kapcsolatának vizsgálata a verpeléti Várhegy és környezetének példáján I. Geológiai felépítés, negyedidőszaki üledékek vizsgálata

The Castle Hill in Verpelét is a Tertiary volcanic parasitic cone situated in the eastern boundar... more The Castle Hill in Verpelét is a Tertiary volcanic parasitic cone situated in the eastern boundary of the Mátra Mts. Because of geological interests this territory was declared as a Local Nature Conservation Area in 1975. Its main geological values are the following: Miocene Badenien volcanic sequence, the structure of the composite volcano, the volcanic vent and andesitic volcanic plug, volcaniclastic deposits and the remnant of the postvolcanic activity. This territory was burried by different sediment layers after the Miocene volcanic activity and this composite volcano was exhumated by the Tarna stream during the Quaternary period. That is why we could examined different, varied Quaternary sediments here: slope sediments rich in volcanic detritus, slope clay, fluvial sediments, loess sedimnt (97–150 cm in depth) and frost-reven detritus in front of andesitic cliffs

A gólyaorr biotikus tájtényezőinek felvételezése

In this article we present the analysis of biotic and antropogenic factors in case of Gólyaorr si... more In this article we present the analysis of biotic and antropogenic factors in case of Gólyaorr situated in Poroszló, in the Heves alluvium microregion between October in 2007. and November in 2008. Our aim was to analyse and survey different landscape factors and to point out system relationships among these landscape factors. In the study area, we could do the research work on the botanical and zoological landscape factors and antropogenic effects on this territory, which is situated in the buffer-zone of the Hortobágy National Park

Bánd természeti és kultúrtörténeti tájértékeinek kataszterezése és állapotfelmérése

Kérdőíves felmérés - a továbbtanulás szempontjából értékelhető tantárgyak fontosságát illetően - egri környezettan szakos hallgatók körében (2009)

Éghajlatváltozások bizonyítékai a Bükkalján geológiai feltárások alapján

LÁSZLÓ UJFALUDI

Tájtényezők kapcsolatának vizsgálata a verpeléti Várhegy és környezetének példáján II. Geomorfológiai, éghajlati, vízrajzi adottságok, talajtani és botanikai vizsgálatok

Our study area – the Castle Hill and its surrounding in Verpelét – is situated int he southern pa... more Our study area – the Castle Hill and its surrounding in Verpelét – is situated int he southern part of the Tarna valley between the Mátra Mts. and the Bü cone which can be found in basin-hil . kk Mts. in North Hungary. The castle Hill is a volcanic parasitic ly environment The aim of our research work was to investigate the relation among different landscape factors in this territory. We have examined the geological building up and Quaternary sediments int he first part of our study. (Dobos A.–Schmidt J. 2005). In this article we explore the relationship among morphological, climatic, hydrographical, soil and botanical conditions

A gólyaorr abiotikus tájtényezőinek felvételezése

In this article we would like to present the analysis of abiotic factors in case of Gólyaorr situ... more In this article we would like to present the analysis of abiotic factors in case of Gólyaorr situated in Poroszló, in the Heves alluvium microregion between October in 2007. and November in 2008. Our aim was to analyse, and survey different landscape factors and to point out system relationships among these landscape factors. In the study area, we could do the research work on the landscape development of this alluvium territory, the Quaternary sediments and soil types of this area, the analysis of water quality, climatic conditions and the special Earth Scientific Values in the buffer-zone of the Hortobágy National Park

Reconstruction of Quaternary landscape development with geomorphological mapping and analysing of sediments at the Cserépfalu Basin (the Bükk Mts., Hungary)

Using geological, geomorphological and soil science description data in archaeological research. Andornaktálya, Gyilkos Hill as a case study

Dobos Anna (2018) A természeti és kultúrtörténeti egyedi tájértékek szerepének vizsgálata

A természeti és kultúrtörténeti egyedi tájértékek szerepének vizsgálata a fejlesztési tervekben, egy bükkaljai település példája alapján, 2018

Dobos Anna (2019) A talajadottságok és a tájhasználati rendszer változásainak vizsgálata Egerszalókon

A talajadottságok és a tájhasználati rendszer változásainak vizsgálata Egerszalókon, 2019

Kiss emoke balla daniel tajokologia kotet formazott

Három bükki völgyi település (Cserépfalu - Egerszólát - Kerecsend) tájhasználat változásai és az antropogén hatások mértékének vizsgálata 1763 és 2012 között, 2022

Felszínfejlődési rekonstrukciós vizsgálatok Eger környéki régészeti feltárások esetében, 2018

INVESTIGATION OF THE RELATIONSHIP BETWEEN SOIL EROSION, LAND COVER AND HEMEROBY LEVEL IN CSERÉPFALU BY ANALYSING SOIL PROFILES

INVESTIGATION OF THE RELATIONSHIP BETWEEN SOIL EROSION, LAND COVER AND HEMEROBY LEVEL IN CSERÉPFALU BY ANALYSING SOIL PROFILES Anna Dobos1*, Tamás Péter Hegyi2, Zoltán Zelei2, Balázs Hegyi3, 2023

We can measure the effects of anthropogenic processes to the nature in case of hilly agricultural... more We can measure the effects of anthropogenic processes to the nature in case of hilly agricultural areas with the rate of soil (water) erosion. There is actual question what kind of connection could be shown between the rate of soil erosion, land cover categories and hemeroby levels? How can the intensity of antropogenic effects influence the rate of soil erosion? We did some research work in the North Hungarian Region, in Cserépfalu in 2014. In Cserépfalu, the northern areas are under nature conservation and belong to the Southern Bükk Mountains while the southern dissected pediment is the extensive agricultural territory. We described the soil types in the southern areas using the soil description method of FAO. We collected data about the rate of soil erosion, the land cover types, slope angle, slope forms, slope aspect and data for the relief conditions too. We could point out the sheet erosion around the 15 investigated soil profiles and we could found 3 strongly eroded, 8 medium eroded and 4 accumulated soil profiles. The land cover categories were given based on FAO category system and topographic map from 1990. Our results showed that land cover categories were changed in time and it caused the change of hemeroby levels as well. The intensity of land cultivation in investigated areas was changed. We could point out in some cases that the stronger soil erosion rate was caused by former land cover system. In summary, some former agricultural areas were changed and became as an abandoned area so that the antropogenic effects were decreased in extensive agricultural areas in Cserépfalu. Our results can be compared with another pediment dissected by valleys where extensive agricultural areas are characteristic in Hungary.

Helyi védelem alatt álló természetvédelmi területek fejlesztési koncepciókba való beillesztése, konfliktuskezelési lehetőségek

Kérdőíves vizsgálat a földrajzi ismeretek mindennapi használatáról országos szinten és az egri környezettan hallgatók körében

The travertine mound as a special hydrogeological value and its surroundings at Egerszalók before the building investment

Felszíni formakincs és recens törmelékképződés rolittufa felszínen

A görögországi meteorák természeti és kultúrtörténeti tájértékei

Sajólád természeti értékei

Sajólád is sittuated in the Borsod-Abaúj-Zemplén county, in the microregion of the areas of Sajó-... more Sajólád is sittuated in the Borsod-Abaúj-Zemplén county, in the microregion of the areas of Sajó-Hernád plains. The fluvial cone of the Sajó-Hernád plain is sittuated in 90–161 meters height above the sea level. We have done the research work about the territorial appearance of geological, geomorphological, botanical and zoological values since 2003. This region mostly consists of Holocene and Pleistocene sediments (like as loess and clay, washed loess, and infused loess). As geomorphological values should be mentioned: Holocene alluvium divided by backwaters and bedremains and Holocene fluvial terraces. We have categorized the spatial distribution of botanical and zoological values in the settlement and we could pointed out that the Sajólád Wood is the most interesting and valuable area here

Tájtényezők kapcsolatának vizsgálata a verpeléti Várhegy és környezetének példáján I. Geológiai felépítés, negyedidőszaki üledékek vizsgálata

The Castle Hill in Verpelét is a Tertiary volcanic parasitic cone situated in the eastern boundar... more The Castle Hill in Verpelét is a Tertiary volcanic parasitic cone situated in the eastern boundary of the Mátra Mts. Because of geological interests this territory was declared as a Local Nature Conservation Area in 1975. Its main geological values are the following: Miocene Badenien volcanic sequence, the structure of the composite volcano, the volcanic vent and andesitic volcanic plug, volcaniclastic deposits and the remnant of the postvolcanic activity. This territory was burried by different sediment layers after the Miocene volcanic activity and this composite volcano was exhumated by the Tarna stream during the Quaternary period. That is why we could examined different, varied Quaternary sediments here: slope sediments rich in volcanic detritus, slope clay, fluvial sediments, loess sedimnt (97–150 cm in depth) and frost-reven detritus in front of andesitic cliffs

A gólyaorr biotikus tájtényezőinek felvételezése

In this article we present the analysis of biotic and antropogenic factors in case of Gólyaorr si... more In this article we present the analysis of biotic and antropogenic factors in case of Gólyaorr situated in Poroszló, in the Heves alluvium microregion between October in 2007. and November in 2008. Our aim was to analyse and survey different landscape factors and to point out system relationships among these landscape factors. In the study area, we could do the research work on the botanical and zoological landscape factors and antropogenic effects on this territory, which is situated in the buffer-zone of the Hortobágy National Park

Bánd természeti és kultúrtörténeti tájértékeinek kataszterezése és állapotfelmérése

Kérdőíves felmérés - a továbbtanulás szempontjából értékelhető tantárgyak fontosságát illetően - egri környezettan szakos hallgatók körében (2009)

Éghajlatváltozások bizonyítékai a Bükkalján geológiai feltárások alapján

LÁSZLÓ UJFALUDI

Tájtényezők kapcsolatának vizsgálata a verpeléti Várhegy és környezetének példáján II. Geomorfológiai, éghajlati, vízrajzi adottságok, talajtani és botanikai vizsgálatok

Our study area – the Castle Hill and its surrounding in Verpelét – is situated int he southern pa... more Our study area – the Castle Hill and its surrounding in Verpelét – is situated int he southern part of the Tarna valley between the Mátra Mts. and the Bü cone which can be found in basin-hil . kk Mts. in North Hungary. The castle Hill is a volcanic parasitic ly environment The aim of our research work was to investigate the relation among different landscape factors in this territory. We have examined the geological building up and Quaternary sediments int he first part of our study. (Dobos A.–Schmidt J. 2005). In this article we explore the relationship among morphological, climatic, hydrographical, soil and botanical conditions

A gólyaorr abiotikus tájtényezőinek felvételezése

In this article we would like to present the analysis of abiotic factors in case of Gólyaorr situ... more In this article we would like to present the analysis of abiotic factors in case of Gólyaorr situated in Poroszló, in the Heves alluvium microregion between October in 2007. and November in 2008. Our aim was to analyse, and survey different landscape factors and to point out system relationships among these landscape factors. In the study area, we could do the research work on the landscape development of this alluvium territory, the Quaternary sediments and soil types of this area, the analysis of water quality, climatic conditions and the special Earth Scientific Values in the buffer-zone of the Hortobágy National Park

Reconstruction of Quaternary landscape development with geomorphological mapping and analysing of sediments at the Cserépfalu Basin (the Bükk Mts., Hungary)

Dobos, A. (2023): Using geological, geomorphological and soil science description data in archaeological research. Andornaktálya, Gyilkos Hill as a case study.

Nowadays, geological, Quaternary sedimentological, soil science and geomorphological research can... more Nowadays, geological, Quaternary sedimentological, soil science and geomorphological research can give new information for analysing and describing archaeological sites. In this article, we have investigated the ancient environmental and landscape conditions in the case of the Upper Palaeolithic archaeological open-air site situated on Gyilkos Hill in Andornaktálya, Hungary. We have analysed the geological situation, Quaternary sediments, soil and geomorphological conditions. Our results show that ancient people lived in a higher but separated and lowered pediment area surrounded by the Eger and Ostoros streams during the Aurignacian culture in the Upper Palaeolithic period (Würm glaciation). Slopes were dissected by dells and the heads of erosional valleys and this territory could be covered by cool continental steppe and tundra vegetation. Soil data show that medium-fertiled Chernozem brown forest soil developed here later which is the remnant of the new forested Late Glacial warmer period. This high, separated hilly territory could be well protected suitable for inhabitants to settle down. That is why archaeological surveys found a Palaeolithic open-air site here. We aim to use this complex research survey method at other archaeological sites.

Természeti és kultúrtörténeti értek Eger térségében_Natural and Cultural heritage in Eger Region_2

Eds. Dobos Anna - Mika János , 2017

TERMÉSZETI ÉS KULTÚRTÖRTÉNETI ÉRTÉKEK EGER TÉRSÉGÉBEN NATURAL AND CULTURAL HERITAGE IN THE EGER REGION_1

eds. Dobos Anna - Mika János, 2017