Barta Károly

Farsang Andrea

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441CHRONICLEHungarian Geographical Bulletin 59 (4) (2010) pp. 441–445.Hungarian Conference of Soil ScienceSzeged, Hungary, September 3–4, 2010A conference entitled “Soils under changing physical and social impacts” was organized jointly by Hungarian Soil Science Society, Committ ee for Soil Science and Agricultural Chemistry of Hungarian Academy of Sciences and Department of Physical Geography and Geoinformatics at University of Szeged. The meeting was. organized by a committ ee composed of Barta, K., Bidló, A., Farsang, A., Fuchs, M., László, P., Pirkó, B., Puskás, I., Szabóné Kele, G. The scientifi c committ ee included members Stefanovits, P., Várallyay, Gy., Máté, F., Michéli, E., Farsang, A., Mezősi, G. and Rajkai, K. More than 140 special-ists took part at the conference both from research and educational institutions and from agricultural agencies and fi rms. The plenary session was proceeded by oral and poster presentations on the fi rst day and a whole day fi eld trip followed on the second day.Szabó, G., rector of the University of Szeged opened the conference, then Mezősi, G., head of Department of Physical Geography and Geoinformatics welcomed the partici-pants. In the course of the plenary session Farsang, A. from the host department showed the status of the soil science at the University of Szeged, and talked about education, research and services related to soil science. The second plenary lecture was given by Michéli, E., professor of Szent István University. She talked about the actual tendencies in the interna-tional and domestic soil science and in the activities of the organizations. In the aft ernoon 23 lectures were delivered in 4 oral sessions and 41 poster was shown.In the session entitled “Processes and evaluation of soil data” lectures were given about the Hungarian soil data bases (e.g. the new soil physical data base combined with agrogeological data base, application possibilities of “MARTHA” data base), the potential development of national land evaluation and the connection between the newly developed Hungarian classifi cation and WRB.The “Changing soils” session included various topics. There were lectures about the long-time monitoring systems in Hungary: about “BIOSOIL” program for the observation of soils under Hungarian forests and about changes of brown forest soils in Somogy County based on “TIM” (Soil Information Monitoring) data. Besides, some serious soil degradation processes (water erosion, changes in soil moisture regime, etc.) were shown and changes in individual soil profi les from diff erent parts of the country presented.Participants heard 6 lectures in session “Biological activity and soil use under chang-ing climate and agricultural practice”. There were tackled the new challenges (soil fertility, renewable ability, multifunctionality), problems of sewage sludge disposal, determination the optimum of forest society based on changing soils and improvement of salt aff ected soils in the Great Hungarian Plain.442The last oral session was entitled “Element traffi  c in soils”. There were reports on fi eld experiments with sewage sludge, diff erent composts, energy plants, phosphorus move-ment by water erosion and lectures about vertical movement of copper and the selenium content in Hungarian soils.The fi eld excursion on the day aft er took place under the label “At the contact of diff erent natural microregions”. Participants had the opportunity to visit 5 soil profi les typi-cal of neighbouring landscapes (South Tisza Valley and Dorozsma–Majsa Sand Ridge) or transitional ones on their border. The fi rst of them is found in the city of Szeged, it is a typical Technosol in the archeological excavation of the museum garden. The second one is part of the Soil Information Monitoring. This Chernozem is located west of Szeged on an The opening ceremony and its public443arable land. The third one is confi ned to the landscape border where sandy soil has been formed on the buried Chernozem. This profi le is only 3 km away from the second profi le and WRB can classify it as Arenosol. The next profi le has formed in a fl at depression near Zsombó village. This sandy Gleysol has a very high carbonate content (70–85%) and it is quite unique in Hungary because of its petrocalcic horizon. The last profi le was that of a thin Gleyic Solonetz near Sándorfalva. Att ractive benches completed the salty morphology in this area. The proceedings of the conference would be read in a special issue of journal Talajvédelem (Soil Conservation) to be published in spring 2011. Károly Barta, Andrea FarsangParticipants of the meeting and discussion in the Arenosol profi le

Hungarian Conference of Soil Science

http://publicatio.bibl.u-szeged.hu/5658/1/HunGeoBull_2010_4_441_443_u.pdf

Hungarian Conference of Soil Science

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