@misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Bodenkundlich-geomorphologische Untersuchung von Meilerpl{\"a}tzen um Weiherhammer}, series = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, volume = {12}, journal = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, issn = {1617-4461}, pages = {433 -- 448}, language = {de} } @misc{RaabHirschRaabetal., author = {Raab, Thomas and Hirsch, Florian and Raab, Alexandra and Schneider, Anna and Bonhage, Alexander and B{\"o}nisch, Eberhard}, title = {B{\"o}den historischer Landnutzung in der Niederlausitz - W{\"o}lb{\"a}cker und Kohlemeiler}, series = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, volume = {26}, journal = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, number = {1/2}, issn = {0947-1995}, pages = {5 -- 14}, abstract = {In der Niederlausitz finden sich - meist unter Kiefern- und Eichenforsten versteckt - zahlreiche Relikte der historischen Landnutzung, die bisher kaum bekannt sind. Zu den auff{\"a}lligsten Formen z{\"a}hlen W{\"o}lb{\"a}cker und Pl{\"a}tze ehemaliger Kohlemeiler. In einigen Regionen der Niederlausitz ist die Verbreitung der Landnutzungsrelikte so groß bzw. ihre Dichte so hoch, dass sie pr{\"a}gend f{\"u}r die Bodenlandschaft werden. Dieser Beitrag zeigt an repr{\"a}sentativen Beispielen die charakteristischen Merkmale und Eigenschaften der B{\"o}den auf W{\"o}lb{\"a}ckern und Relikten von Holzkohlenmeilern (HKM).}, language = {de} } @misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Bonhage, Alexander and Raab, Thomas}, title = {Relikte historischer Kohlenmeier ini der Oberpfalz - Verbreitung und Erhaltung in Abh{\"a}ngigkeit vom Naturraum}, series = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, journal = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, number = {13}, issn = {1617-4461}, pages = {531 -- 546}, language = {de} } @misc{RaabRaabTaklaetal., author = {Raab, Alexandra and Raab, Thomas and Takla, Melanie and Nicolay, Alexander and B{\"o}nisch, Eberhard and R{\"o}sler, H.}, title = {B{\"o}den als Archive der Landschaftsgeschichte im Vorfeld des Tagebaus J{\"a}nschwalde}, series = {Exkursionsf{\"u}hrer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam}, journal = {Exkursionsf{\"u}hrer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam}, publisher = {Deutsche Bodenkundliche Gesellschaft}, address = {Oldenburg}, pages = {84 -- 96}, language = {de} } @misc{SeiffertNenovMaureretal., author = {Seiffert, Thomas and Nenov, Rossen and Maurer, Thomas and Gerwin, Werner and Veste, Maik and Raab, Thomas}, title = {Microdrone-based photogrammetry for water catchment monitoring}, series = {Dimensions of ecology - from global change to molecular ecology, (Gf{\"O}) 39th annual conference, University of Bayreuth, 14th - 18th September 2009}, journal = {Dimensions of ecology - from global change to molecular ecology, (Gf{\"O}) 39th annual conference, University of Bayreuth, 14th - 18th September 2009}, editor = {Holzheu, Stefan and Thies, B.}, publisher = {Bayreuther Zentrum f{\"u}r {\"O}kologie und Umweltforschung (BayCEER) Selbstverlag}, address = {Bayreuth}, pages = {S. 129}, language = {en} } @misc{Raab, author = {Raab, Thomas}, title = {Was ist eigentlich Geopedologie?}, series = {Forschung \& Lehre : alles was die Wissenschaft bewegt}, volume = {22}, journal = {Forschung \& Lehre : alles was die Wissenschaft bewegt}, number = {8}, issn = {0945-5604}, pages = {646 -- 647}, abstract = {Die Geopedologie kann den Erd- und Umweltwissenschaften zugerechnet werden. Sie hat ihre Wurzeln in der Geomorphologie und der Bodenkunde. Hinzu kommen Aspekte der Geologie, der Mineralogie und Petrologie. Geforscht wird interdisziplin{\"a}r.}, language = {de} } @misc{HirschRaab, author = {Hirsch, Florian and Raab, Thomas}, title = {Stratigraphy and distribution of Late Quaternary sediments in the Aragon- and Gallego Valley (Aragonese Pyrenees, Spain)}, series = {Quaternary International}, volume = {279-280}, journal = {Quaternary International}, doi = {10.1016/j.quaint.2012.08.370}, pages = {S. 202}, abstract = {Within the scope of the research project post-LGM pedogenesis and geomorphodynamics in the Aragonese Pyrenees (Spain), funded by the DFG (Az RA 931/3-1), soils and sediments are used to reconstruct the Late Quaternary landscape formation. By employing multiple field and laboratory methods, several sediment facies (glacial, periglacial, fluvial and anthropogenic induced colluvial displacement) can be distinguished. Due to small scale horizontal and vertical distribution of the Quaternary sediments, the genetic differentiation is crucial for the dating of periglacial and glacial phases. The polygenetic sediment sequences indicate periods of post-glacial geomorphodynamic, probably induced by changing climatic or anthropogenic influences. The glacial sediments are preserved as lateral and terminal moraines. Due to the arrangement of the moraines, several Pleistocene glacial advances can be recognized. Cold climate conditions led to the formation of periglacial slope deposits which are classified as lower and upper heads in accordance to findings from Central Europe (Raab \& V{\"o}lkel 2003, Raab et al. 2010). Although lower heads are restricted to the Pleistocene extraglacial landscape, upper heads can be located in the Pleistocene extraglacial and glacial landscape. Upper heads are characterized by a high amount of silt, which is interpreted as the result of an aeolian admixture. The aeolian component is not limited to the upper head but can also be found as loess deposit on glaciofluvial and fluvial terraces. Due to the characteristically low inclination of the terraces the aeolian cover was only sparsely affected by erosion. On the other hand, on steeper slopes, intensive land use results in residual shallow sediment cover above the bedrock in the upper slopes and deep colluvial layers on the foot slopes and valley bottoms.}, language = {en} } @misc{HirschRaab, author = {Hirsch, Florian and Raab, Thomas}, title = {Chronology of Late Quaternary sediments in the Aragonese Pyrenees}, series = {Quaternary International}, volume = {279-280}, journal = {Quaternary International}, doi = {10.1016/j.quaint.2012.08.371}, pages = {S. 202}, abstract = {The Spanish Pyrenees are a type region for Quaternary glaciations. Although the history of glacial research dates back until the first fieldtrips of Charpentier in 1841 and Penck in 1883, the maximum extent of Pleistocene glaciers and the exact chronology is still discussed. Whereas some authors suggest a last glacial maximum (LGM) synchronous to the European Alps, there are also several authors preferring a much earlier Pyrenean LGM. The differing ages for the LGM research using absolute chronological methods reveal the need for a clear stratigraphical and sedimentological approach prior to chronological sampling on Quaternary sediments. Within the scope of the research project post-LGM pedogenesis and geomorphodynamics in the Aragonese Pyrenees (Spain) funded by the DFG (Az RA 931/3-1) Quaternary sediments are differentiated by a combination of multiple field and laboratory methods. This identification of the sediments, combined with the stratigraphic approach forms the basis for the dating of the sediment facies and therefore the prevailing climate conditions at the time of the sedimentation. The studies are mainly conducted in the Aragon- and Gallego Valley, which are both situated in the Aragonese Pyrenees (Spain). We use optically stimulated luminescence (OSL) to date the uppermost unit of the periglacial slope deposits which typically cover glacial sediments in most parts of the study area. There is clear evidence that the glacial and periglacial sediments are partly eroded due to human impact. First OSL and 14C dating reveal relatively young ages for this phase of soil erosion and redepostion on the slopes (approximately 300 a BP).}, language = {en} } @misc{Raab, author = {Raab, Thomas}, title = {Zur Bedeutung der historischen Montanwirtschaft f{\"u}r die Landschaftsentwicklung und Geoökologie des Vilstals in der Oberpfalz}, series = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, volume = {12}, journal = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, number = {59}, issn = {1617-4461}, pages = {319 -- 336}, language = {de} } @misc{GerwinRaabBauriegeletal., author = {Gerwin, Werner and Raab, Thomas and Bauriegel, Albrecht and Nicolay, Alexander}, title = {Junge B{\"o}den der Niederlausitz}, series = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, volume = {22}, journal = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, number = {1}, issn = {0947-1995}, pages = {137 -- 148}, abstract = {In der Niederlausitz finden sich sehr unterschiedliche Beispiele f{\"u}r junge Bodenbildungen, die oftmals durch menschliche Eingriffe ausgel{\"o}st wurden. In dem Beitrag werden neben den j{\"u}ngsten Bodenentwicklungen auf Bergbaufolgestandorten auch j{\"u}ngere B{\"o}den auf seit dem Mittelalter mit Flugsanden {\"u}berdeckten Standorten vorgestellt. Obwohl die Genese der auf diesen Flugsanddecken anzutreffenden B{\"o}den bereits seit bis zu 1 000 Jahre andauert, sind hier erst B{\"o}den der Klasse der Ah/C-B{\"o}den entwickelt. Auf den Bergbaufolgestandorten wird versucht, die Bodenbildung durch spezielle Meliorationsmaßnahmen zu f{\"o}rdern. Untersuchungen an diesen besonders jungen B{\"o}den lassen gut die Prozesse der initialen Bodenentwicklung erkennen.}, language = {de} } @misc{GerwinRaabBiemeltetal., author = {Gerwin, Werner and Raab, Thomas and Biemelt, Detlef and Bens, Oliver and H{\"u}ttl, Reinhard F.}, title = {The artificial water catchment "Chicken Creek" as an observatory for critical zone processes and structures}, series = {Hydrology and Earth System Sciences}, volume = {6}, journal = {Hydrology and Earth System Sciences}, number = {2}, issn = {1812-2116}, doi = {10.5194/hessd-6-1769-2009}, pages = {1769 -- 1795}, language = {en} }