TY - CHAP A1 - Nicolay, Alexander A1 - Raab, Alexandra A1 - Raab, Thomas T1 - Evidence of (pre-) historic to modern landscape development and land use history in Lower Lusatia (Brandenburg, Germany) T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - In the apron of three active lignite opencast pits in Lower Lusatia (Brandenburg, Germany), archaeological survey trenches were investigated in areas where Quaternary aeolian sand deposits are widespread. The investigated palaeoenvironmental archives in Jänschwalde, Cottbus-Nord and Welzow contain evidence of fluvial and aeolian morphodynamics, soil formation and agricultural land use from (pre-)historic to modern times. To study the age and the causes of sand drifting and landform stabilization, standard soil physical and chemical laboratory analyses as well as optically stimulated luminescence (OSL) and radiocarbon dating (14C) were carried out. Two main sedimentological units were identified: Unit 1 consists of glacio-fluvial and Late Weichselian aeolian sands representing the parent material for the native Podsol-Braunerde and Podsol development, while Unit 2 represents the Late Holocene aeolian deposits. Four periods of Late glacial and Holocene aeolian activity and three phases of geomorphological stability have been identified: (i) Aeolian sedimentation during the Late glacial, (ii) Mesolithic reactivation of aeolian processes, (iii) soil formation until Late Roman Iron Age settlers intensified the agricultural land use, (iv) intensive drift sand formation during the High Middle Ages due to agricultural expansion, (v) stabilization of the drift sands and weak soil formation, (vi) reactivation of aeolian processes due to the increasing wood consumption and charcoal production from the early 16th until the mid-19th century, (vii) surface stabilization and formation of Regosols since the mid-19th century due to afforestation. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-3404-1.pdf N1 - EGU2014-3404-1 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Raab, Thomas A1 - Raab, Alexandra A1 - Nicolay, Alexander A1 - Takla, Melanie A1 - Hirsch, Florian A1 - Schneider, Anna A1 - Rösler, Horst A1 - Bönisch, Eberhard T1 - Human-induced landscape dynamics in South Brandenburg - findings from different geoarchives T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - South Brandenburg is the central part of the North European Lowland (NEL) extending as a plain landscape from the North and Baltic Sea to the foothills of the Central European Highlands and reaching from the Netherlands to Poland. Since many decades lignite opencast mines have been operating in this region which is known as the Lusatian mining district. The total land demand in Lusatia is about 852 square kilometres and mining will continue for many more years or even decades. Large-scale outcrops resulting from these mining activities are excellent archives to study the younger Earth’s history. The scope of our research in open cast mines is to reconstruct the Late Quaternary landscape development and to distinguishing natural from anthropogenic forcing and processes. In more detail, the aims are to identify and to quantify the impact of past land uses, i.e. changes of vegetation, landforms and soils induced by agriculture and/or forestry. Here, we are presenting latest results from our research and review important findings giving novel insights into man-induced environmental changes in Lusatia within the past thousands years and thus improving the general understanding of Late Quaternary landscape dynamics. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-1852-1.pdf N1 - EGU2014-1852-1 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Hirsch, Florian A1 - Nicolay, Alexander A1 - Pötzsch, Bastian A1 - Fritzsche, Marie A1 - Raab, Alexandra A1 - Raab, Thomas T1 - Influence of charcoal burning induced pyrolysis on soils T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - In Lusatia, Northeastern Germany, the production of ironware between the 16th and 19th century left behind a remarkable amount of charcoal kilns in the forests north of Cottbus. Remote sensing surveys, underpinned by archaeological studies, show that charcoal was gained around Cottbus from several thousand charcoal kilns which had internal diameters up to 20 m. For the study site with 35 km2 area, the until now prospected total ground area below the charcoal kilns which was potentially affected by the pyrolysis is about 0,5 km2. Historic data indicates that the pyrolysis in the charcoal kiln took up to several weeks, for the kilns with a diameter of 20 m about 20 days. To characterize the depth of thermal alteration of soils below the kiln our current focus is on the differentiation of the iron hydroxides by small-scale vertical analysis of soil profiles. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-2557.pdf N1 - EGU2014-2557 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Raab, Alexandra A1 - Frantiuc, Alexandru A1 - Brademann, Brian A1 - Ott, Florian A1 - Hirsch, Florian A1 - Brauer, Achim A1 - Raab, Thomas T1 - Proxies of pre-industrial charcoal production and land use in lake sediments from South Brandenburg, Germany T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - During the last decades, archaeological research has revealed that large-scale charcoal burning was carried out in Lower Lusatia (South Brandenburg) situated within the North Germany Lowland. From the 17th to the 19th century, charcoal was mainly produced for the ironwork in Peitz. Within the framework of the ICLEA project lake sediments from two lakes, Byhleguhrer See and Großsee, are investigated to study the impact of pre-industrial charcoal production on the environment. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-3278.pdf N1 - EGU2014-3278 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Nicolay, Alexander A1 - Schulz, Deborah A1 - Raab, Thomas A1 - Raab, Alexandra T1 - Landscape and soil development in Lower Lusatia - results from archaeological and soil-geomorphological investigations on a small dune field nearby Jänschwalde (Brandenburg, Germany) T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - Within the apron of the opencast mine Jänschwalde (SE Brandenburg, Germany) archaeological excavations on a multiple populated small dune were complemented with soil-geomorphological investigations in the vicinity. Archaeological findings in the dune stratigraphy (especially cremation graves) are intercalated within aeolian sediments and/or buried soils and thus give a record of the Late Quaternary geomorphodynamic and soil development. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-3426.pdf N1 - EGU2014-3426 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Gerwin, Werner A1 - Raab, Thomas A1 - Seifert, Thomas T1 - Analyzing initial geomorphologic processes and structures: An alternative remote sensing approach T2 - EGU General Assembly 2010, held in Vienna, Austria, 02 – 07 May 2010 Y1 - 2010 N1 - EGU2010-11367 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Hirsch, Florian A1 - Bonhage, Alexander A1 - Bauriegel, Albrecht A1 - Schneider, Anna A1 - Raab, Thomas A1 - Raab, Alexandra A1 - Gypser, Stella T1 - The occurrence, soil parameters and genesis of rubified soils (‘Fuchserden’) of northeastern Germany T2 - Catena Y1 - 2019 U6 - https://doi.org/10.1016/j.catena.2018.11.039 SN - 0008-7769 SN - 1872-6887 VL - 175 SP - 77 EP - 92 ER - TY - GEN A1 - Spröte, Roland A1 - Fischer, Thomas A1 - Veste, Maik A1 - Raab, Thomas A1 - Wiehe, Wolfgang A1 - Lange, Philipp A1 - Bens, Oliver A1 - Hüttl, Reinhard F. T1 - Biological topsoil crusts at early successional stages on Quaternary substrates dumped by mining in Brandenburg, NE Germany T2 - Geomorphologie: relief, processus, environnement N2 - The influence of biological soil crusts in natural ecosystems on structures and processes is well investigated. However, in South-Brandenburg (Germany), it is possible to study the development of biological soil crusts (BSC) during initial ecosystem genesis on two artificial water catchments with well-known ages and under differing starting conditions. The two experimental sites are located in the recultivation area of the lignite open-cast mining district of southern Brandenburg with a distance of approximately 1 km between them. Two different topographies were constructed at the experimental sites: the experimental plot at the catchment Neuer Lugteich was shaped like a dune, whereas the artificial water catchment Hühnerwasser was modelled as an inclined slope. The catchment Neuer Lugteich is four years older than Hühnerwasser. The original substrate at Neuer Lugteich is more sandy and carbonate-free compared to the original substrate dumped at Hühnerwasser. At both sites geomorphological differentiation and crust development were compared and the importance of substrate-dependent water availability and crust type clarified. Once settled, the crusts influenced the water regime of the soils by delaying infiltration through enhanced water repellency, and by limiting water infiltration. Chlorophyll analysis revealed that all crusts were at early stages of development. At Neuer Lugteich, the establishment of the biological soil crusts was closely associated with the vegetation succession, whereas no clear succession of the crusts could be observed at Hühnerwasser. The mosaic-like pattern of the biological soils crusts is associated with the distribution of fine-grained material here.zeige weniger Y1 - 2010 UR - http://geomorphologie.revues.org/8083 U6 - https://doi.org/10.4000/geomorphologie.8083 SN - 1957-777X VL - 16 IS - 4 SP - 359 EP - 370 ER - TY - GEN A1 - Hirsch, Florian A1 - Spröte, Roland A1 - Fischer, Thomas A1 - Forman, Steven L. A1 - Raab, Thomas A1 - Bens, Oliver A1 - Hüttl, Reinhard F. T1 - Late Quaternary aeloian dynamics, pedostratigraphy and soil formation in the North European Lowlands - new findings from the Baruther ice-marginal valley T2 - Die Erde N2 - The formation of dunes in central Europe reflects ample sediment supply during the last deglacial hemicycle. A Quaternary inland dune complex in southern Brandenburg, Germany, was studied to frame the duration of pedogenesis in two outcrops containing buried paleosols. An integrative approach, which combined geomorphological, sedimentological, pedological and chronological methods was used to identify aeolian deposition events, ensuing pedogenesis and anthropogenic remobilization. At the outcrops, which were situated approximately 2 km apart from each other, a total of twelve samples of the aeolian sands were dated using optically stimulated luminescence (OSL) and a further six samples using 14C dating. Although the dunes have similar morphological features, these forms have a different history of aeolian sand deposition and pedogenesis. At the older dune (Gl 1) the surface soil is a well developed Podzol, whereas soil development of the younger dune (Gl 2) is clearly in an initial state. The studied sites of the dune complex also differ in grain size distribution and in the presence of buried soils, thereby indicating a climatic impact on aeolian remobilization. Y1 - 2017 U6 - https://doi.org/10.12854/erde-148-30 SN - 0013-9998 VL - 148 IS - 1 SP - 58 EP - 73 ER - TY - CHAP A1 - Spröte, Roland A1 - Fischer, Thomas A1 - Veste, Maik A1 - Lange, Philipp A1 - Bens, Oliver A1 - Raab, Thomas A1 - Hüttl, Reinhard F. T1 - Hydrophobicity in sandy soils triggered by the development of Scots Pine stands in southern Brandenburg, Germany T2 - EGU General Assembly 2010, held in Vienna, Austria, 02 – 07 May 2010 Y1 - 2010 UR - http://meetingorganizer.copernicus.org/EGU2010/EGU2010-4154.pdf N1 - EGU2010-4154 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Fischer, Thomas A1 - Spröte, Roland A1 - Veste, Maik A1 - Wiehe, Wolfgang A1 - Lange, Philipp A1 - Bens, Oliver A1 - Raab, Thomas A1 - Hüttl, Reinhard F. T1 - Functions of biological soil crusts on central European inland dunes:Water repellency and pore clogging influence water infiltration T2 - EGU General Assembly 2010, held in Vienna, Austria, 02 – 07 May 2010 Y1 - 2010 UR - http://meetingorganizer.copernicus.org/EGU2010/EGU2010-4449.pdf N1 - EGU2010-4449 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Dimitrova, Tsvetelina A1 - Repmann, Frank A1 - Freese, Dirk T1 - Degradation of ferrocyanide by natural isolated bacteria T2 - International Journal of Phytoremediation N2 - This study aims at investigating the iron cyanide (CN) degradation potential of two natural bacterial isolates with the purpose of their application in iron CN phytoremediation. The strains were isolated from contaminated soil and incubated over 4 months with 50mg L⁻¹CN (as ferrocyanide) as the sole iron and nitrogen source. Unlike previous reports, the study provides control for bacterial growth, biotic and abiotic CN losses. Bacterial growth, CN, ammonium, and nitrate concentrations were monitored regularly. Both strains grew less rapid with iron CN compared with the positive control. However, the growth was diauxic. The CN concentration in the media decreased with 20% and 25% respectively, while that in the sterile controls remained stable. Ammonium was detected in the media of both strains implying that a fraction of the initially applied ferrocyanide has been converted. The nitrogen lost from the system evened out with that in the cells at the end of the experiments. These results showed that the investigated strains were undoubtedly able to grow on iron CN as an alternative nitrogen source, but contrary to some previous findings, the iron CN utilization is much slower and takes place only after complete exhaustion of the cellular nitrogen reserves. Y1 - 2019 U6 - https://doi.org/10.1080/15226514.2019.1633996 SN - 1549-7879 SN - 1522-6514 VL - 22 IS - 1 SP - 20 EP - 28 ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Fischer, Thomas A1 - Repmann, Frank A1 - Raab, Thomas A1 - Dimitrova, Tsvetelina T1 - Feasibility of field portable near infrared (NIR) spectroscopy to determine cyanide concentrations in soil T2 - Water, Air and Soil Pollution N2 - Vicinities of manufactured gas plants were often contaminated with solid iron–cyanide complexes as a result of the coal gasification process. During the remediation of affected soils, knowledge about contaminant concentrations is crucial, but laboratory methods are often expensive and time consuming. Rapid and non-destructive field methods for contaminant determination permit an analysis of large sample numbers and hence, facilitate identification of ‘hot spots’ of contamination. Diffuse near infrared reflectance spectroscopy has proven to be a reliable analytical tool in soil investigation. In order to determine the feasibility of a Polychromix Handheld Field Portable Near-Infrared Analyzer (FP NIR), various sample preparation methods were examined, including homogenizing, sieving, drying, and grinding. Partial least squares calibration models were developed to determine near infrared (NIR) spectral responses to the cyanide concentration in the soil samples. As a control, the contaminant concentration was determined using conventional flow injection analysis. The experiments revealed that portable near-infrared spectrometers could be a reliable device for detecting cyanide concentrations >2,400 mgkg−1 in the field and >1,750 mgkg−1 after sample preparation in the laboratory.We found that portable NIR spectrometry cannot replace traditional laboratory analyses due to high limits of detection, but that it could be used for identification of contamination ‘hot spots’. Y1 - 2012 U6 - https://doi.org/10.1007/s11270-012-1298-y SN - 1573-2932 VL - 223 IS - 8 SP - 5495 EP - 5504 ER - TY - GEN A1 - Gerwin, Werner A1 - Repmann, Frank A1 - Schaaf, Wolfgang A1 - Raab, Thomas T1 - Bodenveränderungen durch Waldbrände – Stoffvorräte und Stoffverlagerungen T2 - Jahrestagung der DBG 2022 "Grenzen überwinden, Skalen überschreiten" 5. - 8. September 2022 in Trier N2 - Die zurückliegenden trocken-heißen Sommer haben im Süden Brandenburgs zu zahlreichen Bränden in den dominierenden Kiefernwäldern geführt, einige davon mit katastrophalen Ausmaßen. Dazu gehören die extremen Brandereignisse 2018 bei Treuenbrietzen sowie 2019 bei Jüterbog und Lieberose, die zusammen weit über 1000 ha Waldfläche zerstört und dabei auch Veränderungen der betroffenen Waldböden verursacht haben. Das seit Mai 2020 von der FNR geförderte Verbundvorhaben Pyrophob befasst sich mit den Auswirkungen von Waldbränden im Süden Brandenburgs auf die Waldökosysteme und mit waldbaulichen Maßnahmen, die mittelfristig zu einer Verringerung der Brandanfälligkeit der Wälder beitragen sollen. Im Rahmen des auf eine fünfjährige Laufzeit ausgelegten Verbundvorhabens finden bodenkundliche Untersuchungen auf zwölf Versuchsflächen bei Treuenbrietzen und Jüterbog statt. An beiden Standorten werden unverbrannte Referenzflächen mit einbezogen. Ergänzend konnten bei Lieberose bereits 2019 nur kurz nach dem Brandgeschehen erste Bodenuntersuchungen durchgeführt werden. Die untersuchten Brandflächen bei Jüterbog und Lieberose sind als Totalreservate ausgewiesen, auf denen auch nach dem Brand waldbauliche Maßnahmen vollständig unterbleiben. Auf den Flächen bei Treuenbrietzen wurden verschiedene Behandlungsvarianten durchgeführt, zu denen auf einem Teil der Flächen die vollständige Entfernung der abgestorbenen Bäume gehörte, während auf anderen Teilflächen Totholz auf der Fläche verblieb. Ziel der bodenkundlichen Arbeiten in Pyrophob ist zum einen eine Charakterisierung der direkten Auswirkungen des Brandes auf Humus und Mineralboden hinsichtlich des Stoffbestandes und bodenbiologischer Prozesse. Zum anderen wird der Stoffaustrag aus dem Oberboden erfasst. Der etwaige Einfluss der unterschiedlichen waldbaulichen Vorgehensweise auf die Bodenverhältnisse wird dabei als ein Indikator für die Auswahl geeigneter Maßnahmen berücksichtigt. In den verschiedenen Untersuchungsvarianten des Vorhabens wurden zu diesem Zweck Humus- und Mineralbodenprofile untersucht. Zudem wurden Mischproben aus dem Ober- und Unterboden entnommen und auf ihren Stoffhaushalt hin analysiert. Auf jeder Untersuchungsfläche wurden je drei frei dränende Kleinlysimeter in 10 cm Bodentiefe installiert, um die zeitlichen Veränderungen der Sickerwasserzusammensetzung und die durch den Brand initiierten Stoffausträge aus dem Oberboden zu quantifizieren. Ergänzend finden Untersuchungen zu möglichen Auswirkungen der Brände auf bodenbiologische Prozesse wie Streuabbau und Stickstoffmineralisation statt. Y1 - 2022 UR - https://www.dbges.de/de/system/files/Trier2022/programmheft-dbg_2022_ou_17052022_lores.pdf SP - 48 ER - TY - GEN A1 - Gypser, Stella A1 - Hirsch, Florian A1 - Schleicher, Anja M. A1 - Freese, Dirk T1 - Impact of crystalline and amorphous iron- and aluminum hydroxides on mechanisms of phosphate adsorption and desorption T2 - Journal of Environmental Sciences Y1 - 2018 U6 - https://doi.org/10.1016/j.jes.2017.12.001 VL - 70 SP - 175 EP - 189 ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Repmann, Frank A1 - Raab, Thomas T1 - Stability of Prussian Blue in Soils of a Former Manufactured Gas Plant Site T2 - Soil and Sediment Contamination N2 - Soil contamination with iron-cyanide complexes is a common problem at former manufactured gas plant (MGP) sites. Dissolution of the cyanide, from Prussian Blue (ferric ferrocyanide), creates an environmental hazard, whereas the risk of groundwater contamination depends on the stability of dissolved iron–cyanide complexes. Lack of a standard leaching method to determine the water-soluble (plant-available) cyanide fraction generates potential limitations for implementing remediation strategies like phytoremediation. Applicability of neutral solution extraction to determine the water-soluble cyanide fraction and the stability of Prussian Blue in surface and near-surface soils of an MGP site in Cottbus, undersaturated and unsaturated water conditions, was studied in column leaching and batch extraction experiments. MGP soils used in the long-term tests varied according to the pH (5.0–7.7) and the total cyanide content (40–1718 mg kg−1). Column leaching, after four months of percolation, still yielded effluent concentrations exceeding the German drinking water limit (> 50 μg L−1) and the solubility of Prussian Blue reported in the literature (< 1 mg L−1) from both alkaline and acidic soils. Long-term (1344 h) extraction of MGP soils with distilled water was sufficient to dissolve 97% of the total cyanide from the slightly alkaline soils and up to 78% from the acidic soils. Both experiments revealed that dissolution of ferric ferrocyanide under circum-neutral pH and oxic water conditions is a function of time, where the released amount is dependent on the soil pH and total cyanide content. Unexpectedly high and continuous solubility of Prussian Blue, both in acidic and slightly alkaline MGP soils, implies the need to introduce an additional cyanide fraction (“readily soluble fraction”) to improve and specify cyanide leaching methods. Long-term extraction of cyanide-contaminated soil in neutral solution seems to be a promising approach to evaluate the potential hazard of groundwater pollution at the MGP sites. Y1 - 2014 U6 - https://doi.org/10.1080/15320383.2014.839626 SN - 1549-7887 VL - 23 IS - 5 SP - 504 EP - 522 ER - TY - CHAP A1 - Sut-Lohmann, Magdalena A1 - Boldt-Burisch, Katja A1 - Raab, Thomas T1 - Effect of ryegrass (Lolium perenne L.) roots inoculation using different arbuscular mycorrhizal fungi (AMF) species on sorption of iron-cyanide (Fe-CN) complexes T2 - European Geosciences Union, General Assembly 2016, Vienna, Austria, 17 April – 22 May 2016 N2 - Soils and groundwater on sites of the former Manufactured Gas Plants (MGPs) are contaminated with various complex iron-cyanides (Fe-CN). Phytoremediation is a promising tool in stabilization and remediation of Fe-CN affected soils, however, it can be a challenging task due to extreme adverse and toxic conditions. Phytoremediation may be enhanced via rhizosphere microbial activity, which can cooperate on the degradation, transformation and uptake of the contaminants. Recently, increasing number of scientist reports improved plants performance in the removal of toxic compounds with the support of arbuscular mycorrhizae fungi (AMF). Series of batch experiments using potassium hexacyanoferrate (II) solutions, in varying concentrations, were used to study the effect of ryegrass roots (Lolium perenne L.) inoculation with Rhizophagus irregularis and a mixture of Rhizophagus irregularis, Funneliformis mosseae, Rhizophagus aggregatus, and Claroideoglomus etunicatum on Fe-CN sorption. Results indicated significantly higher colonization of R. irregularis than for the mixture of AMF species on ryegrass roots. Sorption experiments revealed significantly higher reduction of total CN and free CN content in the mycorrhizal roots, indicating greater cyanide decrease in the treatment inoculated with R. irregularis. Our study indicates contribution of AM fungi in phytoremediation of Fe-CN contaminated soil. Y1 - 2016 UR - http://meetingorganizer.copernicus.org/EGU2016/EGU2016-4223-2.pdf N1 - EGU2016-4223-2 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Repmann, Frank A1 - Raab, Thomas T1 - Retardation of iron-cyanide complexes in the soil of a former manufactured gas plant site T2 - Journal of Environmental Science and Health, Part A N2 - The soil in the vicinities of former Manufactured Gas Plant (MGP) sites is commonly contaminated with iron-cyanide complexes (ferric ferrocyanide). The phenomenon of cyanide mobility in soil, according to the literature, is mainly governed by the dissolution and precipitation of ferric ferrocyanide, which is only slightly soluble (<1 mg L¡1) under acidic conditions. In this paper, retention properties of the sandy loam soil and the potential vertical movement of the solid iron-cyanide complexes, co-existing with the dissolution, sorption and precipitation reactions were investigated. Preliminary research conducted on a former MGP site implied colloidal transport of ferric ferricyanide from the initial deposition in the wastes layer towards the sandy loam material (secondary accumulation), which possibly retarded the mobility of cyanide (CN). A series of batch and column experiments were applied in order to investigate the retardation of iron-cyanide complexes by the sandy loam soil. Batch experiments revealed that in circumneutral pH conditions sandy loam material decreases the potassium ferro- and ferricyanide concentration. In column experiments a minor reduction in CN concentration was observed prior to addition of iron sulfide (FeS) layer, which induced the formation of the Prussian blue colloids in circumneutral pH conditions. Precipitated solid iron-cyanide complexes were mechanically filtered by the coherent structure of the investigated soil. Additionally, the reduction of the CN concentration of the percolation solutions by the sandy loam soil was presumably induced due to the formation of potassium manganese iron-cyanide (K2Mn[Fe(CN)6]). Y1 - 2015 U6 - https://doi.org/10.1080/10934529.2015.981116 SN - 1532-4117 SN - 1093-4529 VL - 50 IS - 3 SP - 282 EP - 291 ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Boldt-Burisch, Katja A1 - Raab, Thomas T1 - Possible evidence for contribution of arbuscular mycorrhizal fungi (AMF) in phytoremediation of iron–cyanide (Fe–CN) complexes T2 - Ecotoxicology N2 - Arbuscular mycorrhizal fungi (AMF) are integral functioning parts of plant root systems and are widely recognized for enhancing contaminants uptake and metabolism on severely disturbed sites. However, the patterns of their influence on the phytoremediation of iron–cyanide (Fe–CN) complexes are unknown. Fe–CN complexes are of great common interest, as iron is one of the most abundant element in soil and water. Effect of ryegrass (Lolium perenne L.) roots inoculation, using mycorrhizal fungi (Rhizophagus irregularis and a mixture of R. irregularis, Funneliformis mosseae, Rhizophagus aggregatus, and Claroideoglomus etunicatum), on iron–cyanide sorption was studied. Results indicated significantly higher colonization of R. irregularis than the mixture of AMF species on ryegrass roots. Series of batch experiments using potassium hexacyanoferrate (II) solutions, in varying concentrations revealed significantly higher reduction of total CN and free CN content in the mycorrhizal roots, indicating greater cyanide decrease in the treatment inoculated with R. irregularis. Our study is a first indication of the possible positive contribution of AM fungi on the phytoremediation of iron–cyanide complexes. Y1 - 2016 UR - http://link.springer.com/article/10.1007%2Fs10646-016-1678-y U6 - https://doi.org/10.1007/s10646-016-1678-y SN - 1573-3017 VL - 25 IS - 6 SP - 1260 EP - 1269 ER - TY - GEN A1 - Dimitrova, Tsvetelina A1 - Repmann, Frank A1 - Raab, Thomas A1 - Freese, Dirk T1 - Uptake of ferrocyanide in willow and poplar trees in a long term greenhouse experiment T2 - Ecotoxicology N2 - Phytoremediation of sites contaminated with iron cyanides can be performed using poplar and willow trees. Poplar and willow trees were grown in potting substrate spiked with ferrocyanide concentrations of up to 2,000 mg kg-1 for 4 and 8 weeks respectively. Soil solution and leaf tissue of different age were sampled for total cyanide analysis every week. Chlorophyll content in the leaves was determined to quantify cyanide toxicity. Results showed that cyanide in the soil solution of spiked soils differed between treatments and on weekly basis and ranged from 0.5 to 1,200 mg l-1. The maximum cyanide content in willow and poplar leaves was 518 mg kg-1 fresh weight (FW) and 148 mg kg-1 FW respectively. Cyanide accumulated in the leaves increased linearly with increasing cyanide concentration in the soil solution. On the long term, significantly more cyanide was accumulated in old leaf tissue than in young tissue. Chlorophyll content in poplar decreased linearly with increasing cyanide in the soil solution and in leaf tissue, and over time. The inhibitory concentration (IC50) value for poplars after 4 weeks of exposure was 173 mg l-1 and for willow after 8 weeks of exposure—768 mg l-1. Results show that willows tolerate much more cyanide and over a longer period than poplars, making them very appropriate for remediating sites highly contaminated with iron cyanides. Y1 - 2015 U6 - https://doi.org/10.1007/s10646-014-1398-0 SN - 1573-3017 VL - 24 IS - 3 SP - 510 ER - TY - CHAP A1 - Kappler, Christoph A1 - Kaiser, Knut A1 - Ganzenmüller, Raphael A1 - Küster, Mathias A1 - Nicolay, Alexander A1 - Fülling, Alexander A1 - Bens, Oliver A1 - Raab, Thomas ED - Schwab, Markus J. ED - Theuerkauf, Martin ED - Brauer, Achim ED - Wilmking, Martin ED - Lampe, Reinhard T1 - A review of geochronological data from northeastern Germany: evaluating late Quaternary soil formation and land surface dynamics T2 - 3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age Y1 - 2014 U6 - https://doi.org/10.2312/GFZ.b103-14028 SP - 43 PB - GFZ German Research Centre for Geosciences CY - Potsdam ER - TY - CHAP A1 - Sut-Lohmann, Magdalena A1 - Boldt-Burisch, Katja A1 - Raab, Thomas T1 - Influence of Arbuscular Mycorrhizal Fungus (AMF) on degradation of iron-cyanide complexes T2 - European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015 KW - arbuscular mycorrhizal fungus Y1 - 2015 UR - http://meetingorganizer.copernicus.org/EGU2015/EGU2015-250.pdf N1 - EGU2015-250 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Sut-Lohmann, Magdalena A1 - Repmann, Frank A1 - Raab, Thomas T1 - Vertical movement of iron-cyanide complexes in soils of a former Manufactured Gas Plant site T2 - European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015 Y1 - 2015 UR - http://meetingorganizer.copernicus.org/EGU2015/EGU2015-9980.pdf N1 - EGU2015-9980 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Mykhailova, Larysa A1 - Raab, Thomas A1 - Gypser, Stella A1 - Fischer, Thomas T1 - Development and hydrology of biological soil crusts -- first results from a surface inoculation experiment T2 - European Geosciences Union, General Assembly 2016, Vienna, Austria, 17 April – 22 May 2016 Y1 - 2016 N1 - EGU2016-6129 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Fischer, Thomas A1 - Repmann, Frank A1 - Raab, Thomas T1 - Long-Term Release of Iron-Cyanide Complexes from the Soil of a Manufactured Gas Plant Site T2 - Journal of Environmental Protection N2 - Iron-cyanide (Fe-CN) complexes have been detected at Manufactured Gas Plant sites (MGP) worldwide. The risk of groundwater contamination depends mainly on the dissolution of ferric ferrocyanide. In order to design effective reme- diation strategies, it is relevant to understand the contaminant’s fate and transport in soil, and to quantify and mathe- matically model a release rate. The release of iron-cyanide complexes from four contaminated soils, originating from the former MGP in Cottbus, has been studied by using a column experiment. Results indicated that long-term cyanide (CN) release is governed by two phases: one readily dissolved and one strongly fixed. Different isotherm and kinetic equations were used to investigate the driving mechanisms for the ferric ferrocyanide release. Applying the isotherm equations assumed an approach by which two phases were separate in time, whereas the multiple first order equation considered simultaneous occurrence of both cyanide pools. Results indicated varying CN release rates according to the phase and soil. According to isotherm and kinetic models, the long-term iron cyanide release from the MGP soils is a complex phenomenon driven by various mechanisms parallely involving desorption, diffusion and transport processes. Phase I (rapid release) is presumably mainly constrained by the transport process of readily dissolved iron-cyanide complexes combined with desorption of CN bound to reactive heterogeneous surfaces that are in direct contact with the aqueous phase (outer-sphere complexation). Phase II (limited rate) is presumably driven by the diffusion controlled processes involving dissolution of precipitated ferric ferrocyanide from the mineral or inner-sphere complexation of fer- ricyanides. CN release rates in phase I and II were mainly influenced by the pH, organic matter (OM) and the total CN content. The cyanide release rates increased with increasing pH, decreased with low initial CN concentration and were retarded by the increase in OM content. Y1 - 2013 U6 - https://doi.org/10.4236/jep.2013.411A2002 SN - 2152-2219 VL - 4 IS - 11B SP - 8 EP - 19 ER - TY - CHAP A1 - Sut-Lohmann, Magdalena A1 - Repmann, Frank A1 - Raab, Thomas T1 - Release of iron-cyanide complexes form contaminated soils - Batch and column experiments on substrates from Manufactured Gas Plant (MGP) site T2 - European Geosciences Union General Assembly 2013, Vienna, Austria, 07 – 12 April 2013 N2 - Soils of former Manufactured Gas Plants (MGPs) are often contaminated with iron-cyanide (Fe-CN) complexes that originate from gas purification process. Cyanide is a potentially toxic substance and its presence in soil and groundwater may cause risk for human health as well as for the environment. MGPs were commonly built on the city suburban areas, which have spread ever since. Nowadays, these sites are typically located in inner cities, causing environmental thread, due to the leaching of pollutants. More recently, columns and batch experiments have been used to study fate and mobility of contaminants is soil. The release of iron-cyanide complexes under unsaturated flow conditions was evaluated with eight columns of 30 cm length and a diameter of 5,4 cm. Cyanide concentrations in the collected leachates were measured with Flow Injection Analysis (FIA). Additionally pH, electrical conductivity (EC) and various ion concentrations were determined. In order to compare the release of Fe-CN complexes in saturated conditions a batch experiment was conducted, where in defined time intervals, 1 ml of the extract water phase was analyzed for CN concentration. Study revealed an analogous trend of cyanide release in both experiments indicating primarily the release of formerly dissolved phase (hexacyanoferrates) followed by continual dissolution of ferric ferrocyanide. We conclude that batch experiments, conducted prior to column analysis, can serve as preliminary prediction of the water soluble cyanide fraction under unsaturated conditions. Y1 - 2013 UR - http://meetingorganizer.copernicus.org/EGU2013/EGU2013-1983.pdf N1 - EGU2013-1983 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Sut-Lohmann, Magdalena A1 - Fischer, Thomas A1 - Repmann, Frank A1 - Raab, Thomas T1 - Feasibility of field portable near infrared (NIR) spectroscopy to determine cyanide concentrations in soil T2 - European Geosciences Union, General Assembly 2013, Vienna, Austria, 07 – 12 April 2013 N2 - In Germany, at more than 1000 sites, soil is polluted with an anthropogenic contaminant in form of iron-cyanide complexes. These contaminations are caused by former Manufactured Gas Plants (MGPs), where electricity for lighting was produced in the process of coal gasification. The production of manufactured gas was restrained in 1950, which caused cessation of MGPs. Our study describes the application of Polychromix Handheld Field Portable Near-Infrared (NIR) Analyzer to predict the cyanide concentrations in soil. In recent times, when the soil remediation is of major importance, there is a need to develop rapid and non-destructive methods for contaminant determination in the field. In situ analysis enables determination of ‘hot spots’, is cheap and time saving in comparison to laboratory methods. This paper presents a novel usage of NIR spectroscopy, where a calibration model was developed, using multivariate calibration algorithms, in order to determine NIR spectral response to the cyanide concentration in soil samples. As a control, the contaminant concentration was determined using conventional Flow Injection Analysis (FIA). The experiments revealed that portable near-infrared spectrometers could be a reliable device for identification of contamination ‘hot spots’, where cyanide concentration are higher than 2400 mg kg-1 in the field and >1750 mg kg-1 after sample preparation in the laboratory, but cannot replace traditional laboratory analyses due to high limits of detection. Y1 - 2013 UR - http://meetingorganizer.copernicus.org/EGU2013/EGU2013-1986.pdf N1 - EGU2013-1986 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Rodionov, Andrei A1 - Nii-Annang, Seth A1 - Fischer, Thomas A1 - Gattinger, Andreas A1 - Bens, Oliver A1 - Raab, Thomas A1 - Hüttl, Reinhard F. T1 - Cross-linked polyacrylates in post-mining substrates: persistence and effects on plant growth T2 - Soil Use and Management N2 - Application of hydrophilic polymers composed of cross-linked polyacrylate can improve soil water-holding capacity and accelerate the restoration of post-mining substrates. In this work, we studied the persistence of a polyacrylate polymer incorporated into a soil and its impact on plant nutrients at a reclamation site of former lignite mining in Lusatia (Germany). In contrast to autumn application, the incorporation of the polymer enhanced the sequestration of plant-derived carbon in the soil, which was reflected by a significant increase in the concentration of a lignin marker. Attenuated total reflexion–Fourier transform infrared spectra (ATR-FTIR) and total elemental contents in the applied polymer suggested an intensive cation exchange between the polymer framework and the soil-forming substrate. In addition, there was an enrichment of carbonaceous material, which seems to reduce the swelling and thus the water-holding capacity of the cross-linked polyacrylate. Conversely, this process protected the polymer structure from rapid decomposition. Y1 - 2014 U6 - https://doi.org/10.1111/sum.12103 SN - 1475-2743 VL - 30 IS - 1 SP - 78 EP - 87 ER - TY - CHAP A1 - Hüttl, Reinhard F. A1 - Flühler, Hannes A1 - Gerke, Horst H. A1 - Maurer, Thomas A1 - Schneider, Anna ED - Hüttl, Reinhard F. ED - Kögel-Knabner, Ingrid ED - Schulin, Rainer ED - Gerwin, Werner T1 - Project C5 – Development of a structure and process model T2 - Structures and processes of the initial ecosystem development phase in an artificial water catchment (Final report CRC/TR 38) Y1 - 2013 UR - http://opus.kobv.de/btu/volltexte/2013/2865/ SP - 101 EP - 110 PB - BTU, Forschungszentrum Landschaftsentwicklung und Bergbaulandschaften (FZLB) CY - Cottbus ER - TY - GEN A1 - Rodionov, Andrei A1 - Nii-Annang, Seth A1 - Bens, Oliver A1 - Trimborn, Manfred A1 - Schillem, Steffi A1 - Schneider, Bernd Uwe A1 - Raab, Thomas A1 - Hüttl, Reinhard F. T1 - Impacts of Soil Additives on Crop Yield and C-Sequestration in Post Mine Substrates of Lusatia, Germany T2 - Pedosphere Y1 - 2012 SN - 1002-0160 VL - 22 IS - 3 SP - 343 EP - 350 ER - TY - CHAP A1 - Krümmelbein, Julia A1 - Zeihser, Uwe ED - Krümmelbein, Julia ED - Raab, Thomas ED - Hüttl, Reinhard F. T1 - Landwirtschaftliche Versuchsfläche Tagebau Jänschwalde - Versuchsdesign und Flächenherstellung T2 - Energieholzproduktion und bodenphysikalische Untersuchungen auf Rekultivierungsflächen des Niederlausitzer Braunkohlereviers Y1 - 2013 SN - 978-3-937728-12-4 SP - 3 EP - 15 PB - BTU CY - Cottbus ER - TY - GEN A1 - Raab, Alexandra A1 - Raab, Thomas A1 - Takla, Melanie A1 - Nicolay, Alexander A1 - Bönisch, Eberhard A1 - Rösler, H. T1 - Böden als Archive der Landschaftsgeschichte im Vorfeld des Tagebaus Jänschwalde T2 - Exkursionsführer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam Y1 - 2011 SP - 84 EP - 96 PB - Deutsche Bodenkundliche Gesellschaft CY - Oldenburg ER - TY - GEN ED - Raab, Thomas ED - Raab, Alexandra ED - Gerwin, Werner ED - Schopper, Franz T1 - Landschaftswandel - Landscape Change Y1 - 2013 PB - Chair of Geopedology and Landscape Development CY - Cottbus ER - TY - GEN A1 - Krümmelbein, Julia A1 - Horn, Rainer A1 - Raab, Thomas A1 - Bens, Oliver A1 - Hüttl, Reinhard F. T1 - Soil physical parameters of a recently established agricultural recultivation site after brown coal mining in Eastern Germany T2 - Soil & Tillage Research N2 - Our study deals with agricultural recultivation of open cast brown coal mining areas in Lusatia, Eastern Germany. In this region the largest brown coal (lignite) mining area of Germany is located. Lignite mining activities lead to major disturbances of the landscape. Recultivation efforts attempt to regenerate mining areas for agricultural land use options. The geological “parent” material is of saaleian origin, has a sandy texture and was excavated from several meters depths before mining and is now used for recultivating the excavated area. Consequently, it is free of recent soil organic carbon. The substrate itself is unstructured. The partly wet or dry substrate is subjected to strong mechanical stresses during the excavation, deposition, refilling and levelling processes throughout the year. This practice leads to more or less compacted soils/substrates which may result in small yields of agricultural crops. In this context we investigate the effect of different organic soil additives in combination with different recultivation crop rotations on the development of soil structure for improved agricultural land use. Our experimental site has been heaped up and levelled off in 2006 and 2007. On each of the 24 experimental sub areas undisturbed soil samples have been taken to characterise the substrates according to their mechanical and hydraulic parameters and to determine the scattering of these parameters on a site that is assumed to be recultivated as homogenously as possible. First results of our ongoing experimental study indicate that the soil physical properties such as texture, bulk density, precompression stress, air permeability and saturated hydraulic conductivity are not identical on each of the 24 subplots. The soil physical properties behave differently in relation to each other. E.g. we found a negative correlation between bulk density (∼1.35–∼1.90 g/cm3) and precompression stress (∼30–70 kPa) and no decisive interrelation between bulk density and air permeability or saturated hydraulic conductivity. Y1 - 2010 UR - http://www.sciencedirect.com/science/article/pii/S0167198710001443 U6 - https://doi.org/10.1016/j.still.2010.08.006 SN - 0167-1987 VL - 111 IS - 1 SP - 19 EP - 25 ER - TY - GEN A1 - Raab, Thomas A1 - Hürkamp, Kerstin A1 - Völkel, Jörg T1 - Stratigraphy and chronology of late Quaternary floodplain sediments in a historic mining area, Vils River Valley, East Bavaria, Germany T2 - Physical Geography N2 - Analysis of 288 percussion drillings from depths of up to seven meters and a 120 m long excavated section provide new and detailed information on the Late Quaternary to Late Holocene floodplain evolution from the most important Central European iron-mining region of the 15th century. The generalized sequence of the Vils River floodplain is built of five units representing facies of different genesis (rock/saprolite, gravel, sand, loam, peat) that are identified by physical, chemical, and mineralogical parameters (grain size, clast shape, and content, TOC, bulk mineralogy). Along the 87 km length of the valley, different units/facies are found at the Upper Vils River (UVR 1-5) and at the Lower Vils River (LVR 1-4b). In both river sections, fine-grained material (flood loam) forms the major part (up to 4 m) of the alluvial sequence. 29 age determinations (24 14C, 4 IRSL, 1 tree-ring analysis) show increasing accumulation of flood loam in the last millennium. The data correlate with the beginning of mining at the Vils River and hence suggest a causal connection with mining activities in the catchment—both on the slopes and in the floodplain—with intense deposition of flood loams. Y1 - 2010 UR - http://www.tandfonline.com/doi/abs/10.2747/0272-3646.31.4.357 U6 - https://doi.org/10.2747/0272-3646.31.4.357 SN - 1930-0557 SN - 0272-3646 VL - 31 IS - 4 SP - 357 EP - 384 ER - TY - GEN A1 - Schneider, Anna A1 - Gerke, Horst H. A1 - Maurer, Thomas T1 - 3D initial sediment distribution and quantification of mass balances of an artificially-created hydrological catchment based on DEMs from aerial photographs using GOCAD T2 - Physics and Chemistry of the Earth Y1 - 2011 UR - http://www.sciencedirect.com/science/article/pii/S1474706510000380 U6 - https://doi.org/10.1016/j.pce.2010.03.023 SN - 1474-7065 VL - 36 IS - 1-4 SP - 87 EP - 100 ER - TY - GEN A1 - Nii-Annang, Seth A1 - Rodionov, Andrei A1 - Raab, Thomas A1 - Bens, Oliver A1 - Hüttl, Reinhard F. A1 - Dilly, Oliver T1 - Impact of Commercial Soil Additives on Microbial Activity and Carbon Isotopic Characteristics of Recultivated Post Lignite Mine Soils T2 - Geomicrobiology Journal Y1 - 2011 SN - 1521-0529 VL - 28 IS - 7 SP - 567 EP - 573 ER - TY - GEN A1 - Heinken, Thilo A1 - Blumröder, Jeanette S. A1 - Adhikari, Yojana A1 - Balthasar, Cathrina A1 - Binder, Anja A1 - Birkhofer, Klaus A1 - Bischoff, Antje A1 - Brosinsky, Arlena A1 - Bubner, Ben A1 - Clerc, Danica A1 - Djoudi, El Aziz A1 - Dobkowitz, Sophia A1 - Francke, Till A1 - Gerwin, Werner A1 - Hartong, Heinrich A1 - Hess, Carsten A1 - Jarling, René A1 - Jouy, Florent A1 - Leinen, Loretta A1 - Meißner, Andreas A1 - Raab, Thomas A1 - Repmann, Frank A1 - Rönnefarth, Susanne A1 - Schaaf, Wolfgang A1 - Schirrmacher, Marina A1 - Schmehl, Marie-Therese A1 - Schmitt, Thomas A1 - Schröder, Jens A1 - Schüle, Maren A1 - Sturm, Knut A1 - Welle, Torsten A1 - Ibisch, Pierre L. T1 - PYROPHOB – A post-fire ecosystem research project to inform management for resilient forest development BT - PYROPHOB – Ein Ökosystemforschungsprojekt auf Waldbrandflächen als Grundlage für das Management einer resilienten Waldentwicklung T2 - Tuexenia N2 - PYROPHOB (fire-resistant) is the name of an interdisciplinary research project that is running for five years from 2020 to 2025. In this project, eight institutions are investigating the ecological effects of wildfires and subsequent forest management strategies in pine forests (plantations) in Brandenburg (NE Germany), with the aim of formulating practical recommendations for managing fire-prone forests and the effective restoration of post-fire forest areas. We provide a brief overview of what is known about the effects of wildfire on abiotic and biotic parameters in temperate pine forests, as well as the effects of silvicultural treatments. To date, we know little about how different components of biodiversity are linked in post-fire forest ecosystems and how management affects their functioning. By describing the project, we illustrate the requirements for the implementation of such an applied research project. We emphasize the importance of the study design for dealing with interdisciplinary questions and for the quantitative synthesis of research results. The project comprises a set of standardised field plots in two wildfire areas covering different post-fire management options. Fifteen study sites were established, including two reference sites in unburned pine stands, each with ten study plots as replicates. In situ nitrogen mineralisation, litter decomposition tests and soil biological activity are used for soil biological characterisation. Microclimate data is measured continuously. Standing and lying dead wood and tree regeneration are recorded as key indicators of the success of forestry treatments. Further methods com-prise terrestrial laser scanning, remote sensing techniques as well as surveys of vegetation and above and below ground biomass. Identification of fruiting body-forming fungi, phytoparasites and ectomycorrhizal fungi is supported by marker gene sequencing. Faunistic indicators comprise predatory soil arthropods (pairs of emergence tents and soil traps), saproxylic beetles (flight traps and funnel traps), moths (automated window traps), mammals (camera traps), and breeding birds (visual and acoustic observation). We discuss the strengths and limitations of the project design. We are able to systematically capture short-term temporal shifts in parameters and trends in post-fire ecosystem development. Research in a real landscape with ongoing environmental changes and interventions pres-ents challenges for experimental design, data analysis and interpretation. The drivers of ecosystem development are rarely completely independent or perfectly balanced, and lack of replication is ine-vitable. The two fires did not occur in the same year and season, resulting in different initial conditions for the colonisation of the burned areas. Finally, a large part of one study area was again affected by a fire in 2022, which destroyed direct comparability with the other sites. Despite these obstacles the project has started to generate valuable results to address management and conservation challenges. Y1 - 2024 U6 - https://doi.org/10.14471/2024.44.004 SN - 0722-494X SN - 2748-3452 VL - 44 ER - TY - GEN A1 - Schmehl, Marie-Therese A1 - Adhikari, Yojana A1 - Balthasar, Cathrina A1 - Binder, Anja A1 - Clerc, Danica A1 - Dobkowitz, Sophia A1 - Gerwin, Werner A1 - Günther, Kristin A1 - Hartong, Heinrich A1 - Heinken, Thilo A1 - Hess, Carsten A1 - Ibisch, Pierre L. A1 - Jouy, Florent A1 - Leinen, Loretta A1 - Raab, Thomas A1 - Repmann, Frank A1 - Rönnefarth, Susanne A1 - Rohlfs, Lilly A1 - Schirrmacher, Marina A1 - Schröder, Jens A1 - Schüle, Maren A1 - Vieth-Hillebrand, Andrea A1 - Francke, Till T1 - Monitoring abiotic and biotic parameters of forest regrowth under different management regimes on former wildfire sites in northeastern Germany – data from the PYROPHOB project T2 - Earth system science data N2 - We present the data recorded by eight institutions within the PYROPHOB project, running from 2020 to 2024 at two forest research sites in the south-west of Brandenburg, Germany. The aim of the project was to monitor abiotic and biotic parameters of forest regrowth under different management regimes on former wildfire sites in northeastern Germany. The observations comprised intermittent and continuous measurements or surveys on meteorological parameters (rainfall, temperature, vapour pressure deficit), soil (soil type and texture, soil chemistry and leaching, water content, soil temperature), deadwood, stand structure, vegetation regrowth, abundance of selected fauna (moths, beetles, mammals), UAV-based remote sensing (stand structure, spatial overview), and photo monitoring (succession). Thus, the multitude of collected data allows not only for detailed analyses of these observables separately, but also considering their interaction for a more multidisciplinary view on forest recovery after a wildfire. The data are available under the following DOIs: https://doi.org/10.23728/b2share.08a6a8b56f774a08a984871e7ef1b5a8 (Part 1, Schmehl et al., 2025a), under embargo until 31 March 2026 (Part 2, Schmehl et al., 2025b), https://doi.org/10.23728/b2share.de1661761da5481f938caf460e4f0ca9 (Part 3.1, Schmehl et al., 2025c), and https://doi.org/10.23728/b2share.51bdf4b6dc854873b6ff44fdddbf4c3b (Part 3.2, Schmehl et al., 2025d). Y1 - 2025 U6 - https://doi.org/10.5194/essd-17-6295-2025 SN - 1866-3516 VL - 17 IS - 11 SP - 6295 EP - 6313 PB - Copernicus GmbH CY - Göttingen ER - TY - GEN A1 - Holmer, Anna A1 - Bősze, Ildikó A1 - Bonhage, Alexander A1 - Susanne, Lindauer A1 - Günther, Moosbauer A1 - Pöllath, Nadja A1 - Kristina, Reetz A1 - Jörg, Völkel T1 - Prehistoric slot pits on a loess covered Rissian Danube terrace at Straubing (SE Bavaria) – structures for fat tanning? T2 - Journal of geomorphology : journal of basic and applied geomorphology N2 - Slot pits are uniquely shaped pits linked to prehistoric settlements in Central Europe, some dating back to the Mesolithic. They are typically long, deep, and narrow, yet their exact function remains unclear despite extensive research. This study aims to synthesize previous archaeological and pedological findings regarding slot pits and refine hypotheses about their function and age. Samples were collected from slot pits, other pit types, and surrounding loess at an excavation site in Straubing-Lerchenhaid, Bavaria, covering periods from the Linear Pottery Culture to the Iron Age. Pedological analysis indicated that the slot pits were not filled with material from nearby chernozemic horizons, and that no measured element was enriched in slot pits but not other pit types. Radiometric dating of bulk sediment samples, charcoal and animal remains, suggested ages ranging from the End Mesolithic to the End Neolithic. Although biomarker analyses showed traces of human faeces, they were not significant enough to suggest that the pits were primarily used as latrines, which was supported by the lack of elevated phosphorus levels in pit samples. A combination of these findings leads to the hypothesis that slot pits may have been utilized in the fat tanning process. KW - Tanning pits KW - Slot pits KW - Linear pottery culture KW - Linearbandkeramik KW - Prehistoric Pedological KW - Environment KW - Neolithic Y1 - 2025 U6 - https://doi.org/10.1127/jgeomorphology/0874 VL - 2 IS - 1 SP - 67 EP - 129 PB - Borntraeger Science Publishers CY - Stuttgart ER - TY - GEN A1 - Schneider, Anna A1 - Raab, Thomas A1 - Raab, Alexandra A1 - Bonhage, Alexander T1 - Soils of former field systems in Northeastern Bavaria, Germany N2 - Analytical data for bulk soil samples from former field system and reference areas in forests of Northeastern Bavaria, Germany. Profile samples taken following soil horizons, transect samples taken in fixed 10 cm depth ranges. Y1 - 2026 UR - https://data.mendeley.com/datasets/59932w7yct/1 U6 - https://doi.org/10.17632/59932w7yct.1 ER - TY - CHAP A1 - Raab, Thomas T1 - Subdued mountains of Central Europe T2 - Mid-Latitude Slope Deposits (Cover Beds) Y1 - 2024 SN - 978-0-323-96003-8 U6 - https://doi.org/10.1016/B978-0-323-96003-8.00011-6 SP - 9 EP - 114 PB - Eslevier ET - Second edition ER - TY - GEN A1 - Schüle, Maren A1 - Heinken, Thilo A1 - Adhikari, Yojana A1 - Binder, Anja A1 - Clerc, Danica A1 - Dobkowitz, Sophia A1 - Francke, Till A1 - Gerwin, Werner A1 - Hartong, Heinrich A1 - Jouy, Florent A1 - Raab, Thomas A1 - Repmann, Frank A1 - Rohlfs, Lilly A1 - Rönnefarth, Susanne A1 - Ibisch, Pierre L. T1 - Intensive post‐fire management drives ecosystem degradation but does not prevent tree regeneration T2 - Journal of applied ecology N2 - In recent years, wildfires have affected relatively large areas of managed forests in Central Europe. Often, forestry uses intensive post‐fire management practices, which can have negative effects on various components of the ecosystem. Fire ecology has been largely neglected in Central Europe and strategies for appropriate management and successful reforestation of burned areas are urgently needed. We have studied the effects of different post‐fire forest management treatments (including different levels of salvage logging and soil disturbances such as ploughing or raking) on soil parameters (phosphorus, nitrogen, calcium, potassium, magnesium, pH), microclimate (temperatures, vapour pressure deficit (VPD), heat and drought stress), deadwood, regrowth (biomass of tree regeneration, herb and bryophyte layer) and species richness (plants and saproxylic beetles) 3 years after wildfire in a Central European Scots pine forest (northeast Germany). Intensive forest management led to more unfavourable abiotic conditions, including stronger temperature extremes and elevated VPD. Consequently, vegetation on these sites experienced increased heat and drought stress and reduced nutrient availability. The biomass of the herb and bryophyte layer, as well as the species richness of plants and saproxylic beetles, was lower on completely salvage logged sites. Tree biomass recovered on all sites, including sites with intensive forest management. Tree regeneration in our study area was mainly driven by the recolonization of the pioneer species European aspen (Populus tremula), which can tolerate a wide range of site conditions. Synthesis and applications. We recommend avoiding intensive management on burned sites, such as complete salvage logging or ploughing, as this creates extreme site conditions that could inhibit the regeneration of more sensitive tree species and result in a long‐term legacy of degradation. In addition, herb and bryophyte layers, as well as the species richness of vegetation and saproxylic beetles, which are important components of forest ecosystems, are negatively affected by intense forest management. KW - Deadwood KW - Microclimate dynamics KW - Plant biomass KW - Post-fire forest management KW - Salvage KW - logging KW - Soil nutrient availability KW - Species diversity KW - Tree regeneration Y1 - 2026 U6 - https://doi.org/10.1111/1365-2664.70257 SN - 0021-8901 SN - 1365-2664 VL - 63 IS - 1 SP - 1 EP - 17 PB - Wiley ER - TY - RPRT A1 - Repmann, Frank A1 - Gerwin, Werner A1 - Kanzler, Michael T1 - Schlussbericht zum Vorhaben "Ermittlung der Bodenqualität zur Bewertung der Ertragspotentiale von Rohstoffpflanzen auf marginalen Standorten (BodenPotential)" Y1 - 2024 U6 - https://doi.org/10.34657/25088 PB - Technische Informationsbibliothek CY - Hannover ER -