TY - JOUR A1 - Käser, Beate A1 - Plassmann, Max A1 - Busch, Michael A1 - Carl, Horst A1 - Rink, Martin A1 - Kaiser, Michael A1 - Jessen, Olaf T1 - Militär und Gesellschaft in der Frühen Neuzeit : Bulletin N2 - - Militär & ländliche Gesellschaft in der FNZ Kolloquium in Rostock (Programm) - Tagung der AG- FNZ, Essen (16.-18. September 1999) - Veröffentlichungen der AMG in der preußischen Armee(B. Käser) - „Vom Untertan zum Staatsbürger...“ (M. Plassmann) - Informationen zum Museum in Wittstock - Absolutistischer Staat und Heeresordnung. (Dr. M. Busch - „Kriegserfahrung und Religion ...1792-1815“ (PD Dr. H. Carl) - „Vom Partheygänger“ zum Partisann (M. Rink) - „Cuius exercitus, eius religio?“ (Dr. M. Kaiser) - „Mars mit Zopf? Aufstieg und Fall des Ernst v. Rüchel“ (1754-1823) (O. Jessen) - AMG-Sitzung auf dem Historikertag in Frankfurt a. M. - Beitrittserklärung T3 - Militär und Gesellschaft in der frühen Neuzeit - 3 Y1 - 1999 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-33401 VL - 3 IS - 3 ER - TY - JOUR A1 - Kaiser, Michael A1 - Kroll, Stefan T1 - Forschungsprojekt Militär und Religiosität in der Frühen Neuzeit JF - Militär und Gesellschaft in der frühen Neuzeit N2 - Inhalt: Militär und Religiosität in der Frühen Neuzeit (Projektskizze) Einführende Literaturhinweise zum Themenkomplex Militär und Religiosität in der Frühen Neuzeit Y1 - 2001 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-28746 SN - 1861-910X SN - 1617-9722 VL - 5 IS - 2 SP - 158 EP - 164 ER - TY - JOUR A1 - Wilson, Peter A1 - Huhtamies, Mikko A1 - Huck, Stephan A1 - Gahlen, Gundula A1 - Herrmann, Michael A1 - Reimer, Torsten F. A1 - Winnige, Norbert A1 - Pöhlmann, Markus A1 - Pauser, Josef A1 - Fuchs, Antje A1 - Möbius, Sascha A1 - Heil, Wolfgang A1 - Jacobs, Rainer A1 - Kaiser, Michael A1 - Kroll, Stefan A1 - Blank, Ralf A1 - Gründel, Olaf A1 - Schlürmann, Jan A1 - Geffarth, Renko A1 - Bavendamm, Gundula T1 - Militär und Gesellschaft in der Frühen Neuzeit N2 - Aus dem Inhalt dieser Ausgabe: BEITRÄGE: Peter H. Wilson: British and american perspectives on early modern warfare Mikko Huhtamies: Kriegswesen und Gesellschaft in der frühen Neuzeit in der finnisch-schwedischen Geschichtsforschung INTERNET: Stephan Huck: Nutzungsmöglichkeiten des Internets Gundula Gahlen , Michael Herrmann, Torsten F. Reimer und Norbert Winnige: Militärgeschichte der Frühen Neuzeit im Internet Die Online-Angebote des AMG und sfn Markus Pöhlmann: Die Internetpräsenz des Arbeitskreises Militärgeschichte e.V. Josef Pauser: Das Online-Angebot des Arbeitskreises .Policey/Polizei im vormodernen Europa. Torsten F. Reimer: Eine Studie in Kriegführung. Eine Vorstellung des H-War Military History Network PROJEKTE: Antje Fuchs: Ein neuer Konfessionskrieg? Erfahrungen von Krieg und Okkupation im Kurfürstentum Hannover und benachbarten geistlichen Fürstentümern zur Zeit des Siebenjährigen Krieges 1756-1763 Sascha Möbius: Ergebnisse der Magisterarbeit .Psychologische Aspekte friederizianischer Taktik im Siebenjährigen Krieg. Wolfgang Heil: Die Gemeinen Soldaten. Das Sozialleben der militärischen Unterschicht im altpreußischen Heer und seine Stellung in der altständischen Gesellschaft. Rainer Jacobs: Militärische Dienstpflichten in der Frühen Neuzeit Michael Kaiser und Stefan Kroll: Forschungsprojekt Militär und Religiosität in der Frühen Neuzeit Ralf Blank: Die Schlosskanonen von Hohenlimburg Artilleriegeschütze mit einer wechselvollen Geschichte Gundula Gahlen und Olaf Gründel: Kataster zur Schlacht bei Wittstock von 1636 Jan Schlürmann: Die Schleswig-Holstein-Gottorfischen Auxiliairtruppen im Spanischen Erbfolgekrieg . Ergebnisse einer Untersuchung BERICHTE: Renko Geffarth: Die besetzte res publica. Zum Verhältnis von ziviler Obrigkeit und militärischer Herrschaft in besetzten Gebieten vom Spätmittelalter bis zum 18. Jahrhundert. Gundula Bavendamm: Operationsgeschichte und moderne Historiographie. Ein Widerspruch? T3 - Militär und Gesellschaft in der frühen Neuzeit - 5, Heft 2 KW - Militär / Geschichte Y1 - 2001 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-28126 SN - 1617-9722 SN - 1861-910X VL - 5 IS - 2 ER - TY - THES A1 - Kaiser, Michael T1 - Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung unterschiedlich stabiler Fraktionen der organischen Bodensubstanz N2 - Ziel dieser Arbeit ist es, ein sequentielles Extraktionsverfahren zur Erfassung unterschiedlich stabiler Anteile der orgnischen Bodensubstanz (OBS) zu entwickeln und zu klären, ob ein Zusammenhang zwischen Löslichkeit und Stabilität besteht. Darüber hinaus sollen der Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung dieser OBS-Anteile und Zusammenhänge zwischen Fourier Transform Infrarot (FT-IR)-Spektroskopiedaten und der Kationenaustauschkapazität (KAK) der OBS analysiert werden. Für die Untersuchungen wurden Böden der Langzeitfeldexperimente (LFE) in Halle, Bad Lauchstädt und Rotthalmünster beprobt. Zur Erfassung unterschiedlicher OBS-Fraktionen wurden im ersten Schritt die wasserlöslichen OBS-Anteile (OBS(W)-Fraktion) aus den Böden isoliert. Im zweiten Schritt wurden aus den Extraktionsrückständen der Wasserextraktion OBS-Anteile mit einer Natrium (Na)-Pyrophosphatlösung extrahiert (OBS(PY)-Fraktion). Die Stabilität der OBS-Fraktionen wurde anhand von δ13C-Bestimmungen und 14C-Messungen untersucht. Die Charakterisierung der Zusammensetzung der OBS-Fraktionen erfolgte mittels FT-IR Spektroskopie. Generell wird mit der OBS(PY)-Fraktion ein größerer Anteil am organischen Kohlenstoffgehalt der Böden erfasst als mit der OBS(W)-Fraktion. Die δ13C- und 14C-Daten zeigen, dass die OBS(W)-Fraktion höhere Anteile jungen organischen Materials als die OBS(PY)-Fraktion enthält. Das entwickelte sequentielle Extraktionsverfahren ist also prinzipiell geeignet unterschiedlich stabile OBS-Anteile anhand ihrer Löslichkeit zu isolieren. Mittels FT-IR spektroskopischer Untersuchungen wird festgestellt, dass Bewirtschaftungsmaßnahmen, wie die Düngung, sowie Standorteigenschaften die Zusammensetzung der OBS-Fraktionen beeinflussen. Für die OBS(PY)-Fraktion ist dies stärker ausgeprägt als für die OBS(W)-Fraktion. Die KAK der OBS(PY)-Fraktion aus den Böden der LFE in Halle und Bad Lauchstädt ist positiv mit der Absorptionsintensität der C=O-Bande in den FT-IR Spektren dieser OBS-Fraktion korreliert. N2 - The aim of this work is the development of a sequential extraction procedure for the isolation of different stable parts of soil organic matter (SOM) according to their solubility and to prove the relationship between solubility and stability. Additionally, the effects of management on amount and composition of different SOM fractions as well as relationships between data sets from Fourier Transform Infrared (FT-IR) spectroscopy and cation exchange capacitity (CEC) of SOM should be analysed. Soils from long term field experiments at Halle, Bad Lauchstädt and Rotthalmünster were sampled from the soil surface up to 30 cm depth. To obtain different SOM fractions water soluble SOM (SOM(W) fraction) were extracted at first before Na-pyrophosphat soluble SOM (SOM (PY) fraction) were isolated from the residue of water extraction. Stability of different SOM fractions were analyzed using 14C- and δ13C-measurements. Functional composition was studied with FT-IR spectroscopy. Generally, SOM(PY) represents a larger part of soil organic carbon (SOC) than SOM(W) in relation to the total SOC-content of the investigated soils. δ13C- and 14C-measurements show that SOM(W) contains more younger material than SOM(PY). The findings suggest that different stable SOM fractions can be obtained according to their solubility by the sequential extraction procedure. FTIR spectra show that SOM composition is influenced by management options like fertilization and field conditions. Such effects are more pronounced for SOM(PY) than for SOM(W). Furthermore data from FT-IR spectra and CEC measurements of SOMPY) show that the CEC is closely related to the C=O absorption intensities. T2 - Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung unterschiedlich stabiler Fraktionen der organischen Bodensubstanz KW - organische Bodensubstanz KW - unterschiedlich lösliche Fraktionen KW - Stabilität KW - FT-IR Spektroskopie KW - soil organic matter KW - different soluble fractions KW - stability KW - FT-IR spectroscopy Y1 - 2004 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-0001886 ER - TY - JOUR A1 - Kaiser, Michael A1 - Ellerbrock, Ruth H. A1 - Sommer, Michael T1 - Separation of coarse organic particles from bulk surface soil samples by electrostatic attraction N2 - Different separation procedures are suggested for studying the stability and functionality of sod organic matter (OM). Density fractionation procedures using high-molarity, water-based salt solutions to separate organic particles may cause losses or transfers of C between particle and soluble OM fractions during separation, which may be a result of solution processes. The objective of this study was to separate coarse organic particles (>0.315 mm) from air- dried surface soil samples to avoid such solution processes as far as possible. Air-dried surface soil samples (<2 mm) from nine adjacent arable and forest sites were sieved into five soil particle size fractions (2-1.25, 1.25-0.8, 0.8- 0.5, 0.5-0.4, and 0.4-0.315 mm). Coarse organic particles were separated from each of these fractions using electrostatic attraction by a charged glass surface. The sum of the total dry matter content of the electrostatically separated coarse organic particles ranged from 0.05 to 140 g kg(-1). Scanning electron microscopy images and organic C (OC) analyses indicated, however, that the coarse organic particle fractions were also composed of 20 to 76% mineral particles (i.e., 200-760 g mineral kg(-1) fraction). The repeatability of the electrostatic attraction procedure falls within a range similar to that of accepted density fractionation methods using high-molarity salt solutions. Based on the similarity in repeatability, we suggest that the electrostatic attraction procedure will successfully remove coarse organic particles (>0.315 mm) from air-dried surface soil samples. Because aqueous solutions are not used, the electrostatic attraction procedure to separate coarse organic particles avoids C losses and transfers associated with solution-dependent techniques. Therefore, this method can be used as a pretreatment for subsequent density- or solubility-based soil OM fractionation procedures. Y1 - 2009 UR - https://www.soils.org/publications/sssaj U6 - https://doi.org/10.2136/sssaj2009.0046 SN - 0361-5995 ER - TY - JOUR A1 - Kaiser, Michael A1 - Walter, K. A1 - Ellerbrock, Ruth H. A1 - Sommer, Michael T1 - Effects of land use and mineral characteristics on the organic carbon content, and the amount and composition of Na-pyrophosphate-soluble organic matter, in subsurface soils JF - European journal of soil science N2 - Land use and mineral characteristics affect the ability of surface as well as subsurface soils to sequester organic carbon and their contribution to mitigation of the greenhouse effect. There is less information about the effects of land use and soil properties on the amount and composition of organic matter (OM) for subsurface soils as compared with surface soils. Here we aimed to analyse the long-term (>= 100 years) impact of arable and forest land use and soil mineral characteristics on subsurface soil organic carbon (SOC) contents, as well as on amount and composition of OM sequentially separated by Na pyrophosphate solution (OM(PY)) from subsurface soil samples. Seven soils with different mineral characteristics (Albic and Haplic Luvisol, Colluvic and Haplic Regosol, Haplic and Vertic Cambisol, Haplic Stagnosol) were selected from within Germany. Soil samples were taken from subsurface horizons of forest and adjacent arable sites continuously used for > 100 years. The OM(PY) fractions were analysed for their OC content (OC(PY)) and characterized by Fourier transform infrared spectroscopy. Multiple regression analyses for the arable subsurface soils indicated significant positive relationships between the SOC contents and combined effects of the (i) exchangeable Ca (Ca(ex)) and oxalate-soluble Fe (Fe(ox)) and (ii) the Ca(ex) and Al(ox) contents. For these soils the increase in OC (OC(PY) multiplied by the relative C=O content of OM(PY)) and increasing contents of Ca(ex) indicated that OM(PY) mainly interacts with Ca2+. For the forest subsurface soils (pH < 5), the OC(PY) contents were related to the contents of Na-pyrophosphate-soluble Fe and Al. The long-term arable and forest land use seems to result in different OM(PY)-mineral interactions in subsurface soils. On the basis of this, we hypothesize that a long-term land-use change from arable to forest may lead to a shift from mainly OM(PY)-Ca2+ to mainly OM(PY)-Fe3+ and -Al3+ interactions if the pH of subsurface soils significantly decreases to < 5. Y1 - 2011 U6 - https://doi.org/10.1111/j.1365-2389.2010.01340.x SN - 1351-0754 VL - 62 IS - 2 SP - 226 EP - 236 PB - Wiley-Blackwell CY - Malden ER - TY - JOUR A1 - Kayler, Z. E. A1 - Kaiser, Michael A1 - Gessler, A. A1 - Ellerbrock, Ruth H. A1 - Sommer, Michael T1 - Application of delta C-13 and delta N-15 isotopic signatures of organic matter fractions sequentially separated from adjacent arable and forest soils to identify carbon stabilization mechanisms JF - Biogeosciences N2 - Identifying the chemical mechanisms behind soil carbon bound in organo-mineral complexes is necessary to determine the degree to which soil organic carbon is stabilized belowground. Analysis of delta C-13 and delta N-15 isotopic signatures of stabilized OM fractions along with soil mineral characteristics may yield important information about OM-mineral associations and their processing history. We anlayzed the delta C-13 and delta N-15 isotopic signatures from two organic matter (OM) fractions along with soil mineral proxies to identify the likely binding mechanisms involved. We analyzed OM fractions hypothesized to contain carbon stabilized through organo-mineral complexes: (1) OM separated chemically with sodium pyrophosphate (OM(PY)) and (2) OM occluded in micro-structures found in the chemical extraction residue (OM(ER)). Because the OM fractions were separated from five different soils with paired forest and arable land use histories, we could address the impact of land use change on carbon binding and processing mechanisms. We used partial least squares regression to analyze patterns in the isotopic signature of OM with established mineral and chemical proxies indicative for certain binding mechanisms. We found different mechanisms predominate in each land use type. For arable soils, the formation of OM(PY)-Ca-mineral associations was identified as an important OM binding mechanism. Therefore, we hypothesize an increased stabilization of microbial processed OM(PY) through Ca2+ interactions. In general, we found the forest soils to contain on average 10% more stabilized carbon relative to total carbon stocks, than the agricultural counter part. In forest soils, we found a positive relationship between isotopic signatures of OM(PY) and the ratio of soil organic carbon content to soil surface area (SOC/SSA). This indicates that the OM(PY) fractions of forest soils represent layers of slower exchange not directly attached to mineral surfaces. From the isotopic composition of the OM(ER) fraction, we conclude that the OM in this fraction from both land use types have undergone a different pathway to stabilization that does not involve microbial processing, which may include OM which is highly protected within soil micro-structures. Y1 - 2011 U6 - https://doi.org/10.5194/bg-8-2895-2011 SN - 1726-4170 VL - 8 IS - 10 SP - 2895 EP - 2906 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Kaiser, Michael A1 - Berhe, Asmeret Asefaw A1 - Sommer, Michael A1 - Kleber, Markus T1 - Application of ultrasound to disperse soil aggregates of high mechanical stability JF - Journal of plant nutrition and soil science = Zeitschrift für Pflanzenernährung und Bodenkunde N2 - Questions remain about the exact ultrasonic energy level that is required to effectively disperse soil aggregates and to what extent this is accompanied by physical damage to individual soil particles. We found maximum aggregate dispersion at energy levels of 1500 J?cm3 and no evidence for the disintegration of particles < 20 mu m even at that energy level. Our findings suggest that sonication at energies much greater than those applied conventionally can disperse aggregates of high mechanical stability. KW - soil aggregates KW - ultrasonication KW - dispersion maxima KW - water-extractable elements Y1 - 2012 U6 - https://doi.org/10.1002/jpln.201200077 SN - 1436-8730 VL - 175 IS - 4 SP - 521 EP - 526 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Kaiser, Michael A1 - Zederer, Dan P. A1 - Ellerbrock, Ruth H. A1 - Sommer, Michael A1 - Ludwig, Bernard T1 - Effects of mineral characteristics on content, composition, and stability of organic matter fractions separated from seven forest topsoils of different pedogenesis JF - Geoderma : an international journal of soil science N2 - Mineral topsoils possess large organic carbon (OC) contents but there is only limited knowledge on the mechanisms controlling the preservation of organic matter (OM) against microbial decay. Samples were taken from the uppermost mineral topsoil horizon (0 to 5 cm) of seven sites under mature deciduous forest showing OC contents between 69 and 164 g kg(-1) and a wide range in mineral characteristics. At first, organic particles and the water-extractable OM were removed from the soil samples. Thereafter, Na-pyrophosphate extractable organic matter (OM(PY)), assumed to be indicative for OM bound via cation mediated interactions, and the OM remaining in the extraction residue (OM(ER)), supposed to be indicative for OM occluded in mechanically highly stable micro-aggregates, were sequentially separated and quantified. The composition of OM(PY) and OM(ER) was analyzed by FTIR and their stability by C-14 measurements. The OC remaining in the extraction residues accounted for 38 to 59% of the bulk soil OC (SOC) suggesting a much larger relevance of OM(ER) for the OM dynamic in the analyzed soils as compared with OM(PY) that accounted for 1.6 to 7.5% of the SOC. The FUR analyses revealed a lower relative proportion of C=O groups in OM(ER) compared to OM(PY) indicating differences in the degree of microbial processing between these fractions. Correlation analyses suggest an increase in the stability of OM(PY) with the soil pH and contents of Na-pyrophosphate soluble Fe, Al, and Mg and an increase in the stability of OM(ER) with the soil pH and the contents of clay and oxalate-soluble Fe and Al. Despite the detected influence of soil mineral characteristics on the turnover of OM(PY) and OM(ER), the Delta C-14 signatures indicated mean residence times less than 100 years. The presence of less stabilized OM in these fractions can be derived from methodological uncertainties and/or the fast cycling compartment of mineral-associated OM. (C) 2015 Elsevier B.V. All rights reserved. KW - Forest mineral topsoil KW - Organic matter stabilization KW - Na-pyrophosphate soluble organic matter KW - Micro-aggregates KW - Infrared spectroscopy KW - C-14 analyses Y1 - 2016 U6 - https://doi.org/10.1016/j.geoderma.2015.08.029 SN - 0016-7061 SN - 1872-6259 VL - 263 SP - 1 EP - 7 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Kaiser, Michael T1 - Spannungsfeld von Warheit und Macht JF - Kunsttherapeutische Stichworte Y1 - 2021 SN - 978-3-946320-29-6 SP - 210 PB - fabrico CY - Hannover ER -