Composition and stability of organic matter fractions in soils under different land use regimes

Soil organic matter (SOM) vitally impacts all soil functions and plays a key role in the global carbon (C) cycle. More than 70% of the terrestric C stocks that participate in the active C cycle are stored in the soil. Therefore, quantitative knowledge of the rates of C incorporation into SOM fractions of different residence time is crucial to understand and predict the sequestration and stabilization of soil organic carbon (SOC). Consequently, there is a need of fractionation procedures that are capable of isolating functionally SOM fractions, i.e. fractions that are defined by their stability. The literature generally refers to three main mechanisms of SOM stabilization: protection of SOM from decomposition by (i) its structural composition, i.e. recalcitrance, (ii) spatial inaccessibility and/or (iii) interaction with soil minerals and metal ions. One of the difficulties in developing fractionation procedures for the isolation of functional SOM fractions is the marked heterogeneity of the soil environment with its various stabilization mechanisms – often several mechanisms operating simultaneously – in soils and soil horizons of different texture and mineralogy. The overall objective of the present thesis was to evaluate present fractionation techniques and to get a better understanding of the factors of SOM sequestration and stabilization. The first part of this study is attended to the structural composition of SOM. Using 13C cross-polarization magic-angle spinning (CPMAS) nuclear magnetic resonance (NMR) spectroscopy, (i) the effect of land use on SOM composition was investigated and (ii) examined whether SOM composition contributes to the different stability of SOM in density and aggregate fractions. The second part of the present work deals with the mineral-associated SOM fraction. The aim was (iii) to evaluate the suitability of chemical fractionation procedures used in the literature for the isolation of stable SOM pools (stepwise hydrolysis, treatments using oxidizing agents like Na2S2O8, H2O2, and NaOCl as well as demineralization of the residue obtained by the NaOCl treatment using HF (NaOCl+HF)) by pool sizes, 13C and 14C data. Further, (iv) the isolated SOM fractions were compared to the inert organic matter (IOM) pool obtained for the investigated soils using the Rothamsted Carbon Model and isotope data in order to see whether the tested chemical fractionation methods produce SOM fractions capable to represent this pool. Besides chemical fractionation, (v) the suitability of thermal oxidation at different temperatures for obtaining stable SOC pools was evaluated. Finally, (vi) the short-term aggregate dynamics and the factors that impact macroaggregate formation and C stabilization were investigated by means of an incubation study using treatments with and without application of 15N labeled maize straw of different degradability (leaves and coarse roots). All treatments were conducted with and without the addition of fungicide. Two study sites with different soil properties and land managements were chosen for these investigations. The first one, located at Rotthalmünster, is a Stagnic Luvisol (silty loam) under different land use regimes. The Ah horizons of a spruce forest and continuous grassland and the Ap and E horizons of two plots with arable crops (continuous maize and wheat cropping) were examined. The soil of the second study site, located at Halle, is a Haplic Phaeozem (loamy sand) where the Ap horizons of two plots with arable crops (continuous maize and rye cropping) were investigated. Both study sites had a C3-/C4-vegetational change on the maize plot for the purpose of tracing the incorporation of the younger, maize-derived C into different SOM fractions and the calculation of apparent C turnover times of these. The Halle site is located near a train station and industrial areas, which caused a contamination with high amounts of fossil C. The investigation of aggregate and density fractions by 13C CPMAS NMR spectroscopy revealed that density fractionation isolated SOM fractions of different composition. The consumption of a considerable part (10–20%) of the easily available O-alkyl-C and the selective preservation of the more recalcitrant alkyl-C when passing from litter to the different particulate organic matter (POM) fractions suggest that density fractionation was able to isolate SOM fractions with different degrees of decomposition. The spectra of the aggregate fractions resembled those of the mineral-associated SOM fraction obtained by density fractionation and no considerable differences were observed between aggregate size classes. Comparison of plant litter, density and aggregate size fractions from soil under different land use showed that the type of land use markedly influenced the composition of SOM. While SOM of the acid forest soil was characterized by a large content (> 50%) of POM, which contained high amounts of spruce-litter derived alkyl-C, the organic matter in the biologically more active grassland and arable soils was dominated by mineral-associated SOM (> 95%). This SOM fraction comprised greater proportions of aryl- and carbonyl-C and is considered to contain a higher amount of microbially-derived organic substances. Land use can alter both, structure and stability of SOM fractions. All applied chemical treatments induced considerable SOC losses (> 70–95% of mineral-associated SOM) in the investigated soils. The proportion of residual C after chemical fractionation was largest in the arable Ap and E horizons and increased with decreasing C content in the initial SOC after stepwise hydrolysis as well as after the oxidative treatments with H2O2 and Na2S2O8. This can be expected for a functional stable pool of SOM, because it is assumed that the more easily available part of SOC is consumed first if C inputs decrease. All chemical treatments led to a preferential loss of the younger, maize-derived SOC, but this was most pronounced after the treatments with Na2S2O8 and H2O2. After all chemical fractionations, the mean 14C ages of SOC were higher than in the mineral-associated SOM fraction for both study sites and increased in the order: NaOCl < NaOCl+HF ≤ stepwise hydrolysis << H2O2 ≈ Na2S2O8. The results suggest that all treatments were capable of isolating a more stable SOM fraction, but the treatments with H2O2 and Na2S2O8 were the most efficient ones. However, none of the chemical fractionation methods was able to fit the IOM pool calculated using the Rothamsted Carbon Model and isotope data. In the evaluation of thermal oxidation for obtaining stable C fractions, SOC losses increased with temperature from 24–48% (200°C) to 100% (500°C). In the Halle maize Ap horizon, losses of the young, maize-derived C were considerably higher than losses of the older C3-derived C, leading to an increase in the apparent C turnover time from 220 years in mineral-associated SOC to 1158 years after thermal oxidation at 300°C. Most likely, the preferential loss of maize-derived C in the Halle soil was caused by the presence of the high amounts of fossil C mentioned above, which make up a relatively large thermally stable C3-C pool in this soil. This agrees with lower overall SOC losses for the Halle Ap horizon compared to the Rotthalmünster Ap horizon. In the Rotthalmünster soil only slightly more maize-derived than C3-derived SOC was removed by thermal oxidation. Apparent C turnover times increased slightly from 58 years in mineral-associated SOC to 77 years after thermal oxidation at 300°C in the Rotthalmünster Ap and from 151 to 247 years in the Rotthalmünster E horizon. This led to the conclusion that thermal oxidation of SOM was not capable of isolating SOM fractions of considerably higher stability. The incubation experiment showed that macroaggregates develop rapidly after the addition of easily available plant residues. Within the first four weeks of incubation, the maximum aggregation was reached in all treatments without addition of fungicide. The formation of water-stable macroaggregates was related to the size of the microbial biomass pool and its activity. Furthermore, fungi were found to be crucial for the development of soil macroaggregates as the formation of water-stable macroaggregates was significantly delayed in the fungicide treated soils. The C concentration in the obtained aggregate fractions decreased with decreasing aggregate size class, which is in line with the aggregate hierarchy postulated by several authors for soils with SOM as the major binding agent. Macroaggregation involved incorporation of large amounts maize-derived organic matter, but macroaggregates did not play the most important role in the stabilization of maize-derived SOM, because of their relatively low amount (less than 10% of the soil mass). Furthermore, the maize-derived organic matter was quickly incorporated into all aggregate size classes. The microaggregate fraction stored the largest quantities of maize-derived C and N – up to 70% of the residual maize-C and -N were stored in this fraction.

Von "weiblichen Vollmenschen" und Klassenkämpferinnen

Zusammenfassung zur Inaugural-Dissertation: Von „weiblichen Vollmenschen“ und Klassenkämpferinnen – Frauengeschichte und Frauenleitbilder in der proletarischen Frauenzeitschrift „Die Gleichheit“ (1891-1923). Die wissenschaftliche Bedeutung, die der SPD-Frauenzeitschrift „Die Gleichheit“ (1891-1923) als Quelle der Geschichte der Frauenbewegung zukommt, spiegelt sich weder in Darstellungen zur Geschichte der SPD noch in der Geschichtsschreibung der deutschen Frauenbewegung wider. Auch ist die „Gleichheit“, Presseorgan der organisierten proletarischen Frauenbewegung Deutschlands und der Sozialistischen Fraueninternationale, bisher kaum Gegenstand einer umfassenden publizistischen Analyse gewesen. Es galt daher, zumindest das Hauptblatt der „Gleichheit“, die an ihr beteiligten Personen, ihre Strukturen und ihr Selbstverständnis möglichst detailliert und anhand publizistischer Kriterien darzustellen. Wandlungen ihres Erscheinungsbildes, ihrer editorischen und personellen Strukturen oder ihres Seitenumfangs markieren entscheidende Wendepunkte der deutschen Politik während des deutschen Kaiserreichs und der Weimarer Republik. Ihr Niveau lag deutlich über dem einer allgemeinen Frauenzeitschrift, eines Mitteilungs- oder Unterhaltungsblattes. Ihr Ziel war es, sowohl politisches Schulungsblatt für die engagierten Genossinnen als auch Agitationsmittel für die indifferenten Proletarierinnen zu sein. Inwieweit sie mit dieser Zielsetzung erfolgreich war, kann jedoch selbst die große Zahl ihrer Abonnements (der Höchststand lag 1914 bei 124.000 Exemplaren) nicht validieren. Tatsächlich ließ gerade der von ihrer langjährigen Redakteurin Clara Zetkin (1857-1933) angestrebte hohe intellektuelle Anspruch die „Gleichheit“ jedoch nicht zu einem Medium der Massen werden. Im Mai 1917 entschied sich der SPD-Parteivorstand, der dem Burgfrieden abträglichen, konsequent sozialistischen und internationalistischen Haltung Zetkins keine öffentliche Plattform mehr zu geben und entließ sie aus der Redaktion. Die Leitung der „Gleichheit“, die auch bis zu diesem Zeitpunkt durchaus keine „One-Woman-Show“ war, oblag schließlich bis zu ihrem letztmaligen Erscheinen im September 1923 noch einigen weiteren Redakteurinnen und Redakteuren (Marie Juchacz (1879-1956), Heinrich Schulz (1872-1932), Clara Bohm-Schuch (1879-1936), Elli Radtke-Warmuth (?-?) und Mathilde Wurm (1874-1935)). Deren Tätigkeit für die „Gleichheit“ wurde jedoch bisher kaum wissenschaftlich reflektiert. Dies gilt auch für die ausgesprochen internationale Zusammensetzung oder die männlichen Mitglieder des MitarbeiterInnenstabes. Indem sie sich selbst in der Tradition und als Teil eines Netzwerkes deutscher Frauen­öffentlichkeit („Die Frauen-Zeitung“ (1849-1852), „Die Staatsbürgerin“ (1886) und „Die Arbeiterin“ (1890-1891)) sah und indem sie besonders mittels frauen­geschichtlicher und frauenbiographischer Inhalte das Selbstbewusstsein ihrer Leserinnen zu fördern versuchte, betrieb die „Gleichheit“ gezielt Frauengeschichtsschreibung. Zahlreiche Artikel porträtieren Frauen aus Geschichte und Gegenwart und stellen in ihrem elaborierten Stil „Typen“ bzw. „Vorbilder“ dar. Um die Frage beantworten zu können, welche Frauen der Geschichte und welche ihrer Charaktereigenschaften von der „Gleichheit“ als vorbildlich für Sozialdemokratinnen erachtet wurden, wurden die biographischen Artikel zu 173 Frauen nach Analyse ihrer Inhalte und ihres Duktus vier Frauenleitbildern zugeordnet. Die Kategorisierung der einzelnen Frauenleitbilder „weiblicher Vollmensch“, „sozialistische Mutter“, „sozialistische Ehefrau“ und „Klassenkämpferin“ lehnt sich wiederum an den von Zetkin bereits 1898 veröffentlichten Artikel „Nicht Haussklavin, nicht Mannweib, weiblicher Vollmensch” (Die Gleichheit, Jg. 08/ Nr. 02/ 19.11.1898/ S. 1.) an. Sämtliche frauenbiographischen Artikel appellieren an die „Gleichheit“-Leserinnen, die oft selbst gesetzten Grenzen ihrer Handlungs – und Entwicklungsmöglichkeiten zu sprengen. Die sich daraus ableitenden Identifikationsangebote waren somit nicht auf dem Reissbrett ent­worfen, sondern basierten auf geschichtlicher Erfahrung und antizipierendem Bewusstsein. Diese Leitbilder versuchten, Realität und Utopie miteinander zu verbinden und konnten daher kaum frei von Widersprüchen sein. Wie die „Gleichheit“ selbst, so blieben auch ihre Ansätze politischer Frauen­bildung teilweise zwischen revolu­tionärem Umsturz und traditioneller Kontinuität gefangen. Indem sich die „Gleichheit“ historischer Vorbilder bediente, machte sie jedoch konkrete Ansprüche geltend: Sie forderte den weiblichen Anteil an Geschichte, an politischer Macht und am öffentlichen Bewusstsein.

The Effects of Visual Discriminability and Rotation Angle on 30-Month-Olds’ Search Performance in Spatial Rotation Tasks

Tracking objects that are hidden and then moved is a crucial ability related to object permanence, which develops across several stages in early childhood. In spatial rotation tasks, children observe a target object that is hidden in one of two or more containers before the containers are rotated around a fixed axis. Usually, 30-month-olds fail to find the hidden object after it was rotated by 180°. We examined whether visual discriminability of the containers improves 30-month-olds’ success in this task and whether children perform better after 90° than after 180° rotations. Two potential hiding containers with same or different colors were placed on a board that was rotated by 90° or 180° in a within-subjects design. Children (N D 29) performed above chance level in all four conditions. Their overall success in finding the object did not improve by differently colored containers. However, different colors prevented children from showing an inhibition bias in 90° rotations, that is, choosing the empty container more often when it was located close to them than when it was farther away: This bias emerged in the same colors condition but not in the different colors condition. Results are discussed in view of particular challenges that might facilitate or deteriorate spatial rotation tasks for young children.