The bonds of democratic politics

This paper is an attempt to analyze bonds and their relevance within the confines of economics. They are discussed as both exogenous and endogenous variables. More specifically, the bonds of democratic politics are compared with those of non-democratic politics. It is argued that only those societies that have at their disposition certain kinds of bonds will be able to sustain democracy. It is further argued that the differential effects of democratic vs. non-democratic regimes on the respective bonds are rather weak. But then again, different kinds of democratic institutions might well have an effect on the prevalent bonds found in a society.

Authentisches Bewerten und Urteilen unter Unsicherheit - Arbeitsmaterialien und didaktische Kommentare für den Themenbereich "Bayessche Regel" für den Stochastikunterricht der Sekundarstufe I

Die vorliegende Unterrichtsreihe basiert auf zwei grundlegenden Vorstellungen zum Lernen und Lehren von Wahrscheinlichkeitsrechnung für Anfänger in der Sekundarstufe I. Zum einen ist die grundsätzliche Überzeugung der Autoren, dass ein sinnvoller und gewinnbringender Unterricht in Stochastik über den aufwendigeren Weg möglichst authentischer und konkreter Anwendungen im täglichen Leben gehen sollte. Demzufolge reicht eine Einkleidung stochastischer Probleme in realistisch wirkende Kontexte nicht, sondern es sollte eine intensive Erarbeitung authentischer Problemstellungen, z.B. mit Hilfe von realen Medientexten, erfolgen. Die Schüler sollen vor allem lernen, reale Probleme mathematisch zu modellieren und gefundene mathematische Ergebnisse für die reale Situation zu interpretieren und kritisch zu diskutieren. Eine weitere Besonderheit gegenüber traditionellen Zugängen zur Wahrscheinlichkeitsrechnung basiert auf kognitionspsychologischen Ergebnissen zur menschlichen Informationsverarbeitung. Durch eine Serie von Studien wurde gezeigt, dass Menschen – und natürlich auch Schüler – große Probleme haben, mit Wahrscheinlichkeiten (also auf 1 normierte Maße) umzugehen. Als viel einfacher und verständnisfördernder stellte sich die kognitive Verarbeitung von Häufigkeiten (bzw. Verhältnissen von natürlichen Zahlen) heraus. In dieser Reihe wird deshalb auf eine traditionelle formale Einführung der Bayesschen Regel verzichtet und es werden spezielle, auf Häufigkeiten basierende Hilfsmittel zur Lösungsfindung verwendet. Die erwähnten Studien belegen den Vorteil dieser Häufigkeitsdarstellungen gegenüber traditionellen Methoden im Hinblick auf den sofortigen und insbesondere den längerfristigen Lernerfolg (vgl. umfassend zu diesem Thema C. Wassner (2004). Förderung Bayesianischen Denkens, Hildesheim: Franzbecker, http://nbn-resolving.org/urn:nbn:de:hebis:34-2006092214705). Die vorliegende Schrift wurde zuerst im Jahre 2004 als Anhang zur o.g. Schrift bei Franzbecker Hildesheim veröffentlicht. Der Verlag hat einer elektronischen Veröffentlichung in der KaDiSto-Reihe zugestimmt.

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.

Settlement history of a mountain oasis in Northern Oman

To unravel the settlement history of oases in northern Oman, data on topography, the agricultural setting, water and soil parameters and archaeological findings were collected in the Wadi Bani Awf with its head oasis Balad Seet. Data collection lasted from April 2000 to April 2003 and was based on the establishment of a 3D-georeferenced map of the oasis comprising all its major infrastructural and agronomic features. At today's Balad Seet, a total of 8.8 ha are planted to 2,800 date palms and 4.6 ha are divided into 385 small fields dedicated to wheat, barley, sorghum, oats, alfalfa, garlic, onion, lime and banana. Radiocarbon dating of charcoal in the lower part of the main terrace system determined its age to 911 ± 43 years. Monthly flow measurements of four major aflaj systems showed a total maximum flow of 32 m^3 h^-1 with the largest falaj contributing 78% of the total flow. During drought periods, average water flow decreased by 3% per month, however, with significant differences between the spring systems. The analysis of the tritium/^3helium ratio in the water led to an estimated water age of up to 10 years. In combination with the flow data, this provided insights into the elasticity of the spring flow over time. The use of the natural resources of the Wadi Bani Awf by a pastoral population started probably in the early 3rd millennium BC. The first permanent settlement might have been established at Balad Seet during the first part of the 1st millennium BC. Presumably it was initiated by settlers from al-Hamra, a village at the southern foot of the Hajar mountains. Given an abundant und stable flow of springs, even in periods of drought, the construction of Balad Seet's first irrigation systems may have occurred at this early time. The combination of topographic, agricultural, hydro-pedological and archaeological data allowed assessment of the carrying capacity of this oasis over the three millennia of its likely existence. The changing scarcity of land and water and the eventual optimisation of their use by different aflaj constructions have been major driving forces for the development and apparent relativeley stable existence of this oasis.

Nutrient cycling and field-based partial nutrient balances in two mountain oases of Oman

Little is known about nutrient fluxes as a criterion to assess the sustainability of traditional irrigation agriculture in eastern Arabia. In this study GIS-based field research on terraced cropland and groves of date palm (Phoenix dactylifera L.) was conducted over 2 years in two mountain oases of northern Oman to determine their role as hypothesized sinks for nitrogen (N), phosphorus (P) and potassium (K). At Balad Seet 55% of the 385 fields received annual inputs of 100–500 kg N ha^-1 and 26% received 500–1400 kg N ha^-1. No N was applied to 19% of the fields which were under fallow. Phosphorus was applied annually at 1–90 kg ha^-1 on 46% of the fields, whereas 27% received 90–210 kg ha^-1. No K was applied to 27% of the fields, 32% received 1–300 kg K ha^-1, and the remaining fields received up to 1400 kg ha^-1. At Maqta N-inputs were 61–277 kg ha^-1 in palm groves and 112–225 kg ha^-1 in wheat (Triticum spp.) fields, respective P inputs were 9–40 and 14–29 kg ha^-1, and K inputs were 98–421 and 113–227 kg ha^-1. For cropland, partial oasis balances (comprising inputs of manure, mineral fertilizers, N2-fixation and irrigation water, and outputs of harvested products) were similar for both oases, with per hectare surpluses of 131 kg N, 37 kg P, and 84 kg K at Balad Seet and of 136 kg N, 16 kg P and 66 kg K at Maqta. This was despite the fact that N2-fixation by alfalfa (Medicago sativa L.), estimated at up to 480 kg ha^-1 yr^-1 with an average total dry matter of 22 t ha^-1, contributed to the cropland N-balance only at the former site. Respective palm grove surpluses, in contrast were with 303 kg N, 38 kg P, and 173 kg K ha^-1 much higher at Balad Seet than with 84 kg N, 14 kg P, and 91 kg K ha^-1 at Maqta. The data show that both oases presently are large sinks for nutrients. Potential gaseous and leaching losses could at least partly be controlled by a decrease in nutrient input intensity and careful incorporation of manure.

Evolving Classifiers - Evolutionary Algorithms in Data Mining

Data mining means to summarize information from large amounts of raw data. It is one of the key technologies in many areas of economy, science, administration and the internet. In this report we introduce an approach for utilizing evolutionary algorithms to breed fuzzy classifier systems. This approach was exercised as part of a structured procedure by the students Achler, Göb and Voigtmann as contribution to the 2006 Data-Mining-Cup contest, yielding encouragingly positive results.

Algorithmen für regelmäßige Kettenbrüche

Die Arbeit soll einen Einblick in die Theorie der Kettenbrüche geben. Wir haben gesehen, dass schwer greifbare Zahlen als Kettenbrüche ausgedrückt werden können. Es ist besonders hervorzuheben, dass irrationale Zahlen mit Hilfe einer Abschätzung vereinfacht durch Kettenbrüche dargestellt werden können. Weiter sind wir auch darauf eingegangen, wie wir Kettenbrüche wieder in eine rationale Darstellung umwandeln können. Es wurde gezeigt, wie wir rationale Zahlen als endlichen Kettenbrüche schreiben können. Die endlichen Kettenbrüche lieferten uns dann die Grundlage, um unendliche zu betrachten, wobei das größte Augenmerk darauf gerichtet war, dass wir eine irrationale Zahl durch einen unendlichen Kettenbruch abschätzen können. Den Kern der Arbeit bildet der Kettenbruch-Algorithmus, mit dessen Hilfe wir irrationale Zahlen in einen Kettenbruch umwandeln können. Ein wichtiger Aspekt sind auch die Abschätzungen, die wir vorgenommen haben. Mit ihrer Hilfe können wir sehen, wie dicht die letzte Konvergente der Kettenbruchentwicklung an der gesuchten irrationalen Zahl liegt. Da die Konvergenten immer aus teilerfremden Zählern und Nennern bestehen, können wir sogar sagen, dass eine Konvergente die beste Approximation an eine irrationale Zahl bietet. Es ist die beste Approximation in dem Sinne, dass keine rationale Zahl mit kleinerem oder gleichem Nenner existiert, die die irrationale Zahl besser annähert. Ein weiterer wichtiger Aspekt der Kettenbruchtheorie ist, dass quadratische Irrationalitäten endlich durch einen periodischen Kettenbruch dargestellt werden können. Es ist bemerkenswert, dass Kettenbrüche von quadratischen Irrationalitäten eine Regelmäßigkeit aufweisen, so dass sie endlich als periodicher Kettenbruch geschrieben werden können.