The main purpose of this thesis was to find ways to maintain a low level of light‐induceddiscolouration at an increased addition of mechanical and chemimechanical pulps in coated highqualityfine paper and magazine paper grades. Current technology allows the production of highyieldpulps such as thermomechanical and chemimechanical pulps with properties suitable formanufacturing high‐quality paper or paperboard with a low basis weight. Coating of woodcontainingpaper will probably be necessary for photo‐stability reasons if lignin‐containing pulps areto be used as the main fibre furnish in long‐life and high‐value products.In order to find the most suitable pulp for this purpose, light‐induced discolouration of a variety ofpaper samples from unbleached and bleached softwood and hardwood pulps was studied under bothaccelerated and long‐term ambient light‐induced ageing conditions. Hardwood high‐yield pulps,especially aspen pulps, were proven to be more photo‐stable compared to softwood pulps. Hardwoodpulps should therefore be the first choice for applications where a high permanence is desirable.Evaluating ageing characteristics using the CIELAB colour system showed that accelerated ageingconditions tend to mainly increase the b* value and decrease the L* value (i.e. yellow the pulp),whereas long‐term ambient ageing also increases the a* value, which makes the pulp more reddish.A new method for studying the influence of the UV‐screening properties of coating layers on abase paper was developed, and used to investigate the effect of pigment, pigment size distribution,binder and UV‐absorbing additives. The coat weight and pigment type were found to be the mostimportant factors for reducing the transmittance of UV‐radiation. Coating colours containing kaolinpigments had a lower UV‐transmittance than calcium carbonate pigments. Of the calcium carbonates,precipitated calcium carbonates were better than ground calcium carbonates and the difference wasgreater at higher coat weights. The particle size distribution should preferable be narrow. When thebest pigment (bleached kaolin) and the best binder (styrene butadiene latex) were combined withtitanium dioxide, the UV‐transmittance could be reduced by about 90% at a coat weight of ~10 g/m2.At a coat weight close to 20 g/m2, the transmittance was close to zero. This shows that it is possible tomore or less fully protect a double coated base paper from harmful UV‐radiation, when the coatinglayer has an optimum composition for that purpose. A prerequisite to reach so far is that the coatinglayer has an even coat weight.

Thermal insulation materials made from natural fibrous materials, such as cellulose fibers, have advantages over others from a sustainability point of view. However, cellulosic materials are generally prone to mold and absorb moisture, and these have negative effects on the insulation properties, the durability of insulation materials, and interior air quality. In this thesis, cellulose-fiber-based insulation foams were prepared from bleached chemithermomechanical softwood pulp, and these foams showed promising thermal insulation properties and fungal resistance. Hydrophobic extractives were isolated from birch (Betula verrucosa) outer bark and used to improve the water resistance of the foams, which were impregnated in solutions of extractives and then dried. The modified foams showed greater water resistance, and the modification had no negative effects on the thermal insulation, fungal resistance, and compressive strength of the foams. Another potential problem with low density cellulosic thermal insulation materials is their poor reaction-to-fire properties. Cellulose-fiber-based insulation foams were prepared from formulations containing bleached chemithermomechanical softwood pulp and commercial fire retardants to improve the reaction of the foams to fire. Single-flame source test results showed that the foams containing 20% expandable graphite (20% EG) or 25% synergetic (25% SY) fire retardant had significantly improved reaction-to-fire properties and passed class E, which reflected that they can resist a small flame attack without substantial flame spreading for a short period according to EN 13501-1. Compared with the reference without any fire retardant, the peak heat release rate (Peak-HRR) of the 20% EG and 25% SY decreased by 62% and 39% respectively when the samples were subjected to a radiance heat flow of 25 kW m-2 in a Cone Calorimeter. The thesis demonstrates that it is possible to produce cellulose-fiber-based insulation materials with improved properties in terms of fungal, improved water resistance and reaction-to-fire properties. / <p>QC 20170428</p> / Energy-efficient cellulosic insulation products/panels for green building solutions

The representation of high-latitude surface processes and quantifying surface-climate feedbacks are some of the most serious shortcomings of present day Arctic land surface modelling. The energy balance of seasonally snow-covered sparse deciduous forests at high latitudes is poorly understood and inaccurately represented within hydrological and climate models. Snow cover plays an important role in wintertime fluxes of energy, water and carbon, controlling the length of the active growing season and hence the overall carbon balance of Arctic ecosystems. Snow cover is non-uniform and spatially variable, as wind redistributes snow from areas of exposed open tundra to sheltered areas within the forest, where a deeper snowpack develops. Low solar zenith angles, coupled with sparse deciduous leafless trees, cast shadows across the snow surface. The spatial distribution of canopy gaps determines the timing of direct radiation which penetrates down through the canopy to the snow surface. The forest canopy also excludes incoming longwave radiation and yet also emits longwave radiation to the snow surface. Consequently the forest canopy plays a key role in the radiation balance of sparse forests. To improve our knowledge of these complex processes, meteorological and field observations were taken in an area of highly heterogeneous birch Betula pubescens ssp. czerepanovii forest in Abisko, Sweden during the spring of 2008 and 2009. Detailed measurements of short and longwave radiation above and below the canopy, hemispherical photographs, tree temperatures and snow surveys were conducted to quantify the radiation balance of the sparse deciduous forest. An array of below canopy pyranometers found the mean canopy transmissivity to be 74 % in 2008 and 76 % in 2009. Hemispherical photographs taken at the pyranometer locations analysed with Gap Light Analyzer (GLA) showed reasonable agreement with a mean canopy transmissivity of 75 % in 2008 and 74 % in 2009. The canopy transmissivity was found to be independent of the diffuse fraction of radiation as the canopy is very sparse. A series of survey grids and transects were established to scale up from the below canopy pyranometers to the landscape scale. Hemispherical photographs analysed with GLA showed the sparse forest canopy had a mean transmissivity of 78 % and a mean LAI of 0.25, whereas the open tundra had a mean transmissivity of 97 % and a mean LAI of < 0.01. Snow surveys showed the sparse forest snow depth to vary between 0.34 and 0.55 m, whereas the snow depth in the open tundra varied between 0.12 and 0.18 m. Observations of canopy temperatures showed a strong influence of incident shortwave radiation warming the tree branches to temperatures up to 15 °C warmer than ambient air temperature on the south facing sides of the trees, and up to 6 °C on the north facing sides of the trees. To reproduce the observed radiation balance, two canopy models (Homogenous and Clumped) were developed. The Homogeneous canopy model assumes a single tree tile with a uniform sparse canopy. The Clumped canopy model assumes a tree and a grass tile, where the tree tile is permanently in shade from the canopy and the grass tile receives all the incoming radiation. These canopy models identified the need for a parameter that accounts for the spatial and temporal variation of the shaded gaps within the sparse forest. JULES (Joint UK Land Environment Simulator) is the community land surface model used in the UK Hadley Centre GCM suite. Modifications of the land-surface interactions were included in JULES to represent the shaded gaps within the sparse deciduous forest. New parameterisations were developed for the time-varying sunlit fractions of the gap (flit), the sky-view fraction (fv), and the longwave radiation emitted from the canopy (LWtree). These model developments were informed by field observations of the forest canopy and evaluated against the below canopy short and longwave radiation observed data sets. The JULES Shaded gap model output showed a strong positive relationship with the observations of below canopy shortwave and longwave radiation. The JULES Shaded gap model improves the ratio of observed to modelled short and longwave radiation on sunny days compared to the JULES model. The JULES Shaded gap model reduces the time to snow melt by 2 to 4 days compared to the JULES model, making the model output more aligned with in-situ observational data. This shortening of the modelled snow-season directly impacts on the simulated carbon and water balance regionally and has wider relevance at the pan-Arctic scale. When JULES Shaded Gap was evaluated on the global scale, it improved the modelled snowmass across large areas of sparse forest in northern Canada, Scandinavia and Northern Russia with respect to GlobSnow. The performance of the land surface-snow-vegetation interactions of JULES was improved by using the Shaded gap to model the radiation balance of sparse forests in climate-sensitive Arctic regions. Furthermore these observational data can be used to develop and evaluate high latitude land-surface processes and biogeochemical feedbacks in other earth system models.

This thesis concerns the relationship between research in experimental archaeology and the intangible of the past. Only a quarter of technological experiments in a sample of 100 studies addresses the intangible of technological practice, and this project sets out to explore if there are conceptual or practical obstacles for this low rate. The thesis begins with an in-depth examination of experimental archaeology and the criteria, paradigms and theories that determine its practice. Through this study, elements of the dichotomy positivism/postmodernism are uncovered and discussed. To resolve this dualism, a third paradigm – philosophical pragmatism – is introduced as an alternative. This conceptual debate represents Part I, and is subsequently collated into a methodological framework for the creation of a typified experiment. Part II consists of the experimental segment of this study, in search for practical obstacles for the exploration of the intangible. Through experimenting with Iron Age Bucket-shaped pots, Mesolithic faceted pebbles and Middle Palaeolithic birch bark tar production, different components of an experiment are highlighted for investigation. An element that comes forward as problematic is the relationship between experimental archaeologists and science ideals that is underscored by experimental tradition. Conclusively, the final discussion leaves the conceptual and practical barriers that may prevent archaeologists from studying the intangible aspects of technology overturned. In sum, this may enable experimental archaeologists to take a fuller view of their own practice and that of the people of the past.

In this investigation of immunotherapy (IT) children 6-16 years old with rhinoconjunctivitis due to birch polli­nosis were included. I. Methodological studies. To monitor IT a reliable provocation test is desirable. The conjunctival provocation test (CPT) was evaluated in 20 children with four repeated challenges. The test was found to have a good preci­sion, it was simple and appeared to be clinically safe. After repeated tests the levels of IgE antibodies against birch increased considerably in three children, indicating an immunological response. A pollen peak affects the symptoms of an atopic individual for several days. Thus pollen counts for previous days must be taken into account when relating symptom scores with the counts. A dynamic time series model was therefore developed by which groups of atopic patients could be compared when exposed to different amounts of pollens. II: Cross-reactivity between deciduous trees during IT. Immunotherapy with pollen allergen preparations made from either birch (B) or a mixture of birch, alder and hazel (M) were compared. As measured with symptom scores the children in the M group improved at least as much as those in the B group. In the B group but not in the M group the improvement correlated with immunochemical findings before IT or early during the treatment, probably an unsignificant finding. Otherwise there was little difference between the two groups. Analysis of sera with crossed radioimmunoelectrophoresis in 20 children revealed that 60% of the children below 13 years had de­veloped IgE antibodies during IT against allergens against which they had not been allergic before IT. This had no appearent clinical implications. III: Oral immunotherapy (OIT). A pilot study of 18 children treated with high doses of a birch pollen allergen preparation in enteric coated capsules and 8 untreated controls indicated that OIT was effective as shown by lower symptom scores, less conjuctival sensitivity and increased levels of IgE antibodies against birch. However, the gastrointestinal side-effects were pronounced. Therefore a second double-blind study, in 30 children, was performed reducing the side-effects through a different dose schedule. Compared with the placebo group, the ac­tively treated children had lower symptom scores (p = 0.04), reduced skin sensitivity (p = 0.01), increasing levels of IgE (p = 0.001) and IgG (p = 0.007) antibodies against birch before the birch pollen season and a suppression of the seasonal increase in levels of IgE antibodies against birch (p &lt;0.001). After three months of OIT but not after ten months they also had a lower sensitivity in CPT than the controls (p = 0.01). The intestinal permeability as assessed by the urinary recovery of differently-sized polyethyleneglycols was studied in 24 of the children during IT. No changes were seen in the group of actively treated children. In two ad­ditional children openly treated with OIT small bowel biopsies were taken with normal morphological findings. Thus OIT did not result in a generalized inflammation of the small bowel. / digitalisering@umu

The nineteenth century in Germany posed a repressive environment for-women as they were defined as inferior to men and forced into the subservient roles of housewives and mothers. This thesis examines the portrayal of femininity in three contemporary writers of the period, Louise Aston, Charlotte Birch-Pfeiffer and Louise von Francois. The first chapter endeavors to situate the writers in their social environment. It examines the mechanics that supported the patriarchal system, such as socializing women through education and categorizing them as inferior to justify and support their traditional roles. Chapters two, three, and four respectively deal with each author, presenting an introduction to their particular conditions and a brief summary of their lives. Following this, the individual tests are analyzed for their portrayal of femininity. These writers' visions of femininity differ greatly. Aston, whose career spanned the revolution of 1848, openly promotes liberal-humanist ideas and advocates the emancipation of women. Her heroines bear male an female traits and rise to positions of power and leadership. Birch-Pfeiffer's women are strong and independent. She frequently reverses the traditional gender roles. However, she upholds the moral code of her time, including the idea of the woman as exemplar of chastity and virtue . Francois idealizes the traditional role of women. However, she elevates that role by extolling motherhood and marital fidelity as supreme virtues. Despite these differences, there are similarities. All three writers offer an alternative picture of femininity despite this adherence, to a greater or lesser degree, to the traditional values of their time. In addition, they all criticize the patriarchal structures of society, revealing their discontent more or less openly. Finally, their portrayal of femininity was in each case based on their particular circumstances of the individual writers lives. Aston exploited the revolutionary times to present a strong claim for female emancipation; Birch- Pfeiffer, in need o f money, adapted strongly to the taste of her audience, finding in turn, interested recipients for her ideas; and Francois, a very private and proud person, chose to upgrade the women's role within the tradition, in attempt to avoid public attention. Within their circumstances, each one of the authors presented the best possible version of femininity as an alternative to traditional values. / Arts, Faculty of / Central Eastern Northern European Studies, Department of / Graduate

Le résultat principal de ce texte est une généralisation de la formule de Gross-Zagier p-adique de Perrin-Riou au cas de courbes de Shimura sur les corps totalement réels. Soit F un corps totalement réel. Soit f une forme modulaire de Hilbert sur F de poids parallel 2, qui est une forme nouvelle et est ordinaire en p. Soit E est une extension quadratique totalement imaginaire de F de discriminant premier à p et au conducteur de f. On peut construire une fonction L p-adique qui interpole valeurs spéciales de la fonction L complexe associée à f, E et caractères de Hecke d'ordre fini de E. La formule p-adique de Gross-Zagier relie la dérivée centrale de cette fonction L p-adique à la hauteur d'un divisor de Heegner sur une certaine courbe de Shimura. La stratégie de la preuve est proche de celle du travail original de Perrin-Riou. Dans la partie analytique, on construit le noyau analytique par calculs adéliques; dans la partie géométrique, on décompose le noyau géométrique en deux parties: places hors de p et places divisant p. Pour les places hors de p, les hauteurs p-adiques sont essentiellement des nombres d'intersection et sont calculées dans les travaux de S. Zhang, et il s'avère que cette partie est bien liée au noyau analytique. Pour les places divisant p, on utilise la méthode dans le travail de J. Nekovar pour montrer que la contribution de cette partie est nulle. / The main result of this text is a generalization of Perrin-Riou's p-adic Gross-Zagier formula to the case of Shimura curves over totally real fields. Let F be a totally real field. Let f be a Hilbert modular form over F of parallel weight 2, which is a new form and is ordinary at p. Let E be a totally imaginary quadratic extension of F of discriminant prime to p and to the conductor of f. We may construct a p-adic L function that interpolates special values of the complex L functions associated to f, E and finite order Hecke characters of E. The p-adic Gross-Zagier formula relates the central derivative of this p-adic L function to the p-adic height of a Heegner divisor on a certain Shimura curve. The strategy of the proof is close to that of the original work of Perrin-Riou. In the analytic part, we construct the analytic kernel via adelic computations, in the geometric part, we decompose the geometric kernel into two parts: places outside p and places dividing p. For places outside p, the p-adic heights are essentially intersection numbers and are computed in works of S. Zhang, and it turns out that this part is closely related to the analytic kernel. For places dividing p, we use the method in the work of J. Nekovar to show that the contribution of this part is zero.

A major argument for incorporating deciduous tree species in coniferous forest stands is their role in the amelioration and stabilisation of biogeochemical cycles. Current forest management strategies in central Europe aim to increase the area of mixed stands. In order to formulate statements about the ecological effects of mixtures, studies at the stand level are necessary. In a mixed stand of Norway spruce (Picea abies (L.) Karst.) and silver birch (Betula pendula Roth) in the Ore Mountains (Saxony, Germany), the effects of these two tree species on chemical and microbial parameters in the topsoil were studied at one site in the form of a case study. Samples were taken from the O layer and A horizon in areas of the stand influenced by either birch, spruce or a mixture of birch and spruce. The microbial biomass, basal respiration, metabolic quotient, pH-value and the C and N contents and stocks were analysed in the horizons Of, Oh and A. Significantly higher contents of microbial N were observed in the Of and Oh horizons in the birch and in the spruce-birch strata than in the stratum containing only spruce. The same was found with respect to pH-values in the Of horizon and basal respiration in the Oh horizon. Compared to the spruce stratum, in the birch and spruce-birch strata, significantly lower values were found for the contents of organic C and total N in the A horizon. The findings of the case study indicated that single birch trees have significant effects on the chemical and microbial topsoil properties in spruce-dominated stands. Therefore, the admixture of birch in spruce stands may distinctly affect nutrient cycling and may also be relevant for soil carbon sequestration. Further studies of these functional aspects are recommended.

In einem für das Erzgebirge (Sachsen, Südostdeutschland) typischen Wirtschaftswald aus ca. 60-jähriger Fichte (Picea abies [L.] KARST.), in den Sand-Birken (Betula pendula Roth) eingemischt sind, sollte die Wirkung der Baumartenmischung auf den Oberbodenzustand erfasst und bewertet werden. Die Befunde stammen aus einem Bestand, der sowohl hinsichtlich der Altersstruktur, des Bodentyps als auch der Stoffeinträge und der Kalkung für das Erzgebirge repräsentativ ist. Analysiert wurden photosynthetisch aktive Strahlung, Bodenvegetation, Streumenge und -verteilung, Dynamik der Streuzersetzung, Humuskörpermorphologie sowie chemische und mikrobiologische Oberbodeneigenschaften. Dabei fand ein einzelbaumweiser Ansatz in Kopplung mit Transekten Anwendung. Es wurden eindeutige Effekte durch einzelbaumweise eingemischte Birken nachgewiesen. Mit Hilfe des Einzelbaumansatzes und davon ausgehenden Transekten wurden reine Fichtenbereiche und Mischungsbereiche untersucht. Zusätzlich wurden für die Auswertung drei Straten gebildet. Die Zuordnung dafür war die folgende: Probepunkte unter der Birkenkrone ergaben das Birken-Stratum, Probepunkte unter der Fichte das Fichten-Stratum und Probepunkte im Übergangsbereich zwischen Birke und Fichte das Fichten-Birken-Stratum. Im Bereich der Birkenkronen waren überwiegend höhere Strahlungswerte festzustellen als unter den Fichtenkronen. Gezeigt wurde aber auch, dass die höheren Strahlungswerte, die unter den Birkenkronen auftraten, auch in lichteren bzw. lückigeren Partien des reinen Fichtenbestandes zu finden waren. Die Sippenanzahl der Bodenvegetation erhöhte sich sowohl unter reiner Fichte als auch in Mischung von Fichte und Birke vor allem mit zunehmender Annäherung zum Kronenrand. Insgesamt waren aber bei der Mischung von Fichte und Birke ähnlich hohe Sippenanzahlen wie im reinen Fichtenbereich zu finden. Allerdings gab es Sippen, die nur auf einer der beiden Flächen auftraten. Es waren höhere Deckungsgrade bei der Mischung von Fichte und Birke im Vergleich zur reinen Fichte sichtbar. Die Befunde der Streusammler ließen erkennen, dass in einer Entfernung von > 16 m vom Birkenstamm kaum noch Birkenstreu auftrat. Nennenswerte Trockenflussdichten wurden nur in einem Radius von 10 m festgestellt. In diesem Bereich ist ein Effekt der Birkenstreu auf die Oberbodeneigenschaften zu erwarten. Die Gesamttrockenmasse einer relativ vitalen Birke mit rund 38 cm Brusthöhendurchmesser betrug im Untersu-chungsjahr rund 8 kg. Die Modellierung unter Hinzunahme weniger vitaler Birken reduzierte die Gesamttrockenmasse auf 6,3 kg. Der Massenverlust der Birkenblätter in den Litter-Bags war in allen drei Straten bei der Mischung der Birkenblätter mit Fichtennadeln im Verhältnis 5:1 am größten. Bei den Fichtennadeln zeigten sich die höchsten Trockenmassenverluste in den reinen Nadel-Litter-Bags. Die Litter-Bags unter der Birkenkrone wiesen für alle Varianten die beste Zersetzung der Birkenblätter und der Fichtennadeln auf. Die C/N-Verhältnisse der Streu ließen keine eindeutigen positiven Effekte der Birkenkrone erkennen. Sie waren aber bei den Birkenblättern in allen Varianten, in allen Straten und zu allen Terminen deutlich enger als die der Fichtennadeln. Desweiteren war der Abfall der C/N-Kurven bei den Birkenblättern steiler als bei den Fichtennadeln. Die Mächtigkeit des Of-Horizontes wies sowohl in der Mischsituation als auch in der reinen Fichtenfläche deutlichere räumliche Muster auf als im Oh-Horizont. Im Of waren dadurch deutliche, vom Einzelbaum abhängige, Muster zu erkennen. Die höchsten Mächtigkeiten traten in Stammnähe auf. Die größten Gesamtmächtigkeiten existierten unter reiner Fichte. Beim Vergleich der Mächtigkeiten in den Straten war in der Of-Lage vor allem das Birken-Stratum signifikant verschieden vom Fichten-Stratum. Für die Oh-Mächtigkeit und somit auch die Gesamtmächtigkeit zeigte zusätzlich das Fichten-Birken-Stratum signifikante Unterschiede im Vergleich zum Birken-Stratum. Als Humusform trat der rohhumusartige Moder auf. Dabei überwog im Fichtenstratum der feinhumusreiche rohhumusartige Moder, im Fichten-Birken-Stratum und im Birken-Stratum dagegen der feinhumusarme rohhumusartige Moder. Signifikante Unterschiede zwischen Straten konnten in der Of-Lage für den pH-Wert, Cges-Vorrat, Ccarbonat-Gehalt, Nges-Gehalt, Nges-Vorrat, und den metabolischen Quotienten erfasst werden. In der Oh-Lage waren es die nachstehenden Oberbo-deneigenschaften: Corg/N-Verhältnis, Cges-Gehalt, Nmik-Gehalt, Cmik/Nmik-Verhältnis, Basalatmungsaktivität, sowie der metabolische Quotient, die sich zwischen den Straten signifikant unterschieden. Im A-Horizont zeigten sich signifikante Unterschiede der Straten beim Corg/N-Verhältnis, Cges-Gehalt, Ccabonat-Gehalt, Corg-Gehalt sowie dem Nges-Vorrat. Mit Hilfe der multivariaten Ordination (mit verschiedenen Elementgehalten und pH-Werten) ist die Stratenbildung erneut bestätigt worden. Dabei hatten die Elemente C, Mg, Ca und N den größten Einfluss. Die Auswertung der Daten der effektiven Kationenaustauschkapazität ließ vor allem für den A-Horizont Unterschiede zwischen den Straten erkennen. Dabei war die Akeff im Fichtenstratum am kleinsten und der prozentuale Anteil der sauren Kationen an der Akeff am größten. Die höchste Akeff besaß das Birken-Stratum. Eine Reihe der untersuchten Größen ließen eindeutige Baumarteneffekte erkennen. Alles in allem wurde der Nachweis erbracht, dass die Effekte in dem Bereich zu finden sind, der durch die Laubstreu der Birken geprägt ist. Bei den Oberbodeneigenschaften wurden keine Veränderungen an Punkten, die mehr als 10 m vom Birkenstamm entfernt waren, festgestellt. Aus den Ergebnissen war abzuleiten, dass für ähnliche Bedingungen wie im Untersuchungsbestand ein Mischungsanteil der Birke von mindestens 10 % zu empfehlen ist. Die Ergebnisse sind aber durch zukünftige Forschung noch zu verifizieren. Dafür sollten vor allem die Produktionsziele und die waldbaulichen Behandlungskonzepte für Mischbestände aus Fichte und Birke in Deutschland erneut konkretisiert werden. Um dafür eindeutige ökologische und ökonomische Kriterien festlegen zu können, wird eine Zusammenführung wichtiger Ergebnisse aus den verschiedenen forstlichen Forschungsbereichen (z. B. Standortskunde, Vegetationskunde, Waldwachstumskunde, Ökonomie, Zoologie, Waldbau) empfohlen. / In a typical managed forest of the Ore Mountains (Saxony, SE Germany), consisting of 60 years old Norway spruce (Picea abies [L.] KARST.) admixed with silver birches (Betula pendula Roth) the impact of the admixture on topsoil properties was quantified and evaluated. This study was conducted in a stand which is representative for the Ore Mountains regarding the soil type, deposition and liming. Photosynthetic active radiation, the layer of herbs and mosses, the mass and distribution of the litter fall, the dynamics of litter decom-position, and morphology of the humus layer as well as the chemical and microbiological topsoil properties were all analyzed. The study was based on a single-tree-approach where samples were collected along transects from selected sample trees of birch and spruce. Transects were established within areas of pure spruce as well as within areas of spruce and birch mixture. Three different strata were defined based on the situation of the examined points in relation to the crowns of birch and spruce: the birch stratum, the spruce stratum and the spruce-birch stratum with measurements from underneath the crowns of birches, spruces and the transition area between spruce and birch crowns, respectively. Higher photosynthetic active radiation values were detected in the area underneath the crowns of birch crowns in comparison with the area underneath the crowns of spruce. Higher values of photosynthetic active radiation were also registered within areas of light foliage and in gaps in the pure spruce stand. The number of ground vegetation species underneath pure spruce and in the mixture of spruce and birch was negatively correlated with the distance to the crown edge. But altogether the same number of ground vegetation species was found in the mixed stand and in the pure spruce stand. A few species were, however, specific for each stand type. A higher coverage of ground vegetation was found in the mixture of spruce and birch in comparison to the pure spruce. The results of the litter traps show marginal densities of birch leaves at a distance of more than 16 m from the birch stem. The majority of the dry flux density was found within a radius of 10 m around the birch stem. Within this area an effect of the birch litter on top soil properties was expected. The whole dry litter mass was measured in the study time of a relative vital birch with a diameter at breast high of ca. 38 cm and was ca. 8 kg. Modeling the amount of litter for birches with lower vitality indicated a dry litter mass of 6.3 kg. The mass lost of the birch leaves in the litter bags was in each stratum the highest at a ratio of 5 to 1 of birch leaves to spruce needles. The greatest loss of dry mass for spruce needles was registered in litter-bags with pure needles. The litter-bags under the birch crowns exhibited the best decomposition rate of birch leaves and spruce needles for all variants. The C/N-ratios of the litter showed no clear positive effects of the birch crown. But they were clearly smaller for the birch leaves in contrast to the spruce needles in all variants, in each stratum and at all dates. Furthermore the C/N-curves drop away more for the birch leaves in contrast to the spruce needles. The thickness of the Of-horizon in contrast to the Oh-horizon showed clear spatial patterns for the mixed situation and the pure spruce area. Thus in the Of-horizon a clear spatial pattern in connection to the single tree was apparent. The highest thickness was found close to the stem. The highest total thickness of the Of- and Oh-horizon was found underneath the pure spruce stand. When comparing the thickness of the humus layers between the stratums, significant differences where found for the Of-layer between the birch stratum and the spruce stratum. In addition, for the thickness of the Oh-layer as well as for the total thickness of all layers, significant differences were observed between the spruce-birch stratum and the birch stratum. The humus form was a mor-like moder. In the spruce stratum more fine-humus-rich variants of the mor-like moder was found, in the spruce-birch stratum and in the birch stratum it was more fine-humus-poor variants of the mor-like moder. Significant differences between the stratums in the Of-layer were found with respect to acidification, the pool of Ctot and Ntot, the content of Ccarbonat and Ntot and the metabolic quotient. For the Oh-layer significant differences between the stratums were found for the ratio of Corg and N, the content of Ctot and Nmic, the ratio of Cmic and Nmic, the basal respiration activity and the metabolic quotient. In the A-horizon significant differences between the stratums were found for the ration of Corg and N, the content of Ctot, Ccarbonat and Corg and the pool of Ntot. The results of multivariate ordination confirm the formation of stratums again. Thereby the contents of C, Mg, Ca and N had the greatest influence. The data analysis of the effective cation exchange capacity (ECEC) showed differences between the stratums mainly for the A horizon. In the spruce stratum the ECEC was lowest and the percentage of acid cations at the ECEC was greatest. The highest ECEC was in the birch stratum. Different results showed clear tree effects. These were only found in areas, which are influenced by birch leaves. In this study, a minimum tree admixture of 10% was required before an impact on the ground conditions of the whole stand was observed. Therefore, based on the results of this study, an admixture of birch of 10% is recommended. These results however must be verified through future research. These findings can be used to assist in meeting the goals of silvicultural management for mixed spruce and birch forests in Germany. Definition of explicit ecological and economic criteria created from a combination of results from different forest research sectors (e. g. Site ecology, Vegetation science, Forest Growth, Economy, Zoology, Silviculture) is recommended.

Eiskristalle fördern die Bildung von Niederschlag und beeinflussen die optischen Eigenschaften einer Wolke. Damit spielen sie eine maßgebliche Rolle für das Wetter und Klima unseres Planeten. In der Atmosphäre entstehen Eiskristalle entweder durch homogene oder durch heterogene Eisnukleation. Letzteres wird durch ein sogenanntes eisnukleierendes Partikel (INP) katalysiert. Bisher ist nur wenig über die speziellen Eigenschaften eines INP bekannt und die Vorhersagbarkeit über die Eisnukleationsfähigkeit verschiedener Materialien ist somit stark limitiert. Im Rahmen dieser Arbeit wurde das Immersionsgefrierverhalten von Birkenpollen, verschiedenen Mineralstäuben sowie Mischungen aus Mineralstaub und Birkenpollen Material untersucht. Ziel dieser Untersuchungen war, das Gefrierverhalten der verschiedenen Substanzen zu quantifizieren sowie deren Bedeutung für die Atmopshärische Eisnukleation besser zu verstehen. Das Gefrierverhalten eisaktiver Birkenpollen Makromoleküle konnte in dieser Arbeit erstmals unter atmosphärisch relevanten Bedingungen quantifiziert werden. Ein Vergleich zweier Birkenpollen Proben mit unterschiedlicher Herkunft demonstrierte die Abhängigkeit der Gefriereigenschaften der Birkenpollen von der geografischen Breite. Es wurden zwei unterschiedlich eisaktive Makromoleküle identifiziert, welche beide bei Temperaturen oberhalb −20°C aktiv sind. Das Gefrierverhalten unterschiedlicher Mineralstaubpartikel wurde hinsichtlich ihres K-Feldspat Anteils verglichen. Dabei zeigte sich, dass der K-Feldspat Anteil das Gefrierverhalten der Mineralstaubpartikel kontrolliert. Außerdem konnte gezeigt werden, dass eine Beschichtung mit Schwefelsäure die Eiskeimfähigkeit von K-Feldspat stark herabsetzt. In der Atmosphäre sind Partikel, welche sowohl aus mineralischen als auch aus biologischen Komponenten bestehen sehr wahrscheinlich. Um zu demonstrieren wie sich ein Mineralstaubpartikel verhält, wenn es mit biologischem Material gemischt wird, wurde in dieser Arbeit das Gefrierverhalten von Mischpartikeln bestehend aus Illit-NX und Birkenpollen Material untersucht. Es konnte gezeigt werden, dass die eisaktiven Makromoleküle der Birkenpolle ihre Eisaktivität beibehalten, auch wenn sie an einem Illit- NX Partikel angelagert sind. Die Mischpartikel zeigen somit das selbe Gefrierverhalten, wie reine Birkenpollen Partikel. Dies zeigt die bisher unterschätzte Bedeutung von biologischem Material für die atmosphärische Eisnukleation. / It is known that ice crystals in clouds play an important role for climate and weather as they influence precipitation initiation and radiative forcing. Ice formation in clouds occurs either through homogeneous or heterogeneous ice nucleation. For the latter case an ice nucleating particle (INP) catalyzes the freezing process. The knowledge about the properties which make a particle act as efficient INP is still limited. As a consequence, the ice nucleation ability of different materials has to be examined by quantitative experimentation. In the framework of the present thesis, the immersion freezing behavior of birch pollen material, different mineral dust particles and internal mixtures of mineral dust and birch pollen material was studied to improve our understanding of the importance of these species for the atmospheric ice nucleation. A quantification of the freezing behavior of ice nucleating active (INA) birch pollen macromolecules under atmospherically relevant conditions was done for the first time. Furthermore, the freezing ability of two birch pollen samples with different local origin was compared. It could be shown that birch pollen are able to produce at least two different types of INA macromolecules, which are both ice active in a temperature regime above −20◦ C. It became obvious that one of the macromolecules is favorably produced in higher latitudes, which indicated the dependence of the freezing properties of birch pollen from their local origin. Concerning mineral dust particles the present thesis demonstrated that the freezing ability of different K-feldspar containing mineral dust proxys like Arizona test dust, kaolinite and illite-NX, is controlled by their K-feldspar content. Furthermore, it was shown that K-feldspar loses its good freezing ability after surface modification with sulfuric acid. As internal mixtures of mineral and biological components are very likely in the atmosphere, the freezing ability of such mixed particles has been investigated in the present thesis. For illite-NX particles which were mixed with birch pollen material, it could be shown that the birch pollen macromolecules maintain their freezing ability when being adsorbed to a mineral dust particle. As a result, the affected mineral dust particle initiates freezing exactly like a birch pollen particle. For atmospheric application this means that it is likely that the ascription of mineral dust to the atmospheric INPs is, at least to a certain extent, due to unnoticed attached ice nucleating biological material.