A mineração é uma das atividades antrópicas mais impactantes aos recursos naturais, e que pode afetar profundamente a resiliência dos ecossistemas em função do elevado nível de degradação do solo e da paisagem. Diante disso, muitas áreas mineradas não são efetivamente recuperadas a ponto de restabelecer parte relevante da biodiversidade e dos serviços ambientais perdidos com a mineração. No entanto, novos métodos de restauração ecológica têm gerados resultados promissores mesmo em situações de degradação tão intensa como as de mineração, o que permitiria rever os níveis mínimos de qualidade ambiental exigidos de áreas que foram mineradas e que precisam passar por um processo de recuperação como forma de mitigação dos impactos causados e cumprimento de demandas legais de compensação ambiental. Assim, o objetivo geral desse estudo é avaliar a recuperação física, química e microbiológica do solo em áreas de mineração de bauxita em processo de recuperação ambiental. Avaliamos inicialmente a restauração do solo em minas de bauxita localizadas em Poços de Caldas-MG, tendo como objetivo contextualizar a melhoria do solo através de vários parâmetros químicos, físicos e microbiológicos em áreas recém-mineradas, em restauração de diferentes idades e remanescentes de floresta nativa. Encontramos que a restauração florestal foi eficiente em desencadear um processo de recuperação do solo, que resultou no restabelecimento, em poucos anos, de características químicas, físicas e microbiológicas já bem similares às do ecossistema de referência. Em seguida, avaliamos a recuperação dos teores de fósforo no solo pela restauração de florestas tropicais em minas de bauxita, e obtivemos como principais resultados a recuperação de importantes frações de P no solo, parte relevante da produção de serapilheira e da estrutura da floresta ao longo da trajetória sucessional nas jovens áreas restauradas após a mineração. A restauração ecológica mostrou-se capaz de restaurar rapidamente importantes atributos do solo, evidenciando o potencial da abordagem de restauração ecológica para mitigar os impactos ambientais negativos da mineração. Dessa maneira, destaca-se que políticas públicas voltadas para a mitigação de danos ambientais causados pela mineração podem exigir níveis mais elevados de qualidade ambiental em áreas de recuperação de minas, protegendo os interesses coletivos envolvidos na mediação de interesses entre empresas e sociedade. / Mining is one of the human activities with the highest impact in natural resources. It can profoundly affect the resilience of ecosystems due to the high level of soil degradation and landscape alteration. Thus, many mined areas are not effectively recovered enough to restore important part of biodiversity and ecosystem services lost. However, new ecological restoration methods showed promising results even in such intense degradation situations such as mining. Thus, it is needed to review the minimum levels of environmental quality required for areas that have been mined and need to recovered to mitigate the impacts and compliance with legal demands of environmental compensation. Thus, the general objective of this study is to evaluate the physical, chemical and microbiological soil in bauxite mining areas under ecological restoration. We initially evaluated soil restoration in bauxite mines located in the county of \"Poços de Caldas\", aiming to contextualize soil improvement through various chemical, physical and microbiological parameters in newly mined areas, restoration of different ages and remaining native forest. We found that forest restoration was effective in triggering a soil recovery process, which resulted in the recuperation, in a few years, of the chemical, physical and microbiological characteristics already very similar values to the references. We then evaluated the recovery of soil phosphorus for the restoration of tropical forests in bauxite mines, and obtained as main results the recovery of important fractions of soil P, litter production and forest structure along the successional trajectory in young restored areas after mining. Ecological restoration proved to be able to quickly restore important soil properties, showing the potential of ecological restoration approach to mitigate the negative environmental impacts of mining. Thus, it is emphasized that public policies to mitigate environmental damage caused by mining may require higher levels of environmental quality in mining recovery areas, protecting the collective interests involved in the mediation of interests between business and society.

Le « topsoil » comme outil de restauration écologique des terrains miniers dégradés, consiste à récupérer la couche de sol naturellement riche en matières organiques, semences et micro-organismes (qui définissent le potentiel biologique de restauration), lors d'une opération qui précède l'exploitation minière, puis à l'épandre sur les sites à restaurer. Au coeur desproblématiques de restauration écologique, les topsoils apparaissent à travers la littérature comme une technique efficiente et leur utilisation est abondamment préconisée. Toutefois celle-ci ne date, en Nouvelle-Calédonie, que des années 2000. Les connaissances actuelles locales liées à cet outil sont encore fragmentaires, et les caractéristiques des topsoils, tout comme les résultats obtenus sont hétérogènes. Ce travail de recherche a permis d'améliorer notre compréhension des interactions entre les composantes biologiques des topsoils et les phénomènes intervenant dansleur évolution (banque de graines, micro-organismes, et caractéristiques physico-chimiques). Les résultats obtenus ont montré que l'utilisation des topsoils en restauration écologique peut favoriser la restauration des écosystèmes ultramafiques néo-calédoniens, et pourraient trouver une application dans la conception de nouvelles stratégies de restauration écologiques des terrains miniers dégradés du territoire. Néanmoins, il est également apparu que les topsoils ne peuvent à eux seuls restaurer la totalité de la diversité végétale qui caractérise les substrats ultramafiques du territoire, et doivent donc être associés à d'autres techniques de restauration. / "Topsoil", as an ecological tool of restoration of the mines made in terraces, consist of getting back the layers full of organic matter, seeds and micro-organisms (which define the biological potential of restoration), during a procedure made following the exploitation of the mines, then could be extend to the sites which require some restoration.While the problem of ecological restoration is at the center of the debate, topsoil appears, according to the literature, as an efficient technique and their uses are well recommended. However, they only have been used in New Caledonia since the beginning of the XXI century. The actual knowledge of this specific tool is still incomplete, and the characteristics of topsoil, same as the results, remain inconsistent. The research made around this topic gave us a better understanding of the interaction between the biological components of topsoil and their way of evolving (seeds’ bank, micro-organisms and the physic and chemical characteristics). The results obtained demonstrate that the use of topsoil as an ecological restoration could be beneficial for the restoration of the ultramafic ecosystem of New Caledonia. It could, as well, find a place in the development of new strategies of ecological restoration of mines in terrace of the country. However, it has been shown in another hand that topsoil would not be sufficient to restore the entire vegetal diversity of the ultramafic bedrock of the country. For this reason, it has to be associated with different techniques of restoration.

The objectives of this study were to determine how seed reserves varied with depth in topsoil stockpiles and to evaluate the effect of length of time of storage on the number of viable seeds and number of species of seeds. Soil samples were taken from five topsoil piles representing zero to three years of storage on the Elkol-Sorenson mine near Kemmerer in southwestern Wyoming. Seeds were extracted using flotation/separation methods and were tested for viability using 2,3,5-triphenyl tetrazolium chloride solution. Data were analyzed using nonparametric statistical tests. Overall density of seeds in topsoil piles was low. No relationship was found between depth into the topsoil pile and the number of seeds or species. The number of seeds and species in the topsoil pile showed no decrease with increasing length of time of storage. The proportion of annual species in the seed reserve was not shown to increase with length of time of storage. Comparisons were made between the species composition of the seed reserve in the topsoil piles and the species composition of vegetation on sites selected to represent the sites of origin of the topsoil. Factors affecting the density, species composition and species richness of stored topsoil were suggested to be the plant community on the soil to be removed, depth of soil removed, and timing of topsoil removal.

This thesis examines the growth response and inter-relationships between shoots and roots of plants grown in compact soil. In the field, two topsoil and two subsoil conditions were created with five vegetable crops sequentially grown. Between 6 and 12% of the root system grew in the compact subsoil, which had a soil strength of 3.1 c.f. 1.9 MPa in the loosened subsoil. Both the root length density (Lv) and the specific root length were lower in the compact subsoil (80% and 30%, respectively). This had no effect on shoot growth when water and nutrients were well supplied. Compensatory root growth in the lose soil above the compact subsoil occurred in broccoli plants. As a result plants grown in soil with or without a compact subsoil had a similar total root length but with altered root distribution. When the water and nitrogen supplied to the soil was reduced, the lower subsoil Lv in the compact subsoil did not restrict water or N acquisition. This was possibly due to a large increase in the specific uptake per unit length of root, by the fewer roots in the compact subsoil. Compared to the subsoil treatments, only small changes in topsoil physical properties occurred when tillage was ceased. From the field trials the proportion and time of root growth into compact soil appeared important in determining the plant response. In a series of split-root experiments (horizontal and vertical arrangements of compact and loose soil) compensatory root growth in the loose soil only occurred when the root system was exposed to horizontally compact soil When compensatory root growth did not occur shoot growth was reduced. This resulted in there being a close relationship between total root length and leaf area. Further test results support a direct effect of mechanical impedance on shoot growth with a rapid (within 10 minutes) and large (50%) reduction in leaf elongation occurring when roots were mechanically impeded. In the field only plants whose roots were totally exposed to compact soil had reduced shoot growth with very compact subsoil having no effect. / Doctor of Philosophy (PhD)

Made available in DSpace on 2015-03-26T13:53:33Z (GMT). No. of bitstreams: 1 texto completo.pdf: 591551 bytes, checksum: dee8edc6806d5c9f152ac58f75d5a11c (MD5) Previous issue date: 2006-02-24 / Conselho Nacional de Desenvolvimento Científico e Tecnológico / The present study evaluated the efficacy of using a soil surface layer (topsoil) to cover deposits of waste-rock piles from granite extraction in order to enable the substratum to establish a plant community. With this objective, a greenhouse experiment was conducted with seven treatments (waste-rock, waste-rock + 5.0 cm topsoil, waste-rock + 10,0 cm topsoil, waste-rock + 20.0 cm topsoil, waste-rock + 10.0 cm B horizon, waste-rock + 4 L of incorporated manure, and waste-rock + 10.0 cm topsoil stored in the previous year). The experimental units consisted of a pot holding 32 dm3 substratum where one Joannesia princeps Vell. seedling was planted as indicator plant. The experiment was monitored over the course of 120 days. In the end of this period the indicator plants were evaluated biometrically, and the dry matter of the spontaneously germinated vegetation in each pot was analyzed. Substratum samples from each pot were also collected for analyses of microbiological aspects (CBM and qMic), of total organic carbon (COT) and of total nitrogen (NT). The results did not show any significant difference between thicknesses of 5, 10 or 20 cm, or even when no topsoil at all was used, regarding the establishment of an initial community of herbaceous plants by means of spontaneous germination. Topsoil (10 cm) addition proved effective, however, to establish tree vegetation, resulting in a significant growth increment of Joannesia princeps Vell. In both situations, the treatment of incorporated manure (4 L) resulted in strongest plant growth. No positive effect was verified by the substitution of topsoil by an equally thick layer of material derived from the soil B horizon. In the case of previously stored topsoil, no quality reduction was verified after a storage time of 12 months. The chemical and microbiological analyses were not able to detect significant alterations in the microbiota of the waste-rock substratum samples, but evidenced a tendency of increased COT and NT contents of the samples with the increasing thickness of the topsoil layers. / O presente trabalho teve por objetivo avaliar a eficiência de utilização da camada superficial do solo (topsoil) como cobertura de depósitos de estéril da extração de granito de modo a proporcionar a este substrato condições para o estabelecimento de uma comunidade vegetal. Para tanto, foi executado um experimento em casa de vegetação com sete tratamentos (estéril, estéril + 5,0 cm topsoil, estéril + 10,0 cm topsoil, estéril + 20,0 cm topsoil, estéril + 10,0 cm horizonte B, estéril + 4 L de esterco de curral incorporado e estéril + 10,0 cm topsoil armazenado no ano anterior). As unidades experimentais foram constituídas por um vaso com capacidade de 32 dm3 de substrato onde foi realizado o plantio de uma muda de Joannesia princeps Vell. como planta indicadora. O experimento foi acompanhado durante 120 dias. Ao fim deste período foram realizadas as avaliações biométricas das plantas indicadoras, bem como análise da matéria seca da vegetação germinada espontaneamente em cada vaso. Também foram coletadas amostras do substrato de cada vaso para análises microbiológicas (CBM e qMic), de carbono orgânico total (COT) e de nitrogênio total (NT). Os resultados não evidenciaram diferença significativa entre as espessuras de 5, 10 e 20 cm, ou mesmo ao não uso do opsoil, para o estabelecimento de uma comunidade inicial de herbáceas através da germinação espontânea. A adição do topsoil (10 cm) mostrou-se eficiente, porém, na etapa de estabelecimento da vegetação arbórea, ao propiciar um incremento significativo no crescimento de Joannesia princeps Vell. Em ambas as situações, a incorporação de esterco de curral (4 L) foi o tratamento que acarretou maior crescimento das plantas. Não foi verificado efeito positivo na substituição do topsoil por camada de igual espessura formada por material oriundo do horizonte B do solo. Quanto à utilização de topsoil já armazenado anteriormente, não foi comprovada diminuição de sua qualidade para o tempo do armazenamento de 12 meses. As análises químicas e microbiológicas utilizadas não foram capazes de detectar significativas alterações na microbiota das amostras do substrato estéril, porém evidenciaram uma tendência de aumento dos teores de COT e NT das amostras ao aumento da espessura da camada de Topsoil.

For successful restoration of unstable ecosystems in the dumps recreating a fully functioning lan dis needed. Dump substrates often have poor grain composition, extreme pH or are toxic. They also lack important recent organic matter, which improves the overall quality of the soil and is therefore necessary for the development of quality and fertile soil. Therefore, restoration of ecosystems in the dumps is initially very slow. A number of reclamation measures was invented to accelerate this process - for example, heaping up of topsoil to dump substrates. With organic matter present in the topsoil soil formation is faster and often with their physical and chemical properties differ significantly from then developed soils. There has already been number of works written considering development of soils on the Velká podkrušnohorská výsypka so far, none of which, however, did not affect grasslands. The aim of this work was to obtain complete information about the development of chemical and microbial properties of soils that were recultivted by reclaimed topsoil and grassed and then to compare them with developments in the areas of overgrown spontaneous succession. It was found that the total carbon content increases with time only in the reclaimed areas and maximum of the increase is in the depth of...

Ecossistemas campestres encontram-se fortemente impactados por conversão de hábitat e por espécies exóticas invasoras. É necessário restaurar os ecossistemas campestres ao redor do globo. Entretanto, para os ecossistemas campestres brasileiros há poucas experiências de restauração e precisamos testar a viabilidade de técnicas normalmente empregadas em outros lugares. O objetivo deste estudo foi testar diferentes combinações de técnicas para restauração de campos invadidos por Urochloa decumbens nos Campos Sulinos, sul do Brasil. Combinaram-se duas técnicas de controle da espécie invasora (aplicação de herbicida e remoção superficial de solo) e duas técnicas de introdução de espécies nativas (transposição de feno e semeadura direta). Foram estabelecidos oito blocos em um experimento bifatorial no Morro Santana, Porto Alegre, combinando dois fatores e cada um com três tratamentos (duas técnicas mais o controle). A cobertura de vários grupos de espécies, riqueza de espécies e composição de espécies foram avaliadas por análises de variância, e então também por análise de coordenadas principais. Adicionalmente, a relação entre a cobertura da invasora e das espécies nativas foi investigada. As técnicas de controle da invasora mostraram-se eficientes tanto na redução da cobertura da espécie, como em permitir a entrada de espécies nativas na comunidade. Comparando as duas técnicas, aplicação de herbicida pareceu ser melhor do que a remoção superficial de solo, pois parcelas que tiveram a aplicação tiveram menor cobertura da invasora e maior riqueza de espécies. Já as técnicas de introdução de espécies mostraram-se insuficientes para adicionar espécies nativas na comunidade para competir com U. decumbens. Padrões de composição de espécies diferiram entre os tratamentos. Técnicas de controle do invasor diferiram grandemente do seu controle, que foi dominado por U. decumbens. Uma clara relação existe entre a cobertura da invasora e a presença e cobertura de espécies nativas. Então o controle da espécie invasora é fundamental para uma maior recuperação da vegetação. Entretanto, os resultados aqui apresentados correspondem a apenas oito meses após a finalização da implementação do experimento, e ações futuras de manejo na área deverão combinar novamente o controle da invasora com introdução de espécies nativas. / Grasslands ecosystems are strongly impacted by land use and invasive species. It is necessary restore these ecosystems around the world. However, there are few experiences with ecological restoration for the Brazilian grasslands and we need to test the viability of techniques normally used in others grasslands ecosystems. The aim of this study was to test different combinations of techniques to the ecological restoration of grasslands invaded by Urochloa decumbens in Campos, Southern Brazil. We combine two techniques to control the invasive species (herbicide application and topsoil removal) and two techniques to introduce native species (hay transfer and direct sowing). We established nine blocks in a bi-factorial experiment on Morro Santana, Porto Alegre, Rio Grande do Sul, combining two factors and each one with three treatments (two techniques plus the control). The coverage of various groups of species, species richness, and species composition were evaluated by variance analyses, and the later also by a principal ordination analysis. Additionally, the relation between invader coverage and native species was investigated. Both techniques to control invasive species have shown to be efficient to reduce the coverage of the invasive species, as well as to allow the arrival of native species. Specifically comparing them, the herbicide application seems to be a better treatment than the topsoil removal, once plots with herbicide had lower invasive species coverage and higher species richness. However, the species introduction techniques failed efficiently to add native species to the community composition and to compete with U. decumbens. Species composition patterns differed among the treatments. The invader control techniques greatly differed from their control, which was dominated by U. decumbens. A clear relationship exists between the invader coverage and the presence and coverage of native species. Thus, the control of the invasive species is fundamental to further vegetation recovery. Nevertheless, results here presented correspond to just eight months from the experiment implantation and future monitoring and management actions on the area should combine once more the control of the invasive species and the introduction of native species.

The aim of this research is to assess various options for the management of topsoil stockpiles on disturbed lands and to evaluate the viability and germinability over time of the seedbanks in these stockpiles for use in rehabilitation. To predict their success, experimental trials were designed and conducted.

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.

The aim of this research is to assess various options for the management of topsoil stockpiles on disturbed lands and to evaluate the viability and germinability over time of the seedbanks in these stockpiles for use in rehabilitation. To predict their success, experimental trials were designed and conducted.