Seismic site response analysis allows an engineer to assess the effect of local soil conditions on the ground motions expected during an earthquake. In seismic site response analysis, an input ground motion on rock is propagated through a site specific soil column. The computed response at the surface is dependent on both the input ground motion and the soil properties that characterize the site. However, there is uncertainty in both the input ground motion and the soil properties, as well as natural variability in the soil properties across a site. To account for the uncertainty in the input ground motions, engineers use a suite of motions that are selected and scaled to fit a scenario input motion. This study introduces a semi-automated method to select and scale the input motions to fit a target input motion and its variability. The proposed method is intended to replace tedious trials of combinations by hand with combinations performed by a computer. However, as in the traditional selection methods, the final selection of the combination is done by the engineer.The effect of the selected ground motion combination on the computed surface response spectrum from the site response analysis, and its variability, was investigated in this study. The results show by using a combination with as few as five motions, the median surface response spectrum can be predicted with an error of 10%. Additionally, the manner used to scale the input motions does not impact the accuracy of the median surface response spectrum, as long as the median response spectrum of the input combination agrees with the target input response spectrum. However, if the standard deviation of the surface response spectrum is to be considered (e.g., to develop median plus one standard deviation spectra), a input combination of at least 20 motions is recommended and the combination must be scaled such that the standard deviation of the input combination matches the standard deviation of the input target spectrum. Monte Carlo simulations were used to assess the impact of soil property variability on surface spectra computed by seismic site response. The results from this study indicate that by accounting for the variability of the shear-wave velocity profile of a site can cause a significant decrease in the median surface response spectrum, as well as a slight increase in the standard deviation of the surface response spectrum at periods less than the site period. By considering the variability of the nonlinear properties (shear modulus reduction and damping ratio) the median response spectrum decreased only slightly, but the standard deviation increased in a manner similar to the increase observed when considering the variability of the shear-wave velocity profile. Simultaneously considering the variability of the shear-wave velocity profile and nonlinear properties resulted in a median surface response spectrumsimilar to the median surface response spectrumcomputed with considering the variability of the shear-wave velocity alone. However, the standard deviation of the surface response spectrum was larger than the standard deviation computed by independent consideration of the variability of the shear-wave velocity or nonlinear properties.

Understanding soil fertility issues in the Middle Mountains of Nepal requires interdisciplinary research, integrating biophysical and socio-economic factors. Soil degradation is associated with a wide range of human activities, natural processes, and the wider economic, political and social aspects of their setting. This study focuses on a in the Middle Mountains and addresses four research questions: What is the current soil fertility status? How is it changing? Why is it changing? and What are the implications for production, sustainability and management? Soil surveys, plot studies, nutrient balance modelling, household questionnaires and GIS mapping techniques are used to address these questions. The overall soil fertility conditions of the study area are poor and appear to be declining under most land uses. Soil pH averages 4.8 ± 0.4 and is below desirable levels for crop production. Soil carbon (0.99 ± 0.5 %) and cation exchange capacity (10.8 ± 4.1 cmol kg⁻¹) are low, and available phosphorus (16.6 ± 18.9 mg kg⁻¹) is a concern given the low pH. Land use is the most important factor influencing soil fertility with khet (irrigated agriculture) showing the best fertility status (pH 5.2, Ca 5.3 cmol kg⁻¹ and available P 21.6 mg kg⁻¹), followed by bari, and grassland, with forest soil fertility being the poorest (pH 4.2, Ca 0.9 cmol kg⁻¹ and available P 0.7 mg kg⁻¹). Soil type is the second most important factor influencing soil fertility, with red soils displaying significantly lower available P than non-red soils (9.8 versus 22.1 mg kg⁻¹). Phosphorus sorption studies indicate the high P fixation capacity of red soils, 1.2 g kg⁻¹ compared to 0.3 g kg⁻¹ calculated for non-red soils. Extrapolation from site specific data to a spatial coverage using statistical analysis and GIS techniques indicates that only 14% of the classified areas have adequate pH, available P and exchangeable Ca, and 29% of the area has a high P fixation capacity (>1.5 g kg⁻¹). Nutrient balance modelling provides estimates of nutrient depletion from the soil pool and raises concerns about the sustainability of upland farming, intensive vegetable crop production and forest nutrient cycling. Dryland maize production results in deficits of 188 kg N, 38 kg P205 and 21 kg Ca per ha furrow slice Rice-wheat cultivation on irrigated land appears to have limited impact on the soil nutrient pool, but the addition of premonsoon maize to the rotation results in deficits of 106 kg N and 12 kg P₂O₅ per ha furrow slice. Rates of soil fertility depletion estimated from differences in soil fertility between land uses indicate substantial N and Ca losses from forest land (94 and 57 kg ha per furrow slice respectively). Land use change, the impact on nutrient flows and relationships between nutrient inputs, crop uptake, nutrient balances and soil fertility provide an understanding of why soil fertility is changing. Historical forest cover data indicates substantial deforestation during the 1950-1960 period, a subsequent reversal in the 1972-1990 period associated with afforestation efforts, and renewed losses in the 1990s. Forest soils receive minimal nutrient inputs and large biomass removal results in a low soil fertility status. Expansion and marginalization of dryland agriculture were noted from 1972-1990, as former grazing, shrub and abandoned lands were terraced and cultivated. Nutrient fluxes indicate that inputs are insufficient to maintain the soil nutrient pool under dryland cultivation due to the high nutrient requirements of maize and nutrient losses through erosion. Nutrient balances for maize and wheat are positively correlated with nutrient inputs but relationships with soil fertility are weak. On irrigated khet lands, cropping has intensified and cash crop production has prompted the use of agrochemicals. Excess fertilization is leading to eutrophication and the high use of agrochemicals is a health concern. Nutrient fluxes on khet fields appear to be sustainable due to the addition of nutrients through irrigation and sediment trapping, but may be insufficient to maintain triple cropping. Grass and shrub land dynamics are characterized by minimal inputs and low productivity. The traditional farming system appears to have been sustainable, but triple cropping and increased vegetable production are threatening sustainability. The transfer of nutrients within the fanriing system is unbalanced. Under intensive production, nutrients on khet land are being depleted, poor farmers are shifting their limited compost inputs from bari to khet fields, and biomass collected from forests, disrupts the natural nutrient cycle. Population growth, land tenure, culture and poverty are the underlying socio-economic factors which influence farming system dynamics, directly impact nutrient inputs, and indirectly drive soil fertility degradation. Population growth rates of 2.6% have contributed to agricultural intensification and marginalization, and pressure on forest resources. The distribution of land is highly skewed with 15% of the surveyed households owning 46% of the land. Women play a central role in soil fertility management through their responsibilities for livestock care, litter collection and compost application, but increasing workloads related to commercial milk production, cash cropping and the off-farm employment of males are a major concern. Agricultural assets, farm gross margins, market oriented production, commercial milk production and off-farm employment provide indicators of economic well-being and are positively correlated with nutrient inputs. Total returns and gross margins are greatest for households growing vegetable crops as part of their rotation, and these households apply significantly more compost and fertilizer to both khet and bari land. Access to land is a key factor driving nutrient management and influencing economic well-being. Land is the main agricultural asset in the study area, khet land is the most productive and khet provides the greatest opportunity of cash crop production. However, given the increased labour demands for triple cropping, vegetable production and commercial milk production, the social sustainability is being threatened. Some 47% of the households were not able to fulfil their basic need requirements from the land they farm. They will have no alternative but to exhaust the capital stock of soil nutrients rather than investing in soil fertility. Maintenance of soil fertility is essential to meet the basic food and resource needs of the growing population. Organic matter management is critical, supplying macro- and micro nutrients, reducing acidification, maintaining soil structure and enhancing microbial activity. Water management and sediment trapping on lowland fields provide additional nutrients on khet land; soil acidity on upland fields and forest land needs to be better managed given the increased fertilizer use on bari and high biomass removal from forests; and the incorporation of N fixing species into agricultural production systems are an option which may provide additional animal fodder and help sustain soil fertility.

Understanding soil fertility issues in the Middle Mountains of Nepal requires interdisciplinary research, integrating biophysical and socio-economic factors. Soil degradation is associated with a wide range of human activities, natural processes, and the wider economic, political and social aspects of their setting. This study focuses on a in the Middle Mountains and addresses four research questions: What is the current soil fertility status? How is it changing? Why is it changing? and What are the implications for production, sustainability and management? Soil surveys, plot studies, nutrient balance modelling, household questionnaires and GIS mapping techniques are used to address these questions. The overall soil fertility conditions of the study area are poor and appear to be declining under most land uses. Soil pH averages 4.8 ± 0.4 and is below desirable levels for crop production. Soil carbon (0.99 ± 0.5 %) and cation exchange capacity (10.8 ± 4.1 cmol kg⁻¹) are low, and available phosphorus (16.6 ± 18.9 mg kg⁻¹) is a concern given the low pH. Land use is the most important factor influencing soil fertility with khet (irrigated agriculture) showing the best fertility status (pH 5.2, Ca 5.3 cmol kg⁻¹ and available P 21.6 mg kg⁻¹), followed by bari, and grassland, with forest soil fertility being the poorest (pH 4.2, Ca 0.9 cmol kg⁻¹ and available P 0.7 mg kg⁻¹). Soil type is the second most important factor influencing soil fertility, with red soils displaying significantly lower available P than non-red soils (9.8 versus 22.1 mg kg⁻¹). Phosphorus sorption studies indicate the high P fixation capacity of red soils, 1.2 g kg⁻¹ compared to 0.3 g kg⁻¹ calculated for non-red soils. Extrapolation from site specific data to a spatial coverage using statistical analysis and GIS techniques indicates that only 14% of the classified areas have adequate pH, available P and exchangeable Ca, and 29% of the area has a high P fixation capacity (>1.5 g kg⁻¹). Nutrient balance modelling provides estimates of nutrient depletion from the soil pool and raises concerns about the sustainability of upland farming, intensive vegetable crop production and forest nutrient cycling. Dryland maize production results in deficits of 188 kg N, 38 kg P205 and 21 kg Ca per ha furrow slice Rice-wheat cultivation on irrigated land appears to have limited impact on the soil nutrient pool, but the addition of premonsoon maize to the rotation results in deficits of 106 kg N and 12 kg P₂O₅ per ha furrow slice. Rates of soil fertility depletion estimated from differences in soil fertility between land uses indicate substantial N and Ca losses from forest land (94 and 57 kg ha per furrow slice respectively). Land use change, the impact on nutrient flows and relationships between nutrient inputs, crop uptake, nutrient balances and soil fertility provide an understanding of why soil fertility is changing. Historical forest cover data indicates substantial deforestation during the 1950-1960 period, a subsequent reversal in the 1972-1990 period associated with afforestation efforts, and renewed losses in the 1990s. Forest soils receive minimal nutrient inputs and large biomass removal results in a low soil fertility status. Expansion and marginalization of dryland agriculture were noted from 1972-1990, as former grazing, shrub and abandoned lands were terraced and cultivated. Nutrient fluxes indicate that inputs are insufficient to maintain the soil nutrient pool under dryland cultivation due to the high nutrient requirements of maize and nutrient losses through erosion. Nutrient balances for maize and wheat are positively correlated with nutrient inputs but relationships with soil fertility are weak. On irrigated khet lands, cropping has intensified and cash crop production has prompted the use of agrochemicals. Excess fertilization is leading to eutrophication and the high use of agrochemicals is a health concern. Nutrient fluxes on khet fields appear to be sustainable due to the addition of nutrients through irrigation and sediment trapping, but may be insufficient to maintain triple cropping. Grass and shrub land dynamics are characterized by minimal inputs and low productivity. The traditional farming system appears to have been sustainable, but triple cropping and increased vegetable production are threatening sustainability. The transfer of nutrients within the fanriing system is unbalanced. Under intensive production, nutrients on khet land are being depleted, poor farmers are shifting their limited compost inputs from bari to khet fields, and biomass collected from forests, disrupts the natural nutrient cycle. Population growth, land tenure, culture and poverty are the underlying socio-economic factors which influence farming system dynamics, directly impact nutrient inputs, and indirectly drive soil fertility degradation. Population growth rates of 2.6% have contributed to agricultural intensification and marginalization, and pressure on forest resources. The distribution of land is highly skewed with 15% of the surveyed households owning 46% of the land. Women play a central role in soil fertility management through their responsibilities for livestock care, litter collection and compost application, but increasing workloads related to commercial milk production, cash cropping and the off-farm employment of males are a major concern. Agricultural assets, farm gross margins, market oriented production, commercial milk production and off-farm employment provide indicators of economic well-being and are positively correlated with nutrient inputs. Total returns and gross margins are greatest for households growing vegetable crops as part of their rotation, and these households apply significantly more compost and fertilizer to both khet and bari land. Access to land is a key factor driving nutrient management and influencing economic well-being. Land is the main agricultural asset in the study area, khet land is the most productive and khet provides the greatest opportunity of cash crop production. However, given the increased labour demands for triple cropping, vegetable production and commercial milk production, the social sustainability is being threatened. Some 47% of the households were not able to fulfil their basic need requirements from the land they farm. They will have no alternative but to exhaust the capital stock of soil nutrients rather than investing in soil fertility. Maintenance of soil fertility is essential to meet the basic food and resource needs of the growing population. Organic matter management is critical, supplying macro- and micro nutrients, reducing acidification, maintaining soil structure and enhancing microbial activity. Water management and sediment trapping on lowland fields provide additional nutrients on khet land; soil acidity on upland fields and forest land needs to be better managed given the increased fertilizer use on bari and high biomass removal from forests; and the incorporation of N fixing species into agricultural production systems are an option which may provide additional animal fodder and help sustain soil fertility. / Graduate and Postdoctoral Studies / Graduate

The August 17, 1999 Kocaeli-Turkey Earthquake (Mw=7.4) caused severe damage to the structures and lifelines in the Marmara region. Soil liquefaction was identified as one of the major causes of this damage. The aim of this study is to determine geotechnical and earthquake engineering factors that contribute to the structural damage observed in Sakarya city after 1999 Kocaeli Earthquake. For this purpose, the results of an extensive field investigation program compiled by General Directorate of Disaster Affairs including subsurface soil characterization and documenting structural performance data were used. The database was carefully screened for poor quality data and was transferred to geographic information system (GIS) framework. Maximum likelihood methodology for the probabilistic assessment of seismically induced structural performance was chosen as the statistical tool. After series of sensitivity analyses, important geotechnical and earthquake engineering parameters of the problem were selected as i) liquefaction severity index, ii) post liquefaction volumetric settlement, iii) peak ground acceleration and, iv) spectral acceleration defined at the period range of conventional buildings. In addition to these parameters, structural performance defined as a) no damage and light, b) moderate damage, c) heavy damage and collapse, as well as the number of storeys of each structure were used as to correlate structural damage with geotechnical earthquake engineering factors. As a conclusion series of vulnerability functions specific to Adapazari shaken by Kocaeli Earthquake were developed. Performance predictions of these vulnerability functions were shown to be consistent with as high as 65 percent of the observed structural performance.

The purpose of this study is to assess the engineering geological and geotechnical characteristics and to perform seismic hazard studies of the Upper Pliocene to Quaternary (Plio-Quaternary) deposits located towards the north of Ankara through surface wave testing methods. Based on a general engineering geological and seismic site characterization studies, site classification systems are assigned in seismic hazard assessments. The objective of the research is to determine the regional and local seismic soil conditions (i.e., shear wave velocities, soil predominant periods and soil amplification factors) and to characterize the soil profile of the sites in this region by the help of surface geophysical methods. These studies have been supported by engineering geological and geotechnical field studies carried out prior to and during this study. By integrating these studies, local soil conditions and dynamic soil characteristics for the study area have been assessed by detailed soil characterization in the region. As a result, seismic hazard assessments have been performed for &Ccedil / ubuk and its close vicinity with the aid of Geographical Information Systems (GIS) through establishing seismic characterization and local soil conditions of the area.

Southern Appalachian Phalaris arundinacea control was investigated by: 1) correlating cover and species richness with soil characteristics across transects; 2) burning and herbicide use to determine conditions facilitating native plant establishment; and 3) hemi-parasitic Pedicularis lanceolata tested as a biological control. Phalaris cover was correlated with subsoil consolidation; areas without Phalaris had consolidated subsoil while Phalaris at >50% cover established on loose soil. Phalaris cover inhibited species richness (r2=0.78). No soil characteristic predicted species richness. Herbicide reduced Phalaris cover and aerial biomass by 23% and 63% respectively, compared to controls. Burning was ineffective. Two summers after herbicide Phalaris subterranean biomass remained 32% less than control biomass. Monocot transplants established readily following herbicide but dicot transplants were less likely to survive. Pedicularis parasitized Phalaris. Pedicularis’ effect on a mixed species total (r2=0.735) was non-linear; implying greater effect on large plants. Non-parasitic native plant species competition reduced biomass of Phalaris by 40%.

Conselho Nacional de Desenvolvimento Científico e Tecnológico / As inundações são fenômenos naturais que ocorrem devido às chuvas de grande magnitude, agravadas nas áreas urbanas pela impermeabilização do solo e ineficiência dos sistemas de drenagem. Os telhados verdes surgem como uma medida compensatória estrutural que pode reter parte da água precipitada, adiando o pico de escoamento. O objetivo deste trabalho foi de desenvolver uma combinação de solo e condicionadores para telhado verde, promovam um aumento relevante na capacidade de retenção hídrica e um maior adiamento do pico de escoamento das águas pluviais. Este estudo foi dividido em duas etapas. Na Etapa 1, foram analisadas, em colunas de percolação, três condicionadores nas seguintes concentrações: Gel retentor Stockosorb (2; 4; 6 g/dm3), Fertilizante de liberação lenta Osmocote (4,7; 7,1; 9,0 g/dm3) e Zeólita (30; 50; 70 g/dm3), em três eventos (regas) consecutivos de chuva simulada na intensidade de 57 mm/h. A avaliação das concentrações mais adequadas dentre as testadas para cada condicionante foi baseada nas análises referentes à retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min) e à qualidade da água percolada (pH, oxigênio dissolvido, turbidez e sólidos). Na Etapa 2, foi avaliada, em vasos, a influência da presença de três espécies de plantas (Arachis pintoi; Raphanus sativus; Lavandula angustifolia) em dois tipos de meio: solo sem condicionadores; solo com condicionadores nas melhores concentrações indicadas na Etapa 1, sendo simulada apenas um evento de chuva de 57 mm/h. Foram analisados parâmetros biológicos (germinação; plantas sobreviventes; comprimento do caule e da raiz; pesos da biomassa do caule e da raiz); retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min); qualidade da água percolada (pH; oxigênio dissolvido; turbidez; sólidos; nitrato; amônia; fósforo total). Os resultados da Etapa 1 indicaram que o gel promoveu de forma significativa um aumento na retenção hídrica, e adiou o início da percolação de água, além de promover ligeira elevação do pH na água percolada. A adição de zeólita resultou em um aumento significativo da retenção hídrica, porém tal aumento não é vantajoso visto que este representa um custo adicional que poderia ser reduzido com o aumento da proporção do gel na coluna. A adição de fertilizantes não promoveu mudanças na qualidade da água percolada. Na Etapa 2, somente o efeito da presença de A. pintoi (maior produção de biomassa de raiz e caule) e R. sativus foram avaliadas. A presença dos condicionantes no solo proporcionou um desempenho significativamente superior em relação a retenção hídrica (altura do substrato e adiamento do pico de chuva) e qualidade da água percolada (pH e turbidez) quando comparados aos testes realizados na presença somente de solo. O fertilizante influenciou nas altas concentrações dos nutrientes (nitrogênio e fósforo) na água percolado nos resultados. A presença do gel no substrato, resultou numa capacidade superior de retenção de hídrica, e consequentemente no adiamento do pico de intensidade de chuva. Sendo assim, recomenda-se a aplicação do gel em telhados verdes para futuros estudos em ambientes externos. / Floods are natural phenomena that occur due to the large magnitude of rains, aggravated in urban areas by soil sealing and inefficient drainage systems. Green roofs emerge as a structural compensatory measure may retain part of the precipitated water, delaying the peak flow. The objective of this study was to develop a combination of soil and conditioners for green roof, promote a significant increase in water retention capacity and greater postponement of the peak stormwater runoff. This study was divided into two stages. In Step 1, were analyzed by percolation columns three conditioners in the following concentrations: Gel STOCKOSORB retainer (2; 4; 6 g / dm3) Osmocote slow-release fertilizer (4,7; 7,1; 9, 0 g / dm3) and zeolite (30; 50; 70 g / dm3), three events (watering) consecutive simulated rainfall intensity of 57 mm / hr. Evaluation of the most suitable among the concentrations tested for each condition was based on the analyzes for water retention (when the medium after watering, the flow delay time; mm retained; intensity of percolated water in mm / min) and the quality of percolated water (pH, dissolved oxygen, turbidity and solids). In Step 2, was evaluated in pots, the effect of the presence of three species of plants (Arachis pintoi, Raphanus sativus, Lavandula angustifolia) in two types of medium: no soil conditioners; best soil conditioners in concentrations indicated in Step 1, only one being simulated rainfall event of 57 mm / hr. Biological parameters were analyzed (germination, surviving plants, stem and root length, stem biomass and root weight); Water retention (after half the time of irrigation, the flow delay time; mm retained; intensity of percolated water in mm / min); quality of soil solution (pH, dissolved oxygen, turbidity, solids, nitrate, ammonia, total phosphorus). The Step 1 results indicated that the gel significantly promoted an increase in water retention, and delayed the start of the percolation of water, and promote slight increase of pH in soil solution. The addition of zeolite resulted in significant improvement of water retention, not as much as the retaining gel. The addition of fertilizers did not cause changes in the quality of the soil solution. In Step 2, only the effect of the presence of A. pintoi (higher biomass of root and stem) and R. sativus were evaluated. The presence of conditions on the ground provided a significantly better performance in relation to water retention (substrate height and postponement of peak rainfall) and quality of the soil solution (pH and turbidity) when compared to tests carried out in the presence only of soil. However, the influence on the high fertilizer concentrations of nutrients (nitrogen and phosphorus) in water leachate in the results, it is concluded that the presence of the gel on the substrate, resulting in a higher water retention ability, and therefore in delaying the peak intensity rain. Thus, the application of the gel is recommended for further studies to green roofs outdoors.

Conselho Nacional de Desenvolvimento Científico e Tecnológico / As inundações são fenômenos naturais que ocorrem devido às chuvas de grande magnitude, agravadas nas áreas urbanas pela impermeabilização do solo e ineficiência dos sistemas de drenagem. Os telhados verdes surgem como uma medida compensatória estrutural que pode reter parte da água precipitada, adiando o pico de escoamento. O objetivo deste trabalho foi de desenvolver uma combinação de solo e condicionadores para telhado verde, promovam um aumento relevante na capacidade de retenção hídrica e um maior adiamento do pico de escoamento das águas pluviais. Este estudo foi dividido em duas etapas. Na Etapa 1, foram analisadas, em colunas de percolação, três condicionadores nas seguintes concentrações: Gel retentor Stockosorb (2; 4; 6 g/dm3), Fertilizante de liberação lenta Osmocote (4,7; 7,1; 9,0 g/dm3) e Zeólita (30; 50; 70 g/dm3), em três eventos (regas) consecutivos de chuva simulada na intensidade de 57 mm/h. A avaliação das concentrações mais adequadas dentre as testadas para cada condicionante foi baseada nas análises referentes à retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min) e à qualidade da água percolada (pH, oxigênio dissolvido, turbidez e sólidos). Na Etapa 2, foi avaliada, em vasos, a influência da presença de três espécies de plantas (Arachis pintoi; Raphanus sativus; Lavandula angustifolia) em dois tipos de meio: solo sem condicionadores; solo com condicionadores nas melhores concentrações indicadas na Etapa 1, sendo simulada apenas um evento de chuva de 57 mm/h. Foram analisados parâmetros biológicos (germinação; plantas sobreviventes; comprimento do caule e da raiz; pesos da biomassa do caule e da raiz); retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min); qualidade da água percolada (pH; oxigênio dissolvido; turbidez; sólidos; nitrato; amônia; fósforo total). Os resultados da Etapa 1 indicaram que o gel promoveu de forma significativa um aumento na retenção hídrica, e adiou o início da percolação de água, além de promover ligeira elevação do pH na água percolada. A adição de zeólita resultou em um aumento significativo da retenção hídrica, porém tal aumento não é vantajoso visto que este representa um custo adicional que poderia ser reduzido com o aumento da proporção do gel na coluna. A adição de fertilizantes não promoveu mudanças na qualidade da água percolada. Na Etapa 2, somente o efeito da presença de A. pintoi (maior produção de biomassa de raiz e caule) e R. sativus foram avaliadas. A presença dos condicionantes no solo proporcionou um desempenho significativamente superior em relação a retenção hídrica (altura do substrato e adiamento do pico de chuva) e qualidade da água percolada (pH e turbidez) quando comparados aos testes realizados na presença somente de solo. O fertilizante influenciou nas altas concentrações dos nutrientes (nitrogênio e fósforo) na água percolado nos resultados. A presença do gel no substrato, resultou numa capacidade superior de retenção de hídrica, e consequentemente no adiamento do pico de intensidade de chuva. Sendo assim, recomenda-se a aplicação do gel em telhados verdes para futuros estudos em ambientes externos. / Floods are natural phenomena that occur due to the large magnitude of rains, aggravated in urban areas by soil sealing and inefficient drainage systems. Green roofs emerge as a structural compensatory measure may retain part of the precipitated water, delaying the peak flow. The objective of this study was to develop a combination of soil and conditioners for green roof, promote a significant increase in water retention capacity and greater postponement of the peak stormwater runoff. This study was divided into two stages. In Step 1, were analyzed by percolation columns three conditioners in the following concentrations: Gel STOCKOSORB retainer (2; 4; 6 g / dm3) Osmocote slow-release fertilizer (4,7; 7,1; 9, 0 g / dm3) and zeolite (30; 50; 70 g / dm3), three events (watering) consecutive simulated rainfall intensity of 57 mm / hr. Evaluation of the most suitable among the concentrations tested for each condition was based on the analyzes for water retention (when the medium after watering, the flow delay time; mm retained; intensity of percolated water in mm / min) and the quality of percolated water (pH, dissolved oxygen, turbidity and solids). In Step 2, was evaluated in pots, the effect of the presence of three species of plants (Arachis pintoi, Raphanus sativus, Lavandula angustifolia) in two types of medium: no soil conditioners; best soil conditioners in concentrations indicated in Step 1, only one being simulated rainfall event of 57 mm / hr. Biological parameters were analyzed (germination, surviving plants, stem and root length, stem biomass and root weight); Water retention (after half the time of irrigation, the flow delay time; mm retained; intensity of percolated water in mm / min); quality of soil solution (pH, dissolved oxygen, turbidity, solids, nitrate, ammonia, total phosphorus). The Step 1 results indicated that the gel significantly promoted an increase in water retention, and delayed the start of the percolation of water, and promote slight increase of pH in soil solution. The addition of zeolite resulted in significant improvement of water retention, not as much as the retaining gel. The addition of fertilizers did not cause changes in the quality of the soil solution. In Step 2, only the effect of the presence of A. pintoi (higher biomass of root and stem) and R. sativus were evaluated. The presence of conditions on the ground provided a significantly better performance in relation to water retention (substrate height and postponement of peak rainfall) and quality of the soil solution (pH and turbidity) when compared to tests carried out in the presence only of soil. However, the influence on the high fertilizer concentrations of nutrients (nitrogen and phosphorus) in water leachate in the results, it is concluded that the presence of the gel on the substrate, resulting in a higher water retention ability, and therefore in delaying the peak intensity rain. Thus, the application of the gel is recommended for further studies to green roofs outdoors.

In der vorliegenden Arbeit wurden wesentliche Einflussfaktoren auf die Entwicklung von hochstämmigen, extensiv gepflegten Obstbäumen untersucht. Der direkte Einfluss von Klimafaktoren auf die Entwicklung der Gehölze konnte nachgewiesen werden. Dazu wurden neue Klimakennziffern definiert und durch dendrochronologische Untersuchungen Beziehungen zum Wachstum der Gehölze hergestellt. Weiterhin konnten komplexe Wechselwirkungen von klimatischen Einflüssen, Bodenwasserverhältnissen und dem Resistenzverhalten der Bäume gegenüber Winterkälte aufgezeigt werden. Für die hochstämmigen Obstbäume wurden in dem Zeitraum von mehr als 120 Jahren klima- und standortabhängige Negativ- und Positivweiserjahre aufgezeigt. Die Beziehungen zwischen den vegetativen Leistungen der Bäume und den Boden-/ und Bodenwasserverhältnissen wurden an ca. 50- , 100- und 200 jährigen Apfelbäumen untersucht und Zusammenhänge zu den Bewertungsmodellen der Reichsbodenschätzung (Bodenarten) und der Mittelmaßstäbigen landwirtschaftlichen Standortkartierung der DDR (Leitbodenformen) dargestellt. Die Gehölze zeigten standortabhängig unterschiedliche Wachstumsintensitäten. Die höchsten Zuwachsleistungen wurden an Grund- bzw. Stauwasser beeinflussten Standorten erzielt. Der Einfluss der Bodenarten an Wasser beeinflussten Standorten war innerhalb der Obstarten gering, zeigte aber Obstart spezifische Unterschiede. Die Apfelbäume erreichten auf sand- bzw. lehmüberlagerten Tonstandorten höhere Zuwachsleistungen als auf Deckton-Standorten. Bei der Obstart Birne waren die Wuchsleistungen auf Tonböden höher als an sand- bzw. lehmüberlagerten Tonstandorten. Wuchsdepressionen traten bei der Obstart Birne erst bei schweren Tonstandorten auf. Die Bedeutung der Leitbodenformen und Bodenarten trat an den Grund- bzw. Stauwasser fernen Standorten deutlich hervor. Von den untersuchten Leitbodenformen wiesen die Tieflehm- Fahlerden unabhängig von den Bodenarten die beste obstbauliche Eignung auf. Für den extensiven Anbau von Apfelbäumen auf den Leitbodenformen Sand-Rosterde und Sand-Braunerde sollten nur Standorte mit mehr als 28 Bodenpunkten verwendet werden (Bodenarten Sl 4D, Sl 3D, lS 4D,lS 3D und SL 4D). Das individuelle Verhalten von alten Apfelsorten in der vegetativen und generativen Leistung wurde auf einer starkwachsenden Klonunterlage untersucht. Eine Abhängigkeit der Zuwachsleistung der Bäume von den verwendeten Sorten, der Ertragsbildung und von den Witterungserscheinungen wurde nachgewiesen. / This thesis studied the factors that exercise essential influence on the development of tall fruit trees in extensive cultivation. We were able to prove that climatic factors directly influence the development of the trees. For achieving this we defined new climatic indicators and established relationships with the growth of the trees by means of dendro-chronological investigations. Further, we were able to prove that complex interactions exist between the climatic influences, soil water conditions and the resistance of the trees against cold in winter. For the tall fruit trees we defined negative and positive indicator years within a period of more than 120 years depending upon the climate and the location. The relationships between the vegetative performance of the trees and the soil/ and soil water conditions were studied in apple trees aged 50, 100 and 200 years and we were able to prove correlations with the evaluation models of the Reichsbodenschätzung (assessment of soil types in the German Reich) and the medium scale agricultural location mapping of the GDR (East Germany) (dominant soil forms). The growth intensity of the trees differed according to their location. The highest growth rates were reached in locations which were influenced by groundwater and/or perched water. At the locations that were influenced by water the type of soil had only minor influence within the same kind of fruit trees, however, we discovered specific differences between the individual kinds of fruit. On locations with clayey soil covered by sand or loam the apple trees reached higher growth rates than at locations where the top soil was clay. Pear trees reached higher growth rates on clayey soils than on clayey soils covered by sand or loam. Growth depressions occurred in pear trees only at locations with heavy clayey soil. Locations that were far from groundwater or perched water made the influence of the dominating soil forms and soil types very clear. From among the dominating soil forms which we investigated the pale soils with deep loam showed to be the most suitable for growing fruit trees irrespective of the kind of fruit. For extensive cultivation of apple trees on the dominating soil forms of sandy rusty soil and sandy brown soils should be used only locations with more than 28 points for soil quality (soil types S1 4D, S1 3D, IS 4D, IS 3D and SL 4D). We studied the individual behaviour of ancient apple species with respect to the vegetative and generative performance on a strongly growing clone stock. We were able to prove that the growth performance of the trees depends upon the chosen species, the yield formation and weather conditions.