Landfill facilities are required to have a barrier system that will limit escape of contaminants to groundwater and surface water for the contaminating lifespan of landfill. Heat generated by the biodegradation of waste and chemical reactions in landfills reduces the service-life of geomembranes by accelerating the ageing process of high-density polyethylene. It may also lead to the desiccation of clay components of the liners. Four considerations with respect to the evaluation of the potential effects of liner temperature on the service-life of liners and the potential control of liner temperature are examined. For the first time, the likely temperature and service-life of a secondary geomembrane in a double composite lining system is predicted. It is shown that, in some cases, the temperature is likely to be high enough to substantially reduce the service-life of the secondary geomembrane. The possible effectiveness of using tire chips as passive thermal insulation between the primary and secondary liners, as well as traditional soil materials, is then explored. For the barrier system and contaminant examined, the results show that tire chips could potentially lower the temperature of the secondary geomembrane sufficiently to significantly extend its service-life. However, the use of tire chips brings about other practical issues, which are also discussed in this study. An active alternative method of controlling the increase in the landfill liner temperature is then examined. This approach, which is inspired by geothermal heat pumps, involves an array of cooling pipes beneath the waste. Numerical modelling showed that the hypotetical introduction of the cooling pipes resulted in a reasonable decrease in liner temperature. It is suggested that the proposed technique warrants further consideration. Finally the conditions that may lead to the desiccation of geosynthetic clay liners used in composite liners due to waste generated heat are examined and recommendations regarding possible means of mitigating the effects of heat on the performance of GCLs are presented. For example, numerical modelling shows that the hydration of GCL prior to waste placement, liner temperature, overburden stress, depth to aquifer and moisture content and grain size of subsoil affect desiccation. / Thesis (Ph.D, Civil Engineering) -- Queen's University, 2011-07-31 07:34:33.165

A literature review of municipal solid waste landfill design was conducted to provide the knowledge base for development of an environmental decision support system (Landfill Advisor). Landfill Advisor integrates the current knowledge of barrier systems into a software program to assist in landfill design. The choices available for each liner component (e.g., drainage layer, geomembrane liner, compacted clay liner, geosynthetic clay liner) and their suitability for different situations (e.g., final cover, base liner, lagoon liner) are presented. Landfill Advisor covers both the design and related operational issues for municipal solid waste landfills, with consideration given to the interactions between components, operating conditions, and the natural environment with a view to maximization of long-term system performance. Unique to Landfill Advisor, the service life of each engineered component is estimated based on results from the latest research. Original research is also presented on the risk of geosynthetic clay liner (GCL) desiccation in low stress applications such as solar ponds. Numerical modelling was undertaken using a thermo-hydro-mechanical model with parameters that were developed and verified by comparison to previously reported laboratory data. A parametric study was performed to establish recommendations for future investigation. The water retention curve of the GCL was found to have a significant effect on the conditions that are expected to cause desiccation. The temperature coefficient of the water retention curve was also found to have a significant effect, yet this parameter is not well defined. Poisson’s ratio was found to affect the risk of desiccation in proportion to the applied stress. As reported by previous researchers, the initial degree of saturation of a GCL was found to be important to desiccation; however, the effect is diminished at low applied stress. / Thesis (Master, Civil Engineering) -- Queen's University, 2012-09-28 18:52:20.106

A presente pesquisa tem por objetivo desenvolver, montar e testar um equipamento de grandes dimensões (largura de 1,5 x 1,5 m e altura de 1,2 m) para o ensaio em laboratório de estruturas de pavimentos com materiais, espessuras de camadas e condições de carregamento similares às de campo. Ainda nesta pesquisa analisou-se o emprego de geossintético como reforço da camada de base de novos pavimentos sobre o efeito da variação da umidade do subleito. O carregamento cíclico é gerado a partir de um cilindro pneumático. A instrumentação é constituída de LVDTs, células de carga e de tensão total que permitem o monitoramento das cargas aplicadas, das tensões no interior das camadas, e deformações elásticas e permanentes na superfície do pavimento. O carregamento cíclico, com frequência de 1 Hz, foi aplicado sobre placas rígidas com diâmetros de 300 mm e 216 mm e magnitudes de 40 kN e 20 kN, respectivamente. A partir das bacias de deflexões obtidas, foi possível, por meio de retro-análise, a determinação dos módulos de resiliência dos materiais e a partir das curvas de recalque obter uma equação da deformação plástica em função do número de ciclos de carga. O equipamento apresentou bom funcionamento, atendeu às expectativas e os transdutores forneceram medidas com a precisão exigida. E a utilização de geogrelha como reforço de camada de base mostrou eficaz tanto na redução das deformações permanentes como elásticas. / This research aims at develop, assembly and test of application of large-scale equipment (width of 1.5 x 1.5 m and height of 1.2 m) for the testing in pavement structures laboratory, with materials, thicknesses of layers and loading conditions similar to the field ones. The research still studied the application of geosynthetics as base layer reinforcement to news pavements by effect of variation in subgrade layer moisture. The loading is cyclic and generated from a pneumatic actuator. The instrumentation is constituted of LVDTs, load-cells and soil pressure transducers that permit monitoring the applied loads and the stress distribution in the interior of the layers, as well as plastic and elastic deformations. The cyclic-loading (frequency of 1 Hz) was applied on a 30-mm-diameter and a 26-mm-diameter rigid plate with force of 40 kN and 20 kN, respectively. From the deflection basin obtained, it is possible, by means of back calculation, the determination of the resilient modulus of the materials and from the deformation basin obtained the equation of permanent deformation in function of the cycle number. The equipment showed a good operation, attended to the expectations and the transducers supplied measures with the precision required.

An investigation was conducted related to the dimensional stability of geosynthetic clay liners (GCLs) in landfill applications. Multiple occurrences of panel separation of overlap seams in GCLs have been documented; however, explanation for the relative contribution of various mechanisms causing shrinkage has been limited. A systematic test program was conducted to determine the effects of a variety of conditions on GCL dimensional stability. Effects of initial moisture content, permeant type, and overburden pressure were tested by subjecting various GCL products to wet-dry cycles and measuring the dimensional change with each cycle. Different GCL types were each tested under various combinations of initial moisture content (as-received, 50, 75, 100, and 125%), permeant types (tap water, distilled water, and 0.1 M CaCl2), and overburden pressures (0, 6, and 20 kPa). Thermal expansion tests were conducted by heating or cooling GCL test specimens to temperatures of 0, 10, 40, 60, and 80°C at constant moisture content. Subgrade tests were conducted by placing GCL test specimens on compacted clay and sand subgrades in different orientations and hydration conditions in sealed containers and measuring dimensional change over time. Mechanical necking tests were conducted by subjecting GCL specimens to varying levels of tension and measuring the longitudinal and transverse strains at each load increment. Field simulation tests were conducted by placing specimens on a compacted sand subgrade beneath an exposed geomembrane liner outdoors in late summer. Initial moisture content tests resulted in shrinkage strains as high as 20% after 20 wet-dry cycles. GCLs ranged from slightly anisotropic [approximately 1.1:1 ratio of machine (MD) to cross-machine (XMD) shrinkage] to highly anisotropic (approximately 3:1 ratio of MD to XMD shrinkage). Most combinations of GCL type and initial moisture content resulted in GCL MD shrinkage strains greater than a value that would cause panel separation (termed panel separation threshold, PST) at roll ends during the first wet-dry cycle. All test specimens contracted beyond the PST in the MD within 3 wet-dry cycles. GCL specimens without attached geomembranes contracted beyond the PST in the XMD within 5 cycles. Permeant type tests demonstrated that hydration with 0.1 M CaCl2 reduced shrinkage by 50-80% compared to permeation with tap water. Overburden tests demonstrated that applying 6 kPa and 20 kPa reduced specimen shrinkage by at least 60% and 80%, respectively. Thermal expansion tests indicated that temperature changes at constant moisture content had little effect on GCL dimensional stability. Subgrade tests demonstrated that subgrade type and moisture as well as GCL type and orientation had effects on dimensional stability. Tensile necking tests demonstrated that transverse shrinkage occurred due to tensile forces in GCLs, but shrinkage was nearly always less than PST. Field simulation tests demonstrated that wet-dry cycles in the field were less intense and/or less frequent than in the laboratory. Results of this testing provide a basis for GCL overlap specifications necessary to maintain full coverage and future research to confirm a suggested method of preconditioning bentonite to prevent shrinkage.

Geosynthetic tubes filled with a slurry-mix are considered. The mix is usually dredged from a nearby area and pumped directly into the tubes. The tubes are used in a variety of applications including breakwaters, groins, and temporary levees. This thesis considers single and stacked geosynthetic tubes resting on rigid and deformable foundations. A two-dimensional analysis is performed on the cross-section of a very long tube. The program Mathematica is utilized for the analysis. A few assumptions are made regarding the general behavior of the tube. The tube is assumed to be an inextensible membrane with no bending stiffness. To allow for a closed-form integral solution, it is assumed that no friction exists between the tubes and at the foundation. A single tube, two stacked tubes, and a 2-1 formation are studied. Both rigid and deformable foundations are considered. The deformable foundation is modeled as a tensionless Winkler foundation with normal forces proportional to the downward deflection of the ground. An external water load on one side is also investigated for a single tube and a 2-1 formation, with rigid blocks to prevent the structure from sliding along the ground. Example cross-sectional profiles are given. Results from the analysis include structure height, circumferential tension, and ground deflections. / Master of Science

Geosynthetic tubes have the potential to replace the traditional flood protection device of sandbagging. These tubes are manufactured with many individual designs and configurations. A small number of studies have been conducted on the geosynthetic tubes as water barriers. Within these studies, none have discussed the dynamics of unanchored geosynthetic tubes. A two-dimensional equilibrium and vibration analysis of a freestanding geosynthetic tube is executed. Air and water are the two internal materials investigated. Three foundation variations are considered: rigid, Winkler, and Pasternak. Mathematica 4.2 was employed to solve the nonlinear equilibrium and dynamic equations, incorporating boundary conditions by use of a shooting method. General assumptions are made that involve the geotextile material and supporting surface. The geosynthetic material is assumed to act like an inextensible membrane and bending resistance is neglected. Friction between the tube and rigid supporting surface is neglected. Added features of viscous damping and added mass of the water were applied to the rigid foundation study of the vibrations about the freestanding equilibrium configuration. Results from the equilibrium and dynamic analysis include circumferential tension, contact length, equilibrium and vibration shapes, tube settlement, and natural frequencies. Natural frequencies for the first four mode shapes were computed. Future models may incorporate the frequencies or combinations of the frequencies found here and develop dynamic loading simulations. / Master of Science

This study presents the climatic effects (rainfall and evaporation) on the stability of reinforced soil walls constructed with nonwoven geotextiles reinforcements using numerical modeling. The evaluation of the climatic effects was organized in two steps: (1) numerical modeling of the infiltration compared to a laboratory full-scale model of a nonwoven reinforced soil wall and; (2) a numerical investigation of a hypothetical geosynthetic-reinforced soil wall subjected to climatic changes including precipitation and evaporation, for a period of 2 years. The numerical modeling of infiltration into the full-scale model was conducted using two representative hydraulic parameters of backfill soil (suction and volumetric moisture content). The infiltration modeling of the laboratory reinforced structure was conducted to provide better understanding around the hydraulic behavior and water path into regions not measured by instrumentation during laboratory tests. Numerical calibration was conducted in order to capture the capillary break developed at soil-geotextile interfaces, including the anchorage of the reinforcements in the wrap-around facing. As a second step of this study, a hypothetical reinforced soil wall constructed with nonwoven geotextile was modeled using the same hydraulic properties of soil and geotextile used in the previously described numerical modeling. The climatic changes were simulated considering the water balance at ground surface. The climatic effects on the reinforced soil wall were assessed by the use of soil suction changes and consequent influences on the factors of safety over 2 years of operation. Results from numerical simulation of infiltration into the laboratory model indicated that water breakthrough did not occur uniformly along the length of the geotextile. In addition, numerical infiltration into the laboratory model showed that the water path into the reinforced zone is influenced by the anchorage of the reinforcement in the wrap-around facing. The results of the climatic variations in the hypothetical structure showed that approximately 50% of potential evaporation and total rainfall effectively evaporates and infiltrates. Also, the results revealed that the capillary barrier did not generate significant surface runoff and did not reduce the effective infiltration in the reinforced zone. On the other hand, water was observed to advance faster outside of the reinforced zone than inside of the reinforced zone because of the capillary barrier. Additionally, simulations showed that soil inside of the reinforced zone never recovered its initial suction value after first wetting because the capillary barrier restricted evaporation. Results also revealed that increases in global factor of safety, after first wetting of the geotextile reinforced soil wall, occurred because of the increases in soil suction of the first reinforced layer. Lastly, cumulative precipitation during successive days of rainfall showed some correlation to changes in global factor of safety. / Este estudo apresenta os efeitos das variações climáticas (chuva e evaporação) em muros de solo reforçado com geotêxtil não tecido através de analises numéricas. A avaliação dos efeitos climáticos foi dividida em duas fases: (1) calibração numérica da infiltração em um protótipo de laboratório de muro reforçado com geotêxtil não tecido e; (2) extrapolação dos resultados de infiltração para uma estrutura hipotética incluindo as variações climáticas de chuva e evaporação por um período de 2 anos. A calibração numérica foi realizada por meio de duas variáveis (sucção e umidade volumétrica) medidas durante a infiltração no protótipo. Estudos numéricos do processo de infiltração foram conduzidos para melhor entender o comportamento hidráulico da infiltração em regiões que não foram monitoradas durante a infiltração no protótipo. A calibração numérica foi conduzida com o objetivo de capturar o efeito da barreira capilar na interface solo-geotêxtil não tecido, incluindo a ancoragem do reforço próximo a face envelopada. A partir dos resultados da calibração, um muro hipotético reforçado com geotêxtil não tecido foi modelado sob condições climáticas reais (chuva e evaporação), e seu desempenho foi avaliado através das variações de sucção e do fator de segurança ao longo de 2 anos. As variações climáticas foram modeladas considerando o balanço de hídrico na superfície do solo. Os resultados da calibração numérica do modelo de laboratório indicaram que a barreira capilar na interface solo-reforço rompeu de forma não uniforme ao longo do geotêxtil não tecido. Além disso, a avaliação da infiltração mostrou que o fluxo de água tem sua direção afetada pela ancoragem do reforço próximo a face. Os resultados das variações climáticas na estrutura hipotética mostraram que aproximadamente 50% da evaporação potencial e da chuva total efetivamente evapora e infiltra. Além disso, os resultados revelaram que a formação de barreira capilar, e consequente retardo na infiltração, não gerou escoamento superficial significativo e não reduziu o volume de água efetivamente infiltrado na zona reforçada. Ademais, as variações de sucção observadas na zona reforçada se mostraram diretamente ligadas aos dias consecutivos de chuva. Por outro lado, observou-se que a frente de umedecimento avançou mais rápido fora da zona reforçada do que dentro da zona reforçada devido à barreira capilar. As simulações mostraram que o solo dentro da zona reforçada nunca recuperou seu valor inicial de sucção após o primeiro umedecimento porque a barreira capilar restringiu a evaporação. Os resultados também revelaram que o aumento no fator global de segurança, após o primeiro umedecimento do muro reforçado com geotêxtil, ocorreu devido ao aumento da sucção do solo da primeira camada reforçada. Por fim, a precipitação acumulada durante dias consecutivos de chuva mostrou correlação com as mudanças no fator de segurança.

Em geral, as recomendações normativas sugerem a utilização de materiais granulares para a construção de estruturas em solo reforçado, principalmente devido à sua elevada resistência ao cisalhamento e boa capacidade de drenagem. No entanto, nem sempre há disponibilidade deste tipo de material no entorno das obras, tornando o uso dos solos finos imperativo para a viabilização desta solução. No Brasil, solos residuais finos são encontrados em abundância e, muitas vezes, apresentam excelentes parâmetros de resistência ao cisalhamento e baixa compressibilidade. Contudo, o seu uso pode induzir poro-pressões indesejáveis durante a construção ou cisalhamento do aterro reforçado. Por outro lado, as elevadas sucções matriciais que podem persistir em seu interior geram um aumento na estabilidade dos maciços reforçados. Neste contexto, este trabalho apresenta os resultados experimentais e discute o efeito da variação climática (umedecimento e secagem) na resistência de interface solo coesivo-fita polimérica de uma estrutura de contenção em solo reforçado. Os ensaios foram realizados com amostras compactadas de um solo residual de gnaisse típico da cidade de São Paulo e uma fita polimérica de alta aderência. Os corpos de prova foram submetidos a ensaios de cisalhamento direto e de arrancamento sob três diferentes níveis de tensão normal e de sucção, além da condição inundada. Ensaios triaxiais saturados (CU) e não saturados (CW) foram realizados para a determinação da envoltória de resistência tridimensional do solo, avaliação da eficiência da interação solo-reforço e para a verificação do comportamento da água intersticial durante o cisalhamento. Os resultados indicam que o solo coesivo em questão apresenta excelentes parâmetros de resistência ao cisalhamento, elevada capacidade de se manter sob pressões negativas da água intersticial e uma eficiente interação com as fitas poliméricas, o que possibilitaria a execução de estruturas estáveis quanto ao arrancamento dos reforços. Além disso, sugerem um crescimento não linear da máxima resistência de interface com o aumento da sucção matricial do solo e uma tendência de redução dos coeficientes de atrito aparente solo-reforço (f*) com o umedecimento das amostras. Porém, mostraram que a sucção matricial exerce pouca influência na resistência residual da interface solo reforço. / Current specifications for reinforced soil structures generally require the use of granular backfill due to their high strength, well drainage capacity and low volume change potential. However, in cases where granular fills are not easily and readily available, poorly draining soils should be used to enable the implementation of a mechanically stabilized earth wall (MSEW). In Brazil, the fine-grained residual soils that cover large areas of its territory frequently present high shear strengths and low compressibility. However, the use of cohesive soils can cause unwanted effects in structure stability due to the water content variations of the backfill soil, and the potential development of pore-water pressures or loss of strength. On the other hand, matric suctions may increase the soil-geosynthetic interface shear strength. In this context, this study presents the experimental results and discusses the effects of seasonal climatic variations (wetting and drying) on shear strength of soil-geosynthetic straps interfaces under unsaturated conditions. For the laboratory investigation, a compacted residual soil of gneiss composed of 80% silty sand passed through a 0.075mm sieve, sourced from São Paulo city, and a high-tenacity polyester strap were used. Direct shear and pullout tests were conducted with three different net normal stresses and levels of matric suction, besides the inundated condition. Triaxial tests under saturated (CU) and unsaturated (CW) conditions with suction measurement using a high capacity tensiometer were performed in order to evaluate the shear strength parameters of the unsaturated soil, the interface efficiency of the soil-geosynthetic strap and the pore water pressure variations during shear. The results indicate that the cohesive soil used in this study has excellent shear strength parameters, a high capacity to maintain negative pore water pressures and presents an efficient interaction with the geosynthetics straps, which would allow the implementation of a stable MSEW for failure by pullout. Furthermore they reveal that the peak shear strength of the soil-geosynthetic strap interface increases nonlinearly with the soil suction, while the apparent friction factor (f*) decreases with the increase in molding moisture contents. On the other hand, the effect of suction on the post-peak shear strength of the interface was negligible.

The use of geosynthetic clay liners (GCLs) as (i) covers for arsenic-rich gold mine tailings and landfills, (ii) subsurface barrier for migration of hydrocarbons in the Arctic, and (iii) basal liner for sewage treatment lagoons were examined. After 4 years in field and laboratory experiments, it was found that best cover configuration above gold mine tailings might include a layer of GCL product with polymer-enhanced bentonite and a geofilm-coated carrier geotextile serving above the tailings under ≥ 0.7 m overburden. However, acceptable performance could be achieved with using a standard GCL with untreated bentonite provided that there is a minimum of 0.7 m of cover soil above the GCL. When GCL samples were exhumed from experimental landfill test cover with complete replacement of sodium in the bentonite with divalent cations in the adjacent soil, it was observed that the (i) hydraulic head across the GCLs, (ii) size of the needle-punched bundles, and (iii) structure of the bentonite can all significantly affect the value of the inferred in-situ hydraulic conductivity measured at the laboratory. The higher the hydraulic head and the larger the size of the needle-punched bundles, the higher the likelihood of internal erosion/structural change of bentonite at bundles that will cause a preferential flow for liquids to occur. A key practical implication was that GCLs can perform effectively as a single hydraulic barrier in covers provided that the water head above the GCL kept low. The hydraulic performance of a GCL in the Arctic was most affected by the location within the soil profile relative to the typical groundwater level with the highest increase in the hydraulic conductivity (by 1-4 orders of magnitude) for GCL below the water table. However, because the head required for jet fuel to pass through the GCL was higher than that present under field conditions, there was no evidence of jet fuel leakage through the barrier system. The leakage through GCLs below concrete lined sewage treatment lagoons was within acceptable limits, in large part, due to the low interface transmissivity between GCLs and the overlying poured concrete. / Thesis (Ph.D, Civil Engineering) -- Queen's University, 2014-02-28 08:53:29.171

Made available in DSpace on 2014-12-17T14:48:18Z (GMT). No. of bitstreams: 1 CarlindoABN_DISSERT.pdf: 3710968 bytes, checksum: c4cde6ddc0e6d0da8c608ea0713d3c5f (MD5) Previous issue date: 2014-02-21 / O controle sobre os processos erosivos ? uma necessidade constatada em v?rios segmentos da engenharia. A movimenta??o de terra necess?ria para a execu??o de taludes rodovi?rios, por exemplo, pode resultar em taludes de corte ou aterro vulner?veis ? eros?o superficial. Dentre as alternativas tecnol?gicas para controle de eros?o a utiliza??o de geossint?ticos se apresenta como uma solu??o potencial. A referida aplica??o encontra-se em amplo desenvolvimento em alguns pa?ses como, por exemplo, nos EUA. No Brasil, a especifica??o de geossint?ticos para controle de eros?o ? limitada pela aus?ncia de caracteriza??o desses produtos e de normas nacionais, sendo a ?nica fonte t?cnica de informa??o, os cat?logos dos fabricantes. Neste contexto, o objetivo deste trabalho ? construir um equipamento e desenvolver m?todos de ensaio para caracteriza??o e avalia??o de geossint?ticos utilizados no controle de eros?o superficial, com base na ASTM D7101. Al?m de um simulador de chuvas, o equipamento ? composto por uma bancada de testes formada por: rampa de escoamento, mesa de suporte e n?cleos de solo. Utilizando a bancada constru?da, foram realizados ensaios para avaliar o funcionamento do equipamento e o desempenho de uma geomanta na redu??o da taxa de eros?o superficial. Os ensaios foram realizados com intensidades de precipita??o de 100 ? 4mm/h e 150 ? 4mm/h, durante 30 minutos, com intervalo de leitura de 5 minutos. Os resultados obtidos nos ensaios sem a presen?a da geomanta mostraram uma perda de solo acentuada durante as chuvas simuladas, com uma iv tend?ncia de crescimento linear da perda de solo acumulada em fun??o do tempo de ensaio. Nos ensaios realizados com a presen?a da geomanta observou-se a a??o de prote??o do geossint?tico com uma redu??o da ordem de 90% da perda de solo acumulada para todas as intensidades de chuvas utilizadas / O controle sobre os processos erosivos ? uma necessidade constatada em v?rios segmentos da engenharia. A movimenta??o de terra necess?ria para a execu??o de taludes rodovi?rios, por exemplo, pode resultar em taludes de corte ou aterro vulner?veis ? eros?o superficial. Dentre as alternativas tecnol?gicas para controle de eros?o a utiliza??o de geossint?ticos se apresenta como uma solu??o potencial. A referida aplica??o encontra-se em amplo desenvolvimento em alguns pa?ses como, por exemplo, nos EUA. No Brasil, a especifica??o de geossint?ticos para controle de eros?o ? limitada pela aus?ncia de caracteriza??o desses produtos e de normas nacionais, sendo a ?nica fonte t?cnica de informa??o, os cat?logos dos fabricantes. Neste contexto, o objetivo deste trabalho ? construir um equipamento e desenvolver m?todos de ensaio para caracteriza??o e avalia??o de geossint?ticos utilizados no controle de eros?o superficial, com base na ASTM D7101. Al?m de um simulador de chuvas, o equipamento ? composto por uma bancada de testes formada por: rampa de escoamento, mesa de suporte e n?cleos de solo. Utilizando a bancada constru?da, foram realizados ensaios para avaliar o funcionamento do equipamento e o desempenho de uma geomanta na redu??o da taxa de eros?o superficial. Os ensaios foram realizados com intensidades de precipita??o de 100 ? 4mm/h e 150 ? 4mm/h, durante 30 minutos, com intervalo de leitura de 5 minutos. Os resultados obtidos nos ensaios sem a presen?a da geomanta mostraram uma perda de solo acentuada durante as chuvas simuladas, com uma iv tend?ncia de crescimento linear da perda de solo acumulada em fun??o do tempo de ensaio. Nos ensaios realizados com a presen?a da geomanta observou-se a a??o de prote??o do geossint?tico com uma redu??o da ordem de 90% da perda de solo acumulada para todas as intensidades de chuvas utilizadas