Academic literature on the topic 'Vegetation erosion'

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Journal articles on the topic "Vegetation erosion"

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Starke, J., T. A. Ehlers, and M. Schaller. "Latitudinal effect of vegetation on erosion rates identified along western South America." Science 367, no. 6484 (2020): 1358–61. http://dx.doi.org/10.1126/science.aaz0840.

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Vegetation influences erosion by stabilizing hillslopes and accelerating weathering, thereby providing a link between the biosphere and Earth’s surface. Previous studies investigating vegetation effects on erosion have proved challenging owing to poorly understood interactions between vegetation and other factors, such as precipitation and surface processes. We address these complexities along 3500 kilometers of the extreme climate and vegetation gradient of the Andean Western Cordillera (6°S to 36°S latitude) using 86 cosmogenic radionuclide–derived, millennial time scale erosion rates and mu
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Goudie, A. S., and J. B. Thornes. "Vegetation and Erosion." Journal of Ecology 78, no. 4 (1990): 1157. http://dx.doi.org/10.2307/2260969.

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Grocholski, Brent. "Erosion-vegetation interactions." Science 367, no. 6484 (2020): 1336.8–1337. http://dx.doi.org/10.1126/science.367.6484.1336-h.

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Scheres, Babette, and Holger Schüttrumpf. "Investigating the Erosion Resistance of Different Vegetated Surfaces for Ecological Enhancement of Sea Dikes." Journal of Marine Science and Engineering 8, no. 7 (2020): 519. http://dx.doi.org/10.3390/jmse8070519.

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Dense grass covers are generally recommended for surface protection of sea dikes against mild and moderate hydraulic loads. The standard seeding mixtures were composed to meet the technical requirements and ensure dike safety. These mixtures are, however, limited in their species diversity. In the present study, four differently vegetated surfaces were tested regarding their erosion resistance against wave impacts and overflow. The test vegetations ranged from a species-poor grass-dominated reference mixture to species-rich herb-dominated mixtures. Two vegetations were reinforced with a three-
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Yang, Qi, Wen Nian Xu, Yu Ding, and Yue Shu Yang. "Experimental Study of Vegetation-Growing Concrete’s Resistance to Rain Erosion." Applied Mechanics and Materials 193-194 (August 2012): 1449–53. http://dx.doi.org/10.4028/www.scientific.net/amm.193-194.1449.

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Taking an experiment of vegetation-growing concrete’s resistance to rain erosion, the influence degree of the related factors on erosion amounts will be obtained. The erosion process of vegetation-growing concrete gunning slope is influenced by cement content, vegetation coverage, rainfall intensity and other factors. In this paper, it talks about the influence of different cement content, rain intensity and maintenance days on vegetation-growing concrete’s erosion. The results show that the anti-erosion ability of vegetation-growing concrete increases significantly with the increase of the ce
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Wei, Hui, Wenwu Zhao, and Han Wang. "Effects of Vegetation Restoration on Soil Erosion on the Loess Plateau: A Case Study in the Ansai Watershed." International Journal of Environmental Research and Public Health 18, no. 12 (2021): 6266. http://dx.doi.org/10.3390/ijerph18126266.

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Large-scale vegetation restoration greatly changed the soil erosion environment in the Loess Plateau since the implementation of the “Grain for Green Project” (GGP) in 1999. Evaluating the effects of vegetation restoration on soil erosion is significant to local soil and water conservation and vegetation construction. Taking the Ansai Watershed as the case area, this study calculated the soil erosion modulus from 2000 to 2015 under the initial and current scenarios of vegetation restoration, using the Chinese Soil Loess Equation (CSLE), based on rainfall and soil data, remote sensing images an
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Harliando, Dimas Prabowo, Chandra Setyawan, and Hanggar Ganara Mawandha. "Spatial Modeling of Vegetation Cover for Soil Erosion Control Based on Arc GIS and the RUSLE Models." Jurnal Teknik Pertanian Lampung (Journal of Agricultural Engineering) 12, no. 1 (2023): 14. http://dx.doi.org/10.23960/jtep-l.v12i1.14-27.

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Deforestation in the Serayu watershed, Central Java province, Indonesia for agriculture and other uses leaves only 0.73% of vegetation. It has triggered a number of problems such as soil loss (erosion), landslides, floods and sedimentation downstream. Environmental damage control needs to be applied through appropriate conservation programs. This study aims to understand the distribution of soil erosion and the effectiveness of soil erosion control by using vegetation cover. Soil erosion modeling and its correlation to vegetation cover was performed by using an Arc GIS based model of the Revis
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Sharma, Hemanti, and Todd A. Ehlers. "Effects of seasonal variations in vegetation and precipitation on catchment erosion rates along a climate and ecological gradient: insights from numerical modeling." Earth Surface Dynamics 11, no. 6 (2023): 1161–81. http://dx.doi.org/10.5194/esurf-11-1161-2023.

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Abstract. Precipitation in wet seasons influences catchment erosion and contributes to annual erosion rates. However, wet seasons are also associated with increased vegetation cover, which helps resist erosion. This study investigates the effect of present-day seasonal variations in rainfall and vegetation cover on erosion rates for four catchments along the extreme climate and ecological gradient (from arid to temperate) of the Chilean Coastal Cordillera (∼ 26–∼ 38∘ S). We do this using the Landlab–SPACE landscape evolution model to account for vegetation-dependent hillslope–fluvial processes
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Gyssels, G., J. Poesen, E. Bochet, and Y. Li. "Impact of plant roots on the resistance of soils to erosion by water: a review." Progress in Physical Geography: Earth and Environment 29, no. 2 (2005): 189–217. http://dx.doi.org/10.1191/0309133305pp443ra.

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Vegetation controls soil erosion rates significantly. The decrease of water erosion rates with increasing vegetation cover is exponential. This review reveals that the decrease in water erosion rates with increasing root mass is also exponential, according to the equation SEP e b RP where SEP is a soil erosion parameter (e.g., interrill or rill erosion rates relative to erosion rates of bare topsoils without roots), RP is a root parameter (e.g., root density or root length density) and b is a constant that indicates the effectiveness of the plant roots in reducing soil erosion rates. Whatever
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Thornes, J. B. "Coupling erosion, vegetation and grazing." Land Degradation & Development 16, no. 2 (2005): 127–38. http://dx.doi.org/10.1002/ldr.655.

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Dissertations / Theses on the topic "Vegetation erosion"

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Fernandes, Royston. "Wind erosion in presence of vegetation." Thesis, Bordeaux, 2019. http://www.theses.fr/2019BORD0194.

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La poussière minérale atmosphérique résultant de l’érosion éolienne des sols affecte le système terrestre. La distribution en taille (PSD) de cette poussière joue un rôle clé dans le bilan radiatif et la chimie atmosphérique, la formation des nuages et la productivité des écosystèmes terrestres et marins. Néanmoins les modèles climatiques peinent à reproduire précisément la PSD de la poussière émise. Ceci vient de la représentation imparfaite des mécanismes d’émission de poussières et des vitesses de vent de surface associées. C’est particulièrement vrai en présence d’éléments de rugosité de s
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Wynn, Theresa M. "The Effects of Vegetation on Stream Bank Erosion." Diss., Virginia Tech, 2005. http://hdl.handle.net/10919/11191.

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Riparian buffers are promoted for water quality improvement, habitat restoration, and stream bank stabilization. While considerable research has been conducted on the effects of riparian buffers on water quality and aquatic habitat, little is known about the influence of riparian vegetation on stream bank erosion. The overall goal of this research was to evaluate the effects of woody and herbaceous riparian buffers on stream bank erosion. This goal was addressed by measuring the erodibility and critical shear stress of rooted bank soils in situ using a submerged jet test device. Additional
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Thompson, Theresa M. "The Effects of Vegetation on Stream Bank Erosion." Diss., Virginia Tech, 2004. http://hdl.handle.net/10919/11191.

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Riparian buffers are promoted for water quality improvement, habitat restoration, and stream bank stabilization. While considerable research has been conducted on the effects of riparian buffers on water quality and aquatic habitat, little is known about the influence of riparian vegetation on stream bank erosion. The overall goal of this research was to evaluate the effects of woody and herbaceous riparian buffers on stream bank erosion. This goal was addressed by measuring the erodibility and critical shear stress of rooted bank soils in situ using a submerged jet test device. Additional
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Meyer, Andrew. "The impacts of nutria on vegetation and erosion in Oregon." Diss., Connect to online resource, 2006. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1433508.

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Collins, Daniel B. G. (Daniel Benjamin Gardiner) 1976. "Modeling the effects of vegetation-erosion coupling on landscape evolution." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/84316.

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Milodowski, David Thomas. "Erosion, vegetation and the evolution of hillslopes in upland landscapes." Thesis, University of Edinburgh, 2016. http://hdl.handle.net/1842/20438.

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The geomorphic and geochemical characteristics of landscapes impose a physical template on the establishment and development of ecosystems. Conversely, vegetation is a key geomorphic agent, actively involved both soil production and sediment transport. The evolution of hillslopes and the ecosystems that populate them, are thus intimately coupled; their co-dependence potentially has a profound impact on the way in which landscapes respond to environmental change. This thesis explores how rates of erosion, integrated over millennia, impact on the structural characteristics of the mixed conifer f
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Gonzales, Howell B. "Aerodynamics of wind erosion and particle collection through vegetative controls." Diss., Kansas State University, 2015. http://hdl.handle.net/2097/20382.

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Doctor of Philosophy<br>Biological & Agricultural Engineering<br>Mark E. Casada<br>Ronaldo G. Maghirang<br>Wind erosion is an important problem in many locations, including the Great Plains, that needs to be controlled to protect soil and land resources. This research was conducted to assess the effectiveness of vegetation (specifically, standing vegetation and tree barriers) as controls for wind erosion. Specific objectives were to: (1) measure sand transport and abrasion on artificial standing vegetation, (2) determine porosity and drag of a single row of Osage orange (Maclura pomifera) barr
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Holz, Dan. "FACTORS AFFECTING EROSION ON A NATURAL GAS PIPELINE IN THE CENTRAL APPALACHIANS." Available to subscribers only, 2009. http://proquest.umi.com/pqdweb?did=1885467581&sid=4&Fmt=2&clientId=1509&RQT=309&VName=PQD.

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Pasaribu, Nursahara. "Restoration of vegetation along a channelized stream." Virtual Press, 1995. http://liblink.bsu.edu/uhtbin/catkey/941378.

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The disturbed soil from a stream channelization project at Cooper Woods was used to evaluate the feasibility of establishing native grasses and forbs and their effectiveness in preventing soil erosion. Treatments included; 1- plots seeded, no application of herbicide, 2-plots seeded, herbicide applied, 3-unseeded and untreated control plots. The effect of variation in slope was assessed for each treatment. Cover and density were significantly different (Ps0.05) during the first and second year of sampling. No significant differences in mean total cover or mean density were attributed to slope
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Zhang, Xiaoyang. "Soil-erosion modelling at the global scale using remote sensing and GIS." Thesis, King's College London (University of London), 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321948.

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Books on the topic "Vegetation erosion"

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B, Thornes John, ed. Vegetation and erosion: Processes and environments. J. Wiley, 1990.

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Heede, Burchard H. Vegetation strips control erosion in watersheds. USDA Forest Service, Rocky Mountain Forest and Range Experiment Station, 1990.

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Watts, Jean. Erosion shoreline stabilization through vegetation planting. Division of Coastal Management, North Carolina Dept. of Natural Resources and Community Development, 1988.

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Khanbilvardi, Reza M. Erosion prediction in watersheds with tall vegetation. s.n, 1988.

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Styczen, Merete. Engineering properties of vegetation. M. Styczen, 1988.

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Paine, Jeffrey G. Shoreline and vegetation-line movement, Texas Gulf Coast, 1974 to 1982. Bureau of Economic Geology, University of Texas at Austin, 1989.

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Paine, Jeffrey G. Shoreline and vegetation-line movement, Texas Gulf Coast, 1974 to 1982. University of Texas at Austin, 1989.

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Garland, G. G. Erosion risk from footpaths and vegetation burning in the central Drakensberg. Natal Town and Regional Planning Commission, 1987.

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H, Gray Donald, ed. Landforming: Natural grading techniques for stability, erosion control, and re-vegetation. John Wiley, 2007.

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Jong, Steven M. de. Applications of reflective remote sensing for land degradation studies in a Mediterranean environment. Koninklijk Nederlands Aardrijkskundig Genootschap, 1994.

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Book chapters on the topic "Vegetation erosion"

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Wang, Zhao-Yin, Joseph H. W. Lee, and Charles S. Melching. "Vegetation-Erosion Dynamics." In River Dynamics and Integrated River Management. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-25652-3_3.

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Stokes, Alexia, Joanne E. Norris, L. P. H. van Beek, et al. "How Vegetation Reinforces Soil on Slopes." In Slope Stability and Erosion Control: Ecotechnological Solutions. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6676-4_4.

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Spaeth, Kenneth E. "Vegetation Effects on Hydrology and Erosion: Grazinglands." In Soil Health on the Farm, Ranch, and in the Garden. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40398-0_5.

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Dunkerley, David. "A Review of the Effects of Throughfall and Stemflow on Soil Properties and Soil Erosion." In Precipitation Partitioning by Vegetation. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29702-2_12.

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van Eerdt, Martha M. "The influence of vegetation on erosion and accretion in salt marshes of the Oosterschelde, The Netherlands." In Ecology of coastal vegetation. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5524-0_40.

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Jafari, Mohammad, Mohammad Tahmoures, Mohammad Ehteram, Majid Ghorbani, and Fatemeh Panahi. "The Role of Vegetation in Confronting Erosion and Degradation of Soil and Land." In Soil Erosion Control in Drylands. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-04859-3_2.

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Rutherfurd, Ian D., and James R. Grove. "The Influence of trees on stream bank erosion: Evidence from root-plate abutments." In Riparian Vegetation and Fluvial Geomorphology. American Geophysical Union, 2004. http://dx.doi.org/10.1029/008wsa11.

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Van De Wiel, Marco J., and Stephen E. Darby. "Numerical modeling of bed topography and bank erosion along tree-lined meandering rivers." In Riparian Vegetation and Fluvial Geomorphology. American Geophysical Union, 2004. http://dx.doi.org/10.1029/008wsa19.

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Spaeth, K. E., Mark A. Weltz, H. Dale Fox, and Frederick B. Pierson. "Spatial Pattern Analysis of Sagebrush Vegetation and Potential Influences on Hydrology and Erosion." In Variability in Rangeland Water Erosion Processes. Soil Science Society of America, 2015. http://dx.doi.org/10.2136/sssaspecpub38.c4.

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Li, Changjia, Bojie Fu, Shuai Wang, et al. "Structure and Functioning of China’s Dryland Ecosystems in a Changing Environment." In Dryland Social-Ecological Systems in Changing Environments. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-99-9375-8_12.

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AbstractChina has one of the largest dryland areas worldwide, covering 6.6 million km2 and supporting approximately 580 million people. Conflicting findings showing a drier China’s drylands with increasing aridity and observed greenness indicate the complexity of environmental processes, highlighting a pressing research need to improve understanding of how active dryland processes, ecosystem structure and functioning will alter. This chapter synthesizes the changes, impacts, and their drivers in China’s dryland ecosystems. Results from analyses covering the period 2000–2015 showed that 58.69%
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Conference papers on the topic "Vegetation erosion"

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Nilles, Alexander, Lars Günther, and Stefan Müller. "Oasis: A Real-Time Hydraulic and Aeolian Erosion Simulation with Dynamic Vegetation." In 20th International Conference on Computer Graphics Theory and Applications. SCITEPRESS - Science and Technology Publications, 2025. https://doi.org/10.5220/0013112100003912.

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Aydin, Elena. "THE HUMAN IMPACT ON THE STRUCTURE OF THE RIPARIAN VEGETATION IN THE RURAL AREA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/5.1/s20.37.

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Riparian vegetation of water streams represents dynamic ecosystem, which meets various functions. Since it forms a buffer zone between the aquatic and terrestrial ecosystems, it is of great importance in the ecological stability of landscape. Its importance is even higher nowadays when the effect of human activities on the environment is much stronger than in the past. The structure and quality of the vegetation comprising the riparian zone plays an important role in its ability to provide various ecosystem functions such as filtration of the sediment being transported by the surface runoff du
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Lackoova, Lenka, and Maria Tarnikova. "ASSESSING THE ROLE OF WINDBREAKS IN REDUCING WIND EROSION: REMOTE SENSING PERSPECTIVE." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/3.2/s13.31.

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Remote sensing (RS) imagery is widely used to assess and detect environmental changes in various areas and the numerous methods resulting from natural and human activities. To understand landscape change, including the role of windbreaks in agricultural regions, RS datasets are essential. Detected by the CORINE Land Cover (CLC) project, agricultural landscapes have undergone changes such as an increase in complex cropping patterns by 164.19% and in pastures by 15.3%, but a decrease in coniferous forest by 10.19% and in land mainly occupied by agriculture with significant areas of natural veget
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Neto, Beatriz, Pedro Santarem Andrade, and Antonio Neves Trota. "INSTABILITY CHARACTERIZATION OF THE GEOLOGICAL FORMATION "AREIAS E ARGILAS DE TAVEIRO" IN THE CONDEIXA AND COIMBRA AREAS (CENTRAL-WESTERN PORTUGAL)." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s02.24.

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The work aims to characterize the slope instabilities present in the Taveiro Sand and Clay - Areias e Argilas de Taveiro - Formation, which occurs in the municipalities of Condeixa and Coimbra, in central-western Portugal. The Areias e Argilas de Taveiro Formation, of Upper Cretaceous � Campanian - age, is made up of successions of metric layers of red, and brownish or pinkish pelites, interbedded with coarse arkosic sandstones. It has as maximum thickness of about 170 m. A total of 27 slopes with stability problems were counted in both municipalities, 16 in Coimbra and 11 in Condeixa. Several
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Eger, Andre, Olivia Burge, and Peter Almond. "Soil Erosion Rejuvenates Vegetation Community Composition." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.647.

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Zhang, Huayong, and Lu Han. "A Dynamic Relationship Between Vegetation and Erosion." In ASME 2008 International Mechanical Engineering Congress and Exposition. ASMEDC, 2008. http://dx.doi.org/10.1115/imece2008-67983.

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In order to give a comprehensive view about the essential relationship between vegetation and erosion, we employ an analysis of systemic dynamic stability based on vegetation-erosion equation raised by Thornes, and the further simulation about the equilibriums (fixed points) of the dynamic system can be given. We get four different types of the real equilibriums of the system. As well as this, the stability about all equilibriums is determined by systematic differential equation qualitative theory -Jacobi method. As a development of the original work of J.B.Thornes, this theoretical study high
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T. M. Wynn, S. Mostaghimi, H.E., and Elizabeth F. Alphin. "The Effects of Vegetation on Stream Bank Erosion." In 2004, Ottawa, Canada August 1 - 4, 2004. American Society of Agricultural and Biological Engineers, 2004. http://dx.doi.org/10.13031/2013.16423.

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Huang, Tousheng, Huayong Zhang, Xinqiang Zhu, Lei Zhao, and Lu Han. "A Study of Dynamical Model on the Competitive Relationship Between Soil Erosion and Vegetation Growth in Humid Regions." In ASME 2010 International Mechanical Engineering Congress and Exposition. ASMEDC, 2010. http://dx.doi.org/10.1115/imece2010-40775.

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In this study, a new dynamical model is established based on Thornes’ model. Then a detailed competitive and interactive relationship between soil erosion process and vegetation growth process is detected in humid regions. By employing the nonlinear dynamical analyses, a globally asymptotically stable equilibrium point is obtained under given parameters. This stable state indicates the vegetation growth process can coexist with soil erosion process. Furthermore, the transitions among different equilibrium states caused by the variation describe the competitive process in diverse environment. T
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Josifovski, Josif, Bojan Susinov, and Aleksandra N. Atanasovska. "Experimental and numerical modeling of soil-vegetation-atmospheric interaction on slopes and erosion control using biopolymers and vegetation." In 4th European Regional Conference of IAEG. University of Zagreb Faculty of Civil Engineering, 2024. https://doi.org/10.5592/co/euroengeo.2024.153.

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The impact of climate change on the infrastructure is alarming, thus creating several challenges that affect their lifespan and transport safety. The large temperature variations and more frequent intense rainfalls are seen as the main contributing factors for soil instabilities, landslides, and erosion. To understand the soil-vegetation-atmospheric interaction a holistic approach has been used that combines theoretical results and laboratory testing, as well as experimental and numerical modeling. The hypothesis that intense rainfalls can have a significant impact on slope stability has been
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Liu, Bing, Gang Xie, Xiaoming Zhang, Yang Zhao, Xiaolin Yin, and Chen Cheng. "Vegetation root system, soil erosion and ecohydrology system: A review." In 2015 International Forum on Energy, Environment Science and Materials. Atlantis Press, 2015. http://dx.doi.org/10.2991/ifeesm-15.2015.52.

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Reports on the topic "Vegetation erosion"

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Waugh, W. J., and S. O. Link. Barrier erosion control test plan: Gravel mulch, vegetation, and soil water interactions. Office of Scientific and Technical Information (OSTI), 1988. http://dx.doi.org/10.2172/6438624.

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Bryant, Duncan, Mary Bryant, and Alison Grzegorzewski. Erosion of coastal foredunes : a review on the effect of dune vegetation. Coastal and Hydraulics Laboratory (U.S.), 2017. http://dx.doi.org/10.21079/11681/21464.

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Bryant, Duncan, Mary Bryant, Jeremy Sharp, Gary Bell, and Christine Moore. The Response of Vegetated Dunes to Wave Attack. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41580.

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Vegetation is believed to increase the stability of dunes during wave attack, but limited data is available. A physical model study was performed to evaluate changes in the dune stability with and without biomass, both above and belowground. The above and belowground biomass was modeled using wooden dowels and coir fibers, respectively. For both the collision and overwash storm impact regimes, the results of this study clearly demonstrate that the inclusion of biomass in the model dune reduces the erosion and overwash. The combination of both above and belowground biomass was the most effectiv
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Bhattarai, Rabin, Yufan Zhang, and Owen Yao. Evaluation of Net-free Erosion Control Blankets. Illinois Center for Transportation, 2023. http://dx.doi.org/10.36501/0197-9191/23-026.

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Erosion control blankets (ECBs) protect soil from being detached and transported by raindrops and subsequential overland runoff while assisting in vegetation growth. ECBs have several characteristics, for example, thickness, mass per unit area, tensile strength, elongation, water absorption, etc. However, the impact of these characteristics on the performance in mitigating erosion has yet to be well understood. To better understand the interactions of ECB properties with the detachment and transport of sediment, field tests were conducted at the Erosion Control Research and Training Center at
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Field, John, Susannah Erwin, Christina Leonard, et al. Best practices for managing bank erosion within the National Park Service and National Wild and Scenic River System. National Park Service, 2025. https://doi.org/10.36967/2306106.

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Riverbank erosion is a natural process that occurs as rivers adjust to disturbance events and to changes in water and sediment delivery over time. The resulting lateral movement of river channels is fundamental to building complex, dynamic, and resilient landscapes. In this sense, bank erosion is crucial to creating healthy rivers and should be preserved whenever possible. However, river managers may deem protection from bank erosion necessary if bank retreat threatens infrastructure, developed land, or other valuable natural and cultural resources. The National Park Service manages over 220,0
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Thoma, David. Landscape phenology, vegetation condition, and relations with climate at Capitol Reef National Park, 2000–2019. Edited by Alice Wondrak Biel. National Park Service, 2023. http://dx.doi.org/10.36967/2297289.

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Quantitatively linking satellite observations of vegetation condition and climate data over time provides insight to climate influences on primary production, phenology (timing of growth), and sensitivity of vegetation to weather and longer-term patterns of weather referred to as climate. This in turn provides a basis for understanding potential climate impacts to vegetation—and the potential to anticipate cascading ecological effects, such as impacts to forage, habitat, fire potential, and erosion, as climate changes in the future. This report provides baseline information about vegetation pr
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Thoma, David. Landscape phenology, vegetation condition, and relations with climate at Canyonlands National Park, 2000–2019. Edited by Alice Wondrak Biel. National Park Service, 2023. http://dx.doi.org/10.36967/2299619.

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Abstract:
Quantitatively linking satellite observations of vegetation condition and climate data over time provides insight to climate influences on primary production, phenology (timing of growth), and sensitivity of vegetation to weather and longer-term patterns of weather referred to as climate. This in turn provides a basis for understanding potential climate impacts to vegetation—and the potential to anticipate cascading ecological effects—such as impacts to forage, habitat, fire potential, and erosion—as climate changes in the future. This report provides baseline information about vegetation prod
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Swanson, David, and Celia Hampton-Miller. Drained lakes in Bering Land Bridge National Preserve: Vegetation succession and impacts on loon habitat. National Park Service, 2023. http://dx.doi.org/10.36967/2296593.

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The northern coastal plain of Bering Land Bridge National Preserve (BELA) lost lakes at an alarming rate over the first two decades of this century, including four lakes over 100 ha in size in 2018-2019 alone. To understand the effects of these lake drainages, we sampled vegetation of these lakes in 2019 (a reconnaissance visit) and 2021 (for the installation of permanent vegetation monitoring plots). We used these data to summarize the changes that occurred in the first three years after drainage, and to create vegetation maps from 3-m resolution satellite images coinciding with the visit dat
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Herman, Brook, Paula Whitfield, Jenny Davis, et al. Swan Island resilience model development; Phase I : conceptual model. Engineer Research and Development Center (U.S.), 2023. http://dx.doi.org/10.21079/11681/46402.

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This report documents the development of an integrated hydrodynamic and ecological model to test assumptions about island resilience. Swan Island, a 25-acre island in Chesapeake Bay, Maryland, was used as a case study. An interagency, interdisciplinary team of scientists and engineers came together in a series of workshops to develop a simplified resilience model to examine the ability of islands to reduce waves and erosion and the impacts to nearby habitats and shorelines. This report describes the model development process and the results from this first key step: model conceptualization. Th
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Davis, Molly. Plant community composition and structure monitoring at Scotts Bluff National Monument: 2022 data report. National Park Service, 2023. http://dx.doi.org/10.36967/2295542.

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This report presents the results of vegetation monitoring efforts in 2022 at Scotts Bluff National Monument (SCBL) by the Northern Great Plains Inventory and Monitoring Network (NGPN) and Fire Ecology Program (NGPFire). NGPN began vegetation monitoring at SCBL in 2011, and this was the twelfth year of combined monitoring efforts between NGPN and NGPFire at SCBL. NGPN did not visit SCBL in 2020 or 2021 due to travel restrictions during the COVID-19 pandemic. However, NGPFire was able to do vegetation monitoring at SCBL during these two years. Crew members from NGPN visited eight long-term monit
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