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Journal articles on the topic 'Vegetation erosion'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

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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2

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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3

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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5

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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10

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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11

Brocard, Gilles, Jane K. Willebring, and Fred N. Scatena. "Shaping of topography by topographically-controlled vegetation in tropical montane rainforest." PLOS ONE 18, no. 3 (2023): e0281835. http://dx.doi.org/10.1371/journal.pone.0281835.

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Topography is commonly viewed as a passive backdrop on which vegetation grows. Yet, in certain circumstances, a bidirectional feedback may develop between the control of topography and the spatial distribution of vegetation and landform development, because vegetation modulates the erosion of the land surface. Therefore, if reinforcing feedbacks are established between erosion and land cover distribution over timescales relevant to landform development, then the interactions between vegetation and topography may create distinctive landforms, shaped by vegetation. We expose here a strong correl

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12

Ma, Mengdi, Wenrui Huang, Sungmoon Jung, Christopher Oslon, Kai Yin, and Sudong Xu. "Evaluating Vegetation Effects on Wave Attenuation and Dune Erosion during Hurricane." Journal of Marine Science and Engineering 12, no. 8 (2024): 1326. http://dx.doi.org/10.3390/jmse12081326.

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This study employs the XBeach surfbeat model (XBSB) to explore the effects of vegetation on wave attenuation and dune erosion in a case study of Mexico Beach during Hurricane Michael. The XBSB model was validated against laboratory experiments of wave-induced dune erosion and wave attenuation by vegetation. In the case study of vegetation on dunes in Mexico Beach during Hurricane Michael, different vegetation drag coefficients were evaluated to investigate the effects of vegetation on wave attenuation and dune erosion. LiDAR data of dune profiles before and after Hurricane Michael were used fo

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13

Shaikh, Janarul, Sudheer Kumar Yamsani, Manash Jyoti Bora, et al. "Impact Assessment of Vegetation Growth on Soil Erosion of a Landfill Cover Surface." Acta Horticulturae et Regiotecturae 22, no. 2 (2019): 75–79. http://dx.doi.org/10.2478/ahr-2019-0014.

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Abstract Soil erosion is a very common phenomenon encountered at many sloped earthen geotechnical structures. For instance, the surface soil of an inclined landfill cover system undergoes the erosion due to various adverse atmospheric variants. This is one of the major causes for performance failure in the cover system. However, previous researchers have rarely conducted the study for field assessment of soil erosion in high rainfall tropical regions such as northeast India. The literature advocates the utilization of vegetation for erosion management. This study investigated the impact of veg

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Gholami, V., and M. R. Khalegi. "The impact of vegetation on the bank erosion (Case study: The Haraz River)." Soil and Water Research 8, No. 4 (2013): 158–64. http://dx.doi.org/10.17221/13/2012-swr.

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Vegetation establishment is a suitable biological method of erosion control. Bank erosion is one form of water erosion and its adverse effects include an increase in turbidity, degradation of riverbank lands, difficulties caused by sediments depositing in the downstream. The rate of riverbank erosion can be decreased by application of biological methods in sensitive reaches identified. In this study, a 3250 m section of the Haraz River was studied to evaluate the effects of vegetation establishment on shear stress, water velocity and finally on the bank erosion. In this research, Geographical

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Thakur, Kannan, Niraj Singh Parihar, and Hemant Sood. "Bio-stabilisation of slopes: A review." E3S Web of Conferences 596 (2024): 01019. http://dx.doi.org/10.1051/e3sconf/202459601019.

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Slope stability is essential for mitigating landslides and erosion risks, especially during heavy rainfall. Vegetation significantly enhances slope stability through soil reinforcement and erosion control. Plant roots stabilize the soil matrix, reducing the likelihood of shallow landslides. However, vegetation's impact varies, with different types potentially influencing slope stability differently—some may even worsen instability under specific conditions. Evidence shows that both rigid and flexible vegetation types improve erosion resistance and slope stability, making them a cost-effective

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16

F.A.Mamatkulova and G.T.Jalilova. "Differentiation of altitude-vegetation geosystems, taking into account the calculations of vegetation indices to improve the soil erosion monitoring system." International Journal of Advanced Biotechnology and Research 13, no. 4 (2022): 1–8. https://doi.org/10.5281/zenodo.7385229.

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Vegetation cover is one of the main factors that cause soil erosion. The lack of permanent vegetation cover leads to extensive soil erosion. Since loose, dry, bare soil is the most susceptible to the erosion process. The article provides material on the possibilities of calculating the vegetation indices NDVI and SAVI using remote sensing images of the research object for 1990, 2000, 2010, 2022. The results of the research made it possible to analyze the state of the flora distributed in the study area, as well as to develop measures aimed at protecting the flora. Based on the analysis of the

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17

Liao, Qiao, Yanhong Fan, and Yan Yan. "The Impact of Land Use and Vegetation Cover Changes on Soil Erosion in the Southwest Karst Region." Journal of Life Sciences and Agriculture 2, no. 1 (2025): 21–30. https://doi.org/10.62517/jlsa.202507104.

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This study investigates the impact of land use and vegetation cover changes on soil erosion in the Southwest Karst region from 2000 to 2020. The InVEST (Integrated Valuation of Ecosystem Services and Trade-offs) model was employed to estimate soil erosion, incorporating analyses of land use transition matrices and fractional vegetation cover (FVC) data. The findings reveal that severe erosion was the predominant erosion intensity; however, both its relative proportion and absolute area exhibited a declining trend. The proportion of severely eroded areas decreased from 92.14% in 2000 to 58.96%

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18

Hellens, Olgah, Dennis Masika, and Albert Long’ora. "The Effect of Land Cover Change on Soil Erosion in Awach Kibuon Sub-basin, Kenya." International Journal of Natural Resource Ecology and Management 9, no. 3 (2024): 82–96. http://dx.doi.org/10.11648/j.ijnrem.20240903.12.

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Land cover change is a significant driver of soil erosion. While soil erosion is a natural process, human activities can significantly alter the landscape, making soil more vulnerable to erosion. This erosion reduces a watershed&apos;s capacity to sustain vital natural resources and ecosystem services. This study investigated the impact of these changes on soil erosion within four hydrological units (Awach Kibuon, Awach Owade, Awach Kasipul, and Awach Kabondo) of the Awach Kibuon sub-basin between 2018 and 2023. The specific objective of the study was to quantify the effect of land cover c

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19

Song, Yantun, Ruixiang Liu, Qiong Yang, et al. "Effects of Patch Properties of Submerged Vegetation on Sediment Scouring and Deposition." Water 16, no. 15 (2024): 2144. http://dx.doi.org/10.3390/w16152144.

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Vegetation plays a key role in trapping sediments and further controlling pollutants. However, few studies were conducted to clarify the erosion and deposition laws of sediments and the influence factors caused by vegetation patch properties, which is not conducive to the revelation of riverbank protection and erosion prevention. Therefore, this study investigated the change in scouring and deposition characteristics around submerged vegetation patches of nine kinds of typical configurations and their influencing factors. Vegetation patches were assembled from three vegetation densities (G/d =

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20

Yang, Jun, Huilan Zhang, and Weiqing Yang. "Coupling Effects of Precipitation and Vegetation on Sediment Yield from the Perspective of Spatiotemporal Heterogeneity across the Qingshui River Basin of the Upper Yellow River, China." Forests 13, no. 3 (2022): 396. http://dx.doi.org/10.3390/f13030396.

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Interactions between precipitation, vegetation, and erosion are crucial and not fully solved issues in the area of earth surface processes. The Qingshui River Basin (QRB), as the main sediment source tributary of the upper reaches of the Yellow River, is characterized by spatial heterogeneity of rainfall, vegetation, and soil erosion. In this study, we investigated the spatiotemporal variations of sediment yields within the QRB and further identified the coupling effects of precipitation and vegetation on soil erosion. We collected annual (1955 to 2016) and daily (2006 to 2016) hydrological an

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21

Xiao, Jianyong, Binggeng Xie, Kaichun Zhou, et al. "Assessment of soil erosion in the Dongting Lake Basin, China: Patterns, drivers, and implications." PLOS ONE 16, no. 12 (2021): e0261842. http://dx.doi.org/10.1371/journal.pone.0261842.

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Soil loss caused by erosion is a global problem. Therefore, the assessment of soil erosion and the its driving mechanism are of great significance to soil conservation. However, soil erosion is affected by both climate change and human activities, which have not been quantified, and few researchers studied the differences in the driving mechanisms of soil erosion depending on the land use type. Therefore, the spatiotemporal characteristics and changing trends of soil erosion in the Dongting Lake Basin were analyzed in this study. Geographic detectors were used to identify the dominant factors

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22

Mansur, Maqsood, Reza Salatin, Tyler McCormack, Qin Chen, Julia Hopkins, and Patrick J. Dickhudt. "FIELD OBSERVATIONS AND MODELING OF BEACH CUSP EVOLUTION IN THE PRESENCE OF AN ARTIFICIAL VEGETATION PATCH." Coastal Engineering Proceedings, no. 37 (September 1, 2023): 26. http://dx.doi.org/10.9753/icce.v37.sediment.26.

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Vegetation has been shown to reduce beach erosion by attenuating wave energy and trapping sediments (Feagin et al., 2015). To date, most of the studies on erosion reduction by vegetation are either theoretical, numerical, or based on laboratory experiments. Field data that quantify the effectiveness of beach vegetation as a protective measure against erosion is sparse owing to the difficulty in conducting controlled field experiments (Feagin et al., 2015). To improve our understanding of wave-beach-vegetation interaction, we conducted a field experiment from September 19 to October 10, 2021, a

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23

Tong, Shengchun, Guorong Li, Xilai Li, et al. "Soil Water Erosion and Its Hydrodynamic Characteristics in Degraded Bald Patches of Alpine Meadows in the Yellow River Source Area, Western China." Sustainability 15, no. 10 (2023): 8165. http://dx.doi.org/10.3390/su15108165.

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Degraded bald patches have been active influencing factors in recent years, leading to meadow degradation and soil erosion in the Yellow River source area. In this study, we aimed to quantify the soil water erosion patterns and the hydrodynamic characteristics of degraded bald patches under different vegetation coverage (10%, 30%, 50%, 70% and 90%) and slope (10°, 20° and 30°) combination treatments through simulated rainfall experiments, and to investigate the influence of rodent activities on meadow degradation and soil erosion using zokor mound bare ground as a control. The results show tha

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24

Ewert, Megan, Ye Su, and Hu Wei Zhang. "Comparison of Two RUSLE Models at the Hillslope Scale in Experimental Plots in Haiyuan, Ningxia, China." Annals of Valahia University of Targoviste, Geographical Series 18, no. 2 (2018): 153–60. http://dx.doi.org/10.2478/avutgs-2018-0017.

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Abstract Topsoil erosion and mass soil losses from hillslopes have negatively affected water quality, vegetation health, local ecosystems, and livelihood. Studies have stated the effectiveness of vegetation in significantly reducing top-soil erosion and enhancing slope stability. This study aims to better understand the application of erosional models in Haiyuan of Ningxia, a semi-arid region of China. The study site is comprised of 20 experimental plots with 11 vegetation covers and 5 slope gradients in design, which were compared to the benchmark of bare land with each slope gradient. Meteor

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Guo, Jinwei, Yanbing Qi, Luhao Zhang, et al. "Identifying and Mapping the Spatial Factors That Control Soil Erosion Changes in the Yellow River Basin of China." Land 13, no. 3 (2024): 344. http://dx.doi.org/10.3390/land13030344.

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The Yellow River Basin has been considered to have the most serious soil erosion in the world, and identifying and mapping the spatial controlling factors would be of great help in adopting targeting strategies for soil erosion prevention. This study used the Universal Soil Loss Equation (USLE) to estimate the spatial and temporal changes in soil erosion from 1985 to 2020 and analyzed the controlling factors. The results indicated that from 1985 to 2020, the average erosion modulus in the Yellow River Basin was 1160.97 t∙km−2∙yr−1, and the erosion modulus in the middle reach was significantly

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Gao, Tian Ming, Rui Qiang Zhang, and Jian Ying Guo. "Research on Wind Erosion of Xilamuren Grassland, Inner Mongolia." Advanced Materials Research 955-959 (June 2014): 3505–8. http://dx.doi.org/10.4028/www.scientific.net/amr.955-959.3505.

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In northern China, grassland has degraded severely and wind erosion occurs remarkably due to irrational land use in recent years. By employing sand sampler and mobile wind tunnel, an observation for 6 years was made to analyze the mechanisms of wind erosion in Xilamuren grassland, the central of Yinshan Mountains, Inner Mongolia. Results show that: (1) vegetation is the decisive factor for controlling wind erosion and the inhibiting effect of vegetation height on wind erosion is greater than that of vegetation coverage. (2) Wind erosion modulus in the initial period of enclosure reaches 1313.7

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Luo, Zeyu, Huilan Zhang, Jianzhuang Pang, Jun Yang, and Ming Li. "Coupling of SWAT and EPIC Models to Investigate the Mutual Feedback Relationship between Vegetation and Soil Erosion, a Case Study in the Huangfuchuan Watershed, China." Forests 14, no. 4 (2023): 844. http://dx.doi.org/10.3390/f14040844.

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Identifying the feedback relationship between soil erosion and vegetation growth would contribute to sustainable watershed management. In order to study the long-term interaction between soil erosion and vegetation change, a comprehensive modeling framework was proposed by combining the Soil and Water Assessment Tool (SWAT) and the Environmental Policy Integrated Climate (EPIC) model. The Huangfuchuan Watershed was taken as an example area due to serious erosion and large-scale conversion of farmland to forest. Based on long-term variation analyses from 1956 to 2020, the effect of land cover c

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Wang, Li, Fan Zhang, Guanxing Wang, et al. "Response of Soil Erosion to Climate and Subsequent Vegetation Changes in a High-Mountain Basin." Sustainability 15, no. 4 (2023): 3220. http://dx.doi.org/10.3390/su15043220.

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Soil erosion is one of the global threats to the environment. Further, climate and vegetation changes have pronounced effects on soil erosion in high-mountain areas. In this study, the revised universal soil loss equation (RUSLE) was improved by developing a method for calculating snowmelt runoff erosivity based on a simulated snowmelt runoff and the observed sediment load, using which the soil erosion rate in the upper Heihe River Basin (UHRB) was calculated. The proposed approach provides an effective method for estimating the soil erosion rate and identifying the causes for its change in hi

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Herawati, Aktavia, Sutarno Sutarno, Mujiyo Mujiyo, and Yogi Sukma Mahendra. "Evaluasi Tingkat Bahaya Erosi Beberapa Penggunaan Lahan di Kecamatan Sidoharjo, Wonogiri, Jawa Tengah dengan Metode USLE (Universal Soil Loss Equation)." Pedontropika : Jurnal Ilmu Tanah dan Sumber Daya Lahan 8, no. 2 (2022): 36. http://dx.doi.org/10.26418/pedontropika.v8i2.56395.

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Erosion is one of the problems in agricultural activities. Soil erosion can cause loss of topsoil that contains nutrients for plants. The diversity of land use in agricultural activities affects the amount of erosion that occurs. This research aims to identify the level of erosion hazard in several agriculture land use and the determine factor of erosion, as well as provide direction for conservation in Sidoharjo District, Wonogiri, Central Java. This research is a survey research with exploratory descriptive approach based on the results of field observation and laboratory analysis. Sampling

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Edwards, Kevin J., and J. B. Thornes. "Vegetation and Erosion: Processes and Environment." Transactions of the Institute of British Geographers 17, no. 1 (1992): 123. http://dx.doi.org/10.2307/622645.

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31

Bernik, Brittany M., Maarten B. Eppinga, Alexander S. Kolker, and Michael J. Blum. "Clonal Vegetation Patterns Mediate Shoreline Erosion." Geophysical Research Letters 45, no. 13 (2018): 6476–84. http://dx.doi.org/10.1029/2018gl077537.

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Pearce, A. J. "Vegetation and erosion. Processes and environments." CATENA 19, no. 2 (1992): 260–61. http://dx.doi.org/10.1016/0341-8162(92)90029-b.

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Gonzales, Howell B., John Tatarko, Mark E. Casada, Ronaldo G. Maghirang, Lawrence J. Hagen, and Charles J. Barden. "Computational Fluid Dynamics Simulation of Airflow through Standing Vegetation." Transactions of the ASABE 62, no. 6 (2019): 1713–22. http://dx.doi.org/10.13031/trans.13449.

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Abstract. Maintaining vegetative cover on the soil surface is the most widely used method for control of soil loss by wind erosion. We numerically modeled airflow through artificial standing vegetation (i.e., simulated wheat plants) using computational fluid dynamics (CFD). A solver (simpleFoam within the OpenFOAM software architecture) was used to simulate airflow through various three-dimensional (3D) canopy structures in a wind tunnel, which were created using another open-source CAD geometry software (Salomé ver. 7.2). This study focused on two specific objectives: (1) model airflow throug

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Song, Gaofeng, Xiaoruan Song, Shiqin He, Dezhong Kong, and Shuai Zhang. "Soil Reinforcement with Geocells and Vegetation for Ecological Mitigation of Shallow Slope Failure." Sustainability 14, no. 19 (2022): 11911. http://dx.doi.org/10.3390/su141911911.

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Soil reinforcement using geocells and vegetation is one of the best forms of soil protection for shallow slope failure control. The geocell supports the vegetation growth and the vegetation cover provides protection against the surface erosion. This work proposed a soil treatment method using geocells for supporting the vegetation growth and stabilizing the shallow slope. A step-by-step installation of the geocells in the field and the development of vegetation growth were also described. The authors developed nine physical models that were reinforced with different sized geocell structures (n

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Maxwald, Melanie, Markus Immitzer, Hans Peter Rauch, and Federico Preti. "Analyzing Fire Severity and Post-Fire Vegetation Recovery in the Temperate Andes Using Earth Observation Data." Fire 5, no. 6 (2022): 211. http://dx.doi.org/10.3390/fire5060211.

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In wildfire areas, earth observation data is used for the development of fire-severity maps or vegetation recovery to select post-fire measures for erosion control and revegetation. Appropriate vegetation indices for post-fire monitoring vary with vegetation type and climate zone. This study aimed to select the best vegetation indices for post-fire vegetation monitoring using remote sensing and classification methods for the temperate zone in southern Ecuador, as well as to analyze the vegetation’s development in different fire severity classes after a wildfire in September 2019. Random forest

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Smets, T., J. Poesen, and E. Bochet. "Impact of plot length on the effectiveness of different soil-surface covers in reducing runoff and soil loss by water." Progress in Physical Geography: Earth and Environment 32, no. 6 (2008): 654–77. http://dx.doi.org/10.1177/0309133308101473.

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Covering the soil surface by rock fragments, organic mulches or vegetation is often done to reduce runoff and soil loss by water erosion compared to a bare soil treatment. The runoff or erosion-reducing effectiveness of these soil surface covers has been investigated for a range of plot lengths under different environmental conditions. Recent research indicates that the effectiveness of soil surface covers in reducing runoff and soil loss by water erosion may be affected by the size of the laboratory or field plots (ie, spatial scale). Therefore, the main objective of this review is to explore

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Zhang, Huayong, Qiang Meng, Qinjing You, Tousheng Huang, and Xiumin Zhang. "Influence of Vegetation Filter Strip on Slope Runoff, Sediment Yield and Nutrient Loss." Applied Sciences 12, no. 9 (2022): 4129. http://dx.doi.org/10.3390/app12094129.

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It is an important branch of erosion research to control soil erosion on eroded gullies and slopes by using vegetation filter strip. Several simulated rainfall experiments were carried out in soil tanks filled with loess sandy loam taken from a typical eroded gully area with less vegetation coverage in Yanghe hilly basin in Xuanhua District, Zhangjiakou City, Hebei Province. The soil and water conservation effects of two different vegetation setting modes were compared under the same vegetation strip width and different rainfall intensities and slopes. During the rainfall process, the changes

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Kong, Bo, and Huan Yu. "Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet." Scientific World Journal 2013 (2013): 1–7. http://dx.doi.org/10.1155/2013/636521.

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The freeze-thaw (FT) erosion is a type of soil erosion like water erosion and wind erosion. Limited by many factors, the grading evaluation of soil FT erosion quantities is not well studied. Based on the comprehensive analysis of the evaluation indices of soil FT erosion, we for the first time utilized the sensitivity of microwave remote sensing technology to soil moisture for identification of FT state. We established an estimation model suitable to evaluate the soil FT erosion quantity in Silingco watershed wetland of Northern Tibet using weighted summation method of six impact factors inclu

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Sarminah, Sri, Farha Shera Prititania, and Karyati . "Effect of Vegetation Diversity on Erosion Rate." AGRIFOR 17, no. 2 (2018): 355. http://dx.doi.org/10.31293/af.v17i2.3621.

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The climate in Indonesia is a tropical climate with high rainfall, making Indonesia vulnerable to erosion. In addition to high rainfall, vegetation, slope and soil types also affect erosion. This study aims to determine the Important Value of Species (NPJ), the relationship between rainfall and surface runoff and the mass of eroded soil and the level of erosion hazard at different vegetation densities. Important Value The highest types of the three dominating types in plot I were Schima wallichii 115.12%, Macaranga gigantea 69.38% and Cratoxylum sumatranum 44.69%. Whereas in plot II the highes

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Liu, Panpan, Bing Guo, Rui Zhang, and Longhao Wang. "Spatial–Temporal Evolution Pattern of Soil Erosion and Its Dominant Factors on the Loess Plateau from 2000 to 2020." Land 13, no. 11 (2024): 1944. http://dx.doi.org/10.3390/land13111944.

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Global changes have led to significant changes in soil erosion on the Loess Plateau. Soil erosion leads to the degradation of land resources and a decline in soil fertility, adversely affecting agricultural production and the socioeconomic situation. Therefore, revealing the spatiotemporal evolution patterns of soil erosion in the Loess Plateau region and investigating the influencing factors that contribute to soil erosion are crucial for its management and restoration. In this study, the RUSLE monthly model and the Geodetector model were utilized to reveal the spatiotemporal trends of soil e

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Saco, P. M., G. R. Willgoose, and G. R. Hancock. "Eco-geomorphology and vegetation patterns in arid and semi-arid regions." Hydrology and Earth System Sciences Discussions 3, no. 4 (2006): 2559–93. http://dx.doi.org/10.5194/hessd-3-2559-2006.

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Abstract. The interaction between vegetation and hydrologic processes is particularly tight in water-limited environments where a positive-feedback links water redistribution and vegetation. The vegetation of these systems is commonly patterned, that is, arranged in a two phase mosaic composed of patches with high biomass cover interspersed within a low-cover or bare soil component. These patterns are strongly linked to the redistribution of runoff and resources from source areas (bare patches) to sink areas (vegetation patches) and play an important role in controlling erosion. In this paper

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Liu, Zhi Yong, Xin Zhang, Ping Zhou, and Dan Wei. "Variability of Soil Erosion under Different Topographical and Vegetation Conditions in Upper Min River Watershed." Applied Mechanics and Materials 260-261 (December 2012): 796–803. http://dx.doi.org/10.4028/www.scientific.net/amm.260-261.796.

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Soil erosion by water is affected by soil factor, rainfall erosivity, geographical factors, vegetation cover factor, and support practice factors. On the basis of quantitative estimation of soil erosion in the Upper Min River (UMR) watershed (located in the Upper Yangtze River basin, Sichuan, China) by applying the Revised Soil Loss Equation (RUSLE) model, Geographical Information System (GIS) software, and Remote Sensing (RS) technology, we explored the effects of topography and vegetation on soil loss for better erosion control measures, and analyzed ecological restoration approaches for the

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Shi, Qian, Caiming Shen, Hongwei Meng, Linpei Huang, and Qifa Sun. "A 1640-Year Vegetation and Fire History of the Lake Haixihai Catchment in Northwestern Yunnan, Southwest China." Forests 14, no. 5 (2023): 990. http://dx.doi.org/10.3390/f14050990.

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Vegetation and fire archives of the late Holocene are essential for understanding the importance of natural and anthropogenic forcings on past and future vegetation successions as well as climate changes. Here we present a 1640-year record of vegetation and fire history of the Lake Haixihai catchment in northwestern Yunnan, southwest China. Pollen and charcoal analyses as well as XRF (X-ray fluorescence) analysis of lacustrine sediments from Lake Haixihai were employed to reveal its regional vegetation, forest fire, and soil erosion intensity changes over the last 1640 years. The results show

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Qin, Qi, Jiaguo Qi, Xiaoping Xin, Dawei Xu, and Ruirui Yan. "Enhanced Wind Erosion Control by Alfalfa Grassland Compared to Conventional Crops in Northern China." Agronomy 15, no. 2 (2025): 387. https://doi.org/10.3390/agronomy15020387.

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Wind erosion poses a significant challenge to agricultural sustainability in Northern China’s arid regions. This study investigated the effectiveness of alfalfa grassland versus conventional cropland in controlling wind erosion across nine study sites in three agroecological regions. Using Sentinel-2 satellite imagery and the Revised Wind Erosion Equation (RWEQ) model, we analyzed vegetation cover duration and quantified soil wind erosion from 2018 to 2020. The results showed that alfalfa grassland extended vegetation cover by 80 days annually compared to cropland, with most extension occurrin

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Chen, Jian Qiang, Man Quan Zhao, and Zhi Chen. "An Experimental Study of the Zhao He Grassland Soil Wind Erosion Characteristics on the Northern Foothills of Yin Shan Mountain." Advanced Materials Research 518-523 (May 2012): 4496–503. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.4496.

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The soil erosion test was carried out for the Zhao He grassland on the northern foothills of Yin Shan Mountain by the use of a portable wind erosion tunnel developed by Inner Mongolia Agricultural University, the variation low of soil wind erosion rate with the different wind speed and different arrangement in pairs of different soil moisture content and different vegetation coverage was obtained and the data analysis indicates that the anti-wind erosion characteristics of ground surface is most satisfactory when the vegetation coverage is 40%, soil moisture content 9.3% and the height of vege

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Feng, Biao, Huang Yong Zhang, Tou Sheng Huang, and Fei Fan Zhang. "Dynamics on the Interactions between Vegetable Growth and Water Erosion." Advanced Materials Research 864-867 (December 2013): 2550–53. http://dx.doi.org/10.4028/www.scientific.net/amr.864-867.2550.

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This research investigates the interaction between vegetation growth and water erosion by a new dynamic model. According to the theoretical and numerical analysis of the research, there are three cases of equilibrium distribution and their dynamics over time. And the dynamics between vegetation and erosion is disparate under the condition of different parameters. Every equilibrium point also has a unique distribution under every set of parameters. When there are two interior equilibriums, a critical curve exists and divides the system into two areas, one is coexistence area and another is domi

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Shaikh, Janarul, Sudheer Kumar Yamsani, Manash Jyoti Bora, Sanjeet Sahoo, Sreedeep Sekharan, and Ravi Ranjan Rakesh. "Influence of infiltration on soil erosion in green infrastructures." Acta Horticulturae et Regiotecturae 24, no. 1 (2021): 1–8. http://dx.doi.org/10.2478/ahr-2021-0018.

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Abstract Rainwater-induced erosion in green geotechnical infrastructures such as a multilayered landfill cover system (MLCS) is a severe concern in the current era. Although vegetation is a proven measure to control erosion in the MLCS, there are other factors such as infiltration rate which influence the control of the phenomenon. Most of the existing studies are limited to understand influence of vegetation on erosion control or infiltration rate alone. In this study, an attempt is made to incorporate infiltration measurements alongside vegetation cover to understand erosion in surface layer

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Wang, He, Xiaopeng Wang, Shuncheng Yang, et al. "Water Erosion Response to Rainfall Type on Typical Land Use Slopes in the Red Soil Region of Southern China." Water 16, no. 8 (2024): 1076. http://dx.doi.org/10.3390/w16081076.

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Land use and rainfall are two important factors affecting soil erosion processes. The red soil region of southern China is a representative region with high rainfall amounts and rapidly changing land use patterns where the water erosion process is sensitive to changes in land use and rainfall. To comprehensively understand the water erosion response to land use and rainfall in this region, a 6-year in situ experiment based on eight plots (bare land and seven typical land uses) was conducted from 2015 to 2020. The 320 rainfall events were divided into 4 types, and there were 3 main rainfall typ

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Jia, Hao, Xidong Wang, Wenyi Sun, et al. "Estimation of Soil Erosion and Evaluation of Soil and Water Conservation Benefit in Terraces under Extreme Precipitation." Water 14, no. 11 (2022): 1675. http://dx.doi.org/10.3390/w14111675.

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In recent years, soil erosion caused by water erosion has gradually increased due to the increase of extreme precipitation. In order to reduce soil erosion caused by extreme precipitation, it is necessary to monitor soil erosion and found out the factors that affect soil erosion under extreme precipitation. The objective of this study was to assess the amount of soil erosion, the damage degree of soil and water conservation measures and benefit evaluation under extreme precipitation in Henan Province. The results indicated that the ridges of terraces in two small watersheds had been damaged to

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Zhang, Hanbing, Yang Gao, Danfeng Sun, Lulu Liu, Yanzhi Cui, and Wenjie Zhu. "Wind Erosion Changes in a Semi-Arid Sandy Area, Inner Mongolia, China." Sustainability 11, no. 1 (2019): 188. http://dx.doi.org/10.3390/su11010188.

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Wind erosion is one of the major environmental problems in drylands. Identifying the dominant natural factors of wind erosion and using targeted treatment measures are the key steps in wind erosion control. Using Horqin Left Back Banner in China as a case study, we applied the revised wind erosion equation to simulate the spatial distribution of wind erosion in the semi-arid sandy area. Contribution assessment and constraint line analysis were used to investigate the contributions of driving forces to wind erosion changes. The results showed that the wind erosion in the whole area was reduced

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