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Journal articles on the topic 'Soil erosion'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

KISS, J. J., E. DE JONG, and H. P. W. ROSTAD. "AN ASSESSMENT OF SOIL EROSION IN WEST-CENTRAL SASKATCHEWAN USING CESIUM-137." Canadian Journal of Soil Science 66, no. 4 (1986): 591–600. http://dx.doi.org/10.4141/cjss86-059.

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Soil erosion in five Rural Municipalities of west-central Saskatchewan was assessed using cesium-137 as an indicator of soil redistribution. Native, noneroded soils across the study area were sampled to determine a baseline value for cesium-137 (2877 Bq m−2), which was used to predict the erosion of cultivated soils since the early 1960s. Soil redistribution estimates were calculated for idealized positions (upper, middle, lower) on medium-textured cultivated hillslopes, and for the total erosional portion of the hillslopes. Mean hillslope soil erosion rates were 23 ± 8 t ha−1 yr−1 for slopes

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2

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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3

Ola, A., I. C. Dodd, and J. N. Quinton. "Can we manipulate root system architecture to control soil erosion?" SOIL 1, no. 2 (2015): 603–12. http://dx.doi.org/10.5194/soil-1-603-2015.

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Abstract. Soil erosion is a major threat to soil functioning. The use of vegetation to control erosion has long been a topic for research. Much of this research has focused on the above-ground properties of plants, demonstrating the important role that canopy structure and cover plays in the reduction of water erosion processes. Less attention has been paid to plant roots. Plant roots are a crucial yet under-researched factor for reducing water erosion through their ability to alter soil properties, such as aggregate stability, hydraulic function and shear strength. However, there have been fe

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4

Lisetsky, Fyodor N., Pavel V. Goleusov, and Zhanna Ar Buryak. "Tolerable soils erosion losses and soil formation rates in the context of carbon balance regulation." Lomonosov Soil Science Journal 79, no. 3, 2024 (2024): 139–51. https://doi.org/10.55959/msu0137-0944-17-2024-79-3-139-151.

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Erosion-accumulation processes are realized through paragenetic processes of soil destruction, transport, redepo- sition and accumulation of pedosediments enriched in organic carbon. A promising approach in modern methods for substantiating permissible erosion losses of soils is the integration of assessments of the quality of soil resources, the rate of erosion and soil formation, including calculations of the balance of organic carbon in soils of agroeco- systems. The range of research tasks included: analysis of current integrated approaches to justify the permissible erosion losses of soil

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Jankauskas, B., and M. A. Fullen. "A pedological investigation of soil erosion severity on undulating land in Lithuania." Canadian Journal of Soil Science 82, no. 3 (2002): 311–21. http://dx.doi.org/10.4141/s01-058.

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It is essential that we can rapidly characterize soil erosion severity. This paper describes a field methodology to classify soil erosion severity on Dystric Albeluvisols in Lithuania. The goal was to assess cumulative soil loss due to the combined action of accelerated and natural soil erosion. Evaluation of soil erosion severity helps us understand which segments of the landscape are susceptible to erosion and therefore require soil conservation. Factors considered in evaluating soil erosion severity included the existing genetic soil horizons remaining after soil erosion processes, the esti

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6

Lin, Yunjie, Cheng Lin, Minghao Liu, and David Evans. "Soil structure effect on soil erosion potential." IOP Conference Series: Earth and Environmental Science 1334, no. 1 (2024): 012008. http://dx.doi.org/10.1088/1755-1315/1334/1/012008.

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Abstract Soil erosion poses a significant threat to water-related infrastructure such as bridges, dams, quays, and levees by detaching and transporting soil grains downstream, thereby compromising the structural support of these installations. While erosion damage is acknowledged in current design practices, understanding soil erosion parameters requires scrutiny. However, existing soil erosion databases mainly rely on reconstituted soil samples, which may differ substantially from in situ erosion due to alterations in soil structure. This study scrutinizes and contrasts the erodibilities of i

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7

Ismail, Fauzilah, Mazidah Mukri, and Zainab Mohamed. "Assessment of Soil Dispersibility Behaviour In-Relation to Soil Internal Erosion Resistance." Scientific Research Journal 5, no. 1 (2008): 39. http://dx.doi.org/10.24191/srj.v5i1.5652.

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A study was conducted to assess soil dispersibility behaviour in-relation to soil internal erosion resistance. Dispersive soils can be a problem for many geotechnical projects and structures. Water flowing in a crack of earth dam or infiltration of rainwater through the crack of slope surface with enough erosion energy can detach the soil particles into suspension and transport it along the movement that will lead to internal erosion process. Soil samples from sloping area within UiTM Shah Alam Campus were collected and a laboratory study was carried out to assess the soil dispersibility behav

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8

Belmana, Adel, Mekki Mellas, and Victor Cavaleiro. "Assessment of Coarse Soil’s Stability Towards Internal Erosion Case of Biskra’s Dam Soil." Civil and Environmental Engineering 20, no. 1 (2024): 332–48. http://dx.doi.org/10.2478/cee-2024-0026.

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Abstract Internal erosion is a phenomenon that occurs in soils constituting hydraulic structures under the influence of internal flow. This erosion occurs because of pipe erosion which becomes widespread, leading in some cases to the rupture of the structure. Soils susceptible to piping, generally have particle size instability. This study aims to provide an empirical understanding of the initiation and development of erosion in coarse soil obtained near Biskra’s dam in Algeria. To assess the soil’s dispersiveness chemical analyses such as SAR and PS were conducted, as well as the particle siz

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9

McHugh, Marianne. "Soil Erosion." Geographical Journal 165, no. 1 (1999): 113. http://dx.doi.org/10.2307/3060530.

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10

Busscher, Warren. "Soil Erosion." Soil Science 154, no. 4 (1992): 338. http://dx.doi.org/10.1097/00010694-199210000-00010.

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11

Pindral, Sylwia, and Marcin Świtoniak. "The usefulness of soil-agricultural maps to identify classes of soil truncation." Soil Science Annual 68, no. 1 (2017): 2–10. http://dx.doi.org/10.1515/ssa-2017-0001.

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Abstract Soil erosion led to the severe transformations of the soil cover of young morainic areas of northern Poland. Main alterations are connected with soil truncation on summits and in upper part of slopes, whereas at foot slopes and within depressions colluvial material is accumulated. Information and knowledge about the extent or intensity of erosion are mainly derived from sophisticated geospatial models or laborious field works. To reduce the effort associated with development of studies on erosion the use of easily available cartographic sources is required. The main aim of the paper i

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12

Mazăre, Mazăre, Anișoara Duma Copcea, Veaceslav Mazăre, and Victor Țiței. "ASSESSMENT OF ERODED AGRICULTURAL LAND IN IZGAR, CARAS SEVERIN COUNTY." "Annals of the University of Craiova - Agriculture Montanology Cadastre Series " 54, no. 1 (2025): 360–65. https://doi.org/10.52846/aamc.v54i1.1581.

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Soil erosion represents an urgent, acute and extremely threatening problem, not only for agriculture, but also for the entire national economy, but also for the state of landscapes and the environment in which man lives. Consequently, not only the agronomic and economic effects of soil erosion will be further analyzed, but also the ecological effects, which have been neglected until now. In essence, we can point out that soil erosion makes the soil water regime more unfavorable, generally affecting water runoff conditions and the hydrological situation of the area; a particular phenomenon call

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Sianturi, Ignatius Bennito, and Cherie Bhekti Pribadi. "IDENTIFIKASI SEBARAN TINGKAT BAHAYA EROSI DI DAS BRANTAS (WILAYAH ADMINISTRASI KOTA SURABAYA) TAHUN 2022." Jurnal Penginderaan Jauh Indonesia 4, no. 1 (2005): 38–46. https://doi.org/10.12962/jpji.v4i1.3449.

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Erosion is a critical environmental degradation event that has profound implications for agricultural productivity, ecosystem stability, and sustainable development. This study aims to quantify the rate of soil erosion in various agro-ecological zones and to evaluate the effectiveness of soil conservation practices. Given that soil conservation processes require predicting the rate of erosion that occurs, erosion rate modeling was conducted. The commonly used modeling of erosion rate values is often limited to modeling the rate of erosion caused by water, such as sheet erosion, gully erosion,

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14

BYTYQI, Valbon, and Tropike AGAJ. "SPATIAL ESTIMATION OF SOIL EROSION USING GEOSPATIAL TECHNIQUE – A CASE STUDY OF JANJEVA RIVER CATCHMENT (KOSOVO)." Carpathian Journal of Earth and Environmental Sciences 19, no. 2 (2024): 233–43. http://dx.doi.org/10.26471/cjees/2024/019/294.

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The aim of the study is to analyse the spatial estimation of soil erosion in a small size river catchment of Janjeva (Kosovo). Soil erosion is becoming a serious threat and its spatial estimation is crucial for soil resource protection and management. The Revised Universal Soil Loss Equation (RUSLE) methodology integrated with GIS techniques was applied to estimate the annual erosion rate. Different datasets including open-source data were used to find main components of soil erosion. The results show different soil erosion classes depending on lithological settings, landforms, climate conditi

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15

Hu, Yaxian, Wolfgang Fister, Yao He, and Nikolaus J. Kuhn. "Assessment of crusting effects on interrill erosion by laser scanning." PeerJ 8 (January 31, 2020): e8487. http://dx.doi.org/10.7717/peerj.8487.

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Background Crust formation affects soil erosion by raindrop impacted flow through changing particle size and cohesion between particles on the soil surface, as well as surface microtopography. Therefore, changes in soil microtopography can, in theory, be employed as a proxy to reflect the complex and dynamic interactions between crust formation and erosion caused by raindrop-impacted flow. However, it is unclear whether minor variations of soil microtopography can actually be detected with tools mapping the crust surface, often leaving the interpretation of interrill runoff and erosion dynamic

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16

S. Yu., Bulygin, and Bulygina M. E. "Methodology for assessing the danger of erosion and formation of soil protection agro-landscapes." Mehanization and electrification of agricultural, no. 15(114) (2022): 189–205. http://dx.doi.org/10.37204/0131-2189-2022-15-25.

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Purpose. On the basis of an in-depth analysis of the erosion safety of the soil cover of Ukraine, to determine the theoretical and applied principles of the formation of an agrolandscape with guaranteed soil protection, mainly by engineering methods. Methods. System comparative analysis of erosion hazard. Mathematical modeling of erosion processes. Physical simulation of anti-corrosion protection. Results. The main causes of progressive soil erosion in Ukraine have been revealed. Classified distributed soil erosion by types and species. The main reason for the development of erosion processes

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17

Gong, Feng Wen, and Li Yuan. "Study on the Soil Erosion Dynamic Changes in Songhuajiang River Watershed Based on RS and GIS." Advanced Materials Research 347-353 (October 2011): 1268–71. http://dx.doi.org/10.4028/www.scientific.net/amr.347-353.1268.

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Based on the RS and GIS, the main data resource of Landsat TM image (1995 and 2005a) was used to study the soil erosion’s spatial-temporal dynamic changes. The results shown that: the reduced area of micro-level and slight soil erosion was 190.8 and 640 km2; the increased area of moderate and intensity soil erosion was 168 and 663 km2, the preserving ratio of micro-level erosion was greatest, intensity soil erosion’s persevering ratio was smallest, the transfer-out probability from intensity to micro-level soil erosion was greatest, the study results could give us some advice on making rationa

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18

Liu, Man, and Guilin Han. "Distribution of soil nutrients and erodibility factor under different soil types in an erosion region of Southeast China." PeerJ 9 (June 16, 2021): e11630. http://dx.doi.org/10.7717/peerj.11630.

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Background Soil erosion can affect the distribution of soil nutrients, which restricts soil productivity. However, it is still a challenge to understand the response of soil nutrients to erosion under different soil types. Methods The distribution of soil nutrients, including soil organic carbon (SOC), soil organic nitrogen (SON), and soil major elements (expressed as Al2O3, CaO, Fe2O3, K2O, Na2O, MgO, TiO2, and SiO2), were analyzed in the profiles from yellow soils, red soils, and lateritic red soils in an erosion region of Southeast China. Soil erodibility K factor calculated on the Erosion

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19

Vopravil, J., M. Janeček, and M. Tippl. "Revised soil erodibility K-factor for soils in the Czech Republic." Soil and Water Research 2, No. 1 (2008): 1–9. http://dx.doi.org/10.17221/2100-swr.

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In the territory of the Czech Republic there are more than 50% of agricultural soils exposed to water erosion; it is a very urgent problem both at present and for the future. It must be solved now when there is still something to be protected. It is rather complicated to describe the soil properties in terms of soil susceptibility to water erosion because it is a complex relation in which many factors participate. For the complex evaluation of all main factors participating in erosion origination it is possible to apply the Universal Soil Loss Equation (USLE). It consists of six factors intera

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20

Chen, Xianghua, Wenxin Chen, Liyuan Zhao, and Yekai Chen. "Influence of Buried Pipeline Leakage on the Development of Cavities in the Subgrade." Buildings 13, no. 7 (2023): 1848. http://dx.doi.org/10.3390/buildings13071848.

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The rapid pace of urbanization has led to an increasing frequency of road collapses, posing a significant threat to urban traffic safety. Underground pipeline leakage stands out as the primary cause of such collapses. This paper presents a macroscopic analysis of the subgrade seepage erosion process caused by pipeline leakage. Model tests were conducted to investigate the formation mechanism and explore the influence of water level, water flow rate, and soil type. The study revealed that the subgrade seepage erosion caused by pipeline leakage undergoes four distinct stages: infiltration, slow

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Mai, Jianjun, Zijun Wang, Feinan Hu, Jinghua Huang, and Shi-wei Zhao. "Study on soil hydraulic properties of slope farmlands with different degrees of erosion degradation in a typical black soil region." PeerJ 11 (October 5, 2023): e15930. http://dx.doi.org/10.7717/peerj.15930.

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In order to explore the impact of soil erosion degradation on soil hydraulic properties of slope farmland in a typical black soil region, typical black soils with three degrees of erosion degradation (light, moderate and heavy) were selected as the research objects. The saturated hydraulic conductivity, water holding capacity and water supply capacity of the soils were analyzed, as well as their correlations with soil physicochemical properties. The results showed that the saturated hydraulic conductivity of black soils in slope farmlands decreased with erosion degradation degree, which was hi

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22

S, Paramananthan, Nurfashareena Muhamad, and Joy Jacqueline Pereira. "Soil Related Factors Controlling Erosion And Landslides In Malaysia." Bulletin Of The Geological Society Of Malaysia 72 (November 15, 2021): 165–75. http://dx.doi.org/10.7186/bgsm72202113.

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The high temperature and rainfall in Malaysia results in intensive tropical weathering and depending on the parent material, the resultant soil can have deep or shallow soil profiles. Thus, a variety of soils can form with different textures (clay content), structure and porosity. With the high rainfall, soils in steep terrain are subjected to surface erosion when exposed or landslides if the rainwater percolates into the soil profile. Key soil-related factors controlling soil erosion and landslides include local climate, parent material of soils and depth of the weathered profile. Slope and g

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23

Smirnova, M. A., A. P. Zhidkin, N. I. Lozbenev, E. A. Zazdravnykh, and D. N. Kozlov. "Digital mapping of erosion degree of soils using the factor - property and factor - process - property models (the south of the Central Russian upland)." Dokuchaev Soil Bulletin, no. 104 (December 3, 2020): 158–98. http://dx.doi.org/10.19047/0136-1694-2020-104-158-198.

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Soil degradation resulting from water erosion poses a serious threat to food and environmental security, therefore the research of soil erosion features and soil erosion mapping do not lose their relevance. The paper presents the results of large-scale digital mapping of the erosion degree of the arable soils in the Prokhorovsky district of the Belgorod region (85 thousand hectares), based on two approaches: (1) linking the factors of erosion-accumulative processes and the erosion degree of soil directly (factor -property model), and (2) due to imitation erosion model WaTEM/SEDEM (factor - pro

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Banu, Shaziya, and Mousa Attom. "Internal Erosion Stabilization of Cohesionless Soil Using Lime." Water 15, no. 11 (2023): 1992. http://dx.doi.org/10.3390/w15111992.

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Soil embankments are valuable for the adequate reserve and supply of water to multiple industries. However, they are susceptible to internal soil erosion, which may ultimately lead to structural collapse. To counteract this issue, soil stabilization is practiced in the construction industry. This paper proposes the internal erosion stabilization of cohesionless soil using quicklime. For this research, two cohesionless soil types were investigated and treated with quicklime: poorly graded and well-graded cohesionless soils. For poorly graded soil, the lime percentage varied from 0.0% to 6.0% ba

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25

Kravchenko, R., and D. D. Guerrero. "Comparative analysis of the eroded soils on the slopes of the Calderon region, Ecuador." Bulletin of Science and Practice, no. 3 (March 15, 2017): 148–52. https://doi.org/10.5281/zenodo.399186.

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The paper presents the comparative analysis of the eroded soils on slopes. The analysis is based on the materials of field investigations and soil erosion loss models. The developed and earlier approved mathematical soil erosion models proved not to be effective for the Equatorial Andes zone. The results, in relative measurements, may be taken into consideration only as the prerequisites for potential soil erosion loss and be primarily used to support the choice of a key–site for field investigations. The slope soils vulnerable to erosion were investigated. It is revealed that the soils are po

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Achasov, Andrii, Alla Achasova, Ganna Titenko, Oleg Seliverstov, and Vladimir Krivtsov. "Assessment of the Ecological Condition of Soil Cover Based on Remote Sensing Data: Erosional Aspect." SHS Web of Conferences 100 (2021): 05014. http://dx.doi.org/10.1051/shsconf/202110005014.

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Soil erosion by water is the most important global environmental problem. A modern system for assessing and monitoring soil erosional degradation should be based on the use of remote sensing data. This raises the issue of correct data decoding. The article proposes a method for visual interpretation of eroded soils according to the Sentinel image obtained in the visible range. The authors give some combinations of decoding signs to determine the manifestations of linear and surface water erosion from images. The article shows possible errors in decoding the manifestations of water erosion and

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Haskevych, Oksana. "Pasmove Pobuzhzhia agricultural landscape soil heterogeneity." Visnyk of the Lviv University. Series Geography 53 (December 18, 2019): 97–103. http://dx.doi.org/10.30970/vgg.2019.53.10659.

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Pasmove Pobuzhzhia belongs to the territories of long agricultural development. Plowing of the slope lands, combined with favourable natural factors, leads to the development of processes of water erosion and the formation of soils ranges of various degrees of erosion, which increases soil heterogeneity. The article analyzes the manifestation of the soil heterogeneity at the level of elemental soil ranges (ESR) of dark gray podzolized soils. The consequence of erosion processes is the isolation of soil ranges of various degrees of erosion. To describe soil ranges, the article gives their area,

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Djalilova, G., F. Mamatkulova, and Z. Mamatkulova. "Long-term Monitoring of the Vegetation Cover of Mountain Territories in the GIS for Soil and Landscape Study of Territories." Bulletin of Science and Practice 7, no. 3 (2021): 33–41. http://dx.doi.org/10.33619/2414-2948/64/03.

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Rational use of natural resources and preservation of environment in good conditions are the basis of stable state of the ecosystem. Mountain soil erosion is the most common process of degradation. Soil protection from erosion is becoming a global problem in the world, and in Uzbekistan, in particular. Natural conditions of the region create a potential danger of soil erosion. The reason for its manifestation is the misuse of land, non-compliance with necessary requirements for soil protection. In most cases, it is due to the location of homesteads and crops on erosion-prone soils that poorly

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Shojaeezadeh, Shahab Aldin, Malik Al-Wardy, Mohammad Reza Nikoo, et al. "Historical Hazard Assessment of Climate and Land Use–Land Cover Effects on Soil Erosion Using Remote Sensing: Case Study of Oman." Remote Sensing 16, no. 16 (2024): 2976. http://dx.doi.org/10.3390/rs16162976.

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Human activities, climate change, and land-use alterations accelerated soil erosion in recent decades and imposed significant threats to soil fertility and stability worldwide. Understanding and quantifying the spatiotemporal variation of soil erosion risks is crucial for adopting the best management practices for surface soils conservation. Here, we present a novel high-resolution (30 m) soil erosion framework based on the G2 erosion model by integrating satellite and reanalysis datasets and Machine Learning (ML) models to assess soil erosion risks and hazards spatiotemporally. The proposed m

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Savelieva, D. A., and V. K. Kalichkin. "Application of digital technologies in the study of water erosion of soils in Western Siberia." Siberian Herald of Agricultural Science 49, no. 4 (2019): 86–100. http://dx.doi.org/10.26898/0370-8799-2019-4-10.

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The analysis of the study of water erosion of soils on the territory of the West Siberian Plain using geo-information technologies (GIS) and Earth remote sensing was carried out. It is shown that GIS and Earth remote sensing are not widely used in erosion studies in Western Siberia and are used by a limited number of modern researchers. However, the use of digital technologies in this area is characterized by the coverage of almost the full range of their capabilities and functions: digital mapping, the formation of spatially-distributed thematic databases, monitoring, space-time analysis, mod

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Eltner, Anette, David Favis-Mortlock, Oliver Grothum, Martin Neumann, Tomáš Laburda, and Petr Kavka. "Using 3D observations with high spatio-temporal resolution to calibrate and evaluate a process-focused cellular automaton model of soil erosion by water." SOIL 11, no. 1 (2025): 413–34. https://doi.org/10.5194/soil-11-413-2025.

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Abstract. Future global change is likely to give rise to novel combinations of the factors which enhance or inhibit soil erosion by water. Thus, there is a need for erosion models, necessarily process-focused ones, which are able to reliably represent the rates and extents of soil erosion under unprecedented circumstances. The process-focused cellular automaton erosion model RillGrow is, given initial soil surface microtopography for a plot-sized area, able to predict the emergent patterns produced by runoff and erosion. This study explores the use of structure-from-motion photogrammetry as a

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Sharafi, Saeed, Mehdi Mohammadi Ghaleni, and Deirdre Dragovich. "Simulated Runoff and Erosion on Soils from Wheat Agroecosystems with Different Water Management Systems, Iran." Land 12, no. 9 (2023): 1790. http://dx.doi.org/10.3390/land12091790.

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In developing countries, the demand for food has increased with significant increases in population. Greater demands are therefore being placed on the agricultural sector to increase production. This has led to increased soil erosion, especially in arid and semi-arid regions. The aim of this study was to simulate runoff and erosion on soils of three different wheat agroecosystems (rainfed farming, traditional irrigation, and industrial irrigation systems). The effect of variations in soil texture, slopes (1, 3 and 5%) and rainfall intensity (10, 25 and 40 mm h−1) on runoff volume, runoff coeff

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Hamanaka, Akihiro, Takashi Sasaoka, Hideki Shimada, and Shinji Matsumoto. "Experimental study on soil erosion under different soil composition using rainfall simulator." Plant, Soil and Environment 65, No. 4 (2019): 181–88. http://dx.doi.org/10.17221/68/2019-pse.

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Soil erosion is one of the major environmental problems in open-cut mines in tropical regions. It causes negative impacts including the removal of nutrient-rich topsoil, destroys aquatic habitat, dam and pond siltation, clogs river by deposition of sediment, and causes water pollution in the rehabilitation process. Soil texture is an important factor to affect soil erosion. In this study, artificial rainfall experiment in the laboratory scale was conducted to clarify the mechanism of soil erosion under the different soil composition and to discuss the methods for minimizing soil erosion. The o

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Makarov, Oleg A., Valery V. Demidov, Dina V. Karpova, et al. "Economic assessment of eroded soils: current state and development prospects." Lomonosov Soil Science Journal 79, no. 3, 2024 (2024): 7–18. https://doi.org/10.55959/msu0137-0944-17-2024-79-3-7-18.

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Summary Soil erosion as one of the types of land degradation aff ects various economic interests of people. It is shown that the most promising areas of erosion studies, where economic methods can be applied, are — assessment of actual damage fr om soil erosion, determination of the magnitude of probable damage from the occurrence of erosion processes in soils, economic analysis in the development of sustainable land use systems for territories whose soils are subject to erosion. Th e group of methods for determining economic damage is characterized by the greatest development, including takin

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Aliyev, Z. "Soil erosion research on determining the extent of the potential dangers of mountain-brown soils of the Quba-Khachmaz zone of Azebajdzhan." Bulletin of Science and Practice, no. 7 (July 13, 2017): 51–58. https://doi.org/10.5281/zenodo.826481.

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On the plots under sowing of field crops traits for which you can define the degree of soil erosion are projective cover and height plants. Enthusiastically steepness of slopes the ability to use crops as indicators of soil erosion reduces soil erosion degree of natural grassland can be estimated based on existing dependencies between the grass plants and extent of soil erosion. Strong enough erosion degree soils of sloping meadows can be recognized for environmental regimes of vegetation habitats.

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Alewell, C., M. Schaub, and F. Conen. "A method to detect soil carbon degradation during soil erosion." Biogeosciences Discussions 6, no. 3 (2009): 5771–87. http://dx.doi.org/10.5194/bgd-6-5771-2009.

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Abstract. Soil erosion has been discussed intensively but controversial both as a significant source or a significant sink of atmospheric carbon possibly explaining the gap in the global carbon budget. One of the major points of discussion has been whether or not carbon is degraded and mineralized to CO2 during detachment, transport and deposition of soil material. By combining the caesium-137 (137Cs) approach (quantification of erosion rates) with stable carbon isotope signatures (process indicator of mixing versus degradation of carbon pools) we were able to show that degradation of carbon o

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Tenge, A. J., F. B. S. Kaihura, R. Lal, and B. R. Singh. "Erosion effects on soil moisture and corn yield on two soils at Mlingano, Tanzania." American Journal of Alternative Agriculture 13, no. 2 (1998): 83–89. http://dx.doi.org/10.1017/s0889189300007712.

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AbstractSoil erosion is a major threat to sustaining agricultural production in Tanzania. However, quantitative information is scanty on its effects on yields of major crops for principal soils and management practices. We conducted this study to determine erosion effects on soil moisture, related properties and corn yield on Tropeptic Haplustox and Ultic Haplustalf soils at Mlingano in Tanzania. Four erosion classes (least, slight, moderate, and severe) on Tropeptic Haplustox and three erosion classes (slight, moderate, and severe) on Ultic Haplustalf were established according to the thickne

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Mandal, D., S. Patra, N. K. Sharma, N. M. Alam, C. Jana, and R. Lal. "Impacts of Soil Erosion on Soil Quality and Agricultural Sustainability in the North-Western Himalayan Region of India." Sustainability 15, no. 6 (2023): 5430. http://dx.doi.org/10.3390/su15065430.

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Erosion by water reduces soil quality and hence crop yield. Understanding the response of crop yields to soil erosion is vital in assessing agriculture’s vulnerability to erosion. However, these effects are difficult to quantify. The study presents a quantitative relationship between soil erosion and soil quality and productivity of rainfed wheat (Triticum aestivum) by comparing field plots with different degrees of erosion in some sub-tropical alfisols in the Doon Valley region of India. By comparing the topsoil depth with the reference site as the control, erosion severity was classified int

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Coelho, C. O. A., A. J. D. Ferreira, A. Laouina, et al. "Changes in land-use and their impact on erosion rates and overland flow generation in the Maghreb region." Revue des sciences de l'eau 17, no. 2 (2005): 163–80. http://dx.doi.org/10.7202/705528ar.

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The ongoing intensification of grazing as well as the replacement of traditional land management systems in the Maghreb has brought to the forefront the fundamental role of land-use in determining soil erosion hazard. This paper reports on erosion rates and soil hydrological characteristics of a variety of land uses in Morocco and Tunisia. The results were obtained through rainfall simulation experiments carried out in the field using a portable simulator, following the design of CERDÀ et al. (1997). Traditional land management systems - typically involving a combination of agriculture, animal

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Nanney, R. D., D. W. Fryrear, and T. M. Zobeck. "Wind Erosion Prediction and Control." Water Science and Technology 28, no. 3-5 (1993): 519–27. http://dx.doi.org/10.2166/wst.1993.0455.

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Few regions of the United States are entirely safe from wind erosion. Whenever the soil surface is loose and dry with limited crop residue cover, and the wind sufficiently strong, soil erosion will occur. Soil erosion by wind causes diffuse pollution, loss of topsoil, reduced crop production, and damage to both public and private facilities. Factors contributing to the wind erosion process can vary daily. This complex process presents a challenge to the science of wind erosion prediction and control. USDA Agricultural Research Service is developing a new Wind Erosion Prediction System (WEPS) t

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Pierson, Derek N., Peter R. Robichaud, Charles C. Rhoades, and Robert E. Brown. "Soil carbon and nitrogen eroded after severe wildfire and erosion mitigation treatments." International Journal of Wildland Fire 28, no. 10 (2019): 814. http://dx.doi.org/10.1071/wf18193.

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Erosion of soil carbon (C) and nitrogen (N) following severe wildfire may have deleterious effects on downstream resources and ecosystem recovery. Although C and N losses in combustion and runoff have been studied extensively, soil C and N transported by post-fire erosion has rarely been quantified in burned landscapes. To better understand the magnitude and temporal pattern of these losses, we analysed the C and N content of sediment collected in severely burned hillslopes and catchments across the western USA over the first 4 post-fire years. We also compared soil C and N losses from areas r

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SESTRAS, Paul, Sevastel MIRCEA, Sanda ROȘCA, et al. "GIS based soil erosion assessment using the USLE model for efficient land management: A case study in an area with diverse pedo-geomorphological and bioclimatic characteristics." Notulae Botanicae Horti Agrobotanici Cluj-Napoca 51, no. 3 (2023): 13263. http://dx.doi.org/10.15835/nbha51313263.

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The complex environmental process of soil erosion is crucial to sustainable land management and conservation. This study uses the Universal Soil Loss Equation (USLE) model to understand the intricate interactions that cause soil erosion in Cluj County, Romania, a region susceptible to complex erosion and landslide phenomenon. The established analysis depicts erosion patterns from localised hotspots to regions of relative stability, providing valuable insights into this critical issue. Spatial distribution maps with color-coded gradients show soil erosion risk and identify vulnerable regions, w

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Alewell, C., M. Schaub, and F. Conen. "A method to detect soil carbon degradation during soil erosion." Biogeosciences 6, no. 11 (2009): 2541–47. http://dx.doi.org/10.5194/bg-6-2541-2009.

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Abstract. Soil erosion has been discussed intensively but controversial both as a significant source or a significant sink of atmospheric carbon possibly explaining the gap in the global carbon budget. One of the major points of discussion has been whether or not carbon is degraded and mineralized to CO2 during detachment, transport and deposition of soil material. By combining the caesium-137 (137Cs) approach (quantification of erosion rates) with stable carbon isotope signatures (process indicator of mixing versus degradation of carbon pools) we were able to show that degradation of carbon o

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Ramazanova, N. E., and Ch Zh Avezkhanov. "DETERMINATION OF SOIL LOSS IN THE ULYSAI RIVER BASIN USING THE RUSLE FORMULA." Hydrometeorology and ecology 100, no. 1 (2021): 42–49. http://dx.doi.org/10.54668/2789-6323-2021-100-1-42-49.

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Since soil erosion is one of the processes that have a significant negative impact on land resources, as well as the economy, it is very important to determine the main types of erosion, calculate the process of soil erosion, rationalize and organize its prevention. Soil erosion is most often observed on fine-grained soils, in areas with high humidity and strong winds, with severe erosion, soil fertility is lost, which accordingly leads to a deterioration in the quality of agricultural products. Today it is effective to use the RUSLE formula to determine the main factors affecting soil erosion

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Higgitt, David L. "Soil erosion and soil problems." Progress in Physical Geography: Earth and Environment 15, no. 1 (1991): 91–100. http://dx.doi.org/10.1177/030913339101500108.

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Higgitt, David. "Soil erosion and soil problems." Progress in Physical Geography: Earth and Environment 16, no. 2 (1992): 230–38. http://dx.doi.org/10.1177/030913339201600205.

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Higgitt, David. "Soil erosion and soil problems." Progress in Physical Geography: Earth and Environment 17, no. 4 (1993): 461–72. http://dx.doi.org/10.1177/030913339301700404.

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Koirala, Pooja, Sudeep Thakuri, Subesh Joshi, and Raju Chauhan. "Estimation of Soil Erosion in Nepal Using a RUSLE Modeling and Geospatial Tool." Geosciences 9, no. 4 (2019): 147. http://dx.doi.org/10.3390/geosciences9040147.

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Soil erosion is a major issue, causing the loss of topsoil and fertility in agricultural land in mountainous terrain. Estimation of soil erosion in Nepal is essential because of its agriculture-dependent economy (contributing 36% to national GDP) and for preparing erosion control plans. The present study, for the first time, attempts to estimate the soil loss of Nepal through the application of the Revised Universal Soil Loss Equation (RUSLE) model. In addition, it analyzes the effect of Land Use and Land Cover (LULC) and slope ( β ) exposition on soil erosion. Nation-wide mean annual soil los

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Sergey, V., and S. Vyacheslav. "An aerodynamic approach in soil hydraulic conductivity estimation for investigating soil erosion degree." Proceedings of the International Association of Hydrological Sciences 367 (March 3, 2015): 66–71. http://dx.doi.org/10.5194/piahs-367-66-2015.

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Abstract. We propose a new method for determining the degree of erosion for zonal soils of the East European Plain. This new approach uses soil porosity and filtration to determine a coefficient of aerodynamic similarity. We evaluated the degree of soil erosion on ranges of the major zonal soils of the eastern part of European Russia by applying this new method. Based on these data, we developed a diagnostic scale to determine the extent of soil erosion in this area.

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Heckrath, G., J. Djurhuus, T. A. Quine, K. Van Oost, G. Govers, and Y. Zhang. "Tillage Erosion and Its Effect on Soil Properties and Crop Yield in Denmark." Journal of Environmental Quality 34, no. 1 (2005): 312–24. http://dx.doi.org/10.2134/jeq2005.0312a.

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ABSTRACTTillage erosion had been identified as a major process of soil redistribution on sloping arable land. The objectives of our study were to investigate the extent of tillage erosion and its effect on soil quality and productivity under Danish conditions. Soil samples were collected to a 0.45‐m depth on a regular grid from a 1.9‐ha site and analyzed for 137Cs inventories, as a measure of soil redistribution, soil texture, soil organic carbon (SOC) contents, and phosphorus (P) contents. Grain yield was determined at the same sampling points. Substantial soil redistribution had occurred dur

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