Soil Erosion, Mass Movements and Pedoclimatic Disequilibrium in Aggradational Landforms

A special issue of Soil Systems (ISSN 2571-8789).

Deadline for manuscript submissions: 15 January 2026 | Viewed by 675

Special Issue Editors


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Guest Editor
Department of Geography, Institute of Geosciences, Universidade Federal do Rio de Janeiro, Rio de Janeiro 21941-916, Brazil
Interests: soil erosion; mass movements; monitoring; modeling; land recuperation

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Guest Editor
Departamento de Ciências Geográficas, Universidade Federal de Pernambuco (UFPE), Recife 50740-550, Brazil
Interests: climatic geomorphology; morphostratigraphy; quaternary; semi-arid environments

Special Issue Information

Dear Colleagues,

This Special Issue seeks to gather original contributions that focus on soil erosion, mass movements, and pedoclimatic disequilibrium in aggradational landforms. These themes are central to addressing the critical environmental challenges of the 21st century, with far-reaching implications for both rural and urban sustainability, ecosystem health, and the protection of human lives and material assets. The accelerating pace of surface processes driven by rapid environmental change presents complex challenges due to their unpredictable nature and substantial contributions to soil loss and land degradation. In particular, soil covers in tropical regions are often remnants of ecological conditions that differ from the current landscape, making them particularly prone to destabilization under contemporary socio-environmental pressures, especially in the context of large-scale commercial agriculture encroachment.

This Special Issue will deal with the pivotal role of soil erosion, recognized as one of the leading causes of land degradation through the removal of the fertile topsoil at alarming rates. The conversion of original vegetation for agricultural purposes serves as a primary triggering factor. We invite contributions that explore the various forms of erosion—such as sheet, rill, and gully erosion—supported by case studies from diverse global landscapes. We also welcome discussions on the responses of soil covers formed on quaternary aggradational landforms to extreme meteorological events, highlighting the need for adaptive management strategies.

Mass movements, or mass wasting, represent the gravitational movement of soil and rock materials, often occurring independently from the influences of water or ice. The dynamics of mass wasting are significantly affected by human activities that alter hillslope stability in both rural and urban settings. Recent shifts in precipitation patterns further exacerbate these challenges, making it urgent to understand and address their implications. Moreover, soil imbalances arising from altered precipitation patterns, rising temperatures, and carbon cycling changes can severely impact soil structure, function, fertility, and plant growth, with direct consequences for food production systems.

This Special Issue will also address how contemporary conditions, including increasing temperatures and intensified precipitation, affect soil covers on aggradational landforms inherited from past environmental and landscape arrangements, such as dunes, sand sheets, paleo-alluvial plains, and colluvial hillslopes. Such insights are vital for predicting landscape changes, assessing land degradation, and implementing sustainable practices for mitigation and reclamation.

We invite submissions that comprehensively address soil erosion, mass movements, and pedoclimatic disequilibrium in depositional landforms, encompassing their causes, consequences, and mitigation strategies. Potential topics may include, but are not limited to, surveying, monitoring, modeling, assessment, prognosis, land reclamation, mitigation strategies, and instrumentation, applicable in both field and laboratory settings. We look forward to your valuable contributions.

Prof. Dr. Antônio José Teixeira Guerra
Prof. Dr. Antonio Carlos de Barros Correa
Guest Editors

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Keywords

  • soil erosion
  • mass movements
  • sheet erosion
  • rill erosion
  • gully erosion
  • alluvium
  • colluvium
  • land reclamation
  • climate change
  • modeling

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Published Papers (1 paper)

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Research

17 pages, 2795 KB  
Article
Soil Properties Governing Erodibility of Cuban Soils: A Univariate Erodibility Equation
by Gustavo R. Alonso, Javier Casalí, Miguel Ángel Campo-Bescós and Jorge Díaz
Soil Syst. 2025, 9(4), 131; https://doi.org/10.3390/soilsystems9040131 - 19 Nov 2025
Viewed by 276
Abstract
Accelerated water erosion is a major soil degradation process that affects soil and water quality. In Cuba, specifically, more than 40% of agricultural lands are affected by severe erosion problems. Estimating accurate erodibility values is a crucial step for the calibration and proper [...] Read more.
Accelerated water erosion is a major soil degradation process that affects soil and water quality. In Cuba, specifically, more than 40% of agricultural lands are affected by severe erosion problems. Estimating accurate erodibility values is a crucial step for the calibration and proper application of erosion models. Several equations have been developed to estimate erodibility from soil properties; however, these are often soil- or site-specific, limiting their application. This study aims to (1) identify soil properties governing the erodibility of tropical soils from western Cuba, (2) find suitable regression models to estimate erodibility from these properties, and (3) test widely applied erodibility equations. To achieve these goals, rainfall simulation experiments were conducted on runoff plots, and erosion-related physical, chemical, and mechanical soil properties were determined for 19 different soils. The main results indicated that good correlations between erodibility and certain soil properties were achieved after clustering soils based on their cation exchange capacity (CEC) values and clay content. Soils characterized by more than 30% of clay and 40 cmol+ kg−1 of CEC were excluded from the main analysis. Generally, clay content controls the erodibility of these tropical soils, exhibiting an inverse relationship. However, in the excluded soils, the clay fraction showed a positive relationship with erodibility. Soil water retention at the lowest matric potentials demonstrated the strongest correlation with soil erodibility, as this variable encompasses compound information related to clay, mineralogy, and organic matter. A new regression model to estimate erodibility based solely on the volumetric water content at 1500 kPa is presented. The optimal fitted logarithmic model accounts for 64% of the predictand variability in the studied soils. When testing known erodibility models, the nomograph was found to best mimic the erodibility trend of these soils, although it exhibited marked uncertainty and underestimation biases. Full article
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