11th International Soil Congress, Nevşehir, Türkiye, 23 - 25 Eylül 2024, ss.1-2
Wind erosion is
known as one of the dominant land degradation processes in terms of the
sustainability of natural resources in semi-arid and arid regions of the world.
Soil crusts form a protective layer on the soil surface, reducing the
probability of particle detachment by erosive winds. A well-developed crust
increases the threshold wind speed necessary to initiate soil particle
movement, thereby reducing the risk of wind erosion. However, weak or fragile
crusts can break down into smaller particles under wind stress, contributing to
dust emission. Thus, crust strength is crucial factor for assessing wind
erosion. Prediction models like the Wind Erosion Prediction System (WEPS) or
Revised Wind Erosion Equation (RWEQ) use crust strength data to simulate
erosion risk under different scenarios, helping land managers make informed
decisions. Wind tunnels, while highly effective for studying wind erosion, can
indeed be time-consuming and costly to operate. They require large
infrastructure, precise control of environmental variables, and can take
significant time to set up and run experiments. Given these challenges, small
experimental units or alternative methods can be more appropriate for certain
studies. A reliable method to measure soil crust strength under erosive winds
could greatly enhance efforts to prevent wind erosion and improve prediction
models for managing these vulnerable ecosystems. In this study, we aimed to
introduce an innovative approach to quantify how well different crusts resist
erosion under varying wind speeds and particle sizes by simulating saltation
transport mechanism to improve prediction models and apply more effective soil
conservation strategies.