Abstract
Gully erosion due to land destruction and depletion of soil moisture, especially in drought periods, has an important role for decreasing biomass production in Iran. The aim of this study was to determine the characteristics, processes, and the main causes of gully incision. Satellite images, aerial photos, and anecdotal evidence with field measurements were used to obtain information to answer the research questions. The results of this study indicated that Iranian gullies with an area more than 1,420,000 ha were distributed from coastal zones to highlands with an altitude higher than 3000 m above the sea level. They occurred mostly in the areas with precipitation of 100–300 mm and 500–1000 mm. Gullies are dominant more in semi-arid, arid, and Mediterranean climates. Most of the studied gullies are continuous and valley side. The survey of the view plans of the gullies indicated that surface runoff was the dominant hydrological process for gully incision. The results revealed that the rangelands and forests area decreased while rain-fed farms and barren land increased during the last decades. Most Iranian gullies were located in the altitude of 0–500 and 1000–2000 m above the sea level. Overgrazing and land-use change from rangeland and forests to cultivated lands were the main causes of gully erosion. Data showed that Iranian gullies with an average length and depth equal to 570 m and 2.8 m produced 21 m3/m sediment per unit gully length.
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Acknowledgments
This project is sponsored by the Institute of Soil Conservation and Watershed Management in Iran. We acknowledge their support and also the Research and Education Centers in Various Provinces in Iran.
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Soufi, M., Bayat, R., Charkhabi, A.H. (2020). Gully Erosion in I. R. Iran: Characteristics, Processes, Causes, and Land Use. In: Shit, P., Pourghasemi, H., Bhunia, G. (eds) Gully Erosion Studies from India and Surrounding Regions. Advances in Science, Technology & Innovation. Springer, Cham. https://doi.org/10.1007/978-3-030-23243-6_23
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