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Title: | Restoring soil properties in the Hyrcanian forests from machine induced compaction: Reforestation of N2‐fixing black alder (Alnus glutinosa (L.) Gaertn.) | Authors: | Kiumarsi, Fatemeh Jourgholami, Meghdad Jafari, Mohammad Lo Monaco, Angela Venanzi, Rachele Picchio, Rodolfo |
Journal: | LAND DEGRADATION & DEVELOPMENT | Issue Date: | 2024 | Abstract: | Among the various species of trees, black alder (Alnus glutinosa (L.) Gaertn.) is one of the most commonly used trees for the reforestation and restoration programs of degraded forestlands in the Hyrcanian forest, particularly in the skid trails. The effects of reforestation with black alder on the recovery of litter (thickness, C, N, C/N) and soil physicochemical, biochemical, biological, and microbial properties in the skid trails with three levels of compactions were examined over a 27-year period. Results showed that the litter characteristics such as thickness, carbon (C), nitrogen (N), and C/N were at the highest level in low intensity traffic as compared to those of medium and frequent intensities. Results showed that the values of total porosity, macroporosity, aggregate stability, silt, and clay were at the lowest level in the natural stand. The highest values of soil pH, C, C/N ratio, and C storage were recorded under the skid trail with frequent machine passages. The restoration values of soil physical and chemical properties were significantly higher in the low level of machine traffic after a period of 27 years where black alder reforestation was performed on the skid trails, as compared to the medium and frequent machine traffic levels, as well as the undisturbed area. Black alder litter affected soil nitrogen and the maximum amounts of earthworm density and dry mass. This also includes fine root biomass. These data were recorded in the trails with low machine traffic as compared to those of medium and frequent traffic. The results clearly showed that black alder is effective in reaching the objectives of restoration programs, given that it promotes soil organic matter, builds up soil structure via root-soil feedback, and improves the soil by creating a major source of nitrogen through enhancing the nitrogen cycle. |
URI: | http://hdl.handle.net/2067/51613 | ISSN: | 1085-3278 | DOI: | 10.1002/ldr.5045 | Rights: | Attribution-NonCommercial-NoDerivatives 4.0 International |
Appears in Collections: | A1. Articolo in rivista |
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