Nature-based solutions (NbS) are increasingly seen as the most sustainable option for addressing climate change challenges such as erosion and landslides. Live slope grid is a NbS used for protection and mitigation of shallow landslides and erosion; it involves a timber grid construction which covers the slope at risk of landslide/erosion with live vegetation planted within the cells of the grid which stabilises the uppermost soil horizons. Live cribwall is another NbS used for retention of unstable soil mass. Vegetation is planted and grows in between the cribwall layers and it anchors the wall to the soil behind while, at the same time, strengthening the backfill. The aim of this case history is to detail the co-design and co-deployment of a live slope grid installed above a live cribwall on a coastal slope in Scotland. The design and construction process is detailed over the range of project stages and will outline stakeholder engagement during this process. Because the NbS structures failed during this process and repair work had to be carried out, this study focuses on sharing the ‘lessons learned’ from the design and construction processes over a timeline of several years. The climate change effects leading to failure of the structure as well as the reactions of the stakeholders are highlighted in this case study in order to help practitioners and other stakeholders in managing similar projects within the framework of sustainability and resilience, especially when the funding is limited. The main conclusions from this study are justification of the urgent need for standardising the design and construction of NbS for slope protection as well as the importance of upskilling and training of the relevant stakeholders in order to incorporate the peculiarities of designing and constructing with vegetation.
Within the mining sector, the revegetation process is increasingly recognized as a global imperative for the closure of tailings facilities. Nonetheless, revegetation strategies on bauxite tailings pose a substantial challenge due to very low or non-existent organic matter content in the substrate. The objective of this study was to investigate the efficacy of inducing ecological succession on bauxite tailings substrates. For this purpose, field experiments were conducted during twelve months with varying conditions of organic matter supplementation. In the control treatment (T3), only tree seedlings were planted on unamended tailings; the T2 treatment introduced both tree planting and green manure; the T1 treatment combined tree seedlings, green manure, and decaying wood. Dendrometry variables, phenological phases, litter production, mortality rate (Mr), and soil's physicochemical parameters (organic matter, soil bulk density, porosity, stability, and nutrient content) were assessed. The T1 treatment displayed the highest OM content (27.08 g kg−1) and CEC values (3.40 cmolc dm−3) at 0–5 cm. The highest biomass production by Crotalaria spectabilis Röth was obtained at T1 (7.81 t ha−1), however, Canavalia ensiformis (L.) DC. produced similar amounts of biomass at T1 and T2. Among tree species, Hymenaea courbaril L. showed the highest mortality rate (16 %). The best results of natural colonization were observed at T2 (111 %). The induction of ecological succession enhanced chemical attributes in the surface layer and promoted the establishment of tree species during the initial stages of closing bauxite tailings facilities. The T1 treatment exhibited the most significant enhancements in substrate fertility within the 0–5 cm layer, T2 proved to be the most favorable for the spontaneous entry of shrub and tree species, and T3 represented the slowest method to achieve substrate improvements and plant colonization during the initial stages of revegetation.
The plateau zokor is an endemic, subterranean rodent native to the Tibetan Plateau. Its burrowing activity results in numerous bare mounds on the ground. These mounds interfere with plant community succession, affect carbon sequestration, reduce grazing areas, and intensify soil erosion, thus serving as key visual indicators of the zokor's ecological disturbances. Conventional views suggest that zokors primarily dig tunnels and then create mounds for mating and food storage in spring and autumn, respectively. Consequently, former studies have focused on mound creations only during these two periods. However, we found that plateau zokors also create mounds during the summer in the summer pastures. We designed experiments to investigate the environmental variables associated with this summer mound-creating phenomenon, and the results indicate that this behavior is closely related to reduced vegetation biomass and nutrition in summer pastures. We further assessed the nutrition of plants and discovered that increasing mounding activity by zokors in summer corresponds with a decline in plant root quality, including reductions in crude protein, fats, and sugars, as well as fiber contents. Utilizing a random forest model, we found that the decrease in crude protein in plant roots as the principal factor influencing zokor mound creation in summer. These findings offer important insights for developing adaptive management strategies for alpine grasslands and assessing the environmental impact of the plateau zokor in alignment with the different grazing regimes.
The aim of this study was to simulate the water flow and reactive transport of pollutants in a horizontal flow (HF) wetland to better understand the recovery time of the treatment performance for peak load events. For the simulation, the processes-based model HYDRUS and its Wetland Module is used. The system under investigation is the first stage of the 9-years old hybrid treatment wetland of a large retail store, located in Catania, Italy. For the calibration of the hydraulic model, the data of a tracer test was used. The data set of the systems is available for a seven year period including organic matter and ammonia nitrogen. The data was split into a standard event representing low loading conditions and determined peak load events with high loadings. The results show that the response time of the model correlates with the hydraulic retention time from the tracer experiment and indicates that higher peak load concentrations at the inlet of the system lead to a longer recovery time of the wetland.