Odebiri Omosalewa, Mutanga Onisimo, Odindi John, Slotow Rob, Mafongoya Paramu, Lottering Romano, Naicker Rowan, Matongera Trylee Nyasha, Mngadi Mthembeni
School of Agricultural, Earth and Environmental Sciences, Discipline of Geography, University of KwaZulu-Natal, Pietermaritzburg, South Africa.
Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, Melbourne, VIC 3125, Australia.
Catena (Amst). 2024 Aug;243:108216. doi: 10.1016/j.catena.2024.108216.
The preservation and augmentation of soil organic carbon (SOC) stocks is critical to designing climate change mitigation strategies and alleviating global warming. However, due to the susceptibility of SOC stocks to environmental and topo-climatic variability and changes, it is essential to obtain a comprehensive understanding of the state of current SOC stocks both spatially and vertically. Consequently, to effectively assess SOC storage and sequestration capacity, precise evaluations at multiple soil depths are required. Hence, this study implemented an advanced Deep Neural Network (DNN) model incorporating Sentinel-1 Synthetic Aperture Radar (SAR) data, topo-climatic features, and soil physical properties to predict SOC stocks at multiple depths (0-30cm, 30-60cm, 60-100cm, and 100-200cm) across diverse land-use categories in the KwaZulu-Natal province, South Africa. There was a general decline in the accuracy of the DNN model's prediction with increasing soil depth, with the root mean square error (RMSE) ranging from 8.34 t/h to 11.97 t/h for the four depths. These findings imply that the link between environmental covariates and SOC stocks weakens with soil depth. Additionally, distinct factors driving SOC stocks were discovered in both topsoil and deep-soil, with vegetation having the strongest effect in topsoil, and topo-climate factors and soil physical properties becoming more important as depth increases. This underscores the importance of incorporating depth-related soil properties in SOC modelling. Grasslands had the largest SOC stocks, while commercial forests have the highest SOC sequestration rates per unit area. This study offers valuable insights to policymakers and provides a basis for devising regional management strategies that can be used to effectively mitigate climate change.
土壤有机碳(SOC)储量的保护和增加对于设计气候变化缓解策略和缓解全球变暖至关重要。然而,由于SOC储量易受环境和地形气候变异性及变化的影响,全面了解当前SOC储量在空间和垂直方向上的状况至关重要。因此,为了有效评估SOC储存和固存能力,需要在多个土壤深度进行精确评估。因此,本研究实施了一种先进的深度神经网络(DNN)模型,该模型结合了哨兵-1合成孔径雷达(SAR)数据、地形气候特征和土壤物理性质,以预测南非夸祖鲁-纳塔尔省不同土地利用类别下多个深度(0-30厘米、30-60厘米、60-100厘米和100-200厘米)的SOC储量。随着土壤深度增加,DNN模型预测的准确性普遍下降,四个深度的均方根误差(RMSE)范围为8.34吨/公顷至11.97吨/公顷。这些发现意味着环境协变量与SOC储量之间的联系随着土壤深度的增加而减弱。此外,在表层土壤和深层土壤中发现了驱动SOC储量的不同因素,植被在表层土壤中的影响最强,随着深度增加,地形气候因素和土壤物理性质变得更加重要。这突出了在SOC建模中纳入与深度相关的土壤性质的重要性。草地的SOC储量最大,而商业森林的单位面积SOC固存率最高。本研究为政策制定者提供了有价值的见解,并为制定可用于有效缓解气候变化的区域管理策略提供了基础。