Solozori
Eroding food security -
Cropland soil loss in the Rwenzori mountains of Uganda (Solozori)
Duration: from 2025 to 2028
Funding Institution: German Research Foundation (DFG)
Principal Investigator(s): Dr. Florian Wilken and Prof. Dr. Peter Fiener
Associate Researchers: Prof. Dr. Markus Keck and Dr. Sebastian Purwins
Research topics: Soil degradation and cropland collapse in the wet tropics of Africa
Description:
A critical hotspot for rising food demands fused to massive soil degradation is Africa's Albertine Rift due to steep terrain, heavy erosive rainfall and low soil cover conditions throughout the cultivation period. The pressure on land resources leads to various problems that will have a tense ecological and social impact. As soil loss under arable use tremendously exceeds soil formation at sloped fields, agricultural use is limited to a certain period of time. After the fertile soil mantle is removed (bedrock is exposed to the surface), these areas lose their ability to host any healthy biotic community quasi-permanently (millennial-scale). The time it takes to remove the soil mantle is heterogenous and controlled by the local soil loss rates and soil depth to bedrock. The main objective of Solozori is to understand and quantify the ongoing soil degradation dynamics and its effects on cropland productivity, soil health and, finally, ecosystem service collapse. The study area is located in the Rwenzori mountains in Uganda, where land use pressure leads to deforestation of steep slopes that rapidly degrade (within decades) and soil productivity collapses due to shallow soils. Due to these shallow soils, the region is a showcase to study processes associated with soil resource limitations that will, in the longer run, accelerate food insecurity, impacting vulnerable subsistence farmers and partially impeding the chance for successful reforestation. Solozori utilises remote sensing to understand land use history and patterns of vegetation dynamics, while proximal sensing topographic landscape features and fallout radionuclides shed light on long-term soil redistribution rates. Soil redistribution rates will be reflected against soil resources (soil depth to bedrock) to get a grip on the spatial extent and remaining time until cropland loss in the Rwenzori mountains. Thereby, Solozori provides a showcase on yield effects caused by soil resource scarcities and serves the vital need to understand long-term soil degradation dynamics to find sustainable solutions that reduce land use pressure on forest resources and mitigate the dramatic loss of forest resources and corresponding ecosystem services. Solozori puts soil system collapse into a temporal perspective to predict soil ecosystem services loss in the African tropics.