National parks are established to reduce human influence on nature and contribute to species conservation, biodiversity and ecological services. Other states of protection like the UNESCO world heritage sites, for example, are created for maintaining culturally important places or lifestyles. In the Matobo Hills (Zimbabwe) both states of protection are present, a national park and a world heritage site. In addition, the land outside the National Park belongs to two different systems of ownership, namely "common"(i.e. community-owned) and "not-common" (privately or governmentally owned)

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On the southern slopes of Mt.Kilimanjaro like in many other regions in East Africa, agriculture strongly depends on irrigation. Water is supplied to farms by an extensive network of open unlined canals, most of them built centuries ago. However, information about the distribution of these irrigation canals and the dynamics of their discharge is rare thus hampering the implementation of sustainable solutions for agricultural water management. We suppose that several factors like topography, soil properties, shifts of cropping patterns, and weak institutions affect availability and management of agricultural water. Therefore, in this study we determined (i) the distribution of irrigation canals, (ii) their discharge patterns, and (iii) constraints to their sustainable management. Mixed-method approach consisting of both quantitative and qualitative methodologies was used. The discharge of canals was measured at 11 locations along an altitudinal gradient and selected canals were mapped to understanding their distribution, physical characteristics, and potential risks that limits their optimal discharge. Terrain attributes were derived from the Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM) and soil physical and hydraulic conductivity were measured to understand permeability and stability of the soil. Additionally, we conducted focus group discussions with participants from 15 villages and 10 key informants interviews. We found that during the dry season the discharge of canals was higher than in the short rainy season. The discharge of canals increased with decreasing elevation. The median daily discharges equaled 12.6, 9.5, and 7.0 l/s in the lower, mid and upper areas, respectively. Landscape in the central part of the study area was the steepest (slope > 60%) and the roughest (Topographic Ruggedness Index > 80 m).We attribute this to terrain heterogeneity across the landscape, thus community decisions about distribution and maintenance of canals could differ across different villages. Furthermore, current shifts of cropping patterns increased irrigation water demands. Both formal and informal water institutions were constrained with several challenges that affected overall management of canals and their sources. Findings of this study could contribute to various efforts dedicated to improve management of water resources around Mt. Kilimanjaro.