Linking selected soil properties to land use and hillslope - A watershed case study in the Ethiopian Highlands

• Published in: Soil and water research 2016-01, Vol.11 (3), p.163-171
• Main Authors: ADDIS, Hailu, KLIK, Andreas, OWEIS, Theib, STROHMEIER, Stefan
• Format: Article
• Language: English
• Subjects: Agricultural land; Agricultural production; agricultural watershed; Bulk density; Correlation analysis; Crop production; Deforestation; Depletion; Forest soils; Forests; Highlands; Lake basins; Land use; Organic carbon; Organic phosphorus; Organic soils; Phosphorus; Rainfall; Sand; Sandy soils; Silt; slope steepness; Slopes; soil attributes; Soil density; Soil erosion; Soil investigations; Soil properties; Soils; Topsoil; Watersheds
• ISSN: 1801-5395; 1805-9384
• DOI: 10.17221/117/2015-SWR

Deforestation of native forests for crop production in the Gumara-Maksegnit watershed, located in the Lake Tana basin, Ethiopia, dramatically increases the vulnerability of the soil for rainfall driven erosion. Hence, the central task of the study is to investigate general links of land-use and topography related to selected soil properties. The 53.7 km2 watershed was divided into a 500 × 500 m square grid to sample bulk density (ρd), pH, soil organic carbon (SOC), total nitrogen (TN), available phosphorus (AP), and texture of topsoil. Such properties were investigated with respect to the two main land-uses, forest and agriculture, and three different slope steepness classes, 0–10%, 10–30%, > 30%. Descriptive statistics and correlation analyses were undertaken to explore potential dependencies of the obtained soil parameters according to land-use and slope steepness. The study indicates higher SOC, TN, silt and sand content in forest soils compared to agricultural soils, while solely ρd is lower in the forest soil. Overall increases of SOC, TN, silt, and sand content from the gentle to the steep slopes have been observed for both land-uses. In contrast, clay content and ρd seem to increase from steep to gentle slopes on agricultural areas, which might be due to accumulation of particularly fine soil particles eroded from the steep areas. Basic correlations valid for all land-uses and slope steepness classes have not been detected. Nevertheless, the study suggests slope steepness as a tool to assess the potential drivers of soil depletion in the Ethiopian Highlands.