Land cover change and its effects on soil properties remain a major concern and pose significant challenges to sustainable agricultural development. This study evaluated the influence of land cover classes (LCC) and slope gradients on soil properties in the Gelda catchment. Surface disturbed and undisturbed soil samples were collected from four land cover classes across three slope gradients. Data were analyzed using analysis of variance (ANOVA), the least significant difference (LSD) post hoc test, and Pearson's correlation coefficient (r). The results revealed that clay content, Si/C ratio, total nitrogen, and organic matter differed significantly among land cover classes (P ≤ 0.05), whereas clay, silt, and sand fractions showed only slight variation across slope gradients. Lower soil pH values observed in forest (5.35) and grassland (5.43) areas were attributed to cation uptake by woody biomass and the addition of acid-forming ions. Grassland (4.04%) and forest soils (0.23%) exhibited higher organic matter contents than farmland soils, a trend also reflected in total nitrogen levels (3.91% in grasslands and 0.22% in forest soils). Variations in cation exchange capacity and exchangeable base contents were largely associated with differences in clay mineralogy and organic matter across land cover classes. Consequently, the observed soil quality limitations in farmlands highlight the need for management practices that enhance soil organic matter and improve soil reaction status in the study area.
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