Effects of Different Land Use Types on Soil Physico-Chemical Properties in Wolaita Zone, Ethiopia

Abstract

Soils are obviously inconstant and their properties are changing across land use types. Essential soil physico-chemical assets impact the performance of soil and, therefore, information on soil property is important. The objective of the study was to determine effects of different land use systems on soil physico-chemical properties in Wolaita zone, southern Ethiopia. Soil samples were collected from three different land uses, enset (Ensete ventricosum), tef (Eragrostis tef (Zucc.) Trotter) and grass lands. Each replicated three times and the composite sample was taken. All the properties are significantly different and determined using appropriate methods. Soil pH, electrical conductivity, total nitrogen, texture, organic matter and phosphate in soil were determined experimentally to study the effects of land use on them. Changes in soil properties in dissimilar land usage forms at two pits (0-15 and 15-30 cm) were detected on various soil properties significant to crop growth. Enset fields had higher pH (5.80), electrical conductivity (EC (0.14 dS/m)), available P (35.25%) and Zn (8.64 mg/kg), exchangeable K (3.12 Cmol(+Kg) which is ascribed due to the input of dung, while tef fields had lowest average K (1.38 cmol (+kg) and Mg (1.89 cmol(+kg), cation exchange capacity (CEC (20.21 cmol(+kg)), total N (0.13%) and OC (1.76%). Most of the physico-chemical properties of the study region were significantly influenced by the different land uses. The evidence derived from the current study will support in mounting maintainable and environmentally constant land use management strategies for the

Soil Physicochemical Properties Variation under Annual Crop and Coffee Landuse in the Chentale Watershed, Upper Blue Nile Basin, Ethiopia

“…In recent studies conducted in Ethiopia, it has been well established that variations in soil physicochemical properties and fertility correspond to land use management practices [7][8][9][10][11][12]. For example, a higher concentration of organic carbon/matter in soil, total N, cation exchange capacity (CEC), electrical conductivity (EC), pH, available P, and exchangeable K were recorded in Enset-based homegarden agroforestry than in croplands in central, south-central, and southeastern Ethiopia [9,[13][14][15]; lower bulk density and higher total porosity were revealed in grasslands than in bareland of northern Ethiopia [16]. Furthermore, the highest clay, pH, organic carbon, EC, total N, available P, CEC, and exchangeable cations were recorded in natural forests compared to cultivated land in the western and northwestern highlands of Ethiopia [7,8,11,17].…”