Abstract

A study was conducted in the Tsegede highlands of Tigray Region, northern Ethiopia to determine the changes in some physical and chemical attributes across three adjacent acidic soil sites with different elevation and three land use types. Analytical results of the collected surface layer soil samples showed significant (P ≤ 0.05) correlation of soil bulk density, OM and total N with elevation. In the lower elevation site (Indaslasie), soil OM content declined by about 43 and 52% compared with that of the two higher elevation sites (Cheguarcudo and Indamariam), respectively. Soil pH, exchangeable acidity, exchangeable Al, OM, total N and available phosphorus also exhibited significant (P ≤ 0.05) disparity across the three land use types of the area. Soils of the forest land were less acidic by 0.43 and 0.68 pH units than the cultivated and grazing lands, respectively. The soil OM content of the cultivated land was significantly lower by about 25 and 35% than the grazing and forest land soils, respectively. Available soil P status was low and showed significant correlations with pH (r = 0.65), exchangeable acidity (r = –0.58) and Al (r = –0.53). In general, the study results revealed altitude did not impose any significant effect in aggravating soil acidity whereas land use type affected significantly not only soil acidity but also the important soil fertility related parameters such as OM, total N and available P contents. Therefore, it can be suggested that besides to the usual acid soil management and/or reclamation practices, introducing proper land use management systems are of paramount importance.

Highlights

  • Soil acidity is one of the most important soil factors which influence plant growth and limit crop production and profitability

  • The existence of high exchangeable acidity in a soil usually indicates the occurrence of exchangeable hydrogen (H), exchangeable aluminum (Al) as either free Al3+ ion or partially neutralized Al-hydroxy compounds such as Al(OH)2+ or lAoild aOl Hsu r2 f,acaensdowf ethaek organic acid ions held at the colsoil [9,10]

  • The study showed that the changes in altitude and land use types had significant impact on the spatial distribution of some physical and chemical properties of acidic soils in the Tsegede highlands of Tigray

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Summary

Introduction

Soil acidity is one of the most important soil factors which influence plant growth and limit crop production and profitability. Together with declining levels of soil fertility under no or only limited use of external nutrient inputs, soil acidity is becoming one of the serious soil degradation problems that hamper sustainable agricultural development mainly in the highlands of Ethiopia [3,4]. Soil acidification is a natural process mainly conditioned by naturally acid parent rocks and leaching of base forming ions attributed to high precipitation [5]. The availability of plant nutrients such as phosphorus (P) and calcium (Ca) can be limiting at low soil pH [11], Al toxicity is probably the foremost plant growth and productivity limiting factor in acid soils [12,13,14]

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