Abstract

Abstract. Land use change can have negative or positive effects on soil quality. Our objective was to assess the effects of land uses changes on the dynamics of selected soil physical and chemical properties. Soil samples were collected from three adjacent soil plots under different land uses, namely forestland, grazing land, and cultivated land at 0–15 cm depth. Changes in soil properties on cultivated and grazing land were computed and compared to forestland, and ANOVA (analysis of variance) was used to test the significance of the changes. Sand and silt proportions, soil organic content, total nitrogen content, acidity, cation exchange capacity, and exchangeable Ca2+ content were higher in forestlands. Exchangeable Mg2+ was highest in grazing land, while clay, available phosphorous, and exchangeable K+ were highest in cultivated land. The percentage changes in sand, clay, soil organic matter, cation exchange capacity, and exchangeable Ca2+ and Mg2+ were higher in cultivated land than in grazing land and forestland. In terms of the relation between soil properties, soil organic matter, total nitrogen, cation exchange capacity, and exchangeable Ca2+ were strongly positively correlated with most of soil properties, while available phosphorous and silt have no significant relationship with any of the other considered soil properties. Clay has a negative correlation with all soil properties. Generally, cultivated land has the least concentration of soil physical and chemical properties except clay and available phosphorous, which suggests an increasing degradation rate in soils of cultivated land. So as to increase soil organic matter and other nutrients in the soil of cultivated land, the integrated implementation of land management through compost, cover crops, manures, minimum tillage, crop rotation, and liming to decrease soil acidity are suggested.

Highlights

  • Land use changes have remarkable effects on the dynamics of soil properties (Biro et al, 2013)

  • The clay fraction on cultivated land and grazing land increased compared to forestland, but the change is greater in cultivated land than grazing land (Table 4)

  • Because the clay particles are very small in size, silt, and sand fractions could be removed by runoff from the cultivated land

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Summary

Introduction

Land use changes have remarkable effects on the dynamics of soil properties (Biro et al, 2013). Land use changes from forest cover to cultivated land may reduce the input or organic residues that lead to a decline in soil fertility (MuñozRojas et al, 2015), increased rates of erosion (Biro et al, 2013), the loss of soil organic matter and nutrients (Saha and Kukal, 2015), and an accelerated rate of soil degradation (Barua and Haque, 2013). Saha and Kukal (2015) found a higher bulk density and lower macroporosity and water retention in cultivated soils than in soils of grassland and forests. This indicated a degradation of soil properties due to the conversion of natural ecosystems to agricultural systems

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