Thesis Abstract

Characterization and evaluation of four toposequences in different soil landscapes were carried out to determine the soil properties and their implications for land use planning. The study focused on understanding the variations in soil characteristics along the toposequences to provide insights into soil management practices. Four toposequences representing different landscapes were selected for the study. The toposequences included upland, mid-slope, lower slope, and valley bottom positions. Soil samples were collected at different depths along each toposequence to analyze various soil properties such as texture, pH, organic matter content, and nutrient levels. The results revealed significant differences in soil properties among the toposequences. The upland position had sandy soils with lower organic matter content compared to other positions. In contrast, the valley bottom position had fine-textured soils with higher organic matter content. The mid-slope and lower slope positions showed intermediate soil properties between the upland and valley bottom positions. Analysis of soil nutrients showed that the upland position had lower nutrient levels, particularly nitrogen and phosphorus, while the valley bottom position had higher nutrient levels. The pH of the soils also varied along the toposequences, with the upland position having slightly acidic soils compared to neutral pH in the valley bottom position. The study also evaluated the implications of these soil variations for land use planning. The differences in soil properties among the toposequences suggested that different management practices would be required for optimal land use. For example, the upland position may benefit from soil amendments to improve nutrient levels, while the valley bottom position may require drainage systems to address waterlogging issues. Overall, the characterization and evaluation of the four toposequences provided valuable information on the soil properties and their spatial variations within different landscapes. The findings of this study can be used to guide land use decisions and sustainable soil management practices in similar soil landscapes. Further research could focus on long-term monitoring of these toposequences to assess the effectiveness of different soil management strategies over time.

Thesis Overview

INTRODUCTION

            Characterization of soil provides a useful means for understanding soil distribution and variability. The modern soil survey is a fundamental basis for land use planning because it contains both qualitative and quantitative data which enable predictions of many kinds to be made. It aids in correlating and predicting the adaptability of   various crops, grasses, and trees, to soils and their behaviour and productivity under different management. Field studies that depict the variability and distribution of soil are panacea for total utilization of a given tract of land. Such understanding enables useful prediction to be made wherever such soils occur making it possible for soils of different parts of the world occurring under similar and different climatic condition to be compared (Buol et al 1980). Soil characterization goes beyond soil testing, it is an integration of both physical and chemical nature of soil. It analysis the inherent characteristics and properties of a given soil with the aim of characterizing them into similar soil units and capability land use units.

Soil suitability evaluation involves characterizing the soil in a given area for specific land use type. The information collected in soil survey helps in the development of land-use plans and to evaluate and predict the effects of the land use on the environment. The suitability of a given piece of land is its natural ability to support a specific land use type. Suitability may be a major kind of land use, such as rain fed agriculture, livestock production, forestry, etc.

As these qualities derived from the land characteristics, such as slope angle and length, and soil texture which are measurable or estimable, it is advantageous to use these latter values to study the suitability. For assessing the suitability of soils for crop production, soil requirements of crops must be known. Also, these requirements must be understood within the context of limitations imposed by land form and other features which do not form a part of the soil but may have a significant influence on use that can be made of the soil (FAO,1976).

Soil classification on the other hand helps to organize our knowledge and facilitate the transfer of experience and technology from one place to another and to compare soil properties. It provides a link between soil characterization and soil survey. According to Lark and Wheeler (2000), variation in soil properties has long been known and had been the subject of much research. It was in recognition of this that Sir Ronald-fisher, and then at Rothamsted, developed a formidable array of statistical methods.

Accordingly, horizons may differ in organic matter content, structure, texture, pH, base saturation, cation exchange capacity as well as many other soil physicals and chemical properties. According to Mullar and Mc Bratney (2001), variability in soil properties at the series level is often caused by small changes in topography that affect the transport and storage of water across and within the soil profile. Hunter et al (1982) and Yost et al (1982) reported that soil-forming factors affect different properties differently at different depths. Variability of soil pH, for e.g. increases with depth (Ogunkunle and Ataga, 1985). Ogunkunle (1993) working on Alfisols of southwestern Nigeria, observed that soil pH was the least variable (low variability) property, irrespective of depth. The variability of properties like organic matter, available phosphorus, total nitrogen and CEC, increases with depth. Properties, such as soil pH and porosity are among the least variable, while those pertaining to water or solute transport are among the most variable. Percentage sand ranges from low to moderate variability. Organic matter and % clay range from moderate to high variability. Available phosphorus and potassium were observed to be highly variable (Jury, 1986 et al, Beven et al, 1993, Wollenhaupt et al, 1997). In general the more variable these properties, the more variable the crop growth and yield. Thus, understanding soil variability is essential in applying location specific (precision-agriculture) management strategies. Therefore, the general objective of this study was to assess the degree of variability of some soil physical and chemical properties along four toposequence  for assessing their agricultural potentials.

The specific objectives were to: (i) characterize and classify the soils of  four toposequences. (ii) assess the effects of slope characteristics on physico-chemical properties.

(iii) evaluate the agricultural potentials of the four toposequences.