Abstract

This study was undertaken in Kitui South in Kitui County in the south eastern parts of Kenya. The main objective of the study was to develop a spatial model that can be used for selection of suitable sites for sand dam in Kitui South. The study also assessed the spatial variation of sand grain sizes and how these determine the suitability of sites for the sand dams. Data analysis was done using three approaches. The first approach involved the use of the Remote Sensing (RS) technique where data was preprocessed and analyzed using Erdas Imagine software and Geographical Information Systems (GIS) for spatial modelling. The distribution of sand particle-sizes was based on sieve analysis on the sand samples collected from seasonal rivers in the study area. The seasonal rivers that were investigated in this study included Mwila, Kakya, Wiitu, Nguni, Ngunyumu, Muvuko, Kanzilu, Masaa, Katiliku, Ngulungu, Nzeeu, Koma and Katitika. Statistical analysis was done to establish the relationships between the various spatial components affecting sand particle distribution. The results from the spatial model which integrated all factors shows that 16% of the studied sites along the seasonal rivers in Kitui South were fairly suitable for construction of sand dams while 79% were classified as suitable and 5% are categorized as very suitable. Several sites in the central and the entire eastern parts of Mutha Ward were found not suitable for sand dam construction due to poor conditions such as the lack of suitable sand particles, lack of bedrock exposure on the riverbeds, flat terrain, very shallow stream banks, and weak soils on the riverbanks. Suitable sites for sand dams were found on the western and central areas of Kitui South where production and high accumulation of coarse sands was observed along the seasonal rivers. The areas near Mutomo hills and the rocky areas in Ikanga wards were found to be characterized by few excellent sites for sand dams. The optimum accumulation of different grades of sand in the seasonal rivers was found on streams with slope of between 1.5 and 6% that were dominated with 0 to 40% coarse sands, 0 to 30% fine gravels, 0 to 20% fine sands, and 20 to 80% medium sands. The accumulation of fine gravels was found to be closely related to the distribution of D30, D60 and D90 sand particle-sizes (0.4-4 mm) while accumulation of coarse sands showed good relationship with the distribution of the medium size sand (0.2-0.4 mm). The accumulation of medium sands was equally high when the occurrence of coarse sands was minimal. Different grades of sand were found to be strongly influenced by the changes in the elevation of the stream especially with regard to the accumulation of the medium sands (r=0.76) and coarse sands(r=0.75). Out of 80 investigated sites, 59% of them were dominated with uniform sands (Cu 5). The study also found that 86% of the sites along the seasonal streams were dominated with medium sands while 10% were dominated with fine sands and the rest (4%) dominated by coarse and gravelly sands. From the results this study concludes that 59% of the 80 sites that were investigated in this study have a high potential for providing suitable sites for sand dams in Kitui South.

Highlights

  • In Kenya 80% of the land is classified as arid and semi-arid and suffer from water shortage (Puttemans, 2004)

  • The results show that 86% of the investigated sites in Kitui South were suitable for the sand dam with a river bed gradient ranging from 0% to 8% which fall within the recommended range for the slope of a potential suitable site for sand dam (Maddrell and Neal, 2012)

  • Sands available along the riverbed in most of the seasonal rivers in Kitui South were wellgraded. 86% of the sites considered suitable for sand dam are dominated with uniform medium size sands which imply that majority of the sites capable of having high capacity for water storage

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Summary

Introduction

In Kenya 80% of the land is classified as arid and semi-arid and suffer from water shortage (Puttemans, 2004). Most of the ASALs in Kenya experience rainfall in short high intensity events that hardly infiltrate into the ground. Between these rainy seasons, communities in the rural areas in ASALs encounter drought with severe water shortages. There has been a growing recognition of the importance of sand dams as a low cost and robust means to enhance water availability in ASALs. Determining a suitable location for a sand dam involves evaluating the favorability of both the physical and environmental conditions (Nelson, 1985). One is the availability of coarse sand supplied by the runoff along the river (Nepal et al, 2014). The bedrock ensures that the water that infiltrate into the sand matrix does not leak away from the subsurface storage (Nissen-Petersen, 2007)

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