Abstract

We examined three soil maps of Zambia, two published at scales of 1:1 million – the Exploratory Soil Map of Zambia (ESMZ) and the Vegetation–Soil Map produced by Trapnell and colleagues in 1947 – and one at 1:3 million, the Soil Atlas of Africa (SAA). We estimated components of variance for measurements of clay, sand and organic carbon content and bulk density of the soil across the country using models which included different mean values for soil map units as random effects. For all but organic carbon content there was significant variation accounted for by differences between legend units for two of the maps, ESMZ with legend units based on the FAO-Unesco and SAA with legend units based on the World Reference Base respectively. This was despite their small cartographic scale. For the Vegetation–Soil Map, we examined differences between broad soil physiographic units. These did not account for significant variation in the soil properties. There were clear similarities between the soil physiographic units of the Soil–Vegetation Map and broader physiographic units into which the legend units of the ESMZ are grouped. The spatial pattern of soil units of the SAA was the most spatially heterogeneous, as measured by the sum of indicator variograms, despite being at the smallest published scale. It was apparent that some of the soil variation within the largest physiographic unit of the Soil–Vegetation Map, the Plateau Soils, as expressed by the map units of the SAA was significantly associated with the different vegetation units mapped in 1947. These studies show how quantitative assessment of legacy soil information may help us understand its potential and limitations.

Highlights

  • Soil information is essential for planning agricultural research, development and extension, and to support policy makers, farmers and environmental managers who are concerned with food security and environmental protection, in particular the protection of soil resources

  • On the basis of this observation we suggest that further work, with a larger set of observations of soil properties in the field, is needed to compare the variation of soil properties between the soil units of Soil Atlas of Africa (SAA) and the Exploratory Soil Map of Zambia (ESMZ) and the vegetation–soil units of Trapnell et al (1947), and to evaluate these alternative representations of soil variation in Zambia

  • We have shown that differences between soil map units of two small-scale soil maps of Zambia, the Exploratory Soil Map of Zambia (ESMZ; Soil Survey Section, 1991) and the Soil Atlas of Africa (SAA; Jones et al, 2013) account for a significant and substantial pro­ portion of variation in sand and clay content and bulk density of the soil

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Summary

Introduction

Soil information is essential for planning agricultural research, development and extension, and to support policy makers, farmers and environmental managers who are concerned with food security and environmental protection, in particular the protection of soil resources. While many countries have limited capacity to undertake soil surveys, they often have a legacy of soil maps. The potential value of this legacy of soil surveys has been recognized by initiatives to preserve soil maps and memoirs and to make them avail­ able online (e.g. through the International Soil Reference and Informa­ tion Centre (ISRIC) library and map collectionhttps://www.isric.org/. The most recent national map of Zambia (Soil Survey Section, 1991), the Exploratory Soil Map of Zambia, was produced at the same scale, 1:1 million, as the vegetation–soil map of Trapnell et al (1947). The soils of Zambia are mapped at 1:3 million as part of the Soil Atlas of Africa produced under the auspices of the Joint Research Centre of the European Union (Jones et al, 2013)

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