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Soil Science Society of America Journal Abstract - Soil Fertility & Plant Nutrition

Soil Heterogeneity and Soil Fertility Gradients in Smallholder Farms of the East African Highlands

 

This article in SSSAJ

  1. Vol. 77 No. 2, p. 525-538
     
    Received: Aug 9, 2012
    Published: February 1, 2013


    * Corresponding author(s): pablo.tittonell@wur.nl
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doi:10.2136/sssaj2012.0250
  1. P. Tittonell *a,
  2. A. Muriukib,
  3. C. J. Klapwijkc,
  4. K. D. Shepherdd,
  5. R. Coed and
  6. B. Vanlauwee
  1. a Farming Systems Ecology Group Wageningen Univ. P.O. Box 563 6700 AN, Wageningen The Netherlands and Tropical Soil Biology and Fertility Institute of the International Centre for Tropical Agriculture (TSBF-CIAT) P.O. Box 30677 Nairobi, Kenya
    b Kenya Agricultural Research Institute P.O. Box 57811Nairobi, Kenya
    c Farming Systems Ecology Group Wageningen Univ. P.O. Box 5636700 AN, Wageningen The Netherlands
    d World Agroforestry Centre (ICRAF) P.O. Box 30677-00100 Nairobi, Kenya
    e Tropical Soil Biology and Fertility Institute of the International Centre for Tropical Agriculture (TSBF-CIAT) P.O. Box 30677 Nairobi, Kenya and International Institute of Tropical Agriculture (IITA)-Kenya P.O. Box 30709Nairobi, Kenya

Abstract

Heterogeneity in soil fertility in these smallholder systems is caused by both inherent soil-landscape and human-induced variability across farms differing in resources and practices. Interventions to address the problem of poor soil fertility in Africa must be designed to target such diversity and spatially heterogeneity. Data on soil management and soil fertility from six districts in Kenya and Uganda were gathered to understand the determinants of soil heterogeneity within farms. Analysis of the variance of soil fertility indicators across 250 randomly selected farms (i.e., 2607 fields), using a mixed model that considered site, sampling frame, farm type, and field as random terms, revealed that the variation in soil organic C (6.5–27.7 g kg−1), total N (0.6–3.0 g kg−1), and available P (0.9–27 mg kg−1) was mostly related to differences in the inherent properties of the soils across sites (50 to 60% of total variance). Exchangeable K+ (0.1–1.1 cmol(+) kg−1), Ca2+ (1.5–14.5 cmol(+) kg−1), Mg2+ (0.6–3.7 cmol(+) kg−1), and pH (5.1–6.9) exhibited larger residual variability associated with field-to-field differences within farms (30 to 50%). Soil fertility indicators decreased significantly with increasing distance from the homesteads. When this variable was included in the model, the unexplained residual variances—associated with soil heterogeneity within farms—were 38% for soil C; 32% for total N; 49% for available P; 56, 49, and 38% for exchangeable K+, Ca2+ and Mg2+, respectively; and 49% for the pH. In allocating nutrient resources, farmers prioritized fields they perceived as most fertile, reinforcing soil heterogeneity. Categorization of fields within a farm with respect to distance from the homestead, and soil fertility classes as perceived by farmers, were identified as entry points to target soil fertility recommendations to easily recognizable, distinct entities.

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Copyright © 2013. Copyright © by the Soil Science Society of America, Inc.