On-farm sampling density and correction requirements for soil moisture determination in irrigated heavy clay soils in the Gezira, central Sudan
Introduction
In line with the call for better understanding of agrodiversity to improve its management, there is an increasing attention for the actual variations of soil properties in cropped soils and the way African farmers may exploit these variations (Steenhuijsen Piters, 1995). Analysis of such cases requires other approaches in research to be further developed in order to characterize, measure and understand relevant variations in agroecosystems in general (Almekinders et al., 1995). The interest for such precision farming is also rising in western agriculture. Sampling methodologies for such studies have to be further developed.
In the Traditional Techniques of Microclimate Improvement Project (TTMI/AN, 1996), traditional cropping techniques are compared with (other) current methods. Tenants in the Gezira scheme, central Sudan, abandoned labour intensive irrigation methods for unattended irrigation that is suspected to waste water. The difference in water use efficiencies between these methods had to be quantified on-farm (Ibrahim et al., 1999).
Little quantitative attention has been given to soil moisture heterogeneities in general and in the irrigated soils of the Gezira in particular. Results from the on-farm over-sampling experiment presented in this paper are intended to contribute to knowledge on sampling density requirements as well as moisture variations in these and other swelling clays. This should lead to better understanding of irrigation water management in farmers' fields, especially in surface irrigation methods which are known for their low application efficiencies (FAO, 1971). Soil-physical studies that have attempted to develop flow theory for swelling soils have not reached an operational stage for field applications (Bouma and Loveday, 1988).
Section snippets
Selection of a measuring approach
To determine water use efficiencies in traditional and current irrigation methods, as a step in our particular research approach (Mungai et al., 1996) in 1986 a method and a sampling procedure had to be selected to allow sufficiently accurate soil moisture measurements under very inhomogeneous on-farm conditions.
Some years before, Greacen (1981)had published essential indications on calibration and the use of the neutron probe in general, also with good attention to cracking clays. Gardner
Daytime air temperature
In Fig. 3, fluctuation of daytime air temperature and the simultaneous fluctuations of the neutron probe counting rates in the shield are in opposite directions but in phase with each other. The latter showed a maximum difference of 3.5% moisture content by volume during the calibration in the water drums. The difference was assumed to be due to air temperature influence on the neutron probe response, as was also found for example by Zuber and Cameron (1966). Because of almost identical
Conclusions and final discussion
Blokhuis (1993)has indicated that the formation of the Gezira Plain clay soils was rather uniform in the parts now forming the irrigation systems. The top 50 cm of the agricultural fields are ploughed since 1926, these days mechanically every 4 years. Despite this homogeneity, shrinkage cracks and less than optimal land levelling have been shown in this paper to seriously influence the soil moisture distribution in the field. At 30 cm (the depth with the largest variations of neutron probe
Acknowledgements
The authors are highly indebted to the Directorate General of International Cooperation research focal program (DGIS/DST/SO) of the Ministry of Foreign Affairs, The Netherlands, that funded all necessary equipment and Dutch co-supervision for the research through the Traditional Techniques of Microclimate Improvement (TTMI) Project. Thanks are also due to the technical staff of the Hydraulics Research Station of the Ministry of Irrigation and the University of Gezira, Wad Medani, Sudan and of
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