Articles | Volume 14, issue 4
Hydrol. Earth Syst. Sci., 14, 627–638, 2010
https://doi.org/10.5194/hess-14-627-2010
Hydrol. Earth Syst. Sci., 14, 627–638, 2010
https://doi.org/10.5194/hess-14-627-2010

  06 Apr 2010

06 Apr 2010

Modelling field scale water partitioning using on-site observations in sub-Saharan rainfed agriculture

H. Makurira1,2,3, H. H. G. Savenije2,3, and S. Uhlenbrook2,3 H. Makurira et al.
  • 1Dept. of Civil Engineering, University of Zimbabwe. P.O. Box MP 167, Mt Pleasant, Harare, Zimbabwe
  • 2Water Resources Section, Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands
  • 3UNESCO-IHE, Institute for Water Education, P.O. Box 3015, 2601 DA Delft, The Netherlands

Abstract. Smallholder rainfed farming systems generally realise sub-optimal crop yields which are largely attributed to dry spell occurrences during crop growth stages. However, through the introduction of appropriate farming practices, it is possible to substantially increase yield levels even with little and highly variable rainfall. The presented results follow research conducted in the Makanya catchment in northern Tanzania where gross rainfall amounts to less than 400 mm/season which is insufficient to support staple food crops (e.g. maize). The yields from farming system innovations (SIs), which are basically alternative cultivation techniques, are compared against traditional farming practices. The SIs tested in this research are runoff harvesting used in combination with in-field trenches and soil bunds (fanya juus). These SIs aim to reduce soil and nutrient loss from the field and, more importantly, promote in-field infiltration and water retention. Water balance components have been observed in order to study water partitioning processes for the "with" and "without" SI scenarios. Based on rainfall, soil evaporation, transpiration, runoff and soil moisture measurements, a water balance model has been developed to simulate soil moisture variations over the growing season. Simulation results show that, during the field trials, the average productive transpiration flow ranged between 1.1–1.4 mm d−1 in the trial plots compared to 0.7–1.0 mm d−1 under traditional tillage practice. Productive transpiration processes accounted for 23–29% while losses to deep percolation accounted for 33–48% of the available water. The field system has been successfully modelled using the spreadsheet-based water balance 1-D model. Conclusions from the research are that the SIs that were tested are effective in enhancing soil moisture retention at field scale and that diversions allow crop growth moisture conditions to be attained with early rains. From the partitioning analysis, it is also concluded that there is more scope for efficient utilisation of the diverted runoff water if storage structures could be installed to minimise runoff and deep percolation and, hence, regulate water flow to the root zone when required.

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