Abstract

Eritrean farmers can cultivate rice by harvesting runoff from >82% available non-agricultural land in agricultural watersheds for crop use and reducing percolation through optimization of tillage. Experiments were conducted with NERICA rice, N11, to optimize irrigation requirements and puddling and compaction to reduce percolation. Experimental field was adjacent to Anseba River at downstream end of the watershed and a pond on the upstream to intercept runoff. Irrigation treatments were runoff farming with maximum runoff application depth of 10 mm (I1), and 50 mm irrigation two (I2), five (I3), and seven (I4) days after disappearance of ponded water in main plots and puddling by one (T1), two (T2) and three (T3) passes of puddler and compaction by three (T4), four (T5) and five (T6) passes of 600 kg roller in sub plots in 3 replications. Soil profile was loam in the surface 0.45 m and coarse sandy loam below forming porous belt. Soil submergence was difficult to maintain, but water table was developed in soil profile due to inflow of seepage from the river and pond. Depth to the water table was within 1.5 ± 0.1 m for >2 months and receded down to 1.7 m by crop maturity. Soil wetness was near field capacity around 0.7 m depth and increased below due to natural sub-irrigation from the water table. Rice roots penetrated 0.8 m in the puddled plots and 0.7 m in the compacted plots. Residual soil moisture of 135 - 146 mm·m-1 after rice harvesting provides opportunity for planting rapeseed mustered following rice. Puddling was superior to compaction in loam soil. Puddling twice and irrigation 50 mm 7 days after ponded water vanished from surface was sufficient for optimum rice grain yield of 4346 kg·ha-1 and straw yield of 4458 kg·ha-1. Optimum puddling and irrigation schedules reduced crop duration by 6 days without significantly affecting yield. Production function showed that rice grain yield of 4789 kg ha-1 could be obtained by 1009 mm applied water through rainfall and irrigation.

Highlights

  • Rice (Oryza sativa L.) is among the oldest and widely grown food crops in the world [1]

  • There was no change in density below 0.2 - 0.3 m layer due to puddling or compaction

  • Amount of water used in I1 (RF) and I4 were almost same but yields were significantly higher in I4 than in I1

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Summary

Introduction

Rice (Oryza sativa L.) is among the oldest and widely grown food crops in the world [1]. Average water requirements of New Rice for Africa (NERICA) under deficit irrigation conditions were about 800 mm for 115 - 120 days crop yielding 2 - 4 t·ha−1 [17] [18]. Soil puddling and compaction are common field practices to reduce percolation losses. Puddling is plowing the field under water-saturated conditions to enhance water retention and reduce deep percolation [20] [21]. Practices to minimize high percolation from rice fields were known and possibilities of runoff farming existed in Eritrea [38], no systematic efforts were made to cultivate rice due to fear of its high water requirements, inadequate rainfall and highly permeable soils.

Methods and Material
Experimental Details
Root Length Density
Bulk Density Variation with Depth in Rice Field
Water Table Fluctuation and Wetness in the Root Zone
Growth Pattern of Rice
Rooting Pattern of Rice
Grain Yield of Rice
Straw Yield of Rice
Water Production Function
Residual Moisture after Rice
Conclusions
Full Text
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