1997
DOI: 10.2134/agronj1997.00021962008900030019x
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Managing Yield and Water Use of Pearl Millet in the Sahel

Abstract: Drought occurs often in the West African Sahel, but studies have shown that soil water availability is not usually the limiting factor to pearl millet [Pennisetum glaucum (L.) R. Br.] production, and that field water‐use efficiency (WUE)—i.e., the ratio of yield to evapotranspiration (ET)—is almost always very low. The purpose of this study was to determine management effects on yield and water use of pearl millet for a range of climate conditions in the Sahel. Grain and aboveground dry matter yield, daily vap… Show more

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Cited by 46 publications
(45 citation statements)
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“…Viets (1962) explained that since the evapotranspiration is little affected by the management, as was the case in the current study (data not presented), any factor that increases yield will increase WUE. These results are consistent with the earlier studies which reported an increment of millet water use efficiency in response to soil fertility management options in the Sahelian zone due to increase in biomass production (Akponikpé et al, 2008;Manyame, 2006;Payne, 1997;Yamoah et al, 2002). The results of the present study are also in agreement with the findings of Wang et al (2013) for maize.…”
Section: Discussionsupporting
confidence: 94%
See 1 more Smart Citation
“…Viets (1962) explained that since the evapotranspiration is little affected by the management, as was the case in the current study (data not presented), any factor that increases yield will increase WUE. These results are consistent with the earlier studies which reported an increment of millet water use efficiency in response to soil fertility management options in the Sahelian zone due to increase in biomass production (Akponikpé et al, 2008;Manyame, 2006;Payne, 1997;Yamoah et al, 2002). The results of the present study are also in agreement with the findings of Wang et al (2013) for maize.…”
Section: Discussionsupporting
confidence: 94%
“…Access tubes were installed in all the plots to monitor weekly soil moisture with a calibrated neutron probe from 0.15 to 2 m depth at 0.15 m intervals. The change in soil water storage in the root zone was calculated from the equation used by Payne (1997) as follows:…”
Section: Soil Moisture Monitoringmentioning
confidence: 99%
“…We directly estimated K at the maximum rooting depth, Z r (1.4 m) using the two stage method proposed by Klaij and Vachaud (1992). Knowledge of K for this depth is needed to calculate root zone drainage and other soil water balance terms (Payne, 1997). In Klaij and Vachaud (1992), stage one represents the beginning of the season when the soil is wetting and the wetting front has not yet passed the bottom of the soil profile (1.8 m).…”
Section: Site Description and Soil Sampling Strategymentioning
confidence: 99%
“…In the same environment drainage is, in many cases, almost equal to the water lost as soil evaporation and transpiration (Gaze et al, 1997;Rockstrom, 1977). Such findings have led many to conclude that the efficiency with which water is used to produce crops could be significantly improved in many rainfed environments (Payne, 1997).…”
Section: Food Production and Water Usementioning
confidence: 99%