1991
DOI: 10.1111/j.1574-0862.1991.tb00174.x
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Modelling stochastic crop response to fertilisation when carry‐over matters

Abstract: Jomini, P.A., Deuson, RR., Lowenberg-DeBoer, J. and Bationo, A., 1991. Modelling stochastic crop response to fertilization when carry-over matters. Agric. Econ.,

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Cited by 6 publications
(7 citation statements)
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“…The static steady‐state‐based tax‐subsidy‐scheme yields almost the same NPV as the first‐best instrument, unless the soil of a target area has a high ability to hold nutrients (clay soils) and the legacy P store, x0 is considerably above its steady‐state level, x (Figure 5). This is because on coarse soils the steady state is reached fast in the beginning of a planning horizon, in line with the findings of the previous literature (Jomini et al, 1991; Kennedy et al, 1973). If x0 is far from x, the static tax‐subsidy‐scheme generates welfare losses from a long period in the beginning of a planning horizon.…”
Section: Quantitative Assessmentsupporting
confidence: 91%
See 1 more Smart Citation
“…The static steady‐state‐based tax‐subsidy‐scheme yields almost the same NPV as the first‐best instrument, unless the soil of a target area has a high ability to hold nutrients (clay soils) and the legacy P store, x0 is considerably above its steady‐state level, x (Figure 5). This is because on coarse soils the steady state is reached fast in the beginning of a planning horizon, in line with the findings of the previous literature (Jomini et al, 1991; Kennedy et al, 1973). If x0 is far from x, the static tax‐subsidy‐scheme generates welfare losses from a long period in the beginning of a planning horizon.…”
Section: Quantitative Assessmentsupporting
confidence: 91%
“…cultivation in southern Finland on coarse and clay textured soils. Our modelling approach extends the approach by Jomini et al (1991), Bäckman and Lansink (2005), and Lambert et al (2007) who studied economically optimal P and N rates (in slightly different settings) while considering P carryover effects, by including N carryover, nutrient loss processes, environmental policy, and several nonlinear interactions among the model components in the analysis. We also extend the approach by Iho (2010), Iho and Laukkanen (2012a, 2012b) by including N in the analysis.…”
Section: Introductionmentioning
confidence: 96%
“…Soils in Niger are generally sandy and low in organic matter (Jomini et al, 1991), deficient in phosphorus (P) and nitrogen (N) (Baïdu‐Forson and Bationo, 1992), and low in moisture‐retention capacity (Mahaman, 1988). Manure can provide organic matter and water retention, but it has very low nutrient value because the livestock eat poorly and because manure is always low in N and P. Only at very high levels of manure (not available to farmers in Niger) of 6 to 10 mt/ha can reasonable levels of N and P be provided.…”
Section: Fertilization Alternativesmentioning
confidence: 99%
“…Unfortunately, the rock generally has very low P levels and is insoluble except in higher rainfall, acidic soil environments. Even with devaluation the rock phosphate generally is so insoluble that it is not likely to become competitive with imported inorganic fertilizers (Jomini et al, 1991). The acidification to make it more soluble depends upon the availability of industrial raw materials not available in sub-Saharan Africa.…”
Section: Inorganic Fertilizersmentioning
confidence: 99%