2011
DOI: 10.1590/s0103-90162011000100016
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Determination of a point sufficiently close to the asymptote in nonlinear growth functions

Abstract: Growth functions with upper horizontal asymptote do not have a maximum point, but we frequently question from which point growth can be considered practically constant, that is, from which point the curve is sufficiently close to its asymptote, so that the difference can be considered non-significant. Several methods have been employed for this purpose, such as one that verifies the significance of the difference between the curve and its asymptote using a t-test, and that of Portz et al. (2000), who used segm… Show more

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Cited by 42 publications
(47 citation statements)
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“…With the water acquisition curve it was possible to characterize Phases I, II and III of germination of A. emarginata seeds, in accordance with the triphasic pattern proposed by Bewley andBlack in 1994 (FERREIRA et al, 2006) (Figure 1). Phase I lasted 109 hours, from the start of imbibition, finishing when the seeds reached 35.2% of water, as described for endospermatic seeds (CARVALHO; NAKAGAWA, 2000).…”
Section: Resultssupporting
confidence: 73%
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“…With the water acquisition curve it was possible to characterize Phases I, II and III of germination of A. emarginata seeds, in accordance with the triphasic pattern proposed by Bewley andBlack in 1994 (FERREIRA et al, 2006) (Figure 1). Phase I lasted 109 hours, from the start of imbibition, finishing when the seeds reached 35.2% of water, as described for endospermatic seeds (CARVALHO; NAKAGAWA, 2000).…”
Section: Resultssupporting
confidence: 73%
“…Periodical weights for the calculation of seed water uptake were performed and by the stabilization of the water intake, the seeds were removed from the water and placed in 'germitest' paper, with the weighing being held until the beginning of phase III, when the emission of the primary root occurs. To study the variation in the seed water content, in phase I and the beginning of phase II, the Brody model, or monomolecular model, was adjusted to the equation y=α [1-β exp (-c x)], with y = moisture degree (%), x = time, α, β e c = model parameter (MISCHAN et al, 2011).…”
Section: Water Acquisition Curvementioning
confidence: 99%
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“…The stability points of the logistic function, mono or diphasic can be determined by various methods (Passos et al, 2012). The method that equates the fourthorder derivative of the function y to zero is employed here (Mischan et al, 2011): , X = exp(-b -γx) (13) which gives the points…”
Section: Methodsmentioning
confidence: 99%
“…The critical points of the functions, such as the infl ection point (pi) and deceleration asymptotic point (pda), are determined using the method developed in Mischan et al (2011) for the model with independent errors, model I, for the logistic function. However, autoregressive models, model II, and mixed model, model III, lead to estimated values that are discrete variables defi ned only for the observed values of x i , i = 1, ..., n. Therefore we propose a new approach, which consists in the determination of the critical points through the function (15) the estimate of F(x i , θ) in (2) and (4), obtained by adjusting the models.…”
Section: Methodsmentioning
confidence: 99%