2003
DOI: 10.1614/p2002-108
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The use of thermal time to model common lambsquarters (Chenopodium album) seedling emergence in corn

Abstract: A mathematical model was developed to predict common lambsquarters seedling emergence in southwestern Quebec. The model was based on the thermal-time concept, using air temperatures in the double-sine calculation method. The model was built using data from five experiment-years for corn naturally infested with weed populations. Once developed, the model was calibrated using different crop seedbed preparation times. The base temperature was then adjusted for each time of seedbed preparation. A power regression … Show more

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Cited by 25 publications
(24 citation statements)
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“…Os parâmetros k, a e c foram estimados por um procedimento de regressão não-linear, usando o método DUD (Doesn't Use Derivative) de computação (Ralston & Jennrich, 1979). Esse é um método de regressão não-linear que usa o método iterativo multivariado secante para estimar os parâmetros de interesse (Bahler et al, 1989).…”
Section: Methodsunclassified
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“…Os parâmetros k, a e c foram estimados por um procedimento de regressão não-linear, usando o método DUD (Doesn't Use Derivative) de computação (Ralston & Jennrich, 1979). Esse é um método de regressão não-linear que usa o método iterativo multivariado secante para estimar os parâmetros de interesse (Bahler et al, 1989).…”
Section: Methodsunclassified
“…Os parâmetros k, a e c foram estimados por um procedimento de regressão não-linear, usando o método DUD (Doesn't Use Derivative) de computação (Ralston & Jennrich, 1979), plotando o tempo hidrotérmico versus porcentagem de germinação.…”
Section: Methodsunclassified
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“…The cumulative soil thermal time (CTT) was estimated daily during the growing season with the following equation (Leblanc et al, 2003;Leguizamon et al, 2005;Izquierdo et al, 2013):…”
Section: Model Descriptionmentioning
confidence: 99%
“…Daily soil temperature and water content were used to calculate accumulated thermal ( Θ T ) and hydrothermal ( Θ H ) time under a range of different base temperatures and base water potentials ( T b and Ψ b , respectively). Although several methods for calculating thermal time have been proposed, we used the mean‐minus‐base method (Leblanc et al. , 2003): where Θ T represents the thermal time to seedling emergence (in growing degree days), i is the starting date to cumulate degree days, n is the time required to complete emergence, T max and T min are the daily maximum and minimum temperatures and T b is the base temperature for emergence.…”
Section: Estimation Of Thermal and Hydrothermal Timementioning
confidence: 99%