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Valutazione dell’equazione di conicità e volume 'polinomiale di 5° grado'

Valutazione dell’equazione di conicità e volume 'polinomiale di 5° grado'

JAIME Antonio Ubiali / Patricia Aparecida Takase / Rodrigo Lemos Gil

49,68 €
IVA incluido
Disponible
Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Botánica y ciencias de las plantas
ISBN:
9786208732592
49,68 €
IVA incluido
Disponible

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Sobre IBD

Lo scopo di questo studio è stato quello di valutare l’accuratezza del modello proposto da Schöepfer (polinomiale di 5° grado) per il diradamento e il volume, per l’insieme dei dati e per classe di diametro, in un popolamento di Tectona grandis L.f. nel comune di Rosário Oeste - MT. Sono stati valutati i seguenti parametri statistici: coefficiente di determinazione aggiustato (R²), errore standard di stima (Syx %) e analisi grafica dei residui sia per i diametri che per i volumi. Il modello si è dimostrato accurato nella stima dei diametri e dei volumi sia per le classi di diametro che per l’insieme dei dati. Questo libro è essenziale per i professionisti del settore forestale e per gli accademici che conducono ricerche dendrometriche su Tectona grandis.

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Otros libros del autor

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  • Evaluation of the '5th degree polynomial' tapering and volume equation
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    The aim of this work was to assess the accuracy of the model proposed by Schöepfer (5th degree polynomial) for thinning and volume, for the total set of data and by diameter class, in a stand of Tectona grandis L.f. in the municipality of Rosário Oeste - MT. The following statistical parameters were evaluated: Adjusted Coefficient of Determination (R²), Standard Error of Estima...
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    Celem tego badania była ocena dokładności modelu zaproponowanego przez Schöepfera (wielomian 5. stopnia) dla przerzedzania i miąższości, dla całego zestawu danych i według klasy średnicy, w drzewostanie Tectona grandis L.f. w gminie Rosário Oeste - MT. Oceniono następujące parametry statystyczne: skorygowany współczynnik determinacji (R²), błąd standardowy oszacowania (Syx %) i...
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