• Aucun résultat trouvé

Calcul d'un Pourcentage d'Augmentation/Diminution avec des Montants en Dollars avec des Intervales de 5 Pour Cent (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Calcul d'un Pourcentage d'Augmentation/Diminution avec des Montants en Dollars avec des Intervales de 5 Pour Cent (A)"

Copied!
2
0
0

Texte intégral

(1)

Pourcentage d'Augmentation/Diminution (A)

Nom: Date:

Calculez le pourcentage d’augmentation ou de diminution.

Valeur de

départ d’arrivéeValeur Augmentation/Diminution

Variation en pourcentage 1. $160 $112 2. $112 $28 3. $960 $1296 4. $740 $37 5. $240 $180 6. $825 $990 7. $430 $731 8. $580 $203 9. $840 $1218 10. $740 $1184 MathsLibres.com

(2)

Pourcentage d'Augmentation/Diminution (A) Réponses

Nom: Date:

Calculez le pourcentage d’augmentation ou de diminution.

Valeur de

départ d’arrivéeValeur Augmentation/Diminution

Variation en pourcentage 1. $160 $112 112−160 160 =‑30% 2. $112 $28 28−112 112 =‑75% 3. $960 $1296 1296−960 960 =35% 4. $740 $37 37−740 740 =‑95% 5. $240 $180 180−240 240 =‑25% 6. $825 $990 990−825 825 =20% 7. $430 $731 731−430 430 =70% 8. $580 $203 203−580 580 =‑65% 9. $840 $1218 1218−840 840 =45% 10. $740 $1184 1184−740 740 =60% MathsLibres.com

Références

Documents relatifs

Lidar observations give access to sev- eral cirrus characteristics such as the cloud absolute geometric height, cloud thickness, backscattering ratio (called here intensity, which

( 2009 ) demon- strated that a change in radius of 2 × 10 −4 perturbs the inter- nal structure down to 0.99 R  through opacity and equation of state variations that could

Pliocene and Late Pleistocene actinopterygian fishes from Santa Maria Island, Azores (NE Atlantic Ocean): palaeoecological and palaeobiogeographical implications... 2 Departamento

Le complément du nom est parfois constitué d’un groupe prépositionnel (GPrép) formé d’une préposition et d’un nom sans déterminant. une divergence d’opinions une bonne dose

A second hypothesis that could explain the observed result would be that different zooplankton communities would be conveyed to the study area in the course of changes in surface

In this context, a model reduction technique is proposed in this paper, for the analysis of asynchronous Boolean networks motivated by biological (namely, signalling or

Further analysis using a photochemical trajectory model and compar- ison with measured concentrations in the Lagrangian match segments will provide an insight into the processes

This study (hereafter referred to as TR2003) calculated the expected increases in stratospheric water vapour resulting from increased con- centrations of atmospheric hydrogen