• Aucun résultat trouvé

Calcul de la Valeur en Pourcentage des Nombres Entiers et la Sélection de Pourcentages (Sommes en Dollars) (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Calcul de la Valeur en Pourcentage des Nombres Entiers et la Sélection de Pourcentages (Sommes en Dollars) (A)"

Copied!
2
0
0

Texte intégral

(1)

Calcul du Pourcentage (A)

Calculez le pourcentage ou la valeur demandée.

1. 2. 3. 4. 5. Quel est 5% de 260 $? 6. 7. 8. 9. 10. Mathslibres.com

Quel est 33⅓% de 5 037 $? Quel est 33⅓% de 3 942 $?

Quel est 50% de 8 768 $? Quel est 20% de 6 545 $?

Quel est 20% de 6 060 $?

Quel est 75% de 3 908 $? Quel est 20% de 3 215 $?

(2)

Calcul du Pourcentage (A) Réponses

Calculez le pourcentage ou la valeur demandée.

1. 2. 3. 4. 5. Quel est 5% de 260 $? 6. 13 $ 7. 8. 643 $ 9. 10. Mathslibres.com

Quel est 33⅓% de 5 037 $? Quel est 33⅓% de 3 942 $?

1 679 $ 1 314 $

Quel est 50% de 8 768 $? Quel est 20% de 6 545 $?

4 384 $ 1 309 $

Quel est 20% de 6 060 $?

1 212 $

Quel est 75% de 3 908 $? Quel est 20% de 3 215 $?

2 931 $

Quel est 66⅔% de 3 390 $? Quel est 33⅓% de 8 946 $?

Références

Documents relatifs

plained by the near-bed hydraulic variables Vx and σVx implies that there is a degree of active or passive selection of hydraulic conditions by benthic invertebrates that occurs

of January, February, November and December). Silicate concentrations measured in March 2003 along a longitudinal transect on the Scheldt showed a conservative behaviour of..

Given the number of inundated building per sector as well as the mean and standard deviation of flood damages in that sector based on the HOWAS data base, one realisa- tion of

Concerning the seismic swarms related with volcanic phenomena, the assessed intensity values for each episode reflect the cumulative effects observed in a certain period of time

On the other hand, the simpler allocation algorithm used in the WAFLEX model, basically upstream to downstream for each water use type, may be more close to how water is

Worsztynowicz Title Page Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc. Printer-friendly Version

The presence of skill in the daily reanalysis temperature data allows the CA method to show superior skill compared to BCSD at reproducing local temperature extremes in some seasons

We used a simple storm loss model based on the following assumptions (a): Losses in- crease with the cube of the maximum daily wind speed (b): Losses only occur if a high