• Aucun résultat trouvé

Addition et Soustraction de Nombres sur une Droite Graduée Jusqu'à 20 avec 1 Chiffre d'Intervalle (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Addition et Soustraction de Nombres sur une Droite Graduée Jusqu'à 20 avec 1 Chiffre d'Intervalle (A)"

Copied!
2
0
0

Texte intégral

(1)

Op´erations sur Une Droite Gradu´ee (A)

Utlisez la droite gradu´

ee pour calculer chaque somme ou diff´

erence.

1.

14 + 2 =

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 2.

12 − 1 =

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 3.

8 + 4 =

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 4.

7 − 4 =

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 5.

14 − 2 =

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

MathsLibres.com

(2)

Op´erations sur Une Droite Gradu´ee (A) R´eponses

Utlisez la droite gradu´

ee pour calculer chaque somme ou diff´

erence.

1.

14 + 2 =

16

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 2.

12 − 1 =

11

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 3.

8 + 4 =

12

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 4.

7 − 4 =

3

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 5.

14 − 2 =

12

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

MathsLibres.com

Références

Documents relatifs

Received: 12 October 2018; Accepted: 30 October 2018; Published: 3 November 2018    Abstract: We discuss the different challenges, pros and cons of the fairly

The two simple models presented here clearly illustrate the importance of using an accurate stochastic model for the prediction uncertainty in order to reliably infer the

Hybrid Finite Element formulation for variably saturated groundwater flow. Hydraulic properties of porous media. State Univ., Fort Collins. Numerical simulations of

As observed for the case of 16 May 2007, the in situ measurements indicate smaller values of ef- fective diameter and extinction than the retrievals obtained from

To confirm the abnormal nature of Group 2 AMS fabric and to check unambiguously the hypothesis of an inverse fabric induced by SD grains (Potter & Stephenson 1988), we measured

In this study, we present a characterisation of the vertical, spatial and seasonal variability of Arctic clouds and MPCs over the entire Arctic region based on satellite active

Comparing the results for the different simulations in Ta- ble 2, it becomes obvious that the total rain mass is highest for the Remote aerosol particle distribution, then decreases

Collection efficiencies measured for drops of 2 mm in diameter as a function of relative humidity, and comparison with the model of Davenport and Peters (1978), a semi-empirical