• Aucun résultat trouvé

Soustraction de Nombres sur Une Droite Graduée Jusqu'à 40 avec 2 Chiffres d'Intervalle (A)

N/A
N/A
Info
Télécharger
Protected

Academic year: 2021

Partager "Soustraction de Nombres sur Une Droite Graduée Jusqu'à 40 avec 2 Chiffres d'Intervalle (A)"

Copied!
2
0
0

Chargement.... (Voir le texte intégral maintenant)

Texte intégral

(1)

Soustraction de Nombres - Droite Gradu´ee (A)

Utlisez la droite gradu´

ee pour calculer chaque diff´

erence.

1.

32 − 20 =

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 2.

12 − 4 =

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 3.

24 − 12 =

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 4.

28 − 26 =

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 5.

16 − 8 =

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40

MathsLibres.com

(2)

Soustraction de Nombres - Droite Gradu´ee (A) R´eponses

Utlisez la droite gradu´

ee pour calculer chaque diff´

erence.

1.

32 − 20 =

12

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 2.

12 − 4 =

8

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 3.

24 − 12 =

12

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 4.

28 − 26 =

2

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 5.

16 − 8 =

8

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40

MathsLibres.com

Références

Télécharger maintenant ( PDF - 2 Page - 58.12 KB )

Documents relatifs

Effects of a polydisperse cloud on tropospheric chemistry

principally produced in aqueous phase, a ratio greater than 1 most likely comes rather from an increase of aqueous production, while a ratio smaller than 1 means either (1) a

Magnetic interactions at the origin of abnormal magnetic fabrics in lava flows: a case study from Kerguelen flood basalts

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

MeLa: A Programming Language for a New Multidisciplinary Oceanographic Float

Most of the mechanisms used to execute the acquisition modes concurrently are managed by the embedded software code; this includes the scheduling of tasks and the exchange of data

Late Cretaceous stratigraphy and paleoceanographic evolution in the Great Australian Bight Basin based on results from IODP Site U1512

Late Cretaceous stratigraphy and paleoceanographic evolution in the Great Australian Bight Basin based on results from IODP Site

Stretching and folding sustain microscale chemical gradients in porous media

Recent theories ( 19 , 20 ) have suggested that laminar flow through three-dimensional porous media may possess the basic ingredients for chaotic advection, which would represent a

Two-stage mid-Brunhes climate transition and mid-Pleistocene human diversification

First, stronger warming of northern hemisphere continents, weaker southern hemisphere warming, and related more extensive northward displacement of the intertropical

Inferring geostatistical properties of hydraulic conductivity fields from saline tracer tests and equivalent electrical conductivity time-series

KLDs and mean relative biases of m ⨙ for the different conditioning data types. Columns 1 and 2 show the

Quality assessment of the Ozone_cci Climate Research Data Package (release 2017) – Part 2: Ground-based validation of nadir ozone profile data products

In this section comparison results between L2 RAL v2.14 nadir ozone profiles and ground-based ozonesonde and lidar measurements are reported in the form of statistics on the me-