• Aucun résultat trouvé

Addition et Soustraction d'un Nombre à 6 Chiffres par un Nombre à 6 Chiffres SANS retenue (Gros Caractère) (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Addition et Soustraction d'un Nombre à 6 Chiffres par un Nombre à 6 Chiffres SANS retenue (Gros Caractère) (A)"

Copied!
2
0
0

Texte intégral

(1)

Addition et Soustraction SANS Retenue (A)

Nom: Date:

Calculez la somme ou la différence de chaque opération.

776939 573211 + 230545127443 443170 + 246625 513171 + 242701 777269 235100 + 721222154236 827477 610427 + 322116562362 110280 + 613603 857444 224021 + 311622412053 145910 + 630041 672925 421700 999628722018 + 214101343550 MathsLibres.com

(2)

Addition et Soustraction SANS Retenue (A) Réponses

Nom: Date:

Calculez la somme ou la différence de chaque opération.

776939 573211 203728 230545 + 127443 357988 443170 + 246625 689795 513171 + 242701 755872 777269 235100 542169 721222 + 154236 875458 827477 610427 217050 322116 + 562362 884478 110280 + 613603 723883 857444 224021 633423 311622 + 412053 723675 145910 + 630041 775951 672925 421700 251225 999628 722018 277610 214101 + 343550 557651 MathsLibres.com

Références

Documents relatifs

This event is a very good example of an appearance of a strong westward electrojet in the evening sector at all EISCAT magnetometer cross stations. The maximum of the negative

A few of the difficulties in accurately modelling high-latitude electron densities with a large-scale numer- ical model of the thermosphere and ionosphere are ad- dressed by

The evolution, and dynamics of Es clouds can be studied from backscatter data obtained by the different radar beams over a period of time.. Velocities can be determined by plotting

Lors- qu’on ne sait pas si le verbe est au mode indicatif ou subjonctif parce qu’il se prononce de la même façon, on suggère de le remplacer par un verbe comme faire ou partir, dont

A comparison of results obtained using steady-state and time-dependent models with the same mean conditions (cross-polar-cap voltage, »pc, and polar cap area) has been undertaken

They were later discriminated into tangential or rotational according to their characteristics: the former possess no ®eld normal to the discontinuity surface but show a

The height-latitude contour plots of monthly mean zonal and meridional winds for all months of the year, and of annual mean wind, amplitudes and phases of annual and

change in the calculated wave azimuth. W can also be calculated from the average of the line-of-sight velocities in the o€-vertical beams, i.e. Figure 6 shows a visible-light