• Aucun résultat trouvé

Addition et Soustraction d'un Nombre à 4 Chiffres par un Nombre à 2 Chiffres (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Addition et Soustraction d'un Nombre à 4 Chiffres par un Nombre à 2 Chiffres (A)"

Copied!
2
0
0

Texte intégral

(1)

Addition et Soustraction de Nombres (A)

Nom: Date:

Calculez la somme ou la différence de chaque opération.

9356 + 32 5469 + 22 9050 68 4023 + 15 5355 + 41 2984 60 6705 11 2613 49 6161 56 1486 34 1737 + 87 8688 86 4140 95 3455 + 36 3511 + 39 7823 26 1782 + 83 1580 + 39 4210 11 9952 + 44 5721 10 7560 23 1938 + 56 3991 61 1355 + 23 MathsLibres.com

(2)

Addition et Soustraction de Nombres (A) Réponses

Nom: Date:

Calculez la somme ou la différence de chaque opération.

9356 + 32 9388 5469 + 22 5491 9050 68 8982 4023 + 15 4038 5355 + 41 5396 2984 60 2924 6705 11 6694 2613 49 2564 6161 56 6105 1486 34 1452 1737 + 87 1824 8688 86 8602 4140 95 4045 3455 + 36 3491 3511 + 39 3550 7823 26 7797 1782 + 83 1865 1580 + 39 1619 4210 11 4199 9952 + 44 9996 5721 10 5711 7560 23 7537 1938 + 56 1994 3991 61 3930 1355 + 23 1378 MathsLibres.com

Références

Documents relatifs

Our present SERRS sandwich-hybridization assay is based on the specific hybridiza- tion of two nucleic probes to target DNA to be detected in solution (Figure 1).. The nucleic

Simulating nitrogen budgets in complex farming systems using INCA: calibration and scenario analyses for the Kervidy catchment but, in terms of nitrate flux, the result is almost

stratosphere and lower mesosphere is presented in Figure 3 for the October 2003 – April 2004 period, using both MIPAS and GOMOS data for latitudes higher than 65°N.. The daily-

Ozone vertical profiles derived from nadir mea- surements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the Univer- sity of Bremen,

(4) and (5), the values of kx and kz are chosen to be the dominant horizontal and vertical wave numbers at each integer hour (shown in Fig. 2), respectively; the values u; w and ma

On the basis of Morlet wavelet transform applied to the hourly values of the amplitudes of diurnal and semidiurnal tides the tidal variability with periods of planetary waves

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

The ionospheric signature of a ¯ux transfer event (FTE) seen in EISCAT radar data has been used as the basis for a modelling study using a new numerical model of the