Experiment alone can tell us the values of m and n; all that the theory tells us is that they are whole numbers.
SENEGAL, a river of West Africa, entering the Atlantic about 16° N., some io m.
N:CH N N:C(CH3) N NH CO NH ' 'CH :CH CH NH2 C :CH C CH 3 CH :CH 0 Pyrimidine Cyanmethine Uracil
Above sea-level, in 10° 28' N., 10 5' W., its source being within 125 m.
On the N.E.
The Bakhoy, in its upper course much interrupted by rapids, flows N.E., but about 12° 15' N.
The Baule flows north and in a series of loops reaches 14° 20' N., where it turns westward and in about 13° 30 N.
The river attains its most northerly point, 16° 30' N., in about 15° 10' W.
N.s., Central nervous system.
It rises in Abyssinia to the N.W.
ALLANTOIN, C 4 H 6 N 4 O 3 or CO Q `, the NH-CO diureide of glyoxylic acid.
It can be obtained by the oxidation of uric acid by means of lead dioxide, manganese dioxide, ozone or potassium permanganate: C 5 H 4 N 4 O 3 + H 2 O + O = C 4 H 6 N 4 O 3 + C02.
On standing with concentrated potassium hydroxide solution it gives potassium allantoate C 4 H 7 N 4 O 4 K.
On heating with water it undergoes hydrolysis into urea and allanturic acid C 3 H 4 O 3 N 2.
It is reduced by sodium amalgam to glycouril C 4 H 6 N 4 O 2, whilst with hydriodic acid it yields urea and hydantoin C 3 H 4 N 2 O 2.
His magnum opus was T Wonder Boeck (n.d.
It has a general trend from N.E.
ASTORGA, a city of N.W.
CH3 CH 2 CO(CH 3) + N 5 3 C .
H HN CEH?Chch C(Ch3)N.Cs The ketonic esters under like treatment yield oxypyrimidines, whilst if cyanacetic ester be employed then amino-oxypyrimidines are obtained.
Cyanmethine, C 6 H 9 N 3 (dimethyl-aminopyrimidine -2.4.
They made their way unscathed through the dining room to their own little corner, where Toby.s favorite food combination of mac-n-cheese and French toast waited for him on the table.
At the general election of 1900 he preferred to contest the N.E.
We can therefore predict that all oxides of carbon will have compositions represented by the ratio of 8m parts of oxygen to 6n parts of carbon, where m and n are whole numbers.
In this particular case, n turns out to be 3, and m has in succession the values I, 2, 3, 4, 5.
When heated with hydriodic acid and phosphorus, it yields n-valeric acid; and with iodine and caustic soda solution it gives iodoform, even in the cold.
If this is true we should have q= an t, where q is the number of ions of one sign made in I cc. of air per second by the emanation, a the constant of recombination, and n the number of ions found simultaneously by, say, Ebert's apparatus.
Karasjok as already mentioned is in the extreme north of Norway (69° 17' N.); Sodankyla was the Finnish station of the international polar year 1882-1883.
Per hour q exceeded unity n 74 cases out of too; but for velocities over 50 km.
ALASSIO, a town of Liguria, Italy, on the N.W.
(2) The acceleration of the element at the origin is - n 2 sin nt; so that the force which would have to be applied to the parts where the density is D' (instead of D), in order that the waves might pass on undisturbed, is, per unit of volume, (D' - D)n 2 sin nt.
Thus by equation (18) of § II of the article Diffraction Of Light, the secondary disturbance is expressed by D' - D n 2 Tsin sin (nt - kr) D 47rb2 r _ D' - D irTsin O sin (nt - kr) (3)1 The preceding investigation is based upon the assumption that in passing from one medium to another the rigidity of the aether does not change.
If the primary wave be represented by = e-ikx the component rotations in the secondary wave are '1'3= P (- AN y) N r2 ' cwi= r x D y N 'y)' lw2=P (- AD + 6,N z2 - x2 ' D r N r2 where ik3T e-ikr _ P - 4 r The expression for the resultant rotation in the general case would be rather complicated, and is not needed for our purpose.
We have 62=W12+W22+032=P2 (N) 2 Y 2+P2 (A I - 3) 2 If AN, AD be both finite, we learn from (7) that there is no direction perpendicular to the primary (polarized) ray in which the secondary light vanishes.
The element of area being 22rr 2 sin 04,, we have f:2 l 2x r2 si n 2 d ?=gam, r so that the energy emitted from T is represented by 87r3 (D, - D) 2 T2 (9) D2 x4' on such a scale that the energy of the primary wave is unity per unit of wave-front area.
In 1897 the ship " Washington " obtained depths of 2220 fathoms in the middle of the eastern Mediterranean; and the Austrian expeditions in the " Pola " discovered in the " Pola Deep " (35° 44' N., 21 45' E.), south-west of Cape Matapan, a maximum depth of 2046 fathoms. Between these two deep areas a ridge runs in a north-westerly direction 550 fathoms from the surface - possibly a projection from the African plateau.