"Oo-oo, my beauty!" exclaimed the count, "she looks better than any of you!"
Item 25.803, idem quod 25M, 8r, Item 9999998.0005021, idem valet quod 9999998 T O M0 - 0, o o oo, & sic de caeteris."
15o,ooo horses and mules are maintained on a peace footing and oo,ooo on a war footing.
On the 2gth of June 1881 the Chamber adopted a Franchise Reform Bill, which increased the electorate from oo,ooo to 2,000,000 by lowering the fiscal qualification from 40 to 19.80 lire in direct taxation, and by extending the suffrage to all persons who had passed through the two lower standards of the elementary schools, and practically to all persons able to read and write.
All civil cases involving less than z oo roubles value were within their competence, and more important cases by consent of the parties.
The following equations give the result of direct experiment :- C +20 = CO 2+943 oo cal.
Along the jet surface A'J', q = Q, b-a' ch nSl= cos 110= a-a la - b sh nft=i sin nO=i a'>u=a'erl"> -oo, giving the intrinsic equation.
Generally, by making a' = -oo, the line x'A' may be taken as a straight stream line of infinite length, forming an axis of symmetry; and then by duplica tion the result can be ob A tained, with assigned n, a, and b, of the efflux from a symmetrical converging FIG.
Thus with a' =o, a stream is split symmetrically by a wedge of angle ' zr/n as in Bobyleff's problem; and, by making a = oo, the wedge extends to infinity; then chnS2= u, sh nS2= b n u.
(12) Along the stream line xABPJ, 4) =o; and along the jet surface PJ, -1 >49> - oo; and putting 4 = -irs/c - I, the intrinsic quation is irs/c =cot 2 nO, (13) hich for n =I is the evolute of a catenary.
0-00, u = b at the branch point B, u = j, j at the end of the two diverging streams where = -oo; while ¢=0 along the stream line which divides at B and passes through A, A'; and 4 ' =m, -m' along the outside boundaries, so that m/Q, m'/Q is the final breadth of the jets, and (m+m')/Q is the initial breadth, c, of the impinging stream.
ZUy2BB0 Bll; reducing, when the liquid extends to infinity and B 3 =0, to = xA o' _ - zUy 2B o so that in the relative motion past the body, as when fixed in the current U parallel to xO, A 4)'=ZUx(I+Bo), 4)'= zUy2(I-B o) (6) Changing the origin from the centre to the focus of a prolate spheroid, then putting b 2 =pa, A = A'a, and proceeding to the limit where a = oo, we find for a paraboloid of revolution P B - p (7) B = 2p +A/' Bo p+A y2 i =p+A'- 2x, (8) p+?
T oo, and in Christianity to A.D.
A green pigment known as Rinmann's green is prepared by mixing I oo parts of zinc vitriol with 2.5 parts of cobalt nitrate and heating the mixture to redness, to produce a compound of the two oxides.
If we assume that s is a linear function of 0, s= so(I +aO), the adiabatic equation takes the form, s 0 log e OW +aso(0 - Oo) +R loge(v/vo) =o
Neglecting small terms of the second order, the equation may then be written in the form v - b=RO/p - co(Oo/O)=V - c,..
We thus obtain E - g o= s 0 (B-o)) - n(pc - poco) (31) We have similarly for the total heat F = E + pv, F - Fo=So(O - oo) - (n+1)(cp - copo)+b(p - p.).
Izerbacea and arctic species generally, to 1 oo ft., and occurring most abundantly in cold or temperate climates in both hemispheres, and generally in moist situations; a few species occur in the tropical and sub-tropical portions of the three great continents.
Thus the contribution to the total impulsive pressure exerted on the area dS in time dt from this cause is mu X udtdS X (11 3 m 3 /,r 3)e hm (u2+v2+w2 )dudvdw (I o) The total pressure exerted in bringing the centres of gravity of all the colliding molecules to rest normally to the boundary is obtained by first integrating this expression with respect to u, v, w, the limits being all values for which collisions are possible (namely from - co too for u, and from - oo to + oo for v and w), and then summing for all kinds of molecules in the gas.
The aggregate amount of these pressures is clearly the sum of the momenta, normal to the boundary, of all molecules which have left dS within a time dt, and this will be given by expression (pp), integrated with respect to u from o to and with respect to v and w from - oo to +oo, and then summed for all kinds of molecules in the gas.
ATTLEBOROUGH, a township of Bristol county, in south-east Massachusetts, U.S.A. Pop. (1890) 7577; (1 9 oo) 11,335, of whom 3237 were foreign-born; (1906, estimate) 12, 9 75.
I g h oo hsuvii where T is the area of a trapezette whose ordinates at successive distances h are o, Ali' (x i), (Al +A4), g 5' (x2), (Az +A 2 + ...
One of these, which settled at Florence before the year II oo, divided in the 13th century into the two branches of San Miniato and Sarzana.
"Oo-oo, my beauty!" exclaimed the count, "she looks better than any of you!"
At the end of the third verse as the last note died away, twenty voices roared out at once: Oo-oo-oo-oo!
At first she frowned, then broke into a huge smile and started to sing, "You oo oo love her."
Of Naples marked his recognition of Vico's merits by appointing him historiographer-royal, with a yearly stipend of t oo ducats.
From 1448 to 1450 £3336 or some £i oo,000 of our money was spent on the church, of which Waynflete with the marquis of Suffolk and the bishop of Salisbury contributed £700 or £21,000.
The dock and victualling yards occupy together an area of some i oo acres spread over the shores on both sides of those arms of the great harbour known as "Dockyard" and "French" creeks, the dockyard being partly on the former, but principally on the latter creek.
B, Digestive gland from interior A, B, and C magnified about of pitcher, in pocket-like deI oo diameters.
Sxst December iSSi 940,oO,000 -.
I8g6 400,000,oO 110,000,000 0,069,233,376 f,579,233,376
Oo f gastropore.
Not only the higher chains of Caucasus and Yaila, but also the Donets ridge, rose above the :oo 4?.
"Middle" or "South Wall" (T6 8ta Oo-ov TE7Xos, Plato, Gorg.
R d, t; oo V ci+;C?..m.os``% ?B,tier°nL.'- 10'1' ï¿½, '.
Wide between Capes Hicacos in Cuba and Arenas in Florida (Key West being a little over i oo m.
Water drifting into the North Atlantic from the equatorial stream has a relatively high salinity (from 36°/oo to 36.5°/00) and a high temperature (from 15°C. to 20°C.), and when the distribution of salinity from season to season is studied it is seen that the area of dense water (salinity 36°/00) extends farther to the N.
The flow culminates about March in each year, when a considerable part of the North Sea is covered with water of 35 °/oo salinity, but in Nov.
For strong magnetizing forces (which in these experiments did not exceed II= 48.9) the permeability remains almost constant at its initial value (about 400), until the temperature is within nearly i oo of the critical point; then the permeability diminishes more and more rapidly until the critical point is reached and the magnetization vanishes.
Pressure is 0'00141 grm., the mass at any absolute temperature 0 is by Charles's law o oo 141 X 2 739 = 0 3 849/9 grm.; hence the susceptibility per unit of volume at 760 mm.
L oo and 300, and adapted to this new use about the latter date.
Long and about oo yds.
By the principle of energy the illumination over the entire focal plane must be equal to that over the diffracting area; and thus, in accordance with the suppositions by which (3) was obtained, its value when integrated from E= co to = -1-x, and from n = - oo to n = -1-oo should be equal to ab.
If the subject of examination be a luminous line parallel to n, we shall obtain what we require by integrating (4) with respect to 77 from - oo to + oo.
By differentiation with respect to g i it may be proved that from g, = - oo to g i = - 2h1, from g, = - 2h, to g1=0, from g, = 0 to g, =2h,, from g,=2h, to g,=oo.
1, may be determined by direct integration of (12), or from the observation that by their constitution G and H vanish when u= oo, coupled with the fact that C and S then assume the value 2.
Buller's operations, too, had cost at Colenso r roo men, at Spion Kop r 700, at Vaalkrantz 400, and now in the last long-drawn effort 16 oo more - over s000 in all.
Rocks the working-places may sometimes exceed z oo or even 200 ft.
When b = o, U 1 =00; and when b = oo, U 1 = -U, so that at infinity the liquid is streaming in the direction xO with velocity U.
An ellipse interior to n = a will move in a direction opposite to the exterior current; and when n = o, U = oo, but V = (m/c) sh a sin 13.
With #=o, the stream is parallel to xo, and 4)=m ch (n-a)cos = - Uc ch (n-a) sh n cos /sh (n-a) (22) over the cylinder n, and as in (12) § 29, =-Ux =-Uc ch n cos t, (23) for liquid filling the cylinder; and _ th n (14) 01 th (7 7 - a) ' over the surface of n; so that parallel to Ox, the effective inertia of the cylinder n, displacing M' liquid, is increased by M'thn/th(n-a), reducing when a= oo to /If' th n = M' (b/a).
D t dy dz where _ oo abcdA A, B ' C ' - (a 2 +A, b 2 ±x, A, c 2 +A) P P 2 = 4(a 2 -F-A) (b 2 ±A) (c2+A).
U - b), u =ae ?, (5) where u =a, a' at the edge A, A l.; u at a corner B; u=o across xx' where 4 = oo; and u = oo, 43-= co across the end J J' of the jet, bounded by the curved lines APJ, A'P'J', over which the skin velocity is Q.
For the 2 polygon has a right angle at a=a, a', and a zero angle at u = b, where 0 changes from o to 27/n and 1 - 2 increases by 21-rr/n; so that dSt A (b -a.b -a') a - (u -b),/ (u - a.u - a where A= tn (II) And the w polygon has a zero angle at u =o, oo, where 4, changes from o to m and back again, so that w changes by im, and du =B, where B=-.
2n u (a -b.b -a')' not requiring the integration of (II) and (12) If 0=a across the end J J' of the jet, where u = oo, q= Q, b-a' a-b ch 7/2,=cos na = I, , sh 162 = i sin na = i,, a - a a-a Then a-a'+(a+a) cos 2na-[a+a'+(a-a) cos 2najcos 2110 (a-a') sin' 2na X cos 211a - cos 2110 Along the wall AB, cos nO =o, sin n0= I, a> u> b, ch n2= i sh log (q) n= i?
Helmholtz, of the efflux of a jet between two edges A and A 1 in an infinite wall, is obtained by the symmetrical duplication of the above, with n = 1, b = o, a' = - oo, as in fig.
5, I ch S2 = u a, sh C2= ' u (I) (I and along the jet APJ, oo > u=aerslc>a, sh S2=i sin 0 =iu=ie zrs/o, (2) PM sin 0 ds = f e ds = 1 = 1 sin 0, (3) cos 272a - cos 2n0 = 2Q - ?ib L a b2 s i n' 27ta u-b A (a- (u -a.u -b') sin 2110 - 2 a-a .u-b ?l (u -a.u -a') = s in 2na u-b 2n b) A (ab.ba') p l u -bJ (u -a.u -a') sh nS2=i sin 110=i then the radius sin 2170 (30) A', cos nO= i, sin n0=o, n 1 ' b-a' ch nS2= ch log (9) = Va -a' n shnS2= shlog (Q) q _ o> u>a'.