Avicenne by Le Bon Carra De Vaux

By Le Bon Carra De Vaux

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WhiHi u*iA invu Tin* nsy# 11 \va In* if' 1! In \*;i n^r through a porcelain tubr maintain*'*! it I MJO (* In «»nhr tn effect th« rapid cooling of tint j»an a wall r r*>f*It<4 * ilv« r tul»»* passed along the axinof tli«: porn-kin tu\n\ fr;unph > t«t *»\) J;I n were drawn from th<* annular Kpan* bc»t\vn*n t }#t }K*rr« lain and the Bilver tub«m by aHpiration through n MJMIJ HIIII* tnb« which paRScd into thr nilvnr tubt* itM*lf. ikt*n oxidoR of nitrogen or hyi]rogi;n piroxirli* U*r U/MIW. 0 (\ at various specdn up to BO rmn, p w wcfintl, hf SKIM#W«*«1 thai tho rate of decomposition of ogonc w a i cxtri«tiittly rapid, I per c e n t O, linking to OtWi per mnt in UUQ1 M&OIK)*.

1 a6, J»f 1902) showed that cmmtj coiiltl \m formed during the rt-duetinn of certain oxidinmg actidn, Mich it1* rhroinir actd, attributed to the intermediary farmattmi t*( im tui^ijilil^ pvtaxnh* with iU Relatively lftrK«*tjimt4iiti«*Hrif«/,Miii*, h«iw#'%«'r. an* in thti autoxtfiation of |iliun|ihuru«t, ntnl sn vww of ih«» cunvdnieaoen «f thin mnthnr! **f (ir«*|mr4tiun lh«* foltowtnc df tatli may bf given: A rupiil rurr«*tit tif air i» p»«t#»f«! fi^#nim ptrmanganate or btchrnmaif!. awly at 6** (3*, whiint the uptimtitti Urmpvrmtutt* H «tftU*

Of NO in Air. 1811 0'35 2033 0*67 2580 2-02 2675 2-35 3200 5-0 Jellinek Qoc. ) likewise calculated the rate of decomposition of nitric oxide to its equilibrium value at various temperatures. Nitric oxide in this respect is markedly different from ozone since it is relatively much more stable at high temperatures; the times for the decomposition of half a given volume of NO to nitrogen and oxygen at atmospheric pressure are as follows:— Temperature. °C. 900 1100 1300 Time in Minutes to Effect 50 Per Cent.

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