IV. The Leaf and Twig Oils of Digger Pine, Lodgepole Pine, and Red Fir

AND RED FIR. By A. W. Schorger. Received November. 2, 1914. It is well known at the present time that the oleo- resins of the digger pine (Pinus sabin...
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T H E J O U R N A L OF I N D U S T R I A L A N D . E N G I N E E R I N G C H E M I S T R Y

cooled t h e pitch under slight pressure, t o avoid t h e formation of voids. T h e slow cooling always caused a marked increase i n apparent specific gravity with t h e harder pitches, while with soft pitches t h e difference is negligible. T h e writer hopes t h a t this paper on t h e homely subject of specific gravity will be useful i n some measure t o workers in general, a n d can s t a t e t h a t , i n his experience, t h e methods recommended here are rapid, convenient, a n d sufficiently accurate, RESEARCH DEPARTMEKT, BARRETT MANUFACTURING Co. 17 BATTERY PLACE. NET%' YORK CITY

OILS OF THE CONIFERAE: IV. THE LEAF AND TWIG OILS OF DIGGER PINE, LODGEPOLE PINE, AND RED FIR By A. W. SCHORCER Received November 2, 1914

It is well known a t t h e present time t h a t t h e oleoresins of t h e digger pine ( P i n u s s a b i n i a n a ) a n d Jeffrey pine ( P i n u s jejveyi) yield oils consisting almost entirely of n-heptane. Examination of t h e leaf a n d twig oil of t h e digger pine has revealed t h e very interesting fact t h a t heptane was present in t h e sample t o t h e extent of only about 3 per cent, t h e remainder of t h e oil consisting of aromatic bodies which are principally terpenes. It m a y be assumed with safety t h a t this small percentage of heptane was derived from t h e small twigs during distillation, since t h e latter were n o t separated from t h e leaves. T h e phytochemical processes taking place in t h e leaves a n d in t h e woody portions of t h e tree are, accordingly, entirely different, since t h e oil from t h e former consists of aromatic compounds a n d t h e oil from t h e latter of aliphatic derivatives. Anisic acid was obtained b y oxidation of certain fractions of t h e oils from digger and lodgepole pines. Lack of material prevented obtaining conclusive evidence a s t o t h e parent substance from which t h e anisic acid was derived, a n d for t h e same reason t h e presence of borneol a n d certain terpenes can n o t be shown with absolute certainty. T h e d a t a obtained, however, should be of i m p o r t a n t assistance t o t h e chemist who is fortunate enough t o obtain material for further investigation. LEAF A N D T W I G OIL OF DIGGER PINE

(Pinus s a b i n i a n a , DOUGL.) T h e physical a n d chemical constants of t h e oils are given in Table I. T h e sample of 238 grams gave t h e following fractions: I O O ~ - I ~ 6~ . 0~ ,per cent; 152'-160', 10.0 per c e n t ; 1 6 0 ~ - 1 7 0 ~5, 2 . 0 per cent; 1 7 0 ~ - 1 8 8 ~ 1, 5 . 0 per c e n t ; 1 8 8 " - 2 3 5 ~ , 8.5 per c e n t ; 235'-2goo, 2.3 per c e n t ; residue, 6 . 0 per cent. HEPTANE-The lower boiling portions of t h e oil were fractionally distilled a n d repeatedly t r e a t e d with concentrated sulfuric acid. B y this t r e a t m e n t 7.2 grams ( 3 . 0 per cent) of oil were finally obtained, having t h e specific gravity 0.7013 at I 5 ' a n d boiling between 9 8 . 5 a n d 101'. P u r e n-heptane boils at 98.4' a n d has a specific gravity a t I ~ of O 0.6880.

V O ~ 7. , NO. I

ff-PINENE-The fraction boiling a t 156-157 ' h a d 0 . 8 6 1 8 a n d ( ~ ~ 2 -26.24'. 0 0 A good yield of pinene nitrosochloride was obtained. T h e nitrosochloride was thoroughly washed with methyl alcohol a n d dissolved i n a small a m o u n t of hot chloroform. T h e crop d150

PHYSICAL AND CHEMICAL CONSTANTS OF THE LEAFAND TWIGOILS Ester No. Optical after Per cent Sp. p. Ref. :nd. rotation Acid Ester acetylayield Sample 15 15 aD200 No. No. tion of oil DIGGERPINE: 2493 0.8566 1.4670 -20.93' 2.05 11.98 37.16 0,102 2494 0.8543 1.4708 -38.36' 1.91 9.48 29.84 0.085 2496 0.8517 1.4671 -30.75' 1.47 6.77 25.86 0.078 LODGEPOLE PINE: 2495 0.8690 1.4831 -17.84' 0.90 32.30 0.234 6.02 RED FIR: 2529 0.8665 1.4861 -16.70' 0.75 0,154 9.93 36.22 TABLEI-THE

of crystals obtained on cooling, after washing with alcohol, melted a t 104-10j '. From t h e chloroform mother liquor a further a m o u n t of crystals was obtained on addition of methyl alcohol. These crystals after washing with methyl alcohol melted a t I D j '. T h e nitrolpiperidine derivative melted a t I I 7 '. T h e t o t a l a-pinene fractions amounted t o 58 t o 59 per cent. T h e relatively small a m o u n t of oil boiling between 160-1 7 0 ' was examined for @-pinene with negative results. LIMoNErz-The t o t a l limonene fractions amounted t o about 24 per cent. T h e fraction boiling a t 1701 7 5 ' a n d having 0LD21° -40.79' gave negative results for phellandrene. Sylvestrene was apparently a b s e n t since t h e dihydrochloride obtained melted a t 49-50'. T h e fraction boiling at 1 7 5 - 1 7 7 ' yielded a tetrabromide melting a t 1 0 4 ', t h e melting point of limonene tetrabromide. E S T E R FRACTION-The portion boiling at 206-23 j ' was saponified a n d distilled with steam. T h e recovered oil was t h e n oxidized with a saturated solution of potassium permanganate a n d again distilled with steam. Only a few drops of oil having t h e odor of camphor were obtained. O n acidifying t h e oxidation liquor a n acid was obtained t h a t crystallized from h o t water in t h i n needles a n d sublimed readily, giving crystals melting a t 183-184'. A portion of t h e acid weighing 0.1637 g. required 10.62 cc. of N / I O N a O H for neutralization, giving a neutralization equivalent of 1 5 4 . 2 . T h e properties of t h e acid showed i t

OCH3

t h e latter melting t o be anisic acid, CaH4