SCIENTIFIC ABSTRACT GRUYEVTSEVA, M.F. - GRUZDEV, B.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000617120016-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 10, 2001
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ZUBARIVA, Zinaida Nikolajvevaa;GRUYMSZVA, M.F., red.; TSYPPO, P.V., tekhn.
red.
[Nature stu4y corner in elementary schools; a mwrjal for teachers in
elementary schools] Ugolok zhivoi pr1rody v rachallnoi shkole-. po-
sobte, dlia uchitells, nachalOnol shkoly. Koskwa, 06s. uchobno-pe-
dagog. lzd-vo H-va prosy. RSM 1957. 125 P. (MIRA 11:7)
(1kture study)

RIKA HKVA, A.F.; GRUZ, B.Ts.; RODINOV, V.M., akademik.
Investigation of the mechanism of reduction of djasonjum salts. Dokl.AN SME
92 no.2:337-30 S '53. (NLVA 6:9)
1. Akademiya nank SSSR (for Rodinov). 2. Institut fizicheskoy khinii in. L.T.
Pisarshevskogo Akademit. nauk Ukr&inskay SBR (for Rekasheva and Orus).
(Diazonium compounds) (Mjdr&zins)
i:~

:: : i 11 -
. r- 7-117F7 -IT---; I I H I " ~' I IF V 1--i ~ i. I! I i~!;
L ; ~

- i , -1.
YAGUPOL'SKIY. L.M.; GRUZ, B.Ye.
Synthesis of nitropheny1hydrazines containing a trifluormethyl
group. Mcr. khim. zhur. 23 no.5:634-636 '57. (MLRL 10:11)
1. Institut organicheakoy khimli AN USSR.
(Hydrarine) (Nethyl group)

7 12 83
AUTHORS: Yagupollskiy, L. M- Gru7 D. Ye, Kiprlanov A. 1,
TITLE: The 31nthenij of ,,.-ilitroplienylhalo~7enrietilyl~.(,,irbinol-.(Sirltez P-
PERIODICAL: Zhurnal obshchey 1-himaii, 1958 Vol. 23, lir 6, Dp. 1"joa-16lo
(USSR)
ABSTRACT: p-.nitronhenylhalogenmetkvlcarb-'~nols are intermediate proiucts
in the synthesis of the syntheti(i antibiotics of synthomycir,
(sintomit3in), The synthesis of p-nitropheriy1chloromethyl.-
carbinol (I ") was first :;arried out from styrene by V, A,,
Yikhalev and co-workers. The chlorohydxin of sTyrene was
acetylated, the acetyl derivative vrao nitrated,, the p-isomer
was separa"ed from the obtained mixture cf nitro products
and was saponified tc the comp:)und (I). It wans of interest
OH to the authors to carry out directly
I the n1--crifization of chlorohydrin styrene.
C11-cif c1 T~ey found that on the additi,)n of this
2 compound to the nitrification mixture
6 1) at a temDerature not above 0 C, nitrogen
Card 1/3 ITO2 ether of the m and p-nitro-~henjlchloro--

The S.,nthp-sbr;f p-l~';-Iroplierqlllial.)f,-enmetiiylcarb--.nol-; .1 ~. 11 / '7'~ ...) ~1 - '. -
0 1 , - , C, 31:/6,4/
iMethy1carbinois form (Ref 2) , The nitrogen ether of the
p-ni.tru derivativ-~ iva3 separated from the mixture by crygtal-
lization. In order to check the structuze this product was
oxidized with permanganate to p-nitrobenzoic acid and was
identified with the above mentioned product (I) by Nlikhalev;
the structure of the m-isomer was determined in an analogous
way. For the syntheois of p-nitrophenylchlcromethylcarbinoI
it was necessary to saponify the nitrogen ether. which, ac-
cording to existing data in publications., was expected to
be very difficult. A perfect saponification ("o yield)
to carbinol was achieved by the authors only by heating
the above mentioned ether with a great excess of concentrat-
ed hydrochloric acid. They further fol.~nd that it is useful
to take a mixture of hydrochloric and phosphoric acid, in
which case a complete saponifi-ation is achieved with a
much smaller amount of acid, As a peculiar fact, the saponi-
fication does not take place with phosphoric acid alone.
Besides the mentioned methods of saponification also others
were found: The heating of nitrogen ether with 6o - 65 % of
sulfuric acid in the presense of urea yields the carbinol
Card 2/3 in a yield of 95 %. Concluding it can be said that the meth-

The SyntheBis of p-Nitrophenylhalogenmethylearbinols 30V/7 9-2 8 -6 - 3 8/6 3
od of the synthesis of p-nitrophenvlchloromethvlcarbinoI
and p-nitrophenylbromomethylcarbinol by nitrification of
the corresponding halogenhydrin styrene, with subsequent
saponification of the formed nitrogen ether was carried out.
There are 7 references, 2 of which are Soviet.
ASSOCIATION; Institut organicheskoy khimii Akademii nauk Ukrainskoy SSR
(Institute of Organic Chemistry,AS Ukr M)
SUBMITTED: May 31, 1957
1. Methanol-Syn'thesis
Card 3/3

YAGTJPOL'SKIY, L.M.; VlSIINEVSKAYA, G.O.; YAVORSKIY, D.F.; GRUZ_,_B.Ye.__-_
WOESIMMO, A.S.; KHASKIN, I.G.; GONbETSKkYA, Ya.V.; KIFAIANW,
A.I.
Improvement in the method for producing p-nitrophenylehloro-
mothylearbinole. Med.prom. 13 no.3:20-21 Kr '59.
(MIRA 12:5)
1. Institut organicheskoy khimii AN USSR I Klyevskly khimiko-
farTiat-96*ticheakiy zavod imeni M.V.Lomonosova.
(MICTUNOL)

IP- :z~~ 1!:I: . ! 11 !],1 -. i
YAGUPOLISKIY, L.M.; GRUZ,-B.Y--e_.., AXIKO, N.I.; KIPRIANOV, A.I.
---M
S~Tnthesis of bilitrast--$-(4-hydroXY-3,5-diiodouhenyl)-v,-phonyl-
propionic acid. Ukr. khim. zhur.926 no.2:233-23~ 160.
(MIRA 1-3:9)
1. Institut organicheskoy khimii AN USSR.
(Phloretic acid)

YAG13POLISKIY, L.M.; GRUZ B. Ye.
-,.
Synthesis of some derivatives of phenyl trifluorometbyl sul-
fide and phenyl trifluoromethyl sulfone. Zbor. ob. khim. 31
no,4:1315-1320 Ap 160. (MIRA .14:4)
1. Institut organicheskoy khImii, Akademli nauk Ukrainskoy
SSR.
(Sulfide) (Sulfone)

YAGUPOLISKIY9 L.M.,-_gUZ,-BIa,-,
Cyanine dyes containing fluorine. Fort 108 Gyanine dyes
containing fluorine in the polyowthine ebain, Zhur,db*khlz,
31 no.12:3955-3961 D t6l. (KIRA 15s2)
1. Institut organicheskoy khJmJi AN Ukrainskoy SSR.
(Cyanines)
Dyes and dyeing)
Fluorine)
~

o b 34 nc.)
r Ln c - sk,

I ;K.1 y ,
t-:-( ~~. ~ ,Tl~ '!~~ , ; YA (,X'~)! . 1 1- M ~
NO. T~' 1 fluo rot-Ohyl) ben7Whl a zoley (I N~ I [-.
I)nrizokhlazole and *Ib",,r "'Ihilr~
khjm~ 35 rio.9-.1639-1644 '~ 10' 5 ~ fp7U
I ~ --)i ti uzt. rrF-in,, rhc-skay kh~rp.' 1, A N .

YAGUIPOL I Y L.M'~ ; 7IW'1'7~,PYAj V I. i GF.O."Z, , B,Y~? . ; V;iNU' U TFIM), N.V .
Cyanina dyes Containing fluorine , Part 127 (yanine dyes from
5-Triflucromethylmercapto-2-yneth;lbenzlir,4-dazole derivative5.
Zhur. ob. khim. 35 no.9sl64.4-1650 5 165, (mlw 18; 10)
1. lns-.-il~ut organicheskoy k~.'n2,4 AN UkrSSR.

GRTjZ, D. M. I SCI (O.Irw) -- "Inves-,: "on F i~p,~)clai nc,'nts
off tile fi:.,st 61-OUP for aifferential equationo wil.h anal--Y-tio F.m"- nop-a-mlyt'~c
vig;iL portionfi". Swma--kand, IC pp (F.[n Hic~lo-r EE~.,uc, T Dqmiil Asia
, -C 6 ic~f-~q, 1:-~L)
statc u ini V. j. L-min), 11~-o copiea (IM 1, Sy -

KUKLISO Its*; GIM, D*Me
Number of operations connected with the use of Frommer method.
Izv. AN Uz. SSR. Ser. fiz.-mt,' nauk no,1:29-45 158. (MIRA 11:6)
(Geometry, Algebraic)
(Differential equationa)
Mma '1~

GRIM, D.M.
Nnmber of operations for distinCiiinhinp the aingular point
of the generalized Briot and Boiiqnet equatlon. Trudy UzGU
no. ?8:3-31 158. (MMA 13:6)
(Differential equations)

KUMS, T.S., GRITZ, D.M.
One analogy of the Kukuhara equation. Trudy UzGEJ no.?8:43-
52 158. (MIRA 13:6)
(Differential equations)

ARC-tr-2079
Ali ELSOMIDS MICR06COPIQ UUUX OF THE PROCUB
OF CATHODIC BRUTrERM". V. Spi"k, f. ff.
Prilexhaeva [Prilez!Uuval, and E. A. Grux. w"-stat"d
from Want, And. Houk pk 400-11
(1951). op.
Us submIcrascopic structure of Al ovinnWted to
cathodic "uttering at reduced pressupos of %jr and lie
has been OWN& Electron miarop-aptis bov'w"" it
possible to vlavaltxo the meet-at m Ak *
I*". Itlectroa emlealan takes place from the r*siaae df
cleavage bet"co IM crystals. Near the ri*10 of
electron embaloo poatt" tons am formed skich
bombard the cloavage planes. West heattita leads to
$11"VILLWIS Of the metal atom#. GrAdUKUY, CM41111f4d
figurv& am formed from wblob the priw1pal brAlvelon of
the atams takes place. Us also of the coria-AApod
figurns, depends. upon the dimensions of this vitystitla. ft
Uo presence air 0 the smission of sloctr*W to rot can-
contrated in Ow reglove. of cleavolov kJA re ca-M.
shaped f1pres are not; fatired. (M.P.Cl.) IV)

K. V. a-lid Gruz, E. A.
TITTILE: D~~termination Phobo,~ra,phic
E'IaulsLons in a Bobatron. (Opredeleniye chavotvitellaosti
yadornyl,:ft t)otatrone)
PERIODI~;AL; Pribory i bek~ni.',,m o kspc rimenta, 1958, lir 5, 23-50
(USSPI)
~'L"PAGT Vari'D(I" of of iiighly scnsitive tl'ijxi~
elimlls.il itis urc coa!3i.dared. TIto
cari-i-ed oat in to determine the s.~_,nsit_ivi~U-y of t~w
-ties. It- is saC-,,-e:-,
plat-s by nea.SLII'J.n- -'rain uenFi t,,d 'h,
6a-2 best, soLwce of radiation for t'.Lis is a L) e -G a tr o a
- i, b c not less
V, an extracted beErii the electron eneril
than 10 _MeV. The electron beam used for IWAs oar--,jase is
t!~e e_-,_~Uracted be-w-_,i ol' biie betatrun of the To.-,is!: Polybech-
-ica- L-,s`itute (15 -UeV). Fi.-,~s.l and a comparJSon
betvv,~-an 15-I'le tl~a.31,1-s to Y-rays (Fi,-:,.l) and electrDias
1/2

0i,
fv-)-i Wit., A;~; can sce-Ill the
`0.~-r
a r,-! s i ii;rr nv~,
i i Ur t r a Til a"" 1
Re-searc,"L I:--stitatc of Cinemato~ra-,Aij and Photograph
Y)
3UB1.11TTED:
ud Ll~?

fni.

BOUGUMOLOV, GRU-", ':~' ,
, -- -
, . I (- 41 q -9 1 t I v ~, r; '
r
"'e of bac icing irradia t ton on the lich t on, ~ ".
photograph-ic materials. Zhur.riauch.l prikl.fot. i k-in. 1C
no.3,.-18(-!--193 Ny--Je 165- (YJ RA 18 -, 23~ )
1. Vzze 3oyuz-,iv.-.,- riauc~mo-issledova te 1 1 skly kinof o tcIrs t - tlu ' .

UM/Chemistry - Manhole, Phenolic my 48
Chemistry - Paraform
"The Derivation of Phenolalcohol From Phenol and
Paraform,- A. A. Vansheydt, F. I. Gruz, Chear of
Plastics, Leningrad Tech last Imeal LenBDVet, 10 Pp
"Mar Priklad Mmil" Vol III, No 5
When phenol is heated vith paraform. at 50 - 700 in
presence of 0.5 - 1% caustic soda, paraform dissolves
and phenol Is fIxed by formaldehyde, vith formation
of viscous products, distinguished by unlimited
solubility In vater. Shove that these products are
simple phenolaloohols. They can be set by heat or by
strong acid.

; .. I '. I I. M:jii iP-., ,-. :: Ioz~ I- I .
VANSHEYDr, A.A.; GRUZ, R.I.
Influence of free radicals of the triphanylmethyl type on styrene
polymerization. Khim. i Fix. Khim. Vysokomolakul. Soedineniy,
DokladY 7-oy Konf. Vysokomolekul. Soedineniyan 152, 80-2. (MIRA 5:7)
(CA 47 no.15!7819 153)
1. Lensovet Technol. Inst., Leningrad.

26868
S/080/6 1/034/004/00- 9/0 12
1 Tu go 3 A057/A129
A M ORS: Vansheydt, A. A., Gruz, R. I.
TITLE: On polymerization of the oyolic trimer of N-methyleneacrylamide
in solutions and crystalline state and on plastics on this base
'PERIODICAL: Zhurnal prikladnoy khimii, V. 34, no. 4, 1961, 895 - 902
TEXT: It was determined in the present work that the cyclic trimer of
N-metk4rleneacrylamide (bezahydro-1,3,5-trialkylyl-sy=.-triazine) polymerizes
in presence and in absence of an initiator (benzoyl peroxide) in solutions or
in crystalline state forming infusible three-dimensional polymers. Properties
of the latter were investigated and the possibility of manufacturing thermostable
(up to 2500C) plastics by heating (160 - 1700C) the crystalline monomer under
pressure was demonstrated. Literature data on polymerization of trimetbvlene-
triacrylamide are not sufficient. Even the melting point was not yet determined
accurately in works published by M. Gradsten and M. Pollock (Ref. P., J. Am. Chem.
soc. 70. 3079, 1948), R. Wegler and A.Ballauf (Ref. 3: ChenL Ber., 81, 530,1948)
or K. Thinius et al. (Ref. 41 Flaste and Kautschuk, 6, 7, 322, 1959). On the
other hand polymerization of this trivinyl monomer is of Interest, since little
Card 1/7

4,
26868
S/080/61/034/004/C)09/012
On polymeriZation-of the ..... A057/A129
is known on polymerization of trivinyl compounds and no investigations were made
on a transfer into three-dimensional polymers in the solid phase. Using the methcd
described by T. Gresham and T. Steadman (Ref. 1i J.Am. Chem. Soo-, 71s 1872p 1949)
in the present work preparation of trimethylenetriacrylamide was carried out and
the melting point was determined as 156-70C. The amide is difficultly soluble in
other dioxane, carbon tetrachloride and other hydrooarbons,better soluble in water
and pyridine, considerably more soluble in alcohols (methanol, ethanol), diohloro-
ethane, and fajxiy soluble in chloroform. A bromine number of 190.8 (instead of
192.5) was found for the hexabromide of the monomer. Polymerization of trimethyl-
enetriacrylamide in solution was 'carried out (under assistance of Ye. Ye. Belomyt-
tseva) in boiling alcoholic solutions (Figure 1), and 2.5% (Figure 2) and 5 %
(Figure 3) alcoholic solutions at 77-30C. It can be seen from the results that
the polymerization rate in boiling-solutions increases initially with the conoon-
tration of the monomer.' After 3 hours 30 - 35 % conversion is attained and the
polymerization rate remains constant. A 0.1 % benzoyl peroxide admixture causes
a second start in polymerization increasing thus the yield considerably. The poly-
merization in absence of initiator admixtures can be explained by the effect of
absorbed oxygen (during preparation and storage of the monomer) resulting in for-
Card 2/ 7

26868
S/080/61/034/OC4/009/oi~-
On polymerization of the A057/A.129
mation of peroxide groups. Thua storage and preparation conditions effect the
polymerization of the monomer. Also the effect of atmospheric oxygen on poly-
merization was determined (curve 1116, Figure 1). Polymerization experiments
at 77-30C indicate the increase in polymerization rate with theamount, of added
benzoyl peroxide (Figures 2 - 4), Experiments (carried out in assistance of Ye.
N..Shchepkina) with arystalline trimethylenetriacrylamide at 98, 134, A3, and
1540C in dry C02 atmosphere demonstrate (Figure 5) an increase in the polymeri-
zation rate withtemperature., Thus near the melting point of the pure monomer
(1540C) a sudden 'polymerization with increasing temperature (exothermia reaction)
is observed. Acceleration of polymerization with 1 % benzoyl peroxide admixture
azrid inhibItion by hydroquinone or pyrogallol indicate a free-radioal mechanism
of the polymerization in absence of admixtures, which can also be explained by
the presence of peroxides in the monomer. Corresponding experiments proved that
monomers with Identical malting points may have a different tendenoy for poly-
m9rization depending on the duration of storage. In determinations of the acti-
vj.ty degree of polymerization this must be allowed for. The obtained non-fut3ible
typical three-dimensional polymer 16 a polyacrylantide with cross-linked metbylene
groups at nitrogen atoms. This was proved by hydrolysis of the white powdered
product obtaining formaldehyde, ammonia and polyacrylic acid. In analogy to re-
Card 3/7

S1,08016!16-4,
jUlymerizatior of the A057/AIP'~
it ia not fuvible and notthermoplastic. The obtained polymer wu~ prrcqezed
6o - 1700C, 00 - 300 atm, and transparent plates with soften:'rijr. p~'.IT. tjbove
were obtained. Mechanical toughness was increased by mixing t,
--lered polymer with saw dust (I : 1) and by subsequent compress i, r av.
.-x for 10 - 15 mlnutes at 160 - I-OOC. Thus a phanolformaldehyde-lik~ resin was
rxined, stabl.--, agninst orgwtia solvent.; anti r:itrong alkali solutloo;*j vit nct
-,able against strong mineral. acids, with the following aharactarisi-Aciz, static
ending strength - 630 kg/om2, speciflo rtiulllenoo (Dinstant) .0 Yg-evom_2,
gmostability (Vick) 20OUC, tangent of the loss angle for % ptjolrAlk
.0c) 0.06, water-absorption in 24 hours - 0.6 - 0.7 %. ThAre aria 4 i.lxtives
4 non-Soviet-bloc references.
A3-IOCIATION: Katedra tekhnologii plastmass Tekhnologichoskogo instituth Imeni
Lensoveta (DeparLment of Technology of Plastics of the TLechnologL-
cal Institute imeni Lensovet).
,_-.-BKTTFD- July 9, 1960
~:;ard 4/7

111 ~ I ,fI ,; !,!i!
CRUZ, R.I.; VANSMYDT, A.A.; KRYUCHKOV, F.A.; POZIN, L.M.; KANEVSKAYA, N.V.
Interaction of alcohols and amines with NNI-methylenediacrylamide and
with cyclic NNIN"-trimethylenetriacrylamide. Zhur.prikl.khim. 36
no.6:1307-131/. Je 163. (MIR& 16:8)
(Alcohols) (Amines) (Acrylamide)

L 13526-66 EWT(m)/IWP(J)/T RPL WW/RM
_iR_/C6i_o7*_
ACC NRs AP6002216 (A) SOURCE CODE: 65/038/012/2749/2757
AUTHOR: Gruz, R. I.; Vansheydt, A. A.; Strakhova,
ORG: none tp
TITLE: Copolymerization 6f
cyclic trimer of
a
N-met
pionamide with an unsaturated polyester resin I
SOURCE: 1hurnal prikladnoy khimii, v. 38, no..12,
1965, 2749-2757
TOPIC TAGS: copolymerization, polymerization kinetics, high polymer,
copolymer, polyester plastic, resin, thermal stability
ABSTRACT: Copolymerization of the cyclic trimer of N-methyleneallylo-
xypropionamide (NN'N'l-trimethylene-tri-O-allyloxypropionamide) with an
unsaturated polyester resin was studied at GSO-1500C, various molar ra-
tios, and in the presence of benzoyl peroxide, dimethylamine, and
methylethylketone. It was found that the copolymer resins are stable
thermally up to 215-2209C. This is about 500C higher than for the cor-
responding copolymers based on styrene. The kinetics of copolymeriza-
tion of amidoester with polyester resin at 1000C is shown in fig. I.
UDC: 678.13
E.
K.
leneallyloxypro-
1/2

L 13526-66
ACC NRi AP6002216
A
fig
B
If
v
- --------- ------
Fig. 1. A--content of solution (t); B--content of nitrogen fixed the
gel-fraction (t); V--time (hours).
Orig. art. bas: 7 figures, 4 tables.
SUB CODE: 07/ SUBM DATE: 27Dec63/ ORIG REF: 004/ OTH REF: 009
2/2
cmd
p:'q ji::;;::

11 41 11 16 1; 0 It X J1 41 13 A a 14 A M W .1 11 it 31 *0 M*641 Gil Odf.10
A I I W y U i.
Cri-

The effect of n0afflactrillyt.4 on the Wo"'Otia P~Qliiafiajft
Of arnailtIams and on the adsorption of arnalgamatitil m*Wa
T. Pflic (ittir Anti J.". Vap (Tudmilinitexiirtend Filikat-
Kimiji 46% MvJv4,,xW InlizvI. Hudap-t' Ming.). HU'01.
Aas Chim 1. No. ;wtentiah of
'
0 n. anti za
-t ins anit di-oppitit Atualtilus of I". fit), Cd.
:0 a -, 4-n~t,-.tnyi-k-..t-nzv
,
l
icarid
.
it'quii nn Vai
To 111.4ke the .4111. A.C. SIAM. was al'.11VA
SMI 1.1,01 *,ibl. And app. were carefilliv In-%,I to 0. Wiwi'
Ihe, atuAlt-Ant ~wncn. was Above Ill "Ill' it.-Atoill per I
illi
i
i
lile to vil
vv
t-;
the eln-tt,vic 1.)tcutiali are relwndw
Ill" .- by the pi-m- .1 "'lachvit"Ayt-
The liolvolialn oarr airtil. partly by the &&-rption of ion,
and ewulral nuil,i. ot, tile liquid.,hir of the biclitittilAry
IWIlinell owilit old wIts . partly 11Y *41-tirvOwl ill tricla)
joll. Ott tile "Inalplill 0.1e of tile doilhip liivvr The lx).
tential of alualgaill electroil" Vad" Ammiding to F - a -
b. loclain). where a anti b are con%ts.. and ij. ) is coeim,
(I the anulcal". Ct~t. b ranged betwicin 0.014 anti
U.tkM: it we% chictly affe"ed by the vislence of the raftel.
t Court. a libowed I*rVr variati~ accordinat to the nature
019-TV-11 -tMOK-11-
-v j.,
pryly"I'M all no Is a
-*0
so
'0
tio
to 0
Aiietal Witit tiet ohit Of Itit-Ifitiv ~Clllghly V AsorlitA
the cotwn. of the nktal Ill the satWginj 'M ~
rneW kmi forin ibe. 1",tive pairt of lh~ 't-thl, UYT, asio
crrjj~,j within the A ~.,Irnlri 1'1-- ocx~ll.' 11rl
it i evin'll' it "frfrnt~ Zo 0
1~tvan FinAy As 40
W�R
too
too
too
n i ~1*
0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
OA 0 9 0 0 0 0 6 0 0 0 0 0 0 0 00 ** go 00~5

US-jR/Microbiology Microorganisms Pathogenic to Humans and F-5
Animals.
Abs Jour : Ref Zhur - Biol., No 3, 1958, 9958
Author : Gruz, V.:;., Starikova, K.I., Tarkov, M.I.
Inst
Title : Agglutination Reaction with Boiled Dysentery Cultures as
a Method of Identification of Atypical Dysentery Strains.
Orig Pub : Sb. tr. Mold. n.-i. in-t epidemiol. mikrobiol. i Gigieny,
1956, No 2, 67-70
Abstract : The specificity of coctagglutination was tested-with dy-
sentery bacteria of Flexner, Newcastle and Sonne, with in-
testinal bacilli vhich do not produce paragglutination,
with dysentery antisera, and with Bact. alcalescens.
89-5% of dysentery strains produced a specific positive
coctagglutinating reaction in diagnc5tic titers, similar
to the usual agglutination reaction. Coctagglutination
with an intestinal bacillus which has no paragglutinating
Card 1/2
USS R/Microbiology - Microorganisms Pathogenic to Humans and F-5
I Animals.
Abs Jour Ref Zhur - Biol., No 3, 1958, 9958
properties was Positive in 5% of cases in titers of 1:loo,
1:200, 1:64o, and 1:12,800. Coctagglutination with Bact.
alcalescens yielded a clear positive reaction in titers
of 1:100 to 1:8oo. The authors believe that data obtained
by them on agglutination of boiled dysentery cultures show
evidence of a lowering the agglutinating titer as a result
of de3truction of the thermolabile component; coctaggluti-
nating reaction permits no differentiation of atypical dy-
sentery strains from Bact. alcalescens.
Card 2/2
GRUZA, V.V.
Geochemistry of alkalies and acid igneous rocks in the central part
of the Altai-Sayan fold area. Dokl. AN SSSR 162 no-5:1152-1155 Je 165.
(MIRA 180)
1. Vsesoy-uznyy naijehno-issledovatellskiy geologiaheskiy institut. Sub-
mitted January 29, 1965.

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GRUZA, G. V. , ,-
C*
e
Ascending air masses and their cooling. Trudy SAGU no.38:81-84
1*4 (NLRA 10:1)
(Atmosphere)

if!! ! A I 1. 11 1: :1!; I I I - .. i -
GRUZA, G.V.
"'LIJI, . ~-: - - I -
10010 Z.onal characteristics of macroturbulence. Izv. AN Uz.SSR. Ber.
f12,mat. nauk no.2:57-67 '58. (MIRA 11:10)
1. Srednnaziatnkiy gowi4arstvennyy univerattet imeni V.I. Lenin&.
(Atmospheric turbuloncm)

.F, i - 11 1 11 .- ~, : -
GRUTA, G.V-
Zone characteristics of freneral atmospheric circ,,latior.. D-,Lrl. AIT
Uz. SSR no.4:5-10 158. ( VI 11 11: 6 )
I.Institut matematiki I mekhaniki im. V.I. Romanovskogo AN UzSSR.
Predstavlano akademikom AN UzSSR U.A. Arifovym.
(Atmosphere)

I")- 5~` -11 -1 _/1~3
A.UTOHOR- Gruza G.
TI!T E7 Thermal Equilibrium In the Ati-ao.,~phere (0 termicheskom
ravnovesii v atracsfere)
PE.~IQDICAL 1zve_-I-,i:,ia Akademii NauIc S3SR.. S'eriya Geofizicl.,es"caya,
1-)58, Dr '-[ (USSR)
pp
113, ~:-TAC TMe a-k-irivisphere is consid.-,,red to be in thermal equilibrium
when verti.cal turbulent heat, flow is equal to 17ero.
Investizat-ion of 11urbulent heat flov,., in -the abmosohere loads
!.o thc! that tho zondition is sot by equality of
the vertical teinperature Cradient and the dry-adiabatic tem-
perrature ;-;'radient, However. it is assumed in turbulent heat
exctan-e ~D that turbulent eddies transport the average poten-
C3
'-,31 'emp-rat-urle of the level of origin, which is not true in
_ne,-al, Tride-ed. any air taking part in the motion, has at
a cr~rtain vertical velocity. w and temperature,
T diff~--rent from the average temperature at the level
C;
WE~, have eq 3'
,uat -on W~ ?c
(-pra W, (IT
wh e r e -~he density C is -the specific heat at con-
-in T ai-e ~he v--i-tical velocity and

in the At-raosphere-
te.mperatiLre oulsations, Cr and cr, a--e t-heir mean square
w T
JUO L I td r the f:orrelation coeffici.ent between w aid
In equilibriuti q = 0 anal the correlation
~.oefficient r 0 With a normal distribution. the
avera~7e tenL--rature of all particles wit'h vertical velocity
w 1,
does iiot de,)end: in this case, on this velocity and is
eoual to k.hrl avera,ge temperature at the g1ven level, i.e.,
T- Thus in t-lier.-iial equilibrium, the particles
~owr. have e same avera-c-, tem-i,.;,rature at the
vln'~~- a,- Or '-' r)
Lgiven I-evel , TiiuE conclusions based on transfer of
avera,-.-E- potei7itialj- t;e,.-irerature are still true if tem.T)erature
pulsations are considered, Recently M. 1. Budyko and Yudin
(Refs.2 -nnd 3), workin- on the connection between the dir-
ection of motion and the sign of the teTperature gradient
have come -to -the conclusion that ther-,aal equilibrium can
exist when therg is increase of potential temperature with
ne i-h t, Tfiesf~ authors suggest
that the generally used
q k aT- + Y should be replaced by:
p NZ a
-ii-rl 2/4

119 - 58 -/1 - 1
Th~_rmal EauilibT-itra, in the Atmosr,,here.,
q k
p
(3)
i e r e q P. k, T z and ya are the correspond-
ins turbulcnt heat flow'density, specific heat, coefficient
of turbulence. temperature, heigiit and dry adiabatic temper-
aature -n-radient is the equilibrium 0'radient introduced
by i. L Budyllco a-rid M. I., Yudin and Pqual, according to the~m.,
Co 0,60C per 100 m, The dev-Lation of the dry-adiabatic
g:,radient from equilibrium is Siven in "Liie form:
w Tly
i (4)
Ya k I
Here V! is the temperature pulsation of theith element
:it th,~ initial level. sis Its cross-section and S is
-he
orea ol the horizontal region over vi-nich the average is
,c-a-en TI-lz-~-tt yais is due, according -to the

i c) r tion letween blie tem_oeratare
and. the vertical ac.~~elerations at" the initial
e a wl; o r &verticalvelocity = 0.. Since, in estimatin.-
also
P tlni~y _-ced data not only from) equilibri,,,im. bulu
n.),-,-eqL'.ilib_r.31um stat-es, they naturally obtained an average
--a I In non-
no,-~ conne,-;ted with the equilibrium state.
libriLua conditions, y
equi ' P may be an essential factor-
aloo appeai,ed in es t
images by A,, R,, Konstantinov (Ref.7)
b-i L_
doe.-, not have the sense of an equi-librium, -radient
~~nd the t,_-rminology should be changed, It seeTas ex-pedient
il-1-o foraiulat~- ~he conditi-on for t-11ermial eq.,iilibrium either as
z~_n equali-ty cf temperature gradient to the dry--adiabatuic, or
_az the cons-17ancy of the potential te-.-i-iperature with height.
Chere a.-E~ Soviet references,
A,1~0~7DITION- Ak-ade-_,ni,-fa Nauk, Uzb, SSR, Institut aa~emati'K-i i me-',:haniki
(Acadenty c)'L Scienr-s,, Uzb,,SSR., In::'Uitute. of 'MaULie.-iiatics and
Mechanics.
1- 1957..
1. Atmosphere--Thermodynamic properties 2. Mpthemati--s
rd 4/4

Z! .1
13
vats
v
tpj u
.4 3 Z a II
-- a1- - V-, - :M. I !. I - a
A Ing A s
81

- GRUZA, G. V., Cand Phys-Math Sci -- (diss) "Research on the general
circula:H-on of the atmosphere with the aid of zonal characteristics
of macroturbuience.1' Tashkent, 1960. 8 pp; (Main Administration of
Hydrometeorological Service under the Council of Ministers USSR, Cer,
tral Asia Scientific Research Inst of Hydrometeorology)i 150 copies;
price not given; (KL, 30-60, 135)

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rxy of the mean se"neamOtt r-ses "or into the aneray of ir"r4lar moments,
th:t to. or cyclon. an,i ..ti~y~lon. (-tLoo.
The 4bOv* mentioned oxch-go or energy bqtveen the various con.tLtutirg
a0vaosent5are connected with the lrr.xular floct-jatlemi of the general circulation
or the at-mos~hsrv 4*1 1p concrato cases has different illroctions.
us have mentioned only the &vvrage StatistiCal result..
The regularity of the fluctuation or the general circulation, studied by
the fluctuatlon of the above stated sixgnitwUs, vill ;wralt in the future to
wra fully Investigate the structure, of the larg-stale movements of Me
st,,o'More.
G r .4
U:!;"T*.R-. - - ,
As"Ol, of th. JU. wos, of U am
O"'Afel"s, 20111111M, liaL-A, 15 J.4 - 6 Augge, IM. 04"1

3(3),3(7)~24(8) S/166/60/000/01/009/011
AUTHOR: -Gruza,G.V.
TITLEi On the Macroturbuient Rxchang'3' Ower the Northern Hemisphere
PERIODICAL- Izvestiya akademii nauk Uzbekskoy SSR, Seriya fiziko-
matematichesklkli nauk, '4960, Nr 1, PP '173-79 (USSR)
ABSTRACT: The author investigates the influence of the macroturbulence,
i.e. the irregular whirls, to the heat exchange, to the
distribution of energy and transformation of energy, and to
atmospheric motions. The investigations base on climatic charts
as well as on components of the geostrophical wind calculated
from the charts of 700 mb-surfaces for 1953 and 1956. By an
everaging of the data the author excludes amall velocity
pulsations and microturbulence. It Is Btated that in high
latitudes the energy of the macroturbulence amounts 80 % of the
whole kinetic energy, and it diminishes only to the south of the
50-th degree of latitude, The author proves a regulating
influence of the polar region to the field of temperature of the
troposphere. The quickest changes of temperature are in the
latitudes of 60 - 750. In November - December and January-
Card 1/2 February there is the most intensive heat exchange in the

On the Macroturbulent Exchange Over the 3/166/160/000/01/009/011
Northern Hemiaphere
meridional directicn, The dynemi-; result of the macro heat
exchange is the appearance of zones with different contrasts of
temperature. The author gives 3ome 4,irther statements which
together give a uniform image of the statistical heat exchange
in the large.
The author mentions A,.S.Monin, L.R.Rakir)ova, II.Ye.Kochin, and
Kh..P.Pogosyan
There are 4 figures, and 4 Soviet references.
ASSOCIATION:Sredneaziatskiy n.-i. gidrometecrologichaskiy institut (Cpntra
Asiatic Scientific Hydrometeorological Research Instit uteT
SUBMITTED: November 30, 1959
Card 2/2

3/0)+9/60/000/01/023/027
E201/9191
AUTHOR: Gruza , G.V.
TITLEi Some Zonal Pro erties of
Atmosphere
PERIUDICALI Izvestiya Akademii nauk
196o, No 1, pp 161-164
the General~Circulatlon of the
SSSR, Serlya geofizicheskaya,
TEXT: Charts of the absolute topography_pf the 700 millibar,
surface were obtained at the Antarctic SovietIttation "Mir It N-V
during the Third Soviet Joint Antarctic Expedit-1-onorgarrf-Mr-by
Acad.Sci. USSR in 1958. These charts were used to determine some
properties of atmospheric motion in the southern hemisphere which
were then compared with analogous quantities for the northern
hemisphere. The method of calculation of the quantities
characterizing air circulation on global scale was described earlier
(Refs 1, 2). The monthly means of some zonal properties of air
circulation are illustrated in Tables I and 2. Figs 1-L~ represent
the latitude distributions of the zonal components of velocity
(Fig 1), total kinetic energy (Fig 2), kinetic energy of zonal
motion (Fig 3) and kinetic energy of meridional motion (Fig LO.
Card 1/2

S/049/60/000/01/023/027
3201/R191
Some Zonal Properties of the General Circulation of the Atmosphere
The results show that cooling of the atmosphere is greater in the
Antarctic than in the Arctic. In considering the global heat
balance of the atmosphere we must remember that heat is carried
into the Arctic region both by air and sea currents, while in the
Antarctic area heat is obtained from lower latitudes through air
currents only. The presence of comparatively warm seawater under
the ice of the Arctic is one of the factors which make the Arctic
climate less severe than that of the Antarctic. The radiation heat
losses in the Arctic are smaller than in the Antarctic, since the
layer of air above the Antarctic is thinner and its humidity lower.
All these factors produce greater temperature contrasts and higher
intensity of zonal circulation in the southern hemisphere.
There are )+ figures, 2 tables and 2 Soviet references.
ASSOCIATION: Sredneaziatskiy nauchno-issledovatel'skiy
gidrometeorologicheskiy Institut
Card 2/2 (Central Asian Hydrometeorological Scientific
Rdmr-O- institute)
SUBMITTED: April 11+, 1959

S/049/60/000/02/021/022
E131/E459
AUTHOR: V.
Ca~za,
Q,
TITLE-. ,
,
Heat Exchange'lBetween Latitudes in the Northern
Hemisphere
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofiziche5kaya,
196o, Nr 2, PP 341-345 (USSR)
ABSTRACT.- The calculation is based on 36 points at the 700 mb
surface between 30 and 80* northern latitude. The
density of macro-turbulent streams of heat q is
defined as Eq (1), where & is the latitudinal
distance, b% - increase of the geopotential AT700 for
20a lat at.every point ' it - zonal magnitude of the
geopotential in respect to Temperature and topography.
The coefficient of horizontal macro-turbulent heat
exchange KT is defined as Eq (2). The loss or gain of
heat due to divergence of the heat stream Q can be
determined from Eq (3), where R - the Earth's radius,
h - thickness of the layer, S(&+ 5, 1') is the surface
of the zone between latitudes 1& + 5 and '&, q-& and
qV+ 5 are the densities of the macro-turbulent heat
stream. The results of calculations for the two years
Card 1/2

A
s/049/60/000/02/021/022
E131/E459
Heat Exchange Between Latitudes in the Northern Hemisphere
1953 and 1956 are illustrated in Fig 1 to 6 and in
the table, p 3lt3* There are 6 figures, 1 table and
8 r-eferences, 5 of which are Soviet and 3 English.
ASSOCIATION:Sredneaziatskiy nauchno-issledovatellskiy
gidrometeorologicheskiy institut
(Central Asiatic Scientific Research Hydro-meteorological
institute)
SUBMITTED% June 8, 1959
Card 2/2

GRUZA. G. T.
Kinetic energy of atmospheric motions* Izv.All SSSR.Ser.geofiz.
no.6:892-897 Je 160. (MIU 13:6)
,.4.. 1. Sredneaziatakiy nauchno-issladovatellskiy gidrometeorolos-i-
cheekly institut.
(Atmosphere)

GRUZA, G.V.
"Seasonal variations in general atmospheric circulation and
long-range forecasts* by A.L.Kats. Reviewed by G.V.GrU2a. Meteor.
i gidrol. no.11:56-61 * N 161. (MIRA 14:10)
(Weather forecasting) (Kato., A.L.)

~T, NEUSUM, A. I.
Gomparison of the real and the geostrophic wind iccording to the
data of the expeditioh. Trudy GGO n0-107:47-51 161. (MMA 14:10)
(Winds)

410U~"?
s/ i 66162100010'-D 3/00 3/0 ) 10
0
B165 Bio4
GrLIZa, G. V. ,Kaznacheyeva, V. 1).
n t~-,c~ structure of the height field of isobaric surfaces
ICt~)! ~:LL -tkn~ie;Ay,- nauk Uzbeitskoy .55H. Izvestiya. - Zeriya fiziXo-
i~!atwi.nt,ichorj',-.ikh nauk,bno. 3, 1962, 25 - 31
":".T: i f" is the height of a qi-,ren isobaric surface over a point an
t--o ..-rr-,ind -;;ith Feopraphical longitude ~ and latitude-li, a zonal 'StruCtV-;;:
~.:-ction 1) (6) is defined as the mean square height difference.
Z 2 X 2 d~
+ qf,
It follo~rs from. this definition that b is an even function of C,-. 'Th i s
', netion. is determined for 0
U -ZA- 75,55 and 35 northc. n latitu,;e and the isc-
surfaces corresponding to pressures of 700 and 5100 m' for the months
,--jar'r an' ' I., L, .
~u'-,, respectively, using data published by t'he Ts'll in the
.A.nternational ~3cophysical Year 1958. A meridional structure function b,.
-'ard 1/2

5/1 3/010
t,~W Structure Of the ... B1 63/B 1011
io --'-t,~fined and deter:!,incd to correspond. The first two %xr;.bers of a
SLr;Ls devolo.)l nt b ~. 2 1,+ and an ani6otrooy
B + B
2
100) are evaluato,.i and
n i:; 0 t v 0,-, -:fficient dccilaz;es ,-,,ith increasin latitude, and c-;,Il:,16
y c oc
,,nit-! at about 50
0 nort',-.ern latitude. The 8tructure function3 irmke'it
-irst and second s:,,a'ial der-;v,
)oZ.Iibie to tht~ error v.,hen the f
tivez; -of the heif-. liul', are repl!aced by divided dif'erences with a Zivc~n
F t e i d t Standards for "he -1irst, and second spatial. derivative:~ in
and 13-~r~it,lda di--ection are roiven in a table for a stem) width,
-/GC there are I figure and 4 tables.
0 01.', T ~- C,:: .-,~:redneazialls*4* nauc,no - isaledovatelli,'Kij. v-idro;Tet,:oroI,),:r-4-
chus' '.iy institut (Central Asian Scientific Research Insti~ultk:
for Iq
ydrometeorolo
I T' -,,' D Augus t 14, 1961
212

O-Le win,l ve,
~T-udy Sreci I,g i-Jrcmi ins t- Ylt.
T
'63
%ph me th( -1 Lhe a[
-1 tS -id
C Li
or,-ram ror the ovalu, --on of aucrua,, j' i'o-,-a7Ls by
lu
~!e co~ r- e a

ACCESSION NR: AT4012409 6/2648/631000/OLSIO128/0131
AUTHOR; Grua&, G. V. ~
TITLE: Concept of seasons in the free atmosphere
SOURCE: Tashkent. Sredneaziatakiy nauchno-isoledovatelookiy gidrometeorologi-
cheskiy institut. Trudy*, no. 15, 1963, 128-131
TOPIC TAGS: atmosphere, free atmosphere, season, atmospheric zone, atmospheric
temperature, topography, atmospheric circulation, heat exchange, solar radiation,
solstice, meteorology
ABSTRACT- By analyzing the processes in the whole Northern hemisphere and
considering the average zonal temperature changes in a particular atmospheric
layer, the author proposes an objective method to determine the seasons in the
free atmosphere. The time of the occurrence of the main maxim= (minimum) in
the yearly curve of zonal values is taken as the middle of suiner (winter),
while the point when the speed of the growth (decrease) of the zonal values is
the greatest is considered to be'the middle of spring (autumn). This determines
the middle of each season, but not the dividing line between them, which is
difficult to define because there is no sbarp transition from one ~eaeon to
Card L/.3

ACCESSION NR: AT4012409
another. The fact that the temperature drop in the lower atmosphere usually
begins in the polar region and proceeds to more moderate latitudes is expected,
but the fact that warming up after minimum winter temperatures occurs earlier in
high latitudes is unexpected. This is explained by consideration of the circula-
tion and the laws of the interlatitudinal macro-turbulent heat exchange. When
temperatures are maximum in summer, a heat balance in established in high lati-
tudes, the weakening of the meridonal heat flow in sumer compensating for the
small radiation losses. Theme beat losses gradually increase, the meridonal
heat flow and its convergence remain weak, and the temperature begins to fall.
In the north this occurs during the last 10 days of June, sufficiently close to
the solstice. At that time, the inflow of solar radiation is sufficiently great
in lower latitudes, its outflow at the expense of the meridonal heat transfer
is still small,.and warming continues. The inter-latitudinal temperature con-
trast begins to grow. The minimum temperature gradient in moderate latitudes
also occurs during the last 10 days of June. With the growth of temperature
contrasts-2 the zonal transfer and inter-latitudinal excharge increase. The beat
losses at the expense of the divergence of the secro-turbulent beat flow in low
latitudes become greaterI whUh begins the cooling; this cooling at a latitude
of 300 N occurs in August only. In the winter, the situation is reversed. The
Card 2/3

ACCESSION NR: AT4012409
middle of winter and surmner in sub-polar regions is close to the winter and
summer solstices, while at lower latitudes solstices occur later, during the
first 10 days of February and August. Orig. art. has: 1 figure and I table.
ASSOCIATION: Sredneaziatakiy nauchno-isoledovatellskiy gidrometeorologicbeakiy
institut, Tashkent (Central Asian Scientific-Research Hydrometeorological
Institute)
SUBMITTED: 00 DATE AOQ: 20F*b64 ENCL- 00
SUB CODE: ES RD RRF SOW: 006 0TRKR: 000
Card 3/3

ACCESSION NR: AT4012396 S/2648/63/000/015/0003/0012
AUTHOR: Cruz&, G. V.; Kaxnachoyava, V. D.; Stral'nikova, Yu. P,
'TITLE: The structure and ageostrophicity of a wind field over the valleys and
;mouncainous z'egions of Central Asia
iSOURCE: Tashkent. Sredneaziatskiy nauchno-insledovatellskiy Sidrometoorologi.
i
,cheskiy institut. Trudy*, no. 15(30), 1963, 3-12
~TOPIC TAGS: wind, saturation rate, ageostrophicity atmospheric circulation,
.'wind velocity, wind profile
~ABSTRAM The main characteristic of the structural function of winds over
:mountains is its rapid saturation, which occurs first at short distances and
ilater does not depend on distance; A formula is derived to calculate this
;independence of the structural function and the distance. Because of local
.circulations connected with the diversity of the mountain relief, wind velocities,.
,even at abort distances, are also statistically independent. To find out the
-difference between the absolute values, average coefficients were calculated
~charaaterizing the anisotropy. It was proved that the flow of wind over mountains
,is more isotropic than over valleys. The turbulent influence of mountain systems
CWd 1A

ACCZSSION NR: AT4012396
,causes an increase in the intensity of the wind. The comparison between real
and geostrophic winds is important, but the differences between these winds do
not correctly represent the ageostrophicity of atmospheric movements. The
ageostropbic deviation& depend on acceleration while the average acceleration in
the atmosphere equals 0. The coefficient of the connection between the vectors
of a real and a geostrophic wind is shown and the value of the vector connection
is calculated according to a derived formula. The vector connectic;n between the
tvo types of winds is no worse over mountains than over valleys. The real and
geostrophic winds are, on the average, stronger over valleys than over mountains.*
The braking effect of orographic obstacles occurs upward along the flow. "A.
Zhamankulova, IML Ibragimova, S. Magdaltyeva, and T. Samisonova, students of the
Tashkentskiy gosudarstwenny*y universitat In. V. 1. Lanins, (Tashkent State
University) participated in the collection and processing of data for the article."
ASSIOCIATM; aredmensiatakLy usueboo-issledevatellskLy gidrowtoorologichaskiy
institut, Tashkent (Central Asian Scientific Researcb.. Hydrametearological
Institute, Tashkent)
SUBMIrm: 00 - DATZ ACQ: 207sb64 ENCL: 00
SUB COI*: RS ND MW SOV: 013 OT 001
2/2.

I L 3072-66 EVJT(d)/EWT(l )IFOGIT MP(d) G.W,
iAcamm KRz AP016517 URIO050165100010071000310010
551-509.3
AUTHORS: Bykhovski-Y, M. L, (Doctor of technical sciences.# Professor); Qrqg1x-Jj-L'
(Candidate of pbyvico 4~ti;a sciences)
TITLEs Principles of an objective method for weather forecasting based Onlprgrm--~-
motion probability logic
SOURCE: keteorologiya i gidrologiya,, no. 7j, 1965., 3-10
TOPIC TAGS: weather forecasting information analysis, probability
ABSTRACTs It is assumed that the task of forecasting conaists of a selection of
a terminal number of previously formulated predictions corresponding to several
weather phases. When the number of phases is two) we have to do with alternative
predictiorw--the simplest type of phase prediction., The authors describe an
algorithm suitable for establishing a method of weather forecasting. This was
developedfor medical diagnosis and was used successfully at the Institut khirurgiij
Im. Ve Ae Vishnevskogo (Surgical Institute) in Moscow. The method is based on
the information-probability approach to the problem of recognition. Conditional
Card 113

L 3072-66-)
ACCESSION NR: AP50165,17
probability and information measure of predicatable characteristics are first
iconsidered. From these it, follows that the probability of arq weather phase may
be computed for any group of observed characteristics. The probability of the
phase may be arranged in decreasing order, the most probable phase coming first,
;but this does not sipply an absolute solution. A system of thresholds may be
jintroducedp one for each weather phase,, and an absolute solution may then be
.~,Obtained. An example of applicability is described. The procedure most fi-equently!
euccessful.19 the followings 1) after all variables have been made discrete,
!compute the information or communication indexs 2) arrange the variables in order
lof decreasing communication (linkage),, 3) make predictions speording to one
,variable most closely linked to the phase function, 4) make predi~tionis according
:to pairs of variables and select the best pair., and 5) test the best pair of,
ivariables in combination with the remaini pairs and find the best triplet. This
process is continued until no appreciable improwment is obtained in results. Orig#:,
:art. has: 1 table and 17 formulas.
ASSOCIATION: Sredneaziatakiy nauchno-insladovatellskiy gidrometeorologicheakiy
institut (Central Asian Scientific Research HydrometeorolorAcal Institute)
Card . 2/3

L 3072--66
ACCLSSION RRI AP5016517
SUMMED: 26Har65.
NO Ra SOV: 006
Card -.313
DEL 1 00
OTMs 001
SUB GWEs

9~,TjIZA, Georg-jy 11, ad i r, "7) FT;
SUBKOMB, G.T., roe.
[Integral characterist-*,CS "el"a ral c i n.-A p t'A f
tsii atmorrery. Leninfrr~d. CHromcLoJLz(lal

- P ~ '' . I
C. It I I 17 A. ) CI.V.
ZonrL!. strn.,,cturc of general at.,nospher1c, c-Ircuirti-lon a'.d
r 0 1 Kv.
acroturbulont oxchrulf:P, arc I'dInt- to 1(.,Y d.,tt, , P-
m
111, -,., P, 1 9: 1 )
k . 1 .1

~~C NR x-6001044
Gruza., Gcor~iy Vadimovich
Integral characteristics of general atmoopheric circulation (Intear~llnyye
kharalcteristiki obshchey tsiriculystsij atmosfex-
y) Leningrad, Gidrometcori-
Zdat, 65. .0123 p. illus., biblio., charts. (At head of title: Glavnoya
xiLzravleniye gidro-,aeteorologicheskoy slu7hby pri Sovete Xinintrov SSSR. Bredne-
aziet,skiy nauchno-issledovatellskiy gidrometeorologicheakiy inatitut)
1,030 copies printed.
TOPIC TAZS: mteorology, climatology, atmospheric circulation, atmospheric
turbulance, geostrophic iiind, atmospheric pressure, atmospheric physics
PURPOSE AND COVERANE: In this book results are given of studies on general
atmospheric circulation with the aid of characteristics of macroturbulance. Basic
new material has been obtained from t7he "ta of 1958P the central period of the
International Geophysical Year. Also some general questions on aeroclimatolography,
-f the baric field and other questions. This book Is recozzmended for
meteorologis-c,o, aspirants and atudeuts of advanced courser. on physics of the
atmosphere.
TA= OF COMINZIS (abridged):
Preface --- 3
UDC- 551-513
Card

ACC NRt
introduction
Ch. I. Integral characteristics of atmospheric circulation and their empirical
dateraination --- 11
Ch. II. Statistical strudture of the field of geopotential heights of isabaric
surfaces --- 33
Ch. Ill. Zonal structure of baric field and its seasonal variations ---59
Ch. IV. Zonal structure of the western transfer (latitudinal component geostrophic
,wind) --- 057
Ch. V. Kinetic energy of geostrophic circulation --- 73
Ch. V1. Zonal structure of the field of resulting geostrophic wind average
monthly maLps of baric topography --- 96
Ch. VII. Geographic distribution of sme statistics of geostrophle vind --104
Ch. VIII. Some additional problesm --- 109
Bibliography ---122
Appendix --- 125
SUB COIE: 04/ SUM DASE: 09=6~/ WM FW; 04T/ 01% JW-*- 005

~GkqZA,_,qeorgiy Vadimovich; PETROSYANTS, M.A., red.; VAYTSMi, A.I., red.;
89ROEYEV, A.N., tekhn. red.
(Large-scale turbulence in general atmospberic circulation] Makro-
turbulentnost' v obstichei tsirkuiiatsii atmosfery. Pod red. M.A.
Petrosiants. Leningrad, Gidrometeorologicheskoe izd-vo 1961.
102 p. . 40RA -14: 10)
(Atmospheric turbulence)

i I I '. ~* ~ :1 :, ! , F1 :11 11 - I 1j, q I : I ; ! I I - i; t ft ; I - .
GRUZA, V.V.
LineRr paragenesia of the main rock formation elements of Devonian
r C
acid effusives in the A! t.&i- f -1,4 --- - P-4 nra& tice of gn(-,; ;,
interpretation of them. Soy. geol. 7 no.12t27-38 D 164. (MIRA 18t4)
1. Vaesoyusnyy nauchno-issledovatellskiy geologlcheskty institut.

p- . I ~ .: , F 1 ~!* - i.1 .11 :1 ~ 1 1! 11 1., 1 . I I i I !~ t ~.~
C.RUZAKCV7,' D *' E -. Senicr Veterinarian, Ko,-A A59R.
ItFat-free sour milkin treatr.ent cf endcretrites
of cattle."
SOs Veterina i1a 25 (3), Mar 1948, P 42
0 0 * 0 0 0 0 0 0 0 0 0 0 0 0 0 0 9 0 0 0 0 0 0 0 0 0 9

I . : .. 1 1: -,;;r . ;l.l.
GRUZANS, A.) -izizh.; j?IZOVS, A., urkhitc-kt; idF.Ko'll"", I
[Fundamentals of construction and oanltar7
celtnieciba:3 pamiiti un eku oanltz--a tolmika.
Latvijas Valsts izd-ba, 1963. 4-1~ 1). [In Lat'V11,111]
C; E?A

3 _3401
7,1 S/666/61/000/000/003/004
D215/D305
AUTHORS. Poplavko,, N.V., Manuylov, N.N. and Gruzbeva, L.A.
TITLED: The welding of titanium alloys
SOURM Svarka tsvetnykh metallov i splavov; abornik statey. Bal-
kovits, D.S. and Poplavko, eds. Mos,_,ow, Oborongiz., 1961,,
72-110
TEXT,- A general review of the subjecto Pickling is necessary to remove
oxide and gas-saturated layer prior to welding. Solution 1- 289-350
CAN3 HCl (s.g.1.19) * 50 g NaF per literi solution 2~ 340-350 cm HCI
+ 55-60 CM3 ,NO_ (s.g.1.14) + 50 g NaF per liter. If surface contamina-
tion. is severe,othen after preliminary descaling by cold rolling or sand
blasting the metal is pickled in 80:20 NaOHNaNO at 420 _4500C or in phos-
0 3
phoric acid at 270 10 C followed by solutions I or 2. In the more power-
ful pickling agents hydrogen absorption is a potesitial danger and may
cause porosity on welding. For good welding it is necessary to (a) use
Card 1/3

33401
S/666/61/000/000/003/00,1
The weld3or, of titanium oa 0215/0305
material at the lower strength limit, but with ample durtility, (b) avoid
Mark l'-1..2 (VTI..Z) commercial Ti, (c) limit interstage pickling, (d) avoi.d
suriace coatings in areas to be welded, and je) use clean filler wire
preferably -vactitim annealed, A discussion is giver, of welding technology,
~ungsten-arc welding, typical. Conditions, nozzle diameter (up to 12"'14
mm. f,?r manual and 14-16 for automatic welding)~ Measures to ensure free-
dom f-rom contamination (gas backing, interpass cleaning etc) are given.
For submerged-arc welding AU-'i (AN.-TI) flux is used, and for electroslag
w&lding fkabove 50 mm (AN--T2), with argon to shield the slag
pool. In resistance welding the electrode tips must be spherical,) with
a radius of 20-250 nun. Alpha-Phass alloy welds are onl.y heat treated for
stress rel;~efq and normaliy bnly manual tungsten arr- welds r&qu-,re this.
Oxygen ~n welds is restricted to a maximum of 0.'. - 0.25'a; up to 14.5516 can
be disv~-Jved, by Mitch it stabilizes and embrit-ths. Nitrogen acts
,n a e~&Alar fash,-o-n., and is restricted to 0.03 -- 0.0% maximum. Together,
these gasrs promote CTaCk formation and reduce ductility, while hydrogen.
~an -aueAe de~lay&d ~~racking due to volume changes accompanying the pre-
,'-P.'tat:-Dn of Ti hydride,) and is kept below 0.015%. 51milax effects Occur
C. ar d 2~/-3

3.3401
S/666/61/000/000/003/004
The welding of titanium D215/11305
An gas-contaminated surface layers. Impact strength if adversely affected
by hydrogen,, particularly at low temperatures, but a mixedc~ structure
is less eensitive than pure d, It 2 also caused porosity at the weld
junction. Effects of alloying elements on joint properties, particularly
fracture strength and bend angle, are described, mentioning Al. Sn. Zr,
Mn, Fe, TL-Al.-Mn alloys, influence of Mo, Ta, Nb, Ti-Al-Mo, Ti-Al.-V and
Ti,Al~-Cu alloys. The influence of small additions of B, Zr, Ce, La and
Re on the weldability of Ti alloys (mainly in terms of effect on angle of
bend) is discussed,, There are 41 figures, 22 tables and 20 references:
12 Soviet-.bloc and 8 non.-Soviet-bloc. The 4 most recent references to the
English--language publications read as follows: G.E. Faulkner, Welding
Journal, v.34, no. 6. (1955); J.R. Ridy, J.B. McAndrew and H. Schwartz,
Welding Journal, v. 33, no. 8, (1954); Welding and Metal Fabricationg
-Y. 25, no. 7, (1957.); Metal Industry, v. 21, no. 5, (1960).
Card 3/3

r-~ 0 kon(7!--,
ice
p
erinari,m
.arch
0 0 0 0 0

i ~ I , :: ~i F 1 ; t, ~:.j j I 1[. 11 : 1~ , ; . I I ! I ! -
,; SERGEYEV, L.; IVANOV, 1.
BABALYAN, B.; IVANOV, G.; GRU DEV,
z . ~ _A,
For a model main air route. Grazhd. av. 21 no.6:20-21 Je 164.
(MIRA 17:8)
----7 , -- -

6(4)
AUTHOR:
TITLE:
PERIODICAL:
ABSTRACT:
ASSOCIATION:
Card 1/1
SOV/107-58-12-15/55
Gruzdev
They Are Studying iadio (Izuehayut radiodelo)
Radio, 1958, Nr 12, p 12 (USSR)
A brief description of r3dio operators'
courses initiated at the Norillsk To,,,,m Com-
mittee of DOSAAF: 15 person-, have success-
fully completed 10 month!, hard study with-
out having their normal work interrupted.
3 female radio operators who have completed
the courses are sho,;.,rn. There is 1 photograph.
The Noril'sk To%,m Committee of' the DOSAAF

GRUZDEVJ, A., deputat Verkhovnogo Soveta SSSR
New tasks and forms of material incentives. Sots.trud 7
no.4t95-1,04 Ap 162. (KRA 161l)
1. 14rektor Leningradskogo metallicheakogo zavoda im. XXII
8"yelds. Kommunisticheskoy partii Sovetakogo Soyuza.
(Leningrad-Wages-Metal industries)
(Bonus system)

(',ruzdev, A.A. "n 1-i ne a r 12 - I ~j / 17
A TPHOP '11~~~~ ' - _ -
TITLE: -Pne Mechanizat-lon of Wheel Guide-Rail Planina on Log Roads
ic-,r ~'ars i,ifekhanizatsi-ya atrozrkJ kolescurovoda avtclazhr-e-
~-ykh dorog~~
P E F. T, C: D 1 c'A I. :~ek~ianizatviya trud~y' mkJM-. i7:yazhomkilch xabct..
p
rii, ~iverllovskiy nauc no-iqs'p__4cv6'91:skJ*,y ins-.1tut lesnoy
p-omyshlezinost,, 't~e '7-terdlovsk .~'icientif;.c :iesearct; '.1sti-
lute of the '.utr .oei mdustry, Inas aesipned and man,_:~factured
~dr-sigming enginer-r .',,A, 1_;tefan-.)v,, Erwinepr'~ a Machine of
iype f'cr the vianing of rLiJLde_.rSjL!j Po~-
and INTAZ-5~)l trucks- T'-e average --apacity of ths- planing
machink- is 130 -.,u:-.rinx mi-~te:.,s, the maximwr, p,-zfcrmsn-,,p be-
ing 159 runm.np meters of pi-aric-d wheel per shifit.
There is I set of drawings.
Card 1/1

L 31217-66 EwVm)
ACC NRi AP6022789 SOURCE CODEt UR/0217/66/011/001/0181/0183
i
r
AUTHOR: Gruzdev, A. D.; Tsellariue, Yu. G.
ORG: Institute of Cytology and G~netica, SO AN SSSR, Novosibirsk (Institut tsitologii
i genetiki SO AN SSSR) I
TITLE: Effect of preliminary irradiationtith short-wave ultraviolet on the lumi-
nescen-c-e-o-T some biological objects excited by long-wave ultraviolet
SOURCE: Biofizika, v. 11, no. 1, 1966, 181-183
TOPIC TAGS: radiation biologic erfectg lumineacencep uv irradiation, photochemistryt
amino acid
ABSTRACT: .'Experiments'earried out on human cartilage, bo~ino' blood serum, I
tyrosin6. phonylalanine, and the tripeptide, glMl-glycyl-glycino indicated
that preliminary irradiation of those substances and biological-objects with
bhortmwav~ UV increased the intonsity of luminescence induced by irradiation
with long-wave UV. -The maximum luminescence involved was in the 480-520
rdl3imicron range. The relative increase In the Intensity of induced
luminescence. which may be ascribed to a photochudcal process, decreased
with the dose of radiation applied, I,e., saturation was reached. Study of a
number of organic substances showed that riany of then exhibited the effect in
4uostion in the crystalline state. but did not adt lmdnescence in the visible.
range in so2utions either before or after irriftation with short-wave UV*
P73t6l1ift Organio substances which showed considerable luidnescence.befo3re
Cad 1/2

L 31217-66
kCC NRt A
irradiation with short-wave LN (9.g,, saUcylio, fluorescent 41YOstuffst tryptlophan)
.Wthibited the opposite effecti the intentity of their badnescerm an Mwitation
'with lom-wave UV incroisod -after prouldna'ry irradiation with short-wave
;~UV. This did not apply to tryptophan In solutions, w*Ach behave like the
bother amino acids studied. The luminescence of callAgen prepared by dialysis'
I of Its solutions in a citrate buffer or In acetic 4oid was wthanced by
~PrOltzbuLrY irradiation with short-wave UY, Collagen film obtained by
; raiAd drying of these solutions. which normally do riot exhibit luidwso
sunder the effect of long-wave UVIs wero activated b tion
wave UVO- - (*ig. art. has: 3 figures. lim]" _V I=&&& . with she
SUB CODE: 06, 20 / SUBM DATE: none / ORIG MW 1 002 / OTH W: 001
C.rd 2/2 &j~-

AGR09KIIk,,k BRODSKIY, V.Ya.; GRUZDEV, A.D.; KOROLEV. N.V.
Some problems in the quantitative spectrophotometric analysis
of the call. TSitologlia 2 n0-3037-352 Y4r-Je 160.
1 (MIRA 13:7)
1. Inatitut morfologiL zhivotnykh AN SSSR, Hookya, i Institut
taitologii i genetiiI Sibirskogo otdelenlya AN SSSR, Novo-
sibirsk.
(SPEMROFHOTOKIWRT) (CILLS)

Gilftil"DIi,~"iIP, F, ~ KIL 1 J
of tilt rav, o-I.et n~ ,,rcArr,,~ :i, rn e~ to-- o r~ ia
r. 1 T j:
.11 no.5:585-587 S -0 1630
1. Laboratcriya obshchey tusitolo,,Iii L -,-.~netIkL
S
ibirzkogo otdelen-iya -F

t'~ ~a rl
r f-,TI
of ce"'
l1 .3ti t S
cvc. 2,

GRUZDEV, A.D.
Orientation of microscopic par",Jcles in eli!ctr--'c fields.
Biofizika 10 no.6:1091-1093 165. (MIRA 19:1)
1. Institut tsitologii i genetik-1 Sibirskogo otdeleniya
AN SSSR., Novosibirsk. Submitted January 25, 1965.

SHPILIBERG, B.A.; SHELESTOV, M.S.; GRUZM, A.K.; PFJ.Vnlffxff, Yea.
FILICHKIN, I.Ye.; ZHAVORONOK,'-V.I.
Zyr7anovsk deposit sulfide complex ore dressing in heavy suspensions.
Biul. THIN tevet. met. no.19/20.-34-39 '57. (mrRA 11:5)
(Zyryanovsk--Sulfides)
(Ore dressing)
'I. .::: t
..:A ~, ~ - ;~ 1i I I !'A - 1;: 1 , ~~'! 11 '1 ~
i 1 H; *:I!.;_ I -; CIIH,gjr~f, W;: ~ , , VII 4F,

I ii i'f i-;j f:ml :1 4-1jr7;;jw:! pp, 11ip'. -j11. 11 1 i1FIII

HEUMI&W.W.AND TUERbWPH=CAL:PROPERTU*
qF MOLTEN UKA"AU=AWr III
"OV704, E, M. Mabxk~SbMj V. A
prinantse ana jL. ya. va"um. MWWJ. Al a-ijus Knom
4 -60(1956).
_'545
An- Invc-3tigatton was undwiNken of beat trusirso to Mol-

ten sdd am during turbulent-fldw iq a rQUIA
copl*e ar".
nickel tube. An interpolation formula was obtatnod.
partments were cond
between liquid sodi4mand a solid wall of copp6i, rJokul.
Wd stainless dal. MotWs vore davefoxAfor; tseustiri4
'
Mont (A. AM-11jit
. temperature ChMuctiVitAnd 11~~y
molton Motalls., Results aregivOn'-for namuramduill GC
T mum, powasi
UM
um "IM "62 tozatiflo ow;

diumandpot4salum
, -F

SOSNIKO, Mikhail Nikolayevich; KONSTANTINOV, L.S., kand,tekhn.nank,
retsenzent; GRUZIST, A.K.. inzh., retsenzent; SWANIN, A.A.,
inzh., red.; GHUMSKATA, G.M.. red.izd-va; UVAROVA, A.F.,
takhn.red.
(Present-day founding molds] Sovremennys litainys formy.
Moskva, Gos.nauchno-t9khn.izd-vo mashinostroit.lit-ry, 1959.
274 p. (MIRA 12:6)
(Molding (Founding))

GRUZDEV, Aleksey Nikolayevich; KOLOSOV, V.N., r(-'d.; ABOLE2.101r,
- --- V.r- ----red-----
(Mechanized corepaking for foundry molds] Vektianizirovan-
noe izgotovlenie sterzhnei dlia liteinykh form. Yo,;kva,
Vysshaia slikola, 1965. 293 p. (MLIA 18:2)

NIKOLAY.&ViL, N.V., inzhener; PAMYiITNYKH. i.S., inzliener-, MUSATOV, T.P.,
inzhener; MAKHMUROV, L.D., Inzhener; DAYTELIAN, G.E., inzhener;
IOFFE, B.F., inzhener; GRUZUV,tL.V,, inzhener; KLMIRIYEV, D.P.,
inzhener; MOS'KIN, V.S.",' ftft*-'d*0'
On the organization of service for district substations. Blek.
sta.25 no.2:36-42 F 154. (HLRA 7:2)
1. Azenergo (for Nikolayeva, Pamyatnykh and Makhmurov).
2. Donbassenergo (for Musatov and Danyelian). 3. Mosenergo (for
Klement'yev). 4. Gorenergo (for Ioffe, Gruzdev and Hoalkin).
(Electric substations)

GRUZDBV,_A.V. Inzhoner,
- -
Dispatcher control of aUctric power systems. Ilek. sta. 28 no.6:
52-53 Je 157. (KLRA 10t8)
(Illecitric power plants)

U3011/14edicine - Poentgenology
Card 1/1
Authors Gruzdev., B. I., Candidate Medical Sciences
Title Concerning the laminar investigation of the gall bladder (choiecysto-
graphy)
Periodical Vest Rentgen i Radiol 1, 40-45, 1954
Abstract Properly administered laminar roentgenological investigation not only
permits the detection of concrements in the gall bladder not possible
by ordinary methods., but also increases the possibilities of chole-
cystography. Three drawings.
Institution Roentgenological Department (Chief-Professor I. A. Shekhter) of the
State Scientific-Research Institute of Roentgenology and RadiolWy
imeni V. M. Molotov (Director-Professor P. D. Yal'tsev)

ill LAU'Llh 4:011trol. no. 3
64. W1 A 1"i iu)
~Aar~'hiy olektro:~,.akluinik -:irov~ico~Y
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!bearing Plant). Foslk-.ra, 'Redizdatsektor 'Jossnaba
333H, 195,1). 159
Sj: Monthly ldst of Russian Accessions, Vol. 6, 7io. 1, iiL~1-11 11~753