SCIENTIFIC ABSTRACT FR:MAMIDZHANYAN, E.A. TO:MAMES, J.
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CIA-RDP86-00513R001032000004-6
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Publication Date:
December 31, 1967
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SCIENTIFIC ABSTR
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AC~C'"$r0i1 NR: A~'~t033062
10 cm in diameter� The fi.i`th and sixth series were placed beneath a lead si~ield.
It was found that the fxegtitancy of the young showers increased by a factor o� 11a-16
fr~nin sea level, to the mount~~in top. Ti~,s indicates that ~.-me~~ons p~.ay an insigW
nilca.cant role in the farmat~.Lon of young showers. The comliribut;ion of ~ -:~esons
z.t: ~~hes� events at a height of 320 m does not exceed l~ of tl~a~ total of the young
sliawer. At soa level, the c:ontxibution may roach 15~. The at~E,enuatior~ length in
thF4 lower layers of the atrn.c-sphere of nuclaor~ with energies af' ~ >~2 ~10~ ev is
1051 + 8 g/cm2, When the a.nt,oraction range of nucleons in the atmosFhere is $0
g/c~m2, an attenuation len~~l;i of 109 g1cm2 c:orrasponds to an average inelasticity
coE~fficient of the nuclaoas of K d 0.~. Wptan the interaction~r~ge is 90 g /cm2,
~ a, O.b. Orig. art. has: 3, formulas.
ASSO~I:ITION: 7nstitut fiz~~a. GKAE (Yerevali~ NIIYaF; N1GU (Insti~tuta of Physics GKAE
(Yerevan) M1'Ya~~, .~1GU); Ye~cevanskiy gosudarstvenny~y universit~at(Yerevan State
University) ,.. -
SU~3I~ITT U: 00
SUr3 CODF,: rS, GP
Card 212
DATE ACQ: 07t~ia~y6t~ Et1CD s 00
NO REF SOV: 003 OTHER: 000
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ACCESSxON Iw~i: AP1~0330b2
s/o~5a,l~fc~3s/OOH%:0~./O~o~,
AUTHORS: Babayan,, Kh. P.; Grigarov, N. L.; Mamidzhanyax~, E. A.; Shestop�rov, D.
Yd.
TITTLE: Tlae height behaviort� of nucleons of h~.gh energy ~,n the atmosphere (Presented
Uy I1. Z. Tor-~~i~.lca~ye],yan, c arxes~onding member of the AN Armyanskoy SSR on 2s
Selpt�mber 1963}
SC~Ul~:L. AP.T Arr~SS;ft. Doklady~, v. 38, no. 2, 19bli, 101-10~t
TC~1C TAGS: nucleon,� atmosphere, attenuation length, mu meson, ir9teraction rare
P.BST~tCT: When a nucleon laf ha.gh energy interacts with a substance, the definite
attenuation lenj;tiil of the nucleon in the substance leas an intrinsic value. Tlus
raper is devoted to a determination of this value ixi the atmos~ohere. Computations
show that dean a.n the atmo+sphsre the attenuation length of nuc;I,ear-active components
is determined onl;y~ by the ;absorption of nucleon companents. Tlie authors have used
tl~~e hei~lt behavior of yoWng atmospheric showers for this purpose. Measurements
~rere made at heights of 2E~~ and 3250 m. The detecting apparatus had a working area
of l0 m? and consisted of ;s,ix series of ionisation chambers, each 330 cm long and
Card if 2
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their energy tl~ primary nuclear-active particles. The investigation of nuclear-~
active componfl~lts of NAS indicates that 'at Eo ~~ l.7 x 1012 ev nuclear-active
pax-`~iclc energies there exists (~rith 0.]..Z. ,~~ ~r `~ 0.27 probability) an almost fully
r. ~ ~ � - mQSan
inc~.s,utic (,H ,:, 1) intc,ractian wi~;h lilt�atomic weight nuclei 70~ 'y"('
ere::^~;~ tray:::,.;: e:~ (to~? ~~pr~y" paz~icles) in a single event o These interactions
~.~:tr~,GUCe more than a ~5N contribution to the energy loss in '~ o -meson forma~-
-~~.on~ Orig~ a.~ c~ has a ~ figures and 1, formula.
?~~L~~.'.~~Ol~rs '~rerev~.ns!tiy ~.rsta.u::t'. fzza,ki GiLh.E {Yerevan Institute of Physics);
~.1TYr;.~ 1-.~L, Yere~tan::r:i.;~ boUu:i~�stver~ny.:~,T universitet (Yere'v.~.n State Universii:y)
~3~.::.~::'~w,~ ~ Op DkTE :�CQs 16Apr61~ ENCLs 00
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l1L~/mil ~{/~ 7
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' x~id NRs ,p~>~o2638o s/oz5;~/6ii/03~/~lj~oog/0015
ACCESS
. Kh ~?. � (3ri~arov, i~. Z.; M~dy~Y~-t l'~� A�; Shastoperw'~
r,~�THOr'3.5. Br~bayan9 . , .~::;:.~._.._-.--.~-~-------�--- .~,...
V. Yao ,
articles Edith light-~-tomic ,
TITLE: Interac~tzan of n.lic].~oar-~activa ~iza.~li-onar~y p prasant4d by corre-
t~rui~ht nuclai, Gharactorized by 1Li..~;j1 u~:s,a~roo of inolasticity
apond:;,ng-member G. 2~. G4ribysn of the ~tcadomy of Sca.ence~ Armenian SSR)
SOU1~Cat ,AN .4rr~SSRo Doklaay~, v. 38, no� 1, 1964, 9-15
.,,r�d ' w r ~ A'
`POl'IC `I'.nGS: d:Lactron-plt~oton atmosphoric shower, a.onization chs~Mx>or~ ,, - ~-~..~',
nuclear-active particla;s, � ir~olaat~-c i ~~i:rtrryction
'hnwars" (TdAS) 11avfl
~~;,~;'ry~i~~�1: `1.Z~3 So-callf)t~ "notia oloctz�on-photon atmospheric Si
The equipment eras spree. ovt~r ,
bean studied aG a 3200-rn, z~.t~.tude above sc~a level.
an a.roa of to ~r~' and consists of 6 ionisation charabur3l~ lobe elec~on photon ax�a~
tion fi7.teru, ,a,~cl two u;~per ser~.es chambers for moa ~
component oi' N,~. xt is assumed that "ne-~r shelt~rQrs" ere ~~tethe~ eater parteof
actions wY~ore a certaa.n number of ~�-mesons t~~ lt) transm~. B~`
�~ ,
Card 1/2
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. , 7
Investigation of the.�. $/048 62/026/005/002/022
H102~1pG
(4} at sea level, the muon aantribution is ,~70~ (N 103 particles) and
�~ 50ya (rv1.104 particles). Tho buret spectrum Ras found to depend greatly
on the area of the measuring arrangement. Plith 2.103 - 2.105 particles,
Goes oust from 1.3T ~ 0.02 for (330 cw)2 to 1.99 0.05 for 10~~330 om2.
The spectrum of buret� with a no energy transfer of 3.1011 - 101'S ev agroea
with that ~of nuclear-active particles, and exhlbite no "breaks". When.
particles ~Nith ~; >1012 ev interact with light nuclei in about 10y6 of the
events, th~a irteraatian is oowplately ineleatio, and the so energy tran~-
fer amountla to 60 6~~/ of the primary-partiolo energy. Suoh interaotiona
obviously allay a aign;ifiaant role in the formation of extensive e~ir
showers wi~ih at least 104 105 particles. There are 8 figures elnd 7 `
tables.
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Investigation of the... B102 H104
ionisation bursts in the filter of the arrangement, for the alltitudo
dependence of the burst frequency, and for the burst speotrum and its
dependence on the size of the arrangenenti the mechanism of local no
generation by single nuclear-aative partioles was investigated. The burets
observed ~vere grouped according to their intensity I, i.e., a~icordfng to
the nuciber of relativistic particles involvedi for each group;, the numbers
of ionization and "struaturalized" bursts were determined for rows I-IV.
The spectrum of ionization burets can be described by N(>I) AI -Y for
all chambers. The index of the intogral spectrum for 2.103G:[~-2.105
equals 1.37 0.02. Ctith an area of w 0.6 m2 it was found that; N2py; of the
bursts were "atruoturalized" for 1.103! I~ 5.103. At I y 1.1014 and 10 m2
50;~ of the bursts (at sea level) and 7gg6 (on the mountains) heave a struc-
ture. ,in analysis of the course of the bursts Nith the altitude has ahoan
that: (1) the integral spoatrum of muon-indUaed bursts with '1.103 - 3.104
particles has an ~exponsnt of ~ . 2.22 � 0.14j (2) for a burst~of equal
intensity, induoed by a singly nuclear-aative partiole, ~ . 1,98 � 0.091
(3) at 3200 m, the muon contribution to single heavy burets ie~ amnll (15~
of all 'burets lsitk- ~ti103 partioles, and n,496 of those with X2.104 partioles ~. �
Card 2/~' ,.~
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l i 7, 3':
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3.~~r~~~ ~~~os,z~-as,x$ds~~ A1o2 a10a
AUTHOR9~t Babayan, Kh. P., Aahetak;i, Ya. S., Boyadzhyan, Ji. 0,,
~,__Z,_A..., Grigorov, td. L., Loskevich, Ye. S.,
,tia~,idt;:hanyan, E. A�, ~aflsal~skiy, Ye. T., Oles~, A. A.,
~~yAk'ova, ..., anrmer is provided with longitu.clinal slots and the working tool forms one piece with--,
the trfu~sformer (see F'ig. 1). ()rig. art. has: l figure. !,
_ _ .._ ._ _ _._ ..e M
Card
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------
/Y~ /9 M ~ T
J~ s
rs~as >: ~aooa sxFlorrAriul rpv/3654
Akoi's1n, !. A., F. 1. And1+Y~, j� 1. Apei'tsln, ti, N. lhtrviaA, A. A.
~;j, Yu. N. Kostrikia, I. 2. Xaehelev, AWP. Maaat, Tu: 0, IaH,~: N.
8eadlk, t. 1W. 1We,YDu111n - _
Ilpravoohnik khiaika-aiargotika. tar It 8yravacJwYir natsrialy obshahego
pawacbealya (Hsndhook of Chemirtry in Foyer Lagfnrrriog. Yol It tlsarrsl
Retbrena Materiel) Noaoov, Oossnesgoiadat, 1960. 327 p� 20,000 copier
printed.
tdr., /'.A. Oolnbtwr, B.N. Oyrriah, Yn. K. 6artrikin, aad A.F. Mtusati Tech.
Id.t K. F. Yoroain.
FUAAO�It Tbir handbook lr intended for absnlete in the HrIA of pover en-
d3naering pereanaal of LborataKre, aolrntitia reeaaro4 inatltuter,
cad plann~ag and control argaaiestioar, e� w21 u for stwi+nte of
uai~~rrsitiee and 1;ekhat.ksers,
OO'lktiAtlgt Thie is the riret of a throe-rolava handbook of ohewirtry in pawn
engtneezlag. It lnaludes data oa the voters ten o: boilerr, cauwr Of
cor:rosia+ and aethoda for aaatroiltng it. It afro aootainr genaral rafas-
eaalr�aterial on neuares cad units, chesScal easF~~, voter and
col+ntiaa+e, rolabiltt~r of eubetanoer la eater and rater Tapor at wriona
taRppeeratarea, aLatroahealatryj ~gsssea, epealriaatlow an4 prlees for
certain reagents cad wteriaU. the Doak lnalndes tabUr, aborts, and
die /o pereoaalitier ors eunttoned. TWre are Sz refexenoest 39
~~ ett 10 ~illaht 8 Gem, cad 1 pvedirh.
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a (~)
Sov/gl-59s~11~~-4/2
AUTHORS: GurvicYl, Soho, Engineer, Kagany D~Ya:~, Candidate of
Technical Sc;.ences, and Mamet~,,,,~:,~'-,~.~, Doctor of Techni-�
~~~~R
cal Sciences
TITLE> Causes of Boiler Corrosion
PERIODICAL; Energetiky 1959, Hr 119 pp 10-13 (US�~R)
ABSTRACTa The authors exnl.ain the passable caua~es of a case of
boiler corrosion at an unidentified plant4 The corro-
sion was detected in a DKV-10-13 boil,ero It was cau-
sed by an interaction of several factors large s,._
mounts of ammonium sulfate were added, to boiler water
in the feed tanks the regeneration of ammonium�-sodi-
um-cat~~onite filters was not performed properly; no
deaeration of the boiler water; improper washing of
the bo~.ler with diluted acids4 They ~~tate that it is
very difficult to estivate the degrees of the influen-
ce of the one or the other factor because of the lack
of sufj�iciently detailed datao In thelir conclusions
the authors give some general instruc,tians for proses--
Card 1/1 sing bailer water
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Ex;pBT�ience in the p1�eparat.ion of magneeite aorbsnt and in the ;50V/96-58-10-10125
de-silication of !'eed-water for high pressure boileren
iiltrsrtion on the egfeetiveness of puriYicatian. Iit will be seen
from i;he graph in Fig.S~ that as the rate is increa~ded from 4 to
107 nnlhr the silica content increases by 0.51 mg~l;itre. The
resuli~a plotted in Fig.a. show that by reducing the hydrated
alkaliinity of the water delivered to the sorbent Tilt�rs, their
effectiveness is improvedo However testa could not be made at
pfl va;Luee below 805 because coagulation of the water by the iron
anlphate was impaired. Thus the best condition Yor removing
silica from water by magnesivaluerofntheswaterc eb8~5t~ 9anditian
of li~uing with which the pH esite sorbent absorbed
In eiz months of~aperation the magn
b72 kg of silica, a third of the theoretical capacity. The use
of magaxeeite sorbent simplified the process of water treatment
and reduced the silica content of the seed water from its former
value o~ OQ8 gM l.3 mg/l~txe to 0"25 - 0.,5 mgllitre. Aoflex
blorr-dawn, ~xae correspondingly reduced-, There i-s a~p~ aditorial
Card 3 f 4
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Ez~~erienae in the ?preparata~~on of magnesite aorbent and in the ~QV~98-6g-14-1.026
de~~silieation of Heed-~-ater for hligh pressure boilers.
availai~le at tb:e power station, is sketched in Fig.l., and the
procedure used to manufacture the aarbent is described. The chemical
analpaia of the: aorbent wasa 36.5 Mgl1; 22~ MgClg; 1.26 CaCl2;
6.$,$ FsCla, they remainder being meanly water. Each filter rtes loaded
with 6.8 tone of aorbent9 to the heights given in Fig.2. Before the
filters oars na~ed, ezcesa chloride use washed out of the aarbent; a
graph of the ua.shing process appears in Figo3. Fnl.l-scale operation
of the filters commenced in March, l96? and the results of si= months
operat~ton are plotted in Fig.4o Which shows that the ailioa content
of the treated water has gradually risen to about 1.~4 mg~litre Si02o
The increase has probably resulted from conta�i.~atiaa of the aorbent
with organic substances and iron ozides. Th� aheaic~al analysis of
the aorbent after 2~ months operation is given in Ta?ble.2;
althou;~h the chemical composition ha$ altered, the mBChanlical strength
is unchanged. There as a considerable increase in the silica and
iron-o~cide contents of the aorbent� The silica eontlent of the
water na~a somewhat higher thaw it should be, and attlsmpta to improve
matter~- by raising the treating temperature by 6�C to 42aC were
Card 2~4 ineffectiveo Tests rusts made of the influence of tells of
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` -AUTHO$s Mamet, A.P. (Dr.Tech.Sci.~ SOV~9a-58-10-1023
Ni o :ayev ~CAp':-~~ngineer)
TITLEa Ezperience in the preparation of magsesite eorbent and in the
de-ei.lioation of feed-water tar high pressure boilors. (flpyt
prigaltovleniya magnesitovogo sorbenta i obeskremni~raniya vody dlya
pitaniya kotlov vysokogo davleniya~
PE~IODICAI,s Teploenergetika, 1958, x'0.10. ppa 42-46 (U$S$)
AB;STBACTa In Soviet porner stations eztensive use is made of a-agnesia treatment
for the de-si:lication of water. Ae various practif ~cygen dissolved in water, of mater ~apo~
f leakage of ; ~o�
�~ a1 in empty and partially e~pty bo~.ters, and o
tinctioa i.s drawn between
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scussecl�
superheated lsteam are di
f shut-dorm periods of a few hours and those of
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��'y the effects a~
nBxet-
sevleral days,. Recoas~endatiaras are ~iv~n Por partial heat
reservation b;,'
for
il � ~Ir�
.
~� ~ p
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in 'the farsne~r case and specific deta M.~'
~t and dry methods in tFe latter. :,r �'
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APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001032000004-6
APPROVED FOR RELEASE: 06/23/91: CIA-R~P86-005'13800'1032000004-6
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