SCIENTIFIC ABSTRACT SKOPINTSEV, B.A. - SKORA, K.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
• Document Release Date: July 13, 2001
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

A qualitritivir chafacterstation of the organic subMance. it,
natural waters it, A. Skopinim% mid I , A MAII01-,
lu,l.. N-t.-hrilLa-L iltd-kh ...
111.1te-I'lly (11VIIIII,11.111 'NI'ltvil"I'l 14, IlkS IIMIIMI~
I-f. its Ilk.. mull.0 .1'.1 ..."1 m-h 1". 11'.
""I'litillit 14jurl .111.1 11 11 11 .4 J tkmrl 'smid"
I"Irl. Itotato Stalch Illatulf.. givels. r'I"Und omcts' md
reservoirs. Natural waters rich In org. matter which 6 ill
the unstable type (in the B.O.D. sense). such as rA,Ilufiuu
or plankton growils, Live a higher oxidatioll itulex ill Ilk.
lhan in acid ine.lia. waters IIa%r a higher 11.4 ).D. Ili
"alit Ifir ..%idalimt I,% At I~ .."Ilg I.I.-
lu".11V m.", -4 ~"-It ."S. 4- It I I I I
ill oIlh Ill. It,
.." 1-t Al-t'd I'V It-
h, 11.4 ).11. 11.4vitn ~A tw, d -u. ,O-mt . ... .......... IA,
Xuar, histidille, Ivtt)NIIu*. twiltmic, t-lig .111tillum. "IM
acid --were Louipatt-d for their oxid.,11"ll IA- its mmll.d.
-~A, and alk. tnedi- In u-t as,s Ihe -i'lation ." lugh'.1
C.I.A. inedLa.urtiept for the tvn~mc. humic acid, varse
"-1. wparaxu '. ;Ili, I CrValuline. J. S.

jry~=*m~al characterWics of the rivers P"b,
fBtTb
I Kurdzkips (tributaries of the river
Kuban.). 0. A, Sk"InflevIllyllrochtm. lint., Nijvi-
chtfitank). Gidrokkim- AtaterialY(IlYdit-lic"t. Matctial-
14. ITJ-7(1048). -Ankilytictl daut of Me witlets durms lhr
immth of June. hKO: pli. ulky. tmnu 11.). ItjflIlw-.
,dt "Mtcllt (CA, Mg. 1jr. cf. SO.). S (pa"lliumill. llitwc'
The am" ad war" of do Veop is Cue ses drift"
WA. !&UON(WV (Ilythm . ISO.. Novo.
F(H We . blawrialle?
4, 140-W IM).-4wo tire liw-~ me& do Sk
34
am=
crowled br dw VOW dorka
star and tirtir Soldbw out Tolian his custom MM dw oft
bmmmnd 9011161011 Is eon&
,tW~wd by :!ra=i= cd the ad purtwor. partidw
of OAOI four. true diarpfew MW an of am&-
0.002 no. lorsesoo as a Mook of dw
deaffroote M a Mesa Olt 7**
spew of - 4 blow
cunce. of M=i~ dw ubw 1111116 And Mak memo.
More NW is Oused is Clue Nate Is Ilie bediftft
M J. S. jalk
Oz

qv-we 0-0 a 4 0 a 0 0 0 C 0 0'
is 23' A B a '20 V J1 it 11 Ad is U 31 J-D 9) At Al 0 a AS
c I L A. W it EE i
tjT
Offluic matter Ln some waters in Podmoskov's (Mos
Co neighborbood). 4~
A',- $Wpi;Auwv. 1),,*':Jy Akad
.\"Wuk S.S.S.R. m. rvix,tt. un 1u
~iruplt~ of water-i front several rivvrs of the arx-j. I)a~u a*
are givtu on the color, fLtrdne,-%. alky.. fxr. nutt,r.
C. N, 1'. and B.O.D. It ii viint"I out that for (jig.
InAttCr in W3tCr-., a factor r-f 2 imlead of 1.72 hould 1w
11-1, .4in~ the C (-otltcnt i~ u,u:iljy J~r to 50~~.
d 1. S. joff'. =*O
00
00
.1. of
'900
bill
";0 0
C-z-
rest
lXJQ.J -L' 1'- 0-1 44-1i-1 cot 0- is,
;N -i~xl~ too
U Is AV M3 IS ~ ' j*, ; 1 ' ' * ' All I S if ew 0 m a I v 04 1 93 0 3 11
0 W D a u it x u K tt is it o( Kin n i I u
000000000060006000. O;i
,a 0 ZO 0 0 0 0 0 0 0 a 0 0 0 0 0 0 0 0 4 1
0 0 0 0 0 0 a 0 a 0 CO 0 - 0 100000 0 0000000900.8061A

8 C D If Q W X L a N 0 Fill 4 1 T t., I It crm ]a it 32 33 u IS 36 37 is 39 a It a 43 Ad n
~'-! ! ~ IT Ol AT U
conflis I F. GNOUPS
09
~Vl jignivilI111i 1w3limnilyliv ..tf.'.Lt ..Dtl 10 :
'1S-1111, V
-1
fog r
1rin)ryl in p1.,)
JIIIvJ.l1!J Jill -~l 11.18111.1ir %amiazapti
0 &Z fit),
1.1%.4plIpAll ppl. till
1.111111lig Ill J- " X.Irl J3311!." 11! ll~%23,qo 3OU Jr Jim:
u411Jm1dol.(qd prolp its -uthummil aql qpA% pal3auumo.mo
Aq Itlaulaalitf.u ifatl) pull (vaziurl,.,111,
VIII-13i 1,11r) vall-.11iml )o xN111-iraildrisp aqL
MV
002 Atli Ill Iffalft"., Ill"'Ill-fl.0ilmll -,a-( -It'ittlittlixt(l 'Is' 0 0
1GOI, -p-MI'm .p1l !.-J1A.( )11,1 )11!41 pill 'I'm Jop., .1111 Itiml
-Iu3J!J J1IJil 1,1! 11AIMIS) J.114. smill-11, Ilpl% stfill"u,
I )Jill, ,%Il it! Ida-rl aia. tit, I -jurpto l.(tld tipAw lwlr~.1141.1
noAxwaj ia)rm mmwilV moij jo ~aajnns taip aqi uiliq
11,111'.'A -)Ill 11 *Aflr,3!I1.JItIpOJ1J.1 p4j"SI'AUS S! '1114K 341 -111111 C.
-1111 Ill all-Ill (1) LIMA Iliftl(IIIA 1111P 'JIffly -fill I
pfJ V'(1 fillij f (,Jilt j) ..tit "Jill
'it" (10 1.')il 11.1: 'Jill (ti: Ill
0 ev J!(%J "llatim, ppr orl ).I!s I.) J,)Jl p1m. .'Jul (I' ,I
aill auozi c.) altiplAcud aIJ.L 'UOvJIII.JdoJ.(Ip1
)o -Illyr ")p Allu!xxNa 'siairia dtur~r
tit .1ftL " 111 00
7
.11, 1-111? Ap.J X, 1.! -L,14. (III iii mat r timil
00.
iiis JtIAIIIJI1jI3 .3111pr till ti.ittlu 11ruairtu upwoi -.1tup 0 0
tit it! alrJo1w jAlp- A11I:p..1,j 'bdittrAts pur smIrl J0II!Ill
law) sr1lom 5r IlAoxq~ Jo.Q!tq.)!.i jilt Ill SJ-IAU(rfJAh 1:1011
tN
Ir 0
A~Iwirloj., -1, -11
lvn4va IQ IZUVW 29"1" JO I"I"(PUP"I NPRIO P S13nPOJd 00
00-.
T
--I t
v i. r 4--i-tw-m-M W v 5 a V-7
A, it It of a K R It It m it a a "
0 oj,g
0 0 UZ "61
--;-- -,, , 0 00 *1

5il.-OpIN,ljlSl!'Vl B.A.
33943 SKOPI14TS.~M, B.A.- 0 SKOROSTI
RAZLOZH,,'NIYA ORGANICHESKOGO VASHCHI-IISTVA
QTM-RSH9GO PIAMONA. TRUDY
VSESOYUZ. GIDROBIOL. D-VA, T.I. 194a
S. 34-43 - BIBLICC-R: 25 NAZV.
SO: LjTOPI-,-~' ZHURNALINYM STAIIZY, VOL. 42, MOSKVA, 194(?

Daltirminallon of orgsitic castmn in ttrah waltr It A
iAi,.d ,;.I. I ss.k zi-
Amal. Abint. 4, 192 Kj 19111). lilt-1114MI I~a Ill'"Illic's-
tion of the Krogh aittl Kt-v mrth,ul W.A. 28,
The coullwit'lams i~ vil"Ird mal ill a K irl.1.1111 tvpv ILIA I.,
the A& arm ot lthich it 11,11,1i'm tkll~ I, he ..
X14,1111.1 gla- J.,illl Ill the diTt"ll'.11 (mm Ill, 1.11 ,1i,1 .-I
III-11,11ml I'll.. lmt-wl il~ ,, l"1111 Ow
Imckt.1 its 1111, 1 : 111.1 ... 1, -4,1-
Isirged with :1 1 g ,( I-lv& Ag. 1111111, VW41 1 -11
I't fllil ~illllfll%- :1 9- OSIwOll' 111119- IKIIIII-11 CM I. All-lo4
1,11111. ixilittil Ph chr,1111.11c. -1-1- 1111tv.. 111111 AM "It.
,. .41 appgott. 3 It,. Awl phlit, 'I It,- tv, I .-Ill 1,11,
i'varrivil Ina %%lilt .. -111. "1 It- , II,q 1 :41.
putrificd 1144' Ile. 11,.4 ),.'A) tviL. , Ilwallat'. Im 11 6. .111.1 C,
(SO.)g 3 C. The climmat~ melt I, pt-liw-I fimit KjCI,I h
10. Ag,CrO. 4. and CrO I g. rhi- Ili% i, fit~trtl ill ;I
uffle whem it i~~ kept f- -`--S mi., after fi,-i-, The
Itielt Lq covlel. ill ;I m--riar. mid I,,tvd fin L.I.-I I,,-
Iirmn 10 to 20 isal. .,f .alt, I, t.,k,-,l f ... ...... [,,,, 1-*,,,,,.
30 to 1141 y of C vall Ile .1,14. I,v it,,- Ilwill-I
NI 11-h

i.;ousUmptLaa of oxygen by stable organic substances In
natural W*10110. U.,A. SiMpiHISCV. GkffOkhiM. MdhyiaJY
(flydrochem. Materials) 16, 6141(IM).-Oxidation curve
of river waters; during long-term (IFA) days) storage in small
tulwa at 16-20 has a logailthinic shape; it can be e.-
1,1~1 by atraction equathinol the lot order. Withfinte.,
%blidatiml [Kvonlrs very 2111311 and Almost mlqt.. as shown
by nearly straight section of (he curve. Calcd. Nn was
(1-01-O.W. Initial consumption corresponds chictly to .
dation of unstable org. compds.; very stuall and practizi?
const. consumptioa observed after 40-60 days correspunds
to oxidation of stable orc. compds. Available data for
sh,wt-tam storage of sea, water indicate curves analogous to
those for river waters. C4LIcd. Ko was ka than 0.10.
Results obWned In 5-10-day tests can be used only for Me-
tive evaluations. particularly. of content of unstable ors.
Suintanecs. For culen. of 0, usni in oxidation of stable
torg. compds.. storage of over 1-1.5 months is necessary.
Further cipts. are necessary to confinn thi-t. Twrnty-ihree
rpf'Tences. It. Z. Kamich

LA
D"On"sition
,;ILb! chloride volu
Nank S.S.S.R.
ti
first-order rate coasts. k (bra..
bjj"d"d. by titration with KNInO., in sains. of 3% 11A
(with borates) to pit 7.11,4.0, at W ~ 1.11% in
of O.S. O.W. vind U.10 W chloride. anti in the
were: with NaCl. OAXW.I. -. 0.1)(117,
U.00018; KCI 0.0196, 0.0092. MOM. 0.00trt5; CaCl',
0.0112. O.OU71, O.OWI, OX01172; MgCh. 0.0154, O.UO91.
0.0039, O.W128. The values of k vwy gotniewhat in dif-
ferent runs with the man chloride but am consistent-
within the same run, the difference between the obirrved
amt. of HA at a given sup and that calcd. front k
reaushming less than -2-37c. Towards the etul of a run,
time was usually a drop ad the pH by --4).S. Increascof
the comm. of NaCl and KCI to 4 M gave an increase of k
to 0.0370-41.0433. Nine4old incresise of the initial concts.
of HA had no affect on k. With sulfates, the rate is very
newly the same as in the %bwsm of salts. Chlorides
clearly do catalyze the dm)tnpn. of HA. hin much Im-
so than iodides. The reaction is reprewnted by 2 steps,
IIA + 2H + 2CI 211.0 + Cis. anti RA + Cis
:.'I I * + 2C1 + O~. N. Thun

CA
meet W so" ft"s a OW 40semposid" of bydm-
ddwWo mlig". A. A- SkOfiltmv-
AL. Nafik S.S.S.R. 0, liM450940'. d.
preceding abm.-(I) In the presitace al KCI, high pit
t8.4) accelerates The decampa. of HA slightlY as COM-.
Imred with the mte at PH 8.0. At low PH (0.0006--0.4
X HO), no decomspn. takes Place at all. At still higher
acidities (4.01-7.0 JV HCI), decompa. is rapid with evolu.
tion of Cis. (2) Cu nits accelerate the decompa. *. thus,
at PH 7.90. KCI 0416 Ar. Cm - 0. 10, 5o. loo, 5W.
1000 -y/1.. the rate emit. A - 0.013. 0.024, 0.064. 0.113.
0.2M, 0.349, witiseat KCI. Cu - 0 and IW, k - 0.0017
and 0.010, with KCI 0.8 Jf, Cu - 0 and 100. k - O=
RudO.M. Salts of Fe+++ first do *ot affect, then slow-
do" the decompa tims writh KCI 0.2b M. Fe - 0, 10,
W. 1001 WO. low'~A.. I - 0.016. 0.019, 0.010, 0.013,
0.(XM, 0.0m. (3) Of WE. cogapdo., proteins and
Analsto SOWS (Peptu". felstin. albumin, asparawne,
histidine. Illycinit. tyToolve) at 6 mg./I., InhitAt the de.
empri. Carbohydrates (illucomr, lactuse, mcraw, nuil-
tome, statch. agar-mar), stsveinic *vA lactic wid, and
kerosene, at 5 mg./I., either have a slight inhibiting or nt
effect st all. The sUpariatt-down effect is couniftracted by
Cu asks. N. Thou

SKOPINTSEV, B. A. Doc Geolog - Mineralog Sci
Dissertation: "Organic Substance in Natural Water." 11/5/50
Inst of Petroleum, Acad Sci USSR
SO Vechn--ryaya Moskva
Surn 71
----- -

SKOPE4TSEV. B. A., AUTHOR
Science
"Organic substance in water (water humus)."
Reviewed by V. Kononov. Gig. i san. No. 4,, 1952.
Monthly List of Russian Accessions, Library of Congress,
September, 1952. UNCIASSIFIED.

C
* 1.7 5. A.
2. us3R (6oo)
4. Black Sea Sea Water
7- Oxidi7,ability of water in the Black and Azov 3eas. Dokl. 'IN SSSR 87 no. 5,
1952.
of Russian Accessions, LibrarT of Congress, March 1953. Unclassified.
9. Monthly List

USSR/Geophysics - Sea Water -Tan/reb 52
"Optical Characteristics of Organic Matter of Bea,
Waters," B. A. Skopintsev, State Oceanographic Inst
"Iz Ak Nauk SSSR, Ser Geofiz" No 1, PP 57-60
Presents results of measurements of weakening of
light in the violet part of spectrum by various
sea-waters. Comparison of obtained results enables
one to establish content of org dye compda in
water (humic substances of terrigenous origin) in-
portant-for analysis of nature of org matter and
for the characterization of sea water. Submitted
5 Apr 52.
205T4

1. 3KCHDIT";6W) 1. A.
2. U3SH ( 6rjr) )
4. Radioactive Tracers
7. Study of processes in bodies of water with the aid of tagged ataris, ?riroda 42, No.
0~
3, 1953-
9. Monthly List of Russian Accessions, Library of Congress, May -1953. Unclassified.

USER/Biology Marine microbiology
Oard 1/3. Pub. 86 - 13/34
Authors Skopintsev,, B. A.,, Dr. of Chem. See
Title The role of chemosynthesizing bacteria in the formation of an organic
substance in natural waters
Periodical Priroda 1,, 88-91., Jan 1954
Abstract i The basic and auxiliary sources instrumental in the formation of
organic substances in natural waters (rivers, lakes, seas,,etc).q
are discussed. The role of chemosynthesizing bacteria,, in the
formation of organic substances in natural waters, is explained.
It is shoi-m that chemosynthesizing autotrophic colorless microorganisms,
like green plants and seaweeds, are capable of synthesizing-organic;
substances from carbon and carbon dic3dde by utilizing solar energy
instead of mWgen. Ei0it references: 6-USSR and 2-USA (19;~7-1953)-
Table.
Institution : Acad. of Sc. USSR., Sea-Hydrophysics Institute
Submitted :

P
icill investigatil)n c:itne out m
Resulis of the hydindiew d
a 13tr ts
th, _clt Sett. B I S' "I I anti F. A. Cutiia. Trwfy
t S,,,mrw!
5, 71-JJ~'I`f 19,55). ral 10:! F cil'-r H-S' *r tJ -if
Ibc Lavie are-tirurly Wnll kt 1 1,V
for W4 wheti ~Alnj?t~.,3 iirc oloilltwd A di~ioreut 13:3*1CAS
frOw itli. wilv! ilepol, flw, diiLlibutfurl of IfiS
Illul 0 Ilivollgh 0'.. rwile 5ttutulu L4 iii)t Urlitotin olving to
wrtica.] -moVemetitS of tile water. Tile itv. 112S C011tent
Mid tile CUM, of d(Matfull obtahicd in I Ma are -
to thc "gullol Yriltios nNitinfIl in 10.51 and
19111, -7. 130ow ,)(X) Ill, it curcd-,~tiotl i,
the lullb. of litS and th't-, miti, Apportlittly unilt urk, Luc
mmits (I the ~-ame prousi. HIS b vviiisly formod : t tile
buUmil, but some f6cmation lakes place in above
3010 m. Out. of-74 examd, a-uuplct~ taken from various
duptln, only , -ri izonlaitied ~iuljlw5 and thioiuMies. - In
;t!s the vivit. did not excviA 1. to mg./1000 cc. Only
inost cas
4 sampt". contained I ~00-2..30 ing./luslo cc, The built of
t1 ownlyard illerease in
3e Salts GWIAAS W
the anas. of the salts,jvgs jotuid. Tli,:y form only a fci% j
of the total Suln Of lg-bt~aring coallid-.3. ~- 'rile Suffaies illc~eazie
down tD M-1000 in. BJw this r1iptb - decreased amts..
%vere nd Ili the iitajotity of cases.- , Tile sulfate-chlotide
Jou
c(xff, vaIttei i cacti tlttoil, mix. ill tlle tmpCr strata. Theyatir..
hirger t1han the, C-urr'nPund valyw.,-, of fl!: cm
he lilglicr C1 welLA the uppl:~r tvamri uf the 131a k Sca
t
,
values decline yradt-:01-y with dqpth. 'I'llcy are CO
The list.
at in. and ilu," ducline agabl, reaebing tilcir lmvest
elo~r- to_tbe 1:6-ttow, The Uheorci~k~Avnt. of fLS calcd. on
iwar bottulu-5 and ' Ueiz.
the bm,~ of the sulrme~, of fl!c-
Swept ill by flie, Bospbotus i,~ sutrovilat larger thall tb~-:
ably.due to the.S,
actual qmt*The dIHerevo2 most prob,
ueed of bacteria and interactl0l betweeii S -and Fe compds.
oil
moll

VDYU&n*s of organic substances In natural watirs.
A A-
"a n
L. P. Krylova. rrudy Vierayus. Ci
4
MOV ERO
-
.
A
1 a d.Sawk S.S.S.R. 6, 38-15(1055).-Expts.
were performed to det. the degree of decautprt. of org.
substances in natural waters. Org. C measured by the
dichromate method (C.4. 44, 3181e) was used as an index. '1~

'
A "wattr humus" in the form of pLinktonle org isms was
added to 15-1. bottles coutg. river water. Atthe
endofIGO

2=1 contents bad been reduced by 99%. of which
4:r
f
orm of sot, ors. sub-
percentage was in the
stances, the majority being transformed Into inorg. C.
Colored sot. substances disappeared in the presence of fight
CQW7iUUtly With the formation Of 4 brown ppt.
Lola H. Reshctko

it,& ~nk iirboin of riVers at the terminal stage of the
r rio4. B. A. Skopintsev. Gidrokkim. Alaterialy
1955).-U-co H-9-dapacity, color intensity,
23
an C eonteni*iii it thefr lowest at the tefhIinal'sta~je of the
i.winterperiod. The same is true of the terminal stage of the
summer period as indicated by the closeness of the O-con-
suming capacity/org. C content ratios of both periods.

5

3;p

_~a~quecu_q
4organic subs-a c
L. Upt"cal PRFJN_~f
of surfac&-walws OfAr -opintsev aud L.~P.
laud. B. Ai S.
R
11014'r 113. 2M, 22-JUM (f. C.A.
y o iA I t I i k ii i b y,-fUscolored vvat
alway-, grew wit(i dk-"cliflc ill wavet, ktigth; tile peiltest
;1hs(;rjlt1.1;l -with Aoki Q6 ing); iti thLr(!d part.of
;
l
dif-
dl
h
Ii
b
f N
i
2
5
l
,
.
~ a & t. (l
-cm. tu
n a
e,
t
ar
e sp
!~
pa
y
bA%vull du! cdor of t1to wattr and,l,hl: sigmiricallce of coeff.
or weahtahig of light hi Lit, vitilet part W1 the s Ull
PMtr 11,
1.
,
Alblwl dew. , rcllut5 t1w. vuntcat ut calur N litilnus 1
.

-C cfy-ff~ I lit
thearg. C cmtent (wal achid 'dll~; 0) and th - of fig
absorptitm ill th~ viulet part of qoctmwn ivaakt~ yNtial
ar)prcc;:.-i icat inadeqnaw for cutrwly, citg, thi: &enoi I coa-
tout of g, su!)Aaiia:.,~ lit sit
i;r rface w3t-.-c Tim! prcdowitiance
'4 (alvic acid in the aq. ht-T-nit.4 of terickEmlous fai Cali
_ghl 6
-
I . .
1
hri
MA, -71 j1=a-

SKOPINTSEV, B.A.; GUBIN, V.A.
StIlfates in the Black Sea water. Gidrokhim. mat. 25:16-27 155.
(MLRA 9:6)
l.Morskoy gidrofizicheakir institut Akademii nauk SSSR.
(Black Sea--Sulfates)

L~) I-
T N T- V 14) -ZE
A,
USSR/Cosm-3chemistry - Geochemistry. Hydr-ocb,~m-1.j~t?:?f., T'
Abet Journal: Referat Zhur - Khimiya, N,:y 19, 1956, 61350
Author: Skypintsev B A. Krylawa, L. P.
Institution; None
Title: 11emoval of Organic Matter by th:-~' L~36~Sast- -,f the Soviet Union
Original
Periodical: Dokl. AN SSSR, 1955, 105, No 4, 70-773
Abstract:
On the basis of monthly data cf -t-Ak---ng 1ritc, ac~:ount
water discharge of river and by me-atia ~,f -f r&461~ cf oxygen
of permanganate oxidability in acid m&.1iwn ' to organic C, there
has been computed outflow of organic matter at the given point of
riverY for each month and summatively f,:x the vt-z;ar.. !m the rivers
Sev. Dvina, Neva, Dnepr., Don, Kubg--,. Volga,. Kuzra, Lena, W. Mag-
nitude of outflow of organic mattl!x by amount of
water discharge of river and czinditions of its
basin. In the case of plain rilrex t~as-fns ---f zaae of excessive
humidification, highest c=central.Laa ---' --z6gqni,~ r-atter is
Card 1/2
L - - --------------------

SKOPIVTSLFV, B.A.
Radox potential of the Black Sea water. DokI. AN SSS'~' 108 no#~6:1120-
1123 Ja '56. (MLBA 9:10)
1. Morskov gidrofizichaskiy institut Akademil nauk SsSR. Predistavlana
Rkademikom A.N. Frumkinym.
(Black Sept-Oceianographic resenrch)

7 5
--------- -- -
V'argidahiat"Wflt the watemof th't y.ofRip-
(maxine HY&Gpl~ys. ItI57'.
Aug4jrLer V
05-70(19,57).-The changm of the analp,-s over the years.
presented in taWes, for the 0-uptake by an oxiclation
with XMaO4. ard for the abeAuption of Ught of 436 m~ in
RZ that had ken filicred througfi -a - gltrr with pares of
0.85 j. diam. This latter clem. furiiishes a -neas-um for the
buly US.fr-=13g co"tituents ir the sea. W.

SKOPINTSEV, B.A.; KARPOV, A.Y.
'q ~-` 9MOWAft
Conditions for conservation and further determination of sulfides
in natural waters. Gidrokhim. mat. 26:230-236 157. (KM 10:8)
1. Morskoy gidrofizicheskiy institut Akademii nauk SSSR, Moskva.
(Sulfides) '(Water)

SKOPINTSEV, B.A.
- ~-
Determining the "colloidal" fraction of organic matter in natural
waters. Gidrokhim. mat. 26--243-245 '57. (MIRA 10:8)
1. Korskoy gidrofizicheskiy institut Almdemil nauk SSSE~ Moskva.
(Colloids) (Water---Analyais) (Organic mtter)

SKDPDITSEV - A*_,_ ~ . ,
Study of the oxidntion-roduction Dotentinle of the Black Sen,
Gidrol,him. mnt. 27:21-36 '57. (MIRA 11:4)
1. Morskoy gldrofizichmakiy inatitut All SSSR, Moskvm.
(BInck Sea-Vater-Analyais)

SKOPINTSRV, B.A.; VOROBITEVA, R.V.; SHTUKOVSKAYA, L.A.
Comi)lexometric method for the determination of calcium and the sum
of calcium and magnesium in sea water. Gidrokhim, mat. 27:146-151
157. (MIRA 11.4)
1. Morskoy gidrofizicheakiy institut All SSSR, Moskva.
(Seawater--Analysis)

AUTHORS3 Gubin, F. A., 20-119-1-33/52
Voroblyeva, R. V., Vershinina, 0. A.
TITLE: The Composition of the Salts of the Chernoye Sea (Black Sea)
(Solevoy sostav vody Chernogo morya)
PERIODICAL: Doklady Akademii Nauk SSSR, 1958, Vol. 119, Nr 1,
pp. 121-124 (USSR)
ABSTRACT: In October 1954 and in June 1955 water samples were taken at
5 points from all depths in the open part of the sea near the
43th degree north latitude. The chlorine content was determin-
ed argentometrically, the alkalinity by direct titratio- with
HC1, the sulfates by the weight method and Ca as well as Mg
complexometrice.lly. Table 1 gives the average quantities of
this determination. The highest content deviations of
individual components at the same depths of all 5 places
from the average attained 4%, which was characteristic of the
upper layer (0-150 m). Farther down the deviations are less
than 1~-, except Ca and alkalinity. The absolute content of
all salt components in the Chernoye Sea (Black Sea) is
smaller than in the ocean, except the alkalinity. The chlorine
Card 1/4 content increases from the surface to the bottom. The change

The Composition of the Salts of the Chernoye Sea (Black Sea) 20-119-1-33/52
of other ions at the vertical is represented in table 2 as
ratio to the chlrrine content. In this manner the contents
are compared with -those of the oceans, where the latter are
constant (ref. 1). The elevated values of the cited
coefficients in the upper 200 m of the Chernoye Sea can be
explained by a comparatively higher influence of the waters
of the flow of the rivers for the higher values of these
coefficients than they are characteristic for the ocean. The
changes of the ratios
so4 HCO
C1 060) and - are connected with the biochemical
and biological processes occurring in the Chernoye Seat a)
the reduction of SO 2- at the bottom of the sea with a
4
simultaneous formation of hydrogen sulfide and HCO b) the
3
oxidation of H2S in an intermediary zone (from 125-150 m to
250-300 m) under formation of sulfates and a corresponding
decrease in HCO! (ref. 2). A marked change of Ca2+ in the
water near the bottom was not observed. Table 3 gives the
calculated average composition of the water in the Chernoye
Card 2/4 Sea. Little difference in comparison with reference 4 is to

The Composition of the Salts of the Che.-t-noye Sea (Black Sea) 20-119-1-33/52
Ca 2+ annualy brought into the Chernoye Sea by the rivers.
Such a chemogeneous carbonate-sedimentation mainly takes
place in the region near the coast (references 3,5). Then
the authors discuss the statements of reference 8 and state
that for the displacement of a water layer of 17 m thickness
about 130 years would be necessary, which disproves the
ab,ove-mentioned statements. There are 3 tables and 8
references, 8 of which are Soviet.
ASSOCIATION: Morskoy gidrofizicheskiy institut Akademii nauk SSSR
(Marine Hydrophysical Institute AS USSR)
PRESENTED: July 13, 1957, by N. M. Strakhov, Member, Academy of
I Sciences, USSR
SUBMITTED: May 12, 1957
ILI
Card 4/4

a-KOFEMIEV, B. A.
.-I
"Tl.~- Qr-anl-c Shibstancc,~~ clf Sea-Water,"
in'
Ccn~;. yore- C I tY, 31 kqc, Il Sep
Rarine HY-Jrophy3ical Acad. 3c.)

KRYLOVA, L.P.; SKOPINTSEV, B.A.
,&mount of organic carbon in river and lake waters of the Moscow
area and large rivers of the Soviet Union. Gidrokhim.,-ot. 28:28-44
159. (MIRA 12:9)
1. Laboratoriya sanitarm-epidemiologicheekoy stantaii Chetvertogo
glavnogo urpavlenlya pri Ifinisteretve zdravookhraneniya SSSR,
g.Moalrva.
(carbon) (water--Composition) (Limnology)

DTSHKO, T.V.; SKOPINTSEV, B.A.
A?Iount of organic nitrogen in river and lake waters of the Moscow
area and large rivers of the Soviet Union. Gidrokbim.,,Iat. 28:
45-58 159. (MIRA 12:9)
1. Laboratprlys: sanitarn-o-spidemiologicheakoy stantaii Chetvertogo
glarnogo-tipravlentya pri Ministerstve zdravockhranentypa SSSR,
9.14oekva.
(Nitrogen) (Water-Composition) (Li"nology)

-- SKOPI14TSEVY B.A.
Organic matter in sea water. Trudy MGI 190?20 060. (MIU 14M
(Sea water-Composition) (Organic matter)
I
k

SKOPINT~EV., B.A.; POPOVA, T.P.
Some results of iron,, manganese, and copper determination in the
water of the Black Sea. Trudy 191 19:2-1-30 160. (MM 14:7)
(Black Sea--gea water-Composition) (Trace elements)

SKCPINTSEV, B.A.; TIMOFMVA, S.N.
Concentration of organic carbon in waters of the northeastern
part of the Atlantic Ocean. DokI.AN SSSR 133 no.3:677-679
11 160. (MIR& 13;7)
1. Morskoy gidrofisichaskiy institut Akademii nauk SSSR.
Predstavleno eked. D.I.Shcherbakovym.
(Atlantic Ocean--Carbon)

SKOPIIITSEV, B.A.; TIMOPEYEVA, 3.11.
Organic carbon in watera 6f the northern part of the Black Sea.
Dokl, AN SSSR 134 no-3:688-690 S 160. (MIRA 13:9)
1. Morskoy gidrofizicheakiy institut Akademii nauk SSSR. Predstavleno
akad. N.M. Strakhovym.
(Black Sea-Organic matter)

SKOPINTSEN, B.A.; KARPOV, A.V.; VMSHININA, O.A.
Experimental study of hydrogen sulfide formation and oxidation
taking as an example the Black Sea. Gidrokbim. mat. 3D.127-141
161* (MIRA 14:3)
1. Morskoy gidrofizicheski7 institut Akademii nauk OSSR9 g. Lyublinoy
Moskovskaya oblast'.
(Black Sea-Hydrogen sulfide)

SKOPINTSEV, B.A.; T11,10FEYEEVA, S.N.
Using the L. P. Krylova's method of dry combustion in determining
the organic carbon in sea water. Gidrokhim. mat. 32:153-164 161.
- (MIRA 14:6)
1. Morskoy gidrofizicheskiy inatitut AN SSSR, Lyublino,
Moskovskaya oblast'.
(Water-Analysis)
(carbon)
(Pyrolysis)

SKOPINTSEV, B~A.~ SMIRNOV, E.V.
Hydrogen sulfide distribution in the Black Sea in the autumn
of 1960. Okeanologila 2 no.3tIa9-434 162. (MIRA 15!7)
1. Chernomorskoye otdeleniye Morskogo gidrofizicheskogo
instituta AN USSR.
(Black Sea-Hydrogen sulfide)

SKOPINTSEV, B. A.
Biochemical cons=ption of oxygen in the waters of the
northern part of the Atlantic Ocean. Okeanologiia 2 no.6:
1009-1013 162. (MIRA 17t2)
1. Morskoy gidrofizicheskiy institut AN UkrSSR.

SKOPINTSEV, B.A,
Recent works on the chemistry of the seal Trudy MGI 25:82-109
'62-. (MIRA 15:2)
(Sea water-Composition)

SK0FINTS,EV_,_13.jV.; TIIM0FEYEVA, S.N.
Concentration of organic carton in waters of the Baltic and North
Seas and the subtropical and tropical regions of the North jitlantic.
Trudy MGI 25:110-117 '62. (MIRA' 15:2)
(Baltic Sea--Organic matter) (North Sea--Organic matter)
(Atlantic Ocean--Organic matter)

SKOPINTSEV, B.A.; ZHAVORONEINA, V,K.
Results of the determination of dissolved oxygen in waters of the
subtropical and tr3pical regions of the North Atlantic during
Aupust-Uctober 1959. Trudy MGI 25:118-129 '62. (MIRA 15:2)
(Atlantic Ocean--Sea water--Oxygen content)

SKOPHITSEV, B. A.
Calculations of formation and oxidation of organic matter in sea water
report submitted for the l3th General Assembly, IUGG (Oceanography) Berkeley,
California, 1.9-31 Aug 63

-SINYUKGV, V.V.; SKOPINTSEV, B.A.
Use of a new pnotoelectric colorimeter for the determination of bio-
genetic elements und*r field work conditions. Okeanologiia 3 no.1:127-
136 163. (MIRA 17:2)
1. Morskoy gidrofizicheskiy institut AN UkrSSR.

--SK,OP.I,NTSEV, B.A.; KARPOV, A.V.; TIVIOFEYEVA, S.N.
Using an autoclave to determine the mineralization of organic matter
in natural waters. Gidrokhim. mat. 35:183-199 163. NIRA 16:7)
1. Morskoy-gidrofizicheskiy institut, AN USSR.
(Water--Composition) (Organic matter)

SKOPINTSEV, B.A.; LEDOVSKOY, M.S.
Dissolved oxygen in the water of the Black Sen during 1959-1960,
Okennologiia 3 no.6:1004-1016 163. (MIRA 17:4)
1. Chernomorskoye otdeleniye Morskogo gidrofizicheskogo instituta
AN UkrSSR.

14" ,1 T.
Ko p N'I'
trace elem-
1; 1 C a Is-:1' -.n t
Jla 4 no.2-205-212 164.
in Okeanolo, - (MTRA 17:5)
-fk
rokcy y instituf Ali i rSSR.

SKOVINT,')EV, B.-A.; POPOVA, 1'. P.
Accumulation of manganese in the waters of hydrogen sulfide
basins as revealed by a study in the Black Sea. Trudy GIN
no. 97:165-181 164. (MIRA 17:5)

KOMSIUK01", dokcor fiz.-utat. nauk, otir. red.; SKOPIDITTEV,
-khim. rAuk, otv. red.; KUI 'KOVSKAYA, N.S.,
red
[Fydrophysical and hydrochemical studies; an inte-rdepart-
mental Reptiblie-wide coIlection] Gidrofizicheskie i g1dro-
kh4micheskie issledovaniia; mezhvedomstveruqi respliblikan-
Skii sbornik. Kiev, Naukova duinka, 1965, 137 p.
(MLU 18z5)
1. Akodeir..iya nank URS11, Kiev.

UT) Puss I BOOK xxpwrr~ 30T/2131
Akadmalya nauk 333R. Norskoy gldrorizichookiy Institut
Torm"ra morya. ShIaLlys norya (Thorwal Regis of the Sea. Chemistry
0 : I
of the Sea) Moscow, AM SSSR. 1958. 145 Y* (Seri a 'to I Trudy.
too 13) Er. to slip Inserted. 1,300 copies printed.
Reap. JK.L;A.O: Kolsonikov, Doctor of Physical and Mathematical
3ol"a 21 of Publishing Rouse: L.X. Nikolayev&; Tech. Ed.:
H.F. Tegorova.
PURPOS z This an'llection of articles In Intended for geophysicists,
hyMphgIcists, and oceanographers.
COVERAOX: these articles deal with problems in the physics and chem-
Istry of sea water. Individual papers treat the turbulent thermal
conductivity and beat OAchangs in sea waters the pulsation@ In *J-r
tom"ra= t the salinity of the Black Sea, the determination of
salaium. magnesium, and copper in sea water. and the determination
of so"um in atmospheric precipitates. FIgur*a, tables. and gra he
aecompany the articles. There are 121 references: 92 Soviet, Is
---------- JNULIAAh- 8 German. 2 Prwnh. and I Swedish.
IIWXGVR. N.1- Son-Stationary lAquld lxchange Between Two Roser-
Tel" of DLfferomt Temperatures 78
P.A. -, H.V. and O.A. Vershinl-na.
Oubin
Main Componects In the Salt Composition of Black Sea Water and
Problome or Water Clmulatior. S9
Skoplateav_.B.A. A Study of the Composition of Suspended Sub-
-st"Ges mod GslcrLe~Organic Compounds In the Azov and Black Seas 113
"Lateov, B.A-, and V.V. Kabanov. An Integrated Method for
batersiming Calcium and Xagnsolua In Sea Weters 130
?Lkhonov, rK_ and V.K. Zh&ToLr'*`okin&- The Problem of Dater-
mining Cop"r In Sea Water 137
;1m.orwwxjns* ?.I., and V.K. Zhat-aronkina. Determination or
Sm"um in Air Precipitates by the Spectral Method 143
ATAILUUA: Library of Congress
Molars
5 11-59

Papers submitted for the lDth P.Cric SOL-m- CmWrls-. Ronnie", g'-%" 21 k't-
6 Sop 1961.
drine ffydmpbyOic. Institute, Acadey of Sciences VWR
MLzer*J-Imtion of crgmic substances of dead
plankton under sn"roble wndLtlms* (Section VII.C.1)
akrmrM D A Institute of Ocewolog7 - "S=e regularities concerning
son.iY-JAributica of ebemIaLl rhmracteri.tLas In the usters of
the central part of the PscIfLc4 (See.Lon VII.C.1)
-MEXQY~J6_A~ All-Unica SciemtLfLe Research Institute of Ytarl- Fishing
and Oceanography - "Subcarime I.Severjwkal - a cov =eans for marine
fishery Investigations" (section rn.c.4)
r~OVA!68. X., In. itute of OccesmoicE7 - "Th-- distributim of deep-oea
to-mb the pool fie in omm.cti.m etb food conditions"
(Section III C)
309CM-Tu"K Institute of BE.Icer of Reservoirs, Acsd~y of Sciences
U= -2;Tha mvb~tno illu-ticattm and the primar7 production of pho-o-
s"the 6 In the B a~ (Section rtrx.4) -
,S=VWI~ D~K, Institute of Bt.-'orj of Reservoirs, Acdeny of qci.re's
MW ~"Tha preblen of BerInglem continental cowcction In the cmitho-
g~.gmphio elucidation" (so 'tion rri.A.S.a)
and -1011MY-7-k-1--tit-te of 0"=ol.a - "-,he =-ure.
et currents tth the of anchor buoys
(imeth.d., Ppo'.Z%l, r,.ult.)"(3-t1.n 'ITI.B.5)
TARETEV, B. A FCHIC-LC7, A. V., Institute of Oconnoloa - "reastrophic
currents 1. the Antarctic sector of the Pacific (Soctlcm 71T.D.1)
Tm-arcrf. V. I., Institute a rGeloa - "Utv data on the tectonic. of
southern )Z--hatk." (3.ctL.. 'M.C)
.TLMM=.-D~D.,Imntltuto of Ubnology - "The othmologle stud7 of the
peoples of Ocesais in the =1" (rkctjon rI.3)
7~,E ~10. B, Institute of Ocesnoloa, "Features of evolution 12 the
botton Upog-Phy of the P&.1fic OT'sa, (S-ctim
VA3m V. A., Institute a.- C,olcGy "C,at.ceoun floras of the
effla c~ii~B the = as a basis for the subdivision of continental
deposits of tiat &&e- (Sective, M.C)
YMXBA=1A,-r-r-, Institute or oc.saoiocy - "C,.rr,;hic&l distribution
of sbyv"I bottom ramn. ona tbc, prable of vertical m.n.tIon"
(Section M.C)
Hose- StAt
9 a University, Gw,7.1,hlc&l F"ult7 -
f the s==er consoc. I. cont AAn~' (Scott.. VI.C)
M., test Ltut~ of (;oolcgy - "The Island arches =tl the p-righerLc
areas In the western belt of the Pacific belt" (3ection ~ir.C)
mlmmy.A, * T.-D., Y. T-rnutLt~te of Earth r.~Y.tcs
L=L 0. To. ScImidt - "S-o NusibIlLtica in interpretation of surlue
-ca of the Pacific" (5,ectLen M.C.2)
-%kHS=, A. L.,.-InstLtwtc of GoloEy - "The tcateale =p of L'urast."
U.~~ctian YII.C)
L~nL.07.d r.re.t,/
Ac'4--.:, ie.1 3. N. r- . "Som pmbl-s im~.lvcd ~tth ~d itu,U-
I. southeast A.W (Zectic., III.A.-, )
-74144,zv, A3,t. DIr"t-, Ceo-,.phical 11-.. 5t.te
U.Lveroi 'F - "The pb7aLco-r~orruphlcml tcnntlcn of the OdYhalin =J
the Xuril IdLaoda" (S-tt'. VEX)
G-l.r_e - "(h the relsti... b,t--n
t1. Upper Cretaceous and r1-- of Au.tmli., N-
=4 SUrASIa' (r,. ctLon IrI.A)
=11111ck,:~_- A., end F:IA-V;A, Z. A, joatjt.t~ of 0.c-.I.rj - "General
re -ularities
Ln the quantLtat.11- md q-litatilve dt3tributtcn of the
I
,.tt- fa- 1. the Pacific"
=AROVA, M~U-,A, 3. ~;,, 1-~it.t~ f Zncl.a, - "7~,
mmudy In method-o of pri-rary pr-ucti- ta--atLFAtion of freah-t-,r
plankton" (,'I-c-L,n IrI.C)
_M1PWX1,-M, A.._V,, T.stitut., of Cy-.1.CD, - "Cytophy.1.1~el'.l ir-'ticutloc,
of to=;~craturo ad3PtMt1Dn3 of in-,ce-bratmm in the mor4h-tern ar,a of
the Pacific Oce-, (r,.cti.a 111.0
-=1AGO, A. V., Institute of Geography - "Outlines of southern ccemn
gecmorphcl.gj~ (Sneti.m. V-,T.D.1)

SKOPINTSYN, B.A.; IVAIT)V, K.I.
Use of photometric measurements in determining ounpended particles and
colored hunic compounds in sea water. Trudy GOIN no.22:113-131 ' 52.
(MIRA 12:1)
(Sea water-knalysis) (Photometry)

DRACHEY, brof.; RAZUMO~, A..S.; 5XOPINTSEV, B.A..; KABANOV, N.M.;
B',=-VICH, S.V.; SOSUNOVA, I.N.; GOWBEVA,, M.T..; BRUK, Te.S.;
MOGIhEV.~KIT, Ts.A..;* RliTkW, M.A.; XOI~~, Lje~.; ANOKHIN,' V.L.;.
BILINKINA" )OCYNIKOV. Te.B., Yed..; B41CHIKOVA, lix.S..,
teklin.red,
(Methods of at-tidying waters from the -point of view of aanitationj
Priemy sanitarnogo izucheniia vodoemov. Pod red. S.M.Drachava.
Moskva, Gos.izd-vo med.lit-ry, 1960. 354 p.
(MIRA 13:11)
tWater--Analysis)

ACC NRi
XL'603 5 087 SOURCE COM: UR/3095A6/035/000/0071/0(Y78
A. A.
ORG: none f
TITLE: Distribution of oxygen and phosphates in waters of the Lomono3ov Current
SOURCE: AN UkrSSR. Morskoy gidrofizicheskiy institut'. Trudy, V. 35p 1966.
GidrofizJ.choskiyo i gidrokhimichoskiyo issladovaniya tropichookoy zony Atlantiki
(Hydrophysical and hydrochemical research in the tropical zone of the Atlantic), 71-
78
TOPIC TAGSt ocean current, o;Wgen, phosphate, research ship.) 0-r-Z'X-'
ABSTRACT: This paper in a summary of observation:; on content of o~Wgon and phos-
phates in the equatorial belt of the Lorionoso-w- Current, collected during e)Teditions
of the scientific research ships Mikhail Lomonosov (SSSR) in 1962 and 1964, the
Zvezda (SSSR) in 1963L and the Crawford (U.S.A.) in 1963. Investigations were
carried out between 5 and 450 W. Long. It was found that the surface layer, to a
depth of 50 m in the western part of the ocean and to 30 M in the eastern part,
remains homogeneous. Oxygen content is 4.6 cc/liter, and phosphate content is about
5 mg P/d. Below this zone, to a depth of 80-100 m, south of 20 to 4-50 S. Lat.
and north of 20 to 5-70 N. Lat.0 the oxygen content docreasoo sharply to 2,5-3,0
Card

ACC NR, AT6035087
cc/liter, and the phosphate content increases to 35-50 n9 pIM3. The greatest
vertical change is observed east of the 30th meridian. In water along the equator
(20 south to 20 north) only insignificant changes in either oxygen or phosphate are
observed in the top 200-m layer between 5-and 350 W. Long. Here the oxygen content
averages 1.2 ccAiter, and the phosphate content averages 10 mg P/m3. A series of
maps and tables is provided to illustrate the variations in ox7gen and phosphate
content. The waters in the Lomonosov Current prove to have more oxygen and less
phosphate than the waters in the belt of trade winds. It is concluded that the
waters in this zone affect the distribution of oxygen and phosphate in the equatori
zone of the Atlantic to depths of 800-1000 m. Orig. art. has: 1+ figures and 3
tables.
SUB CODE: 08/ SUBM DATE: none/ ORIG REF: 008/ OTH W: 006
C,rd 2/2

SEIV, B,A. ; SMIRNOV, E.V.
Hydrogen s--,ilfid~,- in the abyssal waters of tho operi part of
the Black Sea. Okeanologiia 5 no.6:969-98,0 165.
(MW 19:1)
1. Morskoy gidrofizicheskiy InstituL AN IjkrSSR, Sevastopol'.
Stibml.Ued March 10, 1965.

SKOPINTSEV, B.L.; KARPOV, &.V.; VERSHIIIIIIA, O.A.
Studying the dynamics of some sulfur coupounds in the Black
Sea under experimental conditions. Trudy I-GI 16:89-111 159.
(14IRA 13:5)
(Black Sea--Sulfur compounds)

ACC-14-AN034006 SOURCE CODE: UR/0213/66/006/005/0799/0806
AUTHOR: Skopintsev, B. A.; Romenskaya, N. N.; Smirnov, E. V.
ORG: Marine Hydrophysical Institute, AN UkrSSR (Morskoy gidrofizicheakiy institut
AN UkrSSR)
TITLE: New determinations of -the oxidation-reduction potential in Black Sea waters
SOURCE: Okeanologlya, v. 6, no. 5, 1966, 799-806
AW_4v%~
TOPIC TAGS: hydrography. hydrographic research, oxidation reduction OatwwtAwA,
electrometrr) mAaatten=z:Fc Oc"-%3 0-rk'~ 7
ABSTRACT: The article deals with the determination of the oxidation-reduction
potential in Black Sea waters in August-September 1964 by means of electrometric
measurements in large-mouth glass jars. Average values of the patential change
rapidly from positive values in the upper layer (+413 mv) to 1--.ilO mv in the inter-
mediate water layer, and then gradually decrease with depth to -0.172 mv. The
results of the calculation of the oxidation-reduction potential performed using the
equation for the hydrogen sulphide-sulphur equilibrium system were close to those
obtained in the.sea. Orig. art. has: 4 tables.
SUB CODE: 08/ SUBM DATE: 06Apr66/ ORIG REF: 014
Card 1/1 UDC;_ 551.464,1;543.242(266.5

GV
ACC NRI AP6020983 (1VJ SOURCE COT-)-,r,,-!--IJR/0213/66/006/003/0441/0450
AUTHOR: Skopintsev, B. A.
ORG: Marine Hy drophysical Institute, AN UkrSSR (Morskoy gidrofizicheskiy
institut AN USSR)
TITLE: Some considerations of the distribution and state of organic matter in
ocean water
SOURCE: Okeanologiya, v. 6, no. 3, 1966, 441-450
TOPIC TAGS- oceanography, ocean property, ocean zooplankton, water humus
phytoplankton, organic matter, sea water N/
ABSTRACT: The total organic matter content of the Aclantic Ocean water,
determined at the Marine Hydrophysical Institute, practically coificides with that
found by othei investigators in the Pacific and Ind-*.an Oceans, but considerably
exceeds the values determined in the' Atlantic Ocean and the Nerwegian Sea by
11/2
2/2

1--L 3316Z-66 EWT(l) GW
i ACC NRi Ap6ol4281 SOURCE CODE: UR/0213/66/oo6/002/0251/026o
AUTHOR: Sk ntsev, B. 2_~
Ti7p S.~N.; Vershinina, 0. A.
/3
iORG: Marine drophysics Institute$AN UkrSSR (Morskoy gidrofizicheskiy instJtut
L_~Y
1 AN
~TITLE: Organic carbon in the waters near the equatorial and southern parts of the
;Atlantic Ocean and in the Mediterranean Sea
1 1 ";_
ISOURCE: Okeanologiya, v. 6, no. 2, 1966, 251-26o
I
ITOPIC TAGS: ocean property, oceanographic expedition,
carbon
ABSTRACT: Observational data carried_put during the 12th and 15th cruis es of the
research vessel "Mikhail Loja9nQAom!LAW"1962-1964 have been used for studies of the
total and suspended organic carbon and of the permanganate oxidizability in alkaline
lor neutral media. It has been determined that the organic carbon content in the
Isouthern and northern parts of the Atlantic Ocean and in the Mediterranean Sea is
jalmost the same, averaging 1.5 mg/l for the Atlantic Ocean. The carbon content shows
la 1.5 decrease from the surface down to 3000 m. A 1.3 decrease is observed from the
Isurface down to 150 m. The suspended carbon content also decreases with depth; it
!comprises ,u 3-9% of the total carbon. Permanganate oxidizability diminishes approxi-
mately by 2 from the surface down.to 3000 m. The oxidizability/organic carbon ratio
Card 1_ 12 nC. 551-464-626(26919631264)

SKOPINTSSV, D. G.
Neurodynamic changes In the period of acuity in peptic ulcer.
Sovet. med. 16 no-5:15-17 MRY 1952, (CLML 22:2)
1. Moscow.

-~l"DpIlllTSZl"'Al;
-1 .1 S. I.
"Kon.,;er.rat-siyu ! retavruts-,ya pr(-~-lrvAov lz motiLL'u, tkariey i bumagi V
- I I
Cjosudarjt-venno,,,i llstorl~.'nleskrlm Rlvlzee.
report submitted for 7-th Intl Conir, kithropological e.-, Ethnological Sciences,
Moscow, 3-10 Aug 64.

ism/Electricity - Induction Motors MY 52
.Mining - MsLchinery
"Synchronization of Electric Induction Motors at Mines
of the "Stalinugol"' Combine," Engr K. 1. Skopkin,.
"Stalinusoll" Combine
"Elektrichestvo" No 5, PP 51-54
Discusses operating experience and engineering and
economic effect of large-scale synchronization of
Induction motors at mines of "Stalinugoll" Combine by
DAG system (synchronization with pha6e-vound rotor
proposed by,USSE engrs I. G. Dankovtoev.,
N. Afanaslyev, and B. K- GureTich, -Certificate
of Authorship No 71956, 1947). From introduction
Of system in 1948 to end of 1951 the combine syn-
chronized 146 motors with total PoVer of 34,883
kv. Submitted 12 Sep 51.
24oT49.

SKOPKOVA, K.
SKO P /?0 V141 4.
SKOPKCVA..
dIKSA,
BAZANT., V.;
J.;
M. "Teeth Caries and Nutrition of Children and Teen-Agers
in the Sedicany, Rakovnik, and Prague Area During the '-.ears 1948 and 1949.11 p. 140.
(Casovis Kelaru Ceskych. Vol. 93, no. 6, Feb. 1954- Praha).
East Eurooean Vol. 3, No. 6 4
30; Monthly List of W12W Adeessions/ Library of Congress, June 1951, Uncl.

SKC-PKOVA, M.
FSfect of food consurption on trends in the food industry. p.232.
(Prumysl Potravin) Vol. 8, No. 15, 1057, Praha, Czechoslovakia)
SO: Monthly List of East European Accessions (EEAL) LC. Vol. 6, Nc. 9, Sept. 1957. Uncl.

m
SKOPOV, V.F., inzh.; SHUROV, O.L., inzh.
Use of cold asphalt mastic in constructLone Energo strois no,32t23-
25 '62, (MM 16.5)
1. Stroitel'stvo Beloyarskoy atomnoy elektrostantsii imeni-Kurcha-
tova tresta "Uralenervostroy".

SKOPMOV, A.G.; SKRYABDJ, K.I., akademik.
Intraspecific behavior of insects living in grcnm societies. Dokl.AN SMR 93
no.1:205-208 N 153. (MTRA 6:10)
1. Akademiya nauk SSSR (for Skryabin). 2. Gosudaratvennyy estestvenno-nauch*7
inatitut im. P.F.Leagafta, Leningrad (for Skaptsov). (Insects--Biology)

SKOFTKIV, A. G.
"Interspecies Relationships of Insects 1,,-,ading a Communal
Form of Life." Cand Biol Sci, Leningrad State Pedagogical Inst,
Leningrad, 1954. CRZhBiol, No 4, Feb 55)
SO: Sum. *ilo. 6-31, 26 Aug 55- Survey of Scientific and Technical
Dissertations Defended at USSR Higher 6ducational Institu-
tions (14)

L 36291-66 9wT(m)/T/EwP(w) IJP(c) EMN-.4/DJ
ACC NRt AR6004032 SOURCE CODE: UR/0277/65/000/009/0042/0042
AUTHORS: Skoptsov, L. M.; Kuznetsovp Ye6 So
TITLE: Vibration of ball bearings
W~._kj
SOURCE: Ref. zh. Mashinostroitel'We matorialy, konstruktaii I ranchet detaley
mashin. Gidroprivod,, Abe. 9648.354
REF SOURCE: Tr. SeWnara po vopr. progressivn. metodov shlifovj I dovo&-i detaley,
obespech, vysok,
1964~ 134-W
TOPIC TAGS: ball bearing, bearing race., 0Fqe,,.uc, e M'J MV 1 (',9 A-
0 '9X'W _K10 4-0
ABSTRACT; Results of experimental investigations of factors (technological, struc-
tural, and exploitational) influencing the vibration of free bearings,,,are analyzed.
One of the basic causes of ball bearing vibration Is pro7auce ~e 'waviness (form
inaccuracy) of the race in the internal ring. The form inaccuracy in the race of the
external ring ewwta a smaller influence on the vibration than the inaccuracy of the
internal ring, The diinnsions of the ball seats in both stamped and massive sepa-
rators should be optimal. Among a nunber of exploitational factors, the greatest
influencjL on the vibration is exerted by the rotation velocity. ffianslation of
abe a
SUB WM 1 23

SKOPTSOV, S.G.
[Peasants', comnittess n.' mitual aid in the White Russian SSR
during the reconstruction period, 1921-1925; author's abstract of
a dissertation offered for the degree of Candidate of the Historical
Sciences] Krestlanskie komitety obsbchestvennoi vzaimopomosbchi
'BSSR v vosstanovitelinyi period (1921-1925 gg.); avtoreferat
dissertataii na soiskanie uchenoi stepeni kandidata istoricheakikh
nauk. Minsk, Belorusakii gos.univAm. V.I.Lenina, 1953. 20 p.
(White Russia--Agriculture) (Peasants) (MIR& 11:12)

SKOPTSOV, V.I.
Machinery industry in China during ten years. Mashinoutroitell no.10:
44-46 0 159. (MIRL 13:2)
(China--Machiner7 industry)

SKOPTSOVJI V.I.
Some prable-.ms in t,he develo,?mentu of in-anches of the mn,~c'ninez-y
industry in 1965. Vest. mashinostr. 45 no.l.;3-6 Ja 165.
(MIRA 18-3:
1. Chlen Goslidarstvennogo komiteta po ma5hinostrovewyu, pri
Gosplane SSSR.

- SKOPTISOV, V.I.
hqprovin~,, the methods for a scien4.-ific organization of labor
z~nd production in the machinery in~-lustrv. Vest.rwishinovtr.
45 no.11:3-6 U 165. (,,fIRA 18:12)

MAZINA, Ye.G.. kand.med.nauk., MUSATOVA. A.V., WAMOVA, M.I., NABOKOA, Ye.K.
SKOPTSOVA, S.M., KLMIETSOVA, S.A., KLRnL', L.M., DAMANSXAYA, N.V.
FILIPPOVA, T.V.
Effectiveness of epidermal vaccination of newborns* Vop.okh.
mat. i det. 3 no.6:53-58 N-D 158 (MIRA 11:12)
1. Iz Yakutskogo filiala (dir. Ye.N. Andreyev) Instituta tuberkuleza
OIN SSSSRO'
(TUBERCUWSIS--PREVEIITIVE INOCULATION)

LIPATIJVA, T.E.; SKOPYNINA, I.S.; LIFTFOV, Yu.b.
Polymerization of styrene in the presence of the glass fiber treated
by titanium tetrachloride. Vysokor%so,-:~d. 3 no.12:1877 D '61.
(HIRA 150)
(Styrene) (Folymerization) (Glass fibers)

,- SKOPYSRDV, A..Y.
Zonality in the crystals of Iceland Bpar. Izv. vys. ucbeb. zav.
geol. i razv. 3 no-7:69-74 il 16o. (MLU 13:9)
1. Leningradskiy gornyy institut.
(Iceland sW)

SKCR, Vaclav: VANOUSOVA, Eva; SOUCKMA, Eva
Roentgenographic changes of the thoracic picture in surgical
patients with mitral stenosis. Cas.lek.cesk.99 no.38:1218-1220
16 S160.
1. IV. interni klinika KU v Prase, prednosta prof. dr. K.Fucik,
(MITRAL STENOSIS surg)

CZMn'#SKI, Andrzaj; SKORA, Klemens
Measurement of relative movements of bone fragments in the leg.
Chir. narz. ruchu 21 no-3:255-266 1956.
1. Z Zakladu fizyki A.M. we Wroclawiu. Kier.: Z-ca prof. mgr.
V. Skora, I I. Klin. chirurg. A.M. we Wroclawiu. Kier. prof.
dr. K. Czyzewski.
(LEG, fractures,
mAasurement of relative movements of bone fragments (Pol))
(FRACTURES,
leg, measurement of relative movements of bone fragments
(Poi))

CZYZBWSKI, K.; MM-ST "TKI, S.; SKORL, K.; DOLINSKI, J.
Experimental observations on the concentration of phosphorus p32
at the site of fracture of the long bones. Chir.narz.rucha 24
no.4:273-276 '59.
1. Z I Kliniki Chirurgicznej A.M. we Wroclawiu Kierownik: prof.
dr K.CzyzownIci i z Katedry Fizyki Wyznzoj Szkoly Rolniazej we
Wroclawin Kierownik: Z-ca prof. mpr B.Przeatalski.
(PHOSPHORUS metab)
(FBACTURES exper)

CZYZEWSKI, K.; PRZESTALSKI, S.; SKORA, K.
Effect of ossopan on the amount of P32 accumulated on the site of
fracture of the long bones. Chir.narz.ruchu ortop.polska 25 no-3:
205-209 6o.
1. Z I Kliniki Chirurgicznej A.M. we Wroclawiu Kierownik: prof.
dr K.Czyzewski i z Katedry Fizyki W.S.R. we Wroclawiu Kierownik:
z-prof. dr S.Przestalski
(FEACTURES exper)
(PHOSPHORUS metab)
(BONE AND BONES extracts)

GZYZEWSKI, K.,* PRZESTIJSKI, S.;__gQ41-K.; DOLINSKI, J.
Effect of fresh and burned bone meal on the process of P32
concentration on the site of bone fracture. Chir.nar-4.ruchu 25 no.4;
317-320 160.
1. Z I Kliniki Chirurgicznej A.M. we Wroclawiu Kierownik: prof.
dr. K.Czyzewski oraz z Katedry Fizyki W.S.R. we Wroklawiu,
Kierownik: z-prof. S.Przestalski.
(FRACTURES exper)
(BONE AND BONES)
(PHOSPHORUS metab)

DOROBISZ, Tadeusz; CHRZANOWSKA, Maria; PRZESTALSKI, Stanislaw; SKORA, Klemens
Penetration of radiophosphorus P32 into the erythrocytes in variouB
stages of preservation. Acts. pbysiol Pol 12 no.5:751-755 161.
1. Z I Kliniki Chirurgicznej P14 we Wroclawiu Kierownik: prof. dr
K. Czyzewski Z Katedry Fizyki WSR we Wroclawiu Kierownik: z-ca prof.
dr S. Przestalski.
(PHOSPHORUS blood) (ERYTHROCYTES chem)
(BLOOD PRESERVATION)

BI",ILICKI, Franciazek; CZY&USKI, Kazimierz;
Concentration of radioactive iodine in the thyroid under the influence
of some drugs blocking the autonomic nervous system. Endodr. pol.
13 no.1:73-79 162.
1. 1 Klinika Chirurgiczna AM we Wroclawiu Kierownik: prof. dr
K. Czyzewski.
(IODIIE metab) (THMOID GLAJID metab)
(AUTONOMIC DRUGS pharmacol)

GZYZEWSKI, Kazimierz,- BIELICKI, Franciszek; SKORA, Klemens,; ZAGROBEU'Y,
Zdzislaw.
Experimental principles for the treatment of thyroid crisis
Polski przegi. chir. 35 no.9:935-938 163.
1. Z I Klinik-i Chirurgicznej LM we Wroclawiu. Kierowniki
prof. dr. K.Czyzewski.
)k

BIELICKI, Franciszek; CHRZP110WSKA, Mariaj- DOROBISZ, Tadeuss; SKORA,Klemens
Clinical value of 1-231 tests in thyroid neoplasms. Polski
przegl. chir. 35 no.9t954-956 163.
1. ZI Kliniki Chirurgicznej we Wroclawiu. Kierownik: prof.
dr. K.Czyzewski.
*,

BRZECKI, Andrzej,- DOROBISZ, Tadeusz; SKORA, IO.emens; SZEPIETOWSKI, Tomasz
Injuries of the ~Tanftft-sffd;J~rain. Pol. F-,zegl. chir. 36 no.!:
21-29 Ja'64
1. Z niniki Chorob Nerwovych P14 we Wroclawiu (kierownik: prof.
dr. R.Arend) i z Kliniki Chirurgicznej AM we Wroclawiu (kie-
rowniks, prof.dr. K.Czyzewski).

ZAGROBI,,U[Y,, Zd,!islaw; GHIP'tAHG,W3K.A, '4aria; i'dZislaw;
SKOF,A, K1ciriens
Anesthesia in surgical therapy of obliteran:;
of lower extremities. Pol. przegl. ch-Jr. 37 no.9:862--871 S 165.
1. Z I Kliniki Chirurgicznej AM we Wroclawiu (Kierownlk: prof.
dr. K. Czyzewski).

.,a
SKORA, Stantslaw, mgr
Characteristics of the roach (1iti-Dis riit-illis L.) from the
Kozlowa Gora Reservoir. Acts. hydrobiol 6 rc~.3:269-284 164.
1. Institute of Water Biology, Polish Academy of Sciences,
Krakow.

SKORA, Stanislaw; BROJER, Zbigniew;. LENDZION, Andrzej
Application of cool hardened epoxy com*sitions for metal gluing.
Polimery tworz wielk 7 no.9:328-330 8 162,.
1. Instytut Tworzyw Sztucznych, Warszawa.

tti n i a ~--w 9 r I'Z'

K U J A ~-,'A - P I'll* J'C 2E K ) D i b i a Y -- j a ; S K,- - I L'~ , St ~-, 4- i 0 2
Adhesi:ves based on epoxy resins and polymethylolamides.
Polimery tworz wielk 8 no.6:241-244 Je 163.
1. Instytut I'worzywr Sztucznych, Warszawa.

SKORA, Stanislaw, mgr
Characteristics of the tench (Tinca tinca L.) from the
Goczalkowice Reservoir. Acta hydrobiol 6 no.2:97-118 164.
1. lnstitutc~ of Hydrobiology, Polish Academy of Sciences,
Krakow.

SKORA, Stardslaw
'haacter-1-stics of -.he roach (Rutilus Lz' living 'Zi the
Gozzaikowice Reservolr. Acta hydrcb--*7,1 6 rc.4:351-374' '64.
Growth ard nutrition of 14- perch (Perca fiu-,riatillts, L.) in
the Koz1owa Gora Reservoir. IlAd.075-387 164.
I. Institute of Hydrogiology, of the Polich Academy of Sciences,
Krakow.

KRUL, Jarouir, dr.; SKOPNOVA, A=&., WC.
a4
u9sueo of X-irradiated chickens.
Changes in the organs
2. Changes in the liver and spleen of chickens after a dose of
600 r and a dose of oxytetracycline,, vitamin Bj.2 and folic acid
given 60 days after irradiation. Veterinarni medicina, 6
no.12.-931-9.16 161.
1. Katedra pro patologickou morfologii a fyziologii, Veterinarni
fakulta, Vysoka skola, zemedelska, Brno.

BALBMiZ, If.; BAMIECK1, W.; BILLICKI, Frtuiciazek; GUZENSKI, Kazimierz;
ROWOSAD4- R.) SKOI?A, Klemens
Concentration of 1-131 in the thyroid after methylthiouracil,
vitamin A and potassium bromide. Endodr. pol. 13 no.1:81-86
,62.
1. 1 Klinika Chirurgiczna ~.M. we Wroclawiu Kierownik: prof. dr
K.Czyoewski Katedra Fizjopatologii Wydz. Wet. Wyzszej Szkoly Rolniczej
we Wroclakiu Kierownik: Zast. - prof. dr. W.Barnecki.
(THYROID GLUD meteb) (IOMME i6etab)
(THIOUIRAGIL pharmacol) (BROIUDM pharmacol) (ViTAMIN A pha~macol)

T~aria
iven 11.1ames
Coiritry: Poland
Acadevuc Degrees: fnot given7
Instj_t_U--te-of Tgxicological and Forensic Chemistry of the
Affiliation: Medical Academy (Zaklad Chemii Toksykologi.,--zn-e-5-1--S-adowej,
Akademia ,-Iedyczna), Krakow
Source: Warsaw, Farinacja Polska, Vol XVI, No 19, 10 October 1961,
PP 399-401
Datat "The Differentiation of Certain Barbiturio Acid Derlvative3
by Paper Chromatography on the Basis of the Decomposition
Products."
Gro 9816%3