Health Physics, Pergmon Press 1965, Vol. Ii, Pp
Total Page:16
File Type:pdf, Size:1020Kb
I MARSHALL ISLANDS FILE TRACKING DOCUMENT Record Number: &z3’/ File Name (TITLE): Document Number (ID): DATE: ‘$&% 5-- Previous Location (FROM): P/C .- AUTHOR: h Hoc&a Addditional Information: J OrMIbox: 1, & CyMIbox: : I -- /, ! ,/’ /, ’ -‘;l> / _-q- .I IL! _ PROCEEDINGS OF THE r,..JORD SYMPOSIUM ON RADIATION AND TERt,,,,RIAL ECOSYSTEMS RICHLAND, WASHINGTON 3-S MAY 1965 “ OFF/C/AL JOURNAL/OF- 3-E‘HEALTH PHYSICS SOCIETY :./’ ’ l.._ _. ‘I \i c . ,. /’ . ./’ >‘\\ I / Volume I I, Number December, I965 ‘\ ,/.’ / ox. 8,’ ! \ / i ,’ i’ I ,,” ‘? ,j’ ._ ! ‘.- \ $7 KARL Z. MORGAN c> \ Editor-in-Chief 0 c --- W. S. SNYDER PERGAMON PRESS NEW YORK OXFORD ’ @h physicsPergamon Press 1965. Vol. 11, pp. 1445-1457. Printed in Northern Ireland \ \ :a1Lbofo. (1964). ‘YWf%p. \ . LARSON, PRELIMINARY STUDIES OF THE PERSISTENCE OF TRITIUM ’ 1 by v. AND “C IN THE PACIFIC PROVING GROUND* q?..$xeinhold, ‘:_.:. ., :’ 2 b 1% 271 JOHN J. KORANDA Bio-Medical Division, Lawrence Radiation Laboratory, University of California, Soil P/. Livermore, California 0 Expm (Presented by J. J. KORANDA) ’ SUPPL nization, Abstract-The results of a preliminary survey of detonation environments in the Pacific Proving Grounds indicate that r&dual tritium and “C are present in relatively high concentra- tions in soil materials of the detonation sites at times up to 12 years after the event. Exchange of soil-bound tritium with the available soil water takes place at a slow but significant rate and tritium is detectable in plants growing in the detonation environments. 1% is also elevated in the terrestrial plants. The basis for the elevated 1% is not implicit in these preliminary data. Tritium and 1’C are also present in elevated concentrations in marine organisms. However, due to the high rate of exchange of the lagoon waters with the open sea, these elevated concen- trations arc highly localized in the vicinity of the detonation site (Mike Crater). INTRODUCTION basic structures of organisms in the detonation THE FATE of residual radioactivity from nuclear environment. detonations in natural environments has been While tritium and 14C have been detected ttudied with increasing intensity since the and studied in worldwide fallout, the fate of beginning of testing in the S.W. Pacific in 1946. these two radioelements in local detonation Sluch of the biological information on the local environments and in the biosphere in general has cffccts of residual radioactivity is about either received little attention. Recent evidence from the atoll environments of the Pacific Proving the Sedan cratering detonation in southern Grounds in the Marshall Islands or the desert Nevada indicates that tritium is present in high areas of the Nevada Test Site. Much of this concentration in the geological materials dis- information pertains to fission products and placed and modified by the detonation 2 years their movement in soils, plants and animals of after the detonation. Therefore, a study was rhc detonation environment although some initiated to investigate the persistence of tritium recentresearch has been concerned with induced and 14C in detonation environments. This paper ndioactivities. presents the results of a preliminary survey for \Vith the advent of therm’onuclear devices and tritium and 14C in an atoll environment of the the subsequent lowering of the fission-fusion Pacific Proving Grounds. Detonations occurred mios, induced radioactivities have grown in from 6 to 12 years ago in the sites sampled, and importance relative to fission products. Tritium tropical vegetation has reinvaded most of the and 14C represent a significant portion of the areas affected. Tritium and 1°C activity was raidual radioactivity from a thermonuclear determined in plants, animals and soils from a detonation. Hydrogen and carbon are ubiqui- variety of habitats. The effects of indigenous KJUSelements in the biosphere and are included substratum, climatology, and uptake by the in every significant biological molecule. Tritium biota on the persistence of tritium and “C are and 14C, therefore, will be incorporated into the discussed. Evidence indicates that both tritium and l*C ‘This work performed under the auspices of the have been retained by the physical materials in U.S. Atomic Energy Commission. the detonation environment in relatively high la 1445 i4-G PERSKSES-CE OF TRITILX .A...D ‘4I IS THE P_KIFIC PRO\-Lh-G CROL-XI concenrrationst and that they are presently in the 1958 series, and in previous sear, detectable at elevated levels in the biota. tower shots were fired on this island. Collectiol, were also made on Aomon, Biijiri and Aaranbini DESCRIPTION OF THE STUDY Islands on the eastern edge of the atoll. The Eniwetok Atoll is in the northern portion of islands were adjacent to shot areas and recei\& the Marshall Islands in the S.W. Pacific Ocean close-in fallout from barge shots in the lagoon, (1 l”30’ N lat, 162”15 E long) and was a proving Aomon Island had a 49-kton tower shot in 1918, ground for nuclear device testing from 1948 to A map of Eniwetok Atoll with the island name 1958 when the last detonations took place. The and crater locations is given in Fig. 1. detonations occurred in various environmental situations within or near the atoll, In11 fur the Sampling procedure purposes of surveying for residual tritium and This survey is intended to be an initial I%, the crater-forming shots were considered examination of the Eniwetok environment to most appropriate. Preliminary studies of a determine if tritium and “C are present in large cratering detonation at the Nevada Test biological and soil materials at times up to 12) Site have indicated that a significant fraction after detonation. Because of the preliminaq of the residual tritium produced becomes nature of the survey, it was desirable to collect a associated with the geological materials in and wide variety of materials without acquiring displaced by the explosion.“) excessively large numbers of samples for analys$. The detonations which produced a distinct In some cases a sample series may be incom. crater at Eniwetok Atoll were few (many shots plete because of sample number limitations 01 being made from barges within the atoll lagoon), its unavailability at the time of collection. In but two areas were selected for survey on the spite of some shortcomings and the preliminaq basis of their physical and biological character- nature of this survey, the data enable us to istics. Cactus Shot (1958 Hardtack Series) pro- describe in some detail the persistence of tritium duced a terrestrial crater at the north end of and 14C in the physical and biological materials Runit Island on the eastern edge of the atoll. of the atoll. The crater has a distinct lip and a throwout The samples were collected on eight islands zone of mounded coral sand and debris. Vas- on Eniwetok Atoll during July and August 1964. cular plants have become reestablished on the This was the beginning of the rainy season in the crater materials, and trees of Scaevola jiutescens northern Marshall Islands. The University of and Messerschmidia argentea with diameters up to Washington, Laboratory of Radiation Biology 4 in. at the crown are growing within 15 ft of the scientific staff was conducting a resurvey of crater lip. Mike Shot (1952 Ivy Series) created Eniwetok and Bikini Atolls at this time and a large submarine crater adjacent to Sanildefonso assisted in collecting the biological specimens. Island. The crater is actually in the coral reef It would not have been possible to obtain the that forms the oval platform on which the wide range of samples reported in this study islands of the atoll have formed. The crater has without their valuable assistance. partially filled with coral sand since the shot At Japtan, Runit and Engebi Islands, wood. date. green leaves, litter and a soil sample were Other islands in the atoll not involved directly collected as an ecological series from the same in any nuclear detonation (but which undoubt- sample site. A wood sample from the south end edly received close-in fallout of large particles) of Runit Island was compared with the sample were also sampled to provide information on the from the north end at Cactus Crater. Wood general tritium background of the atoll. Igurin samples were also obtained from four other Island at the southern end of the atoll and islands. Japtan Island on the eastern edge were islands Two plant species were often present in the farthest from the detonation sites which were habitats of the detonation sites. These were sampled in this series, Engebi Island at the Triumfetta procumbeq a prostrate vine in the northeast corner of the atoll was also sampled. Tiliaceae, and Leptunu repent, a short grass. Thw This island was adjacent to many barge shot sites species were collected on Runit Island adjacent J. J. KORANDA Series, ctions nbiru Thrr\e .rivnl <C\\I\, i91:;. ‘w>nn,-._.>..c.i!..;. initial :nt IO nt in ’ 12v ina lect a liring IlYSii. tom. ns or . In narY 1s to tium :rials ands 964. 1 the Y of- ‘osy r’ of and ens. the UdY )od, rere ._*.*.....,:< . lme a&p,,:,&%+&nd IPlC 3od her Fro. 1. Map of Eniwetok Atoll. the ere the ese cnt 1448 PERSISTENCE OF TRITIUM AND “C IN THE PACIFIC PROVING GROUX~ to Cactus Crater and on Sanildcfonso Island the soil particles (in this case, alm%s c near Mike Crater. CaCO,and Car@~~,,\vemoi?ti~c~ ;,; ,_,. 3”.+/A rildt’ 01.!!irlri?l;i’ . tir1c <.l:f;Y?,<.-f’ti’ .Iirl*.~~.;r-_ :;li;’ :Iie ihX?ZC-~ ;7XlCIUfZS in .i ': I cnfims ..v:thin ihe ia,goon. Fishes were obtained containing copper oxide at 6OOilO\,;c. near I,gurin Island, Runit Island and off is collected from the effluent gas by a frccrr Sanildefonso Island at the edge of Mike Crater.