LARGE, LOW-BACKGROUND WELL-TYPE DETECTORS FOR MEASUREMENTS OF ENVIRONMENTAL-RADIOACTIVITY

被引:133
作者
REYSS, JL
SCHMIDT, S
LEGELEUX, F
BONTE, P
机构
[1] Centre des Faibles Radioactivités (CFR), Domaine du CNRS, 91 198 Gif sur Yvette Cedex, Avenue de la Terrasse
关键词
D O I
10.1016/0168-9002(95)00021-6
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
During the two last decades, the development of gamma counting techniques has led to the application of natural radioactivity to the study of numerous processes occurring in the environment. Such work flourished particularly when large HP germanium detectors with low background became available. For some studies, the sample to be measured is small (e.g. sediment, BaSO4 precipitate). In such cases, the use of high efficiency well-type detectors, when compared with similar detectors of conventional shape, provides the best choice. This paper describes three large, well-type detectors used for environmental studies. The background of the crystals has been lowered by: i) placing the detectors in an underground laboratory (Laboratoire Souterrain de Modane, LSM), shielded from cosmic radiation by 1700 m of rocks; ii) using only very low activity materials for the detector assembly and copper-lead shield. Results from various oceanic samples such as particles, sediments, water and hydrothermal sulphides are presented to illustrate the usefulness of this kind of detector for the measurement of environmental radioactivity. For sample volumes of about 10 cm(3), these installations are shown to be the most sensitive way to measure nuclides as Ra-226, Ra-228, Th-228 and Cs-137.
引用
收藏
页码:391 / 397
页数:7
相关论文
共 15 条
[1]   DISTRIBUTION OF THORIUM ISOTOPES BETWEEN DISSOLVED AND PARTICULATE FORMS IN THE DEEP-SEA [J].
BACON, MP ;
ANDERSON, RF .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1982, 87 (NC3) :2045-2056
[2]   MEASUREMENT OF LOW-LEVEL RADIOACTIVITY IN THE MODANE UNDERGROUND LABORATORY [J].
BOURLAT, Y ;
MILLIESLACROIX, JC ;
ABT, D .
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION A-ACCELERATORS SPECTROMETERS DETECTORS AND ASSOCIATED EQUIPMENT, 1994, 339 (1-2) :309-317
[3]   PARTICLE MIXING RATES IN SEDIMENTS OF THE EASTERN EQUATORIAL PACIFIC - EVIDENCE FROM PB-210, PU-239, PU-240 AND CS-137 DISTRIBUTIONS AT MANOP SITES [J].
COCHRAN, JK .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (05) :1195-1210
[4]  
COCHRAN JK, 1992, URANIUM SERIES DISEQ, P395
[5]   RATES OF SEDIMENT REWORKING AT THE HEBBLE SITE BASED ON MEASUREMENTS OF TH-234, CS-137 AND PB-210 [J].
DEMASTER, DJ ;
MCKEE, BA ;
NITTROUER, CA ;
BREWSTER, DC ;
BISCAYE, PE .
MARINE GEOLOGY, 1985, 66 (1-4) :133-148
[6]  
FLEER AP, 1991, GEOPH MONOG SERIES, V63, P223
[7]  
GRASTY RL, 1988, CAN MINERAL, V26, P627
[8]   DISTRIBUTION OF RA-228 IN WORLD OCEAN [J].
KAUFMAN, A ;
TRIER, RM ;
BROECKER, WS ;
FEELY, HW .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (36) :8827-8848
[9]   ACTINIDE-SERIES DISEQUILIBRIUM AS A TOOL TO ESTABLISH THE CHRONOLOGY OF DEEP-SEA HYDROTHERMAL ACTIVITY [J].
LALOU, C ;
REYSS, JL ;
BRICHET, E .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1993, 57 (06) :1221-1231
[10]   PARTICLE MIXING RATES IN SEDIMENTS OF THE NORTHEAST TROPICAL ATLANTIC - EVIDENCE FROM PB-210(XS), CS-137, TH-228(XS) AND TH-234(XS) DOWNCORE DISTRIBUTIONS [J].
LEGELEUX, F ;
REYSS, JL ;
SCHMIDT, S .
EARTH AND PLANETARY SCIENCE LETTERS, 1994, 128 (3-4) :545-562