Be-10 and dust

被引：42

作者：

Baumgartner, S

Beer, J

Wagner, G

Kubik, P

Suter, M

Raisbeck, GM

Yiou, F

机构：

[1] ETH HONGGERBERG, PAUL SCHERRER INST, CH-8093 ZURICH, SWITZERLAND

[2] ETH HONGGERBERG, INST PARTICLE PHYS, CH-8093 ZURICH, SWITZERLAND

[3] CTR SPECTROMETRIE NUCL & SPECTROMETRIE MASSE, IN2P3, CNRS, F-91405 ORSAY, FRANCE

来源：

NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS | 1997年 / 123卷 / 1-4期

关键词：

D O I：

10.1016/S0168-583X(96)00751-3

中图分类号：

TH7 [仪器、仪表];

学科分类号：

0804 ; 080401 ; 081102 ;

摘要：

The Be-10 flux at a given geographical location consists of recent atmospherically produced Be-10 and of recycled Be-10, which is brought in with dust particles. The importance of the latter fraction for the geophysical interpretation of Be-10 in rain, snow and ice is examined, Experimental methods are proposed to separate the two sources for Be-10.

引用

收藏

页码：296 / 301

页数：6

相关论文

共 18 条

[1]

[Anonymous], 1978, Microphysics of Clouds and Precipitation, DOI 10.1007/978-94-009-9905-3

[2] USE OF BE-10 IN POLAR ICE TO TRACE THE 11-YEAR CYCLE OF SOLAR-ACTIVITY [J].

BEER, J ;

BLINOV, A ;

BONANI, G ;

FINKEL, RC ;

HOFMANN, HJ ;

LEHMANN, B ;

OESCHGER, H ;

SIGG, A ;

SCHWANDER, J ;

STAFFELBACH, T ;

STAUFFER, B ;

SUTER, M ;

WOLFLI, W .

NATURE, 1990, 347 (6289) :164-166

[3] THE CAMP CENTURY BE-10 RECORD - IMPLICATIONS FOR LONG-TERM VARIATIONS OF THE GEOMAGNETIC DIPOLE-MOMENT [J].

BEER, J ;

ANDREE, M ;

OESCHGER, H ;

SIEGENTHALER, U ;

BONANI, G ;

HOFMANN, H ;

MORENZONI, E ;

NESSI, M ;

SUTER, M ;

WOLFLI, W ;

FINKEL, R ;

LANGWAY, C .

NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 1984, 5 (02) :380-384

[4] EVIDENCE FOR GENERAL INSTABILITY OF PAST CLIMATE FROM A 250-KYR ICE-CORE RECORD [J].

DANSGAARD, W ;

JOHNSEN, SJ ;

CLAUSEN, HB ;

DAHLJENSEN, D ;

GUNDESTRUP, NS ;

HAMMER, CU ;

HVIDBERG, CS ;

STEFFENSEN, JP ;

SVEINBJORNSDOTTIR, AE ;

JOUZEL, J ;

BOND, G .

NATURE, 1993, 364 (6434) :218-220

[5] A NEW GREENLAND DEEP ICE CORE [J].

DANSGAARD, W ;

CLAUSEN, HB ;

GUNDESTRUP, N ;

HAMMER, CU ;

JOHNSEN, SF ;

KRISTINSDOTTIR, PM ;

REEH, N .

SCIENCE, 1982, 218 (4579) :1273-1277

[6] CONTINUOUS MEASUREMENTS OF HYDROGEN-PEROXIDE, FORMALDEHYDE, CALCIUM AND AMMONIUM CONCENTRATIONS ALONG THE NEW GRIP ICE CORE FROM SUMMIT, CENTRAL GREENLAND [J].

FUHRER, K ;

NEFTEL, A ;

ANKLIN, M ;

MAGGI, V .

ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1993, 27 (12) :1873-1880

[7] A COMPARISON OF DEEP ANTARCTIC ICE CORES AND THEIR IMPLICATIONS FOR CLIMATE BETWEEN 65,000 AND 15,000 YEARS AGO [J].

JOUZEL, J ;

RAISBECK, G ;

BENOIST, JP ;

YIOU, F ;

LORIUS, C ;

RAYNAUD, D ;

PETIT, JR ;

BARKOV, NI ;

KOROTKEVITCH, YS ;

KOTLYAKOV, VM .

QUATERNARY RESEARCH, 1989, 31 (02) :135-150

[8] PARTITION OF RADIOTRACERS BETWEEN SUSPENDED PARTICLES AND SEAWATER [J].

LI, YH ;

BURKHARDT, L ;

BUCHHOLTZ, M ;

OHARA, P ;

SANTSCHI, PH .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1984, 48 (10) :2011-2019

[9] THE GLOBAL-AVERAGE PRODUCTION-RATE OF BE-10 [J].

MONAGHAN, MC ;

KRISHNASWAMI, S ;

TUREKIAN, KK .

EARTH AND PLANETARY SCIENCE LETTERS, 1986, 76 (3-4) :279-287

[10] APPLICATIONS OF COSMOGENIC BE-10 TO PROBLEMS IN THE EARTH-SCIENCES [J].

MORRIS, JD .

ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, 1991, 19 :313-350