DETERMINATION OF EROSION RATES WITH COSMIC-RAY PRODUCED CL-36

被引：28

作者：

DOCKHORN, B ^{[1
]}

NEUMAIER, S ^{[1
]}

HARTMANN, FJ ^{[1
]}

PETITJEAN, C ^{[1
]}

FAESTERMANN, H ^{[1
]}

KORSCHINEK, G ^{[1
]}

MORINAGA, H ^{[1
]}

NOLTE, E ^{[1
]}

机构：

[1] PAUL SCHERRER INST,CH-5232 VILLIGEN,SWITZERLAND

来源：

ZEITSCHRIFT FUR PHYSIK A-HADRONS AND NUCLEI | 1991年 / 341卷 / 01期

关键词：

D O I：

10.1007/BF01281283

中图分类号：

O57 [原子核物理学、高能物理学];

学科分类号：

070202 ;

摘要：

We present results of the determination of Cl-36 (T 1/2 = 3.0.10(5) a) in rock samples produced in situ by cosmic rays and natural radioactivities. These experiments were designed to determine the feasibility of using Cl-36 for studying erosion processes in calcium rich minerals like limestone or dolomite. The Cl-36/Cl ratios in the samples have been determined with accelerator mass spectrometry (AMS) at the Munich accelerator laboratory. A first application is the investigation of the erosion in the last million years in Allchar (Yugoslavia) for the feasibility study of the geochemical Tl-205 solar neutrino experiment.

引用

页码：117 / 119

页数：3

共 17 条

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