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    中国百强科技报刊

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    Volume 27 Issue 2
    Mar.  2002
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    WAN Jun-wei, LIU Cun-fu, WANG Zeng-yin, CHAO Nian-ying, WANG Pei-yi, 2002. Theory and Method of Determining Erosion Rate in Limestone With 36Cl. Earth Science, 27(2): 173-176.
    Citation: WAN Jun-wei, LIU Cun-fu, WANG Zeng-yin, CHAO Nian-ying, WANG Pei-yi, 2002. Theory and Method of Determining Erosion Rate in Limestone With 36Cl. Earth Science, 27(2): 173-176.

    Theory and Method of Determining Erosion Rate in Limestone With 36Cl

    • Received Date: 2001-11-15
    • Publish Date: 2002-03-25
    • Five origins of 36Cl in calcite were studied theoretically: (1)near-surface production by Ca spallation and spallogenic neutron capture, (2)negative muon capture by calcium, (3)neutron emission following negative muon capture, (4)neutrons from photodisintegration reactions initiated by fast muons, (5) neutron from uranium fission and(α, n)reactions. Four characteristics of 36Cl distribution for deep profile in limestone have been discussed: (1)36Cl concentration is reduced with depth, (2)depth naturally separates 36Cl contributions from the various production reactions, (3)in order to partition measured 36Cl concentrations into contributions from muon capture on Ca and capture of muon-produced neutrons on 35Cl, the sample set must possess a range of Ca/Cl ratios, (4)limestone erosion is inevitable under even the most arid conditions and plays a significant role in determining steady-state concentrations.Sampling method of 36Cl and AMS analytical technique are described in detail.Mathematical model of determining erosion rate in limestone is studied and some surface erosion rate of limestone are evaluated.

       

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