Derivation of travel time of limestone cave drip water using tritium/helium 3 dating method

12Citations
Citations of this article
17Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

A method of deriving the travel time of drip water based on the tritium/ helium 3 (3H/3 He) dating method was demonstrated in limestone caves in Indonesia. The examined drip waters from two caves, which were taken using different methods, included 2.15 (± 0.84) TU and 1.35 (± 0.77) TU of tritiogenic 3He. From the derived tritiogenic 3He contents and the measured tritium concentrations of the drip water samples (2.02 ± 0.27 TU and 1.19 ± 0.40 TU), the 3H/3 He ages (travel times) of the drip waters from the two caves were estimated as 12.9 ± 3.8 years and 13.5 ± 6.3 years. The latter age is probably overestimated because re-equilibration of He between drip water and cave air is expected to occur during sampling. For reliable derivation of 3H/3He age, it is advisable to take a drip water sample that is kept isolated from the cave air. Copyright 2008 by the American Geophysical Union.

Cite

CITATION STYLE

APA

Yamada, M., Ohsawa, S., Matsuoka, H., Watanabe, Y., Brahmantyo, B., Maryunani, K. A., … Yoden, S. (2008). Derivation of travel time of limestone cave drip water using tritium/helium 3 dating method. Geophysical Research Letters, 35(8). https://doi.org/10.1029/2008GL033237

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free