New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS)

被引:59
作者
Affolter, S. [1 ,2 ]
Fleitmann, D. [2 ]
Leuenberger, M. [1 ,2 ]
机构
[1] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland
[2] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland
基金
瑞士国家科学基金会;
关键词
RATIO MASS-SPECTROMETRY; RING-DOWN SPECTROSCOPY; HYDROUS MINERALS; STABLE-ISOTOPE; CAVE SYSTEM; DELTA-O-18; DELTA-H-2; VAPOR; PRECISION; CALIBRATION;
D O I
10.5194/cp-10-1291-2014
中图分类号
P [天文学、地球科学];
学科分类号
070403 [天体物理学];
摘要
A new online method to analyse water isotopes of speleothem fluid inclusions using a wavelength scanned cavity ring down spectroscopy (WS-CRDS) instrument is presented. This novel technique allows us simultaneously to measure hydrogen and oxygen isotopes for a released aliquot of water. To do so, we designed a new simple line that allows the online water extraction and isotope analysis of speleothem samples. The specificity of the method lies in the fact that fluid inclusions release is made on a standard water background, which mainly improves the delta D robustness. To saturate the line, a peristaltic pump continuously injects standard water into the line that is permanently heated to 140 degrees C and flushed with dry nitrogen gas. This permits instantaneous and complete vaporisation of the standard water, resulting in an artificial water background with well-known delta D and delta O-18 values. The speleothem sample is placed in a copper tube, attached to the line, and after system stabilisation it is crushed using a simple hydraulic device to liberate speleothem fluid inclusions water. The released water is carried by the nitrogen/standard water gas stream directly to a Picarro L1102-i for isotope determination. To test the accuracy and reproducibility of the line and to measure standard water during speleothem measurements, a syringe injection unit was added to the line. Peak evaluation is done similarly as in gas chromatography to obtain delta D and delta O-18 isotopic compositions of measured water aliquots. Precision is better than 1.5% for delta D and 0.4 parts per thousand for delta O-18 for water measurements for an extended range (-210 to 0 parts per thousand for delta D and -27 to 0 parts per thousand for delta O-18) primarily dependent on the amount of water released from speleothem fluid inclusions and secondarily on the isotopic composition of the sample. The results show that WS-CRDS technology is suitable for speleothem fluid inclusion measurements and gives results that are comparable to the isotope ratio mass spectrometry (IRMS) technique.
引用
收藏
页码:1291 / 1304
页数:14
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