Georg,R.B., Zhu,C., Reynolds,B.C. and Halliday,A.N.(2009): Stable silicon isotopes of groundwater, feldspars, and clay coatings in the Navajo Sandstone aquifer, Black Mesa, Arizona, USA. Geochimica et Cosmochimica Acta, 73, 2229-2241.

『米国アリゾナ州のブラックメサのナバジョ砂岩帯水層における地下水と長石と粘土被膜の安定ケイ素同位体』

『Abstract
　We present some of the first analyses of the stable isotopic composition of dissolved silicon (Si) in groundwater. The groundwater samples were from the Navajo sandstone aquifer at Black Mesa, Arizona, USA, and the Si isotope composition of detrital feldspars and secondary clay coatings in the aquifer were also analyzed. Silicon isotope compositions were measured using high-resolution multi-collector inductively coupled mass spectrometry (HR-MC-IPC-MS) (Nu1700 & NuPlasma HR). The quartz dominated bulk rock and feldspar separates have similar δ30Si of -0.09±0.04‰ and -0.15±0.04‰ (±95％ SEM), respectively, and clay separates are isotopically lighter by up to 0.4‰ compared to the feldspars. From isotopic mass-balance considerations, co-existing aqueous fluids should have δ30Si values heavier than the primary silicates. Positive δ30Si values were only found in the shallow aquifer, where Si isotopes are most likely fractionated during the dissolution of feldspars and subsequent formation of clay minerals. However, δ30Si decreases along the flow path from 0.56‰ to -1.42‰, representing the most negative dissolved Si isotope composition so far found for natural waters. We speculate that the enrichment in 28Si is due to the dissolution of partly secondary clay minerals and low-temperature silcretes in the Navajo Sandstone. The discovery of the large range and systematic shifts of δ30Si values along a groundwater flow path illustrates the potential utility of stable Si isotopes for deciphering the Si cycling in sedimentary basins, tracing fluid flow, and evaluating global Si cycle.』

1. Introduction
2. Geology, hydrogeology, and mineralogy
3. Sampling and analytical methods
　3.1. Sampling and analyzing groundwater
　3.2. Solid sampling and size fractionation
　3.3. Silicon isotope determination - mass spectrometry
4. Results
5. Discussion
　5.1. Clay precipitation induced Si isotope fractionation
　5.2. Silicon isotopic evolution of groundwater
6. Conclusions
Acknowledgments
Appendix A. Hydrochemistry data and discussion
References

ホームへ