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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Comment on: 'Origin, timing, and temperature of secondary calcite-silica mineral formation at Yucca Mountain, Nevada' by N. S. F. Wilson, J. S. Cline, and Y. V. Amelin
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Comment on: 'Origin, timing, and temperature of secondary calcite-silica mineral formation at Yucca Mountain, Nevada' by N. S. F. Wilson, J. S. Cline, and Y. V. Amelin

机译:N. S. F. Wilson,J。S. Cline和Y. V. Amelin发表评论:“内华达州尤卡山次方解石-二氧化硅矿物形成的起源,时间和温度”

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摘要

Yucca Mountain in southern Nevada is being evaluated as a potential site for the geological disposal of high-level nuclear waste. A reliable assessment of the future performance of the repository will require detailed paleohydrogeological information. Hydrogenic secondary minerals from the vadose zone of Yucca Mountain are being studied as paleohydrogeological indicators. A phenomenological model envisaging the deposition of secondary minerals by meteoric fluids infiltrating downward though the vadose zone was proposed in the reviewed paper. Our evaluation reveals that the model is not supported by empiric evidence reported in the paper. Copyright (c) 2005 Elsevier Ltd.
机译:内华达州南部的丝兰山正在被评估为高放核废料地质处置的潜在场所。对储存库未来性能的可靠评估将需要详细的古水文地质信息。尤卡山渗流带的水生次生矿物正在被用作古水文地质指标。在这篇论文中,提出了一种现象学模型,该模型设想了通过渗流通过渗流带向下渗透的次级流体沉积的次生矿物质。我们的评估表明该模型不受本文报道的经验证据的支持。版权所有(c)2005 Elsevier Ltd.

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