首页> 外文期刊>Journal of Volcanology and Geothermal Research >Phase segregation, boiling, and reinjection at the Los Azufres Geothermal Field, Mexico, monitored by water stable isotopes, chloride, and enthalpy
【24h】

Phase segregation, boiling, and reinjection at the Los Azufres Geothermal Field, Mexico, monitored by water stable isotopes, chloride, and enthalpy

机译:墨西哥Los Azufres地热田的相分离,沸腾和再注入,由水稳定同位素,氯化物和焓监测

获取原文
获取原文并翻译 | 示例
           

摘要

Monitoring the impact of brine reinjection is crucial to the sustainable exploitation of geothermal resources. Reinjection monitoring at the Los Azufres Geothermal Field (Mexico) has historically been carried out by investigating the temporal and spatial evolution of chloride and the stable isotopic composition of water. Here, we review the evolution of the stable isotopic composition of the total fluid discharge (ID) since the earliest measurements in 1980, integrating new data obtained in 2014. Based on 8D 1D and delta O-18(TD) values measured in 2014, two groups of fluids were identified. The first group is characterized by delta D-TD and delta O-18(TD) similar to those measured in previous survey years, 1980-1982, 1983-1986, and 2000. The second group shows a large positive shift in the hydrogen isotopic composition (Delta D-TD of +10 parts per thousand) compared to the first group. The evolution of reinjected brines and production wells over time between 1980 and 2014 shows delta(18)Om and EiD m enrichment until 2000. This is followed, between 2000 and 2014, by a slight decrease in delta O-18(TD) values and a net increase in delta D-TD, explained by extensive phase segregation and boiling, at temperatures of over 280 degrees C. The observed trend suggests that a steam phase, caused by boiling, is invading the reservoir, and the phenomenon is observed in both production and reinjected fluids. A comparison of the spatially kriged 2000 and 2014 delta O-18(TD) and delta D-TD datasets reveals that reinjected brine is spreading progressively to the eastern part of the field, mainly in the southern production zone (SPZ), and through E-W corridors delimited by the E-W fault systems, which underlie the secondary permeability of the reservoir. However, reinjection is still not able to suppress boiling in the main production zone. This situation needs to be taken into account in developing future reinjection strategies to counterbalance the substantial fluid extraction from the field. (C) 2019 Elsevier B.V. All rights reserved.
机译:监测注入盐水的影响对于可持续开发地热资源至关重要。历史上,Los Azufres地热田(墨西哥)的回注监测是通过调查氯化物的时空演变和水的稳定同位素组成进行的。在这里,我们结合了2014年获得的新数据,回顾了自1980年最早进行测量以来,总流体排放(ID)的稳定同位素组成的变化。基于2014年测量的8D 1D和δO-18(TD)值,确定了两组液体。第一组的特征是δD-TD和δO-18(TD)与以前的调查年份(1980-1982、1983-1986和2000年中测得的相似)相似。第二组显示出氢同位素的大正位移相较于第一组,其组成(Delta D-TD为千分之十)。 1980年至2014年间,随着时间的推移,再注入盐水和生产井的演变过程显示,δ(18)Om和EiD m富集直至2000年。随后,在2000年至2014年之间,δO-18(TD)值略有下降,并且在超过280摄氏度的温度下,δD-TD的净增加,这是由于大量的相分离和沸腾造成的。观察到的趋势表明,由沸腾引起的蒸汽相正在侵入储层,并且在两种情况下都观察到了这种现象。生产和回注液。对2000年和2014年三角O-18(TD)空间数据和三角洲D-TD数据集进行的比较表明,注入的盐水正逐渐扩散到油田的东部,主要在南部生产区(SPZ),并通过EW由EW断层系统界定的走廊,这是储层次生渗透率的基础。但是,再注入仍不能抑制主产区中的沸腾。在制定未来的回注策略时,必须考虑到这种情况,以平衡从油田抽出的大量液体。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Journal of Volcanology and Geothermal Research》 |2020年第15期|106751.1-106751.12|共12页
  • 作者

  • 作者单位

    Univ Michoacana Fac Ciencias Ingn Quim Morelia Michoacan Mexico;

    Univ Quebec Montreal Res Ctr Dynam Earth Syst Geotop Montreal PQ Canada;

    Univ Michoacana Fac Ingn Civil Morelia Michoacan Mexico;

    Isotope Tracer Technol Inc Waterloo ON Canada;

    Desert Res Ctr Hydrogeochem Dept Div Water Resources & Arid Land Cairo Egypt;

    Univ Michigan Dept Earth & Environm Sci Ann Arbor MI 48109 USA;

    CFE Gerencia Proyectos Geotermoelect Morelia Michoacan Mexico;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号