• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    固定铝log(Q/K)图解在温泉中的应用

    张展适 孙占学 李满根 王素娟

    张展适, 孙占学, 李满根, 王素娟, 2004. 固定铝log(Q/K)图解在温泉中的应用. 地球科学, 29(3): 352-356.
    引用本文: 张展适, 孙占学, 李满根, 王素娟, 2004. 固定铝log(Q/K)图解在温泉中的应用. 地球科学, 29(3): 352-356.
    ZHANG Zhan-shi, SUN Zhan-xue, LI Man-gen, WANG Su-juan, 2004. Application of Fixed-Al Modified log(Q/K) Graph in Hot Spring System. Earth Science, 29(3): 352-356.
    Citation: ZHANG Zhan-shi, SUN Zhan-xue, LI Man-gen, WANG Su-juan, 2004. Application of Fixed-Al Modified log(Q/K) Graph in Hot Spring System. Earth Science, 29(3): 352-356.

    固定铝log(Q/K)图解在温泉中的应用

    基金项目: 

    国家自然科学基金项目 40242018

    详细信息
      作者简介:

      张展适(1965-), 女, 副教授, 长期从事地球化学、水文地球化学的教学与研究工作.E-mail: zhszhang@ecit.edu.cn

    • 中图分类号: P314.1

    Application of Fixed-Al Modified log(Q/K) Graph in Hot Spring System

    • 摘要: 为探讨常规和固定铝log (Q/K) 图解法对温泉系统是否有效, 采用WATCH程序, 对江西3个温度较高的温泉, 即庐山温泉、汤湖温泉和横泾温泉, 进行了探测性的研究.采用常规log (Q/K) 图解法计算时, 由于参加计算的4个水样的铝含量均未检出, 计算结果显示只有不含铝的矿物玉髓和方解石相交于温度1 0 0℃附近, 热储总体上没有达到平衡.在采用了固定铝log (Q/K) 图解法并同时考虑冷水的稀释作用计算后, 中低温地热系统中常见的蚀变矿物如浊沸石、纤蛇纹石、萤石和玉髓均显示了较好的收敛性, 收敛的温度大致在1 0 0~ 1 4 0℃.并且上述矿物组合可见于某些温泉的深部钻孔中, 计算结果与实际地质情况相吻合.结果表明固定铝log (Q/K) 图解法可以恢复温泉系统的热平衡状态

       

    • 图  1  研究的温泉分布位置示意图[据李学礼等(2000)修改]

      Fig.  1.  Location of selected hot springs (modified after Li et al. (2000))

      图  2  江西选择性温泉的log (Q/K) 图解

      Fig.  2.  log (Q/K) -t diagram for selected hot springs in Jiangxi Province

      图  3  江西选择性温泉的固定铝log (Q/K) 图解

      Fig.  3.  Fixed-Al log (Q/K) diagram for selected hot springs in Jiangxi Province

      表  1  江西代表性温泉水化学分析结果

      Table  1.   Chemical composition of Tanghu, Lushan and Hengjing hot springs

    • [1] Arnórsson, S., 2000. Isotopic and chemical techniques in geothermal exploration, development and use: Sampling methods, data handling, interpretation. International Atomic Energy Agency, Vienna.
      [2] Bjarnason, J. ., 1994. The speciation program WATCH, version 2.1. Orkustofnun, Reykjavik, 7.
      [3] Browne, P. R. L., 1978. Hydrothermal alteration in active geothermal fields. Ann. Rev. Earth Planet. Sci., 6: 229- 250. doi: 10.1146/annurev.ea.06.050178.001305
      [4] Fenner, C.N., 1936. Bore-hole investigations in Yellowstone Park. J. Geol., 44: 225- 315. doi: 10.1086/624425
      [5] Huang, S.Y., 1993. Hot spring resources in China. China Cartographic Publishing House, Beijing(in Chinese).
      [6] Kristmannsdóttir, H., 1978. Alteration of basaltic rocks by hydrothermal activity at 100- 300 ℃. International Clay Conference, 359- 367.
      [7] Kristmannsdóttir, H., 1982. Alteration in the IRDP drill hole compared with other drill holesin Iceland. Journal of Geophysical Research, 87(8): 6525- 6531.
      [8] Kristmannsdóttir, H., Tómasson, J., 1978. Zeolite zones in geothermal areas in Iceland. In: Sand, L.B., et al., eds., Natural zeolites, occurrence, properties, use. Pergamon Press Ltd., Oxford, 277- 284.
      [9] Li, X.L., Sun, Z.X., Zhou, W.B., 2000. Fossil hydrothemal system and the mineralization of uranium. Geological Publishing House, Beijing(in Chinese).
      [10] Pang, Z.H., 1996. The fixed-Al method applied to Zhangzhou geothermal system, Southeast China. In: Pang, Z. H., Zhang, J.D., Sun, J.H., eds., Advances in solid earth sciences. Science Press, Beijing, 144- 153.
      [11] Pang, Z., Reed, M., 1998. Theoretical chemical thermometry on geothermal waters: Problems and methods. Geochim. Cosmochim. Acta, 62: 1083- 1091. doi: 10.1016/S0016-7037(98)00037-4
      [12] Spycher, N.F., Reed, M.H., 1998. SOLVEQ: A computer program for computing aqueous-mineral-gas equilibria. Revised preliminary edition. Department of Geological Sci- ences, University of Oregon, Eugene, OR 97403.
      [13] Sun, Z.X., 1998. Geothermometry and chemical equilibria of geothermal fluids from Hveragerdi, SW-Iceland, and selected hot springs, Jiangxi Province, SE-China. Geothermal training in Iceland, 373- 402.
      [14] Sun, Z.X., Wu, H.M., 1999. Calculation of the mineral-fluid equilibrium and the reservoir temperature in geothermal system. Acta Geoscientia Sinica, 20(Suppl. ): 595- 598 (in Chinese with English abstract).
      [15] Zhang, W.M., 1999. Origin analysis of geothermal water and evaluation of geothermal reservoir temperature in the Hengjing area, south Jiangxi Province, China. Geotectonica et Metallogenia, 23(2): 155- 165.
      [16] Zhang, Z.S., 2001. Water-rock interaction in the Bakki low- temperature geothermal field, South-west Iceland. Report 17. In: Geothermal training in Iceland 2001. UNU G.T. P., Iceland, 405- 434.
      [17] Zhang, Z.S., Sun, Z.X., Wang, S.J., 2003. Successful recon-structing the equilibrium status of Tanghu hot spring by using fixed-Al method and its meaningness. Journal of East China Geological Institute, 26(4): 306- 310(in Chinese with English abstract).
      [18] 黄尚瑶, 1993. 中国温泉资源. 北京: 中国地图出版社.
      [19] 李学礼, 孙占学, 周文斌, 2000. 古水热系统与铀成矿作用. 北京: 地质出版社.
      [20] 孙占学, 吴红梅, 1999. 地热系统中矿物-流体化学平衡的判断及热储温度的估计. 地球学报, 20 (增刊): 595-598. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199910001104.htm
      [21] 张展适, 孙占学, 王素娟, 2003. 固定铝方法成功恢复汤湖温泉热储平衡温度及其研究意义. 华东地质学院学报, 26 (4): 306-310. doi: 10.3969/j.issn.1674-3504.2003.04.002
    • 加载中
    图(3) / 表(1)
    计量
    • 文章访问数:  3197
    • HTML全文浏览量:  126
    • PDF下载量:  6
    • 被引次数: 0
    出版历程
    • 收稿日期:  2003-09-29
    • 刊出日期:  2004-05-25

    目录

      /

      返回文章
      返回