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深海pH探测电极自校正技术实验研究 被引量:2

Experimental study on self-calibration technique of deep-sea pH exploration electrode
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摘要 为了实现深海热液pH值的长期原位探测,采用2种缓冲液对pH探测电极在海底进行原位自校正.利用Fluent软件对容积为10 mL的探头腔进行了结构优化设计,为保证探头腔内的液体被冲洗干净,对腔体的主要结构参数进行了仿真计算.仿真结果表明,当入射半角为37°,长宽比为1.5时,探头腔内流体的总体流动趋势较理想,回流现象较少.为了实现自校正的功能,设计了一种利用2种缓冲液进行标定的流体控制系统.利用该流体控制系统,实验测试了pH=4.003和6.864的2种缓冲液在所设计的10 mL探头腔内相互冲洗的效果.结果表明,2种缓冲液的相互冲洗都可以在6 min内完成,从而证实了所设计的冲洗装置有实用价值. pH exploration electrodes need to be self-calibrated in the seafloor in order to implement long-time in-situ pH exploration for the deep-sea hydrothermal fluid.A method was presented using two buffers to on-line calibrate pH electrodes,and a 10 mL probe chamber was designed.Fluent software was used to simulate and calculate the main structure parameters of the chamber to ensure a kind of liquid in the chamber be replaced by another kind of liquid completely.The simulation indicates that the whole flow is re...
出处 《浙江大学学报(工学版)》 EI CAS CSCD 北大核心 2007年第11期1773-1777,共5页 Journal of Zhejiang University:Engineering Science
基金 国家科技部国际合作重点资助项目(2004DFA04900) 美国国家自然科学基金资助项目(0525907) 国家自然科学基金重点资助项目(40637037)
关键词 热液 PH电极 标定 缓冲液 hydrothermal fluid pH electrode calibration buffer
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参考文献7

  • 1[1]RUBIN K.Degassing of metals and metalloids from erupting seamount and mid-ocean ridge volcanoes:observations and predictions[J].Geochemica et Cosmochimica Acta,1997,61:3525-3542.
  • 2[2]DING K,SEYFRIED W E JR.In-situ measurement of dissolved H2 in aqueous fluid at elevated temperatures and pressures[J].Geochemica et Cosmochimica Acta,1995,59:4769-4773.
  • 3[3]DING K,SEYFRIED W E JR.Direct pH measurement of NaCl-bearing fluid with an in situ sensor at 400 degrees C and 40 megapascals[J].Science,1996,272:1634-1636.
  • 4[4]DING K,SEYFRIED W E JR,TIVEY M K,et al.In-situ measurement of dissolved H2 and H2S in high temperature hydrothermal vent fluids at the Main Endeavour field,Juan de Fuca Ridge[J].Earth and Planetary Science Letters,2001,186(3/4):417-425.
  • 5[5]BAKER E T.Patterns of event and chronic hydrothermal venting following a magmatic intrusion:new perspectives from the 1996 Gorda Ridge eruption[J].Deep-Sea Research II,1998,45(12):2599-2618.
  • 6[6]MASSOTH G J,BAKER E T,FEELY R A,et al.Manganese and iron in hydrothermal plumes resulting from the 1996 Gorda Ridge Event[J].Deep-Sea Research II,1998,45(12):2683-2712.
  • 7[7]WANG M,YAO S,MADOU M,A long-term stable iridium oxide pH electrode[J].Sensors and Actuators B,2002,81(2/3):313-315.

同被引文献19

  • 1赖锡军,汪德爟,姜加虎,黄群.斜坡上异重流的三维数值模拟[J].水科学进展,2006,17(3):342-347. 被引量:4
  • 2DING K, SEYFRIED W E. Direct pH measurement of NaCl-bearing fluid with an in situs sensor at 400 degrees C and 400 mcgapascals[J]. Science, 1996, 272(6). 1 634-1 636.
  • 3PHILLIPS H, WELLS L E, JOHNSON R V, et al. LAREDO: A new instrument for sampling and in situ incubation of deep-sea hydrothermal vent fluids[J]. Deep-Sea Research I, 2003, 50:1 375-1 387.
  • 4DING K, SEYFRIED W E. In situ measurement of pH and dissolved H2 ill mid-ocean ridge hydrothermal fluids at elevated temperatures and pressures[J]. Chemical Rev., 2007, 107: 601-622.
  • 5WANG M, YAO S, MADOU M. A long-term stable iridium oxide pH electrode [J]. Sensors and Actuators B, 2002, 81 (2-3). 313-315.
  • 6SERWAY R A, BELCHER R J. Physics for scientists and engineers[M]. Fort Worth: Saunders College Publishing, 2000.
  • 7WILLIAMS A E. Fluid density distribution in a high temperature, stratified thermohaline system: implications for saline hydrothermal circulation[J]. Earth and Planetary Letter, 1997, 146: 121-136.
  • 8SEONG G H, CROOKS R M. Efficient mixing and reactions within microfluidic channels using microbead supported catalysts[J]. Journal of the American Chemical Society, 2002, 124(45): 13 360-13 361.
  • 9BAINES P G. Mixing in flows down gentle slopes into stratified environments[J]. J. Fluid Mech., 2001, 443: 237-270.
  • 10HOFMANN H. Mixing at the front of gravity currents[J] Dynamics of Atmospheres and Oceans, 1996, 24: 197-205.

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