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南翼山油田卤水低温结晶过程研究
引用本文:李青海,顾同欣,于升松,姚燕,李冰,李武. 南翼山油田卤水低温结晶过程研究[J]. 物理化学学报, 2011, 27(8): 1803-1808. DOI: 10.3866/PKU.WHXB20110823
作者姓名:李青海  顾同欣  于升松  姚燕  李冰  李武
作者单位:1. State Key Laboratory of Frozen Soil Engineering Cold and Arid Regions Environmental & Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000;2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008;3. Graduate University of Chinese Academy of Sciences, Beijing 100049
基金项目:国家自然科学基金(41073023); 国家十一五科技支撑计划项目(2006BAB09B07)资助~~
摘    要:自行设计搭建了一套油田水低温冷冻实验设备, 使用该设备研究了南翼山油田原始卤水在-18.90 °C到-30.90 °C范围内的结冰析盐过程, 精确测量了油田水随温度降低第一种和第二种固相的析出温度. 化学分析得到了该温度范围内Ca2+、Mg2+、K+、Cl-、B2O3、Na+六种常量组分在液相中的含量变化趋势. 使用低温X射线衍射法对原始卤水在低温下得到的固相进行了初步的鉴定, 并对南翼山油田水的低温相变过程进行了实时监测. 实验结果表明: 南翼山油田水降温至-19.10 °C析出第一种盐NaCl·2H2O, 降至-23.55 °C同时析出冰和NaCl·2H2O.

关 键 词:油田卤水  冷冻  NaCl·2H2O    低温X射线衍射  
收稿时间:2011-03-28
修稿时间:2011-06-21

Study on the Precipitation Pathway of Nanyishan Oilfield Brine at Subzero Temperatures
LI Qing-Hai,GU Tong-Xin,YU Sheng-Song,YAO Yan,LI Bing,LI Wu. Study on the Precipitation Pathway of Nanyishan Oilfield Brine at Subzero Temperatures[J]. Acta Physico-Chimica Sinica, 2011, 27(8): 1803-1808. DOI: 10.3866/PKU.WHXB20110823
Authors:LI Qing-Hai  GU Tong-Xin  YU Sheng-Song  YAO Yan  LI Bing  LI Wu
Affiliation:1. State Key Laboratory of Frozen Soil Engineering Cold and Arid Regions Environmental & Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000;2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008;3. Graduate University of Chinese Academy of Sciences, Beijing 100049
Abstract:The crystallization processes of oilfield brine components from the Nanyishan area at temperature between-18.90 and-30.90 ℃ were studied by a self-designed refrigeration instrument and the precipitation temperatures of the first and second salts were measured accurately.The concentrations of the major ions(Ca2+,Mg2+,K+,Cl-,B2O3,Na+) in the liquid phase of the brine at different temperatures(from-18.90 to-30.90 ℃) were determined by chemical analyses.The solids obtained at low temperature were identified and the phase changes of the oilfield brine at temperatures between-10.0 and-30.0 ℃ were monitored in situ by subzero temperature X-ray powder diffraction.The results show that the first salt(hydrohalite) precipitates at-19.10 ℃ and the ice and NaCl·2H2O co-precipitate at-23.55 ℃.
Keywords:Oilfield brine  Freezing  Hydrohalite  Ice  X-ray diffraction at subzero temperature  
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