globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6441047
论文题名:
鄂尔多斯盆地马家沟组马五_1亚段地层水特征及对CO_2地质封存的意义
其他题名: Water characteristics of Majiagou formation Ma5_1 submember in Ordos Basin and the significance for CO_2 geological sequestration
作者: 孙玉景1; 周立发1; 霍斐斐1
刊名: 地球环境学报
ISSN: 1674-9901
出版年: 2019
卷: 10, 期:1, 页码:8098-8106
语种: 中文
中文关键词: 马五1亚段 ; 矿化度 ; 卤水 ; CO_2封存 ; 鄂尔多斯盆地
英文关键词: Ma51 submember ; mineralization ; brine ; CO_2 sequestration ; Ordos Basin
WOS学科分类: MINERALOGY
WOS研究方向: Mineralogy
中文摘要: CO_2地质封存技术是实现碳减排的有效措施,对鄂尔多斯盆地马家沟组马五_1亚段地层水特征进行研究,是下一步实施工程化CO_2封存的首要前提。本文依据对深部钻井取样的直观观察与实验测试,采用单项指标分类评价和多项指标综合评价的方法深入分析了马家沟组马五_1亚段地层水的物理性质、化学性质、地层水类型和水化学特征参数。结果表明:马家沟组马五_1亚段地层水密度较大、矿化度极高,属于卤水,含量最多的离子是Cl-,其次是Ca~(2+),地层水是CaCl_2型。钠氯系数、氯镁系数、脱硫系数和镁钙系数的分析表明马五_1亚段地层水封闭性极好,处于较强的还原环境。综合分析认为马家沟组马五_1亚段地层水具备实施CO_2封存的良好条件,非常适宜进行CO_2封存。
英文摘要: Background, aim, and scope Global warming caused by emission of greenhouse gases dominated by CO_2 has become a severe challenge to human being. Many measures have been taken to combat global warming all over the world. What is worth mentioning is the CO_2 geological sequestration, it is an effective and burgeoning measure to achieve carbon emission reduction. The CO_2 sequestration potential is very huge in Ordos Basin. So, in this paper the formation water characteristics in Ma5_1 submember of Majiagou formation are systematically studied, which is the precondition for further engineering design of CO_2 sequestration in Ordos Basin. Materials and methods Based on the direct observations and experimental tests of deep drilling samplings, the method of single index classification evaluation and multiple index comprehensive evaluation is adopted. The physical properties, chemical properties, formation water types and hydrochemical characteristic parameters of the Majiagou formation Ma5_1 submember are analyzed in detail. Results The results indicate that the pH of the water ranges from 3.5 to 8.6, mainly from 4.5 to 6.5; the water density ranges from 1.0 g · cm~(-3) to 1.5 g · cm~(-3), mostly 1.1 1.3 g · cm~(-3); the mineralization degree is generally greater than 50 g · L~(-1), and average mineralization degree is 166 g · L~(-1); the highest concentration ion is Cl~-, followed by Ca~(2+); the concentration order of the ions is r Cl~-> r Ca~(2+)>r ( Na~+ + K~+ ) >rHCO_3-Mg~(2+)>rSO_4~(2-)>r , and the formation water is CaCl_2 type. The analysis results of water chemical characteristic parameters show that Na / Cl factor (r Na~+ / r Cl~-) ranges from 0.18 to 0.55, 0.34 on average; Cl / Mg factor (r Cl~-/ r Mg~(2+)) ranges from 11.04 to 165.16, 32.11 on average; desulfurization factor (100 * rSO_4~(2-)/ r Cl~-) ranges from 0 to 0.45, 0.09 on average; Mg / Ca factor (r Mg~(2+) / r Ca~(2+)) range from 0.01 to 0.30, 0.17 on average. Discussion Most samples have a pH of 4.5 6.5, which does not meet the drinking water standard (6.5 8.5). The density is generally 1.1 1.3 g · cm~(-3), indicating that the salinity may be high.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/155580
Appears in Collections:气候变化事实与影响

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作者单位: 1.西北大学地质学系
2.二氧化碳捕集与封存技术国家地方联合工程研究中心, 大陆动力学国家重点实验室
3.二氧化碳捕集与封存技术国家地方联合工程研究中心, 西安
4.西安,
5.710069
6.710069

Recommended Citation:
孙玉景,周立发,霍斐斐. 鄂尔多斯盆地马家沟组马五_1亚段地层水特征及对CO_2地质封存的意义[J]. 地球环境学报,2019-01-01,10(1):8098-8106
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