Qualitative and Quantitative Changes of Carbonate Rocks Exposed to SC CO2 (Basque-Cantabrian Basin, Northern Spain)

被引:12
作者
Berrezueta, Edgar [1 ]
Kovacs, Timea [2 ]
Luquot, Linda [3 ]
机构
[1] Inst Geol & Minero Espana, C Matemat Pedrayes 25, Oviedo 33005, Spain
[2] C La Estrecha 46,16Q 4 Izq, Oviedo 33011, Spain
[3] CNRS, Hydrosci Montpellier, 300 Ave Pr Emile Jeanbrau CC57, F-34090 Montpellier, France
来源
APPLIED SCIENCES-BASEL | 2017年 / 7卷 / 11期
关键词
carbonate rocks; SC CO2; SC CO2-rich brine; Quantitative petrography; numerical modelling; MOUNT SIMON SANDSTONE; GEOLOGICAL STORAGE; MECHANICAL-PROPERTIES; DISSOLUTION KINETICS; CALCITE DISSOLUTION; SALT PRECIPITATION; FLOW-RATE; SEQUESTRATION; INJECTION; RESERVOIR;
D O I
10.3390/app7111124
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
This study aims at the qualitative and quantitative determination of porosity, mineralogical and textural changes in carbonate rock samples after injection of (i) supercritical CO2-rich brine and (ii) dry supercritical CO2, under similar experimental conditions (P approximate to 75 bar, T approximate to 35 degrees C, 970 h exposure time and no CO2 flow). The studied rocks were sampled in the western Basque-Cantabrian Basin, North Spain, and consist of vuggy carbonates ("Carniolas") of the Puerto de la Palombera formation (Hettangian). Mineralogical and pore space characterization is completed using optical microscopy, scanning electron microscopy and optical image analysis. In addition, X-ray fluorescence analyses are performed to refine the mineralogical information and to obtain whole rock geochemical data and the brine composition is analysed before and after the experiment. Mineralogical and chemical results indicate that the carbonate rocks exposed to supercritical CO2 in dry conditions do not suffer significant changes. However, the injection of supercritical CO2-rich brine induces chemical and physical changes in the rock due to the high reactivity of calcite at the low pH conditions produced by the acidified brine. Numerical modelling validates the experimental observations. These results can be used to characterize the behaviour of carbonate rocks under conditions similar to the vicinity of a CO2 injection well. The results should be considered only at the scale of the studied samples and not at reservoir scale.
引用
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页数:17
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