首页|川中简阳须家河组地层水化学特征和成因——来自水化学和锶同位素的证据

川中简阳须家河组地层水化学特征和成因——来自水化学和锶同位素的证据

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近年来,四川盆地须家河组致密气勘探开发成果显著,其中川中简阳区块为增储上产新重点关注区域.然而,在开发过程中钻遇了大量地层水,使得储层气相渗透率降低,导致气产量下降,阻碍了下一步的勘探开发,因此,研究区地层水来源和成因亟待研究.文中利用地层水化学参数及锶同位素87Sr/86Sr值对川中天府气田简阳区块须家河组9 口钻井的地层水进行系统分析,结果显示:1)川中简阳地区须家河组地层水为CaCl2型,平均矿化度为85 969.70 mg/L,平均钠氯系数为0.77,平均变质系数为7.72,脱硫系数多为0,平均阳离子交换系数为0.252,指示须家河组地层水处于封闭环境;2)地层水Sr2+,Br-,Li+质量浓度分别为146.00~1 980.00,207.00~1 510.00,2.47~22.60 mg/L,远大于海水,可以作为须家河组地层水特征参数;3)地层水具有Ca2+富集,Na+,Mg2+亏损的特征,该现象与储层中含钙矿物的溶解、钙长石的钠长石化、方解石的白云石化及绿泥石的形成有关;4)地层水的87Sr/86Sr值在0.715 697~0.718 454,表明地层水中的Sr主要来自砂岩储层.研究区钠氯系数和87Sr/86Sr的分布规律高度相似,该参数可以为地层水来源研究提供数据支持.
Hydrochemical characteristics and genesis of Xujiahe Formation formation water in Jianyang,central Sichuan:evidence from hydrochemistry and strontium isotope
In recent years,significant achievements have been made in the exploration and development of tight gas in Xujiahe Formation,Sichuan Basin,with the Jianyang block in central Sichuan being a new focus area for increasing reserves and production.However,in the development process,a large amount of formation water was encountered during drilling,which led to a decrease in reservoir gas permeability,resulting in a gas production decrease and hindering further exploration and development.Therefore,there is an urgent need to study the source and genesis of the formation water in the study area.In this paper,formation water chemical parameters and strontium isotopes are used to systematically analyze the formation water of nine drilling wells in Xujiahe Formation of Jianyang block,Tianfu Gas Field,central Sichuan.The results show that:(1)The formation water of Xujiahe Formation in Jianyang area,central Sichuan is of type CaCl2,with an average mineralization degree of 85 969.70 mg/L,an average sodium chloride coefficient of 0.77,an average metamorphic coefficient of 7.72,a majority of 0 desulfurization coefficients,and an average cation exchange coefficient of 0.252,indicating that the formation water of Xujiahe Formation is in a closed environment.(2)The mass concentration of Sr2+,Br-,and Li+in the formation water is 146.00-1 980.00,207.00-1 510.00,2.47-22.60 mg/L respectively,which is much higher than that of seawater.It can be used as a characteristic parameter for the formation water of Xujiahe Formation.(3)The formation water has the characteristics of Ca2+enrichment and Na+and Mg2+depletion,which is related to the dissolution of calcium-containing minerals in the reservoir,the albitization of calcium feldspar,the dolomitization of calcite,and the formation of chlorite.(4)The 87Sr/86Sr value of formation water is 0.715 697-0.718 454,indicating that the Sr in formation water mainly comes from sandstone reservoirs.The distribution patterns of sodium chloride coefficient and 87Sr/86Sr in the study area are highly similar,and this parameter can provide data support for the study of formation water sources.

water chemical characteristicswater-rock interactionstrontium isotopeformation waterXujiahe Formation

唐友军、徐文畅、王小娟、庞小婷、陈双玲、张晓丽、孙鹏

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长江大学资源与环境学院,湖北武汉 430100

油气资源与勘探技术教育部重点实验室(长江大学),湖北武汉 430100

中国石油西南油气田公司勘探开发研究院四川成都 610000

长江大学石油工程学院,湖北武汉 430100

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水化学特征 水-岩相互作用 锶同位素 地层水 须家河组

国家自然科学基金青年科学基金

42202163

2024

断块油气田
中原石油勘探局

断块油气田

CSTPCD北大核心
影响因子:1.493
ISSN:1005-8907
年,卷(期):2024.31(3)
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