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2. School of Mines Engineering, North China University of Science and Technology, Tangshan 063009, China;
3. The Second Geological Brigade of Hebei Geology and Mineral Exploration Bureau, Tangshan 063004, China;
4. Qinggong College, North China University of Science and Technology, Tangshan 064000, China, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=iMMTdIovf6tJ4QIrJGSUJQ==, pdfFileSize=12113507, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1242135293659259686, articleId=1242135289506898699, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=乙酸条件下方解石溶解特征及其地质意义, columnId=1146540929516700224, journalTitle=科技导报, columnName=研究论文, runingTitle=null, highlight=null, articleAbstract=针对方解石溶解的显微岩相学特征难以识别的问题,以纯净方解石为对象,依据松辽盆地扶余油层地质条件,通过乙酸-方解石相互作用实验,研究了方解石的溶解特征及其地质意义。结果表明,方解石在不同温度下发生尺度不同的溶解作用及质量损失,离子质量浓度呈现规律性变化,Ca2+ 离子浓度为684.68~1255.25 mg/L,HCO3 - 离子浓度为2239~3821 mg/L,矿化度为3088~5456 mg/L;方解石溶解的显微岩相学特征包括残余锥、残余细晶叠瓦状排列、齿状残余锥、瘤状残余锥及尖锐残余锥等;乙酸条件下方解石最适合的溶解温度为100~130℃。这项研究可为方解石溶解地质特征鉴定、油气藏储层成岩作用及次生孔隙预测等提供一定的理论基础。, authors=王明格1,2 , 宋土顺2 , 徐九华1 , 李占芳3 , 田壮4 , 刘胜昌2 , authorsList=王明格, 宋土顺, 徐九华, 李占芳, 田壮, 刘胜昌, authorCompany=1. 北京科技大学资源工程系, 北京 100083;
2. 华北理工大学矿业工程学院, 唐山 063009;
3. 河北省地矿局第二地质大队, 唐山 063004;
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科技导报
| 研究论文 2016, 34(18): 230-235
乙酸条件下方解石溶解特征及其地质意义
全屏
王明格1,2 , 宋土顺2 , 徐九华1 , 李占芳3 , 田壮4 , 刘胜昌2
作者信息
1. 北京科技大学资源工程系, 北京 100083;
2. 华北理工大学矿业工程学院, 唐山 063009;
3. 河北省地矿局第二地质大队, 唐山 063004;
4. 华北理工大学轻工学院, 唐山 064000
Characteristics and geological significance of calcite dissolution under acetic acid conditions
Affiliations
出版时间: 2016-09-28
doi: 10.3981/j.issn.1000-7857.2016.18.031
文章导航
针对方解石溶解的显微岩相学特征难以识别的问题,以纯净方解石为对象,依据松辽盆地扶余油层地质条件,通过乙酸-方解石相互作用实验,研究了方解石的溶解特征及其地质意义。结果表明,方解石在不同温度下发生尺度不同的溶解作用及质量损失,离子质量浓度呈现规律性变化,Ca2+ 离子浓度为684.68~1255.25 mg/L,HCO3 - 离子浓度为2239~3821 mg/L,矿化度为3088~5456 mg/L;方解石溶解的显微岩相学特征包括残余锥、残余细晶叠瓦状排列、齿状残余锥、瘤状残余锥及尖锐残余锥等;乙酸条件下方解石最适合的溶解温度为100~130℃。这项研究可为方解石溶解地质特征鉴定、油气藏储层成岩作用及次生孔隙预测等提供一定的理论基础。
Since it is difficult to identify microscopic petrographic features of calcite dissolution, we take, pure calcite as the research object, and base on the Fuyu reservoir geological conditions of Songliao basin to study the calcite dissolution characteristics and geological significance through acetic acid-calcite interaction experiments. Results show the followings. Ccalcite is found of having different scale dissolutions and mass losses in different temperatures; ion concentration show regular changes, with Ca2+ ion concentration being 684.68~1255.25 mg/L, HCO3 - ion concentration 2239~3821 mg/L, salinity 3088~5456 mg/L; calcite dissolution microscopic features include residual cone, residual fine crystal imbricate arrangement, dentate residual cone, tumor residual cone, residual sharp cone, etc.; under the acetic acid condition the most suitable temperature for calcite dissolution is 100~130℃. This study provides a certain theoretical basis for the identification of geological features of calcite dissolution reservoir and the function of reservoir into rock, and secondary porosity prediction.
calcite
/
dissolution characteristics
/
dissolution temperature
/
acetic acid
王明格, 宋土顺, 徐九华, 李占芳, 田壮, 刘胜昌.
乙酸条件下方解石溶解特征及其地质意义.
科技导报,
2016
, 34
(18)
: 230
-235
.
DOI: 10.3981/j.issn.1000-7857.2016.18.031
WANG Mingge, SONG Tushun, XU Jiuhua, LI Zhanfang, TIAN Zhuang, LIU Shengchang.
Characteristics and geological significance of calcite dissolution under acetic acid conditions[J].
Science & Technology Review ,
2016
, 34
(18)
: 230
-235
.
DOI: 10.3981/j.issn.1000-7857.2016.18.031
2016年第34卷第18期
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文章信息
doi: 10.3981/j.issn.1000-7857.2016.18.031
接收时间:2016-01-04
首发时间:2016-10-21
出版时间:2016-09-28
收稿日期:2016-01-04
修回日期:2016-05-06
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2016.18.031
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2种不同金属材料的力学参数
科 Family 属数 Number of genus 种数 Number of species 占总种数比例 Percentage of total species (%) 属 Genus 种数 Number of species 占总种数比例 Percentage of total species (%) 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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