Chemistry of major and minor elements,87Sr/86Sr,δD,δ18O and δ34S of brines were measured from Tertiary strata and Quaternary salt lakes in the western Qaidam Basin.The water chemistry data show that all oilfield br...Chemistry of major and minor elements,87Sr/86Sr,δD,δ18O and δ34S of brines were measured from Tertiary strata and Quaternary salt lakes in the western Qaidam Basin.The water chemistry data show that all oilfield brines are CaCl2 type.They were enriched in Ca2+,B3+,Li+,Sr2+,Br-,and were depleted in Mg2+,SO42-,which indicated that these brines had the characteristics of deeply circulated water.The relationship between δD and δ18O shows that all data of these brines decline towards the Global Meteoric Water Line(GWL) and Qaidam Meteoric Water Line(QWL),and that the intersection between oilfield brines and Meteoric Water Lines was close to the local spring and fresh water in the piedmont in the western Qaidam Basin.The results suggest that oilfield brines has initially originated from meteoric water,and then might be affected by water-rock metamorphose,because most oilfield brines distribute in the range of metamorphosing water.The 87Sr/86Sr values of most oilfield brines range from 0.71121 to 0.71194,and was less than that in salt lake water(>0.712),but close to that of halite in the study area.These imply that salt dissolution occurred in the process of migration.In addition,all oilfield brines have obviously much positive δ34S values(ranging from 26.46‰ to 54.57‰) than that of salt lake brines,which was caused by bacterial sulfate reduction resulting in positive shift of δ34S value and depleteed SO42-in oilfield brines.Combined with water chemical data and δD,δ18O,87Sr/86Sr,δ34S values,we concluded that oilfield brines mainly originate from the deeply circulated meteoric waters,and then are affected by salt dissolution,water-rock metamorphose,sulfate reduction and dolomitization during the process of migration.These processes alter the chemical compositions of oilfield brines and accumulate rich elements(such as B,Li,Sr,Br,K and so on) for sustainable utilization of salt lake resources in the Qaidam Basin.展开更多
We analyzed the ^(87)Sr/^(86)Sr ratios of basaltic rocks and basin water in Xuyi,China,and found a big difference,which may challenge conventional wisdom on the contribution of basalt weathering in end-member analysis...We analyzed the ^(87)Sr/^(86)Sr ratios of basaltic rocks and basin water in Xuyi,China,and found a big difference,which may challenge conventional wisdom on the contribution of basalt weathering in end-member analysis.Results of an in-house weathering experiment suggest that rainwater and dust are not responsible for the difference.By isolating the major minerals in basalt,we found that plagioclase has much higher ^(87)Sr/^(86)Sr ratios than bulk basalt and basin water,which might explain the difference in ^(87)Sr/^(86)Sr ratios of basalt and basin water.We inferthatlow-temperaturehydrothermalalteration increased the ^(87)Sr/^(86)Sr ratios of plagioclase.Future analyses of end-member contribution in a mixed-rock basin should take into account that basin water and plagioclase have higher ^(87)Sr/^(86)Sr ratios than basaltic rocks.展开更多
目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectr...目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectrometry,TIMS)分析检测^(87)Sr/^(86);样品用锡囊包裹后,利用元素分析-稳定同位素比质谱法分析检测δ^(13)C;利用SPSS 25.0软件对进口大麦的^(87)Sr/^(86)Sr和δ^(13)C进行正态性验证、方差分析、事后多重比较分析和判别分析。结果不同进口国大麦中的^(87)Sr/^(86)Sr和δ^(13)C具有显著性差异,经判别分析,进口自澳大利亚、法国和美国的大麦可以达到100%正确判别率,整体正确判别率达到86.2%,若将美国和加拿大进口的大麦归类为北美洲进口大麦,则可实现进口自北美、法国和澳大利亚大麦的100%正确判别率。结论利用^(87)Sr/^(86)Sr和δ^(13)C可以对不同进口国大麦进行产地溯源分析。展开更多
基金supported by CAS Major Basic Preliminary Program (2004CCA03500)the National Natural Science Foundation of China (No. 40603007)
文摘Chemistry of major and minor elements,87Sr/86Sr,δD,δ18O and δ34S of brines were measured from Tertiary strata and Quaternary salt lakes in the western Qaidam Basin.The water chemistry data show that all oilfield brines are CaCl2 type.They were enriched in Ca2+,B3+,Li+,Sr2+,Br-,and were depleted in Mg2+,SO42-,which indicated that these brines had the characteristics of deeply circulated water.The relationship between δD and δ18O shows that all data of these brines decline towards the Global Meteoric Water Line(GWL) and Qaidam Meteoric Water Line(QWL),and that the intersection between oilfield brines and Meteoric Water Lines was close to the local spring and fresh water in the piedmont in the western Qaidam Basin.The results suggest that oilfield brines has initially originated from meteoric water,and then might be affected by water-rock metamorphose,because most oilfield brines distribute in the range of metamorphosing water.The 87Sr/86Sr values of most oilfield brines range from 0.71121 to 0.71194,and was less than that in salt lake water(>0.712),but close to that of halite in the study area.These imply that salt dissolution occurred in the process of migration.In addition,all oilfield brines have obviously much positive δ34S values(ranging from 26.46‰ to 54.57‰) than that of salt lake brines,which was caused by bacterial sulfate reduction resulting in positive shift of δ34S value and depleteed SO42-in oilfield brines.Combined with water chemical data and δD,δ18O,87Sr/86Sr,δ34S values,we concluded that oilfield brines mainly originate from the deeply circulated meteoric waters,and then are affected by salt dissolution,water-rock metamorphose,sulfate reduction and dolomitization during the process of migration.These processes alter the chemical compositions of oilfield brines and accumulate rich elements(such as B,Li,Sr,Br,K and so on) for sustainable utilization of salt lake resources in the Qaidam Basin.
基金Support for this work comes from National Natural Science Foundation of China(Grant No.41422205)
文摘We analyzed the ^(87)Sr/^(86)Sr ratios of basaltic rocks and basin water in Xuyi,China,and found a big difference,which may challenge conventional wisdom on the contribution of basalt weathering in end-member analysis.Results of an in-house weathering experiment suggest that rainwater and dust are not responsible for the difference.By isolating the major minerals in basalt,we found that plagioclase has much higher ^(87)Sr/^(86)Sr ratios than bulk basalt and basin water,which might explain the difference in ^(87)Sr/^(86)Sr ratios of basalt and basin water.We inferthatlow-temperaturehydrothermalalteration increased the ^(87)Sr/^(86)Sr ratios of plagioclase.Future analyses of end-member contribution in a mixed-rock basin should take into account that basin water and plagioclase have higher ^(87)Sr/^(86)Sr ratios than basaltic rocks.
文摘目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectrometry,TIMS)分析检测^(87)Sr/^(86);样品用锡囊包裹后,利用元素分析-稳定同位素比质谱法分析检测δ^(13)C;利用SPSS 25.0软件对进口大麦的^(87)Sr/^(86)Sr和δ^(13)C进行正态性验证、方差分析、事后多重比较分析和判别分析。结果不同进口国大麦中的^(87)Sr/^(86)Sr和δ^(13)C具有显著性差异,经判别分析,进口自澳大利亚、法国和美国的大麦可以达到100%正确判别率,整体正确判别率达到86.2%,若将美国和加拿大进口的大麦归类为北美洲进口大麦,则可实现进口自北美、法国和澳大利亚大麦的100%正确判别率。结论利用^(87)Sr/^(86)Sr和δ^(13)C可以对不同进口国大麦进行产地溯源分析。
