OXYGEN ISOTOPE OF QUARTZ IN SEDIMENTS FROM THE YANGTZE (CHANGJIANG) AND YELLOW(HUANGHE) RIVERS

QIAO Shu-qing; YANG Zuo-sheng; LI Yun-hai; CHEN Xiao-hui

Marine Geology & Quaternary Geology > 2006 > 26(3): 15-19.

QIAO Shu-qing, YANG Zuo-sheng, LI Yun-hai, CHEN Xiao-hui. OXYGEN ISOTOPE OF QUARTZ IN SEDIMENTS FROM THE YANGTZE (CHANGJIANG) AND YELLOW(HUANGHE) RIVERS[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 15-19.

Citation:

PDF (308 KB)

OXYGEN ISOTOPE OF QUARTZ IN SEDIMENTS FROM THE YANGTZE (CHANGJIANG) AND YELLOW(HUANGHE) RIVERS

Institute of Estuarine Coastal Studies, Ocean University of China, Qingdao 266003, China

More Information

Received Date: October 18, 2005
Revised Date: December 22, 2005

Graphical Abstract

Abstract

Abstract

Quartz in sediments from the Yangtze and Yellow Rivers was separated by potassium hydrogen sulfate (KHSO₄) fusing-hydrofluorosilic acid (H₂SiF₆). Oxygen was extracted from the quartz fraction by BrF₅ (used as oxidant), and then its isotopic composition was analyzed by mass-spectrometer, expressed as δ¹⁸O (¹⁸O/¹⁶O)values (relative to SMOW). The results show that δ¹⁸O values generally increase with grain size of quartz changing from coarse to fine. The oxygen isotope ratios (δ¹⁸O) of quartz from the Yangtze River are higher than those from the Yellow River. The differences in δ¹⁸O values of the same grain-size quartz between the Yangtze and Yellow Rivers may have resulted from different sediment sources and climate conditions along these two river basins.
- quartz,
- sediment,
- oxygen isotope ratio,
- the Yangtze River,
- the Yellow River

FullText(HTML)

References (19)

References

[1]	汤奇成,熊怡.中国河流水文[M].北京:科学出版社,1998:127-153.[TANG Qi-cheng, XIONG Yi. Hydrological Characteristics of Rivers in China[M]. Beijing:Science Press,1998:127 -153.]
[2]	任美锷.任美锷地理论文选[M].北京:商务印书馆,1991:368-385.[REN Mei-e. REN Mei-e's Thesis about Geography[M]. Beijing:The Commercial Press, 1991:368 -385.]
[3]	Kiely P V, Jackson M L. Quartz, feldspar, and mica determination for soils by sodium pyrosulfate fusion[J]. Soil Sci. Amer. Pro., 1965, 29:159-163.
[4]	Clayton R N, Jackson M L, Sridhar K. Resistance of quartz silt to isotopic exchange under burial and intense weathering conditions[J]. Geochim. Cosmochim. Acta.,1978,42:1517-1522.
[5]	Jackson M L. Oxygen isotope ratios in quartz as an indicator of provenance of dust[J]. Geological Society of America-Special Paper, 1981, 186:27-36.
[6]	Aléon Jérôme, Chaussidon Marc, Marty Bernard, et al. Oxygen isotopes in single micrometer-sized quartz grains:tracing the source of Saharan dust over long-distance atmospheric transport[J]. Geochimica et Cosmochimica Acta, 2002, 66(19):3351-3365.
[7]	GU Zhao-yan, LIU Tung-sheng, ZHENG Shu-hui. A preliminary study on quartz isotope in Chinese loess and soil[C]//Aspects of Loess Research. Beijing:China Ocean Press, 1987:291-301.
[8]	Mizota C, Matsuhisa Y. Isotopic evidence for the eolian origin of quartz and mica in soils developed on volcanic materials in the Canary Archipelago[J]. Geoderma, 1995, 66:313-320.
[9]	Mizota C, Faure K, Yamamoto M. Provenance of quartz in sedimentary mantles and laterites overlying bedrock in West Africa:evidence from oxygen isotopes[J]. Geoderma, 1996,72:65-74.
[10]	Xiao J L, Yoshio Inouchi, Liu Tungsheng. Eolian quartz flux to Lake Biw, central Japan, over the past 145000 years[J]. Quaternary Research, 1997, 48:48-57.
[11]	侯圣山,杨石岭,丁仲礼.风成沉积物4~16μm石英氧同位素记录及其物质来源意义[J].中国科学D辑,2003,33(6):535-542. [HOU Sheng-shan, YANG Shi-ling, DING Zhong-li. Oxygen isotope compositions of quartz grains (4~16μm) from Chinese eolian deposits and their implications for provenance[J]. Science in China (Series D), 2003, 33(6):535-542.]
[12]	中华人民共和国国家标准(GB/T 13909-92)[S]. 海洋调查规范:海洋地质地球物理调查.北京:国家技术监督局,1992:11-28.[GB/T 13909-92 [S]. Specification for oceanographic survey-Marine geology and geophysics investigation. Beijing:1992:11-28.]
[13]	万世明,蒋恒毅,李安春.海洋沉积物中石英单矿物的化学分离[J].海洋地质与第四纪地质,2003,23(3):123-127. [WAN Shi-ming, JIANG Heng-yi, LI An-chun. Chemical separation of quartz from marine sediment samples[J]. Marine Geology and Quaternary Geology, 2003, 23(3):123-127.]
[14]	孙有斌.黄土样中石英单矿物的分离[J].岩矿测试,2001,20(1):23-26. [SUN You-bin. Separation of quartz minerals from loess samples[J]. Rock and Mineral Analysis, 2001, 20(1):23-26.]
[15]	李延河,万德芳,张国柄,等.氧化物、硅酸盐矿物的氧同位素分析方法-BrF₅法[C]//稳定同位素分析方法研究进展.北京:科学技术出版社,1992:37-43.[LI Yan-he, WAN De-fang, ZHANG Guo-bing, et al. An analysis method of oxygen isotope in oxide and silicates -BrF₅ method[C]//Advance in Analysis Methods of Stable Isotopes. Beijing:Science Press, 1992 :37-43.]
[16]	YANG Shou-ye, JUNG Hoi-Soo, LI Cong-xian. Two unique weathering regimes in the Changjiang and Huanghe drainage basins:geochemical evidence from river sediments[J]. Sedimentary Geology, 2004, 169:19-34.
[17]	CHEN Jing-sheng, WANG Fei-yue, XIA Xing-hui, et al. Major element chemistry of the Changjiang (Yangtze River)[J]. Chemical Geology, 2002, 187:231-255.
[18]	REN Mei-e, SHI Yun-liang. Sediment discharge of the Yellow River (China) and its effect on the sedimentation of the Bohai and the Yellow Sea[J]. Cont. Shelf Res., 1986, 6:785-810.
[19]	孙继敏.中国黄土的物质来源及其粉尘的产生机制与搬运过程[J].第四纪研究,2004,24(2):175-183. [SUN Ji-min. Provenance, forming mechanism and transport of loess in China[J]. Quaternary Sciences, 2004, 24(2):175-183.]

[1]	LIN Xinru, XIAO Guoqiao, YANG Jilong, PAN Qing, ZHAO Qingyu, LIANG Meiyan. The Yellow River never flows into the sea through the Yongding River[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 46-54. DOI: 10.16562/j.cnki.0256-1492.2024013103
[2]	XING Lvyang, LI Guangxue, LIU Siyu, LI Haonan, PAN Yufeng. Formation of the Diaokou Lobe in Yellow River Delta[J]. Marine Geology & Quaternary Geology, 2023, 43(4): 97-104. DOI: 10.16562/j.cnki.0256-1492.2023040901
[3]	AI Lina, HAN Zongzhu, WU Xiao, BI Naishuang, WANG Houjie. Geochemical characteristics of clay-sized sediments of the Yangtze and Yellow Rivers and their implications for provenance[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 109-118. DOI: 10.16562/j.cnki.0256-1492.2019050603
[4]	XUE Chunting, LIU Jian, KONG Xianghuai. CHANNEL SHIFTING OF LOWER YELLOW RIVER IN 1128-1855AD AND ITS INFLUENCE TO THE SEDIMENTATION IN BOHAI, YELLOW AND EAST CHINA SEAS[J]. Marine Geology & Quaternary Geology, 2011, 31(5): 25-36. DOI: 10.3724/SP.J.1140.2011.05025
[5]	CHANG Fangqiang, JIA Yonggang. DISASTERS CAUSED BY WAVE-INDUCED SEDIMENT LIQUEFACTION AT THE YELLOW RIVER DELTA,CHINA[J]. Marine Geology & Quaternary Geology, 2011, 31(2): 43-48. DOI: 10.3724/SP.J.1140.2011.02043
[6]	YANG Xiujuan, JIA Yonggang, LIU Hongjun, SHAN Hongxian. RESEARCH ON CONSOLIDATION CHARACTERISTICS AND ORIGIN OF THE YELLOW RIVER ESTUARY SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 29-34. DOI: 10.3724/SP.J.1140.2009.05029
[7]	QIAO Shu-qing, YANG Zuo-sheng. COMPARISON OF RARE EARTH ELEMENT COMPOSITIONS IN DIFFERENT GRAIN-SIZE FRACTIONS OF SEDIMENTS FROM THE YANGTZE AND YELLOW RIVERS AND THE SEA[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 9-16.
[8]	TANG Min, YANG Shou-ye, LI Bao-hua, LI Cong-xian, WANG Qiang, ZHAO Quan-hong. COMPOSITIONS OF ORGANIC CARBON AND NITROGEN AND CARBON ISOTOPE OF POSTGLACIAL SEDIMENTS IN THE YANGTZE RIVER DELTA AND THE PALEOENVIRONMENT IMPLICATION[J]. Marine Geology & Quaternary Geology, 2006, 26(5): 1-10.
[9]	BIE Jun, HUANG Hai-jun, FAN Hui, BI Shi-pu. GROUND SUBSIDENCE OF THE MODERN YELLOW RIVER DELTA AND ITS CAUSES[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 29-35.
[10]	WU Jing-lu, LIN Lin, ZENG Hai-ao, ZHANG En-lou, YANG Xiang-dong. CHARACTERISTICS OF OXYGEN ISOTOPIC COMPOSITION OF THE LAKES ALONG THE MID-LOWER REACHES OF THE YANGTZE RIVER[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 53-56.

Cited By

Cited by

Periodical cited type(2)

1.	陈能，邱彬焕，张杰，余欢，刘演，El Said Shetaia，孙千里，于俊杰，陈静. 沉积成因Sr/Ba指示的福建潮控海湾全新世沉积环境及海平面意义. 海洋地质与第四纪地质. 2024(05): 95-106 . 本站查看
2.	黄晓，葛晨东，殷勇，纪振强，丁俊英. 扬子浅滩MIS6阶段沉积物流体包裹体特征及物源分析. 矿物岩石地球化学通报. 2023(05): 1173-1181 .

Other cited types(0)

Get Citation

PDF

XML

Article views (1599) PDF downloads (9) Cited by(2)

Turn off MathJax

Article Contents

Abstract

References

OXYGEN ISOTOPE OF QUARTZ IN SEDIMENTS FROM THE YANGTZE (CHANGJIANG) AND YELLOW(HUANGHE) RIVERS