Skip to main content

Advertisement

Log in

Chemical composition of the Zeya River sediments in weathering trend of river sediments of Asia

  • Original Article
  • Published:
Environmental Earth Sciences Aims and scope Submit manuscript

Abstract

The chemical composition of river sediments reflects bedrock geochemistry in the area of erosion and characterizes trend of weathering in the catchment area. The article presents data about chemical composition of Zeya River sediments. This river is one of the largest watercourses in the Amur River basin. The chemical composition of river sediments was analyzed by X-ray fluorescence spectrometry. Compared with the upper continental crust, the river sediments are depleted in almost all analyzed major elements. According to the analysis of major element the ratio, degree of weathering of river sediments in Middle Reach of the Zeya increases down the river. The chemical composition of studied river sediments is close to those in the rivers of northeastern China.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  • Afshar FA, Ayoubi S, Ahmad J (2010) Soil redistribution rate and its relationship with soil organic carbon and total nitrogen using 137Cs technique in a cultivated complex hillslope in western Iran. J Environ Radioact 101:606–614

    Google Scholar 

  • Ahmad I, Chandra R (2013) Geochemistry of loess-paleosol sediments of Kashmir Valley, India: provenance and weathering. J Asian Earth Sci 66:73–89

    Google Scholar 

  • Babechuk MG, Widdowson M, Kamber BS (2014) Quantifying chemical weathering intensity and trace element release from two contrasting basalt profiles, Deccan Traps, India. Chem Geol 363:56–75

    Google Scholar 

  • Besalatpour AA, Ayoubi S, Hajabbasi MA, Mosaddeghi MR, Schulin R (2013) Estimating wet soil aggregate stability from easily available properties in a highly mountainous watershed. Catena 111:72–79

    Google Scholar 

  • Borges JB, Huh Y, Moon S, Noh H (2008) Provenance and weathering control on river bed sediments of eastern Tibetan Plateau and Russian Far East. Chem Geol 254:52–72

    Google Scholar 

  • Chen Y, Li X, Han Z, Yang S, Wang Y, Yang D (2008) Chemical weathering intensity and element migration features of the Xiashu loess profile in Zhenjiang, Jiangsu Province. J Geogr Sci 18:341–352

    Google Scholar 

  • Chesworth W (1973) The residua system of chemical weathering. J Soil Sci 24:69–81

    Google Scholar 

  • Chetsworth W, Dejou J, Larrogue P (1981) The weathering of basalt and relative mobilities of the major elements at Belbex, France. Geochim Cosmochim Acta 45:1235–1243

    Google Scholar 

  • Dalai TK, Krishnaswami S, Sarin MM (2002) Major ion chemistry in the headwater of the Yamuna river system: chemical weathering, its temperature dependence and CO2 consumption in the Himalaya. Geochim Cosmochim Acta 66:3397–3416

    Google Scholar 

  • Edmond JM, Huh Y (1997) Chemical weathering yields from basement and orogenic terrains in hot and cold climates. In: Ruddiman WF (ed) Tectonic uplift and climate change. Plenum Press, New York, pp 329–351

    Google Scholar 

  • Fedo CM, Nesbitt HW, Young GM (1995) Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance. Geology 23:921–924

    Google Scholar 

  • Gaillardet J, Dupré B, Allégre CJ (1999) Geochemistry of large river suspended sediments: silicate weathering or recycling tracer? Geochim Cosmochim Acta 63(23/24):4037–4051

    Google Scholar 

  • Gordeev VV (1983) River flow into the ocean and features of its geochemistry. Nauka, Moscow (in Russian)

    Google Scholar 

  • Harnois L (1988) The CIW index: a new chemical index of weathering. Sed Geol 55(3–4):319–322

    Google Scholar 

  • Hren M, Chamberlain CP, Hilley GE, Blisniuk PM, Bookhagen B (2007) Major ion chemistry of the Yarlung Tsangpo-Brahmaputra River: chemical weathering, erosion, and CO2 consumption in the southern Tibetan Plateau and eastern syntaxis of the Himalaya. Geochim Cosmochim Acta 71:2907–2935

    Google Scholar 

  • Krasny LI, Yunbiao Peng (1999) Geological map of the Amur area and adjacent regions, scale 1:2 500 000. VSEGEI, St. Petersburg

    Google Scholar 

  • Li C, Yang S (2010) Is chemical index alteration (CIA) a reliable proxy for chemical weathering in global drainage basins? Am J Sci 310:111–127

    Google Scholar 

  • Liu Z, Colin C, Huang W, Le KP, Tong S, Chen Z, Trentesaux A (2007) Climatic and tectonic controls on weathering in south China and Indochina Peninsula: clay mineralogical and geochemical investigation from the Pearl, Red, and Mekong drainage basins. Geochem Geophys Geosyst 8(5):2195–2205

    Google Scholar 

  • Liu Z, Tuo S, Colin C, Liu JT, Huang C-Y, Selvaraj K, Chen C-TA, Zhao Y, Siringan FP, Boulay S, Chen Z (2008) Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation. Mar Geol 255(3–4):149–155

    Google Scholar 

  • Makhinova AF, Makhinov AN, Kuptsova VA, Liu S, Ermoshin VV (2014) Landscape-geochemical zoning of the Amur Basin (Russian Territory). Russ J Pac Geol 8(2):138–150

    Google Scholar 

  • Millot R, Gaillardet J, Dupre B et al (2002) The global control of silicate weathering rates and the coupling with physical erosion: new insights from river of Canadian Shield. Earth Planet Sci Lett 196:83–98

    Google Scholar 

  • Muranov AP (ed) (1966) Resources of the surface waters of the USS. Gidrometeoizdat, Leningrad (in Russian)

    Google Scholar 

  • Nessbit HW, Young GM (1982) Early proterozoic climates and plate motion inferred from major element chemistry of lutites. Nature 299:715–717

    Google Scholar 

  • Parker A (1970) An index of weathering for silicate rocks. Geol Mag 107:501–504

    Google Scholar 

  • Qiu S, Zhu Z, Yang T, Wu Y, Bai Y, Ouyang T (2014) Chemical weathering of monsoonal eastern China: implications from major elements of topsoil. J Asian Earth Sci 81:77–90

    Google Scholar 

  • Roaldset E (1972) Mineralogy geochemistry of quaternary clays in the Numedal Area, southern Norway. Norsk Grolisk Tidsskrift 52:335–369

    Google Scholar 

  • Ruxton BP (1968) Measures of the degree of chemical weathering of rock. J Geol 76:518–527

    Google Scholar 

  • Savenko VS (2006) Chemical composition of suspended sediments in rivers of the world. GEOS, Moscow (in Russian)

    Google Scholar 

  • Selvaraj K, Chen TA (2006) Moderate chemical weathering of subtropical Taiwan: constraints from solid-phase geochemistry of sediments and sedimentary rocks. J Geol 114:101–116

    Google Scholar 

  • Shao J, Yang S, Li C (2012) Chemical indices (CIA and WIP) as proxies for integrated chemical weathering in China: inferences from analysis of fluvial sediments. Sed Geol 265–266:110–120

    Google Scholar 

  • Singh P (2010) Geochemistry and provenance of stream sediments of the Ganga River and its major tributaries in the Himalayan region, India. Chem Geol 269:220–236

    Google Scholar 

  • Sirotskii SE, Kharitonova GV, Kim VI, Klimin MA, Chizhikova NP, Tyugai Z, Konovalova NS, Utkina EV (2014) The granulometric and microelemental composition of bottom sediments in the Amur River middle and lower reaches. Russ J Pac Geol 33(3):88–98

    Google Scholar 

  • Sklyarov EV (ed) (2001) Interpretation of geochemical data. Intermet Inzhiniring, Moscow (in Russian)

    Google Scholar 

  • Sorokina OA, Zarubina NV (2011) Chemical composition of the bottom sediments in the middle reaches of the Amur River. Russ J Pac Geol 5(5):469–476

    Google Scholar 

  • Sorokina OA, Zarubina NV (2013) The content of chemical elements in alluvial soils and bottom sediments of the Urkan River (the Amur River Basin). Eurasian Soil Sci 46(6):644–653

    Google Scholar 

  • Taylor SR, McLennan SM (1985) The continental crust: its composition and evolution. Blackwell Scientific Publications, Oxford

    Google Scholar 

  • Viers J, Dupré B, Gaillardet J (2009) Chemical composition of suspended sediments in World Rivers: new insights from a new database. Sci Total Environ 407:853–868

    Google Scholar 

  • Vogt T (1927) Sulitjemafeltets geologi og petrografi. Norges Geologiske Undersokelse 121:1–560

    Google Scholar 

  • Voskresensky SS (1973) Morphology of the Amur-Zeya plain and low mountains of the Small Khingan. University Press Moscow, Russia, p 276

    Google Scholar 

  • Wang H, Liu Z, Sathiamurthy E, Colin C, Li JR, Zhao YL (2011) Chemical weathering in Malay Peninsula and North Borneo: clay mineralogy and element geochemistry of river surface sediments. Sci China Earth Sci 54(2):272–282

    Google Scholar 

  • Wu W, Zheng H, Xu S, Yang J, Liu W (2013) Trace element geochemistry of riverbed and suspended sediments in the upper Yangtze river. J Geochem Explor 124:67–78

    Google Scholar 

  • Yang SY, Jung HS, Li CX (2004) Two unique weathering regimes in the Changjiang and Huanghe drainage basins: geochemical evidence from river sediments. Sed Geol 164:19–34

    Google Scholar 

  • Yang SM, Pitawala A, Ishiga H (2013) Geochemical characteristics of stream sediments, sediment fractions, soil, and basement rocks from the Mahaweli River and its catchment Sri Lanka. Chemie der Erde 73(3):357–371

    Google Scholar 

  • Yudovich YE (1981) Regional geochemistry of sedimentary strata. L.: Nauka, 276 p (in Russian)

  • Yudovich YE, Ketris MP (2000) Foundations of lithochemistry. Nauka, S-Pb (in Russian)

    Google Scholar 

  • Yousefifard M, Ayoubi S, Jalalian A, Khademi H, Makkizaden MA (2012) Mass balance of major elements in relation to weathering in soils developed on igneous rocks in semiarid region, northwestern Iran. J Mt Sci 9:41–58

    Google Scholar 

  • Yousefifard M, Ayoubi S, Poch RM, Jalalian A, Khademi H, Khormali F (2015) Clay transformation and pedogenic calcite formation on a lithosequence of igneous rocks in northwestern Iran. Catena 133:186–197

    Google Scholar 

Download references

Funding

The study was conducted with the support of Russian Foundation for Basic Research, Project no. 18-05-00151.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to O. A. Sorokina.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Sorokina, O.A. Chemical composition of the Zeya River sediments in weathering trend of river sediments of Asia. Environ Earth Sci 79, 49 (2020). https://doi.org/10.1007/s12665-019-8686-1

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12665-019-8686-1

Keywords

Navigation