Mineral Properties of Euphrates and Shatt Al-Arab River Sediments

Authors

  • Mohanad H Al-Jaberi Geology Department, College of Science, Universty of Basrah, Basrah, Iraq
  • Mohammed L Hussein Geology departments, College of Science, University of Babylon, Babylon, Iraq

DOI:

https://doi.org/10.48165/

Keywords:

Euphrates, Tigris, Shatt Al-Arab, Basrah, Qurna

Abstract

The mineralogical research described in this paper was carried out during 2018, about 30 samples from  twelve river core sediments (from S1 to S12)at six sites in Euphrates and Shatt Al-Arab rivers from  Hilla to Basrah cities . The coordinate number of these cores are between 38°41°32.48′′N– 38°14′24.10′′N latitude and 39°56′4.59′′E–39°8°13.41′′E longitude.The mineralogy is determined by  X- ray diffraction, and reveals that carbonate minerals, quartz, and anorthite feldspar are the main of  light minerals in the different depth intervals, whileKaolinite, palygoreskite and chlorite are the main of  clay minerals. Calcite and dolomite are more abundance than quartz. Calcite is present at high  percentage in Basrah city (S11) compare with the other area.The highest value of dolomite is pointed in  Diwaniya (S4) and Qurna (S9), whereas the lowest in Simawa and Nasiria cities (S5 and S8). The  abundant ratio of quartz reduces to south Euphrates River direction and downward of depth intervals.  Anorthite feldspar is absent inNasiria and Basra, whereas it is present in other sites. Major oxides  represented by SiO2,Al2O3, Fe2O3, CaO, MgO, Na2O, K2O, and TiO2are the main in the sediments, it  detect by Inductively Coupled Plasma – Atomic Emission Spectrometry (ICP-AES) analyses. Silica is  attribute to quartz minerals, while alumina is connect with clay minerals. The domination of calcite  with lack of dolomite reflected in the low content of the MgO. Redox elements (Fe and Ti) contents in  the sediments of studied cores were high within the uppermost part of the profiles, but with increase the  depth it have undergoing some degree of depletion. Sodium is originated from halite, and clay minerals,  while potassium from illite. Micro and nano texture features took place by SEM-EDAX. There are  several of mechanical and chemical features are detected; conchoidal, rounded, pits,and microgranular.  These features resulted from dissolution by river water (chemical) or during long distance of  transportation.  

Downloads

Download data is not yet available.

References

. Hassan, K.M., & Al-Bassam, K.S. (2006). Distribution and ecology of recent mollusks in the Euphrates River–Iraq. Iraqi Bulletin of Geology and Mining, 2(1), 57-66.

. Al-Hashimi, H.A.J., &Amer, R.M. (1985). Tertiary microfacies of Iraq. DG geol. Surv. Min. Invest. Puli., Baghdad, 56pp, 17figs., 159pls.(SOM).

. Jawad Ali, A. (1977). Heavy minerals provinces of the recent sediments of Euphrates-tigris basin. Journal of the Geological Society of Iraq, 10, 33-48.

. Al-Jaberi, M H., & Al-Humaidan, Z.A. (2018). Geochemistry of trace elements in Iraqi marine environment. Bulletin of Pure & Applied Sciences-Geology, 37(2), 172-185.

. Al-Marsoumi, A.M.H., & Al-Jabbri, M.H.A. (2007). Basrah Soils; Geochemical Aspects and Physical Properties-A Review. basrah journal of science, 25 (1C english), 89-103. [6]. Al-Mukhtar, L.E. (2015). Heavy Mineral Analysis of the Quaternary Sediments in the Southern Part of the Mesopotamia Plain, Iraq. Iraqi Bulletin of Geology and Mining, 11(2), 59- 73..

. Al-Rawi, Y., & Sadik, J.M. (1981). Sedimentology of the Dibdibba Clastic Formation, Iraq. J GeolSoc Iraq, 14(1), 55-69.

. Aswad, K.J., Aziz, N.R., &Koyi, H.A. (2011). Cr-spinel compositions in serpentinites and their implications for the petrotectonic history of the Zagros Suture Zone, Kurdistan Region, Iraq. Geological magazine, 148(5-6), 802-818.

. Banat, K.M., & Al-Rawi, Y.T. (1986). Hydrochemestry, clay minerals and carbonates of the Euphrates River. Iraqi J. Sci, 27, 347-362.

. Brumsack, H.J. (2006). The trace metal content of recent organic carbon-rich sediments: implications for Cretaceous black shale formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 232(2-4), 344-361.

. Jassim, S.Z., & Goff, J.C. (2006). Geology of Iraq (p. 341). Brno: Dolin, Prague and Moravian Museum.

. Kahn, A.H., Nolting, R.F., Van der Gaast, S.J., & Van Raaphorst, W. (1992). Trace element geochemistry at the sediment-water interface in the North Sea and the Western Wadden Sea. NIOZ-RAPPORT, 10.

. Kalender, L., &Aytimur, G. (2016). REE Geochemistry of Euphrates River, Turkey. Journal of Chemistry, 2016.

. Aarabi, M.H., Mirhashemi, S.M., Ani, M., &Moshtaghie, A.A. (2011). Comparative binding studies of titanium and iron to human serum transferrin. Asian J Biochem, 6, 191-199. [15]. Margolis, S.V., &Krinsley, D.H. (1971). Submicroscopic frosting on eolian and subaqueous quartz sand grains. Geological Society of America Bulletin, 82(12), 3395-3406.

. Philip, G. (1968). Mineralogy of the recent sediments of Tigris and Euphrates rivers and some of the older detrital deposits. Journal of Sedimentary Research, 38(1), 35-44.

. Roudgarmi, P., &Farahani, E. (2016). Characterization of Sand Dunes to Detect the Sand Source and their Stabilization, Abardej, Iran. International Journal of Geography and Geology, 5(1), 1-9.

. Sissakian, V.K., & Fouad, S.F. (2012). Geological Map of Iraq, scale 1: 1000 000, 4th edit. GEOSURV, Baghdad, Iraq.

Published

2019-10-12

How to Cite

Al-Jaberi, M.H., & Hussein, M.L. (2019). Mineral Properties of Euphrates and Shatt Al-Arab River Sediments . Bulletin of Pure and Applied Sciences-Geology , 38(2), 164–176. https://doi.org/10.48165/