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MORADI HARSINI, K., KHAMEHCHIYAN, M., HAFEZI MOGHADAS, N., AMINI, A.. (1385). GEOTECHNICAL PROPERTIES OF BAHMANSHIR SERIES, SOUTHWEST KHUZESTAN, IRAN*. , 31(1), 123-129. doi: 10.22099/ijsts.2007.2322
K. MORADI HARSINI; M. KHAMEHCHIYAN; N. HAFEZI MOGHADAS; A. AMINI. "GEOTECHNICAL PROPERTIES OF BAHMANSHIR SERIES, SOUTHWEST KHUZESTAN, IRAN*". , 31, 1, 1385, 123-129. doi: 10.22099/ijsts.2007.2322
MORADI HARSINI, K., KHAMEHCHIYAN, M., HAFEZI MOGHADAS, N., AMINI, A.. (1385). 'GEOTECHNICAL PROPERTIES OF BAHMANSHIR SERIES, SOUTHWEST KHUZESTAN, IRAN*', , 31(1), pp. 123-129. doi: 10.22099/ijsts.2007.2322
MORADI HARSINI, K., KHAMEHCHIYAN, M., HAFEZI MOGHADAS, N., AMINI, A.. GEOTECHNICAL PROPERTIES OF BAHMANSHIR SERIES, SOUTHWEST KHUZESTAN, IRAN*. , 1385; 31(1): 123-129. doi: 10.22099/ijsts.2007.2322

GEOTECHNICAL PROPERTIES OF BAHMANSHIR SERIES, SOUTHWEST KHUZESTAN, IRAN*

Iranian Journal of Science
مقاله 13، دوره 31، شماره 1، اردیبهشت 2007، صفحه 123-129    اصل مقاله (377.48 K)
نوع مقاله: Research Note
شناسه دیجیتال (DOI): 10.22099/ijsts.2007.2322
نویسندگان
K. MORADI HARSINI* 1؛ M. KHAMEHCHIYAN1؛ N. HAFEZI MOGHADAS2؛ A. AMINI3
1Department of Geology, University of Tarbiat Modares, Tehran, I. R. of Iran
2Department of Geology, University of Shahrood, Shahrood, I. R. of Iran
3Department of Geology, University of Tehran, Tehran, I. R. of Iran
چکیده
Holocene in Southwest Khuzestan is represented by a fluvio-tidal succession termed the
Bahmanshir Series which consists of two clayey layers separated by silty sand to silt beds. This paper
describes the geotechnical properties of the clayey layers that have wide exposure in the lowlands of the
Persian Gulf coast. Studied layers are generally clay sized and consist of a lesser percentage of clay minerals.
Most of the clayey layers have intermediate plasticity, and low potential for expansion. The variation of
physical and engineering properties of the layers from base to top and along the Bahmanshir River is
investigated in this research. The engineering properties of the beds seem to be affected by tidal and river
flow currents and totally by their formation sedimentary environments. Links of the geotechnical data with
geological features as formation sources in the upstream of the basin, the cementation due to the capillary
feature in the floodplain sub-environment and the flocculated texture of clays in the brackish water, have been discussed in this paper. Overall, it is observed that the geotechnical data could be correlated with the
geological features of the Bahmanshir Series.
کلیدواژه‌ها
Bahmanshir؛ series؛ clay؛ geotechnical properties؛ sedimentary environment؛ Holocene
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