عنوان مقاله :
ارزيابي بخش هاي پايدار و ناپايدار فلزات سنگين (Fe, Mn, Cr, Ni) در رسوبات سطحي حوزه جنوبي درياي خزر دو ايستگاه( تنكابن و اميرآباد )
پديد آورندگان :
زرشناس، رامين نويسنده 1- دانشكده محيطزيست وانرژي، دانشگاه آزاد اسلامي واحد علوم و تحقيقات تهران، ايران ، صندوق پستي: 14515/775 , , نصر اله زاده ساروي، حسن نويسنده 2- پژوهشكده اكولوژي درياي خزر، موسسه تحقيقات علوم شيلاتي كشور، سازمان تحقيقات، , , فرشچي، پروين نويسنده 1- دانشكده محيطزيست وانرژي، دانشگاه آزاد اسلامي واحد علوم و تحقيقات تهران، ايران ، صندوق پستي: 14515/775 , , نجف پور، شعبان نويسنده ,
كليدواژه :
رسوبات سطحي , فلزات سنگين , استخراج پي درپي , درياي خزر
چكيده فارسي :
بررسي آلودگي فلزات سنگين در رسوبات براي ارزيابي احتمال آلودگي در يك منطقه، از اهميت ويژه اي برخوردار است.يكي از روش هاي تشخيص دخالت هاي انساني و ورود آلاينده هايي با منشا انساني به محيط هاي آبي، بررسي ميزان غلظت فلزات سنگين در رسوبات مي باشد.(Zhou et al., 2007)
چكيده لاتين :
This study was conducted to determine some heavy metals (Fe, Mg, Cr, Ni) of surface sediment in
the southern Caspian Sea during two seasons (Summer and Winter) in 2014-2015. 36 surface
sediments samples (with triplicate) were collected at two stations (Tonekabon and Bandar
Amirabad). All samples were analyzed using sequential extraction to indicate natural and
anthropogenic sources. The results indicated that the percentage of non-resistance fraction in
Tonekabon area were measured 3.5,45.0, 22.1 and 6.0 for Fe, Mg,Cr, Ni, respectively and in
Amirabad area were 23.0,2.6,1.8 and 4.0, respectively. On the other hand, the percentage of
resistance fraction values were obtained 96.5, 55.0, 77.9 and 94.0 in Tonekabon, and 77.0, 97.4,
98.2, and 96.0 in Amirabad region. The chemical speciation of Fe, Mg, Cr, Ni in most sampling
stations were in the order of residual > oxidisable-organic > acid-reducible > exchangeable. The
order of total concentration, non-resistance and resistance fraction were observed Fe > Mn > Ni > Cr,
Mn > Fe > Ni > Cr and Fe > Mn > Ni > Cr, respectively. As a conclusion, results of total concentration,
resistnace and non-resistance of Fe, Mn, Ni and Cr were lower than standard and earth shell (Igeo)
in this area. This is shown that surface sediments of this area were not polluted with these heavy
metals and bioavaiable fraction provides little indication of potential interactions with the biotic
components present in this environment.
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