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. (1395). تغییرات خاک‌های پیرامون دریاچه ارومیه: ویژگی‌های فیزیکوشیمیایی و کانی‌شناسی. سامانه مدیریت نشریات علمی, 30(1), 81-94. doi: 10.22092/ijsr.2015.106322
. "تغییرات خاک‌های پیرامون دریاچه ارومیه: ویژگی‌های فیزیکوشیمیایی و کانی‌شناسی". سامانه مدیریت نشریات علمی, 30, 1, 1395, 81-94. doi: 10.22092/ijsr.2015.106322
. (1395). 'تغییرات خاک‌های پیرامون دریاچه ارومیه: ویژگی‌های فیزیکوشیمیایی و کانی‌شناسی', سامانه مدیریت نشریات علمی, 30(1), pp. 81-94. doi: 10.22092/ijsr.2015.106322
. تغییرات خاک‌های پیرامون دریاچه ارومیه: ویژگی‌های فیزیکوشیمیایی و کانی‌شناسی. سامانه مدیریت نشریات علمی, 1395; 30(1): 81-94. doi: 10.22092/ijsr.2015.106322

تغییرات خاک‌های پیرامون دریاچه ارومیه: ویژگی‌های فیزیکوشیمیایی و کانی‌شناسی

پژوهش های خاک
مقاله 8، دوره 30، شماره 1، خرداد 1395، صفحه 81-94    اصل مقاله (829.67 K)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.22092/ijsr.2015.106322
چکیده
تغییرات ویژگی­های فیزیکوشیمیایی و کانی­شناسی خاک­های مجاور دریاچه اورمیه در دو گروه اراضی متأثر و غیرمتأثر از دریاچه در منطقه دیزج­دول مورد بررسی قرار گرفتند. تجزیه واریانس خصوصیات فیزیکوشیمیایی خاک­ها نشان داد که مقدار OC و CEC خاک­های دو ردیف اراضی در سطح احتمال 1% و مقادیر EC، SAR،ESp و سدیم تبادلی آنها در سطح احتمال 1/0%تفاوت معنی­داری داشتند، ولی  تفاوت عمق خاک و مقدار رس آن معنی­دار نشد. مطالعات کانی­شناسی حضور کانی­های اسمکتایت، ایلایت، کائولینایت، کلرایت و ورمی­کولایت را در خاک­های هر دو ردیف اراضی نشان داد. منشا ایلایت، کلرایت، کائولینایت توارث از مواد مادری و منشا اسمکتایت و ورمی­کولایت پدوژنیک بوده و از تغییرشکل ایلایت حاصل شده­اند. در خاکرخ­های واقع در اراضی متأثر از دریاچه، نوتشکیلی عامل اصلی تشکیل اسمکتایت می­باشد. مقایسه کانی­شناسی رس خاک­های دو ردیف اراضی نشان داد که پیشروی دریاچه اورمیه طی سال­های 1376-1375سبب حضور مقادیر خیلی بیشتر اسمکتایت و حضور ورمی­کولایت با هیدروکسی بین­لایه­ای (HIV) در خاک­های متأثر از دریاچه گردیده است.
کلیدواژه‌ها
اسمکتایت؛ کانی های رس؛ نوتشکیلی
عنوان مقاله [English]
Changes in Soils Around Urmia Lake: Physicochemical and Mineralogical Properties
چکیده [English]
Differences in physicochemical and mineralogical properties of soils close to Urmia Lake in two groups of soils (affected and unaffected by Urmia Lake), were studied in Dizaj-Dol region. Variance analysis of physicochemical properties of these soils showed that the values of OC and CEC in these two groups of soils were significantly different (P ≤ 0.1), and the values of EC, SAR, ESP and exchangeable Na of these soils were highly significantly different (P ≤ 0.01). However, soil depth and clay content in these two groups of soils were not significantly different. Clay mineralogical studies showed the presence of smectites, illites, kaolinites, chlorites and vermiculites in both groups of soils. Illites, chlorites and kaolinites are inherited from parent material, while smectites and vermiculites have pedogenic origin and have been formed via transformation of illite. In the soils which have been affected by Urmia Lake, neoformation from soil solution is the main origin of smectites. Comparision of clay minerals in the two groups of soils showed that the rising level of Urmia Lake during 1994-1995 caused the presence of high amounts of smectite and some hydroxy interlayer vermiculite in the soils affected by Urmia Lake.
کلیدواژه‌ها [English]
Clay minerals, Neoformation, Smectites, Illites
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