مقایسه‎ ‎خصوصیات‎ ‎خاک‌های زیست بوم بیابانی با پوشش گیاهی متفاوت‏ ‏ (مطالعه موردی: جنوب غربُ سیستان)‏

محورهای موضوعی : منابع طبیعی و جنگلداری و مراتع

منصور جهان تیغ ¹ , معین جهان‌تیغ ²

1 - دانشیار بخش منابع و آبخیزداری مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی سیستان، سازمان تحقیقات، آموزش و ترویج کشاورزی، زابل
2 - دکتری آبخیزداری

تاریخ دریافت : 1395/09/19 تاریخ پذیرش : 1401/03/07 تاریخ انتشار : 1401/01/01

کلید واژه: ‎ ‎‏ مناطق بیابانی, جنوب غرب سیستان‏, خصوصیات‎ ‎فیزیکی‎ ‎شیمیایی, نمونه‌های خاک,

چکیده مقاله :

هدف: هدف از انجام این پژوهش بررسی خصوصیات فیزیکی شیمیایی خاک‌های مناطق بیابانی با پوشش گیاهی متفاوت می‌باشد. این پژوهش در دو منطقه تاسوکی و ترش‌آب (جاریکا) واقع در جنوب غرب سیستان که دارای دو پوشش گیاهی متفاوت گز و تاغ هستند صورت پذیرفت. روش بررسی: برای اجرای این تحقیق، ابتدا با استفاده از نقشه‌ توپوگرافی محدوده مورد مطالعه مشخص و با استفاده از GPS کنترل گردید. با توجه به شرایط اکولوژیکی و فیزیوگرافی منطقه 4 نمونه خاک از هر محل (عمق 45-0 سانتی‌متر) برداشت و خصوصیات، pH، EC، مواد آلی، کربن آلی، ازت، کربنات کلسیم، درصد رطوبت اشباع، درصد رطوبت خاک، کلسیم، پتاسیم، سدیم، فسفر، منزیم، مقدار نسبت جذب سدیم، کلر و بافت خاک اندازه‌گیری شد. همچنین پوشش گیاهی منطقه مورد شناسایی قرار گرفت. داده‌ها با استفاده از برنامه آماری SPSS مورد تجزیه و تحلیل قرار گرفت. یافته ها: نتایج نشان داد که بین ویژگی‌های pH، ازت، فسفر، رطوبت، منزیم و سیلت نمونه‌های خاک دو منطقه مورد مطالعه در سطح 05/0 اختلاف معنی‌داری وجود ندارد. (05/0P>) ولی بین مواد آلی، کربن آلی، کربنات کلسیم، کلسیم، پتاسیم، سدیم، کلر، نسبت جذب سدیم، رس و شن در سطح 01/0 اختلاف معنی‌داری وجود دارد (01/0P<). بحثونتیجه گیری: نتیجه‌گیری می‌شود خاک‌های دو منطقه مورد بررسی دارای محدودیت برای توسعه پوشش گیاهی نمی‌باشند.

چکیده انگلیسی:

Objective: The objective of the study was to compare the desert environments soil physical and chemical characteristics with different vegetation types. This study has done in southwestern of Sistan region (Tasoki and Torsh Ab). Study Method: The study areas were distinguished based on geologic maps in scales of 1:50,000 and field observations, and global positioning system (GPS). Four soil samples were taken from the 0-45 cm depth at each location and analyzed for pH, EC, organic matter, organic carbon, nitrogen, CaCO3, ESP, potassium, moisture, sodium, phosphorus, magnesium, calcium, sodium adsorption ratio, chlorine and texture. Dates were analyzed using SPSS software.  Findings: The data indicated that there are no statistically significant differences between soil properties including: pH, nitrogen, phosphorus, moisture, magnesium, and silt, at the 0.05 levels (p> 0.05). But, there are statistically significant differences between soil properties including: organic matter, organic carbon, CaCO3, ESP, potassium, sodium adsorption ratio, calcium, clay and sand were statistically significant at the 0.05 levels (p< 0.01). Concluded: Concluded that the study area soil no limits to incrase of vegetation cover. The studies concluded that there were no soil limite for incrase of vegetation cover in study area.

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