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جلالی, سعیده, نصرتی, کاظم, بهرامی, شهرام. (1403). تعیین سهم نسبی کاربری اراضی در تولید رسوب با استفاده از شاخص‌های هوازدگی در حوضه آبخیز چهل چای. سامانه مدیریت نشریات علمی, 38(3), 287-304. doi: 10.22092/ijsr.2024.366332.752
سعیده جلالی; کاظم نصرتی; شهرام بهرامی. "تعیین سهم نسبی کاربری اراضی در تولید رسوب با استفاده از شاخص‌های هوازدگی در حوضه آبخیز چهل چای". سامانه مدیریت نشریات علمی, 38, 3, 1403, 287-304. doi: 10.22092/ijsr.2024.366332.752
جلالی, سعیده, نصرتی, کاظم, بهرامی, شهرام. (1403). 'تعیین سهم نسبی کاربری اراضی در تولید رسوب با استفاده از شاخص‌های هوازدگی در حوضه آبخیز چهل چای', سامانه مدیریت نشریات علمی, 38(3), pp. 287-304. doi: 10.22092/ijsr.2024.366332.752
جلالی, سعیده, نصرتی, کاظم, بهرامی, شهرام. تعیین سهم نسبی کاربری اراضی در تولید رسوب با استفاده از شاخص‌های هوازدگی در حوضه آبخیز چهل چای. سامانه مدیریت نشریات علمی, 1403; 38(3): 287-304. doi: 10.22092/ijsr.2024.366332.752

تعیین سهم نسبی کاربری اراضی در تولید رسوب با استفاده از شاخص‌های هوازدگی در حوضه آبخیز چهل چای

پژوهش های خاک
دوره 38، شماره 3، آذر 1403، صفحه 287-304    اصل مقاله (1.55 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.22092/ijsr.2024.366332.752
نویسندگان
سعیده جلالی1؛ کاظم نصرتی* 2؛ شهرام بهرامی3
1گروه جغرافیای طبیعی، دانشکده علوم زمین، دانشگاه شهید بهشتی، تهران، ایران.گروه جغرافیای طبیعی، دانشکده علوم زمین، دانشگاه شهید
2گروه جغرافیای طبیعی، دانشکده دانشکده علوم زمین، دانشگاه شهید بهشتی، تهران،
3گروه جغرافیای طبیعی، دانشکده علوم زمین، دانشگاه شهید بهشتی ، تهران، ایران
چکیده
مسأله­ی مهم و قابل توجه در پژوهش‌های کاربردی برای مدیریت حوزه‌های آبخیز، آگاهی از چگونگی فرآیند تولید رسوب حوضه­های آبخیز است. در دو دهه­ی اخیر، منشأیابی رسوب به عنوان یک روش مناسب برای تعیین منابع رسوب استفاده می­شود. هدف از این پژوهش بررسی سهم انواع منابع سطحی(جنگل، مرتع، کشاورزی و باغ) و زیرسطحی(کناره آبراهه) در تولید رسوب با استفاده از تکنیک منشأیابی رسوب با کاربرد شاخص های هوازدگی در حوزه آبخیز چهل­چای استان گلستان بود. برای این منظور، در مرحله­ی اول، نمونه رسوب معلق طی هشت رخداد سیلاب در بازه­ی زمانی بهمن 1399 تا فروردین 1400 برداشته شد. شاخص های هوازدگی بر اساس غلظت ردیاب­های ژئوشیمیایی محاسبه شد. پس از آزمون‌های دامنه، کروسکال-والیس و تحلیل تشخیص،  شاخص تغییر شیمیایی (CPA)، نسبت آ ال کا(ALK)، شاخص منیزیوم (MgIndex)، شاخص بی ای1(ba1) و شاخص کالمگ (CALMAG Index) که بالاترین درصد توان تفکیک­پذیری را داشتند برای تعیین سهم منابع تولید رسوب انتخاب شدند.  نتایج اجرای مدل منشأیابی در حوضه آبخیز چهل چای نشان داد که در بین منابع سطحی و زیرسطحی، کاربری کشاورزی، 6/88% کل رسوب را تولید می­کند. سهم سایر کاربری­ها به ترتیب مرتع(1/4%)، باغ(3/2%) و آبراهه 5% بود. با آگاهی از سهم بالای زمین های کشاورزی در تولید رسوب، طراحی و اجرای عملیات حفاظت خاک  متناسب با موقعیت منطقه، امری ضروری به شمار می­آید.
کلیدواژه‌ها
منشأیابی رسوب؛ حفاظت خاک؛ فرسایش خاک؛ ردیاب‌های ژئوشیمیایی
عنوان مقاله [English]
Determining the Relative Contribution of Land Use in Sediment Yield by Using Weathering Indices in Chehl Chay Watershed
نویسندگان [English]
Saeedeh Jalali1؛ Kazem Nosrati2؛ Shahram Bahrami3
1Department of Physical Geography, Faculty of Earth sceince Science, University of Shaheid Beheshti, Tehran, Iran.
2Department of Physical Geography, Earth science Science, University of Shaheid Beheshti, Tehran
3Department of Physical Geography, Earth sceince Science, University of Shaheid Beheshti, Tehran, Iran.
چکیده [English]
A significant issue in applied research for the management of watersheds is to know the integrated sediment yield process in watershed. In the recent decades, sediment fingerprinting method was proven as one of the key methods for determining contribution of sediment proportion. This study's purpose was to determine the relative source contribution of surface (forest, pasture, agriculture and gardening) and sub-surface (bank erosion) in sediment yield by using weathering indices in Chehel-Chaye Catchment, Golestan Province, Iran. In eight flood events, suspended sediment sampling was done in March to April 2021.  Thirty-six weathering indices were calculated. After Bracket, Kruskal-Wallis, and Discernment Function Analysis, CPA,ALK, MgIndex, ba1, CALMAG Index  had the highest discernment percentage in all of the tracers. Based on Bayesian mixing model, the highest proportion of suspended sediment was produced by agricultural land (88/6%), followed by pasture (4/1%), forest (2/3%), and bank erosion(5%) of the suspended sediment. Thus, knowing the high contribution of agriculture in sediment yield, it is necessary to design and implement soil conservation operations according to the location of the watershed.
کلیدواژه‌ها [English]
Sediment tracing, Soil conservation, Soil erosion, Geo-chemical tracers
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