پديد آورندگان :
حزباوي، زينب دانشگاه محقق اردبيلي - دانشكده كشاورزي و منابع طبيعي - گروه منابع طبيعي , عزيزي، الهام دانشگاه محقق اردبيلي - دانشكده كشاورزي و منابع طبيعي - گروه منابع طبيعي , شريفي، زهرا دانشگاه محقق اردبيلي - دانشكده كشاورزي و منابع طبيعي - گروه منابع طبيعي , علايي، نازيلا دانشگاه محقق اردبيلي - دانشكده كشاورزي و منابع طبيعي - گروه منابع طبيعي , مصطفي زاده، رئوف دانشگاه محقق اردبيلي - دانشكده كشاورزي و منابع طبيعي - گروه منابع طبيعي , بهزادفر، مرتضي سازمان مديريت و برنامه ريزي استان خراسان شمالي , اسپالويچ، وليبور دانشگاه مونته نگرو - دانشكده فلسفه - گروه جغرافيا
كليدواژه :
اراضي مرتعي , الگوي مكاني , تخريب زمين , شدت فرسايش , هدررفت خاك
چكيده فارسي :
تحقيق حاضر با هدف برآورد مؤلفههاي مرتبط با فرسايش و رسوب با استفاده از مدل (IntErO (Intensity of Erosion and Outflow در حوزه آبخيز كوزهتپراقي، استان اردبيل انجام شد. براي اجراي اين مدل ابتدا 26 داده ورودي شامل ويژگيهاي هندسي، توپوگرافي، حداكثر جريان خروجي، هيدرولوژي، هواشناسي و شدت فرسايش براي كل حوزه آبخيز و 36 زيرحوضه آن استخراج شد. سپس منطبق با استانداردهاي مورد نياز مدل، بانك اطلاعاتي آنها در محيط Excel تهيه و وارد نرمافزار شد. پس از اجراي مدل IntErO، 22 مؤلفه مرتبط با فرآيند فرسايش حوزه آبخيز كوزهتپراقي بهدست آمد. اكثر مؤلفههاي فرسايشي در سطح 36 زيرحوزه آبخيز مورد مطالعه داراي تغييرات مكاني زيادي بوده و اين مساله بيانگر تنوع شرايط اكولوژيكي و بيوفيزيكي در سطح حوزه آبخيز است. در اين پژوهش، حداكثر و حداقل مقدار ضريب شدت فرسايش خاك (Z) در زيرحوضههاي 6 و 10 واقع در بخش شرقي حوضه مورد مطالعه برآورد شد. ميانگين كل رسوب توليدي ناشي از فرسايش سطح حوزه آبخيز (Wgod) برابر با 222854/65مترمكعب در سال بود. علت بالا بودن فرسايش ويژه با مقادير بالاي 200 مترمكعب بر كيلومترمربع در سال در برخي از زيرحوضهها را ميتوان به بهرهبرداري و دخالت شديد صورت گرفته نسبت داد. براساس نتايج به دست آمده مقدار ميانگين و انحراف معيار ضريب تهنشست مجدد رسوبات حاصل از فرسايش (Ru) براي كل حوزه آبخيز برابر با 0/09±0/26 بوده است. مقادير فرسايش خاك واقعي (Ggod) و فرسايش خاك واقعي ويژه (Ggod/km2) برابر با 172704/90 مترمكعب در سال و 215/50 مترمكعب بر كيلومترمربع در سال ارزيابي شد. نتايج مطالعات انجام شده حاكي از نفوذپذيري زياد، درزيرحوضههاي بالادست، است. در اين زيرحوضهها وجود اراضي مرتعي با پوشش گياهي علفزار، موجب نفوذ بيشتر آب در لايه هاي خاك ميشود. نتايج بهدست آمده، در مدلسازي فرآيندهاي مختلف اكولوژيكي، هيدرولوژيكي و مديريتي حوزه آبخيز، اولويتبندي مناطق بحراني و اجراي پايدار و مؤثر اقدامات احيايي و حفاظتي كاربرد دارند.
چكيده لاتين :
1- Introduction
Soil erosion is one of the most important environmental issues that causes various
ecological, social and economic problems. Today, the use of various models for estimating and
predicting hydrological data of watersheds is increasing. Soil erosion risk assessment is a
special form of land resources evaluation, and its purpose is to divide the land into small areas
based on the type of erosion and its amount, which is essential in the soil conservation
planning. Developing comprehensive soil erosion models applicable in different environmental
conditions is highly important. The Intensity of Erosion and Outflow (IntErO) model is a new
graphical model that has a user-friendly software and could present a comprehensive view
from watershed erosional components. Awareness of important coefficients such as watershed
development, river basin tortuousness, erosion energy of the basin's relief, the region's
permeability, vegetation cover, and deposit retention coefficients that provided by IntErO
model has a key role to adapt proper watershed management and conservative measures,
particularly the best management practices (BMPs) that are currently considered by
policymakers and executive managers.
2- Methodology
Due to the positive reports on the proper efficiency of the IntErO model in some parts of the
areas such as Bosnia & Herzegovina, Bulgaria, Croatia, Czech Republic, Italy, Brazil, and
recently in North Khorasan and Kurdistan provinces, the present study was conducted with the
aim of obtaining comprehensive information on the erosional characteristics of the
KoozehTopraghi Watershed located in the southern part of Ardabil Province. The studied
watershed with an area of 801.40 km2 was divided into 36 sub-watersheds according to
topographical and hydrological properties. Totally, the IntErO program package for estimating
soil erosion and sediment yield components uses 26 input data including geometric,
topographic, maximum outflow, hydrological and soil erosion intensity properties. All primary
maps for total watershed and its 36 sub-watersheds were processed and provided in the ArcGIS
10.6 environment. Then, according to the required standards of the model, the data bank was
provided in the Excel 2016 environment and accordingly uploaded to the IntErO software.
Finally, after running the IntErO model, 22 components related to the soil erosion process of
KoozehTopraghi Watershed were obtained.
3- Results
According to the results of the IntErO model, the spatial variability was confirmed in
relation to the most of erosional components through 36 sub-watersheds which indicate the
diversity of ecological and biophysical conditions at the whole watershed. In general, the
maximum and minimum of soil erosion coefficient (Z) were estimated in the sub-watersheds 6
and 10, respectively. According to the obtained results, most of the study sub-watersheds have
experienced severe erosion. It was also found that the mean of the production of erosion
material in the river basin (Wgod) was equal to 222854.65 m3 y-1, respectively whereby it’s
minimum and maximum were obtained in the sub-watersheds 6 and 33, respectively. The
reason for the high amount of specific sediment yield in some sub-watersheds can be attributed
to their severe exploitation for human needs and consequently severe erosion. The results also
showed that the mean value and standard deviation of the coefficient of the deposit retention
(Ru) for the whole watershed was 0.26 ± 0.09. The values of real soil loss (Ggod) and specific
real soil loss (Ggod/km2) were evaluated as 172704.90 m3 y-1 and 215.50 m3 km2 y-1. The
results showed that there was a lot of permeability in the upland sub-watersheds. In these subwatersheds, due to the existence of rangelands and higher vegetation cover, more water
penetrates.
4- Discussion & Conclusions
In general, the results showed that the erosion values at the lowlands of the study watershed
are much higher than at the highlands. The present results are consistent with the other
researches that reported the high level of ecological sensitivity in the lowlands of the
KoozehTopraghi Watershed. The results of the present study can be used as a useful
managerial tool in the field of sustainable agricultural production and optimal use of natural
resources. Finally, it is recommended to compare the applicability of the IntErO model in
different environmental conditions, considering its comprehensiveness in analyzing the
erosional status. The results of this study, in addition to its capability for modeling different
watershed ecological, hydrological and managerial processes, their analysis is useful to
prioritize the critical regions as well as sustainable and effective implantation of restoration and
conservative practices in the KoozehTopraghi Watershed.