Journal of Spatial Analysis Environmental Hazards
تحلیل فضایی مخاطرات محیطی
Journal of Spatial Analysis Environmental Hazards
Literature & Humanities
http://jsaeh.khu.ac.ir
1
admin
2423-7892
2588-5146
10.61186/jsaeh
fa
jalali
1394
1
1
gregorian
2015
4
1
2
1
online
1
fulltext
fa
بررسی سطح ایستابی آب زیرزمینی دشت اردبیل
Evaluation of the groundwater table using multi-criteria decision making and spatial analysis, case study: Ardebil Plain
تخصصي
Special
پژوهشي
Research
<p dir="RTL" style="margin-right: 26.05pt; text-align: justify;"><span style="font-family:nasimyw;"><span style="font-size: 14px;"><strong>آبهای زیرزمینی</strong> <strong>منبع</strong> <strong>بسیار</strong> <strong>مهمی</strong> <strong>برای</strong> <strong>تأمین</strong> <strong>آب</strong> <strong>مصرفی</strong> <strong>در</strong> <strong>بخشهای کشاورزی،</strong> <strong>صنعت</strong> <strong>و</strong> <strong>شرب</strong> <strong>دشت اردبیل</strong> <strong>است. ازاینرو، بررسی تغییرات منابع آب زیرزمینی در برنامهریزی و مدیریت پایدار این منابع اهمیت فراوانی دارد. در این پژوهش، هدف سطحبندی وضعیت دهستانهای موجود در دشت اردبیل بهلحاظ بحران آب زیرزمینی و تغییرات آن طی سالهای 1360 و 1391 است. بنابراین، از اطلاعات 39 چاه پیزومتری موجود در سطح دشت اردبیل (اخذشده از سازمان آب منطقهای) استفاده شد. با استفاده از تکنیک وزندهی جمعی سادهی فازی و روشهای درونیابی، سطح ایستابی پیزومترها درونیابی و نحوهی تغییرات سطح ایستابی آنها طی این دو دوره نمایش داده شدند. سپس، نقشهی نهایی فازیشده و وزندار از دو نقشهی سال 60 و سال 91 تهیه گردید. نتایج تحلیل، کاهش تقریباً 47 درصدی سطح ایستابی را در سال 1391 نسبتبه سال 1360 نشان میدهد. سرانجام، با استفاده از اطلاعات بهدست آمده میتوان گفت که دهستانهای شرقی، ویلکیج مرکزی و فولادلوی شمالی بیشترین تغییرات را بهلحاظ افت سطح آب زیرزمینی داشتهاند که قسمت شرق و جنوب شرق دشت را شامل میشوند. همچنین، دهستانهای شمالی دشت نیز به سمت بحران پیش میروند که، با توجه به نقشهی سطح کشت و تراکم چاه عمیق، برداشت بیش از حد از منابع آب زیرزمینی را در این ناحیه میتوان عامل اصلی بحران قلمداد کرد. </strong></span></span></p>
<p style="text-align: justify;">Groundwater resources are important sources for the supply of water in agriculture, industry and drinking in Ardabil plain, therefore underground water resources planning and sustainable management of these resources are important. The purpose of this study is grading the villages in the plain of Ardabil in underground water crisis and changes during the years 1360-1391. The information obtained from 39 wells, piezometers in plain of Ardabil. Using simple techniques and fuzzy cumulative weighting and interpolation methods, the piezometers interpolation of shallow water table and how it changes during the period is showd.</p>
<p style="text-align: justify;">Introduction<br>
Groundwater is one of the main sources of drinking water supply for many people around the world, especially in rural areas. Groundwater can be contaminated by natural or human activities are numerous. All activities including residential, municipal, commercial, industrial and agriculture can affect groundwater quality<span dir="RTL">.</span> Groundwater contamination can result, such as the loss of a source of water supply, high cost of clearing the high cost of alternative water supply or cause potential health problems. Given the importance of determining the results of the plains of the country, the aim of this study was to determine changes in aquifer storage of Ardabil using statistics and analysis on multi-criteria decision-making and evaluation of groundwater is a crisis situation.</p>
<p style="text-align: justify;">Data and Methods</p>
<p style="text-align: justify;"> In this study, the data of piezometers wells in of Ardabil plain scattered through the city of Ardabil Regional Water Authority have been prepared. Also, the surface layers and point to the plains of Ardabil, political divisions and the location of wells, piezometers villages for final maps have been used. The data of deep wells, as well as cultivation of four major product with a high water requirement of wheat, barley, potatoes and forage to determine the relationship between ground water and water harvesting has been a drop in water table<span dir="RTL">.</span></p>
<p style="text-align: justify;">The study area</p>
<p style="text-align: justify;"> Plain study area is located in the north-west of Iran in Ardabil province (Figure 2 and Figure 3). The average height is about 1360 meters above sea level It covers an area of approximately 820 square kilometers and is located in the Gharasoo watershed.</p>
<ul>
<li style="text-align: justify;">Inverse Distance Weight;</li>
<li style="text-align: justify;">Global Polynomial Interpolation;</li>
<li style="text-align: justify;">Local Polynomial Interpolation;</li>
<li style="text-align: justify;">Radial Basis Functions;</li>
<li style="text-align: justify;">Straight Ranking;</li>
<li style="text-align: justify;">Fuzzy Normalized;</li>
<li style="text-align: justify;">Fuzzy multi-criteria decision-making;</li>
<li style="text-align: justify;">FSAW.</li>
</ul>
<p style="text-align: justify;"> The first step is to evaluate each process and required hydrological data collection, and the coordinatingits location. The geostatistical methods of IDW, GPI, LPI, and RBF in the ArcGIS software were used for interpolating all existing data and a drop in water table in the area of standards for grades 10 class (raster) within restricted fields of Ardebil were determined.</p>
<p style="text-align: justify;"> Finally, using simple collective weight, weight-bearing layers and layers of loss data water table for the years 60 and 90 is obtained. To get the final map of water table drops, the two layers are deducted and the final map of Ardabil plain water table drop that phase is obtained.</p>
<p style="text-align: justify;"> Analysis showed the reduction of water table almost 47 percent in 1391 compared to 1360. As can be seen in Figures 12 and 13, maximum of 45 meters water table wells, piezometers in 1360 to more than 70 m in 1390 has come to reveal the deterioration of the aquifer Ardabil.</p>
<p style="text-align: justify;"> Pholadloo_e_Shomali district with the highest concentration of deep wells in the near future to continue the removal of existing deep wells, groundwater resources will go into sharp decline.</p>
<p style="text-align: justify;"> Sharghi Village goes to the crisis and in the meantime, the central Vilkij district includes the eastern part of the plain, the drop in water table aquifer at greatest risk to the two villages in East and Central Vilkij.</p>
<p style="margin-left: 14.2pt; text-align: justify;">• Due to the limitations of traditional agricultural development potential ground water;<br>
• Increase the efficiency of irrigation, changing crop patterns of water needed to fill low-power consumption;<br>
• Efficient use of water resources and prevent unauthorized digging deep wells to exploit the nutritional front, especially in the East and Southeast plains.</p>
تصمیمگیری چند معیاری فازی, آب زیرزمینی, سطح ایستابی, تحلیل فضایی, دشت اردبیل.
fuzzy multi-criteria decision, groundwater, water table, spatial analysis, Ardabil plain.
31
42
http://jsaeh.khu.ac.ir/browse.php?a_code=A-10-1-4&slc_lang=fa&sid=1
Hashem
Rostamzadeh
هاشم
رستم زاده
1003194753284600695
1003194753284600695
No
دانشگاه تبریز
Esmaeil
Asadi
اسماعیل
اسدی
1003194753284600696
1003194753284600696
No
دانشگاه تبریز
Jafar
Jararzadeh
جعفر
جعفرزاده
jjafar1364@gmail.com
1003194753284600697
1003194753284600697
Yes
دانشگاه تبریز