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
1393
10
1
gregorian
2015
1
1
1
4
online
1
fulltext
fa
ارزیابی فعالیتهای نو زمینساختی با استفاده از شاخصهای ژئومورفولوژیک در حوضههای آبریز کلانشهر تهران
Assessment of Neotectonic Activities Using Geomorphological Indicators in Tehran Metropolis watersheds
تخصصي
Special
پژوهشي
Research
<p dir="RTL" style="text-align: justify;"><span style="font-family:nasimyw;"><strong>شاخصهای</strong> <strong>ژئومورفیک</strong> <strong>و مورفومتریک</strong> <strong>ابزاری</strong> <strong>برای</strong> <strong>تحلیلهای</strong> <strong>مورفوتکتونیکی</strong> <strong>مناطق</strong> <strong>گوناگون</strong> <strong>محسوب</strong> <strong>میشوند. این</strong> <strong>شاخصها</strong> <strong>به</strong> <strong>صورت ابزار</strong> <strong>شناسایی</strong> <strong>پایه</strong> <strong>برای</strong> <strong>تشخیص</strong> <strong>تغییر</strong> <strong>شکلهای</strong> <strong>تکتونیکی</strong> <strong>یا</strong> <strong>تخمین</strong> <strong>ناپایداری</strong> <strong>نسبی</strong> <strong>فعالیتهای</strong> <strong>تکتونیکی</strong> <strong>در</strong> <strong>منطقهای</strong> <strong>ویژه به</strong> <strong>کار</strong> <strong>میروند. این تحقیق رویکری توصیفی- تحلیلی دارد که با استفاده از مطالعات کتابخانهای با هدف بررسی</strong> <strong>میزان</strong> <strong>فعالیتهای</strong> <strong>نو زمینساختی</strong> <strong>در هفت</strong> <strong>حوضهی آبریز کلانشهر تهران (کن، وسک، فرحزاد، درکه، ولنجک، دربند و دارآباد) صورت گرفت. پژوهش با استفاده از شاخصهای</strong> <strong>سینوزیتهی</strong> <strong>جبههی</strong> <strong>کوهستان (</strong><span dir="LTR">Smf</span><strong>)، پیچوخم رودخانه اصلی (</strong><strong><span dir="LTR">S</span></strong><strong>)، عدمتقارن حوضهی زهکشی (</strong><span dir="LTR">Af</span><strong>)، تراکم سنجی آبراههها (</strong><span dir="LTR">D</span><strong>)، انتگرال هیپسومتریک (</strong><span dir="LTR">HI</span><strong>)، نسبت شکل حوضه (</strong><span dir="LTR">BS</span><strong>)، نسبت پهنای کف دره به ارتفاع آن (</strong><span dir="LTR">Vf</span><strong>)، شاخص گرادیان</strong> <strong>طولی</strong> <strong>رودخانه (</strong><span dir="LTR">SL</span><strong>) انجام شد. سرانجام، فعالیت نسبی همهی حوضهها با استفاده از شاخص تکتونیک فعال (</strong><span dir="LTR">IAT</span><strong>) ارزیابی گردید. شاخصهای مذکور از</strong> <strong>طریق</strong> <strong>نقشههای</strong> <strong>توپوگرافی</strong> <strong>و</strong> <strong>زمینشناسی و تصاویر ماهواره</strong><strong><span dir="LTR">‎</span></strong><strong>ای </strong><span dir="LTR">Google Earth</span><strong> منطقهی مطالعه و با به کار گیری نرمافزارهای</strong> <span dir="LTR">Arc GIS </span><strong>و </strong><span dir="LTR">Global Mapper</span><strong> بررسی و ارزیابی</strong> <strong>شدند. بر اساس شاخص تکتونیک فعال،</strong> <strong>نتایج</strong> <strong>تحقیق</strong> <strong>نشان</strong> <strong>میدهد</strong> <strong>حوضههای کن و دربند در کلاس 2 با فعالیت نئوتکتونیکی بالا و حوضههای وسک، فرحزاد، درکه، ولنجک و دارآباد در کلاس 3 با فعالیت نئوتکتونیکی متوسط قرار گرفتهاند و همهی حوضهها</strong> <strong>به علت وجود گسلهای</strong> <strong>اصلی و فرعی</strong> <strong>منطقه و</strong> <strong>نزدیکی</strong> <strong>به آنها</strong> <strong>دارای</strong> <strong>فعالیت تکتونیکی</strong> <strong>نسبتاً بالایی</strong> <strong>هستند. نتیجه اینکه، با</strong> <strong>توجه</strong> <strong>به</strong> <strong>وجود گسلهای متعدد، فعالیتهای تکتونیکی و سوابق لرزهخیزی در کلان شهر تهران و حوضههای آبریز آن احتمال وقوع زمینلرزه در منطقهی مطالعه دور از انتظار نیست و این مسئله نیازمند توجه جدی و مدیریتی همهجانبه است.</strong></span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">Tectonic geomorphology is part of Earth Sciences, which deal with study of the interaction of tectonic and geomorphology. In other words it studies the effective tectonic processes in forming and changing the landforms. Geomorphic and morphometric indicators are suitable tools to the morphotectonic analysis for different areas. These indicators are used as the base tool to identify and recognition of tectonic deformation or estimates of the relative instability of tectonic activity in a particular region. Some of geomorphic indicators has been widely used, then the results of research projects are used to obtain comprehensive information about active tectonics. Full assessment of contemporary tectonics and tectonic activities, especially the young tectonic and its hazards need to Full understanding of geomorphologic processes speed and made for this purpose, geomorphological methods play an important role in this context.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;"> This research uses a descriptive-analytical approach, using library studies and aims at determininge the activity of Neotectonic in 7 Watersheds of Tehran metropolis (from west to east: Kan, Vesk, Farahzad, Darakeh, Velenjak, Darband and Darabad). In the first step, using topographic and geological maps of under the studied area, faults, drainage networks and watersheds are identified, then to evaluation the indicators of Mountain Front sinuosity (Smf), the main river sinuosity (S), the drainage watershed asymmetry (Af), rivers density index (D), hypsometric integral (HI), the ratio of the watershed shape (BS), the ratio of valley floor width to valley height (Vf), river longitudinal gradient index (SL) and Index active Tectonic(IAT) have been determined. Survey of these indicators by topographic and geologic maps and Google Earth images of the under studied area using software of Google Earth, Arc GIS and Global Mapper are derived and calculated. In the following, parameters and how they are calculated are given:</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">-Mountain Front sinuosity is the result from equation (1):</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">Smf = Lmf / Ls (1)</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">In the equation (1), Smf is index of sinuosity Mountain Front. Lmf is the front along the foothills and mountains of the specified slope failure and Ls: straight line along the front of the mountain.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">- The main river sinuosity index is as follows: S = C / V. In this formula, S is main river sinuosity. C: along of the river. V: valley along of the straight line.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">- Rivers density index, drainage density is obtained from the formula:</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;"> µ= </span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">Li is length in kilometers of drainage Watershed, A is area in square kilometers, μ is total drainage watershed in terms of kilometers per square kilometer.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">- Hypsometric integral is an indicator which represents the distribution of surface heights variation from equation (2) is obtained:</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">HI= H - Hmin / H max – H min (2)</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">In this equation Hi is hypsometric integral, Hmin and Hmax respectively are the minimum and maximum height and H is the height of watershed.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">- The ratio of width to height of the valley floor is another geomorphologic parameters to investigate the tectonic forces in the region .This index is obtained from the equation (3):</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">VF = (3)</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">VF, represents the relationship of the valley floor width to valley height, VFW: the valley, Eld and Erd to the height of the left and right and Esc is valley floor elevation valley.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">- The ratio of the area ratio of the area and the equation (4) is obtained:</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">BS= Bl / BW (4)</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">-BS; the shape of the watershed; Bl; length dividers watershed of water to the bottom of the watershed outlet and BW: width of the flat portion of the watershed.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">-The longitudinal gradient index (SL) for a range of drainage path is calculated and determined by the relationship: SL = (ΔH / Δ L) * L. In this regard, SL: the longitudinal gradient index, ΔH: height difference between two points measured, ΔL: during the interval and L: total length of the specified channel to assess where the index to the highest point of the canal.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">The classification provided for indicators Sl, Smf, Vf, Bs, Af by Homduni et al (2008), this indicator is obtained based on the amount of 1, 2, 3 classified in three classes. Index of active tectonic (Iat) Geomorphic indicators by means of different classes Calculated based on the value of (S /n) is divided into four classes, That the division are characterized by class 1 with very high activity Neotectonic, Class 2 with high Neotectonic activity, Class 3 with medium Neotectonic activities and and Class 4 with low Neotectonic activity. In this classification of Class1 have the highest and Class 3 have the lowest Neotectonic activities (Table11).</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">On the basis of Iat indicator Neotectonic activities in the under studied area were assessment and results were is in table (13). Based on the data in Table (13) , watersheds of Kan and Darband hava a high Neotectonic activities and located in Class 2 and watersheds of Vesk, Frahzad, Darakeh, Velenjak and Darabad have a medium Neotectonics activities and and located in Class 2, and Neotectonic activities are a high relative tectonic activity in all watersheds. Geomorphic indicators are reflecting activities in the metropolitan Tehran watersheds can say that tectonically active watershed has not yet reached stability and tectonic activity are relatively high. Geomorphologic indicators drainage watershed asymmetry, the main river sinuosity, the valley floor width to height ratio of density of rivers and valleys, structural geology and tectonic activity in the7watersheds of Tehran metropolis better show it.</span></p>
<p style="text-align: justify;"><span style="font-family:times new roman;">The results show that Tehran metropolis Watersheds have a high relative tectonic activity in all watersheds, because of the proximity to the major faults (such as Mosha- Fasham and North Tehran faults) and minor faults, tectonic activity exists. Finally it can be stated that, due to the presence of multiple faults and background seismicity and tectonic activity in Tehran metropolis and its watersheds, occurrence of earthquakes in the study area is not unexpected and this issue requires serious consideration and management.</span></p>
ارزیابی, نو زمینساخت, شاخصهای ژئومورفولوژیک, حوضه های آبریز, کلانشهر تهران.
Neotectonic activities, Geomorphological indicators, Tehran metropolis.
1
22
http://jsaeh.khu.ac.ir/browse.php?a_code=A-10-1-25&slc_lang=fa&sid=1
Amir
Saffari
اسماعیل
نجفی
amirsafari@yahoo.com
1003194753284600658
1003194753284600658
No
دانشگاه خوارزمی
Amir
Saffari
امیر
صفاری
1003194753284600659
1003194753284600659
Yes
دانشگاه خوارزمی
Ezatollah
Ghanavati
عزت الله
قنواتی
1003194753284600660
1003194753284600660
No
دانشگاه خوارزمی
Amir
karam
امیر
کرم
1003194753284600661
1003194753284600661
No
دانشگاه خوارزمی