Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model
Vulnerability assessment and mapping of hazard pollution is raised on as an important management strategy to protect the karst. Karstic aquifers in semi-arid regions of the West of Iran with regard to the natural conditions of the region, are susceptible to contamination. Estimation of amount and vu...
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| Language: | fas |
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Kharazmi University
2019-03-01
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| Series: | تحقیقات کاربردی علوم جغرافیایی |
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| Online Access: | http://jgs.khu.ac.ir/article-1-2880-en.pdf |
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| author | amjad maleki sajad bageri sara mataee |
| author_facet | amjad maleki sajad bageri sara mataee |
| author_sort | amjad maleki |
| collection | DOAJ |
| description | Vulnerability assessment and mapping of hazard pollution is raised on as an important management strategy to protect the karst. Karstic aquifers in semi-arid regions of the West of Iran with regard to the natural conditions of the region, are susceptible to contamination. Estimation of amount and vulnerability mapping of aquifers in the karst religion of Bistoun- Paraw – Kermanshah plain against poullution emissions using the COP model are theaims of this study. This model using of three parameters - covering layer (O), concentration of flow (C) and regime of precipitation (P) - assesses the vulnerability of karst water resources against pollution. The results show that %31/4of the area has located in the zone of average vulnerability and %30/7of area has been in the low vulnerability area and %37/9of the area has taken a very low vulnerabilities value. The later zone has been included most part of the plain. Major areas of low and moderate vulnerabilityzones has been located in the high part of the area on wherethe developed limestone territory of karst formations is found. Vegetation cover of these regions areforest-steppe vegetation where is located in the low vulnerability zone and without vegetation cover where is in the moderate vulnerability zones. The latest has over 800 mm Precipitation. Totally, the Parameters that have most important role in vulnerability level in the areaare C, P and O respectively. |
| format | Article |
| id | doaj-art-eba61bdf492e4050adfb4e01646531c1 |
| institution | Kabale University |
| issn | 2228-7736 2588-5138 |
| language | fas |
| publishDate | 2019-03-01 |
| publisher | Kharazmi University |
| record_format | Article |
| series | تحقیقات کاربردی علوم جغرافیایی |
| spelling | doaj-art-eba61bdf492e4050adfb4e01646531c12025-01-31T17:25:14ZfasKharazmi Universityتحقیقات کاربردی علوم جغرافیایی2228-77362588-51382019-03-011952129145Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Modelamjad maleki0sajad bageri1sara mataee2 Vulnerability assessment and mapping of hazard pollution is raised on as an important management strategy to protect the karst. Karstic aquifers in semi-arid regions of the West of Iran with regard to the natural conditions of the region, are susceptible to contamination. Estimation of amount and vulnerability mapping of aquifers in the karst religion of Bistoun- Paraw – Kermanshah plain against poullution emissions using the COP model are theaims of this study. This model using of three parameters - covering layer (O), concentration of flow (C) and regime of precipitation (P) - assesses the vulnerability of karst water resources against pollution. The results show that %31/4of the area has located in the zone of average vulnerability and %30/7of area has been in the low vulnerability area and %37/9of the area has taken a very low vulnerabilities value. The later zone has been included most part of the plain. Major areas of low and moderate vulnerabilityzones has been located in the high part of the area on wherethe developed limestone territory of karst formations is found. Vegetation cover of these regions areforest-steppe vegetation where is located in the low vulnerability zone and without vegetation cover where is in the moderate vulnerability zones. The latest has over 800 mm Precipitation. Totally, the Parameters that have most important role in vulnerability level in the areaare C, P and O respectively.http://jgs.khu.ac.ir/article-1-2880-en.pdfvulenerabiltymethod copkarstic aquiferspoullutionareforest-steppe. |
| spellingShingle | amjad maleki sajad bageri sara mataee Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model تحقیقات کاربردی علوم جغرافیایی vulenerabilty method cop karstic aquifers poullution areforest-steppe. |
| title | Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model |
| title_full | Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model |
| title_fullStr | Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model |
| title_full_unstemmed | Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model |
| title_short | Assessing Vulenerabilty of Karstic Aquifers in Kermanshah Plain and Bistoon-Parao Mass Using COP Model |
| title_sort | assessing vulenerabilty of karstic aquifers in kermanshah plain and bistoon parao mass using cop model |
| topic | vulenerabilty method cop karstic aquifers poullution areforest-steppe. |
| url | http://jgs.khu.ac.ir/article-1-2880-en.pdf |
| work_keys_str_mv | AT amjadmaleki assessingvulenerabiltyofkarsticaquifersinkermanshahplainandbistoonparaomassusingcopmodel AT sajadbageri assessingvulenerabiltyofkarsticaquifersinkermanshahplainandbistoonparaomassusingcopmodel AT saramataee assessingvulenerabiltyofkarsticaquifersinkermanshahplainandbistoonparaomassusingcopmodel |