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جستجوی مقالات
سه شنبه 15 مهر 1404
Ecopersia
، جلد ۱، شماره ۱، صفحات ۲۳-۳۹
عنوان فارسی
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کلیدواژههای فارسی مقاله
عنوان انگلیسی
Antecedent Rainfall Thresholds for the Triggering of Deep-Seated Landslides (Case study: Chaharmahal & Bakhtiari Province, Iran)
چکیده انگلیسی مقاله
Rainfall is recognized as one of the main triggering factors of landslides. Researchers have long attempted to determine the amount of precipitation required to trigger slope failures. One of the landslide zones in Iran is Chaharmahal & Bakhtiari province where many landslides cause high casualties in recent decades. It is significant that most of these landslides occur after a rainy period. Thus, determination of rainfall thresholds in this province seems to be necessary as the first step to present an effective landslide warning system. In this research, we tried to introduce some antecedent rainfall thresholds for deep-seated landslides. The antecedent periods considered for the events examined in this study were 5, 10, 15, 20, 25, 28 and 30 days. Since most of landslides occurred by cumulative rainfall for more than 10 days, the results of 5 days and shorter time periods appear not logically connected. We have also established rainfall thresholds for the 15-day antecedent period and 2, 3 and 5 days rainfall events. Results indicate that for 10 to 30 days antecedent periods, mean total rainfall needed to induce landslides varies between about 140 and 280 mm. Finally, we recommend more research on relation between rainfall characteristics and destabilization of different soil classes in the study area (especially clayey-marly deposits).
کلیدواژههای انگلیسی مقاله
نویسندگان مقاله
| Ali Reza Nafarzadegan
Yazd University, Yazd
| Ali Talebi
Yazd University, Yazd
| Hossein Malekinezhad
Yazd University, Yazd
| Naeim Emami
Res. Cent. of Agri. and Nat. Res., Shahrekord
نشانی اینترنتی
http://journals.modares.ac.ir/browse.php?a_code=A-24-1000-1922&slc_lang=en&sid=24
فایل مقاله
اشکال در دسترسی به فایل - ./files/site1/rds_journals/391/article-391-590647.pdf
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en
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