Arid
DOI10.1016/j.earscirev.2020.103086
Frequency of boulders transport during large floods in hyperarid areas using paleoflood analysis - An example from the Negev Desert, Israel
Greenbaum, Noam1; Schwartz, Uri1; Carling, Paul2; Bergman, Nathaniel1; Mushkin, Amit3; Zituni, Rami1; Halevi, Rafi4; Benito, Gerardo5; Porat, Naomi3
通讯作者Greenbaum, Noam
来源期刊EARTH-SCIENCE REVIEWS
ISSN0012-8252
EISSN1872-6828
出版年2020
卷号202
英文摘要Direct measurements of boulder entrainment in desert wadis are not available. The 2004 flood (peak discharge 470 m(3) s(-1); recurrence interval - 120 years) in the hyperarid, ungauged Nahal Hatzera ephemeral stream (45 km(2)), transported and deposited 0.85-2.1 m concrete boulders and slabs detached from infrastructure upstream and natural boulders. EDM and drone air-photographic surveys documented the geometry of the study reach and the location of boulders. Analyses of flood slackwater deposits established a paleoflood record of 23 floods with peak discharges of 200-760 m(3) s(-1), during the last 600 years. 1-D HEC-RAS hydraulic analysis provided water surface profiles, discharges and hydraulics, along the study reach and velocity, shear stress and stream power for each boulder. MAX program and Pearson 3 distribution were used for flood frequency analysis. Most of the concrete boulders were deposited in the sub-critical backwater of channel constrictions where velocities were 1.5-2.1 m s(-1). The largest boulders were deposited in super-critical flow where velocity was 8-9.2 m s(-1). The alluvial channel enabled to transport these concrete boulders, reflecting the unstable, active sandy layer of the channel bed over which the boulders moved. The maximum flood shear stress and stream power characterize medium-large floods with return period of 20-120 years and not for the largest floods, as expected. Boulders about 2.1 m and weighing about 15 t can be transported at least once in 120 years. The shear stress and stream power indicate that the moderate-large floods are the most geomorphically effective floods rather than the largest floods in Nahal Hatzera basin. Nevertheless, the 'geomorphic effectiveness' of the 2004 flood - a typical desert flash flood with high peak and short duration, was small based on the minor changes along the channel and banks indicating that their resistance thresholds were not exceeded and energy expenditure was mainly on boulders entrainment and transport.
英文关键词Boulders transport Paleoflood hydrology Ungauged catchments Desert flood Flood frequency analysis Shear stress Stream power Geomorphic effectiveness
类型Review
语种英语
国家Israel ; England ; Spain
开放获取类型Green Accepted
收录类别SCI-E ; SSCI
WOS记录号WOS:000526786000012
WOS关键词COLORADO RIVER ; FLASH FLOODS ; NAHAL ZIN ; HYDROLOGY ; PALEOHYDROLOGY ; DEPOSITS ; RECORD ; ENVIRONMENTS ; CATCHMENT ; EROSION
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/314330
作者单位1.Univ Haifa, IL-3498838 Haifa, Israel;
2.Univ Southampton, Southampton SO17 1BJ, Hants, England;
3.Geol Survey Israel, IL-9692100 Jerusalem, Israel;
4.Nehara, Misgav, Israel;
5.CSIC, Museo Nacl Ciencias Nat, E-28006 Madrid, Spain
推荐引用方式
GB/T 7714
Greenbaum, Noam,Schwartz, Uri,Carling, Paul,et al. Frequency of boulders transport during large floods in hyperarid areas using paleoflood analysis - An example from the Negev Desert, Israel[J],2020,202.
APA Greenbaum, Noam.,Schwartz, Uri.,Carling, Paul.,Bergman, Nathaniel.,Mushkin, Amit.,...&Porat, Naomi.(2020).Frequency of boulders transport during large floods in hyperarid areas using paleoflood analysis - An example from the Negev Desert, Israel.EARTH-SCIENCE REVIEWS,202.
MLA Greenbaum, Noam,et al."Frequency of boulders transport during large floods in hyperarid areas using paleoflood analysis - An example from the Negev Desert, Israel".EARTH-SCIENCE REVIEWS 202(2020).
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