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International Journal of Erosion Control Engineering最新文献

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Urban Expansion and Landslide Risk: Investigating the August 2022 Landslide Events in South Korea 城市扩张与山体滑坡风险:2022 年 8 月韩国山体滑坡事件调查
Pub Date : 2024-06-10 DOI: 10.13101/ijece.17.35
Ki-Hwan Lee, Hee-Young Ahn, In-Seop Kim, Yong-Ju Seo, Song Eu, Jun-Pyo Seo, Choong-Sik Woo
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引用次数: 0
A Case Study of the Evaluation of Slip Surfaces using Mineralogical, Chemical, and Physical Tests 利用矿物学、化学和物理测试评估滑动表面的案例研究
Pub Date : 2024-04-08 DOI: 10.13101/ijece.17.15
M. Okawara, Yoshinori Hotta, Rina Kubo, Tamotsu Teramura, Tatsuya Sato, Syunsuke Ohtubo, Sachihiko Ozawa
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引用次数: 0
Feasibility of Using Permeable Block Sabo Dams Incorporating Breakwater Structures for Volcanic Sediment Management 利用包含防波堤结构的透水块状萨博坝管理火山沉积物的可行性
Pub Date : 2024-04-08 DOI: 10.13101/ijece.17.27
N. Harada, Masamitsu Fujimoto, Y. Satofuka, Takahisa Mizuyama
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引用次数: 0
Characteristics of Slope Failures Seen outside the Designated Landslide-prone Areas 指定易发生山泥倾泻地区以外的斜坡破坏特征
Pub Date : 2023-09-04 DOI: 10.13101/ijece.16.13
Naoki Kawahara, N. Osanai, Hiroaki Nakaya
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引用次数: 0
Evaluation of Slip Surface Strength of a Pseudo-Slip Surface Created by Cutting Rock Samples 岩样切割伪滑面滑面强度评价
Pub Date : 2023-09-04 DOI: 10.13101/ijece.16.22
Yoshinori Hotta, Koki Sawano, Koichiro Yokota, M. Okawara
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引用次数: 0
Effects of Shallow Groundwater on Deep Groundwater Dynamics in a Slow-Moving Landslide Site 缓动滑坡场地浅层地下水对深层地下水动力学的影响
Pub Date : 2023-03-17 DOI: 10.13101/ijece.16.1
K. Yokoyama, T. Egusa, Takashi Ikka, Hiroto Yamashita, F. Imaizumi
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引用次数: 1
Sediment-related Disasters in Petrópolis, Brazil, on February 15 and March 20, 2022 2022年2月15日和3月20日,巴西Petrópolis与沉积物有关的灾害
Pub Date : 2022-12-12 DOI: 10.13101/ijece.15.31
Hideto Ochi, Y. Shimoda, Yosuke Nishio, R. P. Machado
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引用次数: 0
Landslide Hazards Induced by Heavy Rainfall in August 2021 in the Northern Part of the Aomori Prefecture, Japan 日本青森县北部2021年8月强降雨引发的滑坡灾害
Pub Date : 2022-08-12 DOI: 10.13101/ijece.15.22
Toshiyuki Kon, C. Tsou, Takashi Koi, Yusuke Yamamoto, N. Koiwa, Ryuzo Noda, M. Irasawa, Kiyokazu Kato, Hiroshi Tsushima, Hiroshi Mori, Hideya Iwata, Tatsuya Sato, H. Ikeda, Yushi Kudo, Motoshiko Kobayashi, K. Arai, Chieko Kuroiwa, Yukina Koga, Takeaki Ishikawa, Misa Tsushima, Eiji Nagano, J. Miura, Haruka Saito, Reona Kawakami
On August 10, 2021, a total of 454 landslides and debris flows in the northern part of the Shimokita Peninsula, Aomori, Japan, resulted in one of the major natural disasters in the region in recent years. Large amounts of rainfall of 385 mm fell on 9 and 10 August, due to low atmospheric pressure and the consequent Typhoon Lupit (No. 9) passing over the Sea of Japan. The event resulted in landslides, flooding, and damage to houses, roads, bridges, and carried large wood and debris into the rivers, which caused blockages at dam locations. Landslides occurred mainly in the fluvial dissected Koakakawa and Ohakakawa River Basins and on the steep slopes of costal terrace scarps nearby Yakeyamasaki. Landslides were primarily associated with weathered tuffaceous mudstone and weathered andesitic green-colored tuff in the Koakakawa and Ohakakawa Basins and weathered pyroclastic flow, colluvium, and gravel layers nearby the Yakeyamasaki. Pipping holes were observed within or at the bottom of weathered tuffaceous mudstone, weathered pyroclastic flow, and colluvium, suggesting the landslide occurrence may have been caused by the amount of groundwater present.
2021年8月10日,日本青森下田半岛北部共发生454次山体滑坡和泥石流,造成该地区近年来最严重的自然灾害之一。8月9日及10日,受低气压影响,加上台风露碧(9号)经过日本海,本港录得385毫米雨量。地震导致山体滑坡、洪水,房屋、道路和桥梁受损,大量木材和碎片被冲入河流,导致大坝位置堵塞。山体滑坡主要发生在河流解剖的小川河和大川河流域以及崖山附近的沿海阶地陡坡上。山体滑坡主要与高川盆地和大川盆地的风化凝灰质泥岩和风化安山岩绿色凝灰岩以及八山崎附近的风化火山碎屑流、崩积层和砾石层有关。在风化凝灰质泥岩、风化火山碎屑流和崩积层内部或底部观察到打孔,表明滑坡的发生可能是由地下水的存在引起的。
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引用次数: 0
A Review of Groundwater Observation Methods for Slow-Moving Landslide 缓动滑坡地下水观测方法综述
Pub Date : 2022-08-12 DOI: 10.13101/ijece.15.7
K. Yokoyama, F. Imaizumi, T. Egusa
Knowing the groundwater dynamics in landslide areas is very important for numerically analyzing slope stability and for planning countermeasure works. This review summarized the observation methods of groundwater within the landslide mass and groundwater inflow into it and classified them into direct and indirect methods. Direct methods such as groundwater level observation and groundwater logging can reveal the temporal and spatial fluctuations of the groundwater level and the depths of groundwater flow layers. The direct methods are still central for understanding groundwater dynamics in landslide areas. However, the information obtained with the methods is limited to the location surveyed. Indirect methods have been remarkably developed in recent years. Airborne electromagnetic surveys rapidly provide wide-area groundwater information in steep mountainous areas where workers are difficult to enter, or large landslides occur. In addition, a method of quantifying the sound of groundwater flow to determine the flow paths of groundwater has been put to practical use. Although the indirect methods have the advantage of providing information in wide areas, they have the risk to misidentify or overlook groundwater. Direct methods and indirect methods can complement each other’s shortcomings. The combination of direct and indirect methods can provide detailed information on spatiotemporal groundwater distribution over wide areas efficiently in term of cost and labor. This enables a more accurate analysis of landslide sliding and more effective construction of landslide countermeasure works.
了解滑坡区地下水动态对边坡稳定性的数值分析和规划对策工作具有重要意义。本文综述了滑坡体内地下水和滑坡体内流入地下水的观测方法,并将其分为直接观测法和间接观测法。地下水位观测和地下水位测井等直接方法可以揭示地下水位和地下水流层深度的时空波动。直接方法仍然是了解滑坡地区地下水动力学的核心。然而,用这种方法获得的信息仅限于所调查的地点。近年来,间接方法得到了显著的发展。在工作人员难以进入或发生大型滑坡的陡峭山区,机载电磁测量可快速提供广域地下水信息。此外,还提出了一种量化地下水流动声来确定地下水流动路径的方法。虽然间接方法具有在大范围内提供信息的优点,但它们存在错误识别或忽视地下水的风险。直接法和间接法的缺点可以相辅相成。直接方法与间接方法相结合,在成本和人工方面可以有效地提供大范围内地下水时空分布的详细信息。这样可以更准确地分析滑坡滑动情况,并更有效地进行滑坡防治工程。
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引用次数: 0
Debris flow disaster in Atami, Japan, in July 2021 2021年7月,日本热海发生泥石流灾害
Pub Date : 2022-06-06 DOI: 10.13101/ijece.15.1
F. Imaizumi, N. Osanai, Shinyu Kato, M. Koike, K. Kosugi, Y. Sakai, Hiroshi Sakaguchi, Y. Satofuka, Shoki Takayama, Takafumi Tanaka, Y. Nishi
On the morning of July 3, 2021, a large debris flow occurred at the Aizome River in the Izusan district of Atami, Shizuoka Prefecture. The debris flow caused extensive damage, causing the death of 26 people, leaving one person missing, and damaging 128 houses (as of October 1, 2021). The Japan Society of Erosion Control Engineering set up the “Emergency Investigation Team of the Landslide in Atami, Shizuoka in July 2021” to understand the actual situation of the disaster and study the future countermeasures. The team conducted a field survey with the cooperation of Shizuoka Prefecture on August 12. This report summarizes characteristics of the debris flow as obtained from the field survey.
2021年7月3日上午,静冈县热海市伊豆山区的Aizome河发生了大规模泥石流。泥石流造成了广泛的破坏,造成26人死亡,1人失踪,128所房屋受损(截至2021年10月1日)。日本侵蚀控制工程学会成立了“2021年7月静冈县热海滑坡应急调查组”,了解灾害实际情况,研究未来对策。研究组于8月12日在静冈县的协助下进行了实地调查。本报告总结了从野外调查中获得的泥石流特征。
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引用次数: 2
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International Journal of Erosion Control Engineering
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