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Water Role in Landslide Hazards Formation: Occurrence, Prevention and Mitigation
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Water Role in Landslide Hazards Formation: Occurrence, Prevention and Mitigation

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water Erosion and Sediment Transport".

Deadline for manuscript submissions: closed (30 August 2023) | Viewed by 3030

Special Issue Editors

Prof. Dr. Zheng-Yi Feng

E-Mail Website
Guest Editor
Department of Soil and Water Conservation, National Chung Hsing University, Taichung, Taiwan
Interests: landslides; debris flow; slope stability; earth dam; dam breach; riverbank erosion; dynamic analysis; seismic signal process; geotechnical engineering
Special Issues, Collections and Topics in MDPI journals
Prof. Dr. Cheng-Yu Ku

E-Mail Website
Guest Editor
Department of Harbor and River Engineering, National Taiwan Ocean University, Keelung, Taiwan
Interests: numerical methods; geotechnical engineering; groundwater modeling; groundwater; landslides modeling; slope stability; engineering geology
Special Issues, Collections and Topics in MDPI journals
Prof. Dr. Frank Tsai

E-Mail Website
Guest Editor
Department of Civil and Environmental Engineering, Louisiana State University, Baton Rouge, LA, USA
Interests: groundwater; hydrogeology; surface and groundwater interactions; subsurface characterization; riverbank seepage; uncertainty analysis
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Frequently, landslide hazards are caused by water, such as soil slump, debris flow, debris flood, avalanche, lateral spreading, landslide dam burst, etc. The prevention and mitigation of landslide hazards are needed to reduce losses. For this end, the water’s role in landslide hazards formation shall be first investigated and understood in order to commence further effective prevention and mitigation designs for landslide hazards.

In this Special Issue, papers focused on landslide hazards induced by water are welcomed. Research methods using numerical, field investigation, experimental and theoretical approaches to advance the understanding of landslide hazards formation are all encouraged. We also appreciate new techniques for monitoring, risk assessment, prewarning, prevention and mitigation.

Prof. Dr. Zheng-Yi Feng
Prof. Dr. Cheng-Yu Ku
Prof. Dr. Frank Tsai
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Water is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • landslide
  • debris flow
  • hydrogeology
  • failure mechanism
  • slope stability
  • groundwater seepage
  • numerical analysis
  • modeling
  • experimental investigation
  • monitoring
  • mitigation
  • pore-water pressure
  • water table
  • soil strength
  • rock mass strength
  • geo-hazard
  • geological engineering
  • remote sensing
  • land use

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Published Papers (2 papers)

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Research

15 pages, 7367 KiB  
Article
Analysis of Debris Flow Damage Using High-Resolution Topographical Data
by Chaeyeon Oh and Kyewon Jun
Water 2023, 15(19), 3454; https://doi.org/10.3390/w15193454 - 30 Sep 2023
Viewed by 1499
Abstract
Mountain disasters, such as landslides and debris flows, are becoming more prevalent due to abnormal weather patterns. Debris flows, triggered by heavy rainfall, are causing escalating damage to residential areas and roads as they surge down mountain streams. In order to both mitigate [...] Read more.
Mountain disasters, such as landslides and debris flows, are becoming more prevalent due to abnormal weather patterns. Debris flows, triggered by heavy rainfall, are causing escalating damage to residential areas and roads as they surge down mountain streams. In order to both mitigate this damage and comprehend the underlying causes of such mountain disasters, comprehensive field investigations were carried out in regions where debris flows had transpired. To establish spatial information for analyzing vulnerable areas, GIS data were employed. Additionally, precise measurements of the actual extent of debris flow in targeted zones were obtained through the utilization of terrestrial LiDAR scanning. Subsequently, the process of debris flow was replicated using FLO-2D, a numerical model designed for such scenarios. This simulation incorporated actual rainfall data that had precipitated debris flow incidents, as well as probability-based rainfall data corresponding to return periods of 30, 50, and 100 years. Key parameters, including flow depth, velocity, and diffusion area, were compared across different scenarios. The sedimentation area of the section where debris flow originated, as determined from terrestrial LiDAR scan data, was estimated to be approximately 21,300 square meters. The outcomes of the FLO-2D simulation revealed that the diffusion area for Case I was approximately 20,900 m2, while the simulated diffusion area for a 100-year return period was calculated to be 40,725 m2. Furthermore, flow depth, velocity and diffusion area exhibited a gradual incremental trend in simulation results. Full article
(This article belongs to the Special Issue Water Role in Landslide Hazards Formation: Occurrence, Prevention and Mitigation)
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20 pages, 6823 KiB  
Article
Analysis of the Role of Precipitation and Land Use on the Size of the Source Area of Shallow Landslides
by Alessia Giarola, Massimiliano Bordoni, Francesco Zucca and Claudia Meisina
Water 2023, 15(19), 3340; https://doi.org/10.3390/w15193340 - 23 Sep 2023
Cited by 3 | Viewed by 1070
Abstract
Rainfall-induced shallow landslides cause damage to human activities and infrastructureseach year, and although the size of a landslide correlates to the damage that it causes, very few studies have previously investigated the factors that influence the size of a shallow landslide. The aim [...] Read more.
Rainfall-induced shallow landslides cause damage to human activities and infrastructureseach year, and although the size of a landslide correlates to the damage that it causes, very few studies have previously investigated the factors that influence the size of a shallow landslide. The aim of this work was to assess the role of precipitation and land use in controlling the size of the source area of rainfall-induced shallow landslides. After ruling out the impact of the slope angle and bedrock lithology in the two selected catchments, the role of land use was investigated: the statistical tests showed that woodlands and vineyards had statistically different source area size distributions, possibly due to the different hydrological behaviours between the two. A correlation was additionally found between the size of a source area and the amount of cumulated rainfall in the three days prior to each analysed event. In both cases, an increase in source area size was linked to an increase in pore pressure. This study aimed to fill the existing gap in the research to help implement policies aimed at reducing the size, and consequently the impact, of shallow landslides. Full article
(This article belongs to the Special Issue Water Role in Landslide Hazards Formation: Occurrence, Prevention and Mitigation)
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