A spatiotemporal object-oriented data model for landslides (LOOM)

被引:0
作者
Mario Valiante
Domenico Guida
Marta Della Seta
Francesca Bozzano
机构
[1] Sapienza University of Rome,Department of Earth Science
[2] Salerno University,C.U.G.RI. (Interuniversity Centre for the Prediction and Prevention of Major Risks)
[3] University of Salerno,Department of Civil Engineering
来源
Landslides | 2021年 / 18卷
关键词
Object-oriented; Landslide system; Landslide complex; Landslide object;
D O I
暂无
中图分类号
学科分类号
摘要
LOOM (landslide object-oriented model) is here presented as a data structure for landslide inventories based on the object-oriented paradigm. It aims at the effective storage, in a single dataset, of the complex spatial and temporal relations between landslides recorded and mapped in an area and at their manipulation. Spatial relations are handled through a hierarchical classification based on topological rules and two levels of aggregation are defined: (i) landslide complexes, grouping spatially connected landslides of the same type, and (ii) landslide systems, merging landslides of any type sharing a spatial connection. For the aggregation procedure, a minimal functional interaction between landslide objects has been defined as a spatial overlap between objects. Temporal characterization of landslides is achieved by assigning to each object an exact date or a time range for its occurrence, integrating both the time frame and the event-based approaches. The sum of spatial integrity and temporal characterization ensures the storage of vertical relations between landslides, so that the superimposition of events can be easily retrieved querying the temporal dataset. The here proposed methodology for landslides inventorying has been tested on selected case studies in the Cilento UNESCO Global Geopark (Italy). We demonstrate that the proposed LOOM model avoids data fragmentation or redundancy and topological inconsistency between the digital data and the real-world features. This application revealed to be powerful for the reconstruction of the gravity-induced deformation history of hillslopes, thus for the prediction of their evolution.
引用
收藏
页码:1231 / 1244
页数:13
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