Damiano Sarocchi

ORCID: 0000-0003-0085-2898
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About
Contact & Profiles
Research Areas
  • Landslides and related hazards
  • Geological formations and processes
  • Granular flow and fluidized beds
  • Hydrology and Sediment Transport Processes
  • earthquake and tectonic studies
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • Soil Geostatistics and Mapping
  • Cryospheric studies and observations
  • Geology and Paleoclimatology Research
  • Geological and Tectonic Studies in Latin America
  • Hydrocarbon exploration and reservoir analysis
  • 3D Surveying and Cultural Heritage
  • Building materials and conservation
  • Flood Risk Assessment and Management
  • Botany and Geology in Latin America and Caribbean
  • Planetary Science and Exploration
  • Earthquake Detection and Analysis
  • Astro and Planetary Science
  • Geological Modeling and Analysis
  • Soil and Unsaturated Flow
  • Fire effects on ecosystems
  • Geophysical Methods and Applications
  • Conservation Techniques and Studies
  • Mineral Processing and Grinding

Autonomous University of San Luis Potosí
2014-2024

Polytechnic University of San Luis Potosí
2023

Boise State University
2016-2020

Universidad Nacional Autónoma de México
2005-2008

University of Urbino
1996-1997

The study of the rheological behavior sediment suspensions is one most important tools for understanding fundamental physical processes that occur between interaction particles and homogeneous fluid. As lahars are natural flows along slopes volcanoes consist large blocks supported by a matrix fine suspended in water, their can be studied from characterization. Most stresses distributed mainly within matrix, due to its abundance flow capacity support blocks.This work proposes an appropriate...

10.5194/egusphere-egu25-564 preprint EN 2025-03-14

Geophysical flows, such as debris avalanches, pyroclastic density currents, etc., represent one of the main sources natural hazards. Some these can be classified dry granular i.e., gravity-driven mixtures discrete grains that are prevalent in a wide range volcanological scenarios (e.g. block and ash etc.). These flows characterized by high degree polydispersity terms grain size density, which turn affects flow properties. Specifically, presence fine particles modifies structure segregating...

10.5194/egusphere-egu25-16616 preprint EN 2025-03-15

Abstract On the basis of rotating drum analogue experiments, we describe a fragmentation process acting within debris flows during transport and its influence on rheologic behavior. Our hypothesis is based detailed textural analysis including granulometry, clast morphology, properties fluid matrix. Results experiments point out that breakage certain granulometric classes produces fine particles like sand silt. The population growth clasts with time leads to an increase in yield strength...

10.1002/2013jf002942 article EN Journal of Geophysical Research Earth Surface 2014-08-21

Abstract Detailed analysis was conducted on large‐scale gravitational‐tectonic deformations and landslides in the Acambay graben, an intra‐arc basin trans‐Mexican volcanic belt (TMVB). Field mapping remote sensing revealed slope instability of northern graben boundary induced by Acambay‐Tixmadejé fault. Two major 0·1 km 3 0·05 volume were identified their characteristics analyzed according to role tectonics, mechanism failure, possible triggering factors. Quaternary faulting played a...

10.1002/esp.1987 article EN Earth Surface Processes and Landforms 2010-04-20
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