Articles | Volume 13, issue 2
https://doi.org/10.5194/esurf-13-295-2025
https://doi.org/10.5194/esurf-13-295-2025
Research article
 | 
03 Apr 2025
Research article |  | 03 Apr 2025

Decadal in situ hydrological observations and empirical modeling of pressure head in a high-alpine, fractured calcareous rock slope

Riccardo Scandroglio, Samuel Weber, Till Rehm, and Michael Krautblatter

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Riccardo Scandroglio on behalf of the Authors (08 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Dec 2024) by Andreas Lang
RR by Luc Illien (13 Jan 2025)
ED: Publish as is (13 Jan 2025) by Andreas Lang
ED: Publish as is (13 Jan 2025) by Tom Coulthard (Editor)
AR by Riccardo Scandroglio on behalf of the Authors (22 Jan 2025)
Download
Short summary
Despite the critical role of water in alpine regions, its presence in bedrock is frequently neglected. This research examines the dynamics of water in fractures using 1 decade of measurements from a tunnel 50 m underground. We provide new insights into alpine groundwater dynamics, revealing that up to 800 L d-1 can flow in one fracture during extreme events. These quantities can saturate the fractures, enhance hydraulic conductivity, and generate pressures that destabilize slopes.
Share