All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Estimating the Permeability-Depth Relation of Slate Formation for Geothermal Project

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F25%3A00638931" target="_blank" >RIV/67985891:_____/25:00638931 - isvavai.cz</a>

  • Result on the web

    <a href="http://hhttps://doi.org/10.1007/s00603-025-04590-w" target="_blank" >http://hhttps://doi.org/10.1007/s00603-025-04590-w</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00603-025-04590-w" target="_blank" >10.1007/s00603-025-04590-w</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Estimating the Permeability-Depth Relation of Slate Formation for Geothermal Project

  • Original language description

    Slate formation is one of the potential geothermal sites in Taiwan. However, the fluid flow capability of slate formations has not been well investigated internationally. This study proposes a procedure to evaluate the permeability-depth relationship in slate formations. We used slate samples from the Hungyeh Formation in Taiwan to measure the permeability (k) of intact slate and the hydraulic aperture (e) of natural/artificial tensile fractures along the foliation, under confining pressures up to 60 MPa (similar to 3500 m depth). Stress-dependent models of permeability and hydraulic aperture were developed using a power law and an exponential function, respectively. The equivalent vertical permeability (k(v,eq)) of slate formation with fractures is calculated using Snow's model, which considers the aperture (e) and spacing (s) of vertical fractures subparallel to the foliation. The matrix permeability (< 0.001 mD) decreases with increasing depth. The k(v,eq) of the slate formation, contributed by fractures along the vertical foliation (assuming s = 1.0 m), is several tens of times greater than the intact slate permeability. Within the target depth range of 1500-1700 m, and assuming s = 0.2 m generated by hydraulic fracturing (HF), the mean k(v,eq) ranges from 3.0 x 10(-2) to 2.3 x 10(-2) mD under an injection pressure of 10 MPa. To enhance energy generation efficiency in slate formations, improving HF design to create denser fractures and identify fracture zones, is suggested. The proposed approach is a simple and feasible way to evaluate the permeability-depth relation of reservoirs for geothermal projects before the detailed site investigation program.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    20701 - Environmental and geological engineering, geotechnics

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Rock Mechanics and Rock Engineering

  • ISSN

    0723-2632

  • e-ISSN

    1434-453X

  • Volume of the periodical

    58

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    16

  • Pages from-to

    8867-8882

  • UT code for WoS article

    001480787100001

  • EID of the result in the Scopus database

    2-s2.0-105004054045