In situ stress database of the greater Ruhr region (Germany) derived from hydrofracturing tests and borehole logs
<p>Between 1986 and 1995, 429 hydrofracturing tests have been carried out in six now-abandoned coal mines and two coal bed methane boreholes at depths between 600 and 1950 <span class="inline-formula">m</span> within the greater Ruhr region in western Germany. From these...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2022-12-01
|
| Series: | Earth System Science Data |
| Online Access: | https://essd.copernicus.org/articles/14/5367/2022/essd-14-5367-2022.pdf |
| Summary: | <p>Between 1986 and 1995, 429 hydrofracturing tests have been carried out in six now-abandoned coal mines and two coal bed methane boreholes at depths between 600 and 1950 <span class="inline-formula">m</span> within the greater Ruhr region in western Germany. From these tests, stress magnitudes and orientations of the stress tensor are derived. The majority of hydrofracturing tests were carried out from mine galleries away from mine workings in a relatively undisturbed rock mass. These data along with detailed information have been disclosed recently. In combination with already published material, we provide the first comprehensive stress database of the greater Ruhr region. Our study summarises the results of the extensive in situ stress test campaign and assigns quality to each data record using the established quality ranking schemes of the World Stress Map project. The stress magnitudes suggest predominantly strike-slip stress regime, where the magnitude of the minimum horizontal stress, <span class="inline-formula"><i>S</i><sub>hmin</sub></span>, is half of the magnitude of the maximum horizontal stress, <span class="inline-formula"><i>S</i><sub>Hmax</sub></span>, implying that the horizontal differential stress is high. We observe no particular change in the stress gradient at depth throughout the Carboniferous layers and no significant difference between tests carried out in coal mines and deep boreholes. The mean <span class="inline-formula"><i>S</i><sub>Hmax</sub></span> orientation varies between 133 <span class="inline-formula">±</span> 13<span class="inline-formula"><sup>∘</sup></span> in the westernmost located Friedrich Heinrich coal mine and 168 <span class="inline-formula">±</span> 23<span class="inline-formula"><sup>∘</sup></span> in the easternmost located Westphalia coal mine. The mean <span class="inline-formula"><i>S</i><sub>Hmax</sub></span> orientation, based on 87 data records from this and already published studies, of 161 <span class="inline-formula">±</span> 43<span class="inline-formula"><sup>∘</sup></span> is in good agreement with the regional stress orientation observed in northwestern Europe. The presented public database provides in situ stress magnitude and stress orientation data records that are essential for the calibration of geomechanical numerical models on regional and/or reservoir scales for, among others, assessing stability issues of borehole trajectories, caverns, and georeservoirs in general. For an application example of this database, we estimate slip and dilation tendencies of major geological discontinuities, discovered during the 700-year-long coal mining activities in the region. The result, although burdened by high uncertainties, shows that the discontinuities striking in the N–S and NW–SE directions have a higher slip tendency compared to the ones striking ENE–WSW and NNW–SSE, whereas a high dilation tendency is observed for discontinuities striking NNW–SSE and a low dilation tendency for the ones striking ENE–WSW. The stress orientation database is available under <a href="https://doi.org/10.24406/fordatis/200">https://doi.org/10.24406/fordatis/200</a> <span class="cit" id="xref_paren.1">(<a href="#bib1.bibx31">Kruszewski et al.</a>, <a href="#bib1.bibx31">2022</a><a href="#bib1.bibx31">a</a>)</span>, the stress magnitude database is available under <a href="https://doi.org/10.24406/fordatis/201">https://doi.org/10.24406/fordatis/201</a> <span class="cit" id="xref_paren.2">(<a href="#bib1.bibx32">Kruszewski et al.</a>, <a href="#bib1.bibx32">2022</a><a href="#bib1.bibx32">b</a>)</span>, whereas the hydrofracturing test reports are available under <a href="https://doi.org/10.24406/fordatis/222">https://doi.org/10.24406/fordatis/222</a> <span class="cit" id="xref_paren.3">(<a href="#bib1.bibx33">Kruszewski et al.</a>, <a href="#bib1.bibx33">2022</a><a href="#bib1.bibx33">c</a>)</span>.</p> |
|---|---|
| ISSN: | 1866-3508 1866-3516 |