Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals
To weather rock, reagents are required. For example, CO2 is found in rainwater as carbonic acid or CO2 is produced by plant roots and by microbes. Through the large fractures carbonic acid and CO2 reach great depth – dissolved in water. Through the fine fractures they reach the interior of the rock....
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GFZ German Research Centre for Geosciences
2023
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5014820 2023-05-15T15:52:21+02:00 Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals von Blanckenburg, F. Schulz, A. 2023-01-25 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014820 eng eng GFZ German Research Centre for Geosciences info:eu-repo/semantics/altIdentifier/doi/10.48440/gfz.3.3.2022.006 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014820 info:eu-repo/semantics/other 2023 ftgfzpotsdam https://doi.org/10.48440/gfz.3.3.2022.006 2023-02-27T00:34:26Z To weather rock, reagents are required. For example, CO2 is found in rainwater as carbonic acid or CO2 is produced by plant roots and by microbes. Through the large fractures carbonic acid and CO2 reach great depth – dissolved in water. Through the fine fractures they reach the interior of the rock. There they dissolve minerals, like the feldspar. New, completely different minerals form, for example clay minerals. They create fine fractures through which water with carbon can penetrate further and the weathering begins again. Other/Unknown Material Carbonic acid GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
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Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
To weather rock, reagents are required. For example, CO2 is found in rainwater as carbonic acid or CO2 is produced by plant roots and by microbes. Through the large fractures carbonic acid and CO2 reach great depth – dissolved in water. Through the fine fractures they reach the interior of the rock. There they dissolve minerals, like the feldspar. New, completely different minerals form, for example clay minerals. They create fine fractures through which water with carbon can penetrate further and the weathering begins again. |
format |
Other/Unknown Material |
author |
von Blanckenburg, F. Schulz, A. |
spellingShingle |
von Blanckenburg, F. Schulz, A. Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
author_facet |
von Blanckenburg, F. Schulz, A. |
author_sort |
von Blanckenburg, F. |
title |
Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
title_short |
Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
title_full |
Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
title_fullStr |
Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
title_full_unstemmed |
Deep Rock Weathering Episode 3 – Reagents that Dissolve Minerals |
title_sort |
deep rock weathering episode 3 – reagents that dissolve minerals |
publisher |
GFZ German Research Centre for Geosciences |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014820 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.48440/gfz.3.3.2022.006 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014820 |
op_doi |
https://doi.org/10.48440/gfz.3.3.2022.006 |
_version_ |
1766387558726500352 |