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....

Full description

Bibliographic Details
Main Authors: von Blanckenburg, F., Schulz, A.
Format: Other/Unknown Material
Language:English
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014820
id ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5014820
record_format openpolar
spelling 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)
institution 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