Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
Authors: |
|
|
---|---|---|
Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
Type: | Resource | |
Storage: | The size of this resource is 49.0 KB | |
Created: | May 29, 2019 at 7:04 p.m. | |
Last updated: | Nov 29, 2021 at 4:47 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 2183 |
Downloads: | 32 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
In order to assess the effects of critical zone processes on Mg concentrations and isotopic signatures of tropical streams, we studied a well constrained, highly weathered andesitic volcaniclastic catchment in the Luquillo Critical Zone Observatory, Puerto Rico. Our results indicate that dissolved Mg concentrations and isotope ratios in the regolith pore water are mainly controlled by rain input, with weathering inputs being more important at sites with thinner regolith (2.7–0.9 m deep) and at depth (>8 m) on a thick ridgetop regolith (∼10 m). In addition to mixing of precipitation and weathering-sourced Mg, an isotopic fractionation process is taking place between dissolved Mg and the regolith, likely during dissolution or recrystallisation of Fe(III)-(hydro)oxides under alternating redox conditions. Bulk regolith is isotopically heavier than both the bedrock and the exchangeable fraction (δ26Mgregolith-bedrock = +0.03 to +0.47‰), consistent with the preferential incorporation of heavy 26Mg into secondary minerals with some exchange of sorbed Mg with isotopically lighter pore water. Magnesium concentrations in the stream show a typical dilution behaviour during a storm event, but the [Mg] – δ26Mg pattern cannot be explained by mixing of rain and pore water; the data are best explained by a steady-state fractionation model with α = 1.00115. During baseflow the stream has δ26Mg = +0.01‰, higher than any of the water samples or the bedrock. In-situ analysis of the Mg isotopic composition of bedrock minerals points at the dissolution of Mg-rich chlorite (δ26Mg = +0.19‰) as the most likely source of this isotopically heavy Mg, with mass balance calculations indicating chlorite dissolution is also the main source of Mg to the stream. Overall, our study highlights the importance of atmospheric input of nutrients to the vegetation in tropical areas covered by thick, highly leached regolith, whereas the Mg flux and Mg isotopic signature of watershed exports are dominated by bedrock dissolution delivered to the stream through deeper, usually un-sampled critical zone pathways.
Subject Keywords
Coverage
Spatial
Temporal
Start Date: | |
---|---|
End Date: |
Content
ReadMe.md
LCZO -- Nutrient Fluxes, Stable Isotopes -- Mg concentrations and isotopic signatures -- Bisley -- (2009-2011)
OVERVIEW
Description/Abstract
In order to assess the effects of critical zone processes on Mg concentrations and isotopic signatures of tropical streams, we studied a well constrained, highly weathered andesitic volcaniclastic catchment in the Luquillo Critical Zone Observatory, Puerto Rico. Our results indicate that dissolved Mg concentrations and isotope ratios in the regolith pore water are mainly controlled by rain input, with weathering inputs being more important at sites with thinner regolith (2.7–0.9 m deep) and at depth (>8 m) on a thick ridgetop regolith (∼10 m). In addition to mixing of precipitation and weathering-sourced Mg, an isotopic fractionation process is taking place between dissolved Mg and the regolith, likely during dissolution or recrystallisation of Fe(III)-(hydro)oxides under alternating redox conditions. Bulk regolith is isotopically heavier than both the bedrock and the exchangeable fraction (δ26Mgregolith-bedrock = +0.03 to +0.47‰), consistent with the preferential incorporation of heavy 26Mg into secondary minerals with some exchange of sorbed Mg with isotopically lighter pore water. Magnesium concentrations in the stream show a typical dilution behaviour during a storm event, but the [Mg] – δ26Mg pattern cannot be explained by mixing of rain and pore water; the data are best explained by a steady-state fractionation model with α = 1.00115. During baseflow the stream has δ26Mg = +0.01‰, higher than any of the water samples or the bedrock. In-situ analysis of the Mg isotopic composition of bedrock minerals points at the dissolution of Mg-rich chlorite (δ26Mg = +0.19‰) as the most likely source of this isotopically heavy Mg, with mass balance calculations indicating chlorite dissolution is also the main source of Mg to the stream. Overall, our study highlights the importance of atmospheric input of nutrients to the vegetation in tropical areas covered by thick, highly leached regolith, whereas the Mg flux and Mg isotopic signature of watershed exports are dominated by bedrock dissolution delivered to the stream through deeper, usually un-sampled critical zone pathways.
Creator/Author
Buss, Heather L.| Pogge von Strandmann, Philip A.E.|Chapela Lara, Maria |Schuessler, Jan A.| Moore, Oliver W.
CZOs
Luquillo
Contact
Miguel Leon, Miguel.Leon@unh.edu
Subtitle
The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment
SUBJECTS
Disciplines
Biogeochemistry
Topics
Nutrient Fluxes|Stable Isotopes
Subtopic
Mg concentrations and isotopic signatures
Keywords
Weathering|Mg isotopes|Mg cycle|Critical zone|LCZO|Puerto Rico
Variables
magnesium|magnesium-25 stable isotope ratio delta|aluminium oxide|calcium oxide| potassium oxide|magnesium oxide|sodium oxide|silicon dioxide|Niobium| titanium dioxide|iron oxide|chromium oxide|manganese oxide|Quartz|Hematite|Goethite|Kaolinite|Illitea|Chlorite|silicon|aluminium|calcium
Variables ODM2
Magnesium|Aluminum|calcium oxide|potassium oxide|magnesium oxide|sodium oxide|silicon dioxide|Niobium, total|Iron, ferric|chromium oxide|manganese oxide|Quartz|Goethite|Clay|Silicon
TEMPORAL
Date Start
2009-05-08
Date End
2011-05-21
SPATIAL
Field Areas
Bisley
Location
Bisley
North latitude
18.322
South latitude
18.3108
West longitude
-65.7485
East longitude
-65.7349
REFERENCE
Citation
Chapela Lara, M., Buss, H. L., Pogge von Strandmann, P. A. E., Schuessler, J. A., & Moore, O. W. (2017): The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment. Geochimica et Cosmochimica Acta. DOI: 10.1016/j.gca.2016.12.032
Publications of this data
Chapela Lara, M., Buss, H. L., Pogge von Strandmann, P. A. E., Schuessler, J. A., & Moore, O. W. (2017). The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment. Geochimica et Cosmochimica Acta http://dx.doi.org/10.1016/j.gca.2016.12.032
CZO ID
7171
Additional Metadata
Name | Value |
---|---|
czos | Luquillo |
czo_id | 7171 |
citation | Chapela Lara, M., Buss, H. L., Pogge von Strandmann, P. A. E., Schuessler, J. A., & Moore, O. W. (2017): The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment. Geochimica et Cosmochimica Acta. DOI: 10.1016/j.gca.2016.12.032 |
keywords | Weathering, Mg isotopes, Mg cycle, Critical zone, LCZO, Puerto Rico |
subtitle | The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment |
variables | magnesium, magnesium-25 stable isotope ratio delta, aluminium oxide, calcium oxide, potassium oxide, magnesium oxide, sodium oxide, silicon dioxide, Niobium, titanium dioxide, iron oxide, chromium oxide, manganese oxide, Quartz, Hematite, Goethite, Kaolinite, Illitea, Chlorite, silicon, aluminium, calcium |
disciplines | Biogeochemistry |
Related Resources
This resource is referenced by | Chapela Lara, M., Buss, H. L., Pogge von Strandmann, P. A. E., Schuessler, J. A., & Moore, O. W. (2017). The influence of critical zone processes on the Mg isotope budget in a tropical, highly weathered andesitic catchment. Geochimica et Cosmochimica Acta http://dx.doi.org/10.1016/j.gca.2016.12.032 |
The content of this resource is derived from | https://doi.org/10.1016/j.gca.2016.12.032 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/![CC-BY](https://storage.googleapis.com/hydroshare-prod-static-media/static/img/cc-badges/CC-BY.04d377d96855.png)
Comments
There are currently no comments
New Comment