The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain
U-series isotopes have been measured in the dissolved phase, suspended load and bedload of the main rivers draining basaltic catchments in Iceland. For the dissolved phase, (234U/238U) and (238U/230Th) range between 1.08 and 2.2, and 7.4 and 516, respectively. For the suspended load and bedload, (23...
| Main Authors: | , , , , , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2006
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| _version_ | 1797057998089093120 |
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| author | Vigier, N Burton, K Gislason, SR Rogers, N Duchene, S Thomas, L Hodge, E Schaefer, B |
| author_facet | Vigier, N Burton, K Gislason, SR Rogers, N Duchene, S Thomas, L Hodge, E Schaefer, B |
| author_sort | Vigier, N |
| collection | OXFORD |
| description | U-series isotopes have been measured in the dissolved phase, suspended load and bedload of the main rivers draining basaltic catchments in Iceland. For the dissolved phase, (234U/238U) and (238U/230Th) range between 1.08 and 2.2, and 7.4 and 516, respectively. For the suspended load and bedload, (234U/238U) and (238U/230Th) range from 0.97 to 1.09 and from 0.93 to 1.05, respectively. Chemical erosion rates, calculated from dissolved major elements, range between 13 and 333 t km- 2 yr- 1. Physical erosion rates have also been estimated, from existing data, and range between 21 and 4864 t/km2/yr, with an average of 519 t km- 2 yr- 1. U-series disequilibria indicate that weathering in Iceland operates at close to steady-state conditions. A model of continuous weathering indicates a maximum weathering timescale of 10 kyr, with an average rate of uranium release into water of 1.6 · 10- 4 yr- 1, which is significant when compared to granitic terrains located at similar latitudes and to tropical basaltic terrains. All river waters display (234U/238U) greater than secular equilibrium, consistent with the effects of alpha-recoil. The same dissolved phase (234U/238U) exhibit a negative trend with physical erosion rates, explained by the dominant effect of close-to-congruent chemical weathering of hyaloclastites in the younger basaltic terrains. Therefore, chemical erosion rate and mineral weathering susceptibility play a major role in determining 234U-238U disequilibria in basaltic river waters. Comparison of global data for river basins in which weathering was recently strongly limited indicates a negative correlation between silicate weathering rates estimated with major elements and the age of weathering estimated with U-series disequilibria. This strongly suggests a key role of time and soil thickness on the chemical erosion of silicates. © 2006 Elsevier B.V. All rights reserved. |
| first_indexed | 2024-03-06T19:44:22Z |
| format | Journal article |
| id | oxford-uuid:21c30d7a-6edf-4bf1-ba83-a014def96faa |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T19:44:22Z |
| publishDate | 2006 |
| record_format | dspace |
| spelling | oxford-uuid:21c30d7a-6edf-4bf1-ba83-a014def96faa2022-03-26T11:35:06ZThe relationship between riverine U-series disequilibria and erosion rates in a basaltic terrainJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:21c30d7a-6edf-4bf1-ba83-a014def96faaEnglishSymplectic Elements at Oxford2006Vigier, NBurton, KGislason, SRRogers, NDuchene, SThomas, LHodge, ESchaefer, BU-series isotopes have been measured in the dissolved phase, suspended load and bedload of the main rivers draining basaltic catchments in Iceland. For the dissolved phase, (234U/238U) and (238U/230Th) range between 1.08 and 2.2, and 7.4 and 516, respectively. For the suspended load and bedload, (234U/238U) and (238U/230Th) range from 0.97 to 1.09 and from 0.93 to 1.05, respectively. Chemical erosion rates, calculated from dissolved major elements, range between 13 and 333 t km- 2 yr- 1. Physical erosion rates have also been estimated, from existing data, and range between 21 and 4864 t/km2/yr, with an average of 519 t km- 2 yr- 1. U-series disequilibria indicate that weathering in Iceland operates at close to steady-state conditions. A model of continuous weathering indicates a maximum weathering timescale of 10 kyr, with an average rate of uranium release into water of 1.6 · 10- 4 yr- 1, which is significant when compared to granitic terrains located at similar latitudes and to tropical basaltic terrains. All river waters display (234U/238U) greater than secular equilibrium, consistent with the effects of alpha-recoil. The same dissolved phase (234U/238U) exhibit a negative trend with physical erosion rates, explained by the dominant effect of close-to-congruent chemical weathering of hyaloclastites in the younger basaltic terrains. Therefore, chemical erosion rate and mineral weathering susceptibility play a major role in determining 234U-238U disequilibria in basaltic river waters. Comparison of global data for river basins in which weathering was recently strongly limited indicates a negative correlation between silicate weathering rates estimated with major elements and the age of weathering estimated with U-series disequilibria. This strongly suggests a key role of time and soil thickness on the chemical erosion of silicates. © 2006 Elsevier B.V. All rights reserved. |
| spellingShingle | Vigier, N Burton, K Gislason, SR Rogers, N Duchene, S Thomas, L Hodge, E Schaefer, B The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title | The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title_full | The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title_fullStr | The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title_full_unstemmed | The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title_short | The relationship between riverine U-series disequilibria and erosion rates in a basaltic terrain |
| title_sort | relationship between riverine u series disequilibria and erosion rates in a basaltic terrain |
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