Changes
On November 28, 2025, 4:09:19 PM UTC,
-
Added resource DataRaw_Part 2_00.zip to How Shells of Different Shapes Affect Current-driven Sand Transport [data and code]
| f | 1 | { | f | 1 | { |
| 2 | "author": "Tjeerd Bouma (Royal Netherlands Institute for Sea | 2 | "author": "Tjeerd Bouma (Royal Netherlands Institute for Sea | ||
| 3 | Research)", | 3 | Research)", | ||
| 4 | "author_email": "tjeerd.bouma@nioz.nl", | 4 | "author_email": "tjeerd.bouma@nioz.nl", | ||
| 5 | "code": "7b.b.0j", | 5 | "code": "7b.b.0j", | ||
| 6 | "contributor": "Royal Netherlands Institute for Sea Research | 6 | "contributor": "Royal Netherlands Institute for Sea Research | ||
| 7 | (NIOZ)", | 7 | (NIOZ)", | ||
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| 11 | \",\"affiliation\":\"Royal Netherlands Institute for Sea | 11 | \",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
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| 13 | Kooistra - Royal Netherlands Institute for Sea Research - ORCID: | 13 | Kooistra - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 14 | 0000-0003-2366-4099 \"},{\"firstname\":\"Steven | 14 | 0000-0003-2366-4099 \"},{\"firstname\":\"Steven | ||
| 15 | "Haarbosch\",\"orcid\":\"0009-0005-1845-5606\",\"affiliation\":\"Delft | 15 | "Haarbosch\",\"orcid\":\"0009-0005-1845-5606\",\"affiliation\":\"Delft | ||
| 16 | University of | 16 | University of | ||
| 17 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Steven | 17 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Steven | ||
| 18 | H. Haarbosch - Delft University of Technology - ORCID: | 18 | H. Haarbosch - Delft University of Technology - ORCID: | ||
| 19 | 0009-0005-1845-5606\"},{\"firstname\":\"Jorn | 19 | 0009-0005-1845-5606\"},{\"firstname\":\"Jorn | ||
| 20 | :\"Bosma\",\"orcid\":\"0000-0002-3275-3686\",\"affiliation\":\"Utrecht | 20 | :\"Bosma\",\"orcid\":\"0000-0002-3275-3686\",\"affiliation\":\"Utrecht | ||
| 21 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Jorn | 21 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Jorn | ||
| 22 | W. Bosma - Utrecht University - ORCID: | 22 | W. Bosma - Utrecht University - ORCID: | ||
| 23 | \":\"Bouma\",\"orcid\":\"0000-0001-7824-7546\",\"affiliation\":\"Royal | 23 | \":\"Bouma\",\"orcid\":\"0000-0001-7824-7546\",\"affiliation\":\"Royal | ||
| 24 | Netherlands Institute for Sea | 24 | Netherlands Institute for Sea | ||
| 25 | "contactemailaddress\":\"tjeerd.bouma@nioz.nl\",\"formatted\":\"Tjeerd | 25 | "contactemailaddress\":\"tjeerd.bouma@nioz.nl\",\"formatted\":\"Tjeerd | ||
| 26 | Bouma - Royal Netherlands Institute for Sea Research - ORCID: | 26 | Bouma - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 27 | 0000-0001-7824-7546 - Corresponding Author - | 27 | 0000-0001-7824-7546 - Corresponding Author - | ||
| 28 | tjeerd.bouma@nioz.nl\"},{\"firstname\":\"Bram C.\",\"lastname\":\"van | 28 | tjeerd.bouma@nioz.nl\"},{\"firstname\":\"Bram C.\",\"lastname\":\"van | ||
| 29 | Prooijen\",\"orcid\":\"0000-0003-1375-1498\",\"affiliation\":\"Delft | 29 | Prooijen\",\"orcid\":\"0000-0003-1375-1498\",\"affiliation\":\"Delft | ||
| 30 | University of | 30 | University of | ||
| 31 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Bram | 31 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Bram | ||
| 32 | C. van Prooijen - Delft University of Technology - ORCID: | 32 | C. van Prooijen - Delft University of Technology - ORCID: | ||
| 33 | \"Soetaert\",\"orcid\":\"0000-0003-4603-7100\",\"affiliation\":\"Royal | 33 | \"Soetaert\",\"orcid\":\"0000-0003-4603-7100\",\"affiliation\":\"Royal | ||
| 34 | Netherlands Institute for Sea | 34 | Netherlands Institute for Sea | ||
| 35 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Karline | 35 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Karline | ||
| 36 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | 36 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 37 | :\"Pearson\",\"orcid\":\"0000-0002-3986-4469\",\"affiliation\":\"Royal | 37 | :\"Pearson\",\"orcid\":\"0000-0002-3986-4469\",\"affiliation\":\"Royal | ||
| 38 | Netherlands Institute for Sea | 38 | Netherlands Institute for Sea | ||
| 39 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Stuart | 39 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Stuart | ||
| 40 | Pearson - Royal Netherlands Institute for Sea Research - ORCID: | 40 | Pearson - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 41 | 0000-0002-3986-4469\"}]", | 41 | 0000-0002-3986-4469\"}]", | ||
| 42 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.0j", | 42 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.0j", | ||
| 43 | "dates": | 43 | "dates": | ||
| 44 | ,\"type\":\"collected\",\"information\":null,\"formatted\":\"collected | 44 | ,\"type\":\"collected\",\"information\":null,\"formatted\":\"collected | ||
| 45 | from: 15/08/2022 to: 15/08/2025 \"}]", | 45 | from: 15/08/2022 to: 15/08/2025 \"}]", | ||
| 46 | "deposit_date": "2025-08-21", | 46 | "deposit_date": "2025-08-21", | ||
| 47 | "depositor": "Tjitske Kooistra (tjitske.kooistra@nioz.nl)", | 47 | "depositor": "Tjitske Kooistra (tjitske.kooistra@nioz.nl)", | ||
| 48 | "distribution_date": "2025-08-21", | 48 | "distribution_date": "2025-08-21", | ||
| 49 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 49 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 50 | Institute for Sea Research)", | 50 | Institute for Sea Research)", | ||
| 51 | "doi_date_published": "2025-11-13T11:04:43", | 51 | "doi_date_published": "2025-11-13T11:04:43", | ||
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| 62 | 21026 - Revealing Hidden Networks of Coastal Sediment Pathways\"}]", | 62 | 21026 - Revealing Hidden Networks of Coastal Sediment Pathways\"}]", | ||
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| 66 | "license_title": null, | 66 | "license_title": null, | ||
| 67 | "maintainer": "Tjitske", | 67 | "maintainer": "Tjitske", | ||
| 68 | "maintainer_email": "tjitske.kooistra@nioz.nl", | 68 | "maintainer_email": "tjitske.kooistra@nioz.nl", | ||
| 69 | "metadata_created": "2025-11-28T16:05:00.664833", | 69 | "metadata_created": "2025-11-28T16:05:00.664833", | ||
| n | 70 | "metadata_modified": "2025-11-28T16:09:01.294816", | n | 70 | "metadata_modified": "2025-11-28T16:09:19.770232", |
| 71 | "name": | 71 | "name": | ||
| 72 | -different-shapes-affect-current-driven-sand-transport-data-and-code", | 72 | -different-shapes-affect-current-driven-sand-transport-data-and-code", | ||
| 73 | "notes": "This dataset and code belongs to the manuscript \"How | 73 | "notes": "This dataset and code belongs to the manuscript \"How | ||
| 74 | Shells of Different Shapes Affect Current-driven Sand Transport\". | 74 | Shells of Different Shapes Affect Current-driven Sand Transport\". | ||
| 75 | \n\nThe seabed rarely consists solely of bare sand: often other | 75 | \n\nThe seabed rarely consists solely of bare sand: often other | ||
| 76 | materials, such as shells are present. They can influence sand | 76 | materials, such as shells are present. They can influence sand | ||
| 77 | transport by armouring the bed and modifying its roughness. Biogenic | 77 | transport by armouring the bed and modifying its roughness. Biogenic | ||
| 78 | shells come in different shapes and sizes, depending on the mollusc | 78 | shells come in different shapes and sizes, depending on the mollusc | ||
| 79 | species that produce them. To understand how changes in bivalve | 79 | species that produce them. To understand how changes in bivalve | ||
| 80 | species composition affect sediment transport, we need a mechanistic | 80 | species composition affect sediment transport, we need a mechanistic | ||
| 81 | understanding of how shell content and shell shape influence the | 81 | understanding of how shell content and shell shape influence the | ||
| 82 | near-bed flow and sand transport. We performed experiments in a | 82 | near-bed flow and sand transport. We performed experiments in a | ||
| 83 | racetrack flume, testing the effect of elongated (Ensis leei) versus | 83 | racetrack flume, testing the effect of elongated (Ensis leei) versus | ||
| 84 | rounded (Spisula subtruncata) shells on unidirectional current-driven | 84 | rounded (Spisula subtruncata) shells on unidirectional current-driven | ||
| 85 | sand transport. For both types of shells, a higher depth-averaged flow | 85 | sand transport. For both types of shells, a higher depth-averaged flow | ||
| 86 | velocity was needed for initiation of motion and a decrease in bedload | 86 | velocity was needed for initiation of motion and a decrease in bedload | ||
| 87 | transport of sand was found. At a shell content of 20%, the threshold | 87 | transport of sand was found. At a shell content of 20%, the threshold | ||
| 88 | of motion of sand increased up to 75%, and bedload transport was | 88 | of motion of sand increased up to 75%, and bedload transport was | ||
| 89 | reduced by up to 50%. These effects are explained by a balance between | 89 | reduced by up to 50%. These effects are explained by a balance between | ||
| 90 | roughness-induced turbulence and bed armouring. Compared to a bare | 90 | roughness-induced turbulence and bed armouring. Compared to a bare | ||
| 91 | bed, shells decreased bed roughness by reducing ripple formation; | 91 | bed, shells decreased bed roughness by reducing ripple formation; | ||
| 92 | rounded shells lowered roughness more than elongated shells, which | 92 | rounded shells lowered roughness more than elongated shells, which | ||
| 93 | formed roughness elements themselves, but also covered a larger | 93 | formed roughness elements themselves, but also covered a larger | ||
| 94 | fraction of the bed. However, there was no clear difference between | 94 | fraction of the bed. However, there was no clear difference between | ||
| 95 | round versus elongated shells on the overall sand transport; only | 95 | round versus elongated shells on the overall sand transport; only | ||
| 96 | shell content was key for the overall effect. Our results imply that | 96 | shell content was key for the overall effect. Our results imply that | ||
| 97 | sediment transport is likely overpredicted when a high number of | 97 | sediment transport is likely overpredicted when a high number of | ||
| 98 | shells is present in the seabed.", | 98 | shells is present in the seabed.", | ||
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| 166 | "subject": "Earth and Environmental Sciences", | 188 | "subject": "Earth and Environmental Sciences", | ||
| 167 | "tags": [ | 189 | "tags": [ | ||
| 168 | { | 190 | { | ||
| 169 | "display_name": "armouring", | 191 | "display_name": "armouring", | ||
| 170 | "id": "ca97da57-13c4-4f37-9fdd-25727890ce37", | 192 | "id": "ca97da57-13c4-4f37-9fdd-25727890ce37", | ||
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| 188 | }, | 210 | }, | ||
| 189 | { | 211 | { | ||
| 190 | "display_name": "sediment transport", | 212 | "display_name": "sediment transport", | ||
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| 195 | }, | 217 | }, | ||
| 196 | { | 218 | { | ||
| 197 | "display_name": "shells", | 219 | "display_name": "shells", | ||
| 198 | "id": "34806f35-38c9-40db-8aa4-3a3b8915838a", | 220 | "id": "34806f35-38c9-40db-8aa4-3a3b8915838a", | ||
| 199 | "name": "shells", | 221 | "name": "shells", | ||
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| 203 | { | 225 | { | ||
| 204 | "display_name": "turbulence", | 226 | "display_name": "turbulence", | ||
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| 209 | } | 231 | } | ||
| 210 | ], | 232 | ], | ||
| 211 | "title": "How Shells of Different Shapes Affect Current-driven Sand | 233 | "title": "How Shells of Different Shapes Affect Current-driven Sand | ||
| 212 | Transport [data and code]", | 234 | Transport [data and code]", | ||
| 213 | "type": "dataset", | 235 | "type": "dataset", | ||
| 214 | "url": "https://doi.org/10.25850/nioz/7b.b.0j", | 236 | "url": "https://doi.org/10.25850/nioz/7b.b.0j", | ||
| 215 | "version": "1" | 237 | "version": "1" | ||
| 216 | } | 238 | } |