Changes
On November 28, 2025, 4:09:56 PM UTC,
-
Added resource DataRaw_Part 2_20.zip to How Shells of Different Shapes Affect Current-driven Sand Transport [data and code]
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| 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", | ||
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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 | ||
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| 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 | ||
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| 32 | C. van Prooijen - Delft University of Technology - ORCID: | 32 | C. van Prooijen - Delft University of Technology - ORCID: | ||
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| 36 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | 36 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | ||
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| 38 | Netherlands Institute for Sea | 38 | Netherlands Institute for Sea | ||
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| 40 | Pearson - Royal Netherlands Institute for Sea Research - ORCID: | 40 | Pearson - Royal Netherlands Institute for Sea Research - ORCID: | ||
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| 43 | "dates": | 43 | "dates": | ||
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| 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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| 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", | ||
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| 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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| 226 | "url": | ||||
| 227 | /fe403254-04f5-4026-854d-cb44d988a626/download/dataraw_part-2_20.zip", | ||||
| 206 | "url_type": "upload" | 228 | "url_type": "upload" | ||
| 207 | } | 229 | } | ||
| 208 | ], | 230 | ], | ||
| 209 | "state": "active", | 231 | "state": "active", | ||
| 210 | "subject": "Earth and Environmental Sciences", | 232 | "subject": "Earth and Environmental Sciences", | ||
| 211 | "tags": [ | 233 | "tags": [ | ||
| 212 | { | 234 | { | ||
| 213 | "display_name": "armouring", | 235 | "display_name": "armouring", | ||
| 214 | "id": "ca97da57-13c4-4f37-9fdd-25727890ce37", | 236 | "id": "ca97da57-13c4-4f37-9fdd-25727890ce37", | ||
| 215 | "name": "armouring", | 237 | "name": "armouring", | ||
| 216 | "state": "active", | 238 | "state": "active", | ||
| 217 | "vocabulary_id": null | 239 | "vocabulary_id": null | ||
| 218 | }, | 240 | }, | ||
| 219 | { | 241 | { | ||
| 220 | "display_name": "bed roughness", | 242 | "display_name": "bed roughness", | ||
| 221 | "id": "d87b0c61-0864-43e0-af7b-2979beb60d28", | 243 | "id": "d87b0c61-0864-43e0-af7b-2979beb60d28", | ||
| 222 | "name": "bed roughness", | 244 | "name": "bed roughness", | ||
| 223 | "state": "active", | 245 | "state": "active", | ||
| 224 | "vocabulary_id": null | 246 | "vocabulary_id": null | ||
| 225 | }, | 247 | }, | ||
| 226 | { | 248 | { | ||
| 227 | "display_name": "bioengineering", | 249 | "display_name": "bioengineering", | ||
| 228 | "id": "a33b11e6-4998-4325-aeb8-afb07d9380de", | 250 | "id": "a33b11e6-4998-4325-aeb8-afb07d9380de", | ||
| 229 | "name": "bioengineering", | 251 | "name": "bioengineering", | ||
| 230 | "state": "active", | 252 | "state": "active", | ||
| 231 | "vocabulary_id": null | 253 | "vocabulary_id": null | ||
| 232 | }, | 254 | }, | ||
| 233 | { | 255 | { | ||
| 234 | "display_name": "sediment transport", | 256 | "display_name": "sediment transport", | ||
| 235 | "id": "b839efe1-bc31-47ba-9acf-18898037b084", | 257 | "id": "b839efe1-bc31-47ba-9acf-18898037b084", | ||
| 236 | "name": "sediment transport", | 258 | "name": "sediment transport", | ||
| 237 | "state": "active", | 259 | "state": "active", | ||
| 238 | "vocabulary_id": null | 260 | "vocabulary_id": null | ||
| 239 | }, | 261 | }, | ||
| 240 | { | 262 | { | ||
| 241 | "display_name": "shells", | 263 | "display_name": "shells", | ||
| 242 | "id": "34806f35-38c9-40db-8aa4-3a3b8915838a", | 264 | "id": "34806f35-38c9-40db-8aa4-3a3b8915838a", | ||
| 243 | "name": "shells", | 265 | "name": "shells", | ||
| 244 | "state": "active", | 266 | "state": "active", | ||
| 245 | "vocabulary_id": null | 267 | "vocabulary_id": null | ||
| 246 | }, | 268 | }, | ||
| 247 | { | 269 | { | ||
| 248 | "display_name": "turbulence", | 270 | "display_name": "turbulence", | ||
| 249 | "id": "155aab36-2b41-40ef-a306-f22f88972cd9", | 271 | "id": "155aab36-2b41-40ef-a306-f22f88972cd9", | ||
| 250 | "name": "turbulence", | 272 | "name": "turbulence", | ||
| 251 | "state": "active", | 273 | "state": "active", | ||
| 252 | "vocabulary_id": null | 274 | "vocabulary_id": null | ||
| 253 | } | 275 | } | ||
| 254 | ], | 276 | ], | ||
| 255 | "title": "How Shells of Different Shapes Affect Current-driven Sand | 277 | "title": "How Shells of Different Shapes Affect Current-driven Sand | ||
| 256 | Transport [data and code]", | 278 | Transport [data and code]", | ||
| 257 | "type": "dataset", | 279 | "type": "dataset", | ||
| 258 | "url": "https://doi.org/10.25850/nioz/7b.b.0j", | 280 | "url": "https://doi.org/10.25850/nioz/7b.b.0j", | ||
| 259 | "version": "1" | 281 | "version": "1" | ||
| 260 | } | 282 | } |