Changes
On May 28, 2026 at 9:07:24 AM MDT,
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Changed title to Particulate Dominance of Organic Carbon Mobilization from Thaw Slumps on the Peel Plateau, NT (previously Particulate dominance of organic carbon mobilization from thaw slumps on the Peel Plateau, NT)
| f | 1 | { | f | 1 | { |
| 2 | "Creator": "Academic Journal", | 2 | "Creator": "Academic Journal", | ||
| 3 | "author": null, | 3 | "author": null, | ||
| 4 | "author_email": null, | 4 | "author_email": null, | ||
| 5 | "creator_user_id": "dc7293e9-87ef-4697-8633-1bf4f3afe74a", | 5 | "creator_user_id": "dc7293e9-87ef-4697-8633-1bf4f3afe74a", | ||
| 6 | "description": "This research highlights how climate driven | 6 | "description": "This research highlights how climate driven | ||
| 7 | permafrost and thaw slumping is affecting the streams in the Peel | 7 | permafrost and thaw slumping is affecting the streams in the Peel | ||
| 8 | Plateau, NWT. ", | 8 | Plateau, NWT. ", | ||
| 9 | "funding_program": "", | 9 | "funding_program": "", | ||
| 10 | "geographic_range": [ | 10 | "geographic_range": [ | ||
| 11 | "NWT" | 11 | "NWT" | ||
| 12 | ], | 12 | ], | ||
| n | 13 | "groups": [], | n | 13 | "groups": [ |
| 14 | { | ||||
| 15 | "description": "", | ||||
| 16 | "display_name": "Permafrost", | ||||
| 17 | "id": "37ba381e-dd8b-4c68-8993-1b35e31ff1de", | ||||
| 18 | "image_display_url": | ||||
| 19 | y.ecc.gov.nt.ca/uploads/group/2023-10-11-164234.587889Permafrost.jpg", | ||||
| 20 | "name": "permafrost", | ||||
| 21 | "title": "Permafrost" | ||||
| 22 | } | ||||
| 23 | ], | ||||
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| 17 | "license_title": "License Not Specified", | 27 | "license_title": "License Not Specified", | ||
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| 19 | "maintainer": null, | 29 | "maintainer": null, | ||
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| 21 | "metadata_created": "2026-05-27T22:24:31.174644", | 31 | "metadata_created": "2026-05-27T22:24:31.174644", | ||
| n | 22 | "metadata_modified": "2026-05-27T22:24:56.830957", | n | 32 | "metadata_modified": "2026-05-28T15:07:24.736208", |
| 23 | "metatags": "Permafrost thaw,Thermokarst,Carbon Cycle,Peel | 33 | "metatags": "Permafrost thaw,Thermokarst,Carbon Cycle,Peel | ||
| 24 | Plateau,Hydrology,Thaw Slumps", | 34 | Plateau,Hydrology,Thaw Slumps", | ||
| 25 | "modified_date": "2020-10-27", | 35 | "modified_date": "2020-10-27", | ||
| 26 | "name": | 36 | "name": | ||
| 27 | -organic-carbon-mobilization-from-thaw-slumps-on-the-peel-plateau-nt", | 37 | -organic-carbon-mobilization-from-thaw-slumps-on-the-peel-plateau-nt", | ||
| 28 | "notes": "This research highlights how climate driven permafrost and | 38 | "notes": "This research highlights how climate driven permafrost and | ||
| 29 | thaw slumping is affecting the streams in the Peel Plateau, NWT. ", | 39 | thaw slumping is affecting the streams in the Peel Plateau, NWT. ", | ||
| 30 | "num_resources": 1, | 40 | "num_resources": 1, | ||
| 31 | "num_tags": 6, | 41 | "num_tags": 6, | ||
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| 33 | "approval_status": "approved", | 43 | "approval_status": "approved", | ||
| 34 | "created": "2023-11-27T15:29:16.450990", | 44 | "created": "2023-11-27T15:29:16.450990", | ||
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| 39 | "is_organization": true, | 49 | "is_organization": true, | ||
| 40 | "name": "academic-journal", | 50 | "name": "academic-journal", | ||
| 41 | "state": "active", | 51 | "state": "active", | ||
| 42 | "title": "Academic Journal", | 52 | "title": "Academic Journal", | ||
| 43 | "type": "organization" | 53 | "type": "organization" | ||
| 44 | }, | 54 | }, | ||
| 45 | "owner_org": "76bec39b-e0d4-4f47-8eb8-0a7e4a6698f3", | 55 | "owner_org": "76bec39b-e0d4-4f47-8eb8-0a7e4a6698f3", | ||
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| 49 | "release_date": "2020-10-27", | 59 | "release_date": "2020-10-27", | ||
| 50 | "resources": [ | 60 | "resources": [ | ||
| 51 | { | 61 | { | ||
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| 54 | "created": "2026-05-27T22:24:56.695209", | 64 | "created": "2026-05-27T22:24:56.695209", | ||
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| 58 | "format": "PDF", | 68 | "format": "PDF", | ||
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| 61 | "last_modified": "2026-05-27T22:24:56.669742", | 71 | "last_modified": "2026-05-27T22:24:56.669742", | ||
| 62 | "metadata_modified": "2026-05-27T22:24:56.837632", | 72 | "metadata_modified": "2026-05-27T22:24:56.837632", | ||
| 63 | "mimetype": "application/pdf", | 73 | "mimetype": "application/pdf", | ||
| 64 | "mimetype_inner": null, | 74 | "mimetype_inner": null, | ||
| 65 | "name": "Particulate dominance of organic carbon mobilization | 75 | "name": "Particulate dominance of organic carbon mobilization | ||
| 66 | from thaw slumps on the Peel Plateau, NT: Quantification and | 76 | from thaw slumps on the Peel Plateau, NT: Quantification and | ||
| 67 | implications for stream systems and permafrost carbon release", | 77 | implications for stream systems and permafrost carbon release", | ||
| 68 | "package_id": "27abdc44-13e9-4ff1-ae15-4393909c9020", | 78 | "package_id": "27abdc44-13e9-4ff1-ae15-4393909c9020", | ||
| 69 | "position": 0, | 79 | "position": 0, | ||
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| 71 | "size": 3940422, | 81 | "size": 3940422, | ||
| 72 | "state": "active", | 82 | "state": "active", | ||
| 73 | "url": | 83 | "url": | ||
| 74 | -7e832970c7bb/download/shakil_2020_environ._res._lett._15_114019.pdf", | 84 | -7e832970c7bb/download/shakil_2020_environ._res._lett._15_114019.pdf", | ||
| 75 | "url_type": "upload" | 85 | "url_type": "upload" | ||
| 76 | } | 86 | } | ||
| 77 | ], | 87 | ], | ||
| 78 | "state": "active", | 88 | "state": "active", | ||
| 79 | "summary": "This study highlights the pressing need for better | 89 | "summary": "This study highlights the pressing need for better | ||
| 80 | knowledge of sedimentary cascades, mobilization, and storage | 90 | knowledge of sedimentary cascades, mobilization, and storage | ||
| 81 | reservoirs in slump-affected streams, and baseline assessments of the | 91 | reservoirs in slump-affected streams, and baseline assessments of the | ||
| 82 | biodegradability of POC and cycling of particulate nutrients within a | 92 | biodegradability of POC and cycling of particulate nutrients within a | ||
| 83 | sedimentary cascade framework. Explicit incorporation of POC dynamics | 93 | sedimentary cascade framework. Explicit incorporation of POC dynamics | ||
| 84 | into our understanding of land-water carbon mobilization in the face | 94 | into our understanding of land-water carbon mobilization in the face | ||
| 85 | of permafrost thaw is critical for understanding implications of | 95 | of permafrost thaw is critical for understanding implications of | ||
| 86 | thermokarst for regional carbon cycling and fluvial ecosystems.", | 96 | thermokarst for regional carbon cycling and fluvial ecosystems.", | ||
| 87 | "tags": [ | 97 | "tags": [ | ||
| 88 | { | 98 | { | ||
| 89 | "display_name": "Carbon Cycle", | 99 | "display_name": "Carbon Cycle", | ||
| 90 | "id": "e8ca93b5-66ed-4fd2-bd0c-e6f762b36d40", | 100 | "id": "e8ca93b5-66ed-4fd2-bd0c-e6f762b36d40", | ||
| 91 | "name": "Carbon Cycle", | 101 | "name": "Carbon Cycle", | ||
| 92 | "state": "active", | 102 | "state": "active", | ||
| 93 | "vocabulary_id": null | 103 | "vocabulary_id": null | ||
| 94 | }, | 104 | }, | ||
| 95 | { | 105 | { | ||
| 96 | "display_name": "Hydrology", | 106 | "display_name": "Hydrology", | ||
| 97 | "id": "90e82f99-c39c-4818-a2a9-5feae1c15365", | 107 | "id": "90e82f99-c39c-4818-a2a9-5feae1c15365", | ||
| 98 | "name": "Hydrology", | 108 | "name": "Hydrology", | ||
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| 100 | "vocabulary_id": null | 110 | "vocabulary_id": null | ||
| 101 | }, | 111 | }, | ||
| 102 | { | 112 | { | ||
| 103 | "display_name": "Peel Plateau", | 113 | "display_name": "Peel Plateau", | ||
| 104 | "id": "a2af3d8d-bfe3-4fbc-a2a7-ef7c41ba3fe4", | 114 | "id": "a2af3d8d-bfe3-4fbc-a2a7-ef7c41ba3fe4", | ||
| 105 | "name": "Peel Plateau", | 115 | "name": "Peel Plateau", | ||
| 106 | "state": "active", | 116 | "state": "active", | ||
| 107 | "vocabulary_id": null | 117 | "vocabulary_id": null | ||
| 108 | }, | 118 | }, | ||
| 109 | { | 119 | { | ||
| 110 | "display_name": "Permafrost thaw", | 120 | "display_name": "Permafrost thaw", | ||
| 111 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | 121 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | ||
| 112 | "name": "Permafrost thaw", | 122 | "name": "Permafrost thaw", | ||
| 113 | "state": "active", | 123 | "state": "active", | ||
| 114 | "vocabulary_id": null | 124 | "vocabulary_id": null | ||
| 115 | }, | 125 | }, | ||
| 116 | { | 126 | { | ||
| 117 | "display_name": "Thaw Slumps", | 127 | "display_name": "Thaw Slumps", | ||
| 118 | "id": "8df558b1-dbdb-4daf-9519-661866ece350", | 128 | "id": "8df558b1-dbdb-4daf-9519-661866ece350", | ||
| 119 | "name": "Thaw Slumps", | 129 | "name": "Thaw Slumps", | ||
| 120 | "state": "active", | 130 | "state": "active", | ||
| 121 | "vocabulary_id": null | 131 | "vocabulary_id": null | ||
| 122 | }, | 132 | }, | ||
| 123 | { | 133 | { | ||
| 124 | "display_name": "Thermokarst", | 134 | "display_name": "Thermokarst", | ||
| 125 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | 135 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | ||
| 126 | "name": "Thermokarst", | 136 | "name": "Thermokarst", | ||
| 127 | "state": "active", | 137 | "state": "active", | ||
| 128 | "vocabulary_id": null | 138 | "vocabulary_id": null | ||
| 129 | } | 139 | } | ||
| 130 | ], | 140 | ], | ||
| t | 131 | "title": "Particulate dominance of organic carbon mobilization from | t | 141 | "title": "Particulate Dominance of Organic Carbon Mobilization from |
| 132 | thaw slumps on the Peel Plateau, NT", | 142 | Thaw Slumps on the Peel Plateau, NT", | ||
| 133 | "type": "dataset", | 143 | "type": "dataset", | ||
| 134 | "url": null, | 144 | "url": null, | ||
| 135 | "version": null | 145 | "version": null | ||
| 136 | } | 146 | } |