Changes
On August 4, 2023 at 9:32:40 AM UTC, admin:
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Moved Morphological, chemical and physical characteristics of cryosolic soils from Arctic Canada from organization PANGEA (Agriculture) to organization PANGAEA (Agriculture)
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Changed value of field
repository_name
toPANGAEA (Data Publisher for Earth & Environmental Science)
in Morphological, chemical and physical characteristics of cryosolic soils from Arctic Canada
f | 1 | { | f | 1 | { |
2 | "author": "Tarnocai Charles", | 2 | "author": "Tarnocai Charles", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.1594/PANGAEA.838954", | 5 | "doi": "10.1594/PANGAEA.838954", | ||
6 | "doi_date_published": "2011", | 6 | "doi_date_published": "2011", | ||
7 | "doi_publisher": "", | 7 | "doi_publisher": "", | ||
8 | "doi_status": "True", | 8 | "doi_status": "True", | ||
9 | "extra_authors": [ | 9 | "extra_authors": [ | ||
10 | { | 10 | { | ||
11 | "extra_author": "Bockheim James G", | 11 | "extra_author": "Bockheim James G", | ||
12 | "orcid": "" | 12 | "orcid": "" | ||
13 | } | 13 | } | ||
14 | ], | 14 | ], | ||
15 | "groups": [], | 15 | "groups": [], | ||
16 | "id": "7fdcff46-5fbb-4ffc-8fc5-486050854f96", | 16 | "id": "7fdcff46-5fbb-4ffc-8fc5-486050854f96", | ||
17 | "isopen": false, | 17 | "isopen": false, | ||
18 | "license_id": "CC-BY-3.0", | 18 | "license_id": "CC-BY-3.0", | ||
19 | "license_title": "CC-BY-3.0", | 19 | "license_title": "CC-BY-3.0", | ||
20 | "metadata_created": "2023-01-12T13:31:16.670775", | 20 | "metadata_created": "2023-01-12T13:31:16.670775", | ||
n | 21 | "metadata_modified": "2023-01-12T13:31:16.670780", | n | 21 | "metadata_modified": "2023-08-04T09:32:40.060681", |
22 | "name": "png-doi-10-1594-pangaea-838954", | 22 | "name": "png-doi-10-1594-pangaea-838954", | ||
23 | "notes": "Cryosols are permafrost-affected soils whose genesis is | 23 | "notes": "Cryosols are permafrost-affected soils whose genesis is | ||
24 | dominated by cryogenic processes, resulting in unique | 24 | dominated by cryogenic processes, resulting in unique | ||
25 | macromorphologies, micromorphologies, thermal characteristics, and | 25 | macromorphologies, micromorphologies, thermal characteristics, and | ||
26 | physical and chemical properties. In addition, these soils are carbon | 26 | physical and chemical properties. In addition, these soils are carbon | ||
27 | sinks, storing high amounts of organic carbon collected for thousands | 27 | sinks, storing high amounts of organic carbon collected for thousands | ||
28 | of years. In the Canadian soil classification, the Cryosolic Order | 28 | of years. In the Canadian soil classification, the Cryosolic Order | ||
29 | includes mineral and organic soils that have both cryogenic properties | 29 | includes mineral and organic soils that have both cryogenic properties | ||
30 | and permafrost within 1 or 2 m of the soil surface. This soil order is | 30 | and permafrost within 1 or 2 m of the soil surface. This soil order is | ||
31 | divided into Turbic, Static and Organic great groups on the basis of | 31 | divided into Turbic, Static and Organic great groups on the basis of | ||
32 | the soil materials (mineral or organic), cryogenic properties and | 32 | the soil materials (mineral or organic), cryogenic properties and | ||
33 | depth to permafrost. The great groups are subdivided into subgroups on | 33 | depth to permafrost. The great groups are subdivided into subgroups on | ||
34 | the basis of soil development and the resulting diagnostic soil | 34 | the basis of soil development and the resulting diagnostic soil | ||
35 | horizons. Cryosols are commonly associated with the presence of ground | 35 | horizons. Cryosols are commonly associated with the presence of ground | ||
36 | ice in the subsoil. This causes serious problems when areas containing | 36 | ice in the subsoil. This causes serious problems when areas containing | ||
37 | these soils are used for agriculture and construction projects (such | 37 | these soils are used for agriculture and construction projects (such | ||
38 | as roads, town sites and airstrips). Therefore, where Cryosols have | 38 | as roads, town sites and airstrips). Therefore, where Cryosols have | ||
39 | high ice content, it is especially important either to avoid these | 39 | high ice content, it is especially important either to avoid these | ||
40 | activities or to use farming and construction methods that maintain | 40 | activities or to use farming and construction methods that maintain | ||
41 | the negative thermal balance.", | 41 | the negative thermal balance.", | ||
42 | "num_resources": 0, | 42 | "num_resources": 0, | ||
43 | "num_tags": 0, | 43 | "num_tags": 0, | ||
44 | "orcid": "", | 44 | "orcid": "", | ||
45 | "organization": { | 45 | "organization": { | ||
46 | "approval_status": "approved", | 46 | "approval_status": "approved", | ||
n | 47 | "created": "2023-01-12T13:31:15.534211", | n | 47 | "created": "2023-08-04T09:32:38.098376", |
48 | "description": "PANGEA (Data Publisher for Earth & Environmental | 48 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
49 | Science): The information system PANGAEA is operated as an Open Access | 49 | Science): The information system PANGAEA is operated as an Open Access | ||
50 | library aimed at archiving, publishing and distributing georeferenced | 50 | library aimed at archiving, publishing and distributing georeferenced | ||
51 | data from earth system research. PANGAEA guarantees long-term | 51 | data from earth system research. PANGAEA guarantees long-term | ||
52 | availability (greater than 10 years) of its content. PANGAEA is open | 52 | availability (greater than 10 years) of its content. PANGAEA is open | ||
53 | to any project, institution, or individual scientist to use or to | 53 | to any project, institution, or individual scientist to use or to | ||
54 | archive and publish data. PANGAEA focuses on georeferenced | 54 | archive and publish data. PANGAEA focuses on georeferenced | ||
55 | observational data, experimental data, and models/simulations. | 55 | observational data, experimental data, and models/simulations. | ||
56 | Citability, comprehensive metadata descriptions, interoperability of | 56 | Citability, comprehensive metadata descriptions, interoperability of | ||
57 | data and metadata, a high degree of structural and semantic | 57 | data and metadata, a high degree of structural and semantic | ||
58 | harmonization of the data inventory as well as the commitment of the | 58 | harmonization of the data inventory as well as the commitment of the | ||
59 | hosting institutions ensures FAIRness of archived data.", | 59 | hosting institutions ensures FAIRness of archived data.", | ||
n | 60 | "id": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 60 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
61 | "image_url": "pangea-logo.png", | 61 | "image_url": "pangea-logo.png", | ||
62 | "is_organization": true, | 62 | "is_organization": true, | ||
n | 63 | "name": "pangea", | n | 63 | "name": "pangaea", |
64 | "state": "active", | 64 | "state": "active", | ||
n | 65 | "title": "PANGEA (Agriculture)", | n | 65 | "title": "PANGAEA (Agriculture)", |
66 | "type": "organization" | 66 | "type": "organization" | ||
67 | }, | 67 | }, | ||
n | 68 | "owner_org": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 68 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
69 | "private": false, | 69 | "private": false, | ||
70 | "publication_year": "2011", | 70 | "publication_year": "2011", | ||
n | n | 71 | "related_identifiers": [ | ||
72 | { | ||||
73 | "authors": "Tarnocai Charles,Bockheim James G", | ||||
74 | "email_authors": "tarnocaict@agr.gc.ca,bockheim@wisc.edu", | ||||
75 | "identifier": "https://doi.org/10.4141/cjss10020", | ||||
76 | "identifier_type": "DOI", | ||||
77 | "orcid_authors": ",", | ||||
78 | "relation_type": "IsSupplementTo", | ||||
79 | "source": "Canadian Journal of Soil Science", | ||||
80 | "title": "Cryosolic soils of Canada: Genesis, distribution, and | ||||
81 | classification", | ||||
82 | "year": "2011" | ||||
83 | } | ||||
84 | ], | ||||
71 | "relationships_as_object": [], | 85 | "relationships_as_object": [], | ||
72 | "relationships_as_subject": [], | 86 | "relationships_as_subject": [], | ||
n | 73 | "repository_name": "PANGEA (Data Publisher for Earth & Environmental | n | 87 | "repository_name": "PANGAEA (Data Publisher for Earth & |
74 | Science)", | 88 | Environmental Science)", | ||
75 | "resource_type": "application/zip - filename: | 89 | "resource_type": "application/zip - filename: | ||
76 | Tarnocai-Bockheim_2011", | 90 | Tarnocai-Bockheim_2011", | ||
77 | "resources": [], | 91 | "resources": [], | ||
t | t | 92 | "services_used_list": "", | ||
78 | "source_metadata_created": "2011", | 93 | "source_metadata_created": "2011", | ||
79 | "source_metadata_modified": "", | 94 | "source_metadata_modified": "", | ||
80 | "state": "active", | 95 | "state": "active", | ||
81 | "subject_areas": [ | 96 | "subject_areas": [ | ||
82 | { | 97 | { | ||
83 | "subject_area_additional": "", | 98 | "subject_area_additional": "", | ||
84 | "subject_area_name": "Agriculture" | 99 | "subject_area_name": "Agriculture" | ||
85 | }, | 100 | }, | ||
86 | { | 101 | { | ||
87 | "subject_area_additional": "", | 102 | "subject_area_additional": "", | ||
88 | "subject_area_name": "Lithosphere" | 103 | "subject_area_name": "Lithosphere" | ||
89 | } | 104 | } | ||
90 | ], | 105 | ], | ||
91 | "tags": [], | 106 | "tags": [], | ||
92 | "title": "Morphological, chemical and physical characteristics of | 107 | "title": "Morphological, chemical and physical characteristics of | ||
93 | cryosolic soils from Arctic Canada", | 108 | cryosolic soils from Arctic Canada", | ||
94 | "type": "vdataset", | 109 | "type": "vdataset", | ||
95 | "url": "https://doi.org/10.1594/PANGAEA.838954" | 110 | "url": "https://doi.org/10.1594/PANGAEA.838954" | ||
96 | } | 111 | } |