Changes
On November 29, 2024 at 7:44:20 AM UTC,
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Set author of Morphological, chemical and physical characteristics of cryosolic soils from Arctic Canada to Tarnocai, Charles (previously Tarnocai Charles)
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Changed value of field
extra_authors
to[{'extra_author': 'Bockheim, James G', 'familyName': 'Bockheim', 'givenName': 'James G', 'orcid': ''}]
in Morphological, chemical and physical characteristics of cryosolic soils from Arctic Canada
f | 1 | { | f | 1 | { |
n | 2 | "author": "Tarnocai Charles", | n | 2 | "author": "Tarnocai, Charles", |
3 | "author_email": "", | 3 | "author_email": "", | ||
n | n | 4 | "citation": [], | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 5 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.1594/PANGAEA.838954", | 6 | "doi": "10.1594/PANGAEA.838954", | ||
6 | "doi_date_published": "2011", | 7 | "doi_date_published": "2011", | ||
7 | "doi_publisher": "", | 8 | "doi_publisher": "", | ||
8 | "doi_status": "True", | 9 | "doi_status": "True", | ||
9 | "extra_authors": [ | 10 | "extra_authors": [ | ||
10 | { | 11 | { | ||
n | 11 | "extra_author": "Bockheim James G", | n | 12 | "extra_author": "Bockheim, James G", |
13 | "familyName": "Bockheim", | ||||
14 | "givenName": "James G", | ||||
12 | "orcid": "" | 15 | "orcid": "" | ||
13 | } | 16 | } | ||
14 | ], | 17 | ], | ||
n | n | 18 | "familyName": "Tarnocai", | ||
19 | "givenName": "Charles", | ||||
15 | "groups": [], | 20 | "groups": [], | ||
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20 | "metadata_created": "2023-01-12T13:31:16.670775", | 25 | "metadata_created": "2023-01-12T13:31:16.670775", | ||
n | 21 | "metadata_modified": "2023-08-04T09:33:46.731724", | n | 26 | "metadata_modified": "2024-11-29T07:44:20.691911", |
22 | "name": "png-doi-10-1594-pangaea-838954", | 27 | "name": "png-doi-10-1594-pangaea-838954", | ||
23 | "notes": "Cryosols are permafrost-affected soils whose genesis is | 28 | "notes": "Cryosols are permafrost-affected soils whose genesis is | ||
24 | dominated by cryogenic processes, resulting in unique | 29 | dominated by cryogenic processes, resulting in unique | ||
25 | macromorphologies, micromorphologies, thermal characteristics, and | 30 | macromorphologies, micromorphologies, thermal characteristics, and | ||
26 | physical and chemical properties. In addition, these soils are carbon | 31 | physical and chemical properties. In addition, these soils are carbon | ||
27 | sinks, storing high amounts of organic carbon collected for thousands | 32 | sinks, storing high amounts of organic carbon collected for thousands | ||
28 | of years. In the Canadian soil classification, the Cryosolic Order | 33 | of years. In the Canadian soil classification, the Cryosolic Order | ||
29 | includes mineral and organic soils that have both cryogenic properties | 34 | 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 | 35 | 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 | 36 | divided into Turbic, Static and Organic great groups on the basis of | ||
32 | the soil materials (mineral or organic), cryogenic properties and | 37 | the soil materials (mineral or organic), cryogenic properties and | ||
33 | depth to permafrost. The great groups are subdivided into subgroups on | 38 | depth to permafrost. The great groups are subdivided into subgroups on | ||
34 | the basis of soil development and the resulting diagnostic soil | 39 | the basis of soil development and the resulting diagnostic soil | ||
35 | horizons. Cryosols are commonly associated with the presence of ground | 40 | horizons. Cryosols are commonly associated with the presence of ground | ||
36 | ice in the subsoil. This causes serious problems when areas containing | 41 | ice in the subsoil. This causes serious problems when areas containing | ||
37 | these soils are used for agriculture and construction projects (such | 42 | these soils are used for agriculture and construction projects (such | ||
38 | as roads, town sites and airstrips). Therefore, where Cryosols have | 43 | as roads, town sites and airstrips). Therefore, where Cryosols have | ||
39 | high ice content, it is especially important either to avoid these | 44 | high ice content, it is especially important either to avoid these | ||
40 | activities or to use farming and construction methods that maintain | 45 | activities or to use farming and construction methods that maintain | ||
41 | the negative thermal balance.", | 46 | the negative thermal balance.", | ||
42 | "num_resources": 0, | 47 | "num_resources": 0, | ||
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44 | "orcid": "", | 49 | "orcid": "", | ||
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46 | "approval_status": "approved", | 51 | "approval_status": "approved", | ||
47 | "created": "2023-08-04T09:32:38.098376", | 52 | "created": "2023-08-04T09:32:38.098376", | ||
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69 | "private": false, | 74 | "private": false, | ||
70 | "publication_year": "2011", | 75 | "publication_year": "2011", | ||
71 | "related_identifiers": [ | 76 | "related_identifiers": [ | ||
72 | { | 77 | { | ||
73 | "authors": "Tarnocai Charles,Bockheim James G", | 78 | "authors": "Tarnocai Charles,Bockheim James G", | ||
74 | "email_authors": "tarnocaict@agr.gc.ca,bockheim@wisc.edu", | 79 | "email_authors": "tarnocaict@agr.gc.ca,bockheim@wisc.edu", | ||
75 | "identifier": "https://doi.org/10.4141/cjss10020", | 80 | "identifier": "https://doi.org/10.4141/cjss10020", | ||
76 | "identifier_type": "DOI", | 81 | "identifier_type": "DOI", | ||
77 | "orcid_authors": ",", | 82 | "orcid_authors": ",", | ||
78 | "relation_type": "IsSupplementTo", | 83 | "relation_type": "IsSupplementTo", | ||
79 | "source": "Canadian Journal of Soil Science", | 84 | "source": "Canadian Journal of Soil Science", | ||
80 | "title": "Cryosolic soils of Canada: Genesis, distribution, and | 85 | "title": "Cryosolic soils of Canada: Genesis, distribution, and | ||
81 | classification", | 86 | classification", | ||
82 | "year": "2011" | 87 | "year": "2011" | ||
83 | } | 88 | } | ||
84 | ], | 89 | ], | ||
85 | "relationships_as_object": [], | 90 | "relationships_as_object": [], | ||
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88 | Environmental Science)", | 93 | Environmental Science)", | ||
89 | "resource_type": "application/zip - filename: | 94 | "resource_type": "application/zip - filename: | ||
90 | Tarnocai-Bockheim_2011", | 95 | Tarnocai-Bockheim_2011", | ||
91 | "resources": [], | 96 | "resources": [], | ||
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93 | "source_metadata_created": "2011", | 97 | "source_metadata_created": "2011", | ||
94 | "source_metadata_modified": "", | 98 | "source_metadata_modified": "", | ||
95 | "state": "active", | 99 | "state": "active", | ||
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100 | }, | 104 | }, | ||
101 | { | 105 | { | ||
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103 | "subject_area_name": "Lithosphere" | 107 | "subject_area_name": "Lithosphere" | ||
104 | } | 108 | } | ||
105 | ], | 109 | ], | ||
106 | "tags": [], | 110 | "tags": [], | ||
107 | "title": "Morphological, chemical and physical characteristics of | 111 | "title": "Morphological, chemical and physical characteristics of | ||
108 | cryosolic soils from Arctic Canada", | 112 | cryosolic soils from Arctic Canada", | ||
109 | "type": "vdataset", | 113 | "type": "vdataset", | ||
110 | "url": "https://doi.org/10.1594/PANGAEA.838954" | 114 | "url": "https://doi.org/10.1594/PANGAEA.838954" | ||
111 | } | 115 | } |