Changes
On August 4, 2023 at 9:33:46 AM UTC, admin:
-
No fields were updated. See the metadata diff for more details.
f | 1 | { | f | 1 | { |
2 | "author": "Lesovaya SN", | 2 | "author": "Lesovaya SN", | ||
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.815783", | 5 | "doi": "10.1594/PANGAEA.815783", | ||
6 | "doi_date_published": "2012", | 6 | "doi_date_published": "2012", | ||
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": "Goryachkin Sergey V", | 11 | "extra_author": "Goryachkin Sergey V", | ||
12 | "orcid": "0000-0002-3489-6584" | 12 | "orcid": "0000-0002-3489-6584" | ||
13 | }, | 13 | }, | ||
14 | { | 14 | { | ||
15 | "extra_author": "Polekhovskii Yu S", | 15 | "extra_author": "Polekhovskii Yu S", | ||
16 | "orcid": "" | 16 | "orcid": "" | ||
17 | } | 17 | } | ||
18 | ], | 18 | ], | ||
19 | "groups": [], | 19 | "groups": [], | ||
20 | "id": "ec912f16-62d2-48cf-ab64-c1ac86dab9db", | 20 | "id": "ec912f16-62d2-48cf-ab64-c1ac86dab9db", | ||
21 | "isopen": false, | 21 | "isopen": false, | ||
22 | "license_id": "CC-BY-3.0", | 22 | "license_id": "CC-BY-3.0", | ||
23 | "license_title": "CC-BY-3.0", | 23 | "license_title": "CC-BY-3.0", | ||
24 | "metadata_created": "2023-01-12T13:31:16.350249", | 24 | "metadata_created": "2023-01-12T13:31:16.350249", | ||
t | 25 | "metadata_modified": "2023-08-04T09:32:39.457947", | t | 25 | "metadata_modified": "2023-08-04T09:33:46.569401", |
26 | "name": "png-doi-10-1594-pangaea-815783", | 26 | "name": "png-doi-10-1594-pangaea-815783", | ||
27 | "notes": "Gravelly clay loamy and clayey soils developed from the | 27 | "notes": "Gravelly clay loamy and clayey soils developed from the | ||
28 | derivatives of ultramafic rocks of the dunite-harzburgite complex of | 28 | derivatives of ultramafic rocks of the dunite-harzburgite complex of | ||
29 | the Rai-Iz massif in the Polar Urals have been studied. They are | 29 | the Rai-Iz massif in the Polar Urals have been studied. They are | ||
30 | represented by raw-humus pelozems (weakly developed clayey soils) | 30 | represented by raw-humus pelozems (weakly developed clayey soils) | ||
31 | under conditions of perfect drainage on steep slopes and by the | 31 | under conditions of perfect drainage on steep slopes and by the | ||
32 | gleyzems (Gleysols) with vivid gley color patterns in the eluvial | 32 | gleyzems (Gleysols) with vivid gley color patterns in the eluvial | ||
33 | positions on leveled elements of the relief. The magnesium released | 33 | positions on leveled elements of the relief. The magnesium released | ||
34 | from the silicates with the high content of this element (mainly from | 34 | from the silicates with the high content of this element (mainly from | ||
35 | olivine) specifies the neutral-alkaline reaction in these soils. | 35 | olivine) specifies the neutral-alkaline reaction in these soils. | ||
36 | Cryoturbation, the accumulation of raw humus, the impregnation of the | 36 | Cryoturbation, the accumulation of raw humus, the impregnation of the | ||
37 | soil mass with humic substances, gleyzation, and the ferrugination of | 37 | soil mass with humic substances, gleyzation, and the ferrugination of | ||
38 | the gleyed horizons are also clearly pronounced in the studied soils. | 38 | the gleyed horizons are also clearly pronounced in the studied soils. | ||
39 | Despite the high pH values, the destruction of supergene smectites in | 39 | Despite the high pH values, the destruction of supergene smectites in | ||
40 | the upper horizons and ferrugination (the accumulation of iron | 40 | the upper horizons and ferrugination (the accumulation of iron | ||
41 | hydroxides) in the microfissures dissecting the grains of olivine, | 41 | hydroxides) in the microfissures dissecting the grains of olivine, | ||
42 | pyroxene, and serpentine, and in decomposing plant tissues take place. | 42 | pyroxene, and serpentine, and in decomposing plant tissues take place. | ||
43 | The development of these processes may be related to the local | 43 | The development of these processes may be related to the local | ||
44 | acidification (neutralization) of the soil medium under the impact of | 44 | acidification (neutralization) of the soil medium under the impact of | ||
45 | biota and carbonic acids. The specificity of gleyzation in the soils | 45 | biota and carbonic acids. The specificity of gleyzation in the soils | ||
46 | developing from ultra-mafic rocks is shown in the absence of iron | 46 | developing from ultra-mafic rocks is shown in the absence of iron | ||
47 | depletion from the fine earth material against the background of the | 47 | depletion from the fine earth material against the background of the | ||
48 | greenish blue gley color pattern.", | 48 | greenish blue gley color pattern.", | ||
49 | "num_resources": 0, | 49 | "num_resources": 0, | ||
50 | "num_tags": 0, | 50 | "num_tags": 0, | ||
51 | "orcid": "", | 51 | "orcid": "", | ||
52 | "organization": { | 52 | "organization": { | ||
53 | "approval_status": "approved", | 53 | "approval_status": "approved", | ||
54 | "created": "2023-08-04T09:32:38.098376", | 54 | "created": "2023-08-04T09:32:38.098376", | ||
55 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 55 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
56 | Science): The information system PANGAEA is operated as an Open Access | 56 | Science): The information system PANGAEA is operated as an Open Access | ||
57 | library aimed at archiving, publishing and distributing georeferenced | 57 | library aimed at archiving, publishing and distributing georeferenced | ||
58 | data from earth system research. PANGAEA guarantees long-term | 58 | data from earth system research. PANGAEA guarantees long-term | ||
59 | availability (greater than 10 years) of its content. PANGAEA is open | 59 | availability (greater than 10 years) of its content. PANGAEA is open | ||
60 | to any project, institution, or individual scientist to use or to | 60 | to any project, institution, or individual scientist to use or to | ||
61 | archive and publish data. PANGAEA focuses on georeferenced | 61 | archive and publish data. PANGAEA focuses on georeferenced | ||
62 | observational data, experimental data, and models/simulations. | 62 | observational data, experimental data, and models/simulations. | ||
63 | Citability, comprehensive metadata descriptions, interoperability of | 63 | Citability, comprehensive metadata descriptions, interoperability of | ||
64 | data and metadata, a high degree of structural and semantic | 64 | data and metadata, a high degree of structural and semantic | ||
65 | harmonization of the data inventory as well as the commitment of the | 65 | harmonization of the data inventory as well as the commitment of the | ||
66 | hosting institutions ensures FAIRness of archived data.", | 66 | hosting institutions ensures FAIRness of archived data.", | ||
67 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | 67 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | ||
68 | "image_url": "pangea-logo.png", | 68 | "image_url": "pangea-logo.png", | ||
69 | "is_organization": true, | 69 | "is_organization": true, | ||
70 | "name": "pangaea", | 70 | "name": "pangaea", | ||
71 | "state": "active", | 71 | "state": "active", | ||
72 | "title": "PANGAEA (Agriculture)", | 72 | "title": "PANGAEA (Agriculture)", | ||
73 | "type": "organization" | 73 | "type": "organization" | ||
74 | }, | 74 | }, | ||
75 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | 75 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | ||
76 | "private": false, | 76 | "private": false, | ||
77 | "publication_year": "2012", | 77 | "publication_year": "2012", | ||
78 | "related_identifiers": [ | 78 | "related_identifiers": [ | ||
79 | { | 79 | { | ||
80 | "authors": "Lesovaya SN,Goryachkin Sergey V,Polekhovskii Yu S", | 80 | "authors": "Lesovaya SN,Goryachkin Sergey V,Polekhovskii Yu S", | ||
81 | "email_authors": ",,", | 81 | "email_authors": ",,", | ||
82 | "identifier": "https://doi.org/10.1134/S1064229312010097", | 82 | "identifier": "https://doi.org/10.1134/S1064229312010097", | ||
83 | "identifier_type": "DOI", | 83 | "identifier_type": "DOI", | ||
84 | "orcid_authors": ",0000-0002-3489-6584,", | 84 | "orcid_authors": ",0000-0002-3489-6584,", | ||
85 | "relation_type": "IsSupplementTo", | 85 | "relation_type": "IsSupplementTo", | ||
86 | "source": "Eurasian Soil Science", | 86 | "source": "Eurasian Soil Science", | ||
87 | "title": "Soil formation and weathering on ultramafic rocks in | 87 | "title": "Soil formation and weathering on ultramafic rocks in | ||
88 | the mountainous tundra of the Rai-Iz massif, Polar Urals", | 88 | the mountainous tundra of the Rai-Iz massif, Polar Urals", | ||
89 | "year": "2012" | 89 | "year": "2012" | ||
90 | } | 90 | } | ||
91 | ], | 91 | ], | ||
92 | "relationships_as_object": [], | 92 | "relationships_as_object": [], | ||
93 | "relationships_as_subject": [], | 93 | "relationships_as_subject": [], | ||
94 | "repository_name": "PANGAEA (Data Publisher for Earth & | 94 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
95 | Environmental Science)", | 95 | Environmental Science)", | ||
96 | "resource_type": "application/zip - filename: Lesovaya_2012", | 96 | "resource_type": "application/zip - filename: Lesovaya_2012", | ||
97 | "resources": [], | 97 | "resources": [], | ||
98 | "services_used_list": "", | 98 | "services_used_list": "", | ||
99 | "source_metadata_created": "2012", | 99 | "source_metadata_created": "2012", | ||
100 | "source_metadata_modified": "", | 100 | "source_metadata_modified": "", | ||
101 | "state": "active", | 101 | "state": "active", | ||
102 | "subject_areas": [ | 102 | "subject_areas": [ | ||
103 | { | 103 | { | ||
104 | "subject_area_additional": "", | 104 | "subject_area_additional": "", | ||
105 | "subject_area_name": "Agriculture" | 105 | "subject_area_name": "Agriculture" | ||
106 | }, | 106 | }, | ||
107 | { | 107 | { | ||
108 | "subject_area_additional": "", | 108 | "subject_area_additional": "", | ||
109 | "subject_area_name": "Lithosphere" | 109 | "subject_area_name": "Lithosphere" | ||
110 | } | 110 | } | ||
111 | ], | 111 | ], | ||
112 | "tags": [], | 112 | "tags": [], | ||
113 | "title": "Soil chemistry and particle size distribution of | 113 | "title": "Soil chemistry and particle size distribution of | ||
114 | mountainous tundra soils in the Rai-Iz Massif", | 114 | mountainous tundra soils in the Rai-Iz Massif", | ||
115 | "type": "vdataset", | 115 | "type": "vdataset", | ||
116 | "url": "https://doi.org/10.1594/PANGAEA.815783" | 116 | "url": "https://doi.org/10.1594/PANGAEA.815783" | ||
117 | } | 117 | } |