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f | 1 | { | f | 1 | { |
2 | "author": "Siewert Matthias Benjamin", | 2 | "author": "Siewert Matthias Benjamin", | ||
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.862961", | 5 | "doi": "10.1594/PANGAEA.862961", | ||
6 | "doi_date_published": "2016", | 6 | "doi_date_published": "2016", | ||
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": "Hugelius Gustaf", | 11 | "extra_author": "Hugelius Gustaf", | ||
12 | "orcid": "" | 12 | "orcid": "" | ||
13 | }, | 13 | }, | ||
14 | { | 14 | { | ||
15 | "extra_author": "Heim Birgit", | 15 | "extra_author": "Heim Birgit", | ||
16 | "orcid": "0000-0003-2614-9391" | 16 | "orcid": "0000-0003-2614-9391" | ||
17 | }, | 17 | }, | ||
18 | { | 18 | { | ||
19 | "extra_author": "Faucherre Samuel", | 19 | "extra_author": "Faucherre Samuel", | ||
20 | "orcid": "0000-0002-2464-4260" | 20 | "orcid": "0000-0002-2464-4260" | ||
21 | } | 21 | } | ||
22 | ], | 22 | ], | ||
23 | "groups": [], | 23 | "groups": [], | ||
24 | "id": "c896cabf-62db-4ed7-af8b-f298857a7f43", | 24 | "id": "c896cabf-62db-4ed7-af8b-f298857a7f43", | ||
25 | "isopen": false, | 25 | "isopen": false, | ||
26 | "license_id": "CC-BY-3.0", | 26 | "license_id": "CC-BY-3.0", | ||
27 | "license_title": "CC-BY-3.0", | 27 | "license_title": "CC-BY-3.0", | ||
28 | "metadata_created": "2023-01-12T13:31:16.904520", | 28 | "metadata_created": "2023-01-12T13:31:16.904520", | ||
t | 29 | "metadata_modified": "2023-08-04T09:32:40.384474", | t | 29 | "metadata_modified": "2023-08-04T09:33:46.856993", |
30 | "name": "png-doi-10-1594-pangaea-862961", | 30 | "name": "png-doi-10-1594-pangaea-862961", | ||
31 | "notes": "To project the future development of the soil organic | 31 | "notes": "To project the future development of the soil organic | ||
32 | carbon (SOC) storage in permafrost environments, the spatial and | 32 | carbon (SOC) storage in permafrost environments, the spatial and | ||
33 | vertical distribution of key soil properties and their landscape | 33 | vertical distribution of key soil properties and their landscape | ||
34 | controls needs to be understood. This article reports findings from | 34 | controls needs to be understood. This article reports findings from | ||
35 | the Arctic Lena River Delta where we sampled 50 soil pedons. These | 35 | the Arctic Lena River Delta where we sampled 50 soil pedons. These | ||
36 | were classified according to the U.S.D.A. Soil Taxonomy and fall | 36 | were classified according to the U.S.D.A. Soil Taxonomy and fall | ||
37 | mostly into the Gelisol soil order used for permafrost-affected soils. | 37 | mostly into the Gelisol soil order used for permafrost-affected soils. | ||
38 | Soil profiles have been sampled for the active layer (mean depth 58 | 38 | Soil profiles have been sampled for the active layer (mean depth 58 | ||
39 | \u00b1 10 cm) and the upper permafrost to one meter depth. We analyze | 39 | \u00b1 10 cm) and the upper permafrost to one meter depth. We analyze | ||
40 | SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, | 40 | SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, | ||
41 | visible ice and water content. These are compared for different | 41 | visible ice and water content. These are compared for different | ||
42 | landscape groupings of pedons according to geomorphology, soil and | 42 | landscape groupings of pedons according to geomorphology, soil and | ||
43 | land cover and for different vertical depth increments. High vertical | 43 | land cover and for different vertical depth increments. High vertical | ||
44 | resolution plots are used to understand soil development. These show | 44 | resolution plots are used to understand soil development. These show | ||
45 | that SOC storage can be highly variable with depth. We recommend the | 45 | that SOC storage can be highly variable with depth. We recommend the | ||
46 | treatment of permafrost-affected soils according to subdivisions into: | 46 | treatment of permafrost-affected soils according to subdivisions into: | ||
47 | the surface organic layer, mineral subsoil in the active layer, | 47 | the surface organic layer, mineral subsoil in the active layer, | ||
48 | organic enriched cryoturbated or buried horizons and the mineral | 48 | organic enriched cryoturbated or buried horizons and the mineral | ||
49 | subsoil in the permafrost. The major geomorphological units of a | 49 | subsoil in the permafrost. The major geomorphological units of a | ||
50 | subregion of the Lena River Delta were mapped with a land form | 50 | subregion of the Lena River Delta were mapped with a land form | ||
51 | classification using a data-fusion approach of optical satellite | 51 | classification using a data-fusion approach of optical satellite | ||
52 | imagery and digital elevation data to upscale SOC storage. Landscape | 52 | imagery and digital elevation data to upscale SOC storage. Landscape | ||
53 | mean SOC storage is estimated to 19.2 \u00b1 2.0 kg C/m**2. Our | 53 | mean SOC storage is estimated to 19.2 \u00b1 2.0 kg C/m**2. Our | ||
54 | results show that the geomorphological setting explains more soil | 54 | results show that the geomorphological setting explains more soil | ||
55 | variability than soil taxonomy classes or vegetation cover. The soils | 55 | variability than soil taxonomy classes or vegetation cover. The soils | ||
56 | from the oldest, Pleistocene aged, unit of the delta store the highest | 56 | from the oldest, Pleistocene aged, unit of the delta store the highest | ||
57 | amount of SOC per m2 followed by the Holocene river terrace. The | 57 | amount of SOC per m2 followed by the Holocene river terrace. The | ||
58 | Pleistocene terrace affected by thermal-degradation, the recent | 58 | Pleistocene terrace affected by thermal-degradation, the recent | ||
59 | floodplain and bare alluvial sediments store considerably less SOC in | 59 | floodplain and bare alluvial sediments store considerably less SOC in | ||
60 | descending order.", | 60 | descending order.", | ||
61 | "num_resources": 0, | 61 | "num_resources": 0, | ||
62 | "num_tags": 0, | 62 | "num_tags": 0, | ||
63 | "orcid": "0000-0003-2890-8873", | 63 | "orcid": "0000-0003-2890-8873", | ||
64 | "organization": { | 64 | "organization": { | ||
65 | "approval_status": "approved", | 65 | "approval_status": "approved", | ||
66 | "created": "2023-08-04T09:32:38.098376", | 66 | "created": "2023-08-04T09:32:38.098376", | ||
67 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 67 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
68 | Science): The information system PANGAEA is operated as an Open Access | 68 | Science): The information system PANGAEA is operated as an Open Access | ||
69 | library aimed at archiving, publishing and distributing georeferenced | 69 | library aimed at archiving, publishing and distributing georeferenced | ||
70 | data from earth system research. PANGAEA guarantees long-term | 70 | data from earth system research. PANGAEA guarantees long-term | ||
71 | availability (greater than 10 years) of its content. PANGAEA is open | 71 | availability (greater than 10 years) of its content. PANGAEA is open | ||
72 | to any project, institution, or individual scientist to use or to | 72 | to any project, institution, or individual scientist to use or to | ||
73 | archive and publish data. PANGAEA focuses on georeferenced | 73 | archive and publish data. PANGAEA focuses on georeferenced | ||
74 | observational data, experimental data, and models/simulations. | 74 | observational data, experimental data, and models/simulations. | ||
75 | Citability, comprehensive metadata descriptions, interoperability of | 75 | Citability, comprehensive metadata descriptions, interoperability of | ||
76 | data and metadata, a high degree of structural and semantic | 76 | data and metadata, a high degree of structural and semantic | ||
77 | harmonization of the data inventory as well as the commitment of the | 77 | harmonization of the data inventory as well as the commitment of the | ||
78 | hosting institutions ensures FAIRness of archived data.", | 78 | hosting institutions ensures FAIRness of archived data.", | ||
79 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | 79 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | ||
80 | "image_url": "pangea-logo.png", | 80 | "image_url": "pangea-logo.png", | ||
81 | "is_organization": true, | 81 | "is_organization": true, | ||
82 | "name": "pangaea", | 82 | "name": "pangaea", | ||
83 | "state": "active", | 83 | "state": "active", | ||
84 | "title": "PANGAEA (Agriculture)", | 84 | "title": "PANGAEA (Agriculture)", | ||
85 | "type": "organization" | 85 | "type": "organization" | ||
86 | }, | 86 | }, | ||
87 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | 87 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", | ||
88 | "private": false, | 88 | "private": false, | ||
89 | "publication_year": "2016", | 89 | "publication_year": "2016", | ||
90 | "related_identifiers": [ | 90 | "related_identifiers": [ | ||
91 | { | 91 | { | ||
92 | "authors": "Siewert Matthias Benjamin,Hugelius Gustaf,Heim | 92 | "authors": "Siewert Matthias Benjamin,Hugelius Gustaf,Heim | ||
93 | Birgit,Faucherre Samuel", | 93 | Birgit,Faucherre Samuel", | ||
94 | "email_authors": | 94 | "email_authors": | ||
95 | hias.siewert@umu.se,gustaf.hugelius@natgeo.su.se,birgit.heim@awi.de,", | 95 | hias.siewert@umu.se,gustaf.hugelius@natgeo.su.se,birgit.heim@awi.de,", | ||
96 | "identifier": "https://doi.org/10.1016/j.catena.2016.07.048", | 96 | "identifier": "https://doi.org/10.1016/j.catena.2016.07.048", | ||
97 | "identifier_type": "DOI", | 97 | "identifier_type": "DOI", | ||
98 | "orcid_authors": | 98 | "orcid_authors": | ||
99 | "0000-0003-2890-8873,,0000-0003-2614-9391,0000-0002-2464-4260", | 99 | "0000-0003-2890-8873,,0000-0003-2614-9391,0000-0002-2464-4260", | ||
100 | "relation_type": "IsSupplementTo", | 100 | "relation_type": "IsSupplementTo", | ||
101 | "source": "CATENA", | 101 | "source": "CATENA", | ||
102 | "title": "Landscape controls and vertical variability of soil | 102 | "title": "Landscape controls and vertical variability of soil | ||
103 | organic carbon storage in permafrost-affected soils of the Lena River | 103 | organic carbon storage in permafrost-affected soils of the Lena River | ||
104 | Delta", | 104 | Delta", | ||
105 | "year": "2016" | 105 | "year": "2016" | ||
106 | }, | 106 | }, | ||
107 | { | 107 | { | ||
108 | "authors": "", | 108 | "authors": "", | ||
109 | "email_authors": "", | 109 | "email_authors": "", | ||
110 | "identifier": "hdl:10013/epic.48156.d001", | 110 | "identifier": "hdl:10013/epic.48156.d001", | ||
111 | "identifier_type": "DOI", | 111 | "identifier_type": "DOI", | ||
112 | "orcid_authors": "", | 112 | "orcid_authors": "", | ||
113 | "relation_type": "References", | 113 | "relation_type": "References", | ||
114 | "source": "", | 114 | "source": "", | ||
115 | "title": "Documentation of landforms of the Lena Delta region", | 115 | "title": "Documentation of landforms of the Lena Delta region", | ||
116 | "year": "" | 116 | "year": "" | ||
117 | }, | 117 | }, | ||
118 | { | 118 | { | ||
119 | "authors": "", | 119 | "authors": "", | ||
120 | "email_authors": "", | 120 | "email_authors": "", | ||
121 | "identifier": "hdl:10013/epic.48156.d003", | 121 | "identifier": "hdl:10013/epic.48156.d003", | ||
122 | "identifier_type": "DOI", | 122 | "identifier_type": "DOI", | ||
123 | "orcid_authors": "", | 123 | "orcid_authors": "", | ||
124 | "relation_type": "References", | 124 | "relation_type": "References", | ||
125 | "source": "", | 125 | "source": "", | ||
126 | "title": "Map of locations", | 126 | "title": "Map of locations", | ||
127 | "year": "" | 127 | "year": "" | ||
128 | } | 128 | } | ||
129 | ], | 129 | ], | ||
130 | "relationships_as_object": [], | 130 | "relationships_as_object": [], | ||
131 | "relationships_as_subject": [], | 131 | "relationships_as_subject": [], | ||
132 | "repository_name": "PANGAEA (Data Publisher for Earth & | 132 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
133 | Environmental Science)", | 133 | Environmental Science)", | ||
134 | "resource_type": "application/zip - filename: Siewart_2016", | 134 | "resource_type": "application/zip - filename: Siewart_2016", | ||
135 | "resources": [], | 135 | "resources": [], | ||
136 | "services_used_list": "", | 136 | "services_used_list": "", | ||
137 | "source_metadata_created": "2016", | 137 | "source_metadata_created": "2016", | ||
138 | "source_metadata_modified": "", | 138 | "source_metadata_modified": "", | ||
139 | "state": "active", | 139 | "state": "active", | ||
140 | "subject_areas": [ | 140 | "subject_areas": [ | ||
141 | { | 141 | { | ||
142 | "subject_area_additional": "", | 142 | "subject_area_additional": "", | ||
143 | "subject_area_name": "Agriculture" | 143 | "subject_area_name": "Agriculture" | ||
144 | }, | 144 | }, | ||
145 | { | 145 | { | ||
146 | "subject_area_additional": "", | 146 | "subject_area_additional": "", | ||
147 | "subject_area_name": "LakesRivers" | 147 | "subject_area_name": "LakesRivers" | ||
148 | }, | 148 | }, | ||
149 | { | 149 | { | ||
150 | "subject_area_additional": "", | 150 | "subject_area_additional": "", | ||
151 | "subject_area_name": "Lithosphere" | 151 | "subject_area_name": "Lithosphere" | ||
152 | } | 152 | } | ||
153 | ], | 153 | ], | ||
154 | "tags": [], | 154 | "tags": [], | ||
155 | "title": "Soil organic carbon storage and soil properties for 50 | 155 | "title": "Soil organic carbon storage and soil properties for 50 | ||
156 | soil profiles in the Lena River Delta including land form description | 156 | soil profiles in the Lena River Delta including land form description | ||
157 | and map", | 157 | and map", | ||
158 | "type": "vdataset", | 158 | "type": "vdataset", | ||
159 | "url": "https://doi.org/10.1594/PANGAEA.862961" | 159 | "url": "https://doi.org/10.1594/PANGAEA.862961" | ||
160 | } | 160 | } |