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On October 12, 2021 at 8:35:34 AM UTC, Administrator:
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Changed value of field
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in Crack propagation speeds in weak snowpack layers from three events: PST, whumpf and slab avalanche
f | 1 | { | f | 1 | { |
2 | "author": "[{\"affiliation\": \"WSL Institute for Snow and Avalanche | 2 | "author": "[{\"affiliation\": \"WSL Institute for Snow and Avalanche | ||
3 | Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", | 3 | Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", | ||
4 | \"affiliation_03\": \"\", \"data_credit\": [\"collection\", | 4 | \"affiliation_03\": \"\", \"data_credit\": [\"collection\", | ||
5 | \"validation\", \"software\", \"publication\"], \"email\": | 5 | \"validation\", \"software\", \"publication\"], \"email\": | ||
6 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | 6 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | ||
7 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, | 7 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, | ||
8 | {\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, | 8 | {\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, | ||
9 | Davos, Switzerland\", \"affiliation_02\": \"SLF\", \"affiliation_03\": | 9 | Davos, Switzerland\", \"affiliation_02\": \"SLF\", \"affiliation_03\": | ||
10 | \"\", \"data_credit\": [\"collection\", \"publication\", | 10 | \"\", \"data_credit\": [\"collection\", \"publication\", | ||
11 | \"supervision\"], \"email\": \"vanherwijnen@slf.ch\", \"given_name\": | 11 | \"supervision\"], \"email\": \"vanherwijnen@slf.ch\", \"given_name\": | ||
12 | \"Alec\", \"identifier\": \"0000-0001-5637-6486\", \"name\": \"van | 12 | \"Alec\", \"identifier\": \"0000-0001-5637-6486\", \"name\": \"van | ||
13 | Herwijnen\"}, {\"affiliation\": \"WSL Institute for Snow and Avalanche | 13 | Herwijnen\"}, {\"affiliation\": \"WSL Institute for Snow and Avalanche | ||
14 | Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", | 14 | Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", | ||
15 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | 15 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | ||
16 | \"software\"], \"email\": \"gregoire.bobillier@slf.ch\", | 16 | \"software\"], \"email\": \"gregoire.bobillier@slf.ch\", | ||
17 | \"given_name\": \"Gr\\u00e9goire\", \"identifier\": \"\", \"name\": | 17 | \"given_name\": \"Gr\\u00e9goire\", \"identifier\": \"\", \"name\": | ||
18 | \"Bobillier\"}, {\"affiliation\": \"Univ. Grenoble Alpes, CNRS, | 18 | \"Bobillier\"}, {\"affiliation\": \"Univ. Grenoble Alpes, CNRS, | ||
19 | ISTerre Grenoble, FR\", \"affiliation_02\": \"\", \"affiliation_03\": | 19 | ISTerre Grenoble, FR\", \"affiliation_02\": \"\", \"affiliation_03\": | ||
20 | \"Univ. Grenoble Alpes, CNRS, ISTerre Grenoble, FR\", \"data_credit\": | 20 | \"Univ. Grenoble Alpes, CNRS, ISTerre Grenoble, FR\", \"data_credit\": | ||
21 | [\"curation\", \"software\"], \"email\": | 21 | [\"curation\", \"software\"], \"email\": | ||
22 | \"eric.larose@univ-grenoble-alpes.fr\", \"given_name\": \"Eric\", | 22 | \"eric.larose@univ-grenoble-alpes.fr\", \"given_name\": \"Eric\", | ||
23 | \"identifier\": \"\", \"name\": \"Larose\"}, {\"affiliation\": \"Univ. | 23 | \"identifier\": \"\", \"name\": \"Larose\"}, {\"affiliation\": \"Univ. | ||
24 | Grenoble Alpes, CNRS, ISTerre Grenoble, FR\", \"affiliation_02\": | 24 | Grenoble Alpes, CNRS, ISTerre Grenoble, FR\", \"affiliation_02\": | ||
25 | \"\", \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | 25 | \"\", \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | ||
26 | \"software\"], \"email\": \"ludovic.moreau@univ-grenoble-alpes.fr\", | 26 | \"software\"], \"email\": \"ludovic.moreau@univ-grenoble-alpes.fr\", | ||
27 | \"given_name\": \"Ludovic\", \"identifier\": \"\", \"name\": | 27 | \"given_name\": \"Ludovic\", \"identifier\": \"\", \"name\": | ||
28 | \"Moreau\"}, {\"affiliation\": \"EPFL, SLAB Snow and Avalanche | 28 | \"Moreau\"}, {\"affiliation\": \"EPFL, SLAB Snow and Avalanche | ||
29 | Simulation Laboratory Lausanne, VD, CH\", \"affiliation_02\": \"\", | 29 | Simulation Laboratory Lausanne, VD, CH\", \"affiliation_02\": \"\", | ||
30 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | 30 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | ||
31 | \"software\"], \"email\": \"bertil.trottet@epfl.ch\", \"given_name\": | 31 | \"software\"], \"email\": \"bertil.trottet@epfl.ch\", \"given_name\": | ||
32 | \"Bertil\", \"identifier\": \"\", \"name\": \"Trottet\"}, | 32 | \"Bertil\", \"identifier\": \"\", \"name\": \"Trottet\"}, | ||
33 | {\"affiliation\": \"EPFL, SLAB Snow and Avalanche Simulation | 33 | {\"affiliation\": \"EPFL, SLAB Snow and Avalanche Simulation | ||
34 | Laboratory Lausanne, VD, CH\", \"affiliation_02\": \"\", | 34 | Laboratory Lausanne, VD, CH\", \"affiliation_02\": \"\", | ||
35 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | 35 | \"affiliation_03\": \"\", \"data_credit\": [\"curation\", | ||
36 | \"software\"], \"email\": \"johan.gaume@epfl.ch\", \"given_name\": | 36 | \"software\"], \"email\": \"johan.gaume@epfl.ch\", \"given_name\": | ||
37 | \"Johan\", \"identifier\": \"0000-0001-8931-752X\", \"name\": | 37 | \"Johan\", \"identifier\": \"0000-0001-8931-752X\", \"name\": | ||
38 | \"Gaume\"}, {\"affiliation\": \"WSL Institute for Snow and Avalanche | 38 | \"Gaume\"}, {\"affiliation\": \"WSL Institute for Snow and Avalanche | ||
39 | Research SLF, Snow Avalanches and Prevention Davos Dorf, CH\", | 39 | Research SLF, Snow Avalanches and Prevention Davos Dorf, CH\", | ||
40 | \"affiliation_02\": \"\", \"affiliation_03\": \"\", \"data_credit\": | 40 | \"affiliation_02\": \"\", \"affiliation_03\": \"\", \"data_credit\": | ||
41 | [\"collection\", \"software\"], \"email\": \"janic.cathomen@slf.ch\", | 41 | [\"collection\", \"software\"], \"email\": \"janic.cathomen@slf.ch\", | ||
42 | \"given_name\": \"Janic\", \"identifier\": \"\", \"name\": | 42 | \"given_name\": \"Janic\", \"identifier\": \"\", \"name\": | ||
43 | \"Cathomen\"}, {\"affiliation\": \"Institute for Mechanical Systems, | 43 | \"Cathomen\"}, {\"affiliation\": \"Institute for Mechanical Systems, | ||
44 | ETH Zurich, Zurich, Switzerland\", \"affiliation_02\": \"ETH | 44 | ETH Zurich, Zurich, Switzerland\", \"affiliation_02\": \"ETH | ||
45 | Z\\u00fcrich\", \"affiliation_03\": \"\", \"data_credit\": | 45 | Z\\u00fcrich\", \"affiliation_03\": \"\", \"data_credit\": | ||
46 | \"supervision\", \"email\": \"dual@imes.mavt.ethz.ch\", | 46 | \"supervision\", \"email\": \"dual@imes.mavt.ethz.ch\", | ||
47 | \"given_name\": \"J\\u00fcrg\", \"identifier\": | 47 | \"given_name\": \"J\\u00fcrg\", \"identifier\": | ||
48 | \"0000-0001-5861-9058\", \"name\": \"Dual\"}, {\"affiliation\": \"WSL | 48 | \"0000-0001-5861-9058\", \"name\": \"Dual\"}, {\"affiliation\": \"WSL | ||
49 | Institute for Snow and Avalanche Research SLF, Snow Avalanches and | 49 | Institute for Snow and Avalanche Research SLF, Snow Avalanches and | ||
50 | Prevention Davos Dorf, CH\", \"affiliation_02\": \"\", | 50 | Prevention Davos Dorf, CH\", \"affiliation_02\": \"\", | ||
51 | \"affiliation_03\": \"\", \"data_credit\": \"supervision\", \"email\": | 51 | \"affiliation_03\": \"\", \"data_credit\": \"supervision\", \"email\": | ||
52 | \"schweizer@slf.ch\", \"given_name\": \"J\\u00fcrg\", \"identifier\": | 52 | \"schweizer@slf.ch\", \"given_name\": \"J\\u00fcrg\", \"identifier\": | ||
53 | \"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]", | 53 | \"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]", | ||
54 | "author_email": null, | 54 | "author_email": null, | ||
55 | "creator_user_id": "c8312541-12f8-4533-a778-53f3d3e6a99b", | 55 | "creator_user_id": "c8312541-12f8-4533-a778-53f3d3e6a99b", | ||
56 | "date": "[{\"date\": \"2021-10-11\", \"date_type\": \"created\", | 56 | "date": "[{\"date\": \"2021-10-11\", \"date_type\": \"created\", | ||
57 | \"end_date\": \"\"}]", | 57 | \"end_date\": \"\"}]", | ||
58 | "doi": "10.16904/envidat.250", | 58 | "doi": "10.16904/envidat.250", | ||
59 | "funding": "[{\"grant_number\": \"200021_169424\", \"institution\": | 59 | "funding": "[{\"grant_number\": \"200021_169424\", \"institution\": | ||
60 | \"Swiss National Science Foundation\", \"institution_url\": \"\"}]", | 60 | \"Swiss National Science Foundation\", \"institution_url\": \"\"}]", | ||
61 | "groups": [], | 61 | "groups": [], | ||
62 | "id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | 62 | "id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | ||
63 | "isopen": false, | 63 | "isopen": false, | ||
64 | "language": "en", | 64 | "language": "en", | ||
65 | "license_id": "wsl-data", | 65 | "license_id": "wsl-data", | ||
66 | "license_title": "WSL Data Policy", | 66 | "license_title": "WSL Data Policy", | ||
67 | "license_url": | 67 | "license_url": | ||
68 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 68 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
69 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | 69 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | ||
70 | Avalanche Research SLF, Davos, Switzerland\", \"email\": | 70 | Avalanche Research SLF, Davos, Switzerland\", \"email\": | ||
71 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | 71 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | ||
72 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}", | 72 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}", | ||
73 | "maintainer_email": null, | 73 | "maintainer_email": null, | ||
74 | "metadata_created": "2021-10-11T10:11:44.154892", | 74 | "metadata_created": "2021-10-11T10:11:44.154892", | ||
n | 75 | "metadata_modified": "2021-10-12T08:35:13.749821", | n | 75 | "metadata_modified": "2021-10-12T08:35:34.893900", |
76 | "name": "crack-propagation-speeds-in-weak-snowpack-layers", | 76 | "name": "crack-propagation-speeds-in-weak-snowpack-layers", | ||
77 | "notes": "For the release of a slab avalanche, crack propagation | 77 | "notes": "For the release of a slab avalanche, crack propagation | ||
78 | within a weak snowpack layer below a cohesive snow slab is required. | 78 | within a weak snowpack layer below a cohesive snow slab is required. | ||
79 | As crack speed measurements can give insight into the underlying | 79 | As crack speed measurements can give insight into the underlying | ||
80 | processes, we analysed three crack propagation events that occurred in | 80 | processes, we analysed three crack propagation events that occurred in | ||
81 | similar snowpacks and covered all scales relevant for avalanche | 81 | similar snowpacks and covered all scales relevant for avalanche | ||
82 | release. For the largest scale, up to 400 m, we estimated crack speed | 82 | release. For the largest scale, up to 400 m, we estimated crack speed | ||
83 | from an avalanche movie, for scales between 5 and 25 meters, we used | 83 | from an avalanche movie, for scales between 5 and 25 meters, we used | ||
84 | accelerometers placed on the snow surface, and for scales below 5 | 84 | accelerometers placed on the snow surface, and for scales below 5 | ||
85 | meters, we performed a Propagation Saw Test. The mean crack speeds | 85 | meters, we performed a Propagation Saw Test. The mean crack speeds | ||
86 | ranged from 36 \u00b1 6 to 49 \u00b1 5 m s^{-1}, and did not exhibit | 86 | ranged from 36 \u00b1 6 to 49 \u00b1 5 m s^{-1}, and did not exhibit | ||
87 | scale dependence. Using the Discrete Element Method and the Material | 87 | scale dependence. Using the Discrete Element Method and the Material | ||
88 | Point Method, we reproduced the measured crack speeds reasonably well, | 88 | Point Method, we reproduced the measured crack speeds reasonably well, | ||
89 | in particular the terminal crack speed observed at smaller | 89 | in particular the terminal crack speed observed at smaller | ||
90 | scales.\r\nThis dataset includes raw data as well as crack speed | 90 | scales.\r\nThis dataset includes raw data as well as crack speed | ||
91 | estimates from the three crack propagation events. \r\nWhere possible, | 91 | estimates from the three crack propagation events. \r\nWhere possible, | ||
92 | we reproduced these field experiments with numerical models based on | 92 | we reproduced these field experiments with numerical models based on | ||
93 | Discrete Element Method (DEM, Bobillier and others, 2020 and 2021) and | 93 | Discrete Element Method (DEM, Bobillier and others, 2020 and 2021) and | ||
94 | Material Point Method (MPM. Gaume and others, 2018 and Trottet and | 94 | Material Point Method (MPM. Gaume and others, 2018 and Trottet and | ||
95 | others, 2021). The input parameters of the models were estimated from | 95 | others, 2021). The input parameters of the models were estimated from | ||
96 | the corresponding snow profiles conducted at each test site.\r\n\r\n## | 96 | the corresponding snow profiles conducted at each test site.\r\n\r\n## | ||
97 | The raw data include:\r\n* Propagation Saw Test movie with mechanical | 97 | The raw data include:\r\n* Propagation Saw Test movie with mechanical | ||
98 | fields derived from Digital image Correlation analysis of the | 98 | fields derived from Digital image Correlation analysis of the | ||
99 | recording\r\n* Acceleration data recorded with wireless time | 99 | recording\r\n* Acceleration data recorded with wireless time | ||
100 | synchronized accelerometers placed on the snow surface during crack | 100 | synchronized accelerometers placed on the snow surface during crack | ||
101 | propagation in a whumpf.\r\n*Video of an artificially triggered | 101 | propagation in a whumpf.\r\n*Video of an artificially triggered | ||
102 | avalanche with widespread crack propagation. The video was used to | 102 | avalanche with widespread crack propagation. The video was used to | ||
103 | georeference surface cracks in order to estimate crack propagation | 103 | georeference surface cracks in order to estimate crack propagation | ||
104 | time and distance, providing crack propagation speed estimates.\r\n* | 104 | time and distance, providing crack propagation speed estimates.\r\n* | ||
105 | Snow profile recorded at each test site\r\n\r\n## Experimental crack | 105 | Snow profile recorded at each test site\r\n\r\n## Experimental crack | ||
106 | speed estimates include:\r\n* Crack speed evolution within the first | 106 | speed estimates include:\r\n* Crack speed evolution within the first | ||
107 | meters derived from the Propagation Saw Test.\r\n* Crack speeds | 107 | meters derived from the Propagation Saw Test.\r\n* Crack speeds | ||
108 | estimated from the time delay of the collapse, observed between | 108 | estimated from the time delay of the collapse, observed between | ||
109 | different accelerometers during crack propagation of a whumpf.\r\n* | 109 | different accelerometers during crack propagation of a whumpf.\r\n* | ||
110 | Crack speed estimates from video analysis of the artificially | 110 | Crack speed estimates from video analysis of the artificially | ||
111 | triggered avalanche.\r\n\r\n## Reproduced crack speeds using the DEM | 111 | triggered avalanche.\r\n\r\n## Reproduced crack speeds using the DEM | ||
112 | an MPM model:\r\n* Modelled Propagation Saw Test using MPM (2D and 3D | 112 | an MPM model:\r\n* Modelled Propagation Saw Test using MPM (2D and 3D | ||
113 | system) and DEM.\r\n* Modelled whumpf using MPM (beam and areal | 113 | system) and DEM.\r\n* Modelled whumpf using MPM (beam and areal | ||
114 | configuration)\r\n* Modelled avalanche using MPM (beam and areal | 114 | configuration)\r\n* Modelled avalanche using MPM (beam and areal | ||
115 | configuration)\r\n\r\nBeside the movies (mp4 format), all data is | 115 | configuration)\r\n\r\nBeside the movies (mp4 format), all data is | ||
116 | either provided as netCDF files or excel sheets (see readme file), | 116 | either provided as netCDF files or excel sheets (see readme file), | ||
117 | depending on the amount of data. A detailed description of the three | 117 | depending on the amount of data. A detailed description of the three | ||
118 | crack propagation events and how crack speed was derived, can be found | 118 | crack propagation events and how crack speed was derived, can be found | ||
119 | in the related publication:\r\n\r\n\r\n\r\n### References for applied | 119 | in the related publication:\r\n\r\n\r\n\r\n### References for applied | ||
120 | models: \r\nBobillier, G., B. Bergfeld, A. Capelli, J. Dual, J. Gaume, | 120 | models: \r\nBobillier, G., B. Bergfeld, A. Capelli, J. Dual, J. Gaume, | ||
121 | A. van Herwijnen and J. Schweizer 2020. Micromechanical modeling of | 121 | A. van Herwijnen and J. Schweizer 2020. Micromechanical modeling of | ||
122 | snow failure. The Cryosphere, 14(1): 39-49.\r\n\r\nBobillier, G., B. | 122 | snow failure. The Cryosphere, 14(1): 39-49.\r\n\r\nBobillier, G., B. | ||
123 | Bergfeld, J. Dual, J. Gaume, A. van Herwijnen and J. Schweizer 2021. | 123 | Bergfeld, J. Dual, J. Gaume, A. van Herwijnen and J. Schweizer 2021. | ||
124 | Micro-mechanical insights into the dynamics of crack propagation in | 124 | Micro-mechanical insights into the dynamics of crack propagation in | ||
125 | snow fracture experiments. Scientific Reports, 11: | 125 | snow fracture experiments. Scientific Reports, 11: | ||
126 | 11711.\r\n\r\nGaume, J., T. Gast, J. Teran, A. van Herwijnen and C. | 126 | 11711.\r\n\r\nGaume, J., T. Gast, J. Teran, A. van Herwijnen and C. | ||
127 | Jiang 2018. Dynamic anticrack propagation in snow. Nature | 127 | Jiang 2018. Dynamic anticrack propagation in snow. Nature | ||
128 | Communications, 9(1): 3047.\r\n\r\nTrottet, B., R. Simenhois, G. | 128 | Communications, 9(1): 3047.\r\n\r\nTrottet, B., R. Simenhois, G. | ||
129 | Bobillier, A. van Herwijnen, C. Jiang and J. Gaume 2021. From | 129 | Bobillier, A. van Herwijnen, C. Jiang and J. Gaume 2021. From | ||
130 | sub-Rayleigh to intersonic crack propagation in snow slab avalanche | 130 | sub-Rayleigh to intersonic crack propagation in snow slab avalanche | ||
131 | release. EGU General Assembly 2021, Online, 19-30 Apr 2021, | 131 | release. EGU General Assembly 2021, Online, 19-30 Apr 2021, | ||
132 | EGU21-8253.\r\n", | 132 | EGU21-8253.\r\n", | ||
133 | "num_resources": 2, | 133 | "num_resources": 2, | ||
134 | "num_tags": 7, | 134 | "num_tags": 7, | ||
135 | "organization": { | 135 | "organization": { | ||
136 | "approval_status": "approved", | 136 | "approval_status": "approved", | ||
137 | "created": "2019-09-27T12:40:13.473824", | 137 | "created": "2019-09-27T12:40:13.473824", | ||
138 | "description": "Snow avalanches \u2013 a type of fast-moving mass | 138 | "description": "Snow avalanches \u2013 a type of fast-moving mass | ||
139 | movement \u2013 occur in snow covered mountain areas throughout the | 139 | movement \u2013 occur in snow covered mountain areas throughout the | ||
140 | world and may cause property damage and loss of life as they interfere | 140 | world and may cause property damage and loss of life as they interfere | ||
141 | with human activities. Most avalanches release from terrain steeper | 141 | with human activities. Most avalanches release from terrain steeper | ||
142 | than about 30\u00b0 during or soon after snow storms, or are triggered | 142 | than about 30\u00b0 during or soon after snow storms, or are triggered | ||
143 | by snow loading due to wind, or by a temperature change. Snow slab | 143 | by snow loading due to wind, or by a temperature change. Snow slab | ||
144 | avalanches can also be triggered artificially by, for example, people | 144 | avalanches can also be triggered artificially by, for example, people | ||
145 | (usually unintentionally) or intentionally by explosives used as part | 145 | (usually unintentionally) or intentionally by explosives used as part | ||
146 | of avalanche control programs. Today, most avalanche fatalities are | 146 | of avalanche control programs. Today, most avalanche fatalities are | ||
147 | recreationists. Independent of the triggering mode, the snowpack | 147 | recreationists. Independent of the triggering mode, the snowpack | ||
148 | layering is decisive for the instability of the snowpack which | 148 | layering is decisive for the instability of the snowpack which | ||
149 | consists of layers with varying properties. The complex microstructure | 149 | consists of layers with varying properties. The complex microstructure | ||
150 | of snow and spatial variations in snow layer properties across the | 150 | of snow and spatial variations in snow layer properties across the | ||
151 | terrain limit the predictability of snow avalanches. Even today, it is | 151 | terrain limit the predictability of snow avalanches. Even today, it is | ||
152 | not possible to predict the exact location, time and extent of an | 152 | not possible to predict the exact location, time and extent of an | ||
153 | avalanche event. Improving avalanche prediction requires a better | 153 | avalanche event. Improving avalanche prediction requires a better | ||
154 | understanding of the underlying processes. ", | 154 | understanding of the underlying processes. ", | ||
155 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 155 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
156 | "image_url": "2019-09-27-104013.456832slf.png", | 156 | "image_url": "2019-09-27-104013.456832slf.png", | ||
157 | "is_organization": true, | 157 | "is_organization": true, | ||
158 | "name": "avalanche-formation", | 158 | "name": "avalanche-formation", | ||
159 | "state": "active", | 159 | "state": "active", | ||
160 | "title": "Avalanche Formation", | 160 | "title": "Avalanche Formation", | ||
161 | "type": "organization" | 161 | "type": "organization" | ||
162 | }, | 162 | }, | ||
163 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 163 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
164 | "private": false, | 164 | "private": false, | ||
165 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | 165 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | ||
166 | \"EnviDat\"}", | 166 | \"EnviDat\"}", | ||
t | 167 | "publication_state": "reserved", | t | 167 | "publication_state": "approved", |
168 | "related_datasets": "", | 168 | "related_datasets": "", | ||
169 | "related_publications": "DOI will be added after publication!", | 169 | "related_publications": "DOI will be added after publication!", | ||
170 | "relationships_as_object": [], | 170 | "relationships_as_object": [], | ||
171 | "relationships_as_subject": [], | 171 | "relationships_as_subject": [], | ||
172 | "resource_type": "datapaper", | 172 | "resource_type": "datapaper", | ||
173 | "resource_type_general": "datapaper", | 173 | "resource_type_general": "datapaper", | ||
174 | "resources": [ | 174 | "resources": [ | ||
175 | { | 175 | { | ||
176 | "cache_last_updated": null, | 176 | "cache_last_updated": null, | ||
177 | "cache_url": null, | 177 | "cache_url": null, | ||
178 | "created": "2021-10-11T12:38:43.593437", | 178 | "created": "2021-10-11T12:38:43.593437", | ||
179 | "description": "Please find the readme file.\r\n", | 179 | "description": "Please find the readme file.\r\n", | ||
180 | "doi": "", | 180 | "doi": "", | ||
181 | "format": "ZIP", | 181 | "format": "ZIP", | ||
182 | "hash": "", | 182 | "hash": "", | ||
183 | "id": "cbe26adb-d263-488d-beb3-e98eabd6c95d", | 183 | "id": "cbe26adb-d263-488d-beb3-e98eabd6c95d", | ||
184 | "last_modified": null, | 184 | "last_modified": null, | ||
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186 | "mimetype": null, | 186 | "mimetype": null, | ||
187 | "mimetype_inner": null, | 187 | "mimetype_inner": null, | ||
188 | "name": "crack propagation speeds", | 188 | "name": "crack propagation speeds", | ||
189 | "package_id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | 189 | "package_id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | ||
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197 | "size": 200147125, | 197 | "size": 200147125, | ||
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