Changes
On October 12, 2021 at 7:00:37 AM UTC, Bastian Bergfeld:
-
Updated description of Crack propagation speeds in weak snowpack layers from three events: PST, whumpf and slab avalanche. from
__ENVIDAT__: this dataset is not accepted for publication in its current form because it doesn't fulfil the necessary quality guidelines: https://www.envidat.ch/#/about/guidelines (It is not enough to point to a related article that is submitted. Please expand the description so anyone reading it can find answers to __what are the research data about__ and a brief summary of the methods. Please delete these comments and replace it with your own description. (EnviDat Admin) ---------------------------- This dataset includes raw data and resulting crack speed measures as described in the related research article: DOI has been reserved.
toFor the release of a slab avalanche, crack propagation within a weak snowpack layer below a cohesive snow slab is required. As crack speed measurements can give insight into the underlying processes, we analysed three crack propagation events that occurred in similar snowpacks and covered all scales relevant for avalanche release. For the largest scale, up to 400 m, we estimated crack speed from an avalanche movie, for scales between 5 and 25 meters, we used accelerometers placed on the snow surface, and for scales below 5 meters, we performed a Propagation Saw Test. The mean crack speeds ranged from 36 ± 6 to 49 ± 5 m s 1, and did not exhibit scale dependence. Using the Discrete Element Method and the Material Point Method, we reproduced the measured crack speeds reasonably well, in particular the terminal crack speed observed at smaller scales. This dataset includes raw data as well as crack speed estimates from the three crack propagation events. Where possible, we reproduced these field experiments with numerical models based on Discrete Element Method (Bobillier and others, 2020 and 2021) and Material Point Method (Gaume and others, 2018 and Trottet and others, 2021). The input parameters of the models were estimated from the corresponding snow profiles conducted at each test site. <b>The raw data include:</b> - Propagation Saw Test movie with mechanical fields derived from Digital image Correlation analysis of the recording - Acceleration data recorded with wireless time synchronized accelerometers placed on the snow surface during crack propagation in a whumpf. - Video of an artificially triggered avalanche with widespread crack propagation. The video was used to georeference surface cracks in order to estimate crack propagation time and distance, providing crack propagation speed estimates. - Snow profile recorded at each test site <b>Resulting experimental crack speed estimates include:</b> - Crack speed evolution within the first meters derived from the Propagation Saw Test. - Crack speeds estimated from the time delay of the collapse, observed between different accelerometers during crack propagation of a whumpf. - Crack speed estimates from video analysis of the artificially triggered avalanche. <b>Reproduced crack speeds using the DEM an MPM model:</b> - Modelled Propagation Saw Test using MPM (2D and 3D system) and DEM. - Modelled whumpf using MPM (beam and areal configuration) - Modelled avalanche using MPM (beam and areal configuration) Beside the movies (mp4 format), all data is either provided as netCDF files or excel sheets (see readme file), depending on the amount of data. A detailed description of the three crack propagation events and how crack speed was derived, can be found in the related publication: ... To be added ... References: Bobillier, G., B. Bergfeld, A. Capelli, J. Dual, J. Gaume, A. van Herwijnen and J. Schweizer 2020. Micromechanical modeling of snow failure. The Cryosphere, 14(1): 39-49. Bobillier, G., B. Bergfeld, J. Dual, J. Gaume, A. van Herwijnen and J. Schweizer 2021. Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments. Scientific Reports, 11: 11711. Gaume, J., T. Gast, J. Teran, A. van Herwijnen and C. Jiang 2018. Dynamic anticrack propagation in snow. Nature Communications, 9(1): 3047. Trottet, B., R. Simenhois, G. Bobillier, A. van Herwijnen, C. Jiang and J. Gaume 2021. From sub-Rayleigh to intersonic crack propagation in snow slab avalanche release. EGU General Assembly 2021, Online, 19-30 Apr 2021, EGU21-8253.
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": "2021-10-11T14:14:09.763720", | n | 75 | "metadata_modified": "2021-10-12T07:00:37.461209", |
76 | "name": "crack-propagation-speeds-in-weak-snowpack-layers", | 76 | "name": "crack-propagation-speeds-in-weak-snowpack-layers", | ||
t | 77 | "notes": "__ENVIDAT__: this dataset is not accepted for publication | t | 77 | "notes": "For the release of a slab avalanche, crack propagation |
78 | in its current form because it doesn't fulfil the necessary quality | 78 | within a weak snowpack layer below a cohesive snow slab is required. | ||
79 | guidelines: https://www.envidat.ch/#/about/guidelines\r\n(It is not | 79 | As crack speed measurements can give insight into the underlying | ||
80 | enough to point to a related article that is submitted. Please expand | 80 | processes, we analysed three crack propagation events that occurred in | ||
81 | the description so anyone reading it can find answers to __what are | 81 | similar snowpacks and covered all scales relevant for avalanche | ||
82 | the research data about__ and a brief summary of the methods. | 82 | release. For the largest scale, up to 400 m, we estimated crack speed | ||
83 | \r\nPlease delete these comments and replace it with your own | 83 | from an avalanche movie, for scales between 5 and 25 meters, we used | ||
84 | description. (EnviDat | 84 | accelerometers placed on the snow surface, and for scales below 5 | ||
85 | Admin)\r\n----------------------------\r\n\r\nThis dataset includes | 85 | meters, we performed a Propagation Saw Test. The mean crack speeds | ||
86 | raw data and resulting crack speed measures as described in the | 86 | ranged from 36 \u00b1 6 to 49 \u00b1 5 m s 1, and did not exhibit | ||
87 | related research article:\r\n\r\nDOI has been reserved.\r\n\r\n\r\n", | 87 | scale dependence. Using the Discrete Element Method and the Material | ||
88 | Point Method, we reproduced the measured crack speeds reasonably well, | ||||
89 | in particular the terminal crack speed observed at smaller | ||||
90 | scales.\r\nThis dataset includes raw data as well as crack speed | ||||
91 | estimates from the three crack propagation events. \r\nWhere possible, | ||||
92 | we reproduced these field experiments with numerical models based on | ||||
93 | Discrete Element Method (Bobillier and others, 2020 and 2021) and | ||||
94 | Material Point Method (Gaume and others, 2018 and Trottet and others, | ||||
95 | 2021). The input parameters of the models were estimated from the | ||||
96 | corresponding snow profiles conducted at each test site.\r\n\r\n<b>The | ||||
97 | raw data include:</b>\r\n- Propagation Saw Test movie with mechanical | ||||
98 | fields derived from Digital image Correlation analysis of the | ||||
99 | recording\r\n- Acceleration data recorded with wireless time | ||||
100 | synchronized accelerometers placed on the snow surface during crack | ||||
101 | propagation in a whumpf.\r\n- Video of an artificially triggered | ||||
102 | avalanche with widespread crack propagation. The video was used to | ||||
103 | georeference surface cracks in order to estimate crack propagation | ||||
104 | time and distance, providing crack propagation speed estimates.\r\n- | ||||
105 | Snow profile recorded at each test site\r\n\r\n<b>Resulting | ||||
106 | experimental crack speed estimates include:</b>\r\n- Crack speed | ||||
107 | evolution within the first meters derived from the Propagation Saw | ||||
108 | Test.\r\n- Crack speeds estimated from the time delay of the collapse, | ||||
109 | observed between different accelerometers during crack propagation of | ||||
110 | a whumpf.\r\n- Crack speed estimates from video analysis of the | ||||
111 | artificially triggered avalanche.\r\n\r\n<b>Reproduced crack speeds | ||||
112 | using the DEM an MPM model:</b>\r\n- Modelled Propagation Saw Test | ||||
113 | using MPM (2D and 3D system) and DEM.\r\n- Modelled whumpf using MPM | ||||
114 | (beam and areal configuration)\r\n- Modelled avalanche using MPM (beam | ||||
115 | and areal configuration)\r\n\r\nBeside the movies (mp4 format), all | ||||
116 | data is either provided as netCDF files or excel sheets (see readme | ||||
117 | file), depending on the amount of data. A detailed description of the | ||||
118 | three crack propagation events and how crack speed was derived, can be | ||||
119 | found in the related publication:\r\n\r\n... To be added | ||||
120 | ...\r\n\r\n\r\n\r\n\r\nReferences:\r\nBobillier, G., B. Bergfeld, A. | ||||
121 | Capelli, J. Dual, J. Gaume, A. van Herwijnen and J. Schweizer 2020. | ||||
122 | Micromechanical modeling of snow failure. The Cryosphere, 14(1): | ||||
123 | 39-49.\r\nBobillier, G., B. Bergfeld, J. Dual, J. Gaume, A. van | ||||
124 | Herwijnen and J. Schweizer 2021. Micro-mechanical insights into the | ||||
125 | dynamics of crack propagation in snow fracture experiments. Scientific | ||||
126 | Reports, 11: 11711.\r\nGaume, J., T. Gast, J. Teran, A. van Herwijnen | ||||
127 | and C. Jiang 2018. Dynamic anticrack propagation in snow. Nature | ||||
128 | Communications, 9(1): 3047.\r\nTrottet, B., R. Simenhois, G. | ||||
129 | Bobillier, A. van Herwijnen, C. Jiang and J. Gaume 2021. From | ||||
130 | sub-Rayleigh to intersonic crack propagation in snow slab avalanche | ||||
131 | release. EGU General Assembly 2021, Online, 19-30 Apr 2021, | ||||
132 | EGU21-8253.\r\n", | ||||
88 | "num_resources": 2, | 133 | "num_resources": 2, | ||
89 | "num_tags": 7, | 134 | "num_tags": 7, | ||
90 | "organization": { | 135 | "organization": { | ||
91 | "approval_status": "approved", | 136 | "approval_status": "approved", | ||
92 | "created": "2019-09-27T12:40:13.473824", | 137 | "created": "2019-09-27T12:40:13.473824", | ||
93 | "description": "Snow avalanches \u2013 a type of fast-moving mass | 138 | "description": "Snow avalanches \u2013 a type of fast-moving mass | ||
94 | movement \u2013 occur in snow covered mountain areas throughout the | 139 | movement \u2013 occur in snow covered mountain areas throughout the | ||
95 | 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 | ||
96 | with human activities. Most avalanches release from terrain steeper | 141 | with human activities. Most avalanches release from terrain steeper | ||
97 | 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 | ||
98 | 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 | ||
99 | avalanches can also be triggered artificially by, for example, people | 144 | avalanches can also be triggered artificially by, for example, people | ||
100 | (usually unintentionally) or intentionally by explosives used as part | 145 | (usually unintentionally) or intentionally by explosives used as part | ||
101 | of avalanche control programs. Today, most avalanche fatalities are | 146 | of avalanche control programs. Today, most avalanche fatalities are | ||
102 | recreationists. Independent of the triggering mode, the snowpack | 147 | recreationists. Independent of the triggering mode, the snowpack | ||
103 | layering is decisive for the instability of the snowpack which | 148 | layering is decisive for the instability of the snowpack which | ||
104 | consists of layers with varying properties. The complex microstructure | 149 | consists of layers with varying properties. The complex microstructure | ||
105 | of snow and spatial variations in snow layer properties across the | 150 | of snow and spatial variations in snow layer properties across the | ||
106 | terrain limit the predictability of snow avalanches. Even today, it is | 151 | terrain limit the predictability of snow avalanches. Even today, it is | ||
107 | 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 | ||
108 | avalanche event. Improving avalanche prediction requires a better | 153 | avalanche event. Improving avalanche prediction requires a better | ||
109 | understanding of the underlying processes. ", | 154 | understanding of the underlying processes. ", | ||
110 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 155 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
111 | "image_url": "2019-09-27-104013.456832slf.png", | 156 | "image_url": "2019-09-27-104013.456832slf.png", | ||
112 | "is_organization": true, | 157 | "is_organization": true, | ||
113 | "name": "avalanche-formation", | 158 | "name": "avalanche-formation", | ||
114 | "state": "active", | 159 | "state": "active", | ||
115 | "title": "Avalanche Formation", | 160 | "title": "Avalanche Formation", | ||
116 | "type": "organization" | 161 | "type": "organization" | ||
117 | }, | 162 | }, | ||
118 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 163 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
119 | "private": false, | 164 | "private": false, | ||
120 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | 165 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | ||
121 | \"EnviDat\"}", | 166 | \"EnviDat\"}", | ||
122 | "publication_state": "reserved", | 167 | "publication_state": "reserved", | ||
123 | "related_datasets": "", | 168 | "related_datasets": "", | ||
124 | "related_publications": "DOI will be added after publication!", | 169 | "related_publications": "DOI will be added after publication!", | ||
125 | "relationships_as_object": [], | 170 | "relationships_as_object": [], | ||
126 | "relationships_as_subject": [], | 171 | "relationships_as_subject": [], | ||
127 | "resource_type": "datapaper", | 172 | "resource_type": "datapaper", | ||
128 | "resource_type_general": "datapaper", | 173 | "resource_type_general": "datapaper", | ||
129 | "resources": [ | 174 | "resources": [ | ||
130 | { | 175 | { | ||
131 | "cache_last_updated": null, | 176 | "cache_last_updated": null, | ||
132 | "cache_url": null, | 177 | "cache_url": null, | ||
133 | "created": "2021-10-11T12:38:43.593437", | 178 | "created": "2021-10-11T12:38:43.593437", | ||
134 | "description": "Please find the readme file.\r\n", | 179 | "description": "Please find the readme file.\r\n", | ||
135 | "doi": "", | 180 | "doi": "", | ||
136 | "format": "ZIP", | 181 | "format": "ZIP", | ||
137 | "hash": "", | 182 | "hash": "", | ||
138 | "id": "cbe26adb-d263-488d-beb3-e98eabd6c95d", | 183 | "id": "cbe26adb-d263-488d-beb3-e98eabd6c95d", | ||
139 | "last_modified": null, | 184 | "last_modified": null, | ||
140 | "metadata_modified": "2021-10-11T12:42:02.341972", | 185 | "metadata_modified": "2021-10-11T12:42:02.341972", | ||
141 | "mimetype": null, | 186 | "mimetype": null, | ||
142 | "mimetype_inner": null, | 187 | "mimetype_inner": null, | ||
143 | "name": "crack propagation speeds", | 188 | "name": "crack propagation speeds", | ||
144 | "package_id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | 189 | "package_id": "ad08d108-113f-4236-b141-a16edc3e4e1c", | ||
145 | "position": 0, | 190 | "position": 0, | ||
146 | "publication_state": "", | 191 | "publication_state": "", | ||
147 | "resource_size": "{\"size_units\": \"mb\", \"size_value\": | 192 | "resource_size": "{\"size_units\": \"mb\", \"size_value\": | ||
148 | \"195\"}", | 193 | \"195\"}", | ||
149 | "resource_type": null, | 194 | "resource_type": null, | ||
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