Changes
On June 23, 2021 at 3:40:43 PM UTC, Bastian Bergfeld:
-
Updated description of Crack propagation in weak snowpack layers: Insights from high-speed photography from
This data set includes material and results described in the related research article (Bergfeld et al. (2021)). # Context: In order to study the crack propagation in weak snow pack layers in great detail, we recorded Propagation Saw Test (PST) experiments using a high-speed camera and applied digital image correlation (DIC) to derive displacement and strain fields in the slab, weak layer, and substrate. We demonstrated the versatility and accuracy of the DIC method by showing measurements from three PST experiments, resulting in slab fracture, crack arrest and full propagation in the related publication. # Content: - Supplementary material for related publication - Ilustrative videos showing crack propagation - High-speed recordings of the Experiments (the raw .cine files are available upon request)
toThis data set includes material and results described in the related research article (Bergfeld et al. (2021)). # Context: In order to study crack propagation in weak snow pack layers in great detail, we recorded Propagation Saw Test (PST) experiments using a high-speed camera and applied digital image correlation (DIC) to derive displacement and strain fields in the slab, weak layer, and substrate. We demonstrated the versatility and accuracy of the DIC method by showing measurements from three PST experiments, resulting in slab fracture, crack arrest and full propagation in the related publication. # Content: - Supplementary material for related publication - Ilustrative videos showing crack propagation - High-speed recordings of the Experiments (the raw .cine files are available upon request)
f | 1 | { | f | 1 | { |
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5 | \"validation\", \"curation\", \"software\", \"publication\"], | 5 | \"validation\", \"curation\", \"software\", \"publication\"], | ||
6 | \"email\": \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | 6 | \"email\": \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | ||
7 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, | 7 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, | ||
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9 | Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": | 9 | Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": | ||
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11 | \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", \"identifier\": | 11 | \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", \"identifier\": | ||
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14 | Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": | 14 | Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": | ||
15 | \"\", \"data_credit\": \"software\", \"email\": | 15 | \"\", \"data_credit\": \"software\", \"email\": | ||
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34 | "date": "[{\"date\": \"2021-06-23\", \"date_type\": \"collected\", | 34 | "date": "[{\"date\": \"2021-06-23\", \"date_type\": \"collected\", | ||
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44 | "license_title": "WSL Data Policy", | 44 | "license_title": "WSL Data Policy", | ||
45 | "license_url": | 45 | "license_url": | ||
46 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 46 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
47 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | 47 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | ||
48 | Avalanche Research SLF, Davos, Switzerland\", \"email\": | 48 | Avalanche Research SLF, Davos, Switzerland\", \"email\": | ||
49 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | 49 | \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", | ||
50 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}", | 50 | \"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}", | ||
51 | "maintainer_email": null, | 51 | "maintainer_email": null, | ||
52 | "metadata_created": "2021-06-23T14:00:28.699523", | 52 | "metadata_created": "2021-06-23T14:00:28.699523", | ||
n | 53 | "metadata_modified": "2021-06-23T15:38:51.575380", | n | 53 | "metadata_modified": "2021-06-23T15:40:42.954234", |
54 | "name": | 54 | "name": | ||
55 | agation-in-weak-snowpack-layers-insights-from-high-speed-photography", | 55 | agation-in-weak-snowpack-layers-insights-from-high-speed-photography", | ||
56 | "notes": "This data set includes material and results described in | 56 | "notes": "This data set includes material and results described in | ||
57 | the related research article (Bergfeld et al. (2021)). \r\n# Context: | 57 | the related research article (Bergfeld et al. (2021)). \r\n# Context: | ||
t | 58 | \r\nIn order to study the crack propagation in weak snow pack layers | t | 58 | \r\nIn order to study crack propagation in weak snow pack layers in |
59 | in great detail, we recorded Propagation Saw Test (PST) experiments | 59 | great detail, we recorded Propagation Saw Test (PST) experiments using | ||
60 | using a high-speed camera and applied digital image correlation (DIC) | 60 | a high-speed camera and applied digital image correlation (DIC) to | ||
61 | to derive displacement and strain fields in the slab, weak layer, and | 61 | derive displacement and strain fields in the slab, weak layer, and | ||
62 | substrate. We demonstrated the versatility and accuracy of the DIC | 62 | substrate. We demonstrated the versatility and accuracy of the DIC | ||
63 | method by showing measurements from three PST experiments, resulting | 63 | method by showing measurements from three PST experiments, resulting | ||
64 | in slab fracture, crack arrest and full propagation in the related | 64 | in slab fracture, crack arrest and full propagation in the related | ||
65 | publication. \r\n# Content:\r\n- Supplementary material for related | 65 | publication. \r\n# Content:\r\n- Supplementary material for related | ||
66 | publication\r\n- Ilustrative videos showing crack propagation\r\n- | 66 | publication\r\n- Ilustrative videos showing crack propagation\r\n- | ||
67 | High-speed recordings of the Experiments \r\n(the raw .cine files are | 67 | High-speed recordings of the Experiments \r\n(the raw .cine files are | ||
68 | available upon request)\r\n", | 68 | available upon request)\r\n", | ||
69 | "num_resources": 3, | 69 | "num_resources": 3, | ||
70 | "num_tags": 5, | 70 | "num_tags": 5, | ||
71 | "organization": { | 71 | "organization": { | ||
72 | "approval_status": "approved", | 72 | "approval_status": "approved", | ||
73 | "created": "2019-09-27T12:40:13.473824", | 73 | "created": "2019-09-27T12:40:13.473824", | ||
74 | "description": "Snow avalanches \u2013 a type of fast-moving mass | 74 | "description": "Snow avalanches \u2013 a type of fast-moving mass | ||
75 | movement \u2013 occur in snow covered mountain areas throughout the | 75 | movement \u2013 occur in snow covered mountain areas throughout the | ||
76 | world and may cause property damage and loss of life as they interfere | 76 | world and may cause property damage and loss of life as they interfere | ||
77 | with human activities. Most avalanches release from terrain steeper | 77 | with human activities. Most avalanches release from terrain steeper | ||
78 | than about 30\u00b0 during or soon after snow storms, or are triggered | 78 | than about 30\u00b0 during or soon after snow storms, or are triggered | ||
79 | by snow loading due to wind, or by a temperature change. Snow slab | 79 | by snow loading due to wind, or by a temperature change. Snow slab | ||
80 | avalanches can also be triggered artificially by, for example, people | 80 | avalanches can also be triggered artificially by, for example, people | ||
81 | (usually unintentionally) or intentionally by explosives used as part | 81 | (usually unintentionally) or intentionally by explosives used as part | ||
82 | of avalanche control programs. Today, most avalanche fatalities are | 82 | of avalanche control programs. Today, most avalanche fatalities are | ||
83 | recreationists. Independent of the triggering mode, the snowpack | 83 | recreationists. Independent of the triggering mode, the snowpack | ||
84 | layering is decisive for the instability of the snowpack which | 84 | layering is decisive for the instability of the snowpack which | ||
85 | consists of layers with varying properties. The complex microstructure | 85 | consists of layers with varying properties. The complex microstructure | ||
86 | of snow and spatial variations in snow layer properties across the | 86 | of snow and spatial variations in snow layer properties across the | ||
87 | terrain limit the predictability of snow avalanches. Even today, it is | 87 | terrain limit the predictability of snow avalanches. Even today, it is | ||
88 | not possible to predict the exact location, time and extent of an | 88 | not possible to predict the exact location, time and extent of an | ||
89 | avalanche event. Improving avalanche prediction requires a better | 89 | avalanche event. Improving avalanche prediction requires a better | ||
90 | understanding of the underlying processes. ", | 90 | understanding of the underlying processes. ", | ||
91 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 91 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
92 | "image_url": "2019-09-27-104013.456832slf.png", | 92 | "image_url": "2019-09-27-104013.456832slf.png", | ||
93 | "is_organization": true, | 93 | "is_organization": true, | ||
94 | "name": "avalanche-formation", | 94 | "name": "avalanche-formation", | ||
95 | "state": "active", | 95 | "state": "active", | ||
96 | "title": "Avalanche Formation", | 96 | "title": "Avalanche Formation", | ||
97 | "type": "organization" | 97 | "type": "organization" | ||
98 | }, | 98 | }, | ||
99 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 99 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
100 | "private": false, | 100 | "private": false, | ||
101 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | 101 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | ||
102 | \"EnviDat\"}", | 102 | \"EnviDat\"}", | ||
103 | "publication_state": "", | 103 | "publication_state": "", | ||
104 | "related_datasets": "", | 104 | "related_datasets": "", | ||
105 | "related_publications": "https://doi.org/10.5194/tc-2020-360", | 105 | "related_publications": "https://doi.org/10.5194/tc-2020-360", | ||
106 | "relationships_as_object": [], | 106 | "relationships_as_object": [], | ||
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109 | "resource_type_general": "datapaper", | 109 | "resource_type_general": "datapaper", | ||
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114 | "created": "2021-06-23T14:40:09.975436", | 114 | "created": "2021-06-23T14:40:09.975436", | ||
115 | "description": "The videos show the cracking process in three | 115 | "description": "The videos show the cracking process in three | ||
116 | example Propagation Saw Tests (flat field). The upper panel shows | 116 | example Propagation Saw Tests (flat field). The upper panel shows | ||
117 | strain on top of the recorded movie frames. The second row shows | 117 | strain on top of the recorded movie frames. The second row shows | ||
118 | vertical (*w*, blue line) and horizontal (*u*, orange line) | 118 | vertical (*w*, blue line) and horizontal (*u*, orange line) | ||
119 | displacement fields. The third and fourth row show the first and | 119 | displacement fields. The third and fourth row show the first and | ||
120 | second time derivatives, namely the velocity and acceleration field. | 120 | second time derivatives, namely the velocity and acceleration field. | ||
121 | ", | 121 | ", | ||
122 | "doi": "", | 122 | "doi": "", | ||
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176 | "description": "# Supplementary material to the publication | 176 | "description": "# Supplementary material to the publication | ||
177 | Bergfeld et al 2021\r\n- description of the reverse crack\r\n- | 177 | Bergfeld et al 2021\r\n- description of the reverse crack\r\n- | ||
178 | additional snow pack parameters derived from the SMP measurements", | 178 | additional snow pack parameters derived from the SMP measurements", | ||
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204 | "spatial_info": "Switzerland", | 204 | "spatial_info": "Switzerland", | ||
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207 | "tags": [ | 207 | "tags": [ | ||
208 | { | 208 | { | ||
209 | "display_name": "CRACK PROPAGATION", | 209 | "display_name": "CRACK PROPAGATION", | ||
210 | "id": "cca7ca78-fafe-4329-af76-45610a10396b", | 210 | "id": "cca7ca78-fafe-4329-af76-45610a10396b", | ||
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222 | { | 222 | { | ||
223 | "display_name": "SNOW", | 223 | "display_name": "SNOW", | ||
224 | "id": "c4e9ea3f-6149-45ce-8631-c872b96a9537", | 224 | "id": "c4e9ea3f-6149-45ce-8631-c872b96a9537", | ||
225 | "name": "SNOW", | 225 | "name": "SNOW", | ||
226 | "state": "active", | 226 | "state": "active", | ||
227 | "vocabulary_id": null | 227 | "vocabulary_id": null | ||
228 | }, | 228 | }, | ||
229 | { | 229 | { | ||
230 | "display_name": "SNOW AVALANCHE", | 230 | "display_name": "SNOW AVALANCHE", | ||
231 | "id": "6083a08c-fd24-4e5a-bb20-559021b89c92", | 231 | "id": "6083a08c-fd24-4e5a-bb20-559021b89c92", | ||
232 | "name": "SNOW AVALANCHE", | 232 | "name": "SNOW AVALANCHE", | ||
233 | "state": "active", | 233 | "state": "active", | ||
234 | "vocabulary_id": null | 234 | "vocabulary_id": null | ||
235 | }, | 235 | }, | ||
236 | { | 236 | { | ||
237 | "display_name": "SNOW MECHANICS", | 237 | "display_name": "SNOW MECHANICS", | ||
238 | "id": "31bab9c5-b32e-452d-bce1-f7500696beab", | 238 | "id": "31bab9c5-b32e-452d-bce1-f7500696beab", | ||
239 | "name": "SNOW MECHANICS", | 239 | "name": "SNOW MECHANICS", | ||
240 | "state": "active", | 240 | "state": "active", | ||
241 | "vocabulary_id": null | 241 | "vocabulary_id": null | ||
242 | } | 242 | } | ||
243 | ], | 243 | ], | ||
244 | "title": "Crack propagation in weak snowpack layers: Insights from | 244 | "title": "Crack propagation in weak snowpack layers: Insights from | ||
245 | high-speed photography", | 245 | high-speed photography", | ||
246 | "type": "dataset", | 246 | "type": "dataset", | ||
247 | "url": null, | 247 | "url": null, | ||
248 | "version": "1.0" | 248 | "version": "1.0" | ||
249 | } | 249 | } |