Changes
On January 27, 2023 at 8:41:40 AM UTC, Jürg Schweizer:
-
Changed value of field
related_publications
toBergfeld, B., van Herwijnen, A., Bobillier, G., Rosendahl, P. L., Weißgraeber, P., Adam, V., Dual, J., and Schweizer, J.: Temporal evolution of crack propagation characteristics in a weak snowpack layer: conditions of crack arrest and sustained propagation, Nat. Hazards Earth Syst. Sci., 23, 293-315, https://doi.org/10.5194/nhess-23-293-2023, 2023.
in Time series data on dynamic crack propagation in long propagation saw tests
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\", \"affiliation_02\": \"\", \"affiliation_03\": \"\", | 3 | Research SLF\", \"affiliation_02\": \"\", \"affiliation_03\": \"\", | ||
4 | \"data_credit\": [\"collection\", \"validation\", \"curation\", | 4 | \"data_credit\": [\"collection\", \"validation\", \"curation\", | ||
5 | \"software\", \"publication\"], \"email\": | 5 | \"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 | 8 | {\"affiliation\": \"WSL Institute for Snow and Avalanche Research | ||
9 | SLF\", \"affiliation_02\": \"SLF\", \"affiliation_03\": \"\", | 9 | SLF\", \"affiliation_02\": \"SLF\", \"affiliation_03\": \"\", | ||
10 | \"data_credit\": [\"collection\", \"validation\", \"supervision\"], | 10 | \"data_credit\": [\"collection\", \"validation\", \"supervision\"], | ||
11 | \"email\": \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", | 11 | \"email\": \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", | ||
12 | \"identifier\": \"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, | 12 | \"identifier\": \"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, | ||
13 | {\"affiliation\": \"WSL Institute for Snow and Avalanche Research | 13 | {\"affiliation\": \"WSL Institute for Snow and Avalanche Research | ||
14 | SLF\", \"affiliation_02\": \"WSL\", \"affiliation_03\": \"ETH\", | 14 | SLF\", \"affiliation_02\": \"WSL\", \"affiliation_03\": \"ETH\", | ||
15 | \"data_credit\": \"supervision\", \"email\": \"schweizer@slf.ch\", | 15 | \"data_credit\": \"supervision\", \"email\": \"schweizer@slf.ch\", | ||
16 | \"given_name\": \"J\\u00fcrg\", \"identifier\": | 16 | \"given_name\": \"J\\u00fcrg\", \"identifier\": | ||
17 | \"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]", | 17 | \"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]", | ||
18 | "author_email": null, | 18 | "author_email": null, | ||
19 | "creator_user_id": "c8312541-12f8-4533-a778-53f3d3e6a99b", | 19 | "creator_user_id": "c8312541-12f8-4533-a778-53f3d3e6a99b", | ||
20 | "date": "[{\"date\": \"2019-01-04\", \"date_type\": \"collected\", | 20 | "date": "[{\"date\": \"2019-01-04\", \"date_type\": \"collected\", | ||
21 | \"end_date\": \"2019-03-19\"}]", | 21 | \"end_date\": \"2019-03-19\"}]", | ||
22 | "doi": "10.16904/envidat.365", | 22 | "doi": "10.16904/envidat.365", | ||
23 | "funding": "[{\"grant_number\": \"Grant/Award: 200021_169424\", | 23 | "funding": "[{\"grant_number\": \"Grant/Award: 200021_169424\", | ||
24 | \"institution\": \"Swiss National Science Foundation\", | 24 | \"institution\": \"Swiss National Science Foundation\", | ||
25 | \"institution_url\": \"\"}]", | 25 | \"institution_url\": \"\"}]", | ||
26 | "groups": [], | 26 | "groups": [], | ||
27 | "id": "24afd6a9-cb86-4a5b-b70b-aec194608c81", | 27 | "id": "24afd6a9-cb86-4a5b-b70b-aec194608c81", | ||
28 | "isopen": false, | 28 | "isopen": false, | ||
29 | "language": "en", | 29 | "language": "en", | ||
30 | "license_id": "wsl-data", | 30 | "license_id": "wsl-data", | ||
31 | "license_title": "WSL Data Policy", | 31 | "license_title": "WSL Data Policy", | ||
32 | "license_url": | 32 | "license_url": | ||
33 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 33 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
34 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | 34 | "maintainer": "{\"affiliation\": \"WSL Institute for Snow and | ||
35 | Avalanche Research SLF\", \"email\": \"bastian.bergfeld@slf.ch\", | 35 | Avalanche Research SLF\", \"email\": \"bastian.bergfeld@slf.ch\", | ||
36 | \"given_name\": \"Bastian\", \"identifier\": \"0000-0002-3316-1922\", | 36 | \"given_name\": \"Bastian\", \"identifier\": \"0000-0002-3316-1922\", | ||
37 | \"name\": \"Bergfeld\"}", | 37 | \"name\": \"Bergfeld\"}", | ||
38 | "maintainer_email": null, | 38 | "maintainer_email": null, | ||
39 | "metadata_created": "2023-01-23T09:20:46.332986", | 39 | "metadata_created": "2023-01-23T09:20:46.332986", | ||
n | 40 | "metadata_modified": "2023-01-27T08:40:28.673409", | n | 40 | "metadata_modified": "2023-01-27T08:41:40.443883", |
41 | "name": | 41 | "name": | ||
42 | ries-data-on-dynamic-crack-propagation-in-long-propagation-saw-tests", | 42 | ries-data-on-dynamic-crack-propagation-in-long-propagation-saw-tests", | ||
43 | "notes": "This data set includes material and results described in | 43 | "notes": "This data set includes material and results described in | ||
44 | the related research article:\r\n\r\nBergfeld, B., van Herwijnen A., | 44 | the related research article:\r\n\r\nBergfeld, B., van Herwijnen A., | ||
45 | Bobillier, G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., | 45 | Bobillier, G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., | ||
46 | and Schweizer, J.: Temporal evolution of crack propagation | 46 | and Schweizer, J.: Temporal evolution of crack propagation | ||
47 | characteristics in a weak snowpack layer: conditions of crack arrest | 47 | characteristics in a weak snowpack layer: conditions of crack arrest | ||
48 | and\r\nsustained propagation, Natural Hazards and Earth System | 48 | and\r\nsustained propagation, Natural Hazards and Earth System | ||
49 | Sciences, 23, 293-315, https://doi.org/10.5194/nhess-23-293-2023, | 49 | Sciences, 23, 293-315, https://doi.org/10.5194/nhess-23-293-2023, | ||
50 | 2023.\r\n\r\nWe performed a series of propagation saw test | 50 | 2023.\r\n\r\nWe performed a series of propagation saw test | ||
51 | experiments, up to ten meters long, over a period of 10 weeks and | 51 | experiments, up to ten meters long, over a period of 10 weeks and | ||
52 | analyzed these using digital image correlation techniques. We derived | 52 | analyzed these using digital image correlation techniques. We derived | ||
53 | the elastic modulus of the slab, the elastic modulus of the weak layer | 53 | the elastic modulus of the slab, the elastic modulus of the weak layer | ||
54 | and the specific fracture energy of the weak layer with a homogeneous | 54 | and the specific fracture energy of the weak layer with a homogeneous | ||
55 | and a layered slab model. During crack propagation, we measured crack | 55 | and a layered slab model. During crack propagation, we measured crack | ||
56 | speed, touchdown distance and the energy dissipation due to compaction | 56 | speed, touchdown distance and the energy dissipation due to compaction | ||
57 | and dynamic fracture. Our data set provides unique insight and | 57 | and dynamic fracture. Our data set provides unique insight and | ||
58 | valuable data to validate models.", | 58 | valuable data to validate models.", | ||
59 | "num_resources": 4, | 59 | "num_resources": 4, | ||
60 | "num_tags": 6, | 60 | "num_tags": 6, | ||
61 | "organization": { | 61 | "organization": { | ||
62 | "approval_status": "approved", | 62 | "approval_status": "approved", | ||
63 | "created": "2019-09-27T12:40:13.473824", | 63 | "created": "2019-09-27T12:40:13.473824", | ||
64 | "description": "Snow avalanches \u2013 a type of fast-moving mass | 64 | "description": "Snow avalanches \u2013 a type of fast-moving mass | ||
65 | movement \u2013 occur in snow covered mountain areas throughout the | 65 | movement \u2013 occur in snow covered mountain areas throughout the | ||
66 | world and may cause property damage and loss of life as they interfere | 66 | world and may cause property damage and loss of life as they interfere | ||
67 | with human activities. Most avalanches release from terrain steeper | 67 | with human activities. Most avalanches release from terrain steeper | ||
68 | than about 30\u00b0 during or soon after snow storms, or are triggered | 68 | than about 30\u00b0 during or soon after snow storms, or are triggered | ||
69 | by snow loading due to wind, or by a temperature change. Snow slab | 69 | by snow loading due to wind, or by a temperature change. Snow slab | ||
70 | avalanches can also be triggered artificially by, for example, people | 70 | avalanches can also be triggered artificially by, for example, people | ||
71 | (usually unintentionally) or intentionally by explosives used as part | 71 | (usually unintentionally) or intentionally by explosives used as part | ||
72 | of avalanche control programs. Today, most avalanche fatalities are | 72 | of avalanche control programs. Today, most avalanche fatalities are | ||
73 | recreationists. Independent of the triggering mode, the snowpack | 73 | recreationists. Independent of the triggering mode, the snowpack | ||
74 | layering is decisive for the instability of the snowpack which | 74 | layering is decisive for the instability of the snowpack which | ||
75 | consists of layers with varying properties. The complex microstructure | 75 | consists of layers with varying properties. The complex microstructure | ||
76 | of snow and spatial variations in snow layer properties across the | 76 | of snow and spatial variations in snow layer properties across the | ||
77 | terrain limit the predictability of snow avalanches. Even today, it is | 77 | terrain limit the predictability of snow avalanches. Even today, it is | ||
78 | not possible to predict the exact location, time and extent of an | 78 | not possible to predict the exact location, time and extent of an | ||
79 | avalanche event. Improving avalanche prediction requires a better | 79 | avalanche event. Improving avalanche prediction requires a better | ||
80 | understanding of the underlying processes. ", | 80 | understanding of the underlying processes. ", | ||
81 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 81 | "id": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
82 | "image_url": "2019-09-27-104013.456832slf.png", | 82 | "image_url": "2019-09-27-104013.456832slf.png", | ||
83 | "is_organization": true, | 83 | "is_organization": true, | ||
84 | "name": "avalanche-formation", | 84 | "name": "avalanche-formation", | ||
85 | "state": "active", | 85 | "state": "active", | ||
86 | "title": "Avalanche Formation and Dynamics", | 86 | "title": "Avalanche Formation and Dynamics", | ||
87 | "type": "organization" | 87 | "type": "organization" | ||
88 | }, | 88 | }, | ||
89 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | 89 | "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52", | ||
90 | "private": false, | 90 | "private": false, | ||
91 | "publication": "{\"publication_year\": \"2023\", \"publisher\": | 91 | "publication": "{\"publication_year\": \"2023\", \"publisher\": | ||
92 | \"EnviDat\"}", | 92 | \"EnviDat\"}", | ||
93 | "publication_state": "published", | 93 | "publication_state": "published", | ||
94 | "related_datasets": "", | 94 | "related_datasets": "", | ||
95 | "related_publications": "Bergfeld, B., van Herwijnen, A., Bobillier, | 95 | "related_publications": "Bergfeld, B., van Herwijnen, A., Bobillier, | ||
n | 96 | G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., and | n | 96 | G., Rosendahl, P. L., Wei\u00dfgraeber, P., Adam, V., Dual, J., and |
97 | Schweizer, J.: Temporal evolution of crack propagation characteristics | 97 | Schweizer, J.: Temporal evolution of crack propagation characteristics | ||
t | 98 | in a weak snowpack layer: conditions of crack arrest and\r\nsustained | t | 98 | in a weak snowpack layer: conditions of crack arrest and sustained |
99 | propagation, Natural Hazards and Earth System Sciences, 2023. | 99 | propagation, Nat. Hazards Earth Syst. Sci., 23, 293-315, | ||
100 | https://doi.org/10.5194/nhess-2022-161", | 100 | https://doi.org/10.5194/nhess-23-293-2023, 2023.", | ||
101 | "relationships_as_object": [], | 101 | "relationships_as_object": [], | ||
102 | "relationships_as_subject": [], | 102 | "relationships_as_subject": [], | ||
103 | "resource_type": "dataset", | 103 | "resource_type": "dataset", | ||
104 | "resource_type_general": "dataset", | 104 | "resource_type_general": "dataset", | ||
105 | "resources": [ | 105 | "resources": [ | ||
106 | { | 106 | { | ||
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109 | "created": "2023-01-23T09:28:38.855303", | 109 | "created": "2023-01-23T09:28:38.855303", | ||
110 | "description": "Snowpack data includes the elastic modulus | 110 | "description": "Snowpack data includes the elastic modulus | ||
111 | (stiffness properties) of the slab, the elastic modulus of the weak | 111 | (stiffness properties) of the slab, the elastic modulus of the weak | ||
112 | layer, and the specific fracture energy of the weak layer determined | 112 | layer, and the specific fracture energy of the weak layer determined | ||
113 | with a homogeneous and a layered slab model. During crack propagation, | 113 | with a homogeneous and a layered slab model. During crack propagation, | ||
114 | we measured the crack speed, touchdown distance, crack arrest length | 114 | we measured the crack speed, touchdown distance, crack arrest length | ||
115 | and energy dissipation due to compaction and dynamic fracture.", | 115 | and energy dissipation due to compaction and dynamic fracture.", | ||
116 | "doi": "", | 116 | "doi": "", | ||
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142 | "created": "2023-01-23T09:45:55.282510", | 142 | "created": "2023-01-23T09:45:55.282510", | ||
143 | "description": "The videos show the cracking process in the | 143 | "description": "The videos show the cracking process in the | ||
144 | Propagation Saw Tests (flat field). The upper panel shows strain on | 144 | Propagation Saw Tests (flat field). The upper panel shows strain on | ||
145 | top of the recorded movie frames. The second row shows vertical (w, | 145 | top of the recorded movie frames. The second row shows vertical (w, | ||
146 | blue line) and horizontal (u, orange line) displacement fields. The | 146 | blue line) and horizontal (u, orange line) displacement fields. The | ||
147 | third and fourth row show the first and second time derivatives, | 147 | third and fourth row show the first and second time derivatives, | ||
148 | namely the velocity and acceleration field.\r\n", | 148 | namely the velocity and acceleration field.\r\n", | ||
149 | "doi": "", | 149 | "doi": "", | ||
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175 | "created": "2023-01-23T10:07:39.415286", | 175 | "created": "2023-01-23T10:07:39.415286", | ||
176 | "description": "Index of self-sustained crack propagation SSP | 176 | "description": "Index of self-sustained crack propagation SSP | ||
177 | (ssp_measured.xlsx) with time. The self-sustained crack propagation | 177 | (ssp_measured.xlsx) with time. The self-sustained crack propagation | ||
178 | index SSP was also modelled for simulated snow stratigraphy | 178 | index SSP was also modelled for simulated snow stratigraphy | ||
179 | (ssp_modelled.xlsx) using crack speed and critical cut length | 179 | (ssp_modelled.xlsx) using crack speed and critical cut length | ||
180 | parameterizations from Heierli (2005) and Richter et al. (2019), | 180 | parameterizations from Heierli (2005) and Richter et al. (2019), | ||
181 | respectively.", | 181 | respectively.", | ||
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205 | { | 205 | { | ||
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208 | "created": "2023-01-23T10:21:30.200742", | 208 | "created": "2023-01-23T10:21:30.200742", | ||
209 | "description": "The snow cover model SNOWPACK (version 3.60) was | 209 | "description": "The snow cover model SNOWPACK (version 3.60) was | ||
210 | used to simulate the evolving snow stratigraphy at our field site. The | 210 | used to simulate the evolving snow stratigraphy at our field site. The | ||
211 | model was driven with data from an automatic weather station which was | 211 | model was driven with data from an automatic weather station which was | ||
212 | located 100m next to the field site (FLS_bunker_snowpack.smet). The | 212 | located 100m next to the field site (FLS_bunker_snowpack.smet). The | ||
213 | SNOWPACK initiation file (FLS_bunker_snowpack.ini) contains the | 213 | SNOWPACK initiation file (FLS_bunker_snowpack.ini) contains the | ||
214 | selected model parameters that result in the modeled snow stratigraphy | 214 | selected model parameters that result in the modeled snow stratigraphy | ||
215 | (FLS_bunker_snowpack.pro).", | 215 | (FLS_bunker_snowpack.pro).", | ||
216 | "doi": "", | 216 | "doi": "", | ||
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222 | "mimetype": null, | 222 | "mimetype": null, | ||
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224 | "name": "SNOWPACK modelling", | 224 | "name": "SNOWPACK modelling", | ||
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244 | "subtitle": "", | 244 | "subtitle": "", | ||
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293 | "version": "1.0" | 293 | "version": "1.0" | ||
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