Changes
On January 21, 2025 at 9:30:00 AM UTC,
-
Added field
deprecatedResources
with value["74c3db20-eaed-40de-a880-f042010cf6cc"]
to Capillary rise rise experiments in snow using neutron radiography
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4 | {\"given_name\": \"Amelie\", \"name\": \"Fees\", \"email\": | 4 | {\"given_name\": \"Amelie\", \"name\": \"Fees\", \"email\": | ||
5 | \"amelie.fees@slf.ch\", \"data_credit\": [], \"identifier\": \"\", | 5 | \"amelie.fees@slf.ch\", \"data_credit\": [], \"identifier\": \"\", | ||
6 | \"affiliation\": \"WSL Institute for Snow and Avalanche Research | 6 | \"affiliation\": \"WSL Institute for Snow and Avalanche Research | ||
7 | SLF\"}, {\"given_name\": \"Anders\", \"name\": \"Kaestner\", | 7 | SLF\"}, {\"given_name\": \"Anders\", \"name\": \"Kaestner\", | ||
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9 | \"identifier\": \"\", \"affiliation\": \"Paul Scherrer Institute | 9 | \"identifier\": \"\", \"affiliation\": \"Paul Scherrer Institute | ||
10 | PSI\"}, {\"given_name\": \"Alec\", \"name\": \"van Herwijnen\", | 10 | PSI\"}, {\"given_name\": \"Alec\", \"name\": \"van Herwijnen\", | ||
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12 | \"identifier\": \"\", \"affiliation\": \"WSL Institute for Snow and | 12 | \"identifier\": \"\", \"affiliation\": \"WSL Institute for Snow and | ||
13 | Avalanche Research SLF\"}, {\"given_name\": \"J\\u00fcrg\", \"name\": | 13 | Avalanche Research SLF\"}, {\"given_name\": \"J\\u00fcrg\", \"name\": | ||
14 | \"Schweizer\", \"email\": \"schweizer@slf.ch\", \"data_credit\": [], | 14 | \"Schweizer\", \"email\": \"schweizer@slf.ch\", \"data_credit\": [], | ||
15 | \"identifier\": \"0000-0001-5076-2968\", \"affiliation\": \"WSL | 15 | \"identifier\": \"0000-0001-5076-2968\", \"affiliation\": \"WSL | ||
16 | Institute for Snow and Avalanche Research SLF\"}, {\"given_name\": | 16 | Institute for Snow and Avalanche Research SLF\"}, {\"given_name\": | ||
17 | \"Peter\", \"name\": \"Lehmann\", \"email\": | 17 | \"Peter\", \"name\": \"Lehmann\", \"email\": | ||
18 | \"peter.lehmann@env.ethz.ch\", \"data_credit\": [], \"identifier\": | 18 | \"peter.lehmann@env.ethz.ch\", \"data_credit\": [], \"identifier\": | ||
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22 | "date": | 22 | "date": | ||
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24 | "doi": "10.16904/envidat.572", | 24 | "doi": "10.16904/envidat.572", | ||
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31 | "license_title": "Creative Commons Attribution", | 37 | "license_title": "Creative Commons Attribution", | ||
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38 | "name": | 44 | "name": | ||
39 | "capillary-rise-rise-experiments-in-snow-using-neutron-radiography", | 45 | "capillary-rise-rise-experiments-in-snow-using-neutron-radiography", | ||
40 | "notes": "This dataset consists of data related to capillary rise | 46 | "notes": "This dataset consists of data related to capillary rise | ||
41 | experiments performed with neutron radiography. There are 4 videos of | 47 | experiments performed with neutron radiography. There are 4 videos of | ||
42 | capillary rise experiments as well as the files used to perform the | 48 | capillary rise experiments as well as the files used to perform the | ||
43 | inverse fitting with Hydrus. The videos show the upward flow of water | 49 | inverse fitting with Hydrus. The videos show the upward flow of water | ||
44 | in glass columns filled with sand and snow or sand, gravel, and snow. | 50 | in glass columns filled with sand and snow or sand, gravel, and snow. | ||
45 | The videos show the 2D evolution of the unitless optical density with | 51 | The videos show the 2D evolution of the unitless optical density with | ||
46 | time. The Hydrus files were used to fit the parameter values of the | 52 | time. The Hydrus files were used to fit the parameter values of the | ||
47 | Mualem-van Genuchten model. The experiments were performed at the Paul | 53 | Mualem-van Genuchten model. The experiments were performed at the Paul | ||
48 | Scherrer Institute (PSI) in Villigen, Switzerland. ", | 54 | Scherrer Institute (PSI) in Villigen, Switzerland. ", | ||
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51 | "organization": { | 57 | "organization": { | ||
52 | "approval_status": "approved", | 58 | "approval_status": "approved", | ||
53 | "created": "2019-09-27T12:40:13.473824", | 59 | "created": "2019-09-27T12:40:13.473824", | ||
54 | "description": "Snow avalanches \u2013 a type of fast-moving mass | 60 | "description": "Snow avalanches \u2013 a type of fast-moving mass | ||
55 | movement \u2013 occur in snow covered mountain areas throughout the | 61 | movement \u2013 occur in snow covered mountain areas throughout the | ||
56 | world and may cause property damage and loss of life as they interfere | 62 | world and may cause property damage and loss of life as they interfere | ||
57 | with human activities. Most avalanches release from terrain steeper | 63 | with human activities. Most avalanches release from terrain steeper | ||
58 | than about 30\u00b0 during or soon after snow storms, or are triggered | 64 | than about 30\u00b0 during or soon after snow storms, or are triggered | ||
59 | by snow loading due to wind, or by a temperature change. Snow slab | 65 | by snow loading due to wind, or by a temperature change. Snow slab | ||
60 | avalanches can also be triggered artificially by, for example, people | 66 | avalanches can also be triggered artificially by, for example, people | ||
61 | (usually unintentionally) or intentionally by explosives used as part | 67 | (usually unintentionally) or intentionally by explosives used as part | ||
62 | of avalanche control programs. Today, most avalanche fatalities are | 68 | of avalanche control programs. Today, most avalanche fatalities are | ||
63 | recreationists. Independent of the triggering mode, the snowpack | 69 | recreationists. Independent of the triggering mode, the snowpack | ||
64 | layering is decisive for the instability of the snowpack which | 70 | layering is decisive for the instability of the snowpack which | ||
65 | consists of layers with varying properties. The complex microstructure | 71 | consists of layers with varying properties. The complex microstructure | ||
66 | of snow and spatial variations in snow layer properties across the | 72 | of snow and spatial variations in snow layer properties across the | ||
67 | terrain limit the predictability of snow avalanches. Even today, it is | 73 | terrain limit the predictability of snow avalanches. Even today, it is | ||
68 | not possible to predict the exact location, time and extent of an | 74 | not possible to predict the exact location, time and extent of an | ||
69 | avalanche event. Improving avalanche prediction requires a better | 75 | avalanche event. Improving avalanche prediction requires a better | ||
70 | understanding of the underlying processes. ", | 76 | understanding of the underlying processes. ", | ||
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75 | "state": "active", | 81 | "state": "active", | ||
76 | "title": "Avalanche Formation and Dynamics", | 82 | "title": "Avalanche Formation and Dynamics", | ||
77 | "type": "organization" | 83 | "type": "organization" | ||
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81 | "publication": | 87 | "publication": | ||
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234 | "vocabulary_id": null | 240 | "vocabulary_id": null | ||
235 | }, | 241 | }, | ||
236 | { | 242 | { | ||
237 | "display_name": "WATER", | 243 | "display_name": "WATER", | ||
238 | "id": "bfb14386-9f8c-42df-a144-1d000dfb5f16", | 244 | "id": "bfb14386-9f8c-42df-a144-1d000dfb5f16", | ||
239 | "name": "WATER", | 245 | "name": "WATER", | ||
240 | "state": "active", | 246 | "state": "active", | ||
241 | "vocabulary_id": null | 247 | "vocabulary_id": null | ||
242 | } | 248 | } | ||
243 | ], | 249 | ], | ||
244 | "title": "Capillary rise rise experiments in snow using neutron | 250 | "title": "Capillary rise rise experiments in snow using neutron | ||
245 | radiography", | 251 | radiography", | ||
246 | "type": "dataset", | 252 | "type": "dataset", | ||
247 | "url": null | 253 | "url": null | ||
248 | } | 254 | } |