Änderungen
Auf 7. September 2023 um 15:34:03 UTC,
Renee Obregon:
-
Folgende Felder wurden zu Promising areas for shallow geothermal energy (Breda formation) hinzugefügt
- harvest_source_title mit dem Wert OverheidNl
- Group mit dem Wert Shared mobility
- harvest_source_id mit dem Wert 2d143cca-7932-40e0-9df7-9fe853be01b4
- harvest_object_id mit dem Wert bb1ea307-afa7-4235-8954-bc0fd96fed8e
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| 8 | "value": "Shared mobility" | ||||
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| 6 | "groups": [], | 23 | "groups": [], | ||
| 7 | "id": "1f84d309-6141-4ea9-b209-0865a3e3133a", | 24 | "id": "1f84d309-6141-4ea9-b209-0865a3e3133a", | ||
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| 15 | "metadata_created": "2023-04-12T08:08:39.837326", | 32 | "metadata_created": "2023-04-12T08:08:39.837326", | ||
| n | 16 | "metadata_modified": "2023-04-12T08:08:39.837331", | n | 33 | "metadata_modified": "2023-09-07T15:34:03.539029", |
| 17 | "name": | 34 | "name": | ||
| 18 | "37928-areas-rich-areas-for-shallow-geothermal-formation-of-breda", | 35 | "37928-areas-rich-areas-for-shallow-geothermal-formation-of-breda", | ||
| 19 | "notes": "This map layer contains calculated clusters based on the | 36 | "notes": "This map layer contains calculated clusters based on the | ||
| 20 | grid level heat demand map. Based on this map and the lower limit of | 37 | grid level heat demand map. Based on this map and the lower limit of | ||
| 21 | 1,000 GJ/ha/year, a selection of areas has been created that have | 38 | 1,000 GJ/ha/year, a selection of areas has been created that have | ||
| 22 | sufficient heat density for a collective solution. A buffer of 50 | 39 | sufficient heat density for a collective solution. A buffer of 50 | ||
| 23 | meters has been created around these clusters to involve neighboring | 40 | meters has been created around these clusters to involve neighboring | ||
| 24 | buildings and addresses that have contributed to the high heat demand | 41 | buildings and addresses that have contributed to the high heat demand | ||
| 25 | density in the cluster. For the remaining clusters, it was first | 42 | density in the cluster. For the remaining clusters, it was first | ||
| 26 | checked whether they meet the lower limit of 500 GJ/year for | 43 | checked whether they meet the lower limit of 500 GJ/year for | ||
| 27 | collective solutions. The remaining clusters were then buffered by 300 | 44 | collective solutions. The remaining clusters were then buffered by 300 | ||
| 28 | meters to identify which clusters could be strung as beads to form a | 45 | meters to identify which clusters could be strung as beads to form a | ||
| 29 | larger network. The heat demand of these large clusters was then | 46 | larger network. The heat demand of these large clusters was then | ||
| 30 | calculated. For the effective use of a shallow geothermal system, a | 47 | calculated. For the effective use of a shallow geothermal system, a | ||
| 31 | lower limit of heat demand is required. In this map layer, this lower | 48 | lower limit of heat demand is required. In this map layer, this lower | ||
| 32 | limit is set at 50,000 GJ/year. Clusters whose heat demand was lower | 49 | limit is set at 50,000 GJ/year. Clusters whose heat demand was lower | ||
| 33 | are therefore excluded. To determine the underground heat supply under | 50 | are therefore excluded. To determine the underground heat supply under | ||
| 34 | the cluster, further work was done from the 'laced clusters'. A buffer | 51 | the cluster, further work was done from the 'laced clusters'. A buffer | ||
| 35 | of 700 meters has been added to these clusters to reach a total of | 52 | of 700 meters has been added to these clusters to reach a total of | ||
| 36 | 1,000 meters from the initial clusters. A heat supply density was | 53 | 1,000 meters from the initial clusters. A heat supply density was | ||
| 37 | calculated from the OGT potential maps of Breda and Brussels in the | 54 | calculated from the OGT potential maps of Breda and Brussels in the | ||
| 38 | soil under the cluster. This density is multiplied by the surface area | 55 | soil under the cluster. This density is multiplied by the surface area | ||
| 39 | of \u200b\u200bthe cluster to calculate the total heat supply. This | 56 | of \u200b\u200bthe cluster to calculate the total heat supply. This | ||
| 40 | calculated heat supply and the calculated heat demand of the cluster | 57 | calculated heat supply and the calculated heat demand of the cluster | ||
| 41 | make a partial sum with the degree of coverage as the answer.", | 58 | make a partial sum with the degree of coverage as the answer.", | ||
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