Groundwater use for snow melting on the road
Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable rang...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kayane, I. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1980 |
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| Schlagwörter: |
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| Anmerkung: |
© Akademische Verlagsgesellschaft 1980 |
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| Übergeordnetes Werk: |
Enthalten in: GeoJournal - Kluwer Academic Publishers, 1977, 4(1980), 2 vom: März, Seite 173-181 |
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| Übergeordnetes Werk: |
volume:4 ; year:1980 ; number:2 ; month:03 ; pages:173-181 |
| Links: |
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| DOI / URN: |
10.1007/BF00705524 |
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| Katalog-ID: |
OLC2113644738 |
|---|
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| 520 | |a Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. | ||
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| 650 | 4 | |a Environmental Management | |
| 650 | 4 | |a Actual Condition | |
| 650 | 4 | |a Groundwater Flow | |
| 650 | 4 | |a Groundwater Recharge | |
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10.1007/BF00705524 doi (DE-627)OLC2113644738 (DE-He213)BF00705524-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn BIODIV DE-30 fid Kayane, I. verfasserin aut Groundwater use for snow melting on the road 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Akademische Verlagsgesellschaft 1980 Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. Japan Environmental Management Actual Condition Groundwater Flow Groundwater Recharge Enthalten in GeoJournal Kluwer Academic Publishers, 1977 4(1980), 2 vom: März, Seite 173-181 (DE-627)13044555X (DE-600)715360-0 (DE-576)015981851 0343-2521 nnns volume:4 year:1980 number:2 month:03 pages:173-181 https://doi.org/10.1007/BF00705524 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 GBV_ILN_72 GBV_ILN_130 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4700 AR 4 1980 2 03 173-181 |
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10.1007/BF00705524 doi (DE-627)OLC2113644738 (DE-He213)BF00705524-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn BIODIV DE-30 fid Kayane, I. verfasserin aut Groundwater use for snow melting on the road 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Akademische Verlagsgesellschaft 1980 Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. Japan Environmental Management Actual Condition Groundwater Flow Groundwater Recharge Enthalten in GeoJournal Kluwer Academic Publishers, 1977 4(1980), 2 vom: März, Seite 173-181 (DE-627)13044555X (DE-600)715360-0 (DE-576)015981851 0343-2521 nnns volume:4 year:1980 number:2 month:03 pages:173-181 https://doi.org/10.1007/BF00705524 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 GBV_ILN_72 GBV_ILN_130 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4700 AR 4 1980 2 03 173-181 |
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10.1007/BF00705524 doi (DE-627)OLC2113644738 (DE-He213)BF00705524-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn BIODIV DE-30 fid Kayane, I. verfasserin aut Groundwater use for snow melting on the road 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Akademische Verlagsgesellschaft 1980 Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. Japan Environmental Management Actual Condition Groundwater Flow Groundwater Recharge Enthalten in GeoJournal Kluwer Academic Publishers, 1977 4(1980), 2 vom: März, Seite 173-181 (DE-627)13044555X (DE-600)715360-0 (DE-576)015981851 0343-2521 nnns volume:4 year:1980 number:2 month:03 pages:173-181 https://doi.org/10.1007/BF00705524 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 GBV_ILN_72 GBV_ILN_130 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4700 AR 4 1980 2 03 173-181 |
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10.1007/BF00705524 doi (DE-627)OLC2113644738 (DE-He213)BF00705524-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn BIODIV DE-30 fid Kayane, I. verfasserin aut Groundwater use for snow melting on the road 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Akademische Verlagsgesellschaft 1980 Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. Japan Environmental Management Actual Condition Groundwater Flow Groundwater Recharge Enthalten in GeoJournal Kluwer Academic Publishers, 1977 4(1980), 2 vom: März, Seite 173-181 (DE-627)13044555X (DE-600)715360-0 (DE-576)015981851 0343-2521 nnns volume:4 year:1980 number:2 month:03 pages:173-181 https://doi.org/10.1007/BF00705524 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 GBV_ILN_72 GBV_ILN_130 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4700 AR 4 1980 2 03 173-181 |
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10.1007/BF00705524 doi (DE-627)OLC2113644738 (DE-He213)BF00705524-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn BIODIV DE-30 fid Kayane, I. verfasserin aut Groundwater use for snow melting on the road 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Akademische Verlagsgesellschaft 1980 Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. Japan Environmental Management Actual Condition Groundwater Flow Groundwater Recharge Enthalten in GeoJournal Kluwer Academic Publishers, 1977 4(1980), 2 vom: März, Seite 173-181 (DE-627)13044555X (DE-600)715360-0 (DE-576)015981851 0343-2521 nnns volume:4 year:1980 number:2 month:03 pages:173-181 https://doi.org/10.1007/BF00705524 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 GBV_ILN_72 GBV_ILN_130 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4700 AR 4 1980 2 03 173-181 |
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Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. 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Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. © Akademische Verlagsgesellschaft 1980 |
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Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. © Akademische Verlagsgesellschaft 1980 |
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Abstract Groundwater use for snow melting on the road began in Nagooka in 1961. Thereafter the shosetsu (snow melting) pipe system using the heat energy of groundwater spread rapidly all over Japan except for Hokkaido. The total length of the shosetsu pipe comprised 571 km in 1977. A preferable range of groundwater temperatures for the shosetsu pipe is from 8° to 18°C, which corresponds to the groundwater temperature in Japan. The actual condition of groundwater use for the shosetsu pipe has been investigated in Nagaoka, where groundwater pumping in total amounts to 5 x $ 10^{5} $ $ m^{3} $/day in the heavy snow season. The use of groundwater for shosetsu pipe in Nagaoka is confronted with two serious problems to be overcome. They are land subsidence and competition with other groundwater uses. For purposes of making clear the mechanism of groundwater recharge and of seeking means of groundwater management for the Nagaoka groundwater basin, a digital simulation of groundwater flow was made by using the horizontal two-dimensional model. The results are satisfactory and reveal that one of the main sources of recharge is the Shinano River which flows through the city. The simulation will be a useful means in considering a future plan of groundwater management. © Akademische Verlagsgesellschaft 1980 |
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