scholarly journals Soil diffuse degassing and thermal energy fluxes from the Southern Lakki Plain, Nisyros (Greece)

2001 ◽  
Vol 28 (1) ◽  
pp. 69-72 ◽  
Author(s):  
Tatjana Brombach ◽  
Johannes C. Hunziker ◽  
Giovanni Chiodini ◽  
Carlo Cardellini ◽  
Luigi Marini
Keyword(s):  
Thermal Energy ◽  
Energy Fluxes ◽  
Diffuse Degassing ◽  
Soil Diffuse Degassing

Hg and CO2 emissions from soil diffuse degassing and fumaroles at Furnas Volcano (São Miguel Island, Azores): Gas flux and thermal energy output

2018 ◽  
Vol 190 ◽  
pp. 39-57 ◽  
Author(s):  
E. Bagnato ◽  
F. Viveiros ◽  
J.E. Pacheco ◽  
F. D'Agostino ◽  
C. Silva ◽  
...  
Keyword(s):  
Co2 Emissions ◽  
Thermal Energy ◽  
Energy Output ◽  
Gas Flux ◽  
Diffuse Degassing ◽  
Furnas Volcano ◽  
Soil Diffuse Degassing

COMPUTER SIMULATION OF AIR-ESTUARY THERMAL ENERGY FLUXES

1980 ◽  
pp. 317-328
Author(s):  
Ned P. Smith
Keyword(s):  
Computer Simulation ◽  
Thermal Energy ◽  
Energy Fluxes

scholarly journals Heat and Helium-3 Fluxes from Teide Volcano, Canary Islands, Spain

Geofluids ◽  
2019 ◽  
Vol 2019 ◽  
pp. 1-12
Author(s):  
Mar Alonso ◽  
Eleazar Padrón ◽  
Hirochika Sumino ◽  
Pedro A. Hernández ◽  
Gladys V. Melián ◽  
...  
Keyword(s):  
Heat Flux ◽  
Heat Flow ◽  
Canary Islands ◽  
Thermal Energy ◽  
Heat Fluxes ◽  
Volcanic System ◽  
Diffuse Degassing ◽  
Helium 3 ◽  
Teide Volcano ◽  
First Time

During July 2016, the first integrated heat flow, CO2, and 3He emission survey was conducted across 0.5 km2 of the summit cone and crater of Teide volcano, Tenerife, Canary Islands, Spain. The thermal energy released from Teide summit cone by diffuse degassing was 2.2 MW, and the heat flux calculated through Dawson’s method was 8.1 MW, difference due to the comparison of purely convective areas as the crater with diffusive areas as the flanks of the volcano. Diffuse CO2 output was 211±20 t d-1, and 3He emission was estimated to be within a range between 0.35 and 0.89 mol y-1. The obtained values of diffuse degassing and heat fluxes are close to others obtained for similar volcanic areas. The calculation of 3He/heat ratio for the first time in this volcanic system supports the presence of an important mantle source for the degassing of Teide volcano.

Continuous monitoring of CO 2 soil diffuse degassing at Phlegraean Fields (Italy): influence of environmental and volcanic parameters

2003 ◽  
Vol 212 (1-2) ◽  
pp. 167-179 ◽  
Author(s):  
D Granieri ◽  
G Chiodini ◽  
W Marzocchi ◽  
R Avino
Keyword(s):  
Continuous Monitoring ◽  
Diffuse Degassing ◽  
Phlegraean Fields ◽  
Soil Diffuse Degassing

Quantification of deep CO2 fluxes from Central Italy. Examples of carbon balance for regional aquifers and of soil diffuse degassing

1999 ◽  
Vol 159 (1-4) ◽  
pp. 205-222 ◽  
Author(s):  
G. Chiodini ◽  
F. Frondini ◽  
D.M. Kerrick ◽  
J. Rogie ◽  
F. Parello ◽  
...  
Keyword(s):  
Carbon Balance ◽  
Central Italy ◽  
Co2 Fluxes ◽  
Diffuse Degassing ◽  
Soil Diffuse Degassing

Carbon dioxide diffuse degassing as a tool for computing the thermal energy release at Cerro Blanco Geothermal System, Southern Puna (NW Argentina)

2021 ◽  
Vol 105 ◽  
pp. 102833
Author(s):  
M.C. Lamberti ◽  
A. Chiodi ◽  
M. Agusto ◽  
R. Filipovich ◽  
A. Massenzio ◽  
...  
Keyword(s):  
Carbon Dioxide ◽  
Energy Release ◽  
Thermal Energy ◽  
Geothermal System ◽  
Diffuse Degassing

The thermal energy method

1978 ◽  
Vol 57 (6) ◽  
pp. 19 ◽  
Keyword(s):  
Thermal Energy ◽  
Energy Method

A heavy isotope in a solid drifts down a thermal energy gradient

1976 ◽  
Vol 37 (3) ◽  
pp. 183-188 ◽  
Author(s):  
R.V. Hesketh
Keyword(s):  
Thermal Energy ◽  
Heavy Isotope ◽  
Energy Gradient

Greenhouses, hot water bottles, cycles and the future of New Zealand climate

2009 ◽  
pp. 61-67
Author(s):  
W.P. De Lange
Keyword(s):  
New Zealand ◽  
Thermal Energy ◽  
Infrared Radiation ◽  
Little Ice Age ◽  
Hot Water ◽  
Ice Age ◽  
The Sun ◽  
Weather Patterns ◽  
Time Periods ◽  
Almost All

The Greenhouse Effect acts to slow the escape of infrared radiation to space, and hence warms the atmosphere. The oceans derive almost all of their thermal energy from the sun, and none from infrared radiation in the atmosphere. The thermal energy stored by the oceans is transported globally and released after a range of different time periods. The release of thermal energy from the oceans modifies the behaviour of atmospheric circulation, and hence varies climate. Based on ocean behaviour, New Zealand can expect weather patterns similar to those from 1890-1922 and another Little Ice Age may develop this century.

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