Results 201 to 210 of about 9,106 (263)

3D upper crustal structure modelling in southwestern Sicily through multiapproach onshore-offshore data: insight into Sciacca Geothermal Field. [PDF]

Sci Rep
Rizzo GF, Maiorana M, Gasparo Morticelli M, Lo Presti V, Agate M, Sulli A.   +5 more
europepmc   +1 more source

Dynamic confinement controls the porous-to-free convection transition. [PDF]

Proc Natl Acad Sci U S A
Schwendener DM, Noir J, Latt J, Coreixas C, Kong XZ.   +4 more
europepmc   +1 more source

Risk assessment of a mixture of pharmaceuticals and personal care products (PPCPs) in thermal waters of Kütahya, Türkiye. [PDF]

Environ Geochem Health
Şener H, Yavuz Güzel E, Karakuş H.
europepmc   +1 more source

Design of aerogel granule size for thermal insulation of petroleum pipelines. [PDF]

Sci Rep
Liu X, Wu J, Zhang J, Zhao P, Momanyi NK, Zhou Z, Jiang W, Xie Y, Liu L.   +8 more
europepmc   +1 more source

Operators' good community engagement practices in energy projects: examples from the UK deep geothermal sector. [PDF]

Energy Sustain Soc
Ryder S, Rohse M, Abesser C.
europepmc   +1 more source

Thermoacoustic wave propagation in hydrodynamic poroelastic media with temperature-dependent thermal conductivity. [PDF]

Sci Rep
Alshehri AM, Lotfy K.
europepmc   +1 more source

RADIOACTIVITY OF GEOTHERMAL SYSTEMS

, 1975
openaire   +1 more source

Life on Mars? The physiological perspective

Experimental Physiology, EarlyView.
Ronan M. G. Berg, Damian M. Bailey
wiley   +1 more source

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Ocean and Geothermal Energy Systems

Proceedings of the IEEE, 2017
This paper presents techno–economic summaries of ocean wave, tidal and current, ocean thermal, and geothermal energy, including grid interface characteristics. These forms of energy represent a significant opportunity to complement diversified energy conversion portfolios.
Annette R. von Jouanne, Ted K. A. Brekken   +1 more
openaire   +1 more source

Fluids in Geothermal Systems

Elements, 2020
Hot fluids are nearly ubiquitous in volcanic environments in the Earth’s crust. Magma at depth heats groundwater which then ascends towards the Earth’s surface through faults, fractures, and otherwise permeable rocks. Fluids in geothermal systems offer direct insight into the many complex chemical and physical processes that occur in these extreme ...
Isabelle Chambefort, Andri Stefánsson
openaire   +1 more source