Over long periods of time (~ Ma), we may consider the oceans, atmosphere and biosphere
as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs …

An In-Depth Introduction to Geothermal Energy Addressing significant changes in the
energy markets since the first edition, Geothermal Energy: Renewable Energy and the …

The atmospheric methane budget is commonly defined assuming that major sources derive
from the biosphere (wetlands, rice paddies, animals, termites) and that fossil, radiocarbon …

Conditional sequential Gaussian simulations (sGs) have been applied for the first time to the
study of soil diffuse degassing from different volcanic and nonvolcanic systems. The …

So far, the role of present-day Earth degassing in global C budget and climate effects has
been focused to volcanic emissions. The non-volcanic escape of CO2–CH4 from the upper …

This work addresses the study of fluid circulation of the Stromboli island using a dense
coverage of self-potential (SP) and soil CO2 data. A marked difference exists between the …

The ratio of CO2 emissions from power plants to natural emissions is a measure of the
environmental impact associated with geothermal power production. Emissions from …

Deep carbon emissions from historically inactive volcanoes, hydrothermal, and tectonic
structures are among the greatest unknowns in the long‐term (∼ Myr) carbon cycle. Recent …

Abstract The northeastern Tibetan Plateau (NETP) is the most intensely uplifted deformation
region in the Tibetan Plateau. The intense gas release caused by uplift has attracted …

Direct measurement of present day CH4 diffuse degassing from the soil represents an
effective tool to better estimate the degassing rate of individual sources and to calibrate …