Hydrogen production by biomass gasification using solar energy is a promising approach for overcoming the drawbacks of fossil fuel utilization, but the storage of discontinuous solar flux is a critical issue for continuous solar hydrogen production.
The coupled effect of terrestrial C and AD-OC may influence the storage and flux of C in receiving water bodies.
Understanding the processes governing the storage and flux of this inorganic C pool is crucial to the development of accurate regional and global C budgets.
Wilmers, C. C., Estes, J. A., Edwards, M., Laidre, K. L. & Konar, B. Do trophic cascades affect the storage and flux of atmospheric carbon?
The storage and flux of carbon from soils, the planet's third largest carbon pool, strongly influence the global carbon cycle and are essential, but poorly constrained, parameters for global climate models.
The knowledge of regional sensitivity of landscapes, whether as C sink or source, the magnitude of C storage or flux and vulnerability to anthropogenic perturbations are all important for understanding regional C budget.
Estuarine freshwater marshes can act as an important ecosystem for carbon storage and flux because of its strategic position in a watershed.
Recent estimates of net annual storage, or flux, indicate that the world's forests are an important carbon sink, removing more carbon from the atmosphere through photosynthesis than they emit through combustion and decay [1].
Recent estimates of net annual storage, or flux, indicate that the world's forests are an important carbon sink, removing more carbon from the atmosphere through photosynthesis than they emit through combustion and decay [ 1].
For example, hydrological models such as Soil and Water Assessment Tool (SWAT) focus on the water cycle and nutrient loadings at watershed scale, whereas biogeochemical models such as DayCent (i.e., daily CENTURY) emphasize carbon/nitrogen storage and fluxes of ecosystems at landscape scale.
