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At the same time, our approach maintains the appropriate incentives/disincentives for beneficial/detrimental actions, i.e. the positive or negative atmospheric impact of changes in management relative to the historical period are fully reflected in the accounts.
In comparison with those cases described above, the Upper Paleozoic tight gas reservoirs of the Ordos Basin show complex pressure systems with pressure coefficients varying greatly across all pressure range (i.e., negative, atmospheric, and overpressure).
Results of these changes will determine the ability of Alaska lands to continue to: provide habitat for local and migratory species; absorb species whose ranges are shifting northward; and experience mitigation or exacerbation of climate change through positive and negative atmospheric feedbacks.
Long-chain fatty acids were analyzed using negative atmospheric pressure chemical ionization (APCI) as previously described [ 15].
A pump provides the vacuum that exposes the submerged plants to a negative atmospheric pressure and draws the air out of the interstitial space of the leaves.
Arora et al. used 5 μm octadecyl silica particles and a linear gradient for separation of β-apocarotenals, epoxy-β-carotenes, and 4-nitro-β-carotene, with UV and triple quadrupole mass spectrometric detection in negative atmospheric pressure chemical ionization (APCI) mode [ 96].
Similar(53)
It includes a halt to global emissions growth by 2020, followed by rapid global emissions reductions, and a massive program to remove carbon from the atmosphere, resulting in net negative emissions — atmospheric clean-up — by late in the century.
Integration of biomass energy technologies with carbon capture and sequestration could yield useful energy products and negative net atmospheric carbon emissions.
This chapter explores the technical feasibility and economic implications of combining biomass energy systems with carbon capture and sequestration (CCS) technology, resulting in energy products with negative net atmospheric carbon emissions.
This challenges the commonly held assumption that streambed under a disconnected stream is always fully saturated, and limits the methods which introduce a negative or atmospheric pressure value at the IBSA to calculate seepage rate or assess stream-aquifer connectivity.
With the changing contact area of the tongue and the palate, a proceeding area of positive pressure may be measured (a combination of active valve tongue pressure and negative compartment atmospheric pressure).
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