Advances in the Geological Storage of Carbon Dioxide: by B.D. Belan, A.V. Fofonov, T.K. Sklyadneva, G.N. Tolmachev PDF

By B.D. Belan, A.V. Fofonov, T.K. Sklyadneva, G.N. Tolmachev (auth.), S. Lombardi, L.K. Altunina, S.E. Beaubien (eds.)

ISBN-10: 1402044690

ISBN-13: 9781402044694

ISBN-10: 1402044712

ISBN-13: 9781402044717

As is now normally approved mankind’s burning of fossil fuels has led to the mass move of greenhouse gases to the ambience, a amendment of the delicately-balanced international carbon cycle, and a measurable swap in world-wide temperatures and weather. even supposing now not the main robust greenhouse gasoline, carbon dioxide (CO) drives weather 2 swap as a result of huge, immense volumes of this fuel pumped into the ambience on a daily basis. Produced in nearly equivalent components by means of the transportation, business and energy-generating sectors, atmospheric CO concentrations have 2 elevated through approximately 50% during the last three hundred years, and in line with a few assets are anticipated to extend by means of as much as two hundred% over pre-industrial degrees throughout the subsequent a hundred years. If we're to opposite this pattern, in an effort to hinder major environmental swap sooner or later, motion needs to be taken instantly. whereas lowered use of fossil fuels (through conservation, elevated potency and multiplied use of renewable power assets) has to be our final target, brief to medium time period ideas are wanted which may make an influence at the present time. a number of kinds of CO garage strategies were proposed to fill this 2 desire, with the injection of this gasoline into deep geological reservoirs being some of the most promising. for instance this technique has the aptitude to develop into a closed loop approach, wherein underground power assets are delivered to floor, their power extracted (via burning or hydrogen extraction), and the ensuing by-products again to the subsurface.

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Extra info for Advances in the Geological Storage of Carbon Dioxide: International Approaches to Reduce Anthropogenic Greenhouse Gas Emissions

Example text

Soil humus mineralisation in ecosystems varies from 3 to 13% in the southern taiga and from 2 to 6% in northern forests. 2% of it in forest tundra and in larch forests of the northern taiga. Experimentally determined phytodetritus decomposing rates, averaged for forest zones and subzones of the Yenisei meridian, are given in Table 1. 1 mg ɋ g-1 day-1) in the direction from forest tundra to southern taiga. 24 Vaganov, Efremov and Onuchin Table 1. Indices of phytodetritus decomposition rate. 011 8 Young forest ecosystems (tree stands of classes I-II in age) of the main Siberian forest-forming species, the southern taiga pine forests and birch stands and larch ecosystems of the northern taiga are a sink for atmospheric carbon.

4, respectively). As Utkin et al. 3. 8 in forest tundra and northern taiga forests, middle and southern taiga, respectively. Intensity of mineralised carbon flux to the atmosphere is practically 90%, determined by phytodetritus decomposition. Between 68% (in southern taiga) and 87% (in forest tundra) of its emission is formed via litter decomposition. Root detritus contribution does not exceed 11-17%, while stem fall increases from forest tundra and northern taiga towards middle and southern taiga (from 2-3 to 14-17%).

The timing of extreme O2 and CO2 values during the diurnal cycle depends on the relative intensities of photosynthesis and organic matter destruction. The amplitude of the diurnal concentration variations of the studied components increases with increasing photosynthesis intensity and decreases with increasing organic matter consumption. Temperature variations, maxim of water masses and gas exchange with the atmosphere do not affect the timing of diurnal concentration maximums and minimums. Figure 11.

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Advances in the Geological Storage of Carbon Dioxide: International Approaches to Reduce Anthropogenic Greenhouse Gas Emissions by B.D. Belan, A.V. Fofonov, T.K. Sklyadneva, G.N. Tolmachev (auth.), S. Lombardi, L.K. Altunina, S.E. Beaubien (eds.)


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