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1.
Changes in the Earth's atmosphere are expected to influence the growth, and therefore, carbon accumulation of European forests. We identify three major changes: (1) a rise in carbon dioxide concentration, (2) climate change, resulting in higher temperatures and changes in precipitation and (3) a decrease in nitrogen deposition. We adjusted and applied the hydrological model Watbal, the soil model SMART2 and the vegetation model SUMO2 to asses the effect of expected changes in the period 1990 up to 2070 on the carbon accumulation in trees and soils of 166 European forest plots. The models were parameterized using measured soil and vegetation parameters and site-specific changes in temperature, precipitation and nitrogen deposition. The carbon dioxide concentration was assumed to rise uniformly across Europe. The results were compared to a reference scenario consisting of a constant CO 2 concentration and deposition scenario. The temperature and precipitation scenario was a repetition of the period between 1960 and 1990. All scenarios were compared to the reference scenario for biomass growth and carbon sequestration for both the soil and the trees. 相似文献
2.
Carbon (C) sequestration through plantations is one of the important mitigation measures for rising levels of carbon dioxide and other greenhouse gases in the atmosphere. This study aimed to assess C s... 相似文献
3.
Aboveground biomass and carbon stock in the largest sacred grove of Manipur was estimated for trees with diameter [10 cm at 1.37 m height.The aboveground biomass,carbon stock,tree density and basal area of the sacred grove ranged from 962.94 to 1130.79 Mg ha~(-1),481.47 to 565.40 Mg ha~(-1) C,1240 to 1320 stem ha~(-1) and79.43 to 90.64 m~2 ha~(-1),respectively.Trees in diameter class of 30–40 cm contributed the highest proportion of aboveground biomass(22.50–33.73%).The aboveground biomass and carbon stock in research area were higher than reported for many tropical and temperate forests,suggesting a role of spiritual forest conservation for carbon sink management. 相似文献
4.
A substantial portion of the carbon (C) fixed by the trees is allocated belowground to ectomycorrhizal (EM) symbionts, but this fraction usually declines after fertilization. The aim of the present study was to estimate the effect of optimal fertilization (including all the necessary nutrients) on the growth of EM fungi in young Norway spruce forests over a three year period. In addition, the amount of carbon sequestered by EM mycelia was estimated using a method based on the difference in δ 13C between C 3 and C 4 plants. Sand-filled ingrowth mesh bags were used to estimate EM growth, and similar bags amended with compost made from maize leaves (a C 4 plant) were used to estimate C sequestration. Fertilizers had been applied either every year or every second year since 2002 and the estimates of EM growth started in 2007. The application of fertilizer reduced EM growth to between 0% and 40% of the growth in the control plots at one site (Ebbegärde), while no significant effect was found at the other three sites studied. The effect of the fertilizer was similar in sand-filled and maize-compost-amended mesh bags, but the total production of EM fungi was 3-4 times higher in maize-compost-amended mesh bags. The fertilizer tended to reduce EM growth more when applied every year than when applied every second year. The amount of C sequestered in maize-compost-amended mesh bags collected from unfertilized treatments was estimated to be between 0.2 and 0.7 mg C g sand −1 at Ebbegärde and between 0.2 and 0.5 mg C g sand −1 at Grängshammar. This corresponds to between 300 and 1100 kg C per ha, assuming a similar production in the soil as in the mesh bags. Fertilization at the Ebbegärde site reduced carbon sequestration, which confirmed the results based on estimates of fungal growth (ergosterol levels). A correlation was found between fungal biomass and δ 13C in mesh bags amended with maize compost. Based on this, it was estimated that a fungal production of 1 μg ergosterol corresponded to 0.33 mg of sequestered carbon. In conclusion, the effect of the fertilizer on EM growth seemed to be dependent on the effect of the fertilizer on tree growth. Thus, at Ebbegärde, were tree growth was less stimulated by the fertilizer, EM growth was reduced upon fertilization. At other sites, where tree growth was more stimulated, the fertilizer did not influence EM growth. The large amounts of carbon sequestered during the experiment may be a result of fungal residues remaining in the soil after the death of the hyphae. 相似文献
5.
Carbon (C) sequestration was studied in managed boreal forest stands and in wood products under current and changing climate in Finland. The C flows were simulated with a gap-type forest model interfaced with a wood product model. Sites in the simulations represented medium fertile southern and northern Finland sites, and stands were pure Scots pine and Norway spruce stands or mixtures of silver and pubescent birch. Changing climate increased C sequestration clearly in northern Finland, but in southern Finland sequestration even decreased. Temperature is currently the major factor limiting tree growth in northern Finland. In southern Finland, the total average C balance over the 150 year period increased slightly in Scots pine stands and wood products, from 0.78 Mg C ha−1 per year to 0.84 Mg C ha−1 per year, while in birch stands and wood products the increase was larger, from 0.64 Mg C ha−1 per year to 0.92 Mg C ha−1 per year. In Norway spruce stands and wood products, the total average balance decreased substantially, from 0.96 Mg C ha−1 per year to 0.32 Mg C ha−1 per year. In northern Finland, the total average C balance of the 150 year period increased under changing climate, regardless of tree species: in Scots pine stands and wood products from 1.10 Mg C ha−1 per year to 1.42 Mg C ha−1 per year, in Norway spruce stands and wood products from 0.69 Mg C ha−1 per year to 0.99 Mg C ha−1 per year, and in birch stands and wood products from 0.43 Mg C ha−1 per year to 0.60 Mg C ha−1 per year. C sequestration in unmanaged stands was larger than in managed systems, regardless of climate. However, wood products should be included in C sequestration assessments since 12–55% of the total 45–214 Mg C ha−1 after 150 years' simulation was in products, depending on tree species, climate and location. The largest C flow from managed system back into the atmosphere was from litter, 36–47% of the total flow, from vegetation 22–32%, from soil organic matter 25–30%. Emissions from the production process and burning of discarded products were 1–6% of the total flow, and emissions from landfills less than 1%. 相似文献
6.
In this study, we present estimated ranges in carbon (C) sequestration per kg nitrogen (N) addition in above-ground biomass and in soil organic matter for forests and heathlands, based on: (i) empirical relations between spatial patterns of carbon uptake and influencing environmental factors including nitrogen deposition (forests only), (ii) 15N field experiments, (iii) long-term low-dose N fertilizer experiments and (iv) results from ecosystem models. The results of the various studies are in close agreement and show that above-ground accumulation of carbon in forests is generally within the range 15–40 kg C/kg N. For heathlands, a range of 5–15 kg C/kg N has been observed based on low-dose N fertilizer experiments. The uncertainty in C sequestration per kg N addition in soils is larger than for above-ground biomass and varies on average between 5 and 35 kg C/kg N for both forests and heathlands. All together these data indicate a total carbon sequestration range of 5–75 kg C/kg N deposition for forest and heathlands, with a most common range of 20–40 kg C/kg N. Results cannot be extrapolated to systems with very high N inputs, nor to other ecosystems, such as peatlands, where the impact of N is much more variable, and may range from C sequestration to C losses. 相似文献
7.
To better understand the effect of forest succession on carbon sequestration, we investigated carbon stock and allocation of evergreen broadleaf forest, a major zonal forest in subtropical China. We so... 相似文献
8.
Four forest stands each of twenty major forest types in sub-tropical to temperate zones (350 m asl–3100 m asl) of Garhwal Himalaya were studied. The aim of the study was to assess the stem density, tree diversity, biomass and carbon stocks in these forests and make recommendations for forest management based on priorities for biodiversity protection and carbon sequestration. Stem density ranged between 295 and 850 N ha −1, while total biomass ranged from 129 to 533 Mg ha −1. Total carbon storage ranged between 59 and 245 Mg ha −1. The range of Shannon–Wiener diversity index was between 0.28 and 1.75. Most of the conifer-dominated forest types had higher carbon storage than broadleaf-dominated forest types. Protecting conifer-dominated stands, especially those dominated by Abies pindrow and Cedrus deodara, would have the largest impact, per unit area, on reducing carbon emissions from deforestation. 相似文献
9.
Conservation of biodiversity and mitigation of global warming are two major environmental challenges today. In this context,
the relationship between biodiversity (especially plant diversity) and soil carbon (C) sequestration (as a means of mitigating
global warming) has become a subject of considerable scientific interest. This relationship was tested for homegardens (HG),
a popular and sustainable agroforestry system in the tropics, in Thrissur district, Kerala, India. The major objectives were
to examine how tree density and plant-stand characteristics of homegardens affect soil C sequestration. Soil samples were
collected at four depths (0–20, 20–50, 50–80, 80–100 cm) from HG of varying sizes and age classes, and their total C content
determined. Tree density and plant-stand characteristics such as species richness (Margalef Index) and diversity (Shannon
Index) of the HG were also determined. Results indicated that the soil C stock was directly related to plant diversity of
HG. Homegardens with higher, compared to those with lower, number of plant species, as well as higher species richness and
tree density had higher soil carbon, especially in the top 50 cm of soil. Overall, within 1 m profile, soil C content ranged
from 101.5 to 127.4 Mg ha −1. Smaller-sized HG (<0.4 ha) that had higher tree density and plant-species density had more soil C per unit area (119.3 Mg ha −1) of land than larger-sized ones (>0.4 ha) (108.2 Mg ha −1). Soil C content, especially below 50 cm, was higher in older gardens. The enhanced soil-C storage in species-rich homegardens
could have relevance and applications in broader ecological contexts.
相似文献
10.
Management implications associated with two different silvicultural strategies in two Spanish pine forests (Scots pine stands
in northern Spain and Mediterranean Maritime pine stands in Central Spain) were explored. Whole-stand yield, growth models
and individual tree equations were used to estimate carbon stock in forests under different silvicultural alternatives and
site indexes. Each alternative was evaluated on the basis of the land expectation value (LEV). Results reveal the appropriateness
of implementing carbon payments, because it can clearly complement traditional management objectives in economic terms. Longer
rotations on the poorest sites result in a positive economic return by introducing carbon output. The proportion of carbon
stock in the final harvest relative to total fixed carbon is always higher in long rotation scenarios. However, short rotation
systems produce the highest values of carbon MAI regardless of site index. The impact of carbon price is higher on the Maritime
pine stands than on Scots pine stands. For both the species, changes in the discount rate have a minor impact on Carbon LEV.
Notwithstanding, the proportion of total LEV due to carbon is greater when the discount rate increases. 相似文献
11.
Secondary forests are a major terrestrial carbon sink and reliable estimates of their carbon stocks are pivotal for understanding the global carbon balance and initiatives to mitigate CO 2 emissions through forest management and reforestation. A common method to quantify carbon stocks in forests is the use of allometric regression models to convert forest inventory data to estimates of aboveground biomass (AGB). The use of allometric models implies decisions on the selection of extant models or the development of a local model, the predictor variables included in the selected model, and the number of trees and species for destructive biomass measurements. We assess uncertainties associated with these decisions using data from 94 secondary forest plots in central Panama and 244 harvested trees belonging to 26 locally abundant species. AGB estimates from species-specific models were used to assess relative errors of estimates from multispecies models. To reduce uncertainty in the estimation of plot AGB, including wood specific gravity (WSG) in the model was more important than the number of trees used for model fitting. However, decreasing the number of trees increased uncertainty of landscape-level AGB estimates substantially, while including WSG had limited effects on the accuracy of the landscape-level estimates. Predictions of stand and landscape AGB varied strongly among models, making model choice an important source of uncertainty. Local models provided more accurate AGB estimates than foreign models, but high variability in carbon stocks across the landscape implies that developing local models is only justified when landscape sampling is sufficiently intensive. 相似文献
12.
We evaluated carbon stocks in the above-ground biomass (AGB) of three dominant mangrove species ( Sonneratia apetala, Avicennia alba and Excoecaria agallocha) in the Indian Sundarbans. We examined whether these carbon stocks vary with spatial locations (western region vs. central region) and with seasons (pre-monsoon, monsoon and post-monsoon). Among the three studied species, S. apetala showed the maximum above-ground carbon storage (t ha −1) followed by A. alba (t ha −1) and E. agallocha (t ha −1). The above-ground biomass (AGB) varied significantly with spatial locations ( p < 0.05) but not with seasons ( p < 0.05). The variation may be attributed to different environmental conditions to which these areas are exposed to such as higher siltation and salinity in central region compared to western region. The relatively higher salinity in central region caused subsequent lowering of biomass and stored carbon of the selected species. 相似文献
13.
In this work the aim was to determine how carbon sequestration in the growing stock of trees in Finland is dependent on the
forest management and increased production potential due to climate change. This was analysed for the period 2003–2053 using
forest inventory data and the forestry model MELA. Four combinations of two climate change and two management scenarios were
studied: current (CU) and gradually warming (CC) climate and forest management strategies corresponding to different rates
of utilisation of the cutting potential, namely maximum sustainable removal (Sust) or maximum net present value (NPV) of wood
production (Max). In this analysis of Finland, the initial amount of carbon in the growing stock was 765 Mt (2,802 Tg CO 2). At the end of the simulation, the carbon in the growing stock of trees in Finland had increased to 894 Mt (3,275 Tg CO 2) under CUSust, 906 Mt (3,321 Tg CO 2) under CUMax, 1,060 Mt (3,885 Tg CO 2) under CCSust and 1,026 Mt (3,758 Tg CO 2) under CCMax. The results show that future development of carbon in the growing stock is not only dependent on climate change
scenarios but also on forest management. For example, maximising the NPV of wood production without sustainability constraints
results, over the short term, in a large amount of wood obtained in regeneration cuttings and a consequent decrease in the
amount of carbon in growing stock. Over the longer term, this decrease in the carbon of growing stock in regenerated forests
is compensated by the subsequent increase in fast-growing young forests. By comparison, no drastic short-term decrease in
carbon stock was found in the Sust scenarios; only minor decreases were observed. 相似文献
15.
This study examines the economic and spatial impacts of afforestation choices for carbon sequestration in Ontario, Canada when the non-permanence of forestry carbon offsets is taken into consideration. We test six scenarios including three long-term projects with red pine, Norway spruce and hybrid poplar plantations and three shorter term hybrid poplar scenarios that produce temporary carbon emission offsets. We convert the break-even costs of sequestering carbon to a permanent carbon offset equivalent and analyze the possible geographical implications of the choices across eastern, southern and central Ontario, Canada.The most financially viable scenarios show a relatively large part of central Ontario with attractive choices at a 4% discount rate but a much smaller area at an 8% rate. The assumption about the future price evolution of temporary carbon offsets is one of the biggest factors that influence the attractiveness of these choices. At the 4% discount rate and the assumption of rising prices of permanent carbon offsets, the scenarios that store carbon for long periods appear to be the least-costly option. Hybrid poplar appears as the best choice in southern Ontario and a mix of conifer species and hybrid poplar in the central and northern parts. When future prices of temporary carbon offsets are assumed to decline, temporary hybrid poplar projects appear to be more attractive in the southern and eastern parts of the province. The variety of alternative scenario choices also depends on the discount rate and future price expectations for temporary carbon offsets. For a relatively narrow deviation of the carbon offset price (±$0.6 t -1 CO 2), only 4% to 9.2% of the total 5.8 million ha area would have one or more potentially viable alternative scenarios at the 4% discount rate and almost zero alternatives at the 8% rate. Higher discount rates lead to fewer attractive choices, suggesting that landowners would be left with very few options when trying to maximize net returns from plantations. 相似文献
16.
This study considers a carbon tax system as a policy tool for encouraging carbon sequestration through modification of management in existing forests and examines its welfare impacts and costs of the carbon sequestered. The simulated carbon tax leads to reduced harvest and increased carbon stock in the standing trees and understory biomass. Changes in the level of silvicultural investments vary by owner, depending on the nature of their initial inventory. In general investment under the tax is concentrated in regimes that establish faster growing plantations. Average rotation age increases, varying in extent across ownerships and site qualities. The carbon tax reduces both consumer and producer surpluses in regional timber markets. Producers are compensated by the carbon subsidies, except at low carbon tax levels. Not all rates of carbon tax will attract interest from private owners if participation is voluntary. Estimates of the marginal cost of sequestering carbon in western Oregon private forests are shown to be within the range of costs for projects considering afforestation alone in some eastern regions of the United States. 相似文献
17.
Bamboo forest is an important forest type in subtropical China and is characterized by fast growth and high carbon sequestration capacity. However, the dynamics of carbon fluxes during the fast growing period of bamboo shoots and their correlation with environment factors are poorly understood. We measured carbon dioxide exchange and climate variables using open-path eddy covariance methods during the 2011 growing season in a Moso bamboo forest(MB, Phyllostchys edulis) and a Lei bamboo forest(LB, Phyllostachys violascens) in Zhejiang province,China. The bamboo forests were carbon sinks during the growing season. The minimum diurnal net ecosystem exchange(NEE) at MB and LB sites were-0.64 and-0.66 mg C m -2 s -1, respectively. The minimum monthly NEE, ecosystem respiration(RE), and gross ecosystem exchange(GEE) were-99.3 ± 4.03, 76.2 ±2.46, and -191.5 ± 4.98 g C m -2 month -1, respectively,at MB site, compared with-31.8 ± 3.44, 70.4 ± 1.41,and -157.9 ± 4.86 g C m -2 month -1, respectively, at LB site. Maximum RE was 92.1 ± 1.32 g C m -2 month -1 at MB site and 151.0 ± 2.38 g C m -2 month -1 at LB site.Key control factors varied by month during the growing season, but across the whole growing season, NEE and GEE at both sites showed similar trends in sensitivities to photosynthetic active radiation and vapor pressure deficit,and air temperature had the strongest correlation with RE at both sites. Carbon fluxes at LB site were more sensitive to soil water content compared to those at MB site. Both onyear(years when many new shoots are produced) and offyear(years when none or few new shoots are produced)should be studied in bamboo forests to better understand their role in global carbon cycling. 相似文献
18.
The carbon sequestration potential in living biomass and soil organic matter under the Grain for Green Program (GGP) in Yunnan Province, one of the most important target provinces of the GGP in China, was estimated in this paper using empirical curves and factors. The area of tree species planted during 2000–2007 was collected, and four scenarios for the annual area of GGP-stands to be planted during 2008–2010 and harvest options were schemed. Empirical growth curves for different tree species were developed based on data about the growth of existing plantation in Yunnan Province from National Forestry Inventory, and were used for the estimation of the carbon stocks in the tree biomass pools by incorporating with basic wood density, biomass expansion factors and carbon fraction. Empirical factors were introduced to estimate the stock change in soil organic carbon (SOC) under the GGP. The results show that the carbon stock in the GGP-stands in Yunnan Province will increase by 12.474–12.608 TgC, 33.016–35.161 TgC, 38.119–47.100 TgC, 43.057–53.626 TgC and 49.918–56.621 by the year 2010, 2020, 2030, 2040 and 2050, respectively. The annual carbon stock change in the GGP-stands will peak at 2.342–2.536 TgC per year in 2013, followed by a gradual decrease. The estimated potential carbon sequestration by GGP-stands amounts to 10.82–12.27% of the carbon stocks of forest ecosystems in Yunnan province in the 1990s. 相似文献
19.
We compare uncertainty through sensitivity and uncertainty analyses of the modelling framework CO2FIX V.2. We apply the analyses to a Central European managed Norway spruce stand and a secondary tropical forest in Central America. Based on literature and experience we use three standard groups to express uncertainty in the input parameters: 5%, 10% and 20%. Sensitivity analyses show that parameters exhibiting highest influence on carbon sequestration are carbon content, wood density and current annual increment of stems. Three main conclusions arise from this investigation: (1) parameters that largely determine model output are stem parameters, (2) depending on initial state of the model, perturbation can lead to multiple equilibrium, and (3) the standard deviation of total carbon stock is double in the tropical secondary forest for the wood density, and current annual increment. The standard deviation caused by uncertainty in mortality rate is more than 10-fold in the tropical forest case than in the temperate managed forest. Even in a case with good access to data, the uncertainty remains very high, much higher than what can reasonably be achieved in carbon sequestration through changes in forest management. 相似文献
20.
Wood products are considered to contribute to the mitigation of carbon dioxide emissions. A critical gap in the life cycle
of wood products is to transfer the raw timber from the forest to the processing wood industry and, thus, the primary wood
products. Therefore, often rough estimates are used for this step to obtain total forestry carbon balances. The objectives
of this study were (1) to examine the fate of timber harvested in Thuringian state forests (central Germany), representing
a large, intensively managed forested region, and (2) to quantify carbon stocks and the lifetime of primary wood products
made from this timber. The analyses were based on the amount and assortments of actually sold timber, and production parameters
of the companies that bought and processed this timber. In addition, for coniferous stands of a selected Thuringian forest
district, we calculated potential effects of management, as expressed by different thinning regimes on wood products and their
lifetimes. Total annual timber sale of soft- and hardwoods from Thuringian state forests (195,000 ha) increased from about
136,893 t C (~0.7 t C ha −1 year −1) in 1996 to 280,194 t C (~1.4 t C ha −1 year −1) in 2005. About 47% of annual total timber harvest went into short-lived wood products with a mean residence time (MRT) < 25
years. Thirty-one per cent of the total harvest went into wood products with an MRT of 25–43 years, and only 22% was used
as construction wood and glued wood, products with the longest MRT (50 years). The average MRT of carbon in harvested wood
products was 20 years. Thinning from above throughout the rotation of spruce forests would lead to an average MRT in harvested
wood products of about 23 years, thinning from below of about 18 years. A comparison of our calculations with estimates that
resulted from the products module of the CO2FIX model (Nabuurs et al. 2001) demonstrates the influence of regional differences in forest management and wood processing industry on the lifetime of
harvested wood products. To our knowledge, the present study provides for the first time real carbon inputs of a defined forest
management unit to the wood product sector by linking data on raw timber production, timber sales and wood processing. With
this new approach and using this data, it should be possible to substantially improve the net-carbon balance of the entire
forestry sector. 相似文献
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