|
|
Carbon sequestration by forest ecosystems in canging climate.
Hlaváčková, Lucie ; Lhotáková, Zuzana (advisor) ; Urban, Otmar (referee)
The global carbon cycle is in the focus of the scientists' interest, because understanding carbon sinks and their relationships can show the solutions of problems related with increasing CO2 concentration in the atmosphere in the future. I focused on the role of forests ecosystems in this carbon cycle. All forests cover almost one third of the Earth's land area. By photosynthesis they bind big part of atmospheric carbon to their biomass. Sink strength of forest can differ according to the type of biome, forest stand age and actual climatic conditions. Forest biomes can be generally divided according to the latitude to three groups: tropical forest biomes, temperate forests and boreal forests. The size of carbon stock decreases in this order. Other parameters, such as net primary production and respiration differ in dependence on the particular ecosystem. Tropical rain forests represent great carbon stock, but their deforestation causes massive C emissions back to the atmosphere. Boreal forests aren't considered as important carbon sink, but they influence local climate. Some speculations can also appear about the old forests. It is possible to find authors, who claims, that old forests are no more carbon sinks, so that their carbon balance is neutral. Many surveys prove that they bind less carbon...
|
|
|
The effect of tree species on soil properties
Hüblová, Lucie ; Frouz, Jan (advisor) ; Veselá, Hana (referee)
Soil quality and its ability to support plant growth and soil organisms is affected by the content of soil organic carbon which can also influence many soil properties. The biggest terrestrial reservoirs of carbon (C) are forests. The amount of C sequestered in soil depends on quantity and quality of organic matter returned to forest floor as leaf litter. For how long and how effectively the C will be stored in soil is largely dependent on the rate of decomposition of organic matter and stabilization mechanisms. In this work I compared data from 40 "common garden" experiments in which different tree species were planted in adjacent plots on homogenous soil. C storage was compared on three types of afforested soils with different previous land use. Forests and former arable soils represented the well- developed soils in late stages of pedogenesis. Post-mining sites represented soils where pedogenesis was in the initial state. I found out that soil age is the controlling factor of carbon sequestration. In well-developed soils more C was stored under conifers. In initial soils on post mining sites on the other hand more C was stored under broadleaves. A negative correlation between sequestered C and C:N ratio in leaf litter was found on post mining sites. The results suggest that different mechanisms...
|
|
|
The importance of mycorrhizal fungi in the root decomposition.
Haiclová, Klára ; Kohout, Petr (advisor) ; Kolaříková, Zuzana (referee)
Mycorrhizal fungi are known as symbionts of many plant species. Fungi provide better access to mineral nutrients and water for host plants, and in return fungi receive carbohydrates from plants. Although a significant proportion of organic matter is bound in the root biomass, little is known about the factors affecting root decomposition. Understanding the process of root decomposition and the factors that affect it, is important to us. Knowledge of root decomposition helps us understand the carbon cycle and answer questions about carbon sequestration in soil. This Bachelor's thesis is focused on the importance and function of mycorrhizal fungi during root decomposition. It describes the influence of mycorrhizal fungi on the decomposition of fine roots colonized by mycorrhizae, the ability of mycorrhizal fungi to decompose organic matter and influence the decomposition rate through competition with saprotrophic organisms. Keywords: mycorrhizal fungi, roots, decomposition, rate, organic matter, soil, importance, carbon sequestration
|
|
|
Carbon sequestration and carbon stock in forest soils
Flašarová, Kristýna ; Chuman, Tomáš (advisor) ; Strouhalová, Barbora (referee)
Carbon sequestration is one of the most important processes in the soil. There is three times more carbon in soil than in the atmosphere, significant part of this soil carbon is deposited in the forest soils of North America, Europe and Asia. Soil, compared with biomass, is able to store carbon for a long time and protect it from decomposition and release back to the air. Carbon sequestration and its stock in soil are influenced by many factors (climate, bedrock, biological activity, relief and land use). Forest soils contain large amount of carbon and with adequate management and tree species composition is possible to increase final amount of soil carbon. This thesis is about, besides other things, measuring soil carbon in different depths and comparing the final results in total amount of carbon in soil. Practical part compare amount of carbon in forest soils of two main tree species in Czech mountain forests: beech and spruce, where the largest amount of soil carbon is stored in the Czech Republic.
|
|
|
Carbon sequestration by forest ecosystems in canging climate.
Hlaváčková, Lucie ; Lhotáková, Zuzana (advisor) ; Urban, Otmar (referee)
The global carbon cycle is in the focus of the scientists' interest, because understanding carbon sinks and their relationships can show the solutions of problems related with increasing CO2 concentration in the atmosphere in the future. I focused on the role of forests ecosystems in this carbon cycle. All forests cover almost one third of the Earth's land area. By photosynthesis they bind big part of atmospheric carbon to their biomass. Sink strength of forest can differ according to the type of biome, forest stand age and actual climatic conditions. Forest biomes can be generally divided according to the latitude to three groups: tropical forest biomes, temperate forests and boreal forests. The size of carbon stock decreases in this order. Other parameters, such as net primary production and respiration differ in dependence on the particular ecosystem. Tropical rain forests represent great carbon stock, but their deforestation causes massive C emissions back to the atmosphere. Boreal forests aren't considered as important carbon sink, but they influence local climate. Some speculations can also appear about the old forests. It is possible to find authors, who claims, that old forests are no more carbon sinks, so that their carbon balance is neutral. Many surveys prove that they bind less carbon...
|
|
| |
|
|
Modelling of ecosystem service change
Cudlín, Pavel ; Pechanec, V. ; Purkyt, Jan ; Jakubínský, Jiří ; Štěrbová, Lenka ; Cudlín, Ondřej ; Plch, Radek ; Seják, J. ; Včeláková, Renata ; Brom, J.
Submitted report introduced results obtained by researchers from the Institute of Global Change Research and the Department of Geoinformatics of University Palacký in Olomouc. From all activities the following activities are the most important: Habitat mapping of agricultural and non-agricultural plots in the Kopanický stream catchment according to Seják at al. (2003) a Seják at al. (2010); Computation of the indicators of landscape fragmentation and ecological stability for Kopanický stream catchment; Valuation of land use change from the point of view of the optimalization of the selected ecosystem functions performance and selected provisioning and regulating ecosystem service provision, including financial valuation; and Valuation of functional land use from point of views territorial planning of small villages and environmental demands to landscape.
|
|
|
The influence of land cover changes and landscape fragmentation on provision of the carbon sequestration ecosystem service
Pechanec, V. ; Purkyt, Jan ; Cudlín, Pavel
The aim of our contribution is to analyse the influence of land cover changes and landscape fragmentation in two small catchments (Všeminka, Fryštácký potok) within the forest–agricultural landscape of eastern Moravia (Czech Republic) on the carbon sequestration ecosystem service. Fragmentation was analysed using landscapeecological indices within ArcGIS 10.x software using the Patch Analyst extension. Data about the carbon sequestration ecosystem service were processed in the InVEST model. In the Všeminka catchment, carbon sequestration increased over the entire period of observation of 1953–2012. In the Fryštácký potok catchment, carbon sequestration decreased from 1950 to 2005, but increased from 2005 to 2012. The changes in fragmentation were not significant between 1953 and 2012, and so changes in carbon sequestration were caused mostly by land cover changes. The relationships among land cover change, fragmentation, and carbon sequestration from 1953 to 2012 are discussed.
|
guest ::
